`IEO`Op @@@ @@@@d^lO EN DB OP )-FP[k G[CollinsRCollins, B. L. 1954. Lista de peixes dos mares dos Aores. Aoreana, II (5), 1-40.[ Fredericq19929> Gorsky19999Le Grand1981K McCartney1993JO Nelson19939i Quro1980x Silva1987aR Vereshchaka1996a@ Vereshchaka1996 Vereshchaka1997 Vereshchaka19972 Vereshchaka1997 Vereshchaka1999 Vereshchaka19993 Vereshchaka1999  Vereshchaka2000C Vereshchaka2000# Verity1993 Verity19933 Villanueva1998 Villanueva1998 VINNICHENKO1979o VINNICHENKO1994 VINNICHENKO1994 VINNICHENKO1995 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1997 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1999 VINNICHENKO1999 VINNICHENKO1999 VINNICHENKO2000  VINNICHENKO2001  VINNICHENKO2001  VINNICHENKO2002G VINNICHENKO.1998 VINNICHENKO.19984 Vinogradov19616 Vinogradov19687 Vinogradov1989< Vinogradov1991 Vinogradov19928 Vinogradov1992 Vinogradov1995; Vinogradov19955 Vinogradov1996@ Vinogradov1996 Vinogradov1997? 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Wells19953 Wells1999 Wheeler1978@ Wheeler1992 White1966 Whitehead1989Whitmore1989Q Widder1997 Widder19970 Widder19988 Widder1999) Widder20011 Widder2002H Wiebe1979 Wiebe1994 Wiebe1994 Wiebe2000S Wilken19921Williams1992Williams19979Williams2001I Williamson1996> Wilson19989A Wirtz1993K Wishner1980P Wishner1984 Wishner1987 Wishner1990 Wishner19929 Wishner1993 Wishner1993} Wishner1995d Wishner1997e Wishner1997| Wishner2000L Wishner2000Q Wohlleben1995 Woodd-Walker2001 Woods1957R Wroblewski1982 YAROVOY1988 YAROVOY1989 YAROVOY1991 Youngbluth1995 ZAFERMAN1977ZAFERMAN1986ZAFERMAN1986ZAFERMAN1987BZaferman1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1996ZAFERMAN1997l ZAFERMAN.1982ZAKHAROV19911 Zeitzschel2002 Zeltner2000 ZEZINA1985 Ziemann1991 ZILANOV1969 ZILANOV1970 ZILANOV1975 Zonfrillo 1989 ZUBCHENKO1975 ZUBCHENKO1976 ZUBCHENKO1978 ZUBCHENKO1978 ZUBCHENKO1979  ZUBCHENKO1981! ZUBCHENKO1981" ZUBCHENKO1981# ZUBCHENKO1984$ ZUBCHENKO1985% ZUBCHENKO19877 Zubchenko.1984 Zuev1971  Zuev1975  Zuev1975  Zuev1975  Zuev1976  Zuev1977 ZYKOV.198387 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838977 ZYKOV.198387 ZYKOV.19838 ZYKOV.19838 ZYKOV.19838chaka19993 Vereshchaka1999  Vereshchaka2000C Vereshchaka2000# Verity1993  Verity19933 Villanueva1998 Villanueva1998 VINNICHENKO1979o VINNICHENKO1994 VINNICHENKO1994 VINNICHENKO1995 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1996 VINNICHENKO1997 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1998 VINNICHENKO1999 VINNICHENKO1999 VINNICHENKO1999 VINNICHENKO2000  VINNICHENKO2001  VINNICHENKO2001  VINNICHENKO2002G VINNICHENKO.1998́ VINNICHENKO.19984 Vinogradov19616 Vinogradov19687 Vinogradov1989< Vinogradov1991 Vinogradov19928 Vinogradov1992 Vinogradov1995; Vinogradov19955 Vinogradov1996@ Vinogradov1996 Vinogradov1997? Vinogradov1997 Vinogradov1998= Vinogradov1998 Vinogradov19999 Vinogradov1999 Vinogradov19993 Vinogradov19999> Vinogradov1999  Vinogradov2000  Vinogradov20000 Vinogradov2000: Vinogradov2000C Vinogradov2000C Vinogradov200009 Vinogradov2002  VINOGRADOVA1990S Vonsteiger1992 Voss1998:Vostokov20000  Wade2001E Wade2001F Wakefield1990+ Waldron1998H Waldron1999 Walne2001 Walne2001 Walsh1987 Walsh1987 Walsh1988a Walsh1988F Walsh19922 Walters1997  Waniek20000 Ward19921 Warner19944 Warner1995 Warner1997 Warner2001 Warner2001G Warren1981̤ Watts1993Q Weaver19959 Weeks1995 Weeks1995= Weeks1995> Weerdt1989 Weikert1992 Weikert1999- Weikert1999 Weikert1999 Weikert1999( Weikert2001 Weikert2001S Weiss1992? Wells19953 Wells1999 Wheeler1978@ Wheeler1992 White1966 Whitehead1989Whitmore1989̛Whitmore1989Q Widder1997̹ Widder19970 Widder19988 Widder1999) Widder20011 Widder2002H Wiebe1979 Wiebe1994 Wiebe1994 Wiebe2000S Wilken19921Williams1992Williams19979Williams2001I Williamson1996> Wilson19989A Wirtz1993K Wishner1980P Wishner1984 Wishner1987 Wishner1990 Wishner19929 Wishner1993 Wishner1993} Wishner1995d Wishner1997e Wishner1997| Wishner2000L Wishner2000Q Wohlleben1995 Woodd-Walker2001 Woods1957R Wroblewski1982 YAROVOY1988 YAROVOY1989 YAROVOY1991 Youngbluth1995 ZAFERMAN1977ZAFERMAN1986ZAFERMAN1986ZAFERMAN1987BZaferman1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1991ZAFERMAN1996ZAFERMAN1997l ZAFERMAN.1982ZAKHAROV19911 Zeitzschel2002  Zeltner2000 ZEZINA1985̷ Ziemann1991 ZILANOV1969 ZILANOV1970 ZILANOV1975 Zonfrillo 1989̠ Zonfrillo 1989 ZUBCHENKO1975 ZUBCHENKO1976 ZUBCHENKO1978 ZUBCHENKO1978 ZUBCHENKO1979  ZUBCHENKO1981! ZUBCHENKO1981" ZUBCHENKO1981# ZUBCHENKO1984$ ZUBCHENKO1985% ZUBCHENKO19877 Zubchenko.1984 Zuev1971  Zuev1975  Zuev1975  Zuev1975  Zuev1976  Zuev1977 ZYKOV.19838c>!BgN,iIed2(7Yf"l#5j/Do<; 0v_3UV@H&n`4bp: AO$+WL8SCh^qT *Mr|}XRZ?~saQ'.w6%xzK]{ Authorsy Journals Keywords m                               O 1X(Eds.), A. F. Martins, Furness, R.W , Houston_DC-. 1985., ANON.a, M. Biscoito in pressAores/89, ExpedioAGAFONOVA, T. B. Agostinho, J. Aguiar, A. Aken, H. M.Aken, H. M. van Akers, P. Aksnes, D. L. Aksness, D.L Alayse, A.-M.ALEKSEEV, F. E.ALEKSEEV, G. V.ALEKSEEVA, A. G.ALEKSEEVA, E. I. Allen, L. D. Alves, M Alves, M.Amelekhina, A.M. Anadon, R Andersen, V Andersen, V.Andrade, J. P. Angel, M. V. Angel, M.V Angel, M.V. ANIKEEV, V.Anokhina, L. L.ANONANON. Antoine, E. Arhan, M.Arkhipkin, A.I.Arnautov, G. N. Arnbom, T. Arruda, L. M.Ashjian, C. J. Asper, V. L. Asper, V.LAstthorson, O.SAstthorsson, O. S.Astthorsson, O.S Atkinson, A. Avery, M. I.Azevedo, J. M.Azevedo, J. M. N.Azevedo, J. N. Baber, I. Backus, R. H. Bacon, S. Baddock, J.BAIDALINOV, A. P. Bainbridge, R BAKAY, Yu. I. BAKAY, Yu.I.BAKAY., Yu. I. Baker, A, CBALABANOVA, L. G.Baldwin, R. J.Balguerias, E. Balsiger, H.Bannerman, D. A.Bannerman, W. M.BARANOV, E. I. Barbier, G. Bard, F. X.BARINOV, A. A.Barraca, I. F.Barreiros, J. P. Barriga, F. Barrois, Th. Barros, M. C.Barthelemy, R. Bass, A. L.Batchelder, H. P. Batiza, R Batiza, R. Batten, S. D.Bauchot, M.-L. Baumann, K-H Baxter, C. Bean, T. H. Beare, D. J. Bearhop_S Becker Becker, G Beckman, W Beckmann, W Beckmann, W. Bedini, P. Bedo, A. Beer, J. Bell, M. V.Bellan-Santini, D.$Berenboim, B.I., Boytsov, V.D.Bernstein, S. A. Bersch, MBersch, M., J. Meincke Bertelsen, E. Bethoux, N. Bett, B.J. Bianchi, A. Bianchi, M Bianchi, M. Bibby, C. J.Bidigare, R. R. Bieler, R.Bienfang, P. K. Biscoito, M.Bitukov, E. P.Bjorndal, K. A. Blackburn, M.BLAZHCHIKHIN, A. I. Blindheim, J Blindheim, J.BLIZNICHENKO, T. E.Bliznichenko, T.EBodvarsdottir, A. R.Bodvarsdottir, A.RBoehlert, G.W. Boer de, C.JBoer, C. J. DeBOGDANOV, S. J.BOGDANOV, Yu. A.BOGOROV, G. V.BOGOVSKI, S.P.BOGOVSKY, S. P.Bollens, S. M. Bollens, S.MBoltachev, A.R. Bolten, A. B. Bolton, MBONDAREV, V. V.Borodin, N. A. Bouchet, P. Bourdillon, ABourdillon, A. Bowen, B. W. Bower, A. S. Boyd, P Boyd, P. Boyle, P. R. Boytsov, V.DBrechner Owens, W Briand, P. Brickle, P. Briggs, J. C. Brink, K.H. Brito, A.Brulport, J.-P. Brum, J. M.Brum, J. M. M. Bryan, KBuchanan, J. Y. Bucklin, A.Buhring, S. I.Bulgakova, Y. V. Burnay, L. P. Burns, M.DBURUKOVSKY, R. N. Bhring, S.IC., Heemstra P. Cain, J. C.Campbell, R. W. Campbell, R.WCapello, F. de B. Carlin, J. L.Carretas, J. P. Cartaxana, A. Carvalho, D. Cascalho, A. Case, J. F. Castillo, R.Castle, P. H. J.Chapman, R. W. Chaves, A. F. Chavigny, J. Chen, E. H.CHERNYAVSKY, E. B.Christiaens, J.Christiansen, BChristiansen, B.CHUKSIN, Yu. V.CHUMAKOV, A. K. Clark, C. W. Clark, D. R. Clark, D.R Clarke, D. C. Clarke, M. Clarke, M. R. Clarke, R. Cocco, M. Cohen, R.E Colaco, A. Collett, R.Collins, B. L. Comtet, T.Copley, J. T. P. Cordeiro, P.Cordell, J. R. Corlett, J. Cornec, L.Cornelius, P. F. S. Costa, V Costa, V. Coutis, P. F.  5 "Meteor" Forschungsergebnisse Meteor Forschungsergebnisse(not published)(unpublished manuscript)$!18-a Semana das Pescas dos Acores 272 pages46A Pesca MartimaAbstract of Doctor Thesis Abstract of the Doctor ThesiszAbstracts of Communications of 4th All-USSR Scientific Conference on Problems of Fisheries Forecasting (Long-Term Aspects)pjAbstracts of Communications of 7th All-USSR Conference on Fisheries Oceanology, Astrakhan, 19-21 May, 1987Abstracts of Communications on III Scientific-Practical Conference of the Crimea "Young Scientists' and Specialists' Contribution to the Decision of the Modern Problems of Oceanology and Hydrobiology", SevastopolD?Abstracts of Scientific Papers of ICES 1990 Shellfish Symposium`]Abstracts of the All-Union Conference on studies of fishes of the World Ocean thalassobathyalHDAbundance and habits of commercial fishes of the North-West Atlantic Aoreana Aoreana (Suplemento 1992) AorenatnAdvanced industrial experience and scientific and technical achievements recommended for introduction. Moscow Advances in Marine Biology AlaudapmAll-USSR Scientific Conference on the Use of Commercial Invertebrates for Food, Fodder and Technical Purposes American Naturalist Am. Nat.An anotated bibliography($Anais do Clube Militar Naval, Lisboa<7Anais do Instituto de Zoologia da Universidade do Porto Anim. BehavAnimal Behaviour Annales BiolAnnales Biologiques@:Annales De L Institut Oceanographique Ann. Inst. Oceanogr.41Annales de la Socit Linnenne de Maine et Loire$Annales Intitut OceanographiqueD>Annalles de la Socit Science Naturelles de Charente-Maritime,&Annals and Magazine of Natural History Annals. Biolog. (1968) 25Annals. Biolog. (1969)D?Annual Review of Ecology and Systematics Annu. Rev. Ecol. Syst.$Arch. Environ. Contam. Toxicol,(Archiv for Mathematik og Naturvidensksab$ Archiv fr Fischereiwissenschaft$Archiv fr Fishereiwissenschaft,'Archiv fr Mathematik og Naturvidenskab84Archives of Environment, Contaminants and Toxicology<6Archives of Environmental Contamination and Toxicology Arquiplago,&Arquiplago - Life and Marine Sciences(%Arquiplago, Life and Marine Sciences,'Arquiplago. Srie Cincias da NaturezaArquivos do DOP$ Arquivos do DOP, Srie CruzeirosArquivos do Museu Bocage  t m 14/C-12 1st antennae20- 26-degrees-n 29-degrees-n3-spined sticklebacks 47-degrees-n76abaco abandoned larvacean houses abundance abyssal-plain Acanthurus acartia-tonsa adaptations adaptiveadaptive significance advantage advectionage aggregatesalgal carotenoids algorithmsalvinocarididae amphipod anatomy animals anomaliesantarctic copepods antarctic intermediate water Aphotopontius arabian seaareas artificial satellites space assemblages assimilation atlanticAtlantic Ocean atlantic-atlantic-ocean atmosphere avoidance azores frontazores triple-junction bacteriabacterioplankton balsfjorden barbados barents sea barophilebasin bathymetricbay behaviorbehavioral sensitivitybehavioural ecologybenthic boundary layerbenthic boundary-layerBENTHIC BOUNDARY-LAYER, CENTRAL RED-SEA, COLD-CORE EDDY, DEEP-SEA, BENTHOPELAGIC PLANKTON, VERTICAL-DISTRIBUTION, EPIBENTHIC SLEDGE, OPEN OCEAN, MID-WATER, COMMUNITYľBENTHIC BOUNDARY-LAYER, HYPERBENTHIC MYSIDS CRUSTACEA, NORTHEAST ATLANTIC-OCEAN, WESTERN INDIAN-OCEAN, DEEP-SEA, VERTICAL-DISTRIBUTION, BENTHOPELAGIC PLANKTON, BIOMASS, ZOOPLANKTON, ZONATIONbenthic macrofaunabenthopelagic plankton biodiversitybiogenic particle fluxesBIOGENIC PARTICLE FLUXES, BENTHIC BOUNDARY-LAYER, SPATIAL VARIABILITY, OXYGEN-CONSUMPTION, NORTH-ATLANTIC, SEDIMENT TRAP, INSITU RATES, PHOTOGRAPHIC EVIDENCE, CALANUS-FINMARCHICUS, MARINE PHYTOPLANKTON Biogeographybiological investigations biology biomass black-seabloombloom experiment boundary-layer zooplankton Brazilbresiliid shrimps bresiliidaebritish-columbiaC-c-14c-helgolandicus cal bp calanoidcalanoid copepodscalanoides-acutus calanusCalanus finmarchicusD>Calanus finmarchicus, reproduction, spring bloom, Labrador seacalanus pacificus calanus-calanus-finmarchicuscalanus-pacificuscalanus-propinquus calibration california canary cape-hatteras capelin carbon carbon fluxtqcarbonate dissolution, deep-water formation, Norwegian-Greenland Sea, North Atlantic, Northern Hemisphere climate carcass Caribbean carideancaridean shrimp carotenoid catalogs celtic seacentral Atlanticcentral north pacific  K]%:DUz .~',"l$(*e78+&6O!ST0 >NNNNNN,,,ii27####555/////DDDv_33n`44444444>!!NNN,Iee222777YYY####///DDDDDDooo<000000vvv_____33V444bAAA$$$$WWLLLLLL888888888CCCCCC tE gelatinous zooplankton gene flow generalgeneral-circulationgeneral-circulation modelgenetic-variabilitygenusGeographical distributionglacial maximum glacialis glucosegonad development gravity- grazinggreenhouse-effect greenland-sea growthgulf Gulf Streamgulf- gulf-streamgulf-stream meanders gut clearancegut fluorescenceguyothawaiian ridgeheat helgolandicus heterogeneity history holoplanktonhoplostethus-atlanticushplchuman population growth hydrographyhydrostatic pressurehydrothermal activityhydrothermal plume|wHYDROTHERMAL PLUME, ENDEAVOR RIDGE, SCATTERING LAYER, ZOOPLANKTON, MACROPLANKTON, SEA, 29-DEGREES-N, COMMUNITIES, OCEANhydrothermal sitehydrothermal vent shrimphydrothermal vents Hydrozoa hyperbenthic mysids crustacea hyperboreus IcelandIcelandic waters ingestion inland sea inorganic insitu insitu rates intensity interannualintermediate waterinterplanetary mediuminvertebrate larvaeinvestigations isafjord-deep island islandsisolated topographyisotope compositionisotope record jellyfish jupiter kosterfjordenlabrador currentXULABRADOR CURRENT, FRONTAL ZONE, GULF-STREAM, OCEAN, PECULIARITIES, COMMUNITIES, FIELD Labrador sealakelarge calanoid copepods larvaelarvae and juvenileslaschamp excursionLATE CENOZOIC UPLIFT, TIME-SLICE RECORD, LAST 30,000 YEARS, DEEP-WATER, EARLY PLEISTOCENE, SOUTHERN ASIA, AMERICAN WEST, LATE PLIOCENE, SEDIMENTARY FACIES, INDIAN-OCEAN lava flowslayerldh-b genotypes lenseslepomis-macrochirus life-cycles life-historylife-history parameters light- lindaspollenelipid metabolismlong-term changelong-term changeslong-term problemslucky-strike segment macroplanktonmacrozooplanktonmagmatic accretionmagnetic intensity mantis shrimpmarginal ice-zone marinemarine copepodmarine copepodsmarine geologymarine phytoplanktonmarine research marine snowmarine zooplanktonmarine-invertebratesmarine-phytoplankton masfjorden masses matter Mediterraneanmediterranean salt tonguemediterranean watermediterranean-sea Medusa medusae megafauna meiofauna meristics meroplanktonmesopelagic communitymesozooplanktonmetabolic activity metabolism methane seepmetrida lucens Metridiametridia-lucensmicro-zooplankton microflagellate food-chain micronekton microscale MICROZOOPLANKTON, CARBON, SEAmid-atlantic ridgePMMID-ATLANTIC RIDGE, EAST PACIFIC RISE, LAVA FLOWS, SEGMENTATION, PLUME, OCEANmid-ocean ridge mid-water midwater midwater food migrant biotamigrating zooplankton migration migrationsmitochondrial-dna mixed-layer mixing ratesmnemiopsis-leidyimodel modelling stage development Monterey Bay morphology morphometrymuseum catalogsmuseum collectionMuseum collectionsnannocalanus-minor nanoplanktonnarcomedusae cnidarianarragansett baynatural history nauplii NE AtlanticHENE Atlantic, deep-sea zooplankton, temporal changes, carbon requireme near-bottom near-uv necrophagousnecrophagous amphipod nematode net sampling new record new records new-england76b4   J0# 1793-1814N$://A1993MC16500006oB;Verity, P. G. Stoecker, D. K. Sieracki, M. E. Nelson, J. R.G{Grazing, Growth and Mortality of Microzooplankton During the 1989 North-Atlantic Spring Bloom at 47-Degrees-N, 18-Degrees-Wm<6Deep-Sea Research Part I-Oceanographic Research Papersmicroflagellate food-chain; marine-phytoplankton; photosynthetic pigments; algal carotenoids; micro-zooplankton; narragansett bay; coastal waters; carbon; dynamics; ocean`YGrazing and growth rates of nano- and microzooplankton were measured as part of the 1989 North Atlantic Bloom Experiment, an interdisciplinary research program of the Joint Global Ocean Flux Study (JGOFS). Samples for shipboard experimental incubations were collected from the mixed layer of a drogued water mass (46-degrees-20'N, 17-degrees-50'W) over a 2 week period in May. Grazing and growth rates, measured using the size fractionation and dilution techniques, were calculated from changes in chlorophylls, accessory pigments, and cell abundances. The phytoplankton community was dominated by phytoflagellates, primarily prymnesiophytes, which passed 10 mum mesh. Chlorophyll a (Chl a) increased at an average rate of 0.9 doublings day-1 when incubated at 60% I0. Grazing by nano- and microzooplankton removed 37-100% of estimated primary production in samples from 10 m, and 100% of that at 30 m. An attempt was made to budget estimated rates of community grazing to major groups of nano- and microzooplankton, using measured biomass and specific ingestion or growth rates from laboratory studies. Aplastidic microflagellates were apparently the most important herbivores. In addition to ciliates and heterotrophic dinoflagellates, various developmental stages of copepods were abundant in the <200 mum fraction. Predation within the microzooplankton community appeared to be substantial. Given the evidence of tight coupling between production and consumption within the upper water column, little material appeared to be available for direct export from the mixed layer to depth during this phase of the spring bloom..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1993 Sep409JCTimes Cited: 53 English Article MC165 DEEP-SEA RES PT I-OCEANOG RESISI:A1993MC16500006VINNICHENKO, V. IB 1979leInfluence of hydrodynamics on behaviour of roundnose grenadier in the open part of the Atlantic Ocean} Status of stocks and dynamics of abundance of pelagic fish of the World Ocean. Theses of papers of the scientific conference 20-21 in Russian81VINNICHENKO, V. I. K. V.GORCHINSKY V. N. SHIBANOV  1994Fishery and biological features on some sea mounts of the North Atlantic Ridge by datarom September-October 1993 cruise of the trawler "Ramoen"RKMaterials of the Report Session on results from NIR PINRO research in 1993181-199 in RussianVINNICHENKO, V. Ii 1995B< On commercial stock of alfoncino in the open North Atlantic^X Theses of Reports of the 4th All-Union Conference on problems of commercial forecasting  32 p3 in RussianVINNICHENKO, V. Ii 1996Results of investigations and fishery of alfoncino in the North Atlantic open areas in 1994-1995. Materials of the Report Session on results from PINRO research in 1995 PINRO 95-106 in RussianVINNICHENKO, V. Ii 1996jdVertical daily migrations of alfoncino Beryx splendens Lowe on sea mounts in the open North Atlantic\UDeep-water fishes: Annual International Symp., 1-5 July 1996. Programme and abstracts 71pp.6 in RussianVINNICHENKO, V. Ii 1996TMRussian Investigations on Fishery on Deep-water fish in the North Azores areaS^WReport of the study Group on the Biology and assessment of Deep-Sea Fisheries resourcesg 13 pp.t in RussianVINNICHENKO, V. It 1996NHNew data on distribution of some tuna (Scombridae) in the North AtlanticVoprosy ikhtiologii  36(5)713-715 in RussianVINNICHENKO, V. Ii 1997|uVertical daily migrations of alfoncino Beryx splendens Lowe on sea mounts of the North Atlantic open areas Vopr. ikhtiol. 37(4) 490-496 in RussianVINNICHENKO, V. Ix 1998b\Alfoncino (Beryx splendens) biology and fishery on the sea mounts in the open North AtlanticICES CM 1998/O 13. in RussianVINNICHENKO, V. Ii 1998VPOn results of the cruise of long liner Skarheim to the Reykjanes Ridge in 1997PJ Materials of PINRO session by results of scientific research in 1996-1997 97-106 in RussianVINNICHENKO, V. Ii 1998b\Spatial and temporal variability of demersal fish catches in the area of the Reykjanes RidgeXQ Theses of papers of the VIIth Russian conference on problems of fishery forecast  65-66 in RussianVINNICHENKO, V. Ig 1999HBRussian investigations and fishery on seamounts in the Azores area(!18-a Semana das Pescas dos Acores 18 p in RussianVINNICHENKO, V. Ii 1999>8Deepwater fishery by passive gear on the Reykjanes RidgepjFisheries investigations of the World Ocean. Papers of the International Conference, 27-29 September, 1999 2 6-7 in RussianVINNICHENKO, V. I. 1999ngAlfoncino of the open part of the North Atlantic: results of investigations and perspectives of fisheryb[ Fishery investigations of the World Ocean. Selected papers of the international conference1119-120 in RussianVINNICHENKO, V. I  2000HARussian deepwater fishery in the open Northeast Atlantic in 1999\^WICES The Study Group on the Biology and Assessment of Deep-sea Fisheries Resources 2000b 1 3. in Russian& VINNICHENKO, V. I V. N. KHLIVNOY 2001VORussian deep-sea investigations and fisheries in the Northeast Atlantic in 2000nTN The Study Group on the Biology and Assessment of Deep-sea Fisheries Resources 1- 13. in Russian60VINNICHENKO, V. I. KHLIVNOY V. N N.M. TIMOSHENKO 2001jcTimoshenko N.M. Russian deep-sea investigations and fisheries in the the Northeast Atlantic in 2001VP The Working Group on the Biology and Assessment of Deep-sea Fisheries Resources  18 p. in RussianVINNICHENKO, V. Ig 2002HBRussian investigations and fishery on seamounts in the Azores area(!18-a Semana das Pescas dos Acores18 in RussianVinogradov, G. M.z 1961*#The feeding of deep-sea zooplanktono Fraser, J.H. Corlett, J.b\Rapports et Proces-Verbaux des Reunions. Conseil Internationale pour l'Exploration de la Mer 153a114-120aVinogradov,M.E 19686/Vertical Distribution of the oceanic zooplaktonu 1-295121-126$://A1989T441600021n("Vinogradov, M. E. Shushkina, E. A.\UMacroscale Distribution of Plankton Quantitative Characteristics in the Pacific-Ocean Okeanologiya Okeanologiya 1989Jan-Feb291'^WPP SHIRSHOV OCEANOL INST,MOSCOW,USSR VINOGRADOV ME PP SHIRSHOV OCEANOL INST,MOSCOW,USSR81Times Cited: 3 Russian Article T4416 OKEANOLOGIYAISI:A1989T441600021c Collins, B. L.XRCollins, B. L. 1954. Lista de peixes dos mares dos Aores. Aoreana, II (5), 1-40.*$Lista de peixes dos mares dos AoresAoreanaII5a 1-40549-559$://A1996VM79400009LECopley, J. T. P. Tyler, P. A. Sheader, M. Murton, B. J. German, C. R.b[Megafauna from sublittoral to abyssal depths along the Mid- Atlantic Ridge south of Iceland'Oceanologica Actamid-ocean ridge; megafauna; Reykjanes Ridge; bathymetric zonation; water mass structure de-fuca ridge; reykjanes-ridge; north-atlantic; vent-field; ocean; communities; volcanism; pressure; ecology101 species were identified from 102 biological samples obtained between 225 and 2600 m depth on the Reykjanes Ridge, extending the biogeographic records for several species. Multivariate analysis of between-sample species similarity reveals a two-zone bathymetric faunal distribution with the transition at 800-1000 m. A hydrographic survey of the ridge axis suggests that this faunal zonation is influenced by the water mass structure. Despite the limitations of a sampling programme not designed a priori for biological sampling, the recovery and preservation of the samples and the insight that they provide serves to reinforce that every effort should be made to capitalise on the opportunities for obtaining samples afforded by non-biological sampling programmes. Oceanol. Acta 1996195'F?UNIV SOUTHAMPTON,SOUTHAMPTON OCEANOG CTR,DEPT OCEANOG,EUROPEAN WAY,SOUTHAMPTON SO14 3ZH,HANTS,ENGLAND UNIV SOUTHAMPTON,SOUTHAMPTON OCEANOG CTR,CHALLENGER DIV SEAFLOOR PROC,SOUTHAMPTON SO14 3ZH,HANTS,ENGLAND Copley JTP UNIV SOUTHAMPTON,SOUTHAMPTON OCEANOG CTR,DEPT OCEANOG,EUROPEAN WAY,SOUTHAMPTON SO14 3ZH,HANTS,ENGLAND 81Times Cited: 3 English Article VM794 OCEANOL ACTAoISI:A1996VM79400009sCornelius, P. F. S.\ 1992 a`ZThe Azores hydroid fauna and its origin, with discussion of rafting and medusa suppression ArquiplagotLife and Earth Sciencesp10 75-99Cornelius, P. F. S.o 1992brMedusa loss in leptolid Hydrozoa (Cnidaria), hydroid rafting, and abbreviated life-cycles among their remote-island fauna: an interim reviewScientia Marina56 (2-3)245-261 1633-1652O$://000081843700007M$Coutis, P. F. Middleton, J. H.TMFlow-topography interaction in the vicinity of an isolated, deep ocean island<6Deep-Sea Research Part I-Oceanographic Research Paperstropical pacific; rotating flow; cobb seamount; west-indies; circulation; chlorophyll; barbados; distributions; disturbance; eddies &The results of two oceanographic surveys designed to delineate the flow response near Cato Island (155 degrees 32'E, 23 degrees 15'S) in the Western Coral Sea are presented. The surveys were conducted in October 1992 and February 1993 and coincided with conditions of strong, steady incident currents and relatively weak, variable currents, respectively. For the strong inflow case study, a surface-intensified cyclonic eddy observed in the wake of the island was co-incident with a zone of strong upwelling. Isotherm displacements within the eddy were in excess of 90 m. The lee side response was strongly depth dependent, with recirculation confined to the upper 120 m. A dynamical systems approach incorporating ADCP data was used to compute Lagrangian trajectories numerically for particles released at various locations in the wake zone. There was no evidence of enhanced chlorophyll concentrations downstream of the island. Comparisons with other dynamically similar studies indicate that eddy shedding is likely during periods of steady incident currents. During the second survey, weaker incident currents resulted in a less pronounced flow disturbance. Small isothermal displacements were capped beneath the strong seasonal thermocline. Lee side currents were weak and variable, with recirculation confined to the upper 50 m, A strong biological response was observed downstream, with increased integrated chlorophyll content and zooplankton biomass in the lee providing evidence of the island mass effect. (C) 1999 Elsevier Science Ltd. All rights reserved.e.(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1999 Sepe469A'VOQueensland Univ Technol, Ctr Stat Sci & Ind Math, POB 2434, Brisbane, Qld 4001, Australia Queensland Univ Technol, Ctr Stat Sci & Ind Math, Brisbane, Qld 4001, Australia Univ New S Wales, Math & Oceanog Lab, Sydney, NSW 2052, Australia Coutis PF Queensland Univ Technol, Ctr Stat Sci & Ind Math, POB 2434, Brisbane, Qld 4001, AustralianHBTimes Cited: 4 English Article 223LZ DEEP-SEA RES PT I-OCEANOG RESISI:000081843700007 n excess of 90 m. The lee side response was strongly depth dependent, with recirculation confined to the upper 120 m. A dynamical systems approach incorporating ADCP data was used to compute Lagrangian trajectories numerically for particles released at various locations in the wake zone. There was no evidence of enhanced chlorophyll concentrations downstream of the island. Comparisons with other dynamically similar studies indicate that eddy shedding is likely during periods of steady incident currents. During the second survey, weaker incident currents resulted in a less pronounced flow disturbance. Small isothermal displacements were capped beneath the strong seasonal thermocline. Lee side currents were weak and variable, with recirculation confined to the upper 50 m, A strong biological response was observed downstream, with increased integrated chlorophyll content and zooplankton biomass in the lee providing evidence of the island mass effect. (C) 1999 Elsevier Science Ltd. All rights reserved.e.(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1999 Sepe469A'VOQueensland Univ Technol, Ctr Stat Sci & Ind Math, POB 2434, Brisbane, Qld 4001, Australia Queensland Univ Technol, Ctr Stat Sci & Ind Math, Brisbane, Qld 4001, Australia Univ New S Wales, Math & Oceanog Lab, Sydney, NSW 2052, Australia Coutis PF Queensland Univ Technol, Ctr Stat Sci & Ind Math, POB 2434, Brisbane, Qld 4001, AustralianHBTimes Cited: 4 English Article 223LZ DEEP-SEA RES PT I-OCEANOG RESISI:000081843700007  >  85-94$://000075337900002&Gislason, A. Astthorsson, O. S.xqSeasonal variations in biomass, abundance and composition of zooplankton in the subarctic waters north of Iceland Polar BiologyEcalanus-finmarchicus; greenland-sea; barents sea; vertical- distribution; isafjord-deep; nova-scotia; southwest; mesozooplankton; hyperboreus; glacialisThe seasonal variations in biomass, abundance and species composition of zooplankton in relation to hydrography and chlorophyll a were studied in the subarctic waters north of Iceland. The sampling was carried out at approximately monthly intervals from February 1993 to February 1994 at eight stations arranged along a transect extending from 66 degrees 16'N-18 degrees 50'W to 68 degrees 00'N-18 degrees 50'W. The mean temperature at 50 m depth showed a clear seasonal pattern, with lowest water temperatures in February (similar to 1.1 degrees C) and the highest in July (similar to 5.4 degrees C). The spring growth of the phytoplankton began in late March and culminated during mid-April (similar to 7.0 mg Chi a m(-3). Both the biomass and the abundance of total zooplankton were low during the winter and peaked once during the summer in late May (similar to 4 g m(-2) and similar to 38,000 individuals m(- 2)). A total of 42 species and taxonomic groups were identified in the samples. Eight taxa contributed similar to 90% of the total zooplankton number. Of these Calanus finmarchicus was by far the most abundant species (similar to 60% of the total zooplankton). Less important groups were ophiuroid larvae (similar to 9%), Pseudocalanus spp. (similar to 8%)) Metridia longa (similar to 4%), C. hyperboreus (similar to 3%), Acartia longiremis (similar to 2%), chaetognaths (similar to 2%) and euphausiid larvae (similar to 2%). The dominant copepods showed two main patterns in seasonal abundance: C. finmarchicus, C. hyperboreus and C. glacialis had one annual peak in numbers in late May, while Pseudocalanus spp., M. longa and A. longiremis showed two maxima during the summer (July) and autumn (October/November). Ophiuroid larvae and chaetognaths (mainly Sagitta elegans) peaked during the middle of July, while the number of euphausiid eggs and larvae was greatest from May to July. The succession in population structure of C. finmarchicus indicated its main spawning to be in April and May, coincident with the phytoplankton spring bloom. A minor spawning was also observed sometime between August and October. However, the offspring from this second spawning contributed only insignificantly to the overwintering stock of C. finmarchicus.0 Polar Biol. 1998 Aug202'Marine Res Inst, Skulagata 4,POB 1390, IS-121 Reykjavik, Iceland Marine Res Inst, IS-121 Reykjavik, Iceland Astthorsson OS Marine Res Inst, Skulagata 4,POB 1390, IS-121 Reykjavik, Iceland6/Times Cited: 7 English Article 109RX POLAR BIOLISI:000075337900002 1619-1627i$://000167224000010\UGislason, A. Astthorsson, O. S. Petursdottir, H. Gudfinnsson, H. Bodvarsdottir, A. R.f`Life cycle of Calanus finmarchicus south of Iceland in relation to hydrography and chlorophyll a$Ices Journal of Marine Sciencegonad development; North Atlantic; stage development; vertical distribution; zooplankton marine copepod; zooplankton; community; norway The life history of Calanus finmarchicus was studied in relation to hydrography and chlorophyll cr dynamics south of Iceland between February 1997 and March 1998. Concentrations of chlorophyll rr on the shelf Mere low through February and March (<0.5 mg m(-3)), started to increase in early April and reached a peak in mid-May ( 5 mg m(-3)). Another peak was observed in mid-June (similar to 5-7 mg m(-3)). and a small increase in August (similar to 2.5 mg m(-3)). During winter, C. finmarchicus was virtually absent from the bank, and the population resided mainly in deep (>400 m) water beyond the shelf. Overwintering animals emerged from diapause in the oceanic area and moulted to adults during February, March, and April, during which time some were advected onto the shelf The number of C. finmarchicus on the shelf started to increase in April and showed two main peaks during summer, in May/June(similar to 105 000 individuals m(-2)) and June/July (similar to 95 000 individuals m(-2)), and a minor one in autumn (September/October. similar to 10 000 individuals m(- 2)). The peaks reflected three recruitment events which, by back-calculation, mag be linked to spawning events in April, June, and August/September. All three estimated peaks of reproduction were in close association with periods of relatively high phytoplankton biomass. As judged by the abundance of young developmental stages (C1-C3), the spawnings in April and June were most important and produced similar numbers of offspring, whereas that in August/September contributed insignificantly to the overwintering stock. The results indicate mixing of generations during summer. (C) 2000 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 2000 Dec 576u:3Times Cited: 1 English Article 406PH ICES J MAR SCInISI:000167224000010n  6677-6686$://A1995QT22200013$Cowles, T. J. Fessenden, L. M.jdCopepod Grazing and Fine-Scale Distribution Patterns During the Marine Light-Mixed Layers Experiment,&Journal of Geophysical Research-Oceanszcalanus-finmarchicus; north-sea; zooplankton; atlantic; plankton; bloom; phytoplankton; helgolandicus; crustacea; flex- 76d]The mesozooplankton in the upper 100 m at 59 degrees N, 21 degrees W were dominated by the copepodite stages of Calanus finmarchicus in both May and August 1991. Abundance of C. finmarchicus in the upper 20 m of the water column was 800 m(- 3) in May and 200 m(-3) in August. Although hydrographic conditions changed from well mixed to stratified between May and August, the fine-scale vertical distribution pattern of C. finmarchicus was essentially the same during these two surveys of the Marine Light-Mixed Layers site. Copepodite stage five (CV) comprised a larger fraction of the population in August compared to May, however. Gut evacuation experiments with C. finmarchicus indicated that late copepodite and adult female life stages had evacuation rates of approximately 4% h(-1) in both May and August. Although these evacuation rates are consistent with others measured for Calanus, the relatively low biomass in the upper 100 m resulted in an estimated daily grazing impact by Calanus of less than 5% of the phytoplankton standing stock in May, and less than 1% in August. The ingestion rates we measured suggest that the total grazing impact of all mesozooplankton grazers is less than 10% of daily primary production. These relatively low ingestion rates on phytoplankton provide these copepods with less than half of the total daily carbon intake required to balance estimated rates of respiration and growth in the field. In order to balance these metabolic costs, we estimate that the mesozooplankton would need to ingest the equivalent of at least 100% of the estimated microzooplankton/protist daily production.J. Geophys. Res.-Oceans 1995 Apr 15 100C4'OREGON STATE UNIV,COLL OCEAN & ATMOSPHER SCI,CORVALLIS,OR 97331 COWLES TJ OREGON STATE UNIV,COLL OCEAN & ATMOSPHER SCI,CORVALLIS,OR 97331@:Times Cited: 21 English Article QT222 J GEOPHYS RES-OCEANSISI:A1995QT22200013ZF Sy, A. 1988Investigation of large-scale circulation patterns in the central North Atalntic: The North Atlantic Current, the Azores Current, and the Mediterranean Water plume in the area of the Mid-Atlantic RidgeDeep Sea Research35383-413 Sy, A Schauer,U Meincke, J 1992xrThe North Atlantic current and its associated hydrographic structure abive and eastwards of the Mid-atlantic RidgeDeep-Sea Research\395825-853|uCOLD-CORE EDDY, GENERAL-CIRCULATION, MEAN CIRCULATION, WATER, OCEAN, 48-DEGREES-N, VARIABILITY, PACIFIC, ENERGY, WESTBased on CTD data sets obtained in 1981-1984, XBT profiles, and long-term current meter moorings, the large-scale circulation field of the northeastern Atlantic north of the Azores was investigated. The mean volume transport through a standard meridional CTD section between 40-degrees-N and 52-degrees-N along the eastern flank of the Mid-Atlantic Ridge (MAR) was estimated to be 30 +/- 9 Sv, with the North Atlantic Current (NAC) transporting 26 Sv. The NAC was found to be composed of clearly defined current branches (jets), that appear in temperature-salinity diagrams as a modal structure of the Central Water. Whereas the northernmost current branch (subarctic front) was found to be topographically fixed at the Gibbs Fracture Zone, the number, intensity and T-S structure of the remaining current branches, as well as their path over the MAR, are subject to intense variability. From 2 years of observations the branches were found to continue into the basins east of the MAR. They appeared as mesoscale features in a region of increased eddy kinetic energy and are interpreted to result from baroclinic instability. No indications of a branch of the NAC moving south, i.e. a recirculation as part of the North Atlantic subtropical gyre, were found."Sy, A. U. Schauer J. Meincke 1992zsThe North Atlantic Current and its associated hydrographic structure above and eastwards of the Mid-Atlantic Ridge.Deep-Sea Research395A825-8543TARNOPOLSKY, A. Gp 1983TMSpatial and temporal statistical structure of large-scale hydrological fields Trudy GOIN  164  67-78 in Russian559-583$://A1996UR64700005  Taylor, A. H. `ZNorth-south shifts of the Gulf Stream: Ocean-atmosphere interactions in the North Atlantic*$International Journal of ClimatologyGulf Stream; North Atlantic; sea-level pressure changes; depression tracks; zooplankton variations; interannual variations; ocean-atmosphere interactions general-circulation; surface-temperature; model; wintereYear-to-year changes in the latitude of the north wall of the Gulf Stream are very similar to those seen in the abundances of zooplankton observed by the Continuous Plankton Recorder Survey around the British Isles and also to those in the abundance of zooplankton in Lake Windermere. These connections must reflect changing weather patterns across the North Atlantic. The index of Gulf Stream position was constructed from the north wall data by principal components analysis. The first principal component, the index used, has eigenvector coefficients that all have the same sign, and is a measure of the latitude of the whole of the north wall. However, the component may represent the occurrences of meanders that are extensive in space and time rather than displacements of the Gulf Stream as a whole. This principal component has been used to calculate weighted averages of monthly mean sea-level pressure and of monthly mean numbers of cyclone tracks in order to show the changes in weather patterns associated with displacements of the north wall. Northward displacements of the north wall were accompanied by significantly reduced cyclone numbers in the northernmost regions of the Atlantic (annually and in the autumn) and in spring, summer, and autumn, a region of reduced atmospheric pressure in the central Atlantic area 40 degrees-60 degrees N, 30 degrees-50 degrees W (locally significant). There was some tendency (not significant) for storm tracks to be deflected around the south side of this region. The pattern in winter is less clear and shows no statistical significance. Changes in the vicinity of the British Isles were generally too small to be statistically significant but were generally consistent with a lower frequency of storms in spring and autumn. As the biological changes appear to be caused by variations in the onset of thermal stratification during the spring they may be the result of relatively small changes in the atmospheric forcing. The atmospheric changes show no indications of the sources of the Gulf Stream displacements, the anomaly winds opposing the displacements. This may be because meanders of the Gulf Stream are not simply related to any single atmospheric variable. The clearest and most statistically significant meteorological signals were all well downstream from the north wall. Although the displacements of the north wall are caused by changing weather patterns over the North Atlantic, the Gulf Stream is also a region of strong heat transfers from the ocean to the atmosphere. Sawyer's criterion indicates that distortions of this heat source could cause noticeable disturbances to the atmospheric circulation over the North Atlantic. A numerical model based on the analytical model of Smagorinsky is used to investigate the perturbations of the zonal circulation that might be caused by displacements of this local heat source. The predictions are in agreement with the changes seen in the central Atlantic during summer, spring, and autumn (but not those during winter). In the region where the model predicts atmospheric pressure reductions should occur, there are no positive correlation coefficients between the position of the north wall and the surface atmospheric pressure but a significant excess of negative correlation coefficients compared with chance, and northward shifts of the Gulf Stream were accompanied by significant reductions in atmospheric pressure. It is therefore possible that displacements of the north wall could influence weather patterns further east. The model predicts that any changes over the European continental shelf will be weak. An accurate description of the dynamics of the Gulf Stream may be an important requirement of coupled ocean-atmosphere models.Int. J. Climatol. 1996 May165:4Times Cited: 10 English Article UR647 INT J CLIMATOLISI:A1996UR64700005CBABOGOROV, G. V. 1969PJMorphometric investigations in the northern part of the Mid-Atlantic Ridge Okeanologiya  IX(6) 1038-1048  in Russian"BOGOVSKI, S.P. Yu. I. BAKAY. 1989Chromatoblastomas and related pigmented lesions in deepwater redfish, Sebastes mentella (Travin), from North Atlantic areas, especially from the Irminger SeaeJournal of Fish Diseases12 1-13.2+BOGOVSKY, S. P. Yu. I. BAKAY A. B. KARASEV.I 1986RKHystological investigation of black spots and melanomas in deep-sea redfish;("Experimental and clinical oncology 7114-120  in Russian 1072-1082$://A1989AY60000010"Bollens, S. M. Frost, B. W.tmZooplanktivorous Fish and Variable Diel Vertical Migration in the Marine Planktonic Copepod Calanus-Pacificus Limnology and OceanographyLimnol. Oceanogr.t 1989 Seph346 'vpUNIV WASHINGTON,SCH OCEANOG,WB-10,SEATTLE,WA 98195 BOLLENS SM UNIV WASHINGTON,SCH OCEANOG,WB-10,SEATTLE,WA 9819582Times Cited: 73 English Note AY600 LIMNOL OCEANOGRISI:A1989AY60000010 1047-1065E$://A1989AQ22500011u"Bollens, S. M. Frost, B. W. F@Predator-Induced Diel Vertical Migration in a Planktonic Copepod"Journal of Plankton ResearchJ. Plankton Res. 1989 Sep115a'vpUNIV WASHINGTON,SCH OCEANOG,WB-10,SEATTLE,WA 98195 BOLLENS SM UNIV WASHINGTON,SCH OCEANOG,WB-10,SEATTLE,WA 98195:4Times Cited: 93 English Article AQ225 J PLANKTON RESISI:A1989AQ225000116 1359-1365e$://A1991GM24500016"Bollens, S. M. Frost, B. W.VPDiel Vertical Migration in Zooplankton - Rapid Individual- Response to Predators"Journal of Plankton Research'2,UNIV WASHINGTON,SCH OCEANOG,SEATTLE,WA 98195$planktonic copepod; evolution While diel vertical migration in zooplankton has been shown recently to be a predator avoidance behavior, the mechanism by which predators induce and maintain such behavior has been debated. We report results of an in situ predator manipulation experiment during which enclosed populations of the marine planktonic copepod Acartia hudsonica rapidly changed their vertical distribution and diel migration behavior depending on presence or absence of the planktivorous fish Gasterosteus aculeatus. These results point unambiguously to phenotypic behavioral plasticity of individual planktonic prey, not, as previously hypothesized, population-genetic level behavioral changes caused by selective fish predation, as the mechanism underlying changes in diel vertical migration in this copepod.J. Plankton Res. 1991 Nov136:4Times Cited: 53 English Article GM245 J PLANKTON RESISI:A1991GM24500016 @x?>=GF>EWade,I.P Heywood,K.J 2001Acoustic backscatter observation of zooplankton abundance and behaviour and the influence of oceanic fronts in the Northeast Atlantic\Deep-Sea ResearchV part II 48899-924&Wakefield, W.W. Smith, K.L. Jr. 1990Onthogenetic vertical migration in Seastolobus altivelis as a mechanism for transport of particulate organic matter at continental slope depthsn#8 Limnology and Oceanography35 1314-1328  Warren, B.A. 1981*#Deep circulation of the world oceanVPEvolution of physical oceanography, scientific surveys in honor of Henry Stommel  Cambridge, MA0  MIT Press 6-412,Weeks, J. M. Rainbow, P. S. Depledge, M. H. 1995sBarnacles (Chthamalus stellatus) as biomonitors of trace metal bioavailability in the waters of So Miguel (Azores) Aoreana Supl.103-111Weerdt, W. H. de 1989jcPhylogeny and vicariance bigeography of the north Atlantic Chalinidae (Haplosclerida, Demospongiae)t Beaufortia393{ 55-88p Wells, F.E. 1995An investigation of marine invertebrate communities in the sediments of Ilhu de Vila Franca off the island of So Miguel, AzoresAoreana Supl.e 57-65 Wheeler, A. 1978*$Key to the Fishes of Northern EuropeFrederick Warne (Publ)  xix 380 Wheeler, A. 1992JDA list of common and scientific names of fishes of the British islesJournal of Fish Biologyn41 Supplement A 1-37JDWhitehead, P. J. M.-L. Bauchot J.-C. Hureau J. Nielsen E. Tortonese  1989>7Fishes of the North-east Atlantic and the Mediterranean UNESCO, Paris8 Vol. I, II and III. 1473429-437$://000082297900004pLEWidder, E. A. Johnsen, S. Bernstein, S. A. Case, J. F. Neilson, D. J.b[Thin layers of bioluminescent copepods found at density discontinuities in the water column3Marine Biologysound-scattering layers; calanus-pacificus; metridia-lucens; marine snow; dinoflagellate luminescence; north-atlantic; zooplankton; plankton; predation; behaviornTo learn how organisms apportion space in the open ocean, biological oceanographers have sought to improve temporal and spatial resolution of ocean sampling systems. Their objectives are to simultaneously measure physical, chemical and biological structure in the water column in order to find significant correlations that may reveal underlying processes. Here we report one such correlation between intense peaks of bioluminescence and density discontinuities in the water column. Intensified video recordings made in these bioluminescent "hot spots" were analyzed with a computer image- recognition program that identifies organisms based on the temporal and spatial characteristics of their luminescent displays. Based on this analysis, the source of the "hot spots" was found to be very thin layers (0.5 m) of the bioluminescent copepod Metridia lucens present at from 5 to 100 times average background concentrations. Given the recent discovery that the vertical distribution of marine snow is also strongly correlated with density discontinuities in the water column, we suggest that this finding may provide a possible explanation for the disparity between estimated energy requirements of marine copepods and measurements of average in situ food concentrations. The energy costs associated with locating food- rich micro-patches is greatly reduced if those patches are spread out into very thin layers, because the search strategy can be reduced from three dimensions to one. Mar. Biol. 1999 Aug  134S3L4-Times Cited: 2 English Article 231FR MAR BIOLrISI:0000822979000049159-164$://A1997WW50400015nPlanque, B. Ibanez, F.TNLong-term time series in Calanus finmarchicus abundance - A question of space?Oceanologica Acta1North Atlantic; Calanus finmarchicus; long-term changes; space- time interactions; Continuous Plankton Recorder continuous plankton records; north-sea; zooplankton; atlanticYear-to-year changes in abundance of the copepod Calanus finmarchicus in the North Atlantic are studied by means of the Continuous Plankton Recorder (CPR). Using data collected during the years 1962 to 1974, the spatial heterogeneity of long-term trends is studied by numerical analysis: Mantel test, Mantel correlogram, and spatio-temporal clustering. Results reveal that (1) interannual changes of C. finmarchicus abundance are spatially autocorrelated; (2) the spatial structures have a radius varying between 400 and 1100 km; and (3) there is a high variability in the annual changes observed between the different zones detected by clustering. These results show that observations made in the Northeast Atlantic cannot be extrapolated to the whole North Atlantic basin, and suggest that identification of the size and location of an ''homogeneous zone for long-term changes'' should be taken into account when determining factors responsible for year-to-year fluctuations in abundance of C. finmarchicus. Oceanol. Acta 199720181Times Cited: 5 English Article WW504 OCEANOL ACTAISI:A1997WW50400015315-326$://A1997WQ10500007960Planque, B. Hays, G. C. Ibanez, F. Gamble, J. C.VPLarge scale spatial variations in the seasonal abundance of Calanus finmarchicus<6Deep-Sea Research Part I-Oceanographic Research Paperscontinuous plankton records; north-atlantic ocean; ecological investigations; zooplankton community; copepods; sea; balsfjorden; variability; succession; patternsData collected by the Continuous Plankton Recorder (CPR) survey between 1962, and 1974 in the North Atlantic and adjacent seas were used to examine large scale spatial variations in the seasonal cycle of near-surface abundance of the copepod Calanus finmarchicus. Through most of this region, the dominant seasonal pattern was minimum abundance between November and February followed by an increase to maximum abundance in May. Two large (> 600 000 km(2)) areas had seasonal cycles that differed markedly from this dominant pattern. South of Newfoundland, maximum abundance occurred between February and May, while south of Greenland, maximum abundance occurred between April and October. This delayed seasonal cycle south of Greenland has not been identified previously, and it is speculated that regional changes in seasonal patterns may result from regional temperature and/or timing of food availability differences. (C) 1997 Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 Feb442JCTimes Cited: 18 English Article WQ105 DEEP-SEA RES PT I-OCEANOG RESISI:A1997WQ10500007t 1528-1535G$://000167224000002 Planque, B. Batten, S. D.leCalanus finmarchicus in the North Atlantic: the year of Calanus in the context of interdecadal changeL$Ices Journal of Marine ScienceCalanus finmarchicus; Continuous Plankton Recorder; copepods; North Atlantic; plankton c-helgolandicus; abundance; environment; zooplankton Using data collected by the Continuous Plankton Recorder survey, ne review the regional characteristics of Calanus populations from distinct areas of the North Atlantic and update the observations of dominant changes that have occurred during the past four decades. Timing of the seasonal cycle of abundance of C. finmarchicus can vary by up to four months between oceanic provinces. We provide the first pan-Atlantic estimate of the contribution of C. finmarchicus to the biomass of the planktonic ecosystem in comparison with other copepod taxa. This estimate reveals that, over most of the North Atlantic, C. finmarchicus represents more than half the copepod biomass sampled by the CPR. Comparison of the abundance of C. finmarchicus recorded during the "Year of Calanus" (1997) with that recorded in the past indicates that, in the Northeast Atlantic, the abundance and relative biomass of the species during the TASC years have been the lon est ever recorded. (C) 2000 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 2000 Dec576:3Times Cited: 1 English Article 406PH ICES J MAR SCIISI:000167224000002u&dR0`d5800006F Angel, M. V.(!Biodiversity of the Pelagic OceanTConservation BiologyThis paper reviews knowledge of biodiversity in open ocean pelagic communities and discusses the possible causal factors for the patterns. The oceanic pelagic ecosystem is by far the largest on Earth and, although locally itAksness,D.L Blindheim,J 1996tmCirculation patterns in the North Atlantic and possible impact on population dynamics of calanus finmarchicusfOphelia\44 7-28|DIEL VERTICAL MIGRATION, WESTERN NORWAY, WINTER DISTRIBUTION, ZOOPLANKTON, MASFJORDEN, LINDASPOLLENE, MICRONEKTON, FISH, SEA$Due to advective impact few consistent time-series describing the population development of the copepod C. finmarchicus exist. Quantitatively, the spring generation seems to be the most important, and especially in the northern areas one generation per year seems to prevail. A fecundity of 10(2)-10(3) eggs female(-1) and a sex ratio 1:1 then give a maximal reproductive rate of 3.9-6.2 year(-1). This low rate seems to be compensated by low mortality due to effective predator avoidance in terms of diurnal and seasonal vertical migrations. We have calculated that the advective renewal of the habitats of C. finmarchicus in the subpolar gyre and in the Nordic Seas are 0.13 and 0.29 year(-1) respectively while the birth and death rates of C.finmarchicus typically are above 3.9 year(-1). This means that the biological rates are likely to dominate over the advective rates in the two ocean areas, and that the C.finmarchicus development is facilitated by Ic cal production in both areas. Rough calculations for the Nordic Seas indicate that our of a total annual production of 74 mill. tonnes, 3.6 mill. tonnes are lost to adjacent seas by advection. Due to the flow of deep and cold waters southward and the seasonal migration of C. finmarchicus it is likely that the loss of individuals from the Nordic Seas southward to the North Atlantic is dominated by copepodite V, and that a higher proportion of younger life stages are carried in the south-north (Barents Sea) and west-east (Norwegian coast and the North Sea) directions with the warmer, Atlantic Water.2,ALEKSEEV, F. E. E. I. ALEKSEEVA N. V. TITOVA 1978Polymorphous system of the muscle esterases, ecological structure of the habitat and studying of species structure in grenadier (Macrurus rupestris Gunn.)f_The union conference on biochemical genetics, karyological polymorphism and mutagenesis in fish  19-20; in Russian2,ALEKSEEV, F. E. E. I. ALEKSEEVA N. V. TITOVA 1979 Polymorphous system of the muscle esterases, ecological structure of the habitat and studying of species structure in grenadier (Macrurus rupestris Gunn.)4-Biochemical and populational genetics of fish1  58-63 in RussianALEKSEEV, F. E.r 1982Reproductive cycle, functional structure of the area and intra-populational differentiation in grenadier Macrurus rupestris Gunn. of the Middle-Atalantic RidgenhUnion Conference on Theory of Formation of Abundance and Rational Exploitation of Commercial Fish Stocks 73-75} in Russian"ALEKSEEV, G. V. I. D. ZYKOV. 1983\UPeculiarities of water dynamics and structure in the area of the ocean station vessels Trudy AANIIb 382l 58-64\ in RussianB>>IIIeeddd22277Yf"##55DDDDDoo<<<<;333VV@@&&nn````pp:OO$$$$+WWLhqT7/|.-,rS83-S102$://A1991GD47900006rVenrick, E. L.xrMidocean Ridges and Their Influence on the Large-Scale Patterns of Chlorophyll and Production in the North Pacific<6Deep-Sea Research Part a-Oceanographic Research Papers`Zhawaiian ridge; seamounts; atlantic; phytoplankton; topography; community; shallow; eddiesJDOcean-wide spatial patterns of chlorophyll a and productivity are investigated along two transects, one through the central North Pacific at 24-degrees-15'N and one through the subarctic Pacific at 47-degrees-N. In the south, large-scale gradients are absent across most of the ocean. In the north, large-scale gradients are significant. Three mid-ocean ridge systems are crossed by these transects: the Hawaiian Ridge and the Mariana Ridge in the central North Pacific and the Emperor Seamount Chain in the subarctic. Significant reductions in chlorophyll a are seen for more than 900 km west of the shallow Hawaiian Ridge in the oligotrophic central North Pacific. A similar band of reduced chlorophyll lies above the deep Emperor Sea Mount Chain in the eutrophic subarctic Pacific. No change in chlorophyll a is associated with the Mariana Ridge. The effect of mid-ocean ridges on the epipelagic ecosystem does not depend directly on the depth of the bottom topography or the ambient nutrient concentration in the euphotic layer. The effect may be more widespread than previously realized. 199138'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,MARINE LIFE RES GRP,LA JOLLA,CA 92093 VENRICK EL UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,MARINE LIFE RES GRP,LA JOLLA,CA 92093JDTimes Cited: 7 English Article 1 GD479 DEEP-SEA RES PT A-OCEANOG RESISI:A1991GD47900006 Venrick, E.L. 1991zsMid-ocean ridges and their influence on the large-scale patterns of chlorophyll and production in the North Pacific Deep-Sea Research38 83-102$Venzke, S. Mnnich,M Latif, M 2000D=On the predictability of decadal changes in the North PacificoClimate Dynamics16379-392126-131$://A1990CU07900021hVereshchaka, A. L.|vVertical-Distribution of Euphausiids, Pelagic Decapods and Mysids in the near-Bottom Layer of the Western Indian-Ocean Okeanologiya Okeanologiya 1990Jan-Feb301'^XPP SHIRSHOV OCEANOL INST,MOSCOW,USSR VERESHCHAKA AL PP SHIRSHOV OCEANOL INST,MOSCOW,USSR81Times Cited: 5 Russian Article CU079 OKEANOLOGIYAISI:A1990CU07900021 88-94$://A1994NF50700015AVereshchaka, A. L.Distribution of Pelagic Macroplankton (Mysids, Euphausiids, Decapods) over Continental-Slope and Seamound of the Western Indian-Ocean Okeanologiya2,northeast atlantic-ocean; near-bottom; layertmDistributions of numbers, biomass, and sizes of 18 species belonging to mysids, euphausiids, and decapods dwelling in the vicinities of seamounts and continental slopes of the Western Indian Ocean, has been reported. Conclusions are based upon materials of 39 horizontal and 15 near-bottom trawl samples at 30 - 1000 m above bottom, obtained during 17th Voyage of R/V ''Vityaz'' (1989 - 1990). Patterns of distribution of pelagic animals in the vicinity of the sea-floor have revealed: (1) rize of lines of equal numbers, biomass, and sizes over slopes up to the lesser depth than in the open-ocean, and (2) abrupt decreasing of numbers, biomass, and sizes at 200 - 400 and less m above the sea-floor. These patterns appear not to depend upon taxonomical site of species, the depths of their dwelling, and their feeding. Possible cause leading to these patterns, are discussed. Okeanologiya 1994Jan-Feb341'b\PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA VERESHCHAKA AL PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA81Times Cited: 3 Russian Article NF507 OKEANOLOGIYAISI:A1994NF50700015 1639-1668 $://A1995TD80600008mVereshchaka, A. L.PJMacroplankton in the near-Bottom Layer of Continental Slopes and Seamounts<6Deep-Sea Research Part I-Oceanographic Research Papersbenthic boundary-layer; hyperbenthic mysids crustacea; northeast atlantic-ocean; western indian-ocean; deep-sea; vertical-distribution; benthopelagic plankton; biomass; zooplankton; zonationDistributions of mysids, euphausiids, shrimps and bottom- dwelling decapod larvae have been studied to reveal their relation to the sea bottom. A total of about 200,000 specimens belonging to 178 species and closer unidentified taxa has been examined. The material has been taken by R.V. Professor Shtokman in the Southeast Pacific (1987-1988) and by R.V. Vityaz in the western Indian Ocean (1989-1990) by sampling at depths of 1500 m and less over seamounts and continental slopes. In addition, aquarium observations on five species and analyses of the gut contents of 14 species have been carried out. Two principal groups of animals have proved to live in the near-bottom layer: pelagic (independent of the bottom) and benthopelagic (related to the bottom). They appear to differ in all studied aspects: distribution, behaviour and feeding. The benthopelagic animals are divided into three subgroups with finer ecological differences: hypo-, epi-, and amphibenthopelagic. The patterns of their distribution and migrations, the near-bottom biological zonation and its relation to the benthic boundary and benthic nepheloid layers are discussed, with (re)definitions of the terms used..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1995 Sep429'RUSSIAN ACAD SCI,INST OCEANOL,KRASIKOVA ST 23,MOSCOW 117218,RUSSIA VERESHCHAKA AL RUSSIAN ACAD SCI,INST OCEANOL,KRASIKOVA ST 23,MOSCOW 117218,RUSSIAHBTimes Cited: 8 English Article TD806 DEEP-SEA RES PT I-OCEANOG RESISI:A1995TD80600008 =TGenetics of commercial fishes and objects of aquaculture. Materials of the union conference on genetics, selection and hybridization of fishes0-Genetics, selection and hybridization of fishGidrometeoizdat Global and Planetary Change84Global Biogeochemical Cycles Glob. Biogeochem. Cycle$GU ZAPRYBA. Zaprybpromrazvedka$ Helgolnder MeeresuntersuchungenHelgolnder MeersuntersHerpetological Review Hydrobiologia Hydrobiologia@;Hydrometeoropogy and Hydrochemistry of the Seas of the USSRIbis,)ICCAT, Recueil de Documents ScientifiquesICES83ICES Annual Science Conference (ICES CM 2000/S:02).ICES CM 1998/O40Ices Journal of Marine Science ICES J. Mar. Sci.\WICES The Study Group on the Biology and Assessment of Deep-sea Fisheries Resources 2000 ICES, CMHDIII All-USSR Conference on Marine Biology, Sevastopol, October, 1988 in pressIncrease of effectiveness of the fishing fleet and further development in the open part of the ocean. Materials of the union conference$Institute of Taxonomic Zoology84Instrumental methods of commercial stocks assessment4.Instrumental methods of fishery investigations40Insufficiently explored fishes of the open oceanD?Inter-university conference of young scientists and specialists84International Council for the Exploration of the Sea<6International Journal of Climatology Int. J. Climatol.PMInternationale Revue Der Gesamten Hydrobiologie Int. Rev. Gesamten Hydrobiol.Interridge NewsPLIntra-species differentiation of the sea commercial fishes and invertebrates(%Invertebrate Biology Invertebr. Biol.83Investigation of bioresources of the North Atlantic85Israel Program for Scientific Translations, JerusalemItogi Nauki i TekhnikiLIIzvestiya Akademii Nauk Seriya Biologicheskaya Izv. Akad. Nauk Ser. Biol. J. Appl. Ecol J. Northwest. Atl. Fich. Sci84Jornal de Sciencias Mathematicas Physicas e Naturaes85Jornal de Sciencias mathematicas, Physicas e NaturaesD@Journal de Sciencias Mathematicas, Physicas e Naturaes, 2 srieJournal marine biology,)Journal of Applied Ecology J. Appl. Ecol.Journal of Avian Biology Journal of Crustacean Biology82Journal of Experimental Marine Biology and EcologyJournal of Fish BiologyJournal of Fish Diseases0-Journal of Fisheries Research Board of Canada$Journal of Geophysical ResearchD>Journal of Geophysical Research-Oceans J. Geophys. Res.-OceansLHJournal of Geophysical Research-Solid Earth J. Geophys. Res.-Solid EarthJournal of Ichthyology,'Journal of Marine Research J. Mar. Res.Journal of Marine Systems($Journal of Oceanography J. Oceanogr.83Journal of Physical Oceanography J. Phys. Oceanogr.0-Journal of Plankton Research J. Plankton Res.(#Journal of Sea Research J. Sea Res.,(Journal of the Linnean Society of LondonHBJournal of the Marine Biological Association of the United Kingdom Journal of Zoology of LondonD>Kongelige Danske Videnskabernes Selskabs Skrifter, Kjbenhaven0,Limnology and Oceanography Limnol. Oceanogr.Manual of methodsMar Ecol Prog SerMar. Ecol. Prog. SerMar. Ecol. Prog. Ser.Marine Biology Mar. Biol.$Marine Ecology Progress Series,(Marine Ecology Progress Series, in press84Marine Ecology-Progress Series Mar. Ecol.-Prog. Ser. Marine Environmental Research0-Marine Micropaleontology Mar. Micropaleontol.Marine Pollution BulletinMarine Research MaritimesLIMaterials of PINRO session by results of scientific research in 1996-1997PKMaterials of the Report Session on results from NIR PINRO research in 1993TQMaterials on methods of searching for fish and non-fish objects in the open oceanD>Materialy rybokhozyaistvennykh issledovanii severnogo basseinaHBMeddlelelser fra Kommissionen for Havunders-gelser, Serie FiskeriMediterranean Odontostomidae Report of the Dana Oceanographical Expeditions 1908-1910 to the Mediterranean and Adjacent Seas Vol. II. Biology, A.",  l XWp Rossby,T 1999On gyre interactionsDeep-Sea Research part II 46139-1649NORTH-ATLANTIC CURRENT, GULF-STREAM MEANDERS, POTENTIAL VORTICITY, SURROUNDING WATERS, FLUID EXCHANGE, CAPE-HATTERAS, SARGASSO SEA, VARIABILITY, TRANSPORT, CIRCULATIONaThe principal meeting point of the subtropical and subpolar gyres of the North Atlantic is at the Tail of the Grand Banks where the two western boundary currents, the Gulf Stream and Labrador Current, join forces as the North Atlantic Current, which flows northeast almost 10 degrees in latitude before turning east as the Subpolar Front, ultimately feeding the Labrador and Nordic Seas and the thermohaline overturning. After the Gulf Stream turns into the North Atlantic Current at the Grand Banks, its role shifts from a wind-driven current to a link in the large-scale thermohaline circulation. The processes governing this transition, in particular the continued transport north of mass and heat, are questions of considerable climatic importance. The North Atlantic Current is a very unusual western boundary current in that its mass transport decreases in the downstream direction. The mean path and annual shifting of the eastward flowing Gulf Stream is conjectured to result from a time-varying shelf-Slope Water overflow of waters from the Labrador shelf. As the volume transport increases in fall and deepens the Slope Water pycnocline, it forces the Gulf Stream south and deepens the Sargasso Sea thermocline as well. The timing of these steps governs the June maximum in baroclinic transport. There is some evidence that this 'back-door' gyre interaction may operate on interannual time scales as well. The question then arises whether the shelf-to-Slope Water Sea transport also plays a role in governing the separation of the Gulf Stream. The widely observed robustness of the width of the Gulf Stream appears to result from a tight balance between the release of available potential energy and the kinetic energy of the current. A broader current would release more energy than can be 'disposed of', while a narrower current requires more kinetic energy than is available to sustain it. It is shown that for plausible dissipation rates in the recirculation gyres, the amount of energy that needs to be expelled from the Gulf Stream is such a small fraction of that advected through as to be vitually undetectable, hence the stiffness of the current. (C) 1999 Elsevier Science Ltd. All rights reserved. Rossby, T. 1999On gyre interaction9Deep-Sea Research II46 1-2139-164N Rossby, T. 2000LFWarm-water pathways in the Subpolar North Atlantic: Some case studies.WOCE NewsletterA38Roule, L 1915ZSSur les poissons abyssaux de la famille des Brotulids dans lOcan Atlantique nordRKComptes Rendus des Scances hbdomadaires de lAcadmie des Sciences, Parisr CLXI 56-58n RUDENKO, M. V 198282Morphological peculiarities of the Reykjanes Ridge82The union conference of oceanographers. Sevastopol  7(1) 101-102n in Russian RUDENKO, M. VL 1986F@Geomorphology of the reef zone of the Reykjanes Ridge in 5830N Okeanologiya  26(4)631-638 in Russian309-315$://A1992HT43300017Rudenko, M. V.vpSome Results Research of the Seamounts in the Atlantic-Ocean on the Submarine Inhabited Apparatus Pisces and Mir OkeanologiyaOn the basis of the original data of the echo-sounding surveys and visual observation from the submarine apparatus the opinion about nature, morphologic differences of seamounts as a result of the regional tectonic and plate tectonic is given.i Okeanologiya 1992Mar-Apr322'd^PP SHIRSHOV OCEANOL INST,KALININGRAD,USSR RUDENKO MV PP SHIRSHOV OCEANOL INST,KALININGRAD,USSR81Times Cited: 0 Russian Article HT433 OKEANOLOGIYAISI:A1992HT43300017 Rudenko, M.V. 19922,Pisces and Mir Studies on Atlantic Seamounts Oceanology322e208-211g(!Seamounts, Atlantic, submersiblesDetailed echo-sounding measurements and observations from submersibles are used to demonstrate geological and tectonical differences in origin, growth, and morphology of Atlantic seamounts.B;RVACHEV, V. D. V. V. KOLESNIKOV R. V. KASABOV A. L. SOROKIN  198481Underwater mountains relief of the North Atlantic5@: Problems of the fisheries oceanography of the North Basin  60-71 in RussianSAGALEVICH, A. M 1987PIOceanography and underwater manned apparatuses. Methods of investigationsf NaukaA 256 in Russian280-289$://A1993LD67500004tHBSaiz, E. Tiselius, P. Jonsson, P. R. Verity, P. Paffenhofer, G. A.ngExperimental Records of the Effects of Food Patchiness and Predation on Egg-Production of Acartia-Tonsa Limnology and Oceanographyplanktonic copepod; marine copepod; vertical migration; zooplankton; phytoplankton; heterogeneity; environments; behavior; microscale; ingestionThe effects of predation and spatial patchiness in food distribution on egg production of the marine calanoid copepod Acartia tonsa were investigated in the laboratory. A postexperiment egg production method was developed to override the decline in number of copepods due to predation. The copepods were able to remain in food patches about 41-47% of the time, and consequently egg production rates were higher than expected from the average food concentration. Predation by the calanoid copepod Labidocera aestiva tended to increase egg production rates of A. tonsa. The interaction of patchiness and predation resulted in relatively less time spent by A. tonsa in the food patches, probably as a consequence of conflict between hunger level and predation risk.Limnol. Oceanogr. 1993 Mar382'SKIDAWAY INST OCEANOG,SAVANNAH,GA 31416 TJARNO MARINE BIOL LAB,S-45296 STROMSTAD,SWEDEN SKIDAWAY INST OCEANOG,SAVANNAH,GA 31416<5Times Cited: 24 English Article LD675 LIMNOL OCEANOGRISI:A1993LD67500004("Saldanha, L M. Biscoito in press aGaidropsarus mauli a new species of gadid fish from the Lucky Strike hydrothermal vent site (mid- Atlantic Ridge) and the Biscay SlopeCopeia, in press Saldanha, L 1977d^Poissons capturs et photographis lors des plongs du bathyscaphe Archimde aux Aores 1969  Arquivos do Museu Bocage 2 Srie, VII,3  35-50 Saldanha, L 1980HB Fauna submarina Atlntica - Portugal continental, Aores, MadeiraEuropa-Amrica 203 Saldanha, L. 1991D>A proteco e conservao do meio marinho nos Aores e Madeira ,&Dias,E. Carretas, J. P. Cordeiro, P.f_Primeiras Jornadas de Protecco do Meio Ambiente (Aores, Madeira, Canrias e Cabo Verde) 1988 *$SRTA/DRA and CMAH, Angra do Herosmo315-317s \1  Guinehut, S Gunkel, J. Gunson, J.Gurney, W. S. C. Gurney, W.S.CGURVICH., E. G.GUSHCHIN, A. V.Gushchin, A.V. Haedrich, R.Haedrich, R. L.Haedrich, R.L. Hamer, K. C.Hamilton, D. C. Harbison, G.R Harbour, D.Harbour, D. S. Harbour, D.S Harding, G.C. Hardy, A.CHAREIDE, N.-R.Hargrave, B.T.Hargreaves, P. M. Harris, L. R. Harris, L.R Harris, R. P. Harris, R.PHarrison, W.G.Hartog, J. C. den Harvey, J. Hastie, L. C. Haury, L. Haury, L.RHawkins, S. J. Hay, S. J. Hays, G. C. Hays, G.CHead, E. J. H. Head, E.J.H Head, R. N. Head, R.N Heath, M. F. Heath, M. R. Heath, M.RHeemstra, P. C.Hemleben, C.H. Henrich, RHeptner, M. V.Herring, P. J. Hewitson, L. Heyman, R.P.Heywood, K. J. Heywood, K.JHilgendorf, F. Hilton, G.M Hilton, G.M. Hilton_G Hilton_GM Hind, A. T. Hind, A.T Hjort, Johan Hobday, A. Hogg, N.G.Hollweg, J. V. Houston Huang, C. Huber, R Hughes, K. Hulsemann, K Humes, A. G. Humes, A.G Hureau, J. C.Hureau, J.- C. Hureau, J.-C. Huskin, I Ibanez, F. ILJIN, A. V.INIPIpavich, F. M. Irigoien, X. Irogoien, X Isidro, E. Isidro, E. J. Isidro, H. A. IVANOV, E. E.IVANOV., V. E. Iwamoto, T. J, Bedoya J., Bedoya J., Geffen A.Jaroslow, G. E. Jensen, K. R.John, A. W. G. Johnsen, S. Johnson, R.K. Joint, IJonasdottir, S. H. Jones, M.BJonsson, P. R. Joos, R. Juniper, K. Kaartvedt, S.KALUGIN, A. N. Kann, L.KAPRALOVA, V. P.KARASEV., A. B.KARASEVA, E. I. Karrer, C.KASABOV, R. V.KASABOV., R. V.KASATKIN, V. I.KASHKIN, N. I.Kaufmann, R. S. Kaupp, S.E Keating, B.H. KELLER, N. B.KEMENOV, V. E.KEMENOV., V. E. Kennedy, H. Kerdoncuff, JKHARZOVA., L. P.KHLIVNOY, V. N.Khripounoff, A.KHROMOV, D. N. Khromov, D.N. Kiefer, D. A. Kikawa, S. Kirby, T.KISELEV., V. N.KISLITSYN, S. P.KISLYAKOV, A. G. Kissel, C. KJERSTAD., M.Klaveren, P. van.KLENOVA, M. V.KLIMENKOV, A. I. Klomp, N. I.Klyuchnik, T.S. Knauer, G. A. Knauer, G.A Knud, S Knudsen, J.Kobyliansky, S. G. Koefoed, E. Koeve, W Koeve, W. Kolber, Z.KOLCHIN, V. A.KOLESNIKOV, V. V.KOLESNIKOV., V. G.KOLESNIKOV., V. V.KOLINKO, A. V.Kolmakov, Yu.A.KOLODNITSKY, B. V.KONOVALENKO., I. I.KONSTANTINOVA, L. L.KONSTANTINOVA., L. L. Koppelmann, RKoppelmann, R. KOPTEV, A. V.KOPTEV., A. V. Korytov, V.G. Korzun, Yu.V Korzun, Yu.V. Koslow, J.A.KOTENEV, B. N.KOTLYAR, A. N.KOVALEVA, A. A. Krause, D. C. Krauss, W. Krug, H. Krug, H. M.Krug, H. M. S. Krug, M. H.Kucheruk, N. V. KUKUEV KUKUEV, E. I.KUKUEV, E. I.. Kukuev, E.I.KUKUEV., E. I.KUSMORSKAYA, A. P.KUZMICHEV., A. P.KUZMINA, V. I.KUZMINA., V. I.KUZNETSOV, A. P.KUZNETSOVA, L. N.L. V. PASHKOVA LaCasce, J. Laj, C. Lallier, F. Lampert, WLampitt, R. S. Lampitt, R.S Lamy, F Lamy, F. Lance, J LANGEDAL, J. Languir, C.Laptikhovsky, V.VLaptikhovsky, V.V. Laranjo_M Larnicol, G Latif, M LAVROV, V. M.LAVROV., V. M. zKXJIyx. Dias, M. L.e 1991tm Pesca exploratria com palangre em guas dos grupos central e oriental do Arquiplago dos Aores (1979-1983)c0)Relatrios Tcnicos e Cientficos do INIP, Lisboa (46) Novembro 19911 26ppB://A1991HF188000094HBVinogradov, M. E. Shushkina, E. A. Gorbunov, A. E. Shachkov, N. L.ZTVertical-Distribution of Mesoplankton and Macroplankton in the Costa-Rica Dom Region Okeanologiya,%eastern tropical pacific; micronekton60The quantitative distribution of meso- and macroplankton was studied in Costa-Rica DOMe region for the layer 0-2000 m, using 150-l bathometers, closed nets and direct countings from manned submersible <>. The high mesoplankton biomass in the upper mixed layer here is compared to that in the richest shelf water off Peru. Below it maximum plankton abundance (to 2 g.m-3) was found in the upper (350-420 m) and lower (550-640 m) parts of O2-minimum layer (0,15-0,2 ml O2/l). Eucalanus inermis (V and VI copepodit stages) mainly contributed to this abundance. The day euphausiid concentrations were observed immediately upon the upper eucalanus layer, and under it and mostly under the lower eucalanus layer lantern fish assemblages occur. At similar low O2 concentrations, mesoplankton quantity in the middle of O2-Minimum layer was two orders less than in its upper and lower parts. According to estimations from <>, in the whole 0-2000 m layer jellylike animals (74%) mostly contributed to the wet biomass, and copepods and lantern fish to that in carbon units. Okeanologiya 1991Sep-Oct31581Times Cited: 4 Russian Article HF188 OKEANOLOGIYAISI:A1991HF18800009115-127$://A1992HN11400015("Vinogradov, M. E. Shushkina, E. A.Peculiarities of Mesoplankton and Macroplankton Vertical- Distribution in the Central Tropical Areas of the Northern Pacific-Ocean OkeanologiyaregionsHAVertical distribution of the total biomass and of the major meso- and macroplankton groups in the central oligotrophic areas of the Northern Pacific is considered based on the collections with the 150 l water bottles and the BR 113/140 plankton net as well as on direct counts from the <> submersible. The mesoplankton biomass in the upper 200 m layer varies from 3.1 to 8.6 g/m2, however, at local patches of salps it may become as great as 98 g/m2. In macroplankton from depths down to 2-3 km gelatinous animals prevail over other forms giving 97-98% in wet weight and more than 30-70% in C(org). They are followed by micronecton fishes (up to 40% in C(org)). The role of biomass of other groups accounted visually from the <> submersible is negligible. The specific distribution of animals at some stations is discussed. Okeanologiya 1992Jan-Feb321'^WPP SHIRSHOV OCEANOL INST,MOSCOW,USSR VINOGRADOV ME PP SHIRSHOV OCEANOL INST,MOSCOW,USSR81Times Cited: 1 Russian Article HN114 OKEANOLOGIYAISI:A1992HN11400015569-573$://A1995RZ52000012HAVinogradov, M. E. Shushkina, E. A. Bulgakova, Y. V. Serobaba,, IIhbThe Consumption of Zooplankton by Comb-Jelly Mnemiopsis-Leidyi and Pelagic Fishes in the Black-Sea Okeanologiya community2,Quantity of the Black Sea plankton consumed by Mnemiopsis was estimated in comparison with total plankton production and its part, consumed by most abundant planktivorous fishes. During the period of the mass development of Mnemiopsis (1989 - 1990) it consumed daily up to 7% of biomass and more than 50% of daily production of the zooplankton consumable to fish. The consumption of zooplankton by fishes was a half of that of Mnemiposis during the time of its mass development(in 1989) and then was comparable to it. In summer fishes and Mnemiopsis together consumed 6 - 13% of the fodder zooplankton biomass and 20 - 120% of its production. Harsh feeding competition has caused the catastrophic decreasing of catches of the planktivorous fishes just within the peak time of Mnemiopsis development and after it. Okeanologiya 1995Jul-Aug354'PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA KERCH SO FISHERY & OCEANOG RES INST,KERCH,UKRAINE VINOGRADOV ME PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA81Times Cited: 8 Russian Article RZ520 OKEANOLOGIYAISI:A1995RZ52000012 71-79$://A1996UC56700011<5Vinogradov, M. E. Vereshchaka, A. L. Shushkina, E. A.sVertical structure of the zooplankton communities in the oligotrophic areas of the Northern Atlantic, and influence of the hydrothermal vent Okeanologiyadeep-sea; scattering layer; benthopelagic plankton; insitu rates; ocean; plume; macrozooplankton; peculiarities; productivity; californiaPatterns of the vertical distribution of the zooplankton above the hydrothermal vents TAG (26 degrees N) and Broken Spur (29 degrees N), Middle Atlantic Ridge, are presented. Material was collected with 150-1 water bottles. BR nets, the data of the direct observation from DSRV ''Mir'', are also used. Local enrichment of the plankton at a distance of several tens and hundreds of meter above the bottom is shown to be absent. The water layer adjacent to the bottom, is dominated by the benthopelagic shrimps of the family Alvinocarididae; net plankton is almost lacking, bottle plankton is rare, the share of dead specimens being high. A supposition that hydrothermal ecosystens are sufficiently closed energetically, is done. Okeanologiya 1996Jan-Feb361'b[PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA Vinogradov ME PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA82Times Cited: 11 Russian Article UC567 OKEANOLOGIYAISI:A1996UC56700011694-702$://00007742680000782Shushkina, E. A. Vinogradov, M. E. Lebedeva, L. P.The biotic balance in the ocean and estimation of the organic matter flux from the epipelagial made on the basis of satellites and field data OkeanologiyaRLpacific-ocean; world ocean; ecosystems; phytoplankton; communities; planktonhaOn the basis of satellite estimation of chlorophyll concentration in the near-surface layers and correlated distribution of various ecosystem parameters (which had been revealed during the ecosystem cruises of Oceanology Institute, Russian Academy of Sciences), the elements of biotic balance of the oceanic pelagial were calculated. Algorithms described earlier have allowed to calculate values of production of the main ecosystem components (phytoplankton, bacteria, protrozoans, mesoplankton) in trophically variable oceanic areas. The shares of these components in the total heterotrophic destruction were evaluated. The rates of detritus production and values of its flux from epipelagial to depths >200 m were calculated. In various areas values of this flux range from 18 to 5% of the primary photoshynthetic production and from 50 to 15% of the total detritus production in the upper 200-m layer. The total heterotrophic destruction in the oceanic epipelagial (0-200 m) was estimated as 86 x 10(9) t C per year and the biotic balance appears when the value of the total primary production is 100 x 109 t per year.h Okeanologiya 1998Sep-Octv385 'PP Shirshov Oceanol Inst, Moscow, Russia PP Shirshov Oceanol Inst, Moscow, Russia Shushkina EA PP Shirshov Oceanol Inst, Moscow, Russiat81Times Cited: 3 Russian Article 146KA OKEANOLOGIYAEISI:0000774268000073768-775$://000083791700014F@Shushkina, E. A. Vinogradov, M. E. Dyakonov, V. Y. Nezlin, N. P.Structural peculiarities of epipelagic communities of the North Atlantic in the waters of different productivity estimated from remote sensing Okeanologiya>7pacific-ocean; world ocean; satellite; plankton; stockstnThe calculated and measured biomass values of small (<3 mm), large (3-30 mm) and total mesoplankton were verfied (compared). Two methods were used to estimate these integral parameters of epipelagic communities. Firstly, we used the estimated earlier regression equations, which correlate these parameters with water transparency. Secondly, we compared the measured values of the listed parameters with calculated mean values typical for waters of different productivity estimated from remote sensed maps produced by NASA. We compared the data for 15 stations collected in September-December in the waters of different productivity in the North Atlantic. In the warm regions (to south from 40 degrees N) the measured and calculated values were close to each other. In the boreal regions in autumn the bulk of mesoplankton descended to deep layers due to seasonal migrations; hence, the agreement between the measured and calculated values was broken. Thus, the correction to season should be included into the actual correlation equations between water transparency and mesoplankton biomass (the integral index of water productivity). Okeanologiya 1999Sep-Octr395i'PP Shirshov Oceanol Inst, Moscow, Russia PP Shirshov Oceanol Inst, Moscow, Russia Shushkina EA PP Shirshov Oceanol Inst, Moscow, Russia581Times Cited: 1 Russian Article 257PX OKEANOLOGIYArISI:000083791700014ty: 1139-1145N$://A1992JH54000006f("Dower, J. Freeland, H. Juniper, K.F?A Strong Biological Response to Oceanic Flow Past Cobb Seamountl<6Deep-Sea Research Part a-Oceanographic Research PapersprofilesWe report results of a CTD and chlorophyll a survey from Cobb Seamount, a shallow seamount in the northeast Pacific. Our results show a several-fold increase in the standing crop of chlorophyll a is centred over the seamount. Current meter and drifter data indicate an anticyclonic deflection of deep currents around Cobb consistent with a theoretical stratified Taylor cone. Cobb differs from other seamounts where similar phenomena have been reported (OWENS and HOGG, 1980, Deep-Sea Research, 27, 1029-1045; GOULD et al., 1981, Deep-Sea Research, 28, 409-440; GENIN and BOEHLERT, 1985, Journal of Marine Research, 43, 907-924) in that its summit penetrates well into the euphotic zone. A Taylor column existing at such shallow depths could locally enhance primary production, providing a significant source of energy for higher trophic levels on the seamount. Indirect evidence for such a scenario comes from observations of a high biomass benthic community on Cobb Seamount. 1992Jul-Aug39 7-8A'UNIV VICTORIA,DEPT BIOL,POB 1700,VICTORIA V8W 2Y2,BC,CANADA UNIV QUEBEC,DEPT OCEANOG,RIMOUSKI G5L 3A1,QUEBEC,CANADA INST OCEAN SCI,SIDNEY V8L 4B2,BC,CANADA DOWER J UNIV VICTORIA,DEPT BIOL,POB 1700,VICTORIA V8W 2Y2,BC,CANADAnJCTimes Cited: 18 English Article JH540 DEEP-SEA RES PT A-OCEANOG RES ISI:A1992JH54000006o'&F%RSAMOKHVALOV, V. Vo 1982{On possibilities of development of fishery for deep-sea redfish in the Irminger Sea and grenadier on the Mid-Atlantic RidgeIncrease of effectiveness of the fishing fleet and further development in the open part of the ocean. Materials of the union conference 102-105 in Russian"Santos, R. S. Martins, H. R. 1987vpEstudos sobre as condies ecolgicas da Lagoa do Santo Cristo (Ilha de S. Jorge), em especial das suas ameijoas4-Relatrio da VII Semana das Pescas dos Aores7(1986)159-1740)Santos, R. S. Goulart, E. Monteiro, L. R. 1989wAbundncia e crescimento da ameijoa Tapes decussatus na Lagoa do Santo Cristo: Aspectos da sua conservao e explorao$52,Relatrio da IX Semana das Pescas dos Aores9(1988)258-2862+Santos, R. S. Martins, H. R. Hawkins, S. J.e 1990pjRelatrio de estudos sobre o estado das populaes de lapas do Arquiplago dos Aores e da Ilha da Madeira2+Relatrio da X Semana das Pescas dos Aores 10 (1989)137-161 =<M\VComplex fisheries investigations of PINRO on the North Basin: results and perspectivesXTComplex fishery investigations of PINRO on the North Basin: results and perspectivesPMComplex investigation of the open part of the Atlantic Ocean. Selected papers4.Complex studying of the Atlantic Ocean nature40Complex studying of nature of the Atlantic Ocean`ZComplex studying of nature of the Atlantic Ocean: theses of the fourth regional conference0,Complex studying of the Atlantic Ocean Basin0-Complex studying of the Atlantic Ocean nature<7Complex studying of the open part of the Atlantic OceanComptes Rendus De L Academie Des Sciences Serie Iii-Sciences De La Vie-Life Sciences Comptes Rendus Acad. Sci. Ser. III-Sci. Vie-Life Sci.PKComptes Rendus des Scances hbdomadaires de lAcadmie des Sciences, ParisLGComptes Rendus des Sances de lAcadmie des Sciences (10 Janvier 1887) Condord^Conference of young scientists of PINRO by results of investigations in 1971. Theses of papers@:Conseil Permanent pour lExploration de la Mer, Copenhague(#Conservation Biology Conserv. Biol. Continental Shelf ResearchLFContributions in Science, Natural History Museum of Los Angeles County Copeia Copeia, 1957Copeia, in press,'Courrier Forschungsinstitut Senckenberg Crustaceana Cybium DAN SSSR Dana-ReportDeep Sea ResearchDeep Sea Research- I Deep Water Calenoid CopepodsDeep-Sea NewsletterDeep-Sea ResearchDeep-Sea Research IDeep-Sea Research IIDeep-Sea Research Part A<6Deep-Sea Research Part a-Oceanographic Research Papersd_Deep-Sea Research Part I-Oceanographic Research Papers Deep-Sea Res. Part I-Oceanogr. Res. Pap.hdDeep-Sea Research Part Ii-Topical Studies in Oceanography Deep-Sea Res. Part II-Top. Stud. Oceanogr. Deep-Sea Water circulation<9Deep-Water Fisheries of the North Atlantic Oceanic SlopeXUDeep-water fishes: Annual International Symp., 1-5 July 1996. Programme and abstracts DiscoveryDiscovery Reports Doklady Akademii Nauk, 322(5)@=dc<BARANOV, E. I. 1972lfMean monthly locations of hydrological fronts in the northern part of the Atlantic Ocean. Okeanologiya  12(2)217-225 in Russian Bard, F. X. 1986zDistribution et abondance des diffrentes espces de thonids dans la Rgion des Aores en relation avec l'Atlantique nord2,Relatrio da VI Semana das Pescas dos Aores6(1985)l 59-82yFisheries biology; parameters; fisheries; statistics; biology; physiology; ecology; vertical distribution; feeding; migration; Geographical distribution Bard, F. X.r 1987@:Pcheries et tat des stocks d'espadon en Ocan Atlantique4-Relatrio da VII Semana das Pescas dos Aores07 (1986) 91-110JDFisheries biology; parameters; fisheries; statistics; biology;growthBARINOV, A. A. 1977Distribution and concentration of some commercial species in dependence on characteristics of seasonal thermocline in the North Atlantic:3Problems of fishery oceanography of the World Ocean.111-112i in RussianBARINOV, A. A.A 1981TNDynamics of frontal zones of the surface layer (0-200 m) of the North AtlanticXQOceanographic bases of formation of biological productivity of the North Atlanticc 85-116 in RussiansBARINOV, A. A. 1986Large-scale features of spatial/temporal variability of zones of up- and down-welling in the epi- and mezopelagic layers of the open part of the Atlantic Ocean2+ Biological resources of the Atlantic Ocean 22-51  in Russian Barreiros, J. P. 1995aAspectos do comportamento e da reproduo do mero Epinephelus marginatus (Lowe, 1934), nos Aoress2H:4Provas de Aptido Pedaggica e Capacidade Cientfica Angra do Herosmo @9Departamento de Cicias Agrrias, Universidade dos Aores 95pp6/Ethology; behavioural ecology; ecology; feeding9 Barrois, Th. 1888<5Catalogue des crustacs marins, recueillis aux Aoresa Lille\ 110 pp 6549-6563$://A1995QT22200003lD=Batchelder, H. P. Vankeuren, J. R. Vaillancourt, R. Swift, E.hSpatial and Temporal Distributions of Acoustically Estimated Zooplankton Biomass near the Marine Light-Mixed Layers Station (59-Degrees-30'n, 21-Degrees-00'w) in the North-Atlantic in May-1991,&Journal of Geophysical Research-Oceanspidoppler current profiler; phaeocystis-pouchetii; plankton; predation; abundance; migration; design; model-Temporal and spatial acoustic backscatter estimates of zooplankton biomass were made using an unmodified hull-mounted 153-kHz acoustic Doppler current profiler (ADCP) during the May 1998 Marine Light-Mixed Layers (MLML) cruises to the North Atlantic. Relative backscattcr from the ADCP was converted to zooplankton biomass estimates using individual plankton taxa abundances amid weights from zooplankton samples collected during the cruises. There was a small but consistent diet pattern in the 20 to 250-m depth-integrated backscatter, with highest values during darkness. Removal of the diet signal with harmonic analysis revealed slightly higher zooplankton biomass to the southwest and west of the mooring than to the northeast, in common with gradients in surface temperature and chlorophyll during the mapping cruise. Overall however, depth-integrated zooplankton biomass during the mapping cruise varied by only a factor of 2, comparable to what one observes in replicate plankton rows. The nightly 0 to 2.50-m obliquely collected zooplankton samples (May 16-24) indicated increasing densities (amid biomasses) of probable zooplankton scatterers (especially the copepod Calanus finmarchicus) during middle to late May, soon after the peak in the spring phytoplankton bloom. This increase in May was mirrored by a comparable increase in depth- integrated acoustic backscatter. The distribution of zooplankton charged following two 50+ kn (1 kn = 1.85 km h(-1)) wind storms on May 19 amid May 21; zooplankton biomass was higher and extended much deeper in the water column at night following these strong mixing episodes. Before the storm events, the patterns of zooplankton diel vertical redistribution were consistent from day to day. Diel patterns of zooplankton variability measured using shipboard acoustics are qualitatively similar to patterns observed from an ADCP on the MLML mooring, presenting the possibility of calculating a nearly continuous seasonal measure of zooplankton biomass from the mooring ADCP data.J. Geophys. Res.-Oceans 1995 Apr 15 100C4@:Times Cited: 12 English Article QT222 J GEOPHYS RES-OCEANSISI:A1995QT222000036 44-66$://A1996TX86500002f 1562-1580$://000167224000005/Heath, M. R. Astthorsson, O. S. Dunn, J. Ellertsen, B. Gaard, E. Gislason, A. Gurney, W. S. C. Hind, A. T. Irigoien, X. Melle, W. Niehoff, B. Olsen, K. Skreslet, S. Tande, K. S.hbComparative analysis of Calanus finmarchicus demography at locations around the Northeast Atlantic$Ices Journal of Marine ScienceAtlantic; egg production; modelling stage development; time- series sampling; zooplankton copepod; sea; zooplankton; abundance; biomass; icelandZSStandardized time-series sampling was carried out throughout 1997 at seven locations around the Northeast Atlantic to investigate regional variations in the seasonal demography of Calanus finmarchicus. Sites ranged from an inshore location in the North Sea. where C. finmarchicus formed only a small component of the zooplankton (< 10 mgC m(-2) during spring and early summer). to the shelf south of Iceland. and Weathership M in the Norwegian Sea. where the species dominated the zooplankton (> 2000 mgC m(-2) during spring and summer). The internal consistency of the demographic time-series from each site was investigated by three partial models of life-cycle processes. In general. the demography of late copepodites could be accounted for by a relatively simple forecast model of stage development and diapause. However. there M as a large discrepancy between nowcast estimates of egg production based on female abundance. temperature. and chlorophyll. and hindcast simulations of the egg production required to account for the observed abundance of early copepodite stages. The results point to a gap in our understanding of seasonal variations in rates of egg production and/or survival of nauplii. Overall. the population sampled at Weathership M appeared to be reasonably self-contained, but all other sites were reliant on invasion of overwintered stock in spring. At least two generations were observed at all but one site, but the extent to which these were generated by discrete bursts of egg production varied between sites and seemed to be partly dependent on the proximity to an overwintering location.ICES J. Mar. Sci. 2000 Dec576'Dept Agr & Fisheries Scotland, Marine Lab, POB 101,Victoria Rd, Aberdeen AB9 9DB, Scotland Dept Agr & Fisheries Scotland, Marine Lab, Aberdeen AB9 9DB, Scotland Marine Res Inst, IS-121 Reykjavik, Iceland Inst Marine Res, N-5817 Bergen, Norway Fisheries Lab Faroes, FO-110 Torshavn, Faroe Isl, Denmark Univ Strathclyde, Dept Stat & Modelling Sci, Glasgow G1 1XH, Lanark, Scotland Plymouth Marine Lab, Plymouth, Devon, England Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany Nordland Coll, Fac Fisheries & Nat Sci, N-8049 Bodo, Norway Univ Tromso, Norwegian Coll Fishery Sci, N-9037 Tromso, Norway Heath MR Dept Agr & Fisheries Scotland, Marine Lab, POB 101,Victoria Rd, Aberdeen AB9 9DB, Scotland:3Times Cited: 1 English Article 406PH ICES J MAR SCIISI:000167224000005 Pereira, J. A. G. 1994TA pesca do atum nos Aores e o atum patudo (Thunnus obesus, Lowe, 1839) do Atlntico,:  Ponta Delgada Universidade dos Aores: 330pp;Tese de Doutoramento Pettersson, H 1957.( The ship, its equipment, and the voyage:4Reports of the Swedish Deep-Sea Expedition 1947-1948Volume I, No. 1 1-123l Prs, J. Mo 1992hbLe bathyscaphe franais Archimde aux Aores: tudes bionomiques et ecologiques du benthos profond Aoreana (Suplemento 1992)| 237-264:4Pierce, G. J. P. R. Boyle L. C. Hastie M. B. Santos  1994RKDiets of squid Loligo forbesi and Loligo vulgaris in the northeast AtlanticoFisheries Research21 (1-2)149-163Pierrot-Bults, A.C 1975\Utaxonomy and zoogeography of sagitta planctonis Steinhaus, 1896 in the Atlantic Oceann$Institute of Taxonomic Zoology23(297)n 27-51 Pietsch, T. W. 1972piXIX Systematics and distribution of Ceratioid Anglerfishes of the Genus Chaenophryne (Family Oneirodidae)4-Bulletin of the Museum of Comparative Zoology 147, 2  75-99 Pietsch, T. W  1972XIX Systematics and distribution of Ceratioid fishes of the Genus Dolopichthys (Family Oneirodidae), with the description of a new species(! Archiv fr Fischereiwissenschaft XXIII, 1 1-28Pietsch, T. W. 1975lfSystematics and distribution of Ceratioidei anglerfishes of a new genus and species from the banda SeaLFContributions in Science, Natural History Museum of Los Angeles County  1-25I Pietsch, T. W. 1979lfSystematics and distribution of Ceratioidei anglerfishes of a new genus and species from the banda SeaLFContributions in Science, Natural History Museum of Los Angeles County  1-25I Pietsch, T. W. 1986ngSystematics and distribution of bathypelagic anglerfishes of the family Ceratiidae (Order: Lophiformes) Copeia (2)479-4932$Pietsch, T. W D. B. Grobecker 1987PIFrogfishes of the World: Systematics, Zoogeography and Behavioral Ecology:81Standford University Press, Standford, Californiae  xii 420Pinchukov, M.A.h 1975xqDistribution, biology and intraspecies structure of the Atlantic flying squid Ommastrephes bartrami Lesueur, 1821a60Unpublished M.A. Thesis, Kazan, Kazan University 68 p.I In Russian 33-41$://A1997XZ98100004RKPiontkovski, S. A. Tokarev, Y. N. Bitukov, E. P. Williams, R. Kiefer, D. A.4.The bioluminescent field of the Atlantic Ocean$Marine Ecology-Progress Seriesplankton bioluminescence; spatial heterogeneity; Atlantic Ocean epipelagic bioluminescence; north-atlantic; sargasso sea; zooplankton.Data from 20 yr (1970 to 1990) of expeditions by the Institute of Biology of the Southern Seas, Ukraine, to the tropical Atlantic Ocean are summarised in the form of a macroscale contour map. The bioluminescent intensity of plankton in the upper 100 m layer was analysed from 2924 casts. Several zones of enhanced bioluminescence are shown from the annual averages (0 to 100 m), associated with major upwellings along the African coast and geostrophic currents forming the westward water mass transport. The macroscale trend of spatial distribution and the stochastic component of the bioluminescence were partitioned by analysis of the autocorrelation functions. General agreement between bioluminescence and zooplankton biomass distributions was noted on an ocean basin scale. The contribution of phyto-and zooplankton fractions to the formation of the integrated bioluminescence potential can Vary significantly in the upper 100 m layer over regions within the tropical zone.Mar. Ecol.-Prog. Ser. 1997 156>7Times Cited: 2 English Article XZ981 MAR ECOL-PROGR SERISI:A1997XZ98100004Institute of Taxonomic Zoology23(297)n 27-51  33-41$://A1997XZ98100004RKPiontkovski, S. A. Tokarev, Y. N. Bitukov, E. P. Williams, R. Kiefer, D. A.4.The bioluminescent field of the Atlantic Ocean$Marine Ecology-Progress Seriesplankton bioluminescence; spatial heterogeneity; Atlantic Ocean epipelagic bioluminescence; north-atlantic; sargasso sea; zooplankton.Data from 20 yr (1970 to 1990) of expeditions by the Institute of Biology of the Southern Seas, Ukraine, to the tropical Atlantic Ocean are summarised in the form of a macroscale contour map. The bioluminescent intensity of plankton in the upper 100 m layer was analysed from 2924 casts. Several zones of enhanced bioluminescence are shown from the annual averages (0 to 100 m), associated with major upwellings along the African coast and geostrophic currents forming the westward water mass transport. The macroscale trend of spatial distribution and the stochastic component of the bioluminescence were partitioned by analysis of the autocorrelation functions. General agreement between bioluminescence and zooplankton biomass distributions was noted on an ocean basin scale. The contribution of phyto-and zooplankton fractions to the formation of the integrated bioluminescence potential can Vary significantly in the upper 100 m layer over regions within the tropical zone.Mar. Ecol.-Prog. Ser. 1997 156>7Times Cited: 2 English Article XZ981 MAR ECOL-PROGR SERISI:A1997XZ981000044 N Levin, A.B. Moiseev, S.I.r 1988^XVertical distribution and behavior of the squid, Gonatus fabricii, in the North AtlanticLE III All-USSR Conference on Marine Biology, Sevastopol, October, 19888*$Abstracts of Communications. Part 1.280-281  In RussianLima,S.L Dill,L.M 1989TMBehavioral decisions made under the risk of predation:a review and prospectusa619-6394.LISITSYN, A. P. Yu. A. BOGDANOV E. G. GURVICH. 199082Hydrothermal formations of reef zones of the ocean  Nauka 256 pp in Russian& LISOVSKY, S. F. I. P. SHESTOPAL. 1990^WOn perspectives of development of ling lining for demersal fishes in the North Atlantic;f_The union conference Reserve food biological resources of the open ocean and seas of the USSRR116-1181 in Russian LITVIN, V. M.  1966^XNew data on structure of a shelf and insular slope in the area of the South-West IcelandD>Materialy rybokhozyaistvennykh issledovanii severnogo basseina 6 97-107 in Russian LITVIN, V. M.  197882New map of the relief of the Atlantic Ocean bottomDAN SSSR 243 (4) 1002-1005n in Russian LITVIN, V. M.K 1980haMorphostructure of the Atlantic Ocean bottom and its development in Mesozoic and Cenozoic periods  Nauka 124 pp in Russian 1165-1184$://A1996VU62300002i*#Llewellyn, C. A. Mantoura, R. F. C.6|Pigment biomarkers and particulate carbon in the upper water column compared to the ocean interior of the northeast Atlantic<6Deep-Sea Research Part I-Oceanographic Research Paperspjspring bloom; deep-sea; phytoplankton; 47-degrees-n; 20- degrees-w; chlorophylls; succession; matter; hplc p iIn situ pumps (SAPs) were used to collect particulates from the upper and interior of the ocean at 47, 52, 56 and 60 degrees N along the 20 degrees W meridian in the northeast Atlantic during 1989. The particulates were analysed for carbon, chlorophylls, chlorophyll degradation products and carotenoids covering a four order of magnitude change in concentration. There was a logarithmic decline in pigment and carbon concentrations from the surface to 1000 m, below which concentrations remained constant. The gradient of the decline for chlorophyll a (chl a) appeared to be directly related to the flux of organic matter from the upper ocean. 19'- Hexanoyloxyfucoxanthin (prymnesiophtyes) and fucoxanthin (diatoms) persisted throughout the water column revealing the importance of prymnesiophytes as well as diatoms in the transfer of biogenic material into the ocean interior. At 60 degrees N there was a two order of magnitude decrease in chl a concentrations in the ocean interior compared to the surface (1 mu g chl a 1(-1)). At 47 degrees, surface chl a concentrations were similar to those 60 degrees N, but in the ocean interior there was a three order of magnitude decrease. Chlorophyll a concentrations throughout the water column and differences in the type of assessory pigment present at the four latitudes were consistent with the timing of the spring bloom at each latitude. At 60 degrees N, we sampled at the end of the spring bloom, and fucoxanthin dominated. At 47 degrees N, the spring bloom was over, and 19'-hexanoyloxyfucoxanthin dominated. Pheophorbide a and pyropheophorbide a were the dominant chlorophyll degradation products, with highest concentrations in the north. Pyropheophorbide a became increasingly important with depth and towards the south. At least 50% of the organic carbon in the upper ocean could not be accounted for in terms of phytoplankton, zooplankton or bacteria, and we speculate that some of the unidentified carbon is related to microzooplankton faecal material. Carbon vertical profiles did not show the large latitudinal variation of the pigments, resulting in carbon/chl a ratios in the ocean interior at 47 degrees N (1855) being 6-fold greater than those at 60 degrees N. The ratios reflected the more highly degraded nature of the biogenic material in the ocean interior at 47 degrees N compared to 60 degrees N. Copyright (C) 1996 Elsevier Science Ltd.(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1996 Aug438'PLYMOUTH MARINE LAB,PROSPECT PL,W HOE,PLYMOUTH PL1 3DH,DEVON,ENGLAND Llewellyn CA PLYMOUTH MARINE LAB,PROSPECT PL,W HOE,PLYMOUTH PL1 3DH,DEVON,ENGLANDHBTimes Cited: 6 English Article VU623 DEEP-SEA RES PT I-OCEANOG RESISI:A1996VU62300002 Em  new-zealand nitrification nitrogen flux nordic seasnorthNorth AtlanticNorth Atlantic Deep Water north pacificnorth pacific seamountsnorth-atlanticnorth-atlantic currentNORTH-ATLANTIC CURRENT, GULF-STREAM MEANDERS, POTENTIAL VORTICITY, SURROUNDING WATERS, FLUID EXCHANGE, CAPE-HATTERAS, SARGASSO SEA, VARIABILITY, TRANSPORT, CIRCULATIONnorth-atlantic oceanNORTH-EAST ATLANTIC, WARM-CORE EDDY, FRONT SOUTHEAST, INGESTION RATE, CYCLONIC EDDY, ZOOPLANKTON, OCEAN, CHLOROPHYLL, PHYTOPLANKTON, REGION north-sea northeastnortheast atlanticnortheast atlantic-oceannortheast pacific northeastern atlantic-oceanNORTHEASTERN ATLANTIC-OCEAN, SANTA-CATALINA BASIN, DEEP-SEA FISH, ROCKALL TROUGH, NEAR-BOTTOM, MIDWATER, WATER, FLOOR, HYDROGRAPHY, ZOOPLANKTONnorthern indian-oceannorthern norway northwestern$northwestern mediterranean-seaNORTHWESTERN MEDITERRANEAN-SEA, VERTICAL NITROGEN FLUX, SUBMARINE CANYONS, RESPIRATORY CARBON, CALANUS-PACIFICUS, MIGRANT BIOTA, NEAR-BOTTOM, MIGRATION, COPEPOD, SHELF norway norwegian seanorwegian-greenland nova-scotianova-scotia shelfnutrient uptake nutrition observationsocean ocean-atmosphere interactions oceanic oceanic primary productionOCEANIC PRIMARY PRODUCTION, DISSOLVED ORGANIC-CARBON, PARTICLE MIXING RATES, EARLY DIAGENESIS, CENTRAL PACIFIC, EUMELI PROGRAM, SARGASSO SEA, MIXED-LAYER, DEEP-OCEAN, MATTER Oceanography open oceanOptical Plankton Counter,'OPTICAL PLANKTON COUNTER, HELGOLANDICUS optimization orange roughy ordinationoregon upwelling zoneorganic-carbonorganic-matter origin Oscillation overwintering ovigerity oxygenoxygen-consumptionozone depletion pacific pacific-ocean pacificus panama basin parameters particleparticle-bound bacteria particles particulate organic-matter patches patchiness patterns peculiaritiespelagic ecosystempenaeus-japonicusphaeocystis-pouchetiiphaeodarian radiolarians phospholipidsphotographic evidence$ photosynthetic energy-conversionphotosynthetic pigments$!photosynthetic primary production phylogenyphysical variability physiology phytoplanktonphytoplankton growthpigment destruction pigments planktonplankton bioluminescenceplankton communityplankton contact ratesplankton distributionplankton recorder surveyplanktonic copepod plasmaplume plumesPoecilostomatoidapolar mode water populationpopulation dynamicspopulation genetics population- populationspossible impact potentialpotential roleprawn predation pressurepreyprey selectionprimary production probes productivity profiles program pseudocalanusPUFA quantitative quantitative characteristicsradiocarbon calibrationrates red-sea reef fishes region regions reproductionreproductive-biology requirementsrespiratory carbonrestricted dispersal resuspensionReykjanes Ridgereykjanes-ridgerhincalanus-gigasridge ridge-transform intersections rift-valley riftia-pachyptila populationsrimicaris-exoculata river plumerockall trough rockfishes rotating flow$roughy hoplostethus-atlanticussssscccccc>>>>>>!!!!!!!!!!!!!!!!!!!NNNNNNNN,,,,eddd7##555////////////////ooo<<<<<<0000vvvv3333333` OOOO$+++++WWWWWWWWLLLSSCC^****XXXX?~~~QQQQ'.www~}|*{z("Guinehut,S Larnicol,G Le Traon,P.Y 2002ZSdesign of an array of profiling floats in the North atlantic from model simulations Journal of Marine Systemsr35 1-9i613-639$://000082594000003("Gunson, J. Oschlies, A. Garcon, V.Sensitivity of ecosystem parameters to simulated satellite ocean color data using a coupled physical-biological model of the North Atlantich Journal of Marine ResearchZTcirculation model; world ocean; assimilation; dynamics; station; optimization; flowsA means of assimilating simulated satellite ocean color data with a coupled physical-biological model of the North Atlantic Ocean is implemented, allowing the relative sensitivities of different biological parameters to those data to be investigated. The model consists of an eddy-permitting general circulation model derived from the WOCE Community Modeling Effort and a nitrogen-based, four-compartment NPZD marine ecosystem model. Many of the parameters in marine ecosystem models are poorly known and via assimilation, we hope to better constrain their values. The control parameters chosen for the variational assimilation are the model parameters involved in parameterizations of recycling as these are the most poorly known. Simulated observations are taken while following several floats seeded in varying dynamical biogeochemical provinces of the North Atlantic model domain over a six-month period. Twin experimental results show that, for the given functional forms of growth, mortality and grazing, the following parameters can be successfully recovered from simulated satellite ocean color data: nitrate and detrital recycling parameters in the trade wind domain, zooplankton parameters at higher latitudes (westerly wind and polar domains), and the phytoplankton mortality rate in all regions. By simultaneously assimilating ocean color data in different biological provinces, it becomes possible to successfully constrain all ecosystem parameters at once. J. Mar. Res. 1999 Jule574 4.Times Cited: 8 English Article 236HK J MAR RESISI:000082594000003("GUSHCHIN, A. V. E. I. KUKUEV 1981XQOn the composition of ichthyofauna of the northern part of the Mid-Atlantic Ridgeg(! Fishes of the open ocean. Moscowo 36-404 in RussianGUSHCHIN, A. V.S 1982piOn feeding of roundnose grenadier (Coryphaenoides rupestris) in thalassic bathyal of the North Atlantic 372-RP-D82 19 pp in RussianGUSHCHIN, A. V.S 1982|uFood composition of roundnose grenadier (Coryphaenoides rupestris) in thalassic bathyal waters of the North AtlanticPpiFeeding and food relations of fish and invertebrates of the Atlantic Ocean. Selected papers of AtlantNIRO  63-67 in RussianGUSHCHIN, A. V.S 1982~wFeeding and food relations of fish of the thalassic bathyal of the North Atlantic on the example of roundnose grenadierD$Abstract of the Doctor Thesist 21 pp.c in RussianGUSHCHIN, A. V.S 1982`YMaterials on feeding of mezopelagic fishes of the thalassic bathyal of the North Atlantic581 Insufficiently explored fishes of the open oceans  66-71 in RussianGushchin, A.V. 1983rlSquids in the feeding of blunt-nose rattail [Coryphaenoides rupestris] of the North Atlantic thalassobathyal*#Taxonomy and Ecology of CephalopodslF?Leningrad, Zoological Institute of the USSR Academy of Sciences1 134  In Russian %Fr 2,Lampitt,R.S Wishner,K.F Turley,C.M Angel,M.V 1993~xMarine snow studies in the NE Atlantic Ocean: distribution, composition and role as a food source for migrating planktonMarine Biology 116689-702VERTICAL NITROGEN FLUX, DIEL MIGRANT BIOTA, DEEP-SEA, CHROOCOCCOID CYANOBACTERIA, COASTAL WATERS, POTENTIAL ROLE, SINKING RATES, FECAL PELLETS, ZOOPLANKTON, PARTICLES zDuring a 25 d Lagrangian study in May and June 1990 in the Northeast Atlantic Ocean, marine snow aggregates were collected using a novel water bottle, and the composition was determined microscopically. The aggregates contained a characteristic signature of a matrix of bacteria, cyanobacteria and autotrophic picoplankton with inter alia inclusions of the tintiniid Dictyocysta elegans and large pennate diatoms. The concentration of bacteria and cyanobacteria was much greater on the aggregates than when free-living by factors of 100 to 6000 and 3000 to 2500000, respectively, depending on depth. Various species of crustacean plankton and micronekton were collected, and the faecal pellets produced after capture were examined. These often contained the marine snow signature, indicating that these organisms had been consuming marine snow. In some cases, marine snow material appeared to dominate the diet. This implies a food-chain short cut whereby material, normally too small to be consumed by the mesozooplankton, and considered to constitute the diet of the microplankton can become part of the diet of organisms higher in the food-chain. The micronekton was dominated by the amphipod Themisto compressa, whose pellets also contained the marine snow signature. Shipboard incubation experiments with this species indicated that (1) it does consume marine snow, and (2) its gut-passage time is sufficiently long for material it has eaten in the upper water to be defecated at its day-time depth of several hundred meters. Plankton and micronekton were collected with nets to examine their vertical distribution and diel migration and to put into context the significance of the flux of material in the guts of migrants. ''Gut flux'' for the T compressa population was calculated to be up to 2% of the flux measured simultaneously by drifting sediment traps and < 5% when all migrants are considered. The in situ abundance and distribution of marine snow aggregates (> 0.6 mm) was examined photographically. A sharp concentration peak was usually encountered in the depth range 40 to 80 m which was not associated with peaks of in situ fluorescence or attenuation but was just below or at the base of the upper mixed layer. The feeding behaviour of zooplankton and nekton may influence these concentration gradients to a considerable extent, and hence affect the flux due to passive settling of marine snow aggregates.Lance,J 1962TMEffects of water of reduced salinity on the vertical migration of zooplanktoneJournal marine biology42131-154l LAVROV, V. M.  1979(!Geology of the Mid-Atlantic Ridger Nauka.d 143 pp in Russian 97-167$://A1987G689900001u Lazzaro, X.thaA Review of Planktivorous Fishes - Their Evolution, Feeding Behaviors, Selectivities, and Impacts HydrobiologiaY'B7Croxall, J.P., Evans, P.G.H. and Schreiber, W.R. (Eds.)82Status and Conservation of the World's Seabirds. ,  Cambridge CBP& ICBP Technical Publication No. 2377-391Leal, J. H. Bouchet, P. 1991pjDistribution patterns and dispersal of prosobranch gastropods along a seamount chain in the Atlantic oceanHBJournal of the Marine Biological Association of the United Kingdom71 11-15:559-572$://A1993KJ95100031 &Lenz, J. Morales, A. Gunkel, J.sMesozooplankton Standing Stock During the North-Atlantic Spring Bloom Study in 1989 and Its Potential Grazing Pressure on Phytoplankton - a Comparison between Low, Medium and High- Latitudes@9Deep-Sea Research Part Ii-Topical Studies in Oceanographyttmmesopelagic community; diel migrations; calanus-pacificus; distributions; zooplankton; size; copepods; weightu60Within the framework of the JGOFS Pilot Study in 1989 mesozooplankton (0.2-20 mm) was sampled by means of a Hydro- Bios multinet in five depth strata (0-25, 25-50, 50-100, 100- 200, 200-500 m) during four Lagrangian drift experiments of 8- 14 days' duration at 18, 33, 46 and 58-degrees-N, to follow the seasonal progress of the phytoplankton spring bloom development in the northeast Atlantic. Mesozooplankton standing stock, measured as dry weight and ash-free dry weight, increased by a factor of about 6 from 18 to 58-degrees-N. Day/night differences amounted to 10-20% of the average and were-with one exception at 18-degrees-N-not statistically significant. Using the data on weight-specific respiration rates measured by colleagues on the same cruise, the ingestion rates and potential community grazing of mesozooplankton on phytoplankton within the upper 100 m of the water column were calculated. During all four drift experiments, quasi-steady-state conditions were observed in phyto- and zooplankton standing stock, primary production and daily sedimentation at 100 m depth. The maximum potential grazing rate by mesozooplankton accounted for about half of the daily primary production. Since sedimentation of fresh phytoplankton was negligible, it is concluded that the grazing pressure exercised by mesozooplankton together with micro- and nanozooplankton was responsible for keeping the phytoplankton standing stock at a more or less constant level during the investigated spring bloom in the four areas. Particle flux was thus dominated by zooplankton faecal material.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 199340 1-2tJCTimes Cited: 25 English Article KJ951 DEEP-SEA RES PT II-TOP ST OCEoISI:A1993KJ95100031 1\( Cowles, T. J. Coxson, C.Craddock, J. E. Crassous, P.<7Croxall, J.P., Evans, P.G.H. and Schreiber, W.R. (Eds.) Cunha, R. Curry, R. G. Curry, R.G Dadou, I Dadou, I. Daly, K. L. Dam, H. G. Dam, H.G. Dando, P.Daulmetov, A.A.Dautzenberg, P. Davies, I.M Dawson, J.De Stasio, B.T.Jrdel Nevo, A .J.del Nevo, A. J. del Nevo, A.J Delgado, J.DEMENIN, N. A. Depledge, M.Depledge, M. H.Desbruyeres, D.Desbruyres, D. Desoutter, M.DETINOVA, N. N. Deuser, W. G. Deuser, W.G Dias, E. Dias, M. L. Dill, L.M Dinter, W.P Dixon, D. R.DMITRIENKO, A. I. Dodson, SDOLGANOV, V. N.Domanski, P.A. DONDUA, V. K.DOP Dower, J. Dower, J. F. Dower, J.F.DROBYSHEVA, S. S. Drout, H. Druke, B.DRUZHININ, A. D. Drke, BDu Buit, M. H. Duarte, P. C.Dunn, E. E. K. Dunn, E. K. Dunn, J Dunn, J. Duron, M.DUSHENKO, V. VDUSHENKO, V. V.DVININ, Yu. F.Dyakonov, V. Y.Edelman, J. L. Ehrich, S. Eiane, K. Eleby, B. Ellertsen, B Ellertsen, B. Ellis, C.J Emmerson, K. Epp, D.Eschmeyer, W. N.Esteves, A. G. Esteves, E. Evans, P.G.H. F.-Tesch Fabri, M. C.Falkowski, P. G.Fallick, A. E.Fasham, M.J.R. Feio, R Feio_RS Felbeck, H.FELDMAN., V. N. Feldmann, J.Fernandes, L. M. R. Fernandez, E. Ferreira, E.Fessenden, L. M. Fey, C.Fiala-Mdioni, A. Figueroa, H Figueroa, H. FILIN, A. A FILIN, A. A.Filippova, Ju.A4/Filippova, Ju.A., Alekseev, D.O., Bizikov, V.A.FINENKO, Z. Z. Fischer, J. Fisk, L. A. Fleming, SFonseca, L. C.Forward, R.B.Jr Foxton, P. Frank, T. M. Frank, T.MFransen, C. H. J. M. Fraser, J. G. Fraser, J.H.Fratantoni, D. M. Fredericq, S. Freeland, H. Frias, A. F. Friesen, V.L. Frost, B. W. Frost, B.W Fryer, P.Fuglister, F. C.Furness, R. W. Furness, R.W Furness, R.W. Furness_RW G., J. Gould G., Yu. Gaard, E Gaard, E.Gaborit-Rezzouk, M.Gaevskaya, A.V.GAEVSKAYA., A. V.Gagarin, V. I. Gal, G.GALAKTIONOV, G. Z.GALAKTIONOV., G. Z.GALAKTIONOVA, A. I.Galhardo, M. L. Galkin, S. V.Gallienne, G.P Galvin, A. B. Gamble, J. C. Garcin, J. Garcon, V Garcon, V. Gardner, D Gardner, W.D. Gebruk, A. Gebruk, A. V. Geiss, J.Geistdoefer, P. Gelfman, C. Genin, A.GEORGIEV, V. T. GERBER, E. M. German, C. R. Gerosa, G. Gersonde, RGEVORKJAN, V. H.Gibbs, R. H. Jr. Gillespie, D. Girard, A. A. Gislason, A Gislason, A. Gliem, F. Gloeckler, G.GLUKHOV, A. A. GLUKHOV, A.A. Goddard, A. Godley, B.JGodman, F. du C. Gofas, S.GOLOVIN., N. V.Gonalves, J. M.Gonalves, J.M. Gooday, A.J. Goode, G. B.Goodman, F. du C.Gorbunov, A. E.GORCHINSKY, K.GORCHINSKY, K. V.GORDINA, A. D. Gordon, J.Gordon, J. D. M. Gordon, J.D.MGordon, J.D.M. Gordon, T. Gorsky, G.Gosliner, T. M. Goulart, E. Gould, J. Gould, W. J. Gowing, M. Gowing, M. M.Granadeiro, J. P.Granadeiro, J.PGranadeiro, J.P. Grant, G. C. Grant, G.CGreenblatt, P. Greene, C. Greene, C. H. Grice, G.D Griffies, S.MGRIGORJEV, G. V.Grobecker, D. B. Gros, M.P. Groz_MP GRUZOV, L. N. Gudfinnson, HGudfinnsson, H. Guerra, A.Guimares, A. R. P.d]\ [XZYXWVU*TSRDQP ~O}|v{N&DROBYSHEVA, S. S. A. V. KOPTEV.i 1991\VSome features of the vertical structure of plankton communities of the North Atlantic*$Fisheries investigations of plankton(! Part I. Oceans and adjacent seass  43-52 in Russian Drout, H. 1858f`Rapport a Sa Majest Le Roi de Portugal sur un Voyage d'Exploration Scientifique aux les Aores2+Mmoires de la Socit Acadmique de l'AubebXXII (extrait) 1-3e.'Scientific expeditions; natural history Drout, H. 1858,%Mollusques marins des les des Aorese82Mmoires de la Socit Linnenne de Maine et Loire4r 53 ppt Drout, H. 1861$lments de la Faune Aorenne  Paris J. B. Baillire and Fils 245 pp Drout, H. 1861aa{Voyage d'Exploration Scientifique aux Iles Aores, effectu par MM. Morelet et Drout pendant le printemps et l't de 1857s81Annales de la Socit Linnenne de Maine et LoireIV4e Anne 81-98iScientific expeditions Drout, H. 1861ba$lments de la Faune Aorenne "J. B. Ballire & Fils, Paris 245pp'4.Natural history; history; ethnology; checklist("DRUZHININ, A. D. B. P. PSHENICHNY. 1979*$Some problems of deepwater fisheriesF? Problems of investigations and exploitation of the World Oceana315-3202 in Russian2,Du Buit, M. H. Ozouf-Costaz, C. Quro, J. C. 19892Observation Concarneau de Cryptopsaras couesi et Certias sp. (Piscea, Lophiiformes, Ceratiidae), espces nouvelles pour la faune ichthyologique franaise. Leur distribution en Atlantique nord-est03: Cybium 13(2) 192 Geographical distribution,&Duarte, P. C. Silva, A. A. Menezes, G. 1999EJuvenile growth of the tope shark, Galeorhinus galeus, in the Azores.#5"XV111 Azorean Fisheries Week  Horta, Faial22-27 March 1999DUSHENKO, V. V.t 1980Preliminary results of investigations on infraspecific groupings of roundnose grenadier in the North Atlantic. ICES C.M. 80/G:22.rDUSHENKO, V. V. 1982ZTPopulational and genetic investigations of roundnose grenadier of the North AtlanticngThe union conference on theory of formation of abundance and rational exploitation of commercial stocks125-126i in RussianDUSHENKO, V. V. 1983Correlation between genetic stability and variability in populations of roundnose grenadier of the North Atlantic.Genetics of commercial fishes and objects of aquaculture. Materials of the union conference on genetics, selection and hybridization of fishes 34-37 in RussianDUSHENKO, V. V. 1985TMOn formation of commercial stock of roundnose grenadier of the North Atlantict& Behaviour of commercial fishes141-145e in RussianDUSHENKO, V. V.V 1987Influence of partial expatriation of young fish on processes of formation of the area and a structure of gene fund of roundnose grenadier of the North Atlantic2+ Genetic investigations of marine organisms107-119  in Russian(!DUSHENKO, V. V P. I. SAVVATIMSKY.i 1987 Intraspecies structure of roundnose grenadier Coryphaenoides rupestris Gunnerus of the North Atlantic: changeability of local groups and prerequisites of their formationVoprosy ikhtiologii 27(5) 784-792 .n in RussianDUSHENKO, V. V.V 1988Intraspecies structure of roundnose grenadier Coryphaenoides rupestris of the North Atlantic considering knowledge on partial expatriation of their young fish: genetic processesvVoprosy ikhtiologiia  28(1) 20-21  in RussianDUSHENKO, V. V.V 1989jdOn intraspecies structure of roundnose grenadier (Coryphaenoides rupestris G.) of the North Atlantic Abstract of Doctor Thesis. 22 pp\ in Russian*#DVININ, Yu. F. L. L. KONSTANTINOVA.e 1977ztTechnochemical composition of some deepwater fishes of Atlantic and recommendations on exploitation of their stocks Trudy PINRO  39 70-84  in Russian *#DVININ, Yu. F. L. L. KONSTANTINOVA.  1978JCTechnochemical composition of some Macruridae of the North AtlanticRybnoe khozyaistvo1 57-59  in Russian.fDVININ, Yu. F. 1981TM Weight and chemical composition of roundnose grenadier of the North Atlantico"Technology of fish productst 3-15 in Russian81DVININ, Yu. F. L. L. KONSTANTINOVA V. I. KUZMINA.K 1981On results of investigations of food and technical value of some deepwater and pelagic fish of the North Atlantic and perspectives of exploitation of their stocksrNH Biological resources of deep and pelagic waters of the open World Ocean 39-40  in Russiand]DVININ, Yu. F. L. L. KONSTANTINOVA V. I. KUZMINA O. V. MOKANU L. V. PASHKOVA, L. P. KHARZOVA.h 1981^XOn technical and chemical characteristics of some deepwater fishes of the North Atlantic" Technology of fish products 16-28  in Russiand]DVININ, Yu. F. L. L. KONSTANTINOVA V. I. KUZMINA O. V. MOKANU L. V. PASHKOVA, L. P. KHARZOVA.s 1981LEOn technical and chemical characteristics of some skates and chimaeran" Technology of fish products 29-51  in Russian. Ehrich, S. 1977*#Die Fiscfauna der Groen Meteorbankc$"Meteor" Forschungsergebnisse9 Reihe D - No.25, Biologies 1-23Anatomy; morphometry; comparative morphology; meristics; checklist; ecology; population dynamics; feeding; geographical distribution; evolution; phylogeny; biogeography; scientific expeditions; cruisesd  KUKUEV, E. I.  1984hbIchthyofauna of thalassic bathyal of the North Atlantic (composition and zoogeographical analysis) Abstract of Doctor Thesisn 25 pp in Russian KUKUEV, E. I.t 1985On composition and zoogeographical structure of bottom and bottom-pelagic ichthyocenoses of underwater eminencies of the North Atlantice4. Complex studying of the Atlantic Ocean nature Part II  49-51 in Russian(!KUKUEV, E. I. V. V. SUKHOVERSHIN.j 1985On cases of catch of frill shark (Chlamydoselachus anguineus Garman, Chlamydoselachidae, Chondricthyes) in thalassic bathyal of the North and South-West Atlantic Bull. MOIP 90(5) 69-71 in RussianKUKUEV, E. I.. 1988TMZoogeographical structure of mezopelagic ichthyocenoses of the North Atlantict,&The union conference on marine biology Part I275-276t in Russian& KUKUEV, E. I. I. I. KONOVALENKO. 1988voNew species of sharks of the Scymnodalatias (Dalatidae) genus from the North Atlantic and south-eastern PacificmVoprosy ikhtiologii  28(2)315-319 in RussianKUKUEV,. 1991f_Ichthyofauna of underwater eminencies of the boreal and subtropical zones of the North Atlantic D= Biological resources of thalassic bathyal of the World Ocean  15-30 in Russian KUKUEV, E. I.O 1998haSystematic and distribution of daggertooth of the Anotopterus genus (Anotopteridae, Aulopiformes)Voprosy ikhtiologii 38(6)745-7496 in Russian  Rossby, Tn 1996JCThe North Atlantic current and surrounding waters:at the crossroadsReviews of Geophysicsc34463-481oEDDY KINETIC-ENERGY, GULF-STREAM, GRAND-BANKS, MEAN CIRCULATION, MESOSCALE VARIABILITY, MEANDERING JET, SOUTHEAST, NEWFOUNDLAND, AZORES, TRANSPORTThe North Atlantic Current is a well-defined western boundary current that flows north along the east side of the Grand Banks from 40 degrees to 51 degrees N, where it turns sharply to the east and begins its journey across the ocean. The current is unique in transporting warm tropical waters to much higher latitudes than any other western boundary current and thus plays a crucial role in ameliorating the climate of the European subcontinent. The North Atlantic Current originates in the Gulf Stream when the latter curves north around the Southeast Newfoundland Rise, a major submarine ridge that stretches SE from the Grand Banks. A well-defined front delineates the path of the current as long as it flows north as a western boundary current. After the current turns east in the north, it broadens into a widening band of eastward drift without a sharp or permanent front in the sense of the eastward flowing Gulf Stream after it separates from Cape Hatteras. The North Atlantic Current transports more than 40 Sv (1 Sv = 10(6) m(3) s(-1)) in the south and about 20 Sv by the time it flows east across the Mid-Atlantic Ridge. The currents along the northward flowing front are quite swift, with typical maximum average speeds in the upper 300 m near 1 m s(-1) (= 2 knots). The current meanders almost as wildly as a ''snaking'' river, but unlike steep meanders in the Gulf Stream these meanders appear to be stable, and with one exception have not been observed to break off to form pools of warm and/or cold waters as frequently occurs in the Gulf Stream. The meanders appear to be induced by major topographic features along the path of the current, namely, the Southeast Newfoundland Rise, the Newfoundland Seamounts, and Flemish Cap. Strong recirculations develop on the concave side of the meanders. One of these, the ''Mann eddy'' at the first meander crest of the North Atlantic Current, should be regarded as a permanent feature of the North Atlantic circulation. Other meanders also contain recirculations that can persist for months. Under certain conditions these can merge together to form an extended SW flow (recirculation) just east of the North Atlantic Current. 691600013aMorales, C. E.Carbon and nitrogen fluxes in the oceans: the contribution by zooplankton migrants to active transport in the North Atlantic during the Joint Global Ocean Flux Studyh"Journal of Plankton Researchdiel vertical migration; wax esters; respiratory carbon; calanoid copepods; bloom experiment; marine copepods; eastern gulf; metabolism; mesozooplankton; ph KUKUEV, E. I.  1984hbIchthyofauna of thalassic bathyal of the North Atlantic (composition and zoogeographical analysis) Abstract of Doctor Thesisn 25 pp in Russian KUKUEV, E. I.t 1985On composition and zoogeographical structure of bottom and bottom-pelagic ichthyocenoses of underwater eminencies of the North Atlantice4. Complex studying of the Atlantic Ocean nature Part II  49-51 in Russian(!KUKUEV, E. I. V. V. SUKHOVERSHIN.j 1985On cases of catch of frill shark (Chlamydoselachus anguineus Garman, Chlamydoselachidae, Chondricthyes) in thalassic bathyal of the North and South-West Atlantic Bull. MOIP 90(5) 69-71 in RussianKUKUEV, E. I.. 1988TMZoogeographical structure of mezopelagic ichthyocenoses of the North Atlantict,&The union conference on marine biology Part I275-276t in Russian& KUKUEV, E. I. I. I. KONOVALENKO. 1988voNew species of sharks of the Scymnodalatias (Dalatidae) genus from the North Atlantic and south-eastern PacificmVoprosy ikhtiologii  28(2)315-319 in RussianKUKUEV,. 1991f_Ichthyofauna of underwater eminencies of the boreal and subtropical zones of the North Atlantic D= Biological resources of thalassic bathyal of the World Ocean  15-30 in Russian KUKUEV, E. I.O 1998haSystematic and distribution of daggertooth of the Anotopterus genus (Anotopteridae, Aulopiformes)Voprosy ikhtiologii 38(6)745-7496 in Russian& 369-382$://000171949700018y&Buhring, S. I. Christiansen, B.,VOLipids in selected abyssal benthopelagic animals: links to the epipelagic zone?7Progress in Oceanographyparticulate organic-matter; fatty-acids; wax esters; deep-sea; north pacific; thysanoessa-macrura; antarctic copepods; zooplankton; atlantic; phospholipids A detailed study of the lipids of selected zooplankton species and scavenging amphipods in the near-bottom water layer (15-100 m above bottom, mab) was carried out at the BENGAL site in late summer 1998. Copepoda were the main contributors to the zooplankton, comprising 75% of the total abundance, followed by Ostracoda and Chaetognatha. Calanoid copepods of the family Metridinidae were predominant and accounted for more than 50% of all copepods. Two types of storage lipids were distinguished: triacylglycerols and wax esters. Ostracoda and the polychaete Vanadis sp. stored exclusively triacylglycerols whilst the bulk of the Copepoda accumulated wax esters, with the exception of the family Aetideidae. In the amphipods both lipid classes were found: Eurythenes gryllus stored wax esters and Paralicella spp. and Orchomene sp. triacylglycerols. The fatty acid composition was characterized by a high level of monounsaturated 18:1 (n-9), which is described as characteristic for animals living in the deeper layers of the water column, and to a lesser degree by 16:1 (n-7) and 20:5 (n- 3), which are typical components of diatom lipids, and 22:6 (n- 3), typical of dinoflagellates. The ratio of 18:1 (n-9):18:1 (n-7) fatty acids was between 5 and 10 in the copepods and indicates a carnivorous/omnivorous feeding behaviour in this group, whereas the higher ratios of 8-18 in the amphipods confirm their necrophagy. The fatty alcohols of the animals storing wax esters were dominated by the monounsaturated isomers 18:1 (n-9) and 18:1 (n-7). The predominance of wax esters as storage lipids in the deep-sea copepods indicates a strong seasonality in the availability of food. This is supported by the high levels of 16:1 (n-7), 20:5 (n-3) and 22:6 (n-3) fatty acids, which point to there being a direct link between the surface primary production and deep-sea copepods, probably via the rapid deposition of phytodetritus. (C) 2001 Elsevier Science Ltd. All rights reserved.Prog. Oceanogr. 200150 1-4'Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, Zeisweg 9, D-22765 Hamburg, Germany Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, D-22765 Hamburg, Germany Christiansen B Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, Zeisweg 9, D-22765 Hamburg, Germany:4Times Cited: 1 English Review SI 488RP PROG OCEANOGRISI:000171949700018HL"yxwvu t s Grice, G.D Hulsemann,K 1965piAbundance,vertical distribution and taxonomy of calanoid copepods at selected stations in the NE Atlantice*$Woods Hole Oceanographic Institution 146213-262 Grice,G.Dr 1971rkThe existence of a bottom-living calanoid copepod fauna in deep water with descriptions of five new species"Deep Water Calenoid Copepods219-242oGriffies,S.M Bryan,K 1997RKA predictability study of simulated North Atlantic multidecadal variabilitynClimate Dynamics13459-487tDECADAL CLIMATE VARIABILITY, OCEAN-ATMOSPHERE MODELS, THERMOHALINE CIRCULATION, TRANSIENT RESPONSES, GRADUAL CHANGES, HEAT-TRANSPORT, DYNAMICS, CO2, OSCILLATION, RESOLUTION ^ WThe North Atlantic is one of the few places on the globe where the atmosphere is linked to the deep ocean through air-sea interaction. While the internal variability of the atmosphere by itself is only predictable over a period of one to two weeks, climate Variations are potentially predictable for much longer periods of months or even years because of coupling with the ocean. This work presents details from the first study to quantify the predictability for simulated multidecadal climate variability over the North Atlantic. The model used for this purpose is the GFDL coupled ocean-atmosphere climate model used extensively for studies of global warming and natural climate variability. This model contains fluctuations of the North Atlantic and high-latitude oceanic circulation with variability concentrated in the 40-60 year range. Oceanic predictability is quantified through analysis of the time-dependent behavior of large-scale empirical orthogonal function (EOF) patterns for the meridional stream function, dynamic topography, 170 m temperature, surface temperature and surface salinity. The results indicate that predictability in the North Atlantic depends on three main physical mechanisms. The first involves the oceanic deep convection in the subpolar region which acts to integrate atmospheric fluctuations, thus providing for a red noise oceanic response as elaborated by Hasselmann. The second involves the large-scale dynamics of the thermohaline circulation, which can cause the oceanic variations to have an oscillatory character on the multidecadal time scale. The third involves nonlocal effects on the North Atlantic arising from periodic anomalous fresh water transport advecting southward from the polar regions in the East Greenland Current. When the multidecadal oscillatory variations of the thermohaline circulation are active, the first and second EOF patterns for the North Atlantic dynamic topography have predictability time scales on the order of 10-20 y, whereas EOF-1 of SST has predictability time scales of 5-7 y. When the thermohaline variability has weak multidecadal power, the Hasselmann mechanism is dominant and the predictability is reduced by at least a factor of two. When the third mechanism is in an extreme phase, the North Atlantic dynamic topography patterns realize a 10-20 year predictability time scale. Additional analysis of SST in the Greenland Sea, in a region associated with the southward propagating fresh water anomalies, indicates the potential for decadal scale predictability for this high latitude region as well. The model calculations also allow insight into regional variations of predictability, which might be useful information for the design of a monitoring system for the North Atlantic. Predictability appears to break down most rapidly in regions of active convection in the high-latitude regions of the North Atlantic.GRIGORJEV, G. V. 1972B://A1988M800100001("Genin, A. Haury, L. Greenblatt, P.yInteractions of Migrating Zooplankton with Shallow Topography - Predation by Rockfishes and Intensification of Patchiness<6Deep-Sea Research Part a-Oceanographic Research Papers 1988 Feb352'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093 USN,CTR OCEAN SYST,SAN DIEGO,CA 92152 UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093JCTimes Cited: 42 English Article M8001 DEEP-SEA RES PT A-OCEANOG RESISI:A1988M800100001 Girard, A. A. 1892:3Les Cphalopodes des les Aores et de l'le MadrerF@Journal de Sciencias Mathematicas, Physicas e Naturaes, 2 srie2-7i210-221f transport system) data, increased in the bathypelagic zone (1000 to 4250 m) from 1.61 mg C m(-2) d(-1) in spring to 4.12 mg C m(-2) d(-1) in summer. The carbon respired by the bathypelagic micro- and mesozooplankton in summer, based on an assumed spring bloom area of 50 000 km(2), was 893 t C d(-1) as a minimum estimate, which was higher than in spring by a factor of 2.6.rMar. Ecol.-Prog. Ser.o 1999 179 >7Times Cited: 4 English Article 195PW MAR ECOL-PROGR SER9ISI:000080261400003aS Krauss, W. 1986"The North Atlantic Current.&Journal of Geophysical Research991C4 5061-5074MKrug, H. 1989iThe Azorean blackspot seabream, Pagellus bogaraveo (Brnnich, 1768) (Teleostei, Sparidae): Age and growth 2 Cybium134347-355Krug, H. 1990The Azorean blackspot seabream, Pagellus bogaraveo (Brnnich, 1768) (Teleostei, Sparidae): Reproductive cycle, hermaphroditism, maturity and fecundity 3 Cybium142151-159"Krug, H. M. S. Silva, H. M. 1990*$Avaliao do stock aoreano de goraz2,Relatrio da IX Semana das Pescas dos Aores9 (1989) 231-23:6zFL3210/.-,+*)z('&%$#"! ANON.n 1977f`The present status and perspectives of development of deepwater trawl fishery on the North Basin Promyshlenno,reybolovstvo1 43 pp in Russian ANON.S 1977rlMethodical material on determination of Myctophidae of open areas of the northern part of the Atlantic Ocean$AtlantNIRO, Zaprybpromrazvedka 52pn in Russian.V ANON.S 1978rlBrief description of results of the cruise in the open areas of Atlantic from 02 August to 26 December, 19774.Research SRTM-0839 "Ladoga"/Sevrybpromrazvedka 23pp in Russian ANON.S 19786/New banks in the area of the Mid-Atlantic Ridge@9Fisheries and technical information of Sevrybpromrazvedka ANON.V 1978RKManual on searching and harvesting of deepwater crabs in the North Atlantice 25 p in Russian. ANON.V 1979rlManual on the search and fishery for deepwater fishes on the underwater eminencies of the Mid-Atlantic Ridge 82 pp in Russian. ANON.S 1980PIMethodical materials on determination of fish of the open North Atlantic9Zaprybpromrazvedka 145 pp in Russian ANON.W 1980PIMethodical recommendations on determination of the age of deep sea fishesn  35 pp in Russian ANON.V 1980F@Manual on bottom fishery for grenadier on the Mid-Atlantic Ridge 35 ppo in Russian ANON.g 1981`ZRecommendations on method of driving of a pelagic trawl on banks of the Mid-Atlantic Ridge"Sevrybpromrazvedka. Murmansk  24 pp in Russian ANON. 1984~wGeological and geophysical and biological investigations of the key zone of the northern part of the Mid-Atlantic Ridgei Okeanologia  24(5)851-854V in Russian ANON. 1984piReference material on of the water surface temperature in the fishery grounds of the open North Atlantic 172 pp in Russian ANON. 1986`ZMethodical materials on determination of deep sea demersal fish of the open North Atlantic 222 pp in Russian ANON. 1987ngMethodical materials on determination of eggs and larvae of fish of the open part of the North Atlantici 160 pp in Russian ANON.V 1988RKBio-oceanographic structure of waters in areas of underwater sea eminenciesN 208 pp in Russian ANON.g 1988JDFisheries description of the northern part of the Mid-Atlantic Ridge<6PINRO,AtlantNIRO,Sevrybpromrazvedka,Zaprybpromrazvedka 179 pp in Russian ANON.S 1989|Background for searching works on studying of possibilities of trawl fishery for tuna in the open part of the North Atlantic pishchevoy promyshlennosti 114 pp in Russian ANON.S 1993XQFisheries description of the North Azores complex of sea mounts and Corner Risingo<6PINRO,AtlantNIRO,Sevrybpromrazvedka,Zaprybpromrazvedka 170 pi in Russian ANON.. 1998,&Macruridae of the North-Atlantic Ridge>8Retrospective review and nowadays possibility of fishery 56pp in Russian Arhan, M.  1990B;The North Atlantic Current and Subarctic Intermediate Waters Journal of Marine Research481109-144 *#Arkhipkin, A.I., Nigmatullin, Ch.M. 1997Ecology of the oceanic squid Onychoteuthis banksi and the relationship between the genera Onychoteuthis and Chaunoteuthis (Cephalopoda: Onychoteuthidae)HBJournal of the Marine Biological Association of the United Kingdom  77(3)839-869f In EnglishD=Arnbom, T. Gordon, J. Martins, H. R. Santos, R. S. Walsh, V.a 1988eIndividual photographic identification of Risso's dolphin (Grampus griseus) near the Azorean Islands.;J  P.G.H. EvansNHProceedings of Second Annual Conference of the European Cetacean Society SNPRCN, Lisboa 39-41>7Arruda, L. M. Azevedo, J. N. Heemstra P. C. Neto, A. I. 1992\VChecklist of the fishes on the "Santa Maria and Formigas 1990: Scientific expedition".*$Arquivos do Museu Bocage, Nova Srie 2, 12263-273670-672$://A1992JA43000063t>7Asper, V. L. Deuser, W. G. Knauer, G. A. Lohrenz, S. E.oVORapid Coupling of Sinking Particle Fluxes between Surface and Deep Ocean Waters Naturesargasso sea; sediment traps; temporal variations; northeast pacific; panama basin; marine snow; carbon; atlantic; matter; resuspensiondjcSETTLING particles are thought to be responsible for much of the transport of mass and energy from the upper ocean to the sea floor. Photosynthetic production by phytoplankton is a major source of these particles, either as phytoplankton biomass sinks directly 1 or as it is transformed into rapidly sinking forms such as aggregates 2,3 and zooplankton faeces 4. Because a variety of processes may act on sinking matter, however, it is not known to what extent fluxes of organic matter to the deep sea are coupled to processes at the ocean surface. Some studies have provided evidence for direct coupling 2, 5-7, but transformation processes and advection exist which have the potential to modify the transmission of surface signals to the deep sea 8-11. If these mechanisms overwhelm surface production signals, seasonal and annual variations in deep-sea geochemistry and biology would be controlled largely by lateral processes associated with ocean circulation rather than by surface processes. Here we report direct measurements of seasonal variations in upper-ocean primary production concurrent with particle fluxes measured at several depths ranging from the upper to the deep ocean in the Atlantic. We find that the productivity signal can be transferred rapidly to the deep sea by settling particles, yielding close temporal coupling between the surface and deep oceans.u Nature 1992 Jun 25 357a 6380'UNIV SO MISSISSIPPI,CTR MARINE SCI,JOHN C STENNIS SPACE CTR,BAY ST LOUIS,MS 39529 WOODS HOLE OCEANOG INST,DEPT CHEM,WOODS HOLE,MA 02543 ASPER VL UNIV SO MISSISSIPPI,CTR MARINE SCI,JOHN C STENNIS SPACE CTR,BAY ST LOUIS,MS 395292,Times Cited: 68 English Article JA430 NATUREISI:A1992JA43000063x yFreeland1992 Frias 1990a' Friesen1998 Frost1989 Frost1989 Frost1991 Frost1991 Frost1993 Frost1994 Frost1994Q Fuglister1960Furness 1989Furness (unpubl.))F Furness1992( Furness1994 Furness1995 Furness1995 Furness1995) Furness19954 Furness19955 Furness19956 Furness19957 Furness1995l Furness1996m Furness19968 Furness19969 Furness1996: Furness1996; Furness1996D Furness1996< Furness1997E Furness1997' Furness1998+ Furness1998, Furness1998- Furness1998. Furness1998= Furness1998> Furness1998? Furness1998G Furness1998/ Furness1999@ Furness1999H Furness1999& Furness2000* Furness20000 Furness20001 Furness2000A Furness2001B Furness2001Furnessin pressFurnessin pressC Furness_RW199992 Furness_RW2000j G.1990AY G.199996 Gaard2000 Gaard2000Gaborit-Rezzouk1976 Gaevskaya1976 GAEVSKAYA.1981 Gagarin1995? Gagarin1997> Gagarin1999 Gal1994n Gal1995b GALAKTIONOV1984d GALAKTIONOV.1990c GALAKTIONOVA1978d GALAKTIONOVA1990Galhardo1990 Galkin1990 Galkin1990 Galkin1997 Gallienne2001S Galvin19922 Gamble19977, Garcin19999 Garcon19999 Garcon20000G Garcon20011 Garcon20011 Gardner Gardner1975 Gardner1977 Gebruk1997+ Gebruk2000 Gebruk2000S Geiss1992f Geistdoefer1971} Gelfman1995| Gelfman2000 Genin1985 Genin1987z Genin1988 Genin1988 Genin1994n Genin1995b Genin2000eGEORGIEV1989f GERBER1993 German19966 Gerosa19929Gersonde2002bg GEVORKJAN1982h GEVORKJAN1986i GEVORKJAN1987j GEVORKJAN1990 Gillespie1987 Gillespie1988 Girard1892CGislason1992DGislason19929Gislason1992AGislason19959BGislason1995?Gislason1996<Gislason19989=Gislason1998>Gislason1998Gislason20000 Gislason20005Gislason20006Gislason200009Gislason2000:Gislason2000Gislason2000Gislason2000Gislason20000S Gliem1992S Gloeckler1992k GLUKHOV1981l GLUKHOV1982m GLUKHOV1983n GLUKHOV1984 GLUKHOV1986 Goddard1989+ Godley19983 Godley19999 Godman1866 Gofas1990GOLOVIN.1977 Gonalves 1993 Gonalves1991a Gonalves1991b Gonalves1992 Gonalves1993 Gonalves1993 Gonalves1994 Gonalves1994 Gonalves1994 Gooday19899 Goode1895 Goodman1870<Gorbunov19911 GORCHINSKY1991o GORCHINSKY1994p GORDINA1985q GORDINA1988r GORDINA1991 Gordon1987 Gordon19879 Gordon1988 Gordon1988 Gordon19889 Gordon19896 Gordon19900; Gordon19919 Gordon19919 Gordon19939 Gordon19999, Gorsky19999, Gorsky19999, Gorsky199999999, Gorsky199999999, Gorsky199999999, Gorsky19999, Gorsky1999919999, Gorsky19999, Gorsky19999, Gorsky1999999, Gorsky19999, Gorsky19999, Gorsky19999, Gorsky1999999, Gorsky19999, Gorsky19999, Gorsky1999999, Gorsky19999, Gorsky19999 Gorsky1999999, Gorsky1999999, Gorsky1999999, Gorsky199999999, Gorsky199999999, Gorsky199999999, Gorsky19999 Gorsky19999, Gorsky19999, Gorsky19999, Gorsky1999999, Gorsky1999999, Gorsky19999, Gorsky19999, Gorsky19999, Gorsky19999 Frost1994 Frost1994Q Fuglister1960Furness 1989̠Furness 1989Furness (unpubl.))F Furness1992( Furness1994 Furness1995 Furness1995 Furness1995) Furness19954 Furness19955 Furness19956 Furness19957 Furness1995l Furness1996m Furness19968 Furness19969 Furness1996: Furness1996; Furness1996D Furness1996< Furness1997E Furness1997' Furness1998+ Furness1998, Furness1998- Furness1998. Furness1998= Furness1998> Furness1998? Furness1998G Furness1998/ Furness1999@ Furness1999H Furness1999& Furness2000* Furness20000 Furness20001 Furness2000A Furness2001B Furness2001Furnessin pressFurnessin pressC Furness_RW199992 Furness_RW2000j G.1990AY G.199996 Gaard2000 Gaard2000Gaborit-Rezzouk1976 Gaevskaya1976 GAEVSKAYA.1981 Gagarin1995? Gagarin1997> Gagarin1999 Gal1994n Gal1995b GALAKTIONOV1984d GALAKTIONOV.1990c GALAKTIONOVA1978d GALAKTIONOVA1990Galhardo1990̍Galhardo1990̅ Galkin1990̆ Galkin1990̾ Galkin1997̻ Gallienne2001S Galvin19922 Gamble19977, Garcin19999 Garcon19999 Garcon20000G Garcon20011 Garcon20011 Gardner Gardner1975 Gardner1975 Gardner1977 Gebruk1997+ Gebruk2000̿ Gebruk2000S Geiss1992f Geistdoefer1971} Gelfman1995| Gelfman2000 Genin1985 Genin1987z Genin1988 Genin1988 Genin1994n Genin1995b Genin2000eGEORGIEV1989f GERBER1993̫ German19966 Gerosa19929k Gerosa19929Gersonde2002bg GEVORKJAN1982h GEVORKJAN1986i GEVORKJAN1987j GEVORKJAN1990 Gillespie1987 Gillespie1987 Gillespie1988 Gillespie1988 Girard1892̏ Girard1892CGislason1992DGislason19929Gislason1992AGislason19959BGislason1995?Gislason1996<Gislason19989=Gislason1998>Gislason1998Gislason20000 Gislason20005Gislason20006Gislason200009Gislason2000:Gislason2000Gislason2000Gislason2000Gislason20000S Gliem1992S Gloeckler1992k GLUKHOV1981l GLUKHOV1982m GLUKHOV1983n GLUKHOV1984 GLUKHOV1986 Goddard1989 Goddard1989+ Godley19983 Godley19999 Godman1866̐ Godman1866 Gofas1990 Gofas1990GOLOVIN.1977 Gonalves 1993̒ Gonalves 1993 Gonalves1991a̓ Gonalves1991a Gonalves1991b̔ Gonalves1991b Gonalves1992 Gonalves1993 Gonalves1993 Gonalves1993 Gonalves1994 Gonalves1994 Gonalves1994 Gonalves1994 Gonalves1994 Gonalves1994 Gooday19899 Goode1895 Goode1895 Goodman1870<Gorbunov19911 GORCHINSKY1991o GORCHINSKY1994p GORDINA1985q GORDINA1988r GORDINA1991 Gordon1987 Gordon19879 Gordon1987̙ Gordon19879 Gordon1988 Gordon1988 Gordon19889a Gordon1988̚ Gordon1988̚ Gordon19889 Gordon1989̛ Gordon19896 Gordon19900; Gordon19919 Gordon19919 Gordon19939l Gordon19939 Gordon19999, Gorsky19999@,F 1113-1120$://000085009000011tB;Bianchi, A. Garcin, J. Gorsky, G. Poulicek, M. Tholosan, O.Stimulation of the potential heterotrophic activity in deep seawater by barotolerant bacteria colonizing faecal pellets produced by migrating zooplanktonZTComptes Rendus De L Academie Des Sciences Serie Iii-Sciences De La Vie-Life Sciencesbacteria; metabolic activity; barophile; hydrostatic pressure; faecal pellets; deep-sea; Mediterranean northwestern mediterranean-sea; particle-bound bacteria; vertical distributions; diel migrations; atlantic-ocean; pressure; micronekton; water; glucose; samplesZTAt a depth of 1 150 m in the northwest Mediterranean, amino acid uptake and bacterial biomass production rates increased, in a 12-day lime interval, 5- and 30-fold, respectively. Simultaneously, bacterial response to pressure changes evolved from barophilic to barotolerant. During the same period, scanning electron microscope observations and in situ observations using Underwater Video Profiler showed a 2-fold increase in particle concentrations, mainly due to faecal pellet production by zooplankton. This input, nutrient rich and largely colonized with bacteria unaffected by pressure variations since they originated from organisms that regularly migrate up and down through the water column, could produce such microbial activity peaking in the deep water masses. (C) 1999 Academie des sciences/Editions scientifiques et medicales Elsevier SAS.<5Comptes Rendus Acad. Sci. Ser. III-Sci. Vie-Life Sci. 1999 Dec 32212'Univ Mediterranee, Fac Sci Luminy, CNRS, Insu,EP 2032, Case 907, F-13288 Marseille 9, France Univ Mediterranee, Fac Sci Luminy, CNRS, Insu,EP 2032, F-13288 Marseille 9, France Observ Oceanol, LOBEPM, ESA 7076, F-06230 Villefranche Sur Mer, France Univ Liege, Inst Zool 1, Lab Ecol Anim & Ecotoxicol, B-4020 Liege, Belgium Bianchi A Univ Mediterranee, Fac Sci Luminy, CNRS, Insu,EP 2032, Case 907, F-13288 Marseille 9, FranceB7Complex studying of the open part of the Atlantic Oceana 79-848 in RussianBoehlert, G.W. Genin, A. 1987B7Seamounts, Islands and Atolls. Geophysical Monograph 43 American Geophysical Union319-334 mE,salps samplessanta-catalina basin sargasso sargasso seaSARGASSO SEA, SEDIMENT TRAPS, TEMPORAL VARIATIONS, NORTHEAST PACIFIC, PANAMA BASIN, MARINE SNOW, CARBON, ATLANTIC, MATTER, RESUSPENSION satellitescattering layerscavenging amphipodsscientific divulgationscientific expeditionsseasea hydrothermal vents sea-floor sea-level pressure changesSEA-SURFACE TEMPERATURE, INTERPENTADAL VARIABILITY, THERMOHALINE CIRCULATION, GENERAL-CIRCULATION, FRESH-WATER, OCEAN, SALINITY, ICE, MODEL, FLUCTUATIONSSEA-SURFACE TEMPERATURE, INTERPENTADAL VARIABILITY, WIND STRESS, OCEAN, SALINITY, CLIMATE, WATER, CIRCULATION, HYDROGRAPHY, OSCILLATION seamountD@Seamount, ATP, Atlantic Ocean, microplankton, Mid Atlantic Ridgeseamount-trapped waves seamounts$!Seamounts, Atlantic, submersiblesseasonal depositionseasonal developmentzSEASONAL DEVELOPMENT, EGG-PRODUCTION, ST-LAWRENCE, ZOOPLANKTON, WATERS, ABUNDANCE, COPEPOD, ICELAND, CYCLE, STRATIFICATION sediment trapsediment traps sedimentation sedimentsseep communities segmentation selectionselective predation seriesseries sampling shallowshelfshelf ecosystems shrimp shrimp rimicaris-exoculata significance sinking sinking ratesSiphonostomatoida site-522size sledgeslope small-scalesmall-scale turbulence solar windsound-scattering layers southern baysouthern-californiasouthern-ocean southwestspace space- spatialspatial heterogeneityspatial variabilityspatial-distributionspecies-diversityspeedspreading ridges spring spring bloom st-lawrence stable-carbonstage development station stations statistics stocksstratification streamsubarctic pacific-oceansubmarine canyons submersiblessubtropical Atlantic succession summersummer zooplanktonsunsuprabenthic mysids surfacesurface-temperaturesurrounding waterssverdrup transports swarms swimmers system Systematicstall isolated seamounttarget strength technologytemora-longicornis temperature temporal temporal abundance patternstemporal changestemporal variations thermohalinethermohaline structurethysanoessa-macruratidal currentstime interactionstime- time-scale time-series topography transport trapped waves trendstrophic behaviour tropicaltropical pacific tube-worms turbulenceturbulent motion typology uncharted underwaterunderwater observations upper ocean upstreamupwelling systemuv-b radiation uv-light variability variation variations veligersventvent communities vent shrimps vent-fieldvernacular names verticalvertical distributionvertical distributions vertical fluxvertical migrationvertical nitrogen fluxVERTICAL NITROGEN FLUX, DIEL MIGRANT BIOTA, DEEP-SEA, CHROOCOCCOID CYANOBACTERIA, COASTAL WATERS, POTENTIAL ROLE, SINKING RATES, FECAL PELLETS, ZOOPLANKTON, PARTICLES vertical-vertical-distribution volcanism vorticity voyager-2waste managementwater water columnwater mass structure waterswave absorbing pigmentswax wax estersweb weddell sea weight west-indieswestern boundary currentwestern indian-oceanwestern north-atlanticwestern norwaywestern sweden wind stress winterwinter distribution world ocean zonationzones zoogeography zooplanktonzooplankton communityzooplankton ecologyzooplankton migrationzooplankton populationszooplankton variations D l Parr, A. E 1960("The fishes of the family Searsidae Dana-Report  51 1-109p Patzner, R. A. 1990*#Fishes in the lagoon of Lajes, PicoghbExpedio Aores/89 1990. Ecologia e Taxonomia do Litoral Marinho dos Aores: Relatrio Preliminar :4Departamento de Oceanografia e Pescas, Horta, AoresParte I; Vol. 1123-126"Patzner, R. A R. S. Santos  1990NHEcologia e Taxonomia do Litoral Marinho dos Aores.-Relatrio PreliminarFishes of the AzoresParte I, Vol. 1152-159:3Patzner, R. A. Santos, R. S. R, P. Nash, R. D. M.c 1992tmLittoral fishes of the Azores: An annotated checklist of fishes observed during the " Expedition Azores 1989"2 ArquiplagoLife and Earth Sciences:10101-111"Patzner, R. A. Santos, R. S. 1993:3Ecology of rocky littoral fishes of the Azores. , ,o.'Courrier Forschungsinstitut Senckenberge 159 423-427,%Paula, J. Cartaxana, A. Queiroga, H.i 1992D=Decapod crustaceans collected by the "Expedition Azores 1989"c ArquiplagocLife and Earth Sciences210 67-74"PAVLOV, A. I O. I. SAMAREVAg 1980vpOn method of determination of the age of slickhead Alepocephalus bairdi Goode et Bean of the North-East AtlanticLEMethods of determination of the age and growth of new commercial fish( 28-29n in Russian PAVLOV, A. I 1988Distribution and behaviour of deep sea redfish (Sebastes mentella Travin) on the Reykjanes Ridge by observations from the underwater device Sever-2sB 4 mm, maximum 13 individuals m(-3)), ostracods (maximum 8 individuals m(-3)), siphonophores (maximum > 2 individuals m(-3)) and peracarids (maximum > 600 individuals 1000 m(-3)) were analysed and represented by isoline diagrams. The biomass of total zooplankton (maximum 18419 mu g C m(-3), 3780 mu g N m(-3)) and large copepods ( > 4 mm maximum 2256 mu g C m(-3), 425 mu g N m(-3)) also were determined. Vertical migration was absent or affected only the epipelagic zone for appendicularians, cladocerans, small copepods and siphonophores. Average amplitude of vertical migration was about 400-500 m for ostracods, some hyperiids and mysids, and large copepods, which were often present in the epipelagic, mesopelagic, and bathypelagic zones. Large copepods can constitute more than 80% of the biomass corresponding to total zooplankton. They may play an important role in the active vertical transfer of carbon and nitrogen. (C) 1999 Elsevier Science Ltd. All rights reserved.MAZHIRINA, G. PF 1992nhPeculiarities of ovaries development in Benthosema glaciale from different regions of the North Atlantic4. Studies of bioresources of the North AtlanticCollected Papers 203-218 in Russian"MAZHIRINA, G. P A. A. FILIN 1992XQPeculiarities of reproductive biology of Notoscopelus kroeyeri Malm (Myctophidae)6HA Studies of bioresources of the North Atlantic. Collected Papersr219-2382 in Russian81McKenzie, C Godley, B.J , Furness, R.W Wells, D.E8 1999zsConcentrations and Patterns of Organochlorine Contaminants in Marine Turtles from Mediterranean and Atlantic Waters $Marine Environmental Research  47117-135.Mead, G. W R. Haedrich  196560The distribution of the Oceanic fish Brama bramaHABulletin of the Museum of Comparative Zoology, Harvard University134 (2) 29-68Mees,J Jones,M.B 1997The hyperbenthos&Oceanography and Marine Biologye35221-255eMELNIKOV, S. P 1999|vVertical structure and mechanism of formation of concentrations of deep-sea redfish in the area of the Reykjanes Ridge`Z Biology and regulation of fishery for demersal fish of the Barents Sea and North Atlantic 75-86I in Russian Menard, H.W. 1964$Marine Geology of the Pacific New York  McGraw-Hill1 Menezes, G. M. 1991a Aspectos da biologia e ecologia de Patella ulyssiponensis aspera e Patella candei candei (Mollusca, Gastropoda, Patellidae) dos Aores. Potencial da sua exploraoc#ACY*$Relatrio de Estgio de Licenciatura Lisboa Faculdade de Cincias de 134 pp( tChristiansen, B Beckman,W Weikert,Hy 2001The structure and carbon demand of the bathyal benthic boundary layer community:a comparison of two oceanic locations in the NE AtlanticDeep-Sea Research part II 48 2409-2424CENTRAL NORTH PACIFIC, SANTA-CATALINA BASIN, DEEP-SEA, VERTICAL-DISTRIBUTION, EURYTHENES-GRYLLUS, NECROPHAGOUS AMPHIPOD, OXYGEN-CONSUMPTIO 2409-2424O$://000169098200012 0)Christiansen, B. Beckmann, W. Weikert, H.fThe structure and carbon demand of the bathyal benthic boundary layer community: a comparison of two oceanic locations in the NE-Atlanticg@9Deep-Sea Research Part Ii-Topical Studies in Oceanographyhcentral north pacific; santa-catalina basin; deep-sea; vertical-distribution; eurythenes-gryllus; necrophagous amphipod; oxygen-consumption; zooplankton; biomass; foodtEstimates of standing stocks were used together with metabolic rates from literature to compare the structure and the respiratory carbon demand of the benthopelagic fauna and epibenthic megafauna at two oceanic locations in the northeast Atlantic. The total standing stock of the benthopelagic fauna and epibentic megafauna (in the following referred to as benthopelagos sensu latu) in the Iceland Basin (59 degreesN/20 degreesW) was 5 times higher than at the BIOTRANS site (West European Basin, 47 degreesN/20 degreesW). While fish were the predominating group at the northern location, followed by epibenthic megafauna, most of the biomass at the southern station could be attributed to epibenthic megafauna whereas fish were even surpassed by zooplankton. The overall respiratory carbon demand of the benthopelagos s.l. in the Iceland Basin was about 50% higher than at the BIOTRANS site. In both areas, a large fraction of the carbon was respired by the megafauna, accounting for 46 % of the total respiratory carbon demand in the Iceland Basin and 86% at the BIOTRANS site. Important consumers in the Iceland Basin were also zooplankton (27%) and fish (26%), whereas at the BIOTRANS site only zooplankton had a significant share (12%) besides megafauna. Compared to the carbon fluxes into the BBL, the faunal groups (without bacteria) remineralize ca. 10-20% of the sedimenting POC. If near-bottom pelagic bacteria are included, the fraction of the POC import flux remineralized by the benthopelagic community amounts to at least 20-50%. That means, the carbon flux as measured in sediment traps is not sufficient to fuel both the benthopelagic community including the megafauna plus the sediment community. (C) 2001 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 20014810'Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, D-22765 Hamburg, Germany Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, D-22765 Hamburg, Germany Christiansen B Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, D-22765 Hamburg, GermanyHBTimes Cited: 2 English Article 439EQ DEEP-SEA RES PT II-TOP ST OCEISI:0001690982000128179-189$://A1995RC87500013.'Turley, C. M. Lochte, K. Lampitt, R. S.u^WTransformations of Biogenic Particles During Sedimentation in the Northeastern Atlantica\VPhilosophical Transactions of the Royal Society of London Series B-Biological Sciencesparticulate organic-matter; diel migrant biota; deep-sea floor; marine snow; north-atlantic; seasonal deposition; bloom experiment; pacific-ocean; vertical flux; carbon fluxp The vertical flux and transformation of biogenic particles are important processes in the oceanic carbon cycle. Changes in the magnitude of the biological pump can occur in the north eastern Atlantic on both a seasonal and interannual basis. For example, seasonal Variations in vertical flux at 47 degrees N 20 degrees W are linked to seasonal ocean productivity variations such as the spring bloom. The size and organic and inorganic content of phytoplankton species, their development and succession also play a role in the scale and composition of the biological pump. The majority of flux is in the form of fast sinking aggregates. Bacteria and transparent exopolymer particle production by phytoplankton have been implicated in aggregate production and mass flux events. Zooplankton grazing and faecal pellet production, their size and composition and extent of their vertical migration also influence the magnitude of vertical flux. Aggregates are formed in the upper ocean, often reaching a maximum concentration just below the seasonal thermocline and can be a food resource to mesozooplankton as well as to the high concentrations of attached bacteria and protozoa. Attached bacteria remineralize and solubilize the aggregate particulate organic carbon. The degree of particle solubilization is likely to be affected by factors controlling enzyme activity and production, for example temperature, pressure or concentration of specific organic molecules, all of which may change during sinking. Attached bacterial growth is greatest on particulate organic matter collected at 500 m which is the depth where studies of(210)po reveal that there is greatest break-up of rapidly sinking particles. Break-up of particles by feeding zooplankton can also occur. The fraction of sinking poc lost between 150-3100 m at one station in the north eastern Atlantic could supply about 90 % of the bacterial carbon demand. Some larger, faster sinking aggregates escape solubilization and disaggregation in the upper 1000 m and arrive in the deep ocean and on the deep-sea bed. Seasonally varying rates of sedimentation are reflected at the deep-sea floor by deposition of phytodetrital material in summer. Approximately 2-4 % of surface water primary production reaches the sea floor in 4500 m depth at 47 degrees N 20 degrees W after a sedimentation time of about 4-6 weeks. In this region, concentrations of chloroplastic pigments increased in summer by an order of magnitude, whereas seasonal changes in activity or biomass parameters were smaller. Breakdown of the generally strongly degraded organic matter deposited on deep-sea sediments is mainly accomplished by bacteria. Rates of degradation and efficiency of biomass production depend largely on the proportion of biologically labile material which decreases with advancing decay. It is likely that different levels of organic matter deposition influence the bioturbation rates of larger benthos, which has an effect on transport processes within the sediment and presumably also on microbial degradation rates.4.Philos. Trans. R. Soc. Lond. Ser. B-Biol. Sci. 1995 May 30 348 1324' PLYMOUTH MARINE LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLAND ALFRED WEGENER INST POLAR & MARINE RES,W-2850 BREMERHAVEN,GERMANY INST OCEANOG SCI,DEACON LAB,WORMLEY GU8 5UB,SURREY,ENGLAND TURLEY CM PLYMOUTH MARINE LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLANDHATimes Cited: 25 English Article RC875 PHIL TRANS ROY SOC LONDON BISI:A1995RC87500013<+*'2&%$h(v)"#;! Tyler, P. A. 1988"Seasonality in the deep sean81Oceanography and Marine Biology: an Annual Review26227-2580*Ueyanagi, S S. Kikawa M. Uto Y. Nishikawa  1970XRDistribution, spawning, and relative abundance of billfishes in the Atlantic Ocean82Bulletin of Far Seas Fisheries Research Laboratory 3 15-55>7UFINTSEV, G. B. V. M. LITVIN N. A. MOROVA M. V. RUDENKOe 1973LFNew data on morphological structure of reef zone of the Atlantic OceanDAN SSSR 208(1)214-217} in Russian$UKRAINSKY, V. V A. P. SHUBENKO 1983ZTSome regular trends of water temperature and meteo-elements at the oceanic station C Trudy GOIN 164 54-66 in Russian Vaillant, Lh 1887<6Considrations sur les Poissons des grands profondeursNH Comptes Rendus des Sances de lAcadmie des Sciences (10 Janvier 1887) 3  Vaillant, L. 1888PoissonshaExpditions Scientifiques du Travailleur et du Talisman pendant les annes 1880, 1881, 1882, 1883n Paris Van Aken, H.M Boer de,C.J 1995\VOn the synoptic hydrography of intermediate and deep water masses in the Iceland BasinDeep-Sea Researchl part I 42e20165-189[Van Aken,H.M Becker,G 1996`YHydrography and through-flow in the north-eastern north Atlantic Ocean:the NANSEN project{Progress in Oceanography38297-346e("Van Der Spoel, S Pierrot-Bults,A.C 1979,&Zoogeography and diversity of plankton("Zoogeography of the Atlantic Ocean168-190t$Van Der Spoel, S Heyman, R.P. 1983("A comparative atlas of zooplankton Bunge, Utrecht 186tVan Der Spoel, S 1985@:What is unique about open-ocean biogeography; zooplankton? JCPierrot-Bults, A.C. van der Spoel, S. Zahuranec, B.J. Johnson, R.K.\F@Pelagic biogeography. Proceedings of an international conference The Netherlandsf254-260K0)UNESCO technical Papers in Marine Science 4929 May- 5 June 1985nVan Der Spoel,Si 199460The basis for boundaries in pelagic biogeographyProgress in Oceanography34121-133 Van Der Spoel, S 1994D>History, progress ans future of theory in pelagic biogeographyProgress in Oceanography34101-107z185-194$://000074814000006Van der Spoel, S.*$Pelagic biogeography and temperature,%Annales De L Institut OceanographiqueD>zooplankton; biogeography; temperature; greenhouse-effect deep,&The influence of recent temperature changes on plankton biogeography and vertical distribution are compared with temperature variations and biogeographical distributions in the geological past. The combination of food supply and temperature is determinant for vertical and horizontal distribution patterns. From studies of paleo-biogeography we have predicted patterns of changes that might take place as a result of possible future climate change. Special attention has been given to likely changes in the Vertical distribution of deep- sea animals.Ann. Inst. Oceanogr. 1997732'Univ Amsterdam, Zool Museum, Mauritskade 61,PB 94766, NL-1090 GT Amsterdam, Netherlands Univ Amsterdam, Zool Museum, NL-1090 GT Amsterdam, Netherlands Van der Spoel S Univ Amsterdam, Zool Museum, Mauritskade 61,PB 94766, NL-1090 GT Amsterdam, Netherlands<6Times Cited: 1 English Article 100JX ANN INST OCEANOGRISI:000074814000006Van Der Spoel, S 1997*$Pelagic biogeography and Temperature&Annales Intitut Oceanographique- 73(2)k185-194ef_Van Dover, C. L. D. Desbruyres N. Segonzac T. Comtet, L. Saldanha A. Fiala-Mdioni C. Languir ( 19966/ Biology of the Lucky Strike hydrothermal field)Deep Sea Research- I 43 (9) 1509-1529Van Soest, R.W.M.r 1979North-South diversity. ,%Van der Spoel, S. Pierrot-Bults, A.C.o,&Zoogeography and diversity of plankton (!(Arnold) London & (Bunge) Utrecht103-111Vecchione, M Grant, G.C 1983^XA mutivariate analysis of planktonic molluscan distribution in the Middle Atlantic Bight"Continental Shelf Researchs 1 (4)l405-424Vedel, G. Depledge, M. 1995leTemperature tolerance and selected trace metal concentrations in some Azorean gastropod molluscs. , ,pAoreana Supl.a113-124\egation in the upper 1000 m and arrive in the deep ocean and on the deep-sea bed. Seasonally varying rates of sedimentation are reflected at the deep-sea floor by deposition of phytodetrital material in summer. Approximately 2-4 % of surface water primary production reaches the sea floor in 4500 m depth at 47 degrees N 20 degrees W after a sedimentation time of about 4-6 weeks. In this region, concentrations of chloroplastic pigments increased in summer by an order of magnitude, whereas seasonal changes in activity or biomass parameters were smaller. Breakdown of the generally strongly degraded organic matter deposited on deep-sea sediments is mainly accomplished by bacteria. Rates of degradation and efficiency of biomass production depend largely on the proportion of biologically labile material which decreases with advancing decay. It is likely that different levels of organic matter deposition influence the bioturbation rates of larger benthos, which has an effect on transport processes within the sediment and presumably also on microbial degradation rates.4.Philos. Trans. R. Soc. Lond. Ser. B-Biol. Sci. 1995 May 30 348 1324' PLYMOUTH MARINE LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLAND ALFRED WEGENER INST POLAR & MARINE RES,W-2850 BREMERHAVEN,GERMANY INST OCEANOG SCI,DEACON LAB,WORMLEY GU8 5UB,SURREY,ENGLAND TURLEY CM PLYMOUTH MARINE LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLANDHATimes Cited: 25 English Article RC875 PHIL TRANS ROY SOC LONDON BISI:A1995RC87500013 SMcKenzie199223McKenzie19995McKenzie20000g Mead1965Medeiros1990Medeiros1993 Medina2001 Mees1997 Meggers2002 Meincke1992Z Meincke1992 Meincke1999 Meir1994P Meise-Munns19846 Melle2000 melle2000MELNIKOV1999 Melo19838 Menard1964 Menard19949Menezes1991aMenezes1991b Menezes19935 Menezes1994 Menezes1995 Menezes1995 MENEZES1996 Menezes1997 Menezes1998 Menezes1999 Menezes2001Y Merrett1980h Merrett1980i Merrett1986} Merrett1990 Michel2002c Middleton1999 Middleton2001 Middleton2001 Mikkelsen1995$ Miller1993f Mills1997I Moeller1996 MOISEEV1986 Moiseev1987 Moiseev1988 Moiseev1988 Moiseev1989 Moiseev1989 MOISEEV1989 Moiseev1992 Moiseev2001 Moiseev2001\ MOKANU19811] MOKANU19811 Monaco1905Monteiro (unpubl.)vMonteiro1986&Monteiro1989Monteiro1990Monteiro1990jMonteiro1990Monteiro1991kMonteiro1991Monteiro1992Monteiro1993Monteiro19959Monteiro1995Monteiro1995)Monteiro19954Monteiro19955Monteiro19956Monteiro19957Monteiro1995lMonteiro1996mMonteiro19968Monteiro19969Monteiro1996:Monteiro1996;Monteiro1996DMonteiro1996<Monteiro1997EMonteiro1997'Monteiro1998.Monteiro19989=Monteiro1998>Monteiro1998>Monteiro1998?Monteiro1998GMonteiro1998@Monteiro1999*Monteiro2000AMonteiro2001BMonteiro2001Monteiroin pressMonteiroin pressC Monteiro_LR1999C Monteiro_PR1999 Moore1994 Moore1995 Moore1995 Moore1995 Morales1991% Morales1993 Morales1997 Morales1999 Morato2001n Moreno1992o Morin1992 MOROVA19737 MOROZENKO1987n Morn1992  Morton1995 Moseley1885 Moskalenko1981Moskalev1990Moskalev1990Moskalev19979  Moss1992o Mourino2001p Mukhacheva1976q Mukhacheva1981 MUKHIN19868 Mukhin19878 Mullineaux1990 Mullineaux1994} Mullineaux1995f Mullineaux1997 MUROMTSEV1963 Murray18858r Murray1912 Murton19966 Musaeva2000C Musaeva2000 Muscheler2002- Mnnich2000 N2001s Nafpaktitis1968t Nafpaktitis1975 NAGURNY1983uNakamura1985vNakamura1993  Nash1991 Nash19929 Nash19929  Nash1993  Nash1994) Nash19949+ Nash19959, Nash19959 NAZAROV1990 NAZIMOV1972 NAZIMOV1974 NAZIMOV1977R Nederbragt1992 NEFEDOV1983Negre-Sadargues2000 Neill1992 Neilson1999# Nelson1993999# Nelson1993999# Nelson19939Nelson19939 Nelson1993999# Nelson19939 Nelson19939 Nelson19939 Nelson19939 Nelson19939 Nelson19939# Nelson19939 Nelson19939 Nelson19939 Nelson19939 Nelson19939n1999# Nelson1993999# Nelson1993999# Nelson1993999# Nelson19939n1999# Nelson1993999# Nelson19939n1999# Nelson1993999# Nelson19939# Nelson1993999# Nelson1993999# Nelson1993999# Nelson19939# Nelson19939# Nelson19939# Nelson19939 Nelson19939 Nelson19939# Nelson19939# Nelson19939# Nelson1993999# Nelson1993999# Nelson1993999# Nelson1993999# Nelson19939McKenzie19995McKenzie20000g Mead1965̴Medeiros1990~Medeiros1990̵Medeiros1993Medeiros1993 Medina2001 Mees1997 Meggers2002 Meincke1992Z Meincke1992 Meincke1999 Meir1994P Meise-Munns19846 Melle2000 melle2000MELNIKOV1999 Melo19838 Melo19838 Menard1964̶ Menard19949 Menard19949Menezes1991aMenezes1991aMenezes1991bMenezes1991b Menezes1993 Menezes19935 Menezes1994 Menezes1995 Menezes1995 MENEZES1996 Menezes1997 Menezes1997 Menezes1998 Menezes1998 Menezes1999 Menezes1999 Menezes2001Y Merrett1980h Merrett1980i Merrett1986} Merrett1990 Michel2002c Middleton1999 Middleton2001 Middleton2001 Mikkelsen1995 Mikkelsen1995$ Miller1993f Mills1997I Moeller1996 MOISEEV1986 Moiseev1987 Moiseev1988 Moiseev1988 Moiseev1989 Moiseev1989 MOISEEV1989 Moiseev1992 Moiseev2001 Moiseev2001\ MOKANU19811] MOKANU19811 Monaco1905 Monaco1905Monteiro (unpubl.)Monteiro (unpubl.)vMonteiro1986&Monteiro1989Monteiro1989̴Monteiro1990Monteiro1990jMonteiro1990~Monteiro1990Monteiro1990Monteiro1991kMonteiro1991Monteiro1991Monteiro1992Monteiro1992̵Monteiro1993Monteiro1993̆Monteiro19959Monteiro1995Monteiro1995)Monteiro19954Monteiro19955Monteiro19956Monteiro19957Monteiro1995Monteiro1995Monteiro1995lMonteiro1996mMonteiro19968Monteiro19969Monteiro1996:Monteiro1996;Monteiro1996DMonteiro1996<Monteiro1997EMonteiro1997'Monteiro1998.Monteiro19989=Monteiro1998>Monteiro1998>Monteiro1998?Monteiro1998GMonteiro1998@Monteiro1999*Monteiro2000AMonteiro2001BMonteiro2001Monteiroin pressMonteiroin pressMonteiroin pressMonteiroin pressC Monteiro_LR1999C Monteiro_PR1999 Moore1994 Moore1994 Moore1995 Moore1995 Moore1995 Moore1995 Moore1995 Moore1995 Morales1991% Morales1993 Morales1997 Morales1997 Morales1999 Morato2001n Moreno1992o Morin1992 MOROVA19737 MOROZENKO1987n Morn1992  Morton1995 Morton1995 Moseley1885 Moskalenko1981̅Moskalev1990̆Moskalev1990̾Moskalev19979  Moss1992 Moss1992o Mourino2001p Mukhacheva1976q Mukhacheva1981 MUKHIN19868 Mukhin19878 Mullineaux1990 Mullineaux1994} Mullineaux1995f Mullineaux1997̿ MUROMTSEV1963 Murray18858r Murray1912̫ Murton19966 Musaeva2000C Musaeva2000 Muscheler2002- Mnnich2000 N2001s Nafpaktitis1968t Nafpaktitis1975 NAGURNY1983uNakamura1985vNakamura1993  Nash1991 Nash1991 Nash19929 Nash19929 Nash19929 Nash19929  Nash1993 Nash1993  Nash1994) Nash19949 Nash1994 Nash19949+ Nash19959, Nash19959 NAZAROV1990 NAZIMOV1972 NAZIMOV1974 NAZIMOV1977R Nederbragt1992̬ NEFEDOV1983Negre-Sadargues2000 Neill1992 Neilson1999# Nelson19939 wVvutHG>Z,&Dam, H.G. Roman, M.R. Youngbluth, M.J. 1995Downward export of respiratory carbon and dissolved inorganic nitrogen by diel-migrant mesozooplankton at the JGOFS Bermuda time-series station.Deep-Sea Research I42 1187-1197Dautzenberg, P.r 1889@9Contribution la faune malacologique des les des Aores2nhRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverain du Monaco(!Fascicule I, Imprimerie du Monaco112 pp. + IV platesDe Stasio,B.T.Jr 1993f`Diel vertical and horizontal migration by zooplankton:population budgets and the diurnal deficitMarine Research}531} 44-648hbdel Nevo, A. J. Dunn, E. E. K. Medeiros, F. M. LeGrand, G. Akers, P. Avery, M. I. Monteiro, L. R. 1990{The status, distribution and conservation of Roseate Tern (Sterna dougallii) and common tern (Sterna hirundo) in the Azores;K^lXQ Relatrio da Universidade dos Aores e Royal Society for the Protection of BirdsS 22ppf_del Nevo, A. J. Dunn, E. K. Medeiros, F. M. Le Grand, G. Akers, P. Avery, M. I. Monteiro, L. R.u 1993ZThe status of Roseate terns Sterna dougallii and Common terns Sterna hirundo in the Azores,>LSeabird 15 30-374D>DEMENIN, N. A. V. A. KOLCHIN A. M. SAFRONOV V. I. VINNICHENKO. 1998{Russian investigations and fishery of Roundnose Grenadier (Coryphaenoides rupestris) on the Mid-Atlantic Ridge in 1996-19979RKThe Study Group on the Biology and Assessment Deep-Sea Fisheries Resourcesc Working doc.: 1-4..(!Desbruyres, D. Alayse, A.-M. Antoine, E. Barbier, G. Barriga, F. Biscoito, M. Briand, P. Brulport, J.-P. Comtet, T. Cornec, L. Crassous, P. Dando, P. Fabri, M. C. Felbeck, H. Lallier, F. Fiala-Mdioni, A. Gonalves, J. M. Menard, F. Kerdoncuff, J Patching, J. Saldanha, L. Sarradin, P.-S.r 1994New information on the ecology of deep-sea vent communities in the Azores triple junction area: preliminary results of the Diva-2 cruise (May 31-July 4 1994)Interridge News838 18-198DETINOVA, N. N.8 1985>8Chaetognaths of the Reykjanes Ridge (the North Atlantic)Moscow. Trudy IOAN 120\ 96-136 in Russiann Dias, M. L. Barraca, I. F. 1971jdSobre a pesca de tundeos nas costas de Portugal continental e ilhas da Madeira e Aores (1961-1970)<5Boletin Informativo do Instituto de Biologia Martima2 14pp0)Fisheries; technology; commercial speciesc*$Dias, M. L. Olsen, K. stvedt, O. J. 1976ZTReport on a cruise by the R. V. "G. O. Sars" to the Aores and the coast of Portugal:4International Council for the Exploration of the SeaC.M. 1976/J:12(!Pelagic Fish (Southern) Committee 44pptnFisheries; cruises; technology; Oceanography; plankton; development; larvae and juveniles; Ecology; demography"Dias, M. L. Monteiro, M. C. 1986HApesca exploratria e observaes hidrolgicas em guas dos Aoresh("22pp + 47 tables, + 4pp+25 figures2,Fisheries; cruises; technology; Oceanography*$Dias, M. L. Krug, M. H. Silva, H. M. 1990B://000080477800001RHargreaves, P. M.l~xThe vertical distribution of micronektonic decapod and mysid crustaceans across the Goban Spur of the Porcupine Seabight Sarsiadecapod crustaceans; North Atlantic; micronekton northeast atlantic-ocean; near-bottom; bathymetric distribution; suprabenthic mysids; diel migrations; slope; water; sea; assemblages; zooplankton4The vertical distribution of micronektonic Decapoda and Mysidacea (Crustacea) is examined along a cross-slope transect of stations with soundings ranging from 192 m to 1800 m in the Porcupine Seabight during spring 1994. Eight species were found only at the three deep-water open oceanic stations to the west of the slope, while the horizontal ranges of others extended from deep-water to the outer (lower) slope station. The numbers of species caught at the inner (upper) slope and shelf station were lower than offshore. The species assemblages were broadly different at the deep-water, upper slope and shelf stations with no species occurring continuously across the whole of the transect. Three deep-living species were found in higher concentrations near-bottom over the slope than at similar depths at the adjacent open ocean stations. Factors affecting distribution of species are discussed. Sarsia 19998412+Times Cited: 1 English Article 199JQ SARSIAISI:000080477800001 zKXJIyx. Dias, M. L.e 1991tm Pesca exploratria com palangre em guas dos grupos central e oriental do Arquiplago dos Aores (1979-1983)c0)Relatrios Tcnicos e Cientficos do INIP, Lisboa (46) Novembro 19911 26ppB://000171207400006fjdKhripounoff, A. Vangriesheim, A. Crassous, P. Segonzac, M. Colaco, A. Desbruyeres, D. Barthelemy, R.~xParticle flux in the Rainbow hydrothermal vent field (Mid- Atlantic Ridge): Dynamics, mineral and biological composition Journal of Marine Researchvplucky-strike segment; endeavor ridge; water ("Joint,I Williams,P.J.Leb Savidge,G 2001|Comparisons of plankton at 59 N and 37 N during two langragian drift experiments in the North Atlantic in june and July 1996Deep-Sea Research\ part II 48 1043-1061\$MICROZOOPLANKTON, CARBON, SEA Data are summarised for two Lagrangian experiments in the North Atlantic in early summer 1996. At 59 degreesN 20 degreesW, plankton dynamics was studied in an SF, tracer release experiment within a mesoscale eddy over a 9-day period. At 37 degreesN 20 degreesW, a second experiment followed a drifting buoy for 7 days. The data obtained in these two experiments have been averaged for 3 depth strata; the euphotic zone, the surface mixed layer (SML), and the seasonal thermocline immediately beneath the surface mixed layer. At 59 degreesN, the euphotic zone was only marginally deeper than the SML, but at 37 degreesN the SML was ca 30 m and the euphotic depth was ca 110 m. At 37 degreesN, nutrient concentrations in the SML were low but significant new production occurred in the thermocline because of light penetration into the nutricline. The particulate organic carbon (POC) concentration of the SML at 59 degreesN was 13-15 mu mol C kg(-1), but at 37 degreesN POC concentrations were 4 mu mol C kg(-1). These POC measurements include biota and detritus. As a way of investigating latitudinal differences in the plankton communities, estimates have been made of the carbon and nitrogen content of phytoplankton, bacterioplankton, microzooplankton and mesozooplankton. At both 59 degreesN and 37 degreesN, phytoplankton was the largest component, accounting for ca 50% of the planktonic biomass in the SML. At 59 degreesN, microzooplankton was 16% of the planktonic carbon, but at 37 degreesN this reduced to 8% of the total. Mesozooplankton was a relatively constant proportion (ca 20%) of the planktonic carbon in the SML at both 59 degreesN and 37 degreesN. Bacterioplankton was 14% of the biomass at 59 degreesN, increasing to 24% in the microbial loop-dominated system at 37 degreesN. Mean carbon fixation rate in the oligotrophic southern station was 24% of that at the north, with more carbon fixation below the SML at 37 degreesN than at 59 degreesN. Respiration rates showed little variation with latitude, and the rates at 37 degreesN were 80% of those at 59 degreesN. Nitrate and ammonium uptake rates were very low in the oligotrophic conditions in the SML at 37 degreesN, but nitrate uptake in the euphotic zone was comparable to that at 59 degreesN. Ammonium uptake by phytoplankton was also significantly greater at 37 degreesN, in both the euphotic zone and thermocline, but uptake in the SML was only 20% of that in the SML at 59 degreesN. (C) 2001 Elsevier Science Ltd. All rights reserved.187-193$://A1989CB38600004c Kaartvedt, S.^WNocturnal Swimming of Gammaridean Amphipod and Cumacean Crustacea in Masfjorden, Norway  Sarsia Sarsia 1989743v'}UNIV BERGEN,DEPT MARINE BIOL,N-5065 BLOMSTERDALEN,NORWAY KAARTVEDT S UNIV BERGEN,DEPT MARINE BIOL,N-5065 BLOMSTERDALEN,NORWAYa2,Times Cited: 17 English Article CB386 SARSIAISI:A1989CB38600004h) Horta D>Departamento de Oceanografia e Pescas, Universidade dos Aores 64pp + anexos@9Fisheries; statistics; biology; age; growth; reproduction Isidro, E. 1996b[Biology and population dynamics of selected demersal fish species of the Azores Archipelagot:4Department of Environmental and Evolutionary Biology University of Liverpooly vi +m249pp (+3 appendices) PhD}<5Fisheries biology; biology; age; growth; reproductionn; MATUL, A. Go 1994On the problem of paleo-oceanological evolution of the area of the Reykjanes Ridge (the North Atlantic) during the last deglaciation by data of studying of Radiolaria  34(6)881-889 in Russian MATUL, A. Go 1999|On relation between distribution of Radiolaria and water masses participating in formation of the North-Atlantic deep waters Okeanologiai 39(1)i152-157 in Russian109-115$://A1991GC13900001 $Mauchline, J. Gordon, J. D. M.leOceanic Pelagic Prey of Benthopelagic Fish in the Benthic Boundary-Layer of a Marginal Oceanic Region$Marine Ecology-Progress Seriesnortheastern atlantic-ocean; santa-catalina basin; deep-sea fish; rockall trough; near-bottom; midwater; water; floor; hydrography; zooplankton6jcThe availability of oceanic plankton and micronekton to the benthopelagic fish assemblages on the slopes of the Rockall Trough, a marginal region of the northeast Atlantic deep-sea environment, is examined. The vertical distribution of pelagic species predated by the fish was determined in the off-slope water column, as were the depths at which they are predated by the fish in the benthic boundary layer of the slope. The benthopelagic fish predated pelagic species at depths on the slope corresponding to the daytime depths of the pelagic prey. The occurrence of these pelagic species at the benthic boundary layer is primarily through truncation of their pelagic vertical distributions rather than horizontal impingement, although this does occur: this applies not only to epi- and mesopelagic but also to the bathypelagic species which can even reach abyssal sediments. Diel vertical migration of the pelagic species did not make them available to slope fishes in shallower depths presumably because vertical migration is strictly upwards within the pelagic water column and not up the contours of the slope sediment.Mar. Ecol.-Prog. Ser. 1991 Aug74 2-3'SCOTTISH MARINE BIOL ASSOC,POB 3,OBAN PA34 4AD,ARGYLL,SCOTLAND MAUCHLINE J SCOTTISH MARINE BIOL ASSOC,POB 3,OBAN PA34 4AD,ARGYLL,SCOTLAND>8Times Cited: 27 English Article GC139 MAR ECOL-PROGR SERISI:A1991GC13900001eoooo0nn''www!NIooAMXX.wographers themselves make their output more accessible and user-friendly for non-scientists, and take advantage of the new technologies which promise to re-vitalise the field.Prog. Oceanogr. 199434 2-3'UNIV CALIF SANTA BARBARA,INST MARINE SCI,SANTA BARBARA,CA 93106 INST OCEANOG SCI,DEACON LAB,GODALMING GU8 5UB,SURREY,ENGLAND KRAUSE DC UNIV CALIF SANTA BARBARA,INST MARINE SCI,SANTA BARBARA,CA 9310681Times Cited: 1 English Review QB204 PROG OCEANOGRISI:A1994QB20400010 3a(`P_Martins, H. R. 1985biSome observations on the naupliosoma and phyllosoma larvae of the Mediterranean locust lobster, Scyllarides latus (Latreille, 1803)t`q ICES CM 1985/K52 13ppMartins, J. A. 1986*$Potencialidades da ZEE Aoriana. , ,2,Relatrio da VI Semana das Pescas dos Aores6 (1985)125-132\2,Martins, H. R. Santos, R. S. Hawkins, S. J. 1987_Exploitation of limpets (Patella spp.) in the Azores, with a preliminary analysis of the stocks   ICES; C.M. 1987/K53 18ppMartins, A. F. M. -Ed. 1990The marine fauna and flora of the Azores. Proceedings of the First International Workshop of Malacology, So Miguel, Azores (11-24 July 1988)5Aoreana Suplemento, Outubro 1990 173pp;Martins, H. R. 1990JCA selected bibliography of the marine fauna and flora of the Azores Arquiplago Life and Earth Sciences8  35-44Martins, R A. Cascalho  1990 Pescarias de profundidade2+Relatrio da X Semana das Pescas dos Aorese10199-206& Martins, H. R. Hargreaves, P. M. 1991ngShrimps of the families Pandalidae and Hippolytidae (Decapoda, Caridae) from the eastern Atlantic Oceans ArquiplagotLife and Earth Sciences9 47-61"Martins, J. A. Santos, R. S. 1991PJBreves consideraes sobre a implementao de reservas marinhas nos Aores ,%Dias, E. Carretas, J. P. Cordeiro, P.2haPrimeiras Jornadas de Protecco do Meio Ambiente (Aores, Madeira, Canrias e Cabo Verde) (1988) Angra do Herosmo SRTA/DRA and CMAH;318-333r@:Martins, H. R. Santos, R. S. Hawkins, S. J. Nash, R. D. M. 1992Expedition Azores 1989: Ecology and taxonomy of the fauna and flora of the marine littoral. An introduction. , Life and Earth Sciences Arquiplago;Life and Earth Sciences10 39-44 Martins, H. R 1992Cephalopods in the Azores.Centenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L Hirondelle. Aoreana (Suplemento 1992)193-1989Martins, A. F. M. -Ed. 1995The marine fauna and flora of the Azores. Proceedings of the Second International Workshop of Malacology and Marine Biology, Vila Franca do Campo, So Miguel, Azores (July 21 - August 3 1991)Aoreana Suplemento Maio 1995J 316ppg"Matsui, T R. H. Rosenblatt y 1984PJReview of the deep-sea fish family Plactytroctidae (Pisces: Salmoniformes)^XBulletin of the Scripps Institution of Oceanography, University of California, San Diego  26 159pp 17-25$://A1997WG29600003n.'Matsumoto, G. I. Baxter, C. Chen, E. H.lHAObservations of the deep-sea trachymedusa Benthocodon pedunculatasInvertebrate BiologyCnidaria; Hydrozoa; Monterey Bay; benthic boundary layer; feeding; morphology benthic boundary-layer; narcomedusae cnidaria; insitu observations; feeding-behavior; zooplankton; hydrozoa; medusae; submersibles; midwater; atlanticRecent observations, from a remotely operated vehicle (ROV) working in the Monterey Submarine Canyon in the northeast Pacific and from the Johnson Sea Link II in the northwest Atlantic, revealed the presence of the trachymedusa Benthocodon pedunculata near the bottom in both oceans. Although feeding was not observed in the field or in the lab, gut contents indicate a preponderance of benthopelagic crustaceans although a wide variety of zooplankton have been found. Two morphologically different tentacle types both possess cnidae with a 3:1 ratio of euryteles to stenoteles. Unencysted metacercariae of a trematode parasite were found in the manubrium of more than half the medusae examined.Invertebr. Biol. 1997 1161'MONTEREY BAY AQUARIUM RES INST,BOX 628,MOSS LANDING,CA 95039 STANFORD UNIV,HOPKINS MARINE STN,PACIFIC GROVE,CA 93950 SUNY STONY BROOK,SCH MED,STONY BROOK,NY 11794 Matsumoto GI MONTEREY BAY AQUARIUM RES INST,BOX 628,MOSS LANDING,CA 95039<6Times Cited: 3 English Article WG296 INVERTEBR BIOLOGYISI:A1997WG29600003LZ| lL.S Smith,D.Kc 1995TNSeamount volca 1576-1593A$://000165267100012t.(Wishner, K. F. Gowing, M. M. Gelfman, C.NHLiving in suboxia: Ecology of an Arabian Sea oxygen minimum zone copepod Limnology and Oceanographyeastern tropical pacific; vertical-distribution; marine snow; southern-california; zooplankton ecology; calanoid copepods; organic-matter; water column; layer; oceani>7Oxygen minimum zones (OMZs) are permanent suboxic features of the oceanic water column that strongly influence zooplankton distributions and biogeochemical cycles. The lower interface of prominent OMZs is characterized by a subsurface zooplankton biomass peak and high biological activity. The calanoid copepod Lucicutia grandis is an indicator species for this habitat. Its ecology in the Arabian Sea was studied during the U.S. Joint Global Ocean Flux Study (JGOFS) program to understand planktonic distributional and developmental adaptations to oxygen gradients in suboxic environments and the role of the OMZ zooplankton in food webs, vertical flux processes, and carbon cycles. Zooplankton samples were obtained in vertically stratified multiple opening-closing net and environmental sensing system (MOCNESS) tows to 1,000 m during four seasonal cruises. The vertical distribution of L. grandis was associated with the steep oxygen gradient from 0.07 to 0.15 ml L-1 at the base of the OMZ about 600-1,000 m. There was a clear progression with age of the depths and oxygen levels inhabited by different developmental stages within this zone, a phenomenon attributed to both physiological constraints and ecological interactions. The seasonal and spatial pattern of reproduction and development was keyed in part to the seasonal monsoon cycle, with final maturation of young stages into reproducing adults probably triggered by the direct and indirect effects of the seasonal or episodic input to depth of sinking particles. Gut contents included surface flux material, deep-sea detrital material, zooplankton remains, and deep-sea aggregate material, indicating that L. grandis occupies at least four different trophic levels. This was an active, not a diapausing, population, since both adults and immature stages fed and reproduced during all seasons. In contrast to the pelagic fauna that are severely impacted by coastal episodic hypoxia, the animals of the oceanic OMZ are uniquely adapted to the very low oxygen and strong spatial and temporal patterns of this widespread suboxic environment.Limnol. Oceanogr. 2000 Nov457' Univ Rhode Isl, Grad Sch Oceanog, S Ferry Rd, Narragansett, RI 02882 USA Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Univ Calif Santa Cruz, Inst Marine Sci, Santa Cruz, CA 95064 USA Wishner KF Univ Rhode Isl, Grad Sch Oceanog, S Ferry Rd, Narragansett, RI 02882 USA:4Times Cited: 1 English Article 373AW LIMNOL OCEANOGRISI:000165267100012 Wishner, K.F 2000"Zooplankton in the Deep sea  Maritimes 9-13e 244-66$://A1996TX86500002fHeptner, M. V.B<The typology of vertical distribution of oceanic zooplankton Zhurnal Obshchei Biologiinbiological investigations; benthopelagic plankton; general typology; north pacific; deep-sea; evolution; migration; community; atlantic; fluxeseThe study is aimed at typological analysis of vertical distribution of different taxa and taxocenes formed by zooplankton in habited diffe931-954$://000071350200002"Saltzman, J. Wishner, K. F.D~Zooplankton ecology in the eastern tropical Pacific oxygen minimum zone above a seamount: 2. Vertical distribution of copepods<6Deep-Sea Research Part I-Oceanographic Research Papersd]boundary-layer zooplankton; calanoid copepods; arabian sea; deep; rates; ocean; system; basing : 3The abundance and vertical distribution (0-1230 m) of copepods were studied in the eastern tropical Pacific near the seamount Volcano 7 to examine the influence of the extreme oxygen minimum zone (OMZ). Maximum zooplankton biomass and copepod abundance were in the thermocline zone. A secondary peak in biomass and copepod abundance was evident between 600 and 1000 m, which included the depth of the lower interface of the OMZ. This prominent secondary peak in zooplankton is a feature unique to OMZ regions. There were four general trends of vertical distribution of copepod abundance. These trends appeared to be related to the oxygen concentration and gradients. The most common vertical distribution was a pattern of maximum abundance in the mixed layer and thermocline zones, with a secondary maximum in the zone of the lower OMZ interface (600-1000 m). Clausocalanus spp., Oncaea, spp., Euchaeta spp., Oithona spp. and Corycaeus spp. showed this trend. Low oxygen concentration did not appear to restrict these groups, since they were present throughout the OMZ. The second vertical distributional pattern was vertical migration between the thermocline and the OMZ. Pleuromamma robusta showed this pattern, with maximum abundance al night in the thermocline zone and during the day in the core of the OMZ. In addition, there was a secondary maximum of abundance at the lower OMZ interface zone. The third type of distribution was shown by copepods that were abundant in the upper OMZ and at the lower OMZ interface zones. Eucalanus inermis, Haloptilus paralongicirrus and Heterostylites longicornis were dominant copepod species that exhibited this pattern. They were either absent from the mixed layer or at similar abundances in the mixed layer and upper OMZ. The fourth pattern was shown by copepod species that live primarily above the OMZ day and night. The majority of the species appeared to be tolerant of the extreme low oxygen concentrations. Rhincalanus spp. was the dominant copepod that was excluded by low oxygen concentrations. In general, species also found in other OMZ regions showed similar distributions in this study, indicating that low oxygen is a major controlling factor. Some vertical niche separation among congeneric species was indicated for Eucalanidae, Metridiidae and Augaptilidae. Published by Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 Jun446'Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Saltzman J Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USAJCTimes Cited: 11 English Article YQ117 DEEP-SEA RES PT I-OCEANOG RESISI:000071350200002_ d139-164$://000079477500008 Rossby, T.On gyre interactions@9Deep-Sea Research Part Ii-Topical Studies in Oceanographypnorth-atlantic current; gulf-stream meanders; potential vorticity; surrounding waters; fluid exchange; cape-hatteras; sargasso sea; variability; transport; circulation The principal meeting point of the subtropical and subpolar gyres of the North Atlantic is at the Tail of the Grand Banks where the two western boundary currents, the Gulf Stream and Labrador Current, join forces as the North Atlantic Current, which flows northeast almost 10 degrees in latitude before turning east as the Subpolar Front, ultimately feeding the Labrador and Nordic Seas and the thermohaline overturning. After the Gulf Stream turns into the North Atlantic Current at the Grand Banks, its role shifts from a wind-driven current to a link in the large-scale thermohaline circulation. The processes governing this transition, in particular the continued transport north of mass and heat, are questions of considerable climatic importance. The North Atlantic Current is a very unusual western boundary current in that its mass transport decreases in the downstream direction. The mean path and annual shifting of the eastward flowing Gulf Stream is conjectured to result from a time-varying shelf-Slope Water overflow of waters from the Labrador shelf. As the volume transport increases in fall and deepens the Slope Water pycnocline, it forces the Gulf Stream south and deepens the Sargasso Sea thermocline as well. The timing of these steps governs the June maximum in baroclinic transport. There is some evidence that this 'back-door' gyre interaction may operate on interannual time scales as well. The question then arises whether the shelf-to-Slope Water Sea transport also plays a role in governing the separation of the Gulf Stream. The widely observed robustness of the width of the Gulf Stream appears to result from a tight balance between the release of available potential energy and the kinetic energy of the current. A broader current would release more energy than can be 'disposed of', while a narrower current requires more kinetic energy than is available to sustain it. It is shown that for plausible dissipation rates in the recirculation gyres, the amount of energy that needs to be expelled from the Gulf Stream is such a small fraction of that advected through as to be vitually undetectable, hence the stiffness of the current. (C) 1999 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 199946 1-2'Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA Rossby T Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USAHBTimes Cited: 3 English Article 182AZ DEEP-SEA RES PT II-TOP ST OCEISI:000079477500008action of that advected through as to be vitually undetectable, hence the stiffness of the current. (C) 1999 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 199946 1-2'Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA Rossby T Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USAHBTimes Cited: 3 English Article 182AZ DEEP-SEA RES PT II-TOP ST OCEISI:00007947750000821 2105-2118O$://0000776170000060"Herring, P. J. Dixon, D. R.ePJExtensive deep-sea dispersal of postlarval shrimp from a hydrothermal vent<6Deep-Sea Research Part I-Oceanographic Research Papers|umid-atlantic ridge; fuca ridge; decapoda; bresiliidae; crustacea; genus; alvinocarididae; populations; plumes; larvaehbHydrothermal vent fields on the Mid-Atlantic Ridge (MAR) are small (no more than 0.1-1.0 km(2)) and widely spaced (a reported average of one field per 175 km between 11 degrees N and 40 degrees N). Their faunas are similar and usually dominated by shrimp of the family Bresiliidae. Little is known about the way these animals (and other members of the vent fauna) disperse and colonize new vents. Vent shrimp juveniles have been taken close to certain vent sites, and in midwater, but their larvae and postlarvae have not been captured. We report here that bresiliid shrimp postlarvae are very widely dispersed around the Broken Spur vent field and extend into the next MAR segment and the Atlantis Fracture Zone beyond. The populations show density gradients declining both vertically and horizontally from the vent site, in contrast to the overall pelagic biomass. This is the furthest recorded dispersal (> 100 km) of identified larvae from a hydrothermal vent and is sufficient to give them access to adjacent vent fields and thus the scope for colonising new sites. (C) 1998 Elsevier Science Ltd. All rights reserved..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1998 Dece4512'Southampton Oceanog Ctr, Empress Dock, Southampton SO14 3ZH, Hants, England Southampton Oceanog Ctr, Southampton SO14 3ZH, Hants, England Plymouth Marine Lab, Plymouth PL1 2PB, Devon, England Herring PJ Southampton Oceanog Ctr, Empress Dock, Southampton SO14 3ZH, Hants, EnglandHBTimes Cited: 9 English Article 149QP DEEP-SEA RES PT I-OCEANOG RESISI:000077617000006tHilgendorf, F. 1888blDie Fische der Azorenr  Simroth, H. @:Zur Keenntniss der Azorenfauna. Archiv fr Naturgeschichte 1(3)179-234n$Checklist; museum collectionsHAHilton, G.M K. Lilliendahl Solmundsson, D.C Houston R.W. Furness _ 2000D=Geographical variation in the size of body organs in seabirdsaFunctional Ecology14 369-379.("Hilton_GM Furness_RW , Houston_DC  2000B;A comparative study of digestion in North Atlantic seabirdso  Journal of Avian Biology  31 36-46. Hogg, N.G. 19804.Effects of Bottom Topography on Ocean Currents NHWMO-ICSU Joint Scientific Committee Global Atmospheric Research Program.F?Orographic Effects in Planetary Flows, GARP Publication Series.23167-205r-336ܿ1vy@QmF31999y22000s (Eds.)1992I=-:New views of the Atlantic. Topical studies in oceanography.1990I 1985.1985a Aores/891990 AGAFONOVA1990 Agostinho1954Z Aguiar1982J Aken1995K Aken1996 Akers1990 Akers1993 Aksnes1996 Aksnes1998 Aksness1996 Alayse1994ALEKSEEV1978ALEKSEEV1979ALEKSEEV1982ALEKSEEV1983ALEKSEEV19844ALEKSEEV1987ALEKSEEV1991ALEKSEEV1995 ALEKSEEVA1978 ALEKSEEVA1979 ALEKSEEVA1979 ALEKSEEVA1979 ALEKSEEVA1983 ALEKSEEVA1984 ALEKSEEVA1984 ALEKSEEVA1987 ALEKSEEVA1991 Allen2000 Alves1990 Alves2000 Amelekhina1985 Anadon2001GAndersen20011Andersen20011 Andrade1995 Angel1975 Angel1982 Angel19899 Angel1993Y Angel1993 Angel1993X Angel1994W Angel1996 ANIKEEV2001:Anokhina20000 ANON1977 ANON.1974 ANON.1974  ANON.1975! ANON.1977" ANON.1977# ANON.1978$ ANON.1978% ANON.1978& ANON.1979' ANON.1980( ANON.1980) ANON.1980* ANON.1981+ ANON.1984, ANON.1984- ANON.1986. ANON.1987/ ANON.19880 ANON.19881 ANON.19892 ANON.19933 ANON.1998 Antoine1994 Arhan1988 Arhan1988L Arhan1990 Arkhipkin1997 Arkhipkin2001 Arkhipkin2001Arnautov19977=Arnautov19988Arnautov19999 Arnbom1987 Arnbom1988 Arnbom1988[ Arruda19919] Arruda19929 Arruda1992} Ashjian1995: Asper1992 Astthorson1992 Astthorson2000C Astthorsson1992D Astthorsson1992A Astthorsson1995B Astthorsson1995? Astthorsson1996< Astthorsson1998= Astthorsson1998> Astthorsson1998 Astthorsson2000  Astthorsson20005 Astthorsson20006 Astthorsson2000: Astthorsson2000 Astthorsson2000 Astthorsson2000Atkinson1992 Avery1990 Avery1993[ Azevedo1991\ Azevedo1992] Azevedo1992 Azevedo1992 Azevedo1992^ Azevedo1995_ Azevedo1995n Azevedo1995 Azevedo1995`Azevedoin press Baber 1989a Backus1970b Backus1977M Bacon1997} Baddock19904 BAIDALINOV19775 BAIDALINOV1979 Bainbridge19546 BAKAY19847 BAKAY1984C BAKAY19868 BAKAY19889 BAKAY1992: BAKAY1997B BAKAY.19898 Baker1982 BALABANOVA1979; BALABANOVA1981 BALABANOVA1981Y Baldwin1992 Balguerias1997SBalsiger19922 Bannerman1966 Bannerman1966< BARANOV1972 Barbier1994c Bard1986d Bard1987= BARINOV1977> BARINOV1981? BARINOV1986t Barraca1971e Barreiros1995- Barreirosin press Barriga1994 Barrois1888 Barros19879 Barthelemy20011 Bass20022  Batchelder1995! Batchelder1995 Batten20000f Bauchot1971 Bauchot1989g Bauchot1993 Baumann20023 Baxter19979 Bean189555 Beare2000C Bearhop_S1999" Becker19969K Becker1996 Beckman2001Beckmann1988Beckmann1995Beckmann1995Beckmann1995(Beckmann20012S Bedini19929 Bedo19919 Beer2002+ Bell20000Bellan-Santini1993 Berenboim1992 Bernstein1999 Bersch1995 Bersch1999N Bersch1999| Bertelsen1985 Bethoux1992 Bett19949, Bianchi1999G Bianchi2001 Bianchi2001 Bibby1991 Bidigare19951 Bieler1995Bienfang19911Biscoito19949 Bitukov1997Bjorndal1992Bjorndal1993 Blackburn1981@ BLAZHCHIKHIN1986 Blindheim1996 Blindheim1996 BLIZNICHENKO1986 Bliznichenko1987  Bodvarsdottir2000 Bodvarsdottir2000Boehlert1985Boehlert1987Boehlert1999J Boer1995# Boer de1995BOGDANOV1969BOGDANOV1990A BOGOROV1969BBOGOVSKI1989CBOGOVSKY1986 Bollens1989 Bollens1989 Bollens1991 Bollens1991 Bollens1993 Bollens1994 Bollens1994 Boltachev1985 Bolten1990 Bolten1992 Bolten19930 Bolton20002BONDAREV1988h Borodin1931 Bouchet19911 Bourdillon1999 Bourdillon1999 Bourdillon19999 Bowen2002O Bower2000 Boyd19979 Boyd19979 Boyle1994 Boytsov1984Brechner Owens1995 Briand19949 Brickle2001 Brickle2001i Briggs1966j Briggs1970k Briggs1974 Brink1990l Brito1983Brulport19949 Brum19878m Brum1992n Brum1995 Brum19951`Brumin presse Bryan1997Buchanan1885 Bucklin2000& Buhring2001; Bulgakova1995Burnay 1990aa- Burns1998/ Burns1999D BURUKOVSKY1993 Bhring2001 C.1992S Cain19929;Campbell2000Campbell2000oCapello1871a Carlin19969 Cartaxana1992Carvalho19979Carvalho1998_Cascalho1990yCascalho1991 Case1999Castillo2000e Castle1982g Castle19939 Chapman1996 Chaves1924Chavigny19323 Chen19979 CHERNYAVSKY1974 Christiaens1973- Christiansen1999 Christiansen1999& Christiansen2001( Christiansen2001 Christiansen2001 Christiansen2001E CHUKSIN1975F CHUKSIN1975CHUMAKOV19919 Clark1988 Clark2001 Clark2001 Clarke1954 Clarke1956 Clarke1981 Clarke19855 Clarke1993p Clarke1995q Clarke1995q Clarke1995 Clarke1996 Clarke1996 Cocco1992 Cohen1983 Colaco20010r Collett1897 Collett1897 Collett1905s Collins1954[CollinsRCollins, B. L. 1954. Lista de peixes dos mares dos Aores. Aoreana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40.reana, II (5), 1-40.ana, II (5), 1-40.ana, II (5), 1-40.ana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40.ana, II (5), 1-40.ana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40. Aoreana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40.reana, II (5), 1-40.ana, II (5), 1-40.oreana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.ana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.oreana, II (5), 1-40.oreana, II (5), 1-40.ana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.a, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.reana, II (5), 1-40.ana, II (5), 1-40.oreana, II (5), 1-40.oreana, II (5), 1-40. II (5), 1-40.(5), 1-40. y Shimko, V.P.SHISHLO, Yu. V.SHLIBANOV, B. I.Shlibanov, V.I. Shores, D. L.SHUBENKO, A. P.Shushkina, E. A.Sieracki, M. E. SIGAEV, I. K. Silva, A. A. Silva, H. M Silva, H. M.SILVA, H. M. da Silva, M. C. Silva, M.C. Simes, P. Simroth, H. Sinha, B.SIROTIN., V. A. Skreslet, S Skreslet, S. Smale, M. J. SMIRNOV, O. V SMIRNOV, V. G Smith, B. 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Tortonese, E Tortonese, E. Tranter, P.Tranter, P. R. G.TRETYACHENKO, Yu. V. Trewavas, E.Tristo da Cunha, R.TROYANOVSKY, F.M TRUNOV, I. A. Tsuchiya, M.TSVETUCHIN., A. S. TSYGANOV, V.FTucholke, B. E. Tucker, G. M. Tums, E. O. Turley, C. M. Turley, C.M Turley, C.M. Tyler, P. A.Uenzelmann-Neben, G Ueyanagi, SUFINTSEV, G. B.UKRAINSKY, V. V Uto, M. Uye, S.V.GORCHINSKY, K.Vaillancourt, R.Vaillancourt, R. D. Vaillant, L Vaillant, L. Van Aken, H.MVan Der Spoel, SVan der Spoel, S.Van Dover, C. L.Van Soest, R.W.M.Vandover, C. L.Vangriesheim, A. Vankeuren, J.Vankeuren, J. R. Vass, W.P. Vecchione, M Vedel, G.Vedernikov, V. I.Venrick, E. L. Venrick, E.L. Venzke, S.Vereshchaka, A. L.Vereshchaka, A.L Verity, P. Verity, P. G.Villanueva, R.VINNICHENKO, V.VINNICHENKO, V. IVINNICHENKO, V. I.VINNICHENKO., V. I.Vinogradov, G. M.Vinogradov, G.MVinogradov, M. E.Vinogradov, M.EVINOGRADOVA, L. AVonsteiger, R. Voss, N.A.Vostokov, S. V. Wade, I. P. Wade, I.PWakefield, W.W. Waldron, S Waldron, S. Walne, A. W. Walne, A.W Walsh, P.M Walsh, V. Walters, K. Waniek, J Ward, P. Warner, A. J. Warner, A.J Warren, B.A. Watts, S.D Weaver, A.J Weeks, J. M.Weerdt, W. H. de Weikert, H Weikert, H. Weiss, W. Wells, D.E Wells, F.E. Wheeler, A. White, E.Whitehead, P. J. Whitmore, C. Widder, E. A. Widder, E.A Wiebe, P. H. Wiebe, P.H Wilken, B.Williams, P.J.Leb Williams, R.Williamson, C. E. Wilson, L Wirtz, P. Wishner, K.Wishner, K. F. Wishner, K.FWohlleben, T.M.HWoodd-Walker, R.S Woods, L. P.Wroblewski, J.SYAROVOY, A. S.Youngbluth, M.J.ZAFERMAN, M. LZaferman, M. L.ZAFERMAN., M. L.Zahuranec, B.J.ZAKHAROV, A. N. Zeitzschel, B Zeltner, A ZEZINA, O. N Ziemann, D. ZILANOV, V. KZILANOV, V. K. Zonfrillo, B.ZUBCHENKO, ?. VZUBCHENKO, ?.VZUBCHENKO, A. VZUBCHENKO, A. V.Zubchenko., A.V. Zuev, G.V. ZYKOV., I. D.b^h 87-93$://000076804200002d*$Eiane, K. Aksnes, D. L. Ohman, M. D.(!Advection and zooplankton fitnessA Sarsiafitness; zooplankton; advection diel vertical migration; calanus-finmarchicus; population- dynamics; north-atlantic; model; bay Successful adaptation to the environment by zooplankton is constrained by the agents of mortality (starvation, predation) and losses due to advection. A fitness measure which explicitly includes risk of advective loss is presented. The authors show that as horizontal current speeds and vertical shear increase, the behavioral strategies that maximize fitness of zooplankton possessing different life history strategies are affected. For a Calanus finmarchicus-type life history, fitness is maximized by diel vertical migrations when advection risk in surface waters is low and by spending less time in the surface layers as flow rate increases. For a Paracalanus parvus-type life history, vertical migration is postulated to occur as advective loss increases. The geographic length scale of the habitat of residence also affects the optimal mode of habitat selection. In the Calanus case an abrupt change in the optimal vertical migration pattern is postulated as a function of length scale of habitat and rate of advection. Sarsia 19988322+Times Cited: 0 English Article 135LX SARSIAISI:000076804200002 Ellis,C.J 1985lfThe effects of proximity to the continental slope sea-bed on pelagic halocyprid ostracods at 49 N,13 WMarine Biology65923-949\Epp, D. Smoot, C.N.1 19896/Distribution of seamounts in the North Atlanticw Nature 3375254-257p254-257$://A1989R858200066Epp, D. Smoot, N. C.6/Distribution of Seamounts in the North-Atlantic Nature Nature 1989 Jan 19 337o 6204'NATL SCI FDN,1800 G ST NW,WASHINGTON,DC 20550 USN,OCEANOG OFF,DIV BATHYMETRY,NSTL,MS 39522 EPP D NATL SCI FDN,1800 G ST NW,WASHINGTON,DC 205502,Times Cited: 26 English Article R8582 NATUREISI:A1989R858200066eEschmeyer, W. N. 1969\VA systematic review of the scorpionfishes of the Atlantic Ocean (Pisces, Scorpaenidae)>7Occasional Papers of the California Academy of Sciences{79 1-142 Esteves, A. G. 198481Pesca da baleia nos Aores: uma resenha histricar*$Anais do Clube Militar Naval, Lisboa 114  1-3h 33-53 82Esteves, E. Simes, P. Silva, H. M. Andrade, J. P. 1995rAgeing of swordfish Xiphias gladius Linnaeus, 1788, from the Azores, using sagittae, anal-fin spines and vertebrae# Arquiplago"Life and Earth Sciences, 13A 39-51.'Biology; age; growth; fisheries biology 55-58$://A1991FV178000670>7Falkowski, P. G. Ziemann, D. Kolber, Z. Bienfang, P. K.aHARole of Eddy Pumping in Enhancing Primary Production in the Oceans NatureF?photosynthetic energy-conversion; pacific-ocean; fluxes; growthevoIN steady-state models of primary production in the open ocean, the upward fluxes of nutrients are balanced by the export of particulate production to the ocean depths. Export production represents the biological effect of carbon production on the net exchange of carbon dioxide between the atmosphere and the ocean. Geochemical estimates of exported production, based on calculations of rates of oxygen usage 1 or heat fluxes 2 are two to three times as high as those determined from biological measurements 3-5. One possible explanation for the differing estimates is that export production, calculated from independent geochemical signals, is too high. Another is that biological measurements severely undersample episodic nutrient injections into the photic zone 1,4. Eddy pumping represents one of the possible mechanisms of nutrient injection 1. Here we examine the enhancement of production by a cyclonic eddy in the subtropical Pacific with instrumentation that allows us to overcome the sampling problem. Our results reveal that eddy pumping markedly stimulates primary production, and that phytoplankton in the upper oligotrophic ocean outside the eddy are not growing near their maximum relative specific growth rates. But if the relative enhancement of production is typical, our results suggest that eddy pumping would enhance total primary production by only approximately 20%. Nature 1991 Jul 4 352 6330'BROOKHAVEN NATL LAB,DIV OCEANOG & ATMOSPHER SCI,UPTON,NY 11973 OCEAN INST,WAIMANALO,HI 96795 FALKOWSKI PG BROOKHAVEN NATL LAB,DIV OCEANOG & ATMOSPHER SCI,UPTON,NY 119732,Times Cited: 81 English Article FV178 NATUREISI:A1991FV17800067 Fasham, M.J.R. Foxton, P.l 1979Zonal distribution of pelagic decapoda (Crustacea) in the eastern North Atlantic and its relation to the physical oceanography.e82Journal of Experimental Marine Biology and Ecology37225-253 Feldmann, J. 1946*#La flore marine des les atlantides .'Mmoires de la Socit de Biogographiee28395-435s Fernandes, L. M. R. 1984*#Artes de Pesca Artesanal nos Aoresi  Horta, Aores5 2+Secretaria Regional da Agricultura e Pescase 150 pp Ferreira, E. 1937aEscombridas dos AoresAoreana I (4)a211-221sTMSystematics; diagnosis; anatomy; checklist; fisheries; scientific divulgationi Ferreira, E. 1938podos dos AoreseAoreanaII1 1-14 Ferreira, E. 1939Selceos dos AoresmAoreana II (2) 79-97 TMSystematics; diagnosis; anatomy; checklist; fisheries; scientific divulgationg Ferreira, E. 1939Selceos dos AoresAorenaII2 79-97\mbridas dos AoresAoreana I (4)a211-221sTMSystematics; diagnosis; anatomy; checklist; fisheries; scientific divulgationi Ferreira, E. 1938podos dos AoreseAoreanaII1 1-14 Ferreira, E. 1939Selceos dos AoresmAoreana II (2) 79-97 TMSystematics; diagnosis; anatomy; checklist; fisheries; scientific divulgationg Ferreira, E. 1939Selceos dos AoresAorenaII2 79-97\eographic affiliationdAoreana Supl.o173-192f"Bolten, A. B. Martins, H. R. 1990*$Kemp's ridley captured in the AzoresMarine Turtle Newsletter4823HBBolten, A. B. Martins, H. R. Bjorndal, K. A. Cocco, M. Gerosa, G. 1992h8Caretta caretta (loggerhead) pelagic movement and growthHerpetological Review23 116>8Bolten, A. B. Martins, H. R. Bjorndal, K. A. Gordon, J. 1993sSize distribution of pelagic-stage loggerhead sea turtles (Caretta caretta) in the waters around Azores and Madeira;J ArquiplagoLife and Marine Sciences 11A 49-54Borodin, N. A. 1931$North-Atlantic deep-sea fishesD=Bulletin of the Museum of Comparative Zoology, Havard Collegef 72(3)s 55-89ijcSystematics; diagnosis; Checklist; anatomy; meristics; morphometry; scientific expeditions; cruises  tnmFlkjiNO Bower, A. S. 2000hbWarm-water pathways in the Subpolar North Atlantic: An overview of the ACCE RAFOS float programme.WOCE Newsletter38 Boytsov, V.D 1984|vOceanological prerequisites of the approaches of arrow squid [Todarodes sagittatus] to the coasts of Norway and MurmanEcology of Biological Resources of the Northern Basin and their Commercial Exploitation. Collection of scientific papers of PINRO PINRO In Russian,English Summary Briggs, J. C. 1966<6Oceanic islands, endemism and marine paleotemperaturesSystematic Zoology 15 (2)153-163(F@Biogeography; zoogeography; marine geology; evolution; phylogeny Briggs, J. C.e 19702,A faunal history of the north Atlantic oceanSystematic Zoology 19(1)  19-34aF@Biogeography; zoogeography; marine geology; evolution; phylogeny Briggs, J. C.e 1974Marine Zoogeographye McGraw-Hill Book Company xi + 475pp Biogeography; zoogeography Brink, K.H. 19902+On the generation of seamount-trapped wavessDeep-Sea Research Part A37 1569-15821 Brito, A. 1983`Tres especies nuevas para la fauna ictiolgica de las Islas Canarias: Hoplostethus mediterraneus Cuvier, 1829, Sphoeroides cutaneus (Gnther, 1870) y Blennius pilicornis Cuvier, 1829 (Pisces: Teleostei)F`oVieraea12(1/2) 17-26NGGeographical distribution; new records; anatomy; meristics; morphometryBrum, J. M. M. 1992zNote on the presence of the great-white shark Chacharodon charcharias (Linnaeus, 1758) in the waters of So Miguel, Azores.EAoreana 7(3)517-521B;Geographical distribution; new record; anatomy; morphometry& Brum, J. M. M. Azevedo, J. M. N. 1995uFirst record of the Galapagos Shark Carcharinus galapagensis (Snodgrass & Heller, 1905) (Carcharinidae) on the Azoresv$<,%Boletin do Musea Municipal do Funchal Supl. No. 4139-143ZSSystematics; diagnosis; anatomy; morphometry; Geographical distribution; new record 1592-1604a$://000167224000007i\VBucklin, A. Astthorsson, O. S. Gislason, A. Allen, L. D. Smolenack, S. B. Wiebe, P. H.Population genetic variation of Calanus finmarchicus in Icelandic waters: preliminary evidence of genetic differences between Atlantic and Arctic populationsh$Ices Journal of Marine ScienceCalanus finmarchicus; dispersal; DNA sequence; Iceland; population genetics north-atlantic; nannocalanus-minor; possible impact; diversity; abundance; copepodLarge-scale circulation patterns in the North Atlantic may partition the ocean basin into three semi-distinct gyre systems: the Norwegian Sea, the northern North Atlantic, and the western North Atlantic. Zooplankton entrained in these gyres may be ecologically, reproductively, and (perhaps) genetically distinct owing to geographic isolation in different circulation systems and/or to isolation by distance. Previous studies have demonstrated that populations of the copepod Calanus finmarchicus in the eastern and western North Atlantic differ significantly in haplotype frequencies of the mitochondrial 16S rRNA. This study documents the results of our search for a more variable and easily assayed molecular population genetic character and provides preliminary evidence of population genetic structuring of C. finmarchicus across the boundary region between Atlantic and Arctic waters surrounding Iceland. The genetic traits used were DNA sequence variation and site-specific allele frequencies of a putative nuclear pseudogene of cytochrome oxidase I (COI), and non-coding (intron) and coding regions of the nuclear gene encoding phosphoglucose isomerase (PGI). All traits and both genes revealed significant population genetic differentiation among samples collected from the Northwest Atlantic, Norwegian Sea, North Sea, and Icelandic waters. All characters revealed significant differences among samples collected in Atlantic and Arctic waters surrounding Iceland. Molecular diversity of PGI and pseudo-COI may be useful in examining geographic partitioning of the C. finmarchicus populations on ecologically relevant time and space scales ranging from small-scale patches to ocean gyres. (C) 2000 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 2000 Dec576:3Times Cited: 1 English Article 406PH ICES J MAR SCIISI:000167224000007) 00337-348$://000078142700011s Johnsen, S. Widder, E. A.nngTransparency and visibility of gelatinous zooplankton from the Northwestern Atlantic and Gulf of MexicoBiological Bulletin:NHdeep-sea; underwater observations; selective predation; behavior; lensestnTransparency measurements (at 400 to 700 nm) were made on living specimens of 29 common species of gelatinous zooplankton from the Northwestern Atlantic Ocean and Gulf of Mexico. Percent transparency ranged from 91% for the hydromedusa Sibogota typa to 0.51% for the pteropod Clione limacina. Percent transparency was linearly and positively correlated with wavelength, with slopes of the regression lines (normalized to the percent transparency at 480 nm) ranging from 0.027%/nm for Sibogota typa to 0.51%/nm for the ctenophore Mnemiopsis macrydi (average 0.17 +/- 0.019%/nm). There was no significant correlation between the percent transparency of an animal and its daytime depth distribution. The relationship between percent transparency and sighting distance when viewed from below was modeled and showed that, due to the increase of the minimum contrast threshold for object detection at lower light levels, the usefulness of transparency as camouflage increases dramatically with depth. A preliminary account of these results was presented by the authors at the fourteenth meeting of the Ocean Optics Society in November 1998. Biol. Bull. 1998 Dec 1953' Harbor Branch Oceanog Inst Inc, Marine Sci Div, 5600 US 1 North, Ft Pierce, FL 34946 USA Harbor Branch Oceanog Inst Inc, Marine Sci Div, Ft Pierce, FL 34946 USA Johnsen S Harbor Branch Oceanog Inst Inc, Marine Sci Div, 5600 US 1 North, Ft Pierce, FL 34946 USA6/Times Cited: 10 English Article 158XL BIOL BULLISI:000078142700011717-730$://000168519900008 Johnsen, S. Widder, E. A.nxrUltraviolet absorption in transparent zooplankton and its implications for depth distribution and visual predationMarine Biologywave absorbing pigments; uv-b radiation; deep-sea; underwater observations; gelatinous zooplankton; marine-phytoplankton; selective predation; vertical migration; ozone depletion; mantis shrimppVOThe use of transparency as camouflage in the epipelagic realm is complicated by the presence of ultraviolet radiation, because the presence of UV-protective pigments decreases UV transparency and may reveal transparent zooplankton to predators and prey with UV vision. During July 1999, September 1999, and June 2000, transparency measurements (from 280 to 500 nm) were made on living specimens of 15 epipelagic (collection depth: 0-20 m, average: 11 +/- 1 m) and 19 mesopelagic (collection depth: 150-790 m, average: 370 +/- 40 m) species of transparent zooplankton from Oceanographer Canyon and Wilkinson Basin in the Northwest Atlantic Ocean. In addition, measurements of downwelling irradiance (from 330 to 500 nm) versus depth were made. The tissues from epipelagic zooplankton had lower UV transparency than those from mesopelagic zooplankton, while the average visible transparency (at 480 nm) of the two groups was not significantly different. Percent transparency was positively correlated with wavelength over most of the measured range, with a rapid decrease below a certain cutoff wavelength. In mesopelagic tissues, the cutoff wavelength was generally 300 nm. In epipelagic tissues, the cutoff wavelength was between 300 and 400 nm. Twelve out of 19 epipelagic tissues had transparencies at 320 nm that were half or less than their 480 nm transparency values, versus only 4 out of 21 mesopelagic tissues. The effects of UV absorption on UV visibility and minimum attainable depth were modeled using contrast theory and the physics of light attenuation. Because UV absorption was generally significantly greater in the UVB than in the UVA spectrum (where UV vision occurs), and because the highest UV absorption was often found in less transparent individuals, its modeled effects on visibility were slight compared to its effects on minimum attainable depth.d Mar. Biol. 2001 Apre 138p4 'Woods Hole Oceanog Inst, Dept Biol, MS 33, Woods Hole, MA 02543 USA Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA Harbor Branch Oceanog Inst Inc, Marine Sci Div, Ft Pierce, FL 34946 USA Johnsen S Woods Hole Oceanog Inst, Dept Biol, MS 33, Woods Hole, MA 02543 USA4-Times Cited: 2 English Article 429MA MAR BIOLISI:000168519900008r detritivores were similar among depths. Particles and microorganisms from the depths were also similar. This finding can be explained by the rapid sinking of particles and aggregates from surface waters and their relatively intact transit through the broad oxygen minimum with its reduced populations of zooplankton. The presence of algal cells in guts and vacuoles of benthic boundary-layer zooplankton suggests that these zooplankton select particles of recent surface origin for consumption. The presence of the guts filled with bacteria-like bodies shows that some deep-sea copepods and mysids that are normally generalist feeders can specialize opportunistically. The similarity of gut contents of crustaceans and vacuole contents or phaeodarians suggests that these two very different groups of particle feeders utilize similar food sources in the deep sea. Mar. Biol. 1992 Mar 1123'UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 95064 UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882 GOWING MM UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 950644.Times Cited: 30 English Article HJ522 MAR BIOLISI:A1992HJ52200013D=Granadeiro, J. P. Monteiro, L. R. Furness, R. W. Silva, M. C.l 1995z5The food of common terns Sterna hirundo in the Azoresw'PIAbstracts of papers presented at the 5th International Seabird Conference Glasgow 20-2124-26 March 1995Ecology; feedingsr8qp$b FE*#Christiansen, B Beckman,W Weikert,Hy 2001The structure and carbon demand of the bathyal benthic boundary layer community:a comparison of two oceanic locations in the NE AtlanticDeep-Sea Research part II 48 2409-2424CENTRAL NORTH PACIFIC, SANTA-CATALINA BASIN, DEEP-SEA, VERTICAL-DISTRIBUTION, EURYTHENES-GRYLLUS, NECROPHAGOUS AMPHIPOD, OXYGEN-CONSUMPTION, ZOOPLANKTON, BIOMASS, FOODaEstimates of standing stocks were used together with metabolic rates from literature to compare the structure and the respiratory carbon demand of the benthopelagic fauna and epibenthic megafauna at two oceanic locations in the northeast Atlantic. The total standing stock of the benthopelagic fauna and epibentic megafauna (in the following referred to as benthopelagos sensu latu) in the Iceland Basin (59 degreesN/20 degreesW) was 5 times higher than at the BIOTRANS site (West European Basin, 47 degreesN/20 degreesW). While fish were the predominating group at the northern location, followed by epibenthic megafauna, most of the biomass at the southern station could be attributed to epibenthic megafauna whereas fish were even surpassed by zooplankton. The overall respiratory carbon demand of the benthopelagos s.l. in the Iceland Basin was about 50% higher than at the BIOTRANS site. In both areas, a large fraction of the carbon was respired by the megafauna, accounting for 46 % of the total respiratory carbon demand in the Iceland Basin and 86% at the BIOTRANS site. Important consumers in the Iceland Basin were also zooplankton (27%) and fish (26%), whereas at the BIOTRANS site only zooplankton had a significant share (12%) besides megafauna. Compared to the carbon fluxes into the BBL, the faunal groups (without bacteria) remineralize ca. 10-20% of the sedimenting POC. If near-bottom pelagic bacteria are included, the fraction of the POC import flux remineralized by the benthopelagic community amounts to at least 20-50%. That means, the carbon flux as measured in sediment traps is not sufficient to fuel both the benthopelagic community including the megafauna plus the sediment community. (C) 2001 Elsevier Science Ltd. All rights reserved.o$CHUKSIN, Yu. V. V. A. SIROTIN. 1975RLDeep water fishery for grenadier by midwater trawl on the Mid-Atlantic Ridge$GU ZAPRYBA. Zaprybpromrazvedka 124 pp in Russian$CHUKSIN, Yu. V. V. A. SIROTIN. 1975^XPeculiarities of search and fishery for grenadier in the areas of the Mid-Atlantic Ridge 125 pp in Russian271-290$://A1988M353400006Clark, C. W. Levy, D. A.VPDiel Vertical Migrations by Juvenile Sockeye Salmon and the Antipredation WindowAmerican NaturalistAm. Nat. 1988 Febl 131 2N'UNIV BRITISH COLUMBIA,INST APPL MATH,VANCOUVER V6T 1Y4,BC,CANADA UNIV BRITISH COLUMBIA,WESTWATER RES CTR,VANCOUVER V6T 1W5,BC,CANADA CLARK CW UNIV BRITISH COLUMBIA,INST APPL MATH,VANCOUVER V6T 1Y4,BC,CANADA<6Times Cited: 133 English Article M3534 AMER NATURALISTISI:A1988M353400006 Clarke, R. 1954ZTOpen boat whaling in the Azores. The history and present methods of a relic industryDiscovery Reports- Cambridge University Press XXVI 281-354, plates XIII-XVIII Clarke, R. 1956 Sperm whales of the Azores Discoveryf28237-298f Clarke, R. 19810*Whales and dolphins and their exploitation@9Report of the International Whaling Commission (SC/32/01)131607-615\.(Clarke, M. R. Martins, H. R. Pascoe, P. 1993MThe diet of sperm whales (Physeter macrocephalus Linnaes 1758) off the Azores 1B7Clarke, M. R. Clarke, D. C. Martins, H. R. Silva, H. M. 1996AThe diet of the blue shark (Prionace glauca L.) in Azorean waters+ Arquiplago"Life and Marine Sciences 14A Ponta Delgada 41-56ISSN 0873-4704Cohen,R.E Lough,R.Gi 1983XRPrey field of larval herring clupea harengous on a continental shelf spawning area$Marine Ecology Progress Series10221-222 Collett, R. 1897HBOm en Samling Fiske fra Azoreme, tilhrende Museet i Ponta Delgada.(Archiv for Mathematik og Naturvidensksab 19(7) 1-17JDSystematics; Checklist; geographical distribution; museum collection Collett, R.  1897HBOm en Samling Fiske fra Azoreme, tilhorende Museet i Ponta Delgada.'Archiv fr Mathematik og Naturvidenskabd19 7 1-17 Collett, R.  19050*On some fishes from the sea off the Azores Zoologischen Anzeiger, Bd. XXVIII 21/22 723-730Collins, B. L. 1954*$Lista de peixes dos mares dos AoresAoreana II (5) 1-40.(Checklist; systematics; vernacular names$ Z197-212$://A1993KJ95100012d2+Dam, H. G. Miller, C. A. Jonasdottir, S. H.etmThe Trophic Role of Mesozooplankton at 47-Degrees-N, 20- Degrees-W During the North-Atlantic Bloom Experiment@9Deep-Sea Research Part Ii-Topical Studies in Oceanographyecontinuous plankton records; vertical nitrogen flux; calanus- finmarchicus; fecal pellets; feeding rates; temora-longicornis; marine z197-212$://A1993KJ95100012d2+Dam, H. G. Miller, C. A. Jonasdottir, S. H.etmThe Trophic Role of Mesozooplankton at 47-Degrees-N, 20- Degrees-W During the North-Atlantic Bloom Experiment@9Deep-Sea Research Part Ii-Topical Studies in Oceanographyecontinuous plankton records; vertical nitrogen flux; calanus- finmarchicus; fecal pellets; feeding rates; temora-longicornis; marine zooplankton; gut fluorescence; norwegian sea; spring bloombThe biomass and grazing rates of three size classes of mesozooplankton-0.2-0.5 mm (small), 0.5-1.0 mm (medium) and 1.0-2.0 mm (large)-were quantified in the vicinity of 47- degrees-N, 20-degrees-W, from 25 April to 7 May (leg 4) and from 18 to 31 May 1989 (leg 5) as part of the North Atlantic Bloom Experiment (NABE) of the Joint Global Ocean Flux Study (JGOFS). Biomass was inversely related to body size, with the small size fraction accounting for > 50% of the entire mesozooplankton biomass. Diel differences in biomass, however, were directly related to body size, indicating that vertical migration became more pronounced as the size of the animals increased. Total zooplankton biomass increased by almost a factor of 3 from the beginning to the end of the study. The average carbon-weight of individuals increased six-fold from leg 4 to leg 5 of the study. Carbon-specific rates of phytoplankton ingestion were (1) inversely related to body size; (2) greater at night for all size fractions; and (3) generally greater on leg 4 than on leg 5, particularly for the small size fraction. Grazing was dominated by the small size fraction (66% of the total grazing) on leg 4 and by the medium size fraction (44% of the total grazing) on leg 5. The removal of the daily primary production by mesozooplankton was not different from leg 4 to leg 5, averaging 2.7% day-1 (range 0.6- 5.2% day-1). Comparisons of (1) estimated metabolic rates and (2) measured nitrogen excretion rates with daily rations of carbon and nitrogen, respectively, for zooplankton suggest that a phytoplankton diet only contributed about 50% of the daily carbon and nitrogen rations of animals. We hypothesize that mesozooplankton fecal pellets contributed < 5% of the POC flux out of the euphotic zone measured with particle traps. However, we estimate that during leg 5, the active flux of dissolved nitrogen out of the euphotic zone due to mesozooplankton diel vertical migration was 26% of the passive PON flux.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 199340 1-2JCTimes Cited: 71 English Article KJ951 DEEP-SEA RES PT II-TOP ST OCEISI:A1993KJ95100012xonomia) e estudos sobre a histria da baleao nos Aores. , , ,4*$Relatrio de Estgio de Licenciatura  Ponta Delgada Universidade dos Aores 330 pp Gardner, D 1975HBObservations on the distribution of dissolved mercury in the ocean Marine Pollution Bulletino6  43-46r Girard, A. A. 1892:3Les Cphalopodes des les Aores et de l'le MadrerF@Journal de Sciencias Mathematicas, Physicas e Naturaes, 2 srie2-7i210-221f j69-105$://000086181200003D.'Haury, L. Fey, C. Newland, C. Genin, A.VJDZooplankton distribution around four eastern Nor 1815-+$://000072322200004rTNHarris, R. P. Boyd, P. Harbour, D. S. Head, R. N. Pingree, R. D. Pomroy, A. J.Physical, chemical and biological features of a cyclonic eddy in the region of 61 degrees 10'N 19 degrees 50'W in the North Atlantic<6Deep-Sea Research Part I-Oceanographic Research Paperscold-core eddy; emiliania-huxleyi; bloom experiment; inorganic carbon; spring bloom; southern bay; ocean; coccolithophore; bacterioplankton; zooplanktonThe second leg (CD61) of a two cruise investigation of coccolithophore biogeochemistry in the NE subarctic Atlantic provided the opportunity to make a detailed study of a cyclonic eddy in the vicinity of 61 degrees N 20 degrees W. The eddy held in the NE Atlantic is thought to be particularly important with regard to the physics of this region, and may influence the resulting chemical and biological properties of subarctic Atlantic waters. This eddy was ca. 50 km in diameter, moved at ca. 1.5 km d(-1) to the north of east, with a geostrophic circulation around the feature of ca. 25 cm s(-1) and probably extended as far as the ocean floor, where it may have interacted with the bottom topography. The horizontal salinity, nitrate and biological gradients between adjacent waters and the eddy were less marked in the present study than in a previous investigation of a cyclonic eddy in the vicinity of 48 degrees N 22 degrees W (Mittelstaedt, 1987), possibly due to the surface waters of the eddy mixing with surrounding waters. Satellite image sequences clearly link this feature with those studied in a mesoscale coccolithophore bloom studied in the same region on a previous cruise (CD60). Rates of primary production within the eddy were almost twice the mean values reported for Ocean Weather Station India (OWSI) at this time of year, but were similar to those noted during studies at the MLML site to the SE of the eddy location. Other biological rate measurements also indicated that the NE sub-polar Atlantic in mid-summer is more active than previously thought. Despite the extensive coccolithophore bloom studied immediately previously by CD60, there was no measurable coccolithophore calcification in the waters within the eddy in the present study. This is consistent with phytoplankton taxonomic data, which demonstrates that coccolithophore abundance was almost one hundred fold lower at this location on CD61 relative to CD60 and that lith and coccolithophore abundances were grestest in the water column beneath the mixed layer, suggesting sinking. These observations suggest that the decline of the bloom had occurred in the period between the two cruises. (C) 1998 Published by Elsevier Science Ltd. All rights reserved. .(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 Novn4411HBTimes Cited: 8 English Article ZA037 DEEP-SEA RES PT I-OCEANOG RESISI:000072322200004 6^ |F9 1628-1635 $://000167224000011ZTHeath, M. R. Fraser, J. G. Gislason, A. Hay, S. J. Jonasdottir, S. H. Richardson, K.LEWinter distribution of Calanus finmarchicus in the Northeast Atlantic$Ices Journal of Marine Sciencenet sampling; Norwegian sea; Optical Plankton Counter; vertical distribution; zooplankton vertical migration; zooplankton; copepod; sea; abundanceData from plankton sampling and Optical Plankton Counter deployments during six cruises between December of 1994 and 1999 have been used to derive a composite three-dimensional distribution of the abundance of Calanus finmarchicus during winter (December-January) in the Norwegian Sea and Northeast Atlantic. There are two centres of abundance, one in the eastern Norwegian Sea and Faroe-Shetland Channel, associated with the interface between Norwegian Sea Deep Water and Intermediate Water layers, and another in the Irminger Sea southwest of Iceland in association with Labrador Sea Water. In the open Northeast Atlantic, the concentration of wintering animals is around 30% of that in the Norwegian Sea and the vertical distribution is more diffuse and on average deeper. Modelling studies have shown that the overwinter distribution and transport are key factors determining the spatial persistence of C. finmarchicus but, apart from the data presented here, there is little knowledge of these large-scale properties.ICES J. Mar. Sci. 2000 Dec576'Dept Agr & Fisheries Scotland, Marine Lab, POB 101,Victoria Rd, Aberdeen AB11 9DB, Scotland Dept Agr & Fisheries Scotland, Marine Lab, Aberdeen AB11 9DB, Scotland Marine Res Inst, IS-121 Reykjavik, Iceland Danish Inst Fisheries & Marine Res, DK-2920 Charlottenlund, Denmark Univ Aarhus, Dept Marine Ecol, DK-8200 Aarhus, Denmark Heath MR Dept Agr & Fisheries Scotland, Marine Lab, POB 101,Victoria Rd, Aberdeen AB11 9DB, Scotland:3Times Cited: 3 English Article 406PH ICES J MAR SCIISI:000167224000011Heath,M.R Astthorsson,O.S Dunn,J Ellertsen,B Gaard,E Gislason,A Gurney, W.S.C Hind,A.T Irogoien,X melle,W Niehoff,B Olsen,K Skreslet,S Tande,K.S 2000haComparative analysis of Calanus Finmarchius demography at locations around the Northeast Atlantic$ICES Journal of Marine Science57 1562-1580\.'Henrich,R Baumann,K-H Huber,R Meggers,Hr 2002carbonate preservation records of the past 3 Myr in the norwegian-Greenland Sea and the northern North Atlantic: implications for the history of NADW productionMarine Biology 184 17-39 carbonate dissolution, deep-water formation, Norwegian-Greenland Sea, North Atlantic, Northern Hemisphere climate LATE CENOZOIC UPLIFT, TIME-SLICE RECORD, LAST 30,000 YEARS, DEEP-WATER, EARLY PLEISTOCENE, SOUTHERN ASIA, AMERICAN WEST, LATE PLIOCENE, SEDIMENTARY FACIES, INDIAN-OCEAN R KCarbonate preservation records from a number of drill sites in the North Atlantic and adjacent Norwegian-Greenland Sea (NGS) are used to reconstruct variations in North Atlantic Deep Water (NADW) production over the past 3 Myr. Before the initiation of major Northern Hemisphere glaciation, good carbonate preservation was recorded in the North Atlantic and the NGS supporting the superconveyor model of accelerated NADW formation in the late Pliocene. After the inception of main Northern Hemisphere glaciation, NADW formation in the NGS was blocked-off during the period 2.8-1.9 Ma. Carbonate was only badly preserved due to (1) low production of carbonate shells in surface waters, (2) sluggish renewal of deep waters induced by a rather stable sea-ice cover, and/or (3) production of carbonate-corrosive dense brines during sea-ice formation (e.g. sea ice dissolution mode). In contrast, contemporaneous good preservation in the adjacent North Atlantic indicates efficient NADW production. During the middle Matuyama (1.9-1.4 Ma), the first intrusions of the Proto-Norwegian Current into a narrow corridor in the southeastern NGS are evidenced by much better carbonate preservation. A decrease both in carbonate content and preservation towards the north and west of this corridor indicates the proximity of the polar front and gives evidence that NADW production was efficiently triggered by the Atlantic water entrainment mode. During the past 1.2 Myr carbonate preservation patterns in the NGS clearly reflect major global events like the Mid-Pleistocene Transition and the mid-Brunhes dissolution event. The onset of the Mid-Pleistocene Transition at 1.2 Ma is characterized by a complete shift to higher carbonate contents in the southeastern NGS and Labrador Sea. Overall, good preservation during both interglacials and glacials is only interrupted by high-frequency, short-term dissolution spikes, which were induced by ice sheet collapse and development of extensive meltwater lids. As a consequence, NADW was produced nearly continuously during glacials in the Nordic Seas. However, due to its lower density it was entrained into intermediate water levels in the North Atlantic and, thus, enforced the intermediate water circulation loop, whereas a decrease in lower-NADW production is observed contemporaneously. (C) 2002 Elsevier Science B.V. All rights reserved.N 44-66$://A1996TX86500002fHeptner, M. V.B://000173726200008<6Rocha, L. A. Bass, A. L. Robertson, D. R. Bowen, B. W.Adult habitat preferences, larval dispersal, and the comparative phylogeography of three Atlantic surgeonfishes (Teleostei : Acanthuridae)Molecular EcologytAcanthurus; biogeography; Brazil; Caribbean; central Atlantic islands; dispersal; reef fishes coral-reef fishes; mitochondrial-dna; patternsAlthough many reef fishes of the tropical Atlantic are widely distributed, there are large discontinuities that may strongly influence phylogeographical patterns. The freshwater outflow of the Amazon basin is recognized as a major barrier that produces a break between Brazilian and Caribbean faunas. The vast oceanic distances between Brazil and the mid-Atlantic ridge islands represent another formidable barrier. To assess the relative importance of these barriers, we compared a fragment of the mitochondrial DNA (mtDNA) cytochrome b gene among populations of three species of Atlantic surgeonfishes:Acanthurus bahianus, A. chirurgus and A. coeruleus. These species have similar life histories but different adult habitat preferences. The mtDNA data show no population structure between Brazil and the mid-Atlantic islands, indicating that this oceanic barrier is readily traversed by the pelagic larval stage of all three surgeonfishes, which spend similar to45-70 days in the pelagic environment. The Amazon is a strong barrier to dispersal of A. bahianus (d = 0.024, Phi(ST) = 0.724), a modest barrier for A. coeruleus (Phi(ST) = 0.356), and has no discernible effect as a barrier for A. chirurgus. The later species has been collected on soft bottoms with sponge habitats under the Amazon outflow, indicating that relaxed adult habitat requirements enable it to readily cross that barrier. A limited ability to use soft bottom habitats may also explain the low (but significant) population structure in A. coeruleus. In contrast, A. bahianus has not been collected over deep sponge bottoms, and rarely settles outside shallow reefs. Overall, adult habitat preferences seem to be the factor that differentiates phylogeographical patterns in these reef-associated species. Mol. Ecol. 2002 Feb112'jdUniv Florida, Dept Fisheries & Aquat Sci, 7922 NW 71st St, Gainesville, FL 32653 USA Univ Florida, Dept Fisheries & Aquat Sci, Gainesville, FL 32653 USA Univ S Florida, Dept Biol, Tampa, FL 33620 USA Smithsonian Trop Res Inst Panama, Unit 0948, APO, AA 34002 USA Rocha LA Univ Florida, Dept Fisheries & Aquat Sci, 7922 NW 71st St, Gainesville, FL 32653 USA4-Times Cited: 0 English Article 519KV MOL ECOLISI:000173726200008 Roden, G.I 1987PJEffect of seamount chains on ocean circulation and thermohaline structure. 60Keating, B.H. Fryer, P. Batiza, R Boehlert, G.W.Geophysical monograph 43  Washington DC American Geophysical Union335-354. Roe,H.S.J 1984lfThe diel migrations and distributions within a mesopelagic community in the NE Atlantic 4 the copepodsProgress in Oceanography13353-388s305-350 $://A1994BB98Q00005 Rogers, A. D.The Biology of Seamounts("Advances in Marine Biology, Vol 30 ACADEMIC PRESS LTDroughy hoplostethus-atlanticus; north pacific seamounts; deep- sea; orange roughy; genetic-variability; new-zealand; thermohaline structure; hydrothermal activity; uncharted seamount; mitochondrial-dna Advances in Marine Biology 199430*$Times Cited: 32 English Review BB98Q London'`ZROGERS AD MARINE BIOL ASSOC UNITED KINGDOM LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLANDISI:A1994BB98Q00005u r8$://000084501100007S Rogers, A. D.fVPThe role of the oceanic oxygen minim Rogers, A.D. 1994The biology of Seamounts Advances in Marine Biology30305-350\119-148$://000084501100007S Rogers, A. D.fVPThe role of the oceanic oxygen minima in generating biodiversity in the deep sea@9Deep-Sea Research Part Ii-Topical Studies in Oceanographyldh-b genotypes; species-diversity; community structure; benthic macrofauna; fundulus-heteroclitus; upwelling system; organic-matter; atlantic-ocean; pacific-ocean; arabian seazsMany studies on the deep-sea benthic biota have shown that the most species-rich areas lie on the continental margins between 500 and 2500 m, which coincides with the present oxygen-minimum in the world's oceans. Some species have adapted to hypoxic conditions in oxygen-minimum zones, and some can even fulfil all their energy requirements through anaerobic metabolism for at least short periods of time. It is, however, apparent that the geographic and vertical distribution of many species is restricted by the presence of oxygen-minimum zones. Historically, cycles of global warming and cooling have led to periods of expansion and contraction of oxygen-minimum layers throughout the world's oceans. Such shifts in the global distribution of oxygen-minimum zones have presented many opportunities for allopatric speciation in organisms inhabiting slope habitats associated with continental margins, oceanic islands and seamounts. On a smaller scale, oxygen-minimum zones can be seen today as providing a barrier to gene-flow between allopatric populations. Recent studies of the Arabian Sea and in other regions of upwelling also have shown that the presence of an oxygen-minimum layer creates a strong vertical gradient in physical and biological parameters. The reduced utilisation of the downward flux of organic material in the oxygen-minimum zone results in an abundant supply of food for organisms immediately below it. The occupation of this area by species exploiting abundant food supplies may lead to strong vertical gradients in selective pressures for optimal rates of growth, modes of reproduction and development and in other aspects of species biology. The presence of such strong selective gradients may have led to an increase in habitat specialisation in the lower reaches of oxygen-minimum zones and an increased rate of speciation. (C) 1999 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 200047 1-2'`ZUniv Southampton, Sch Ocean & Earth Sci, Southampton Oceanog Ctr, European Way, Southampton SO14 3ZH, Hants, England Univ Southampton, Sch Ocean & Earth Sci, Southampton Oceanog Ctr, Southampton SO14 3ZH, Hants, England Rogers AD Univ Southampton, Sch Ocean & Earth Sci, Southampton Oceanog Ctr, European Way, Southampton SO14 3ZH, Hants, EnglandHATimes Cited: 4 English Review 269WU DEEP-SEA RES PT II-TOP ST OCEISI:000084501100007MLg Kc 1995TNSeamount volcanism at the Reykjanes Ridge:relationship to the Iceland hot spot&Journal of Geophysical Research 1009B5 8449-8468TMMID-ATLANTIC RIDGE, EAST PACIF837-858$://A1996VL00300003i Dower, J. F. Mackas, D. L.JD''Seamount effects'' in the zooplankton community near Cobb Seamount<6Deep-Sea Research Part I-Oceanographic Research Paperslarge calanoid copepods; trapped waves; pacific-ocean; north pacific; isolated topography; flow; ordination; island; phytoplankton; rockfishes Oceanic seamounts often support large nektonic stocks. Since the mid-1950s it has been believed that this high productivity results, in part, from biological response to the physical interaction between oceanic currents and the abrupt topographic profiles represented by most seamounts. The ''classic theory'' for the production/maintenance of seamount nektonic stocks suggests that (i) the combination of localized upwelling and the trapping/concentrating action of closed anticyclonic vortices (i.e. Taylor cones) enhance local primary production, (ii) thereby promoting local secondary productivity that, (iii) supports local nektonic populations. Here we test one element of this theory: whether proximity to a shallow seamount is associated with changes in zooplankton abundance and species composition. Zooplankton samples were collected near Cobb Seamount, a shallow (<100 m) northeast Pacific seamount 50-km west of Vancouver Island. Both upwelling and closed recirculations occur at Cobb Seamount, but the latter is confined to depths >100 m and is not an effective retention mechanism. Total zooplankton abundance did not vary significantly on- versus off-seamount. However, using a variety of nonparametric multivariate techniques we demonstrate that a ''seamount effect'' on zooplankton-community composition is detectable up to 30 km from the seamount summit. This effect is superimposed on (and locally much stronger than) the expected slow decline in resemblance as between-sample geographic distance increases. Possible mechanisms by which this effect operates include: differential growth or reproduction, differential mortality and behavioral or migratory effects. The on-off seamount differences are accounted for largely by the increased relative abundances of two fast-growing opportunists, doliolids (Dolioletta sp.) and larvaceans (Oikopleura sp.), near Cobb Seamount. Predation pressure from seamount fish and active avoidance of the seamount by zooplankton may also play a role in generating the seamount effect. The absence of an effective trapping mechanism and the fact that total 2ooplankton abundance does not increase near the seamount lead us to conclude that the bottom-up model of localized energy transfer proposed under the ''classic hypothesis'' is incorrect for Cobb Seamount: nektonic stocks at Cobb Seamount (and, possibly, other shallow seamounts) are more likely supported by how-through (i.e. advected) rather than local production. Copyright (C) 1996 Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1996 Jun436'UNIV VICTORIA,DEPT BIOL,VICTORIA,BC V8W 2Y2,CANADA INST OCEAN SCI,SIDNEY,BC V8L 4B2,CANADA UNIV VICTORIA,DEPT BIOL,VICTORIA,BC V8W 2Y2,CANADAHBTimes Cited: 5 English Article VL003 DEEP-SEA RES PT I-OCEANOG RESISI:A1996VL00300003Dower, J.F. Mackas, L.D. 1996HA"Seamount effect" in the zooplankton community near Cobb SeamountsDeep-SEa Researchs436s837-85881DROBYSHEVA, S. S. B. V. KOLODNITSKY A. V. KOPTEV.u 1985F@Vertical structure of plankton communities of the North Atlantic6/ Complex studying of the Atlantic Ocean naturei Part II  77-78 in Russian81DROBYSHEVA, S. S. B. V. KOLODNITSKY A. V. KOPTEV.a 1986leInvestigation of a microstructure of vertical distribution of plankton by the underwater observationsa*$ Underwater fisheries investigations105-119  in Russian: ://A1992HA43700004C,%Gloeckler, G. Geiss, J. Balsiger, H. Bedini, P. Cain, J. C. Fischer, J. Fisk, L. 1727-1739o$://000167224000019 &Gislason, A. Astthorsson, O. S..ztWinter distribution, ontogenetic migration, and rates of egg production of Calanus finmarchicus southwest of Iceland$Ices Journal of Marine Scienceegg production; North Atlantic; overwintering; vertical distribution; zooplankton reproductive-biology; north-atlantic; marine copepod; water masses; st-lawrence; zooplankton; phytoplankton; fecundity; ecology; biomassnhThe winter distribution. seasonal vertical migration, and reproduction of Calanus finmarchicus in relation to water masses and chlorophyll tr were investigated southwest of Iceland between Nov ember 1996 and June 1997 as part of the TASC programme. During winter (November/December. January/February) overwintering C. finmarchicus were generally located beyond the shelf (5000-30000 individuals m(-2)); by contrast, overwintering animals were usually scarce on the banks (<800-2000 individuals m(-2)). In the Iceland Basin, overwintering C. finmarchicus resided mainly from 400 m depth to the bottom (>2000 m) at temperatures of similar to3-8 degreesC, whereas in the Irminger Basin the distribution was mainly similar to 200-1800 m in waters of similar to3-6 degreesC. During winter, most of the stock Ras present as C5 (84-86%), with a smaller proportion as C4 (12- 14%) and females (1-2%). Overwintering animals resided mainly in water of Atlantic origin, but some animals were found in Labrador Sea Water and Iceland-Scotland Ridge Overflow Water. Ascent to upper layers probably took place mainly during March and April, and continued until May. On the basis of the horizontal and vertical distribution of overwintering animals and the general surface current pattern, the banks seem to be repopulated mainly from the south. By April the spring growth of the phytoplankton was about to begin on the banks, and C. finmarchicus had started to lay eggs (0-7 eggs female(-1) d(- 1). Maximum individual rates of egg production (2-46 eggs female(-1) d(-1)) were observed in June. at the time of maximum phytoplankton biomass accumulation. During April, the population's average rate of egg production on the banks ( similar to 1000 eggs m(-2) d(-1)) was rather similar to that in the open ocean (similar to 600 eggs m(-2) d(-1)), whereas during June it was significantly higher in the oceanic region ( similar to 16 000 eggs m(-2) d(-1)) than in shelf waters (similar to 900 eggs m(-2) d(-1)), mainly because of the greater number of spawning females in the oceanic environment. (C) 2000 International Council For the Exploration of the Sea.ICES J. Mar. Sci. 2000 Dec576h'Inst Marine Res, POB 1390,Skolagata 4, IS-121 Reykjavik, Iceland Inst Marine Res, IS-121 Reykjavik, Iceland Gislason A Inst Marine Res, POB 1390,Skolagata 4, IS-121 Reykjavik, Iceland9:3Times Cited: 3 English Article 406PH ICES J MAR SCIISI:000167224000019A Gislason,A Astthorson,O.S 2000zsWinter distribution, ontogenetic migration, and rates of egg production of Calanus finmarchius southwest of Icelandu$ICES Journal of Marine Science57 1727-1739PJGislason,A Astthorsson, O.S Petursdottir,H Gudfinnson,H Bodvarsdottir, A.R 2000f_Life cycle of Calanus Finmarchicus south of iceland in relation to hydrography and chlorophyl ap$ICES Journal of Marine Science57 1619-1629.( POPOVA, M. N 1975PJOceanographic investigations in the area of the underwater Reykjanes Ridge Trudy PINRO 35  35-41 in Russian POPOVA, M. N 1977D>On circulation of waters in the area of the Mid-Atlantic Ridge<6 Problems of fisheries oceanography of the World Ocean 33-35 in Russian POPOVA, M. N 1978^XSome peculiarities of distribution of water masses in the area of the Mid-Atlantic Ridge Trudy PINRO40 94-98 in Russian$POPOVA, M. N L. G. BALABANOVAo 1979hbInter-seasonal variability of location of hydrological front in the area of the Mid-Atlantic Ridge<6 Problems of fisheries oceanography of the World Ocean 130-131 in Russian$POPOVA, M. N L. G. BALABANOVAp 1981ZSSome peculiarities of hydrological conditions of the area of the Mid-Atlantic RidgeeXR Oceanographic basis of formation of biological productivity of the North Atlantic 426-438 in Russian$Porteiro, F. M. Martins, H. R. 1992mFirst finding of natural laid eggs from Loligo forbesi Steenstrup, 1856 (Mollusca, Cephalopoda) in the Azores(6 ArquiplagoLife and Earth Sciences10119-120"Porteiro, F.M. H.R. Martins 1994Biology of Loligo forbesi Steenstrup, 1856 (Mollusc: Cephalopoda) in the Azores: sample composition and maturation of squid caught by jiggingr Fisheries Research21103-114Post, A F.-Tesch  1982pjMidwater trawl catches of adolescent and adult anguilliform fishes during Sargasso Sea Eel Expedition 1979& Helgolnder Meeresuntersuchungen35341-356Post, AE 1985~w Zur taxomnomie und verbreitung einiger Gonostomatidae und Photichthyidae (Osteichtheys, Stomiiformes) des Nordatlantik& Archiv fr Fischereiwissenschaft36 (1/2) 235-256Post, A J.-C. Quro  1991ZT Distribution et taxonomie des Howella (Perciformes, Percichthyidae) de lAtlantique Cybium 15 (2)111-128"Prud'homme van Reine, W. F.p 1988.'Phytogeography of seweeds of the Azores5Helgolnder Meersuntersr42165-1854-PSHENICHNY, B. P. A. N. KOTLYAR A. A. GLUKHOVO 1986<6Fish resources of the Atlantic Ocean thalassic bathyal2+ Biological resources of the Atlantic Ocean230-252 in RussianQuro, J. C. M. Duron  1980d]Sur la limite nord de laire de repartition dAntigonia capros (Pisces, Zeiformes, Caproidae)dD>Annalles de la Socit Science Naturelles de Charente-Maritime  6 (7)693-696 Ramalho, A 1929Beryx decadactylusleFaune Ichthyologique de lAtlantique Nord. Conseil Permanent pour lExploration de la Mer, Copenhaguel(!Cahiers 1-18 (cards not numbered)9"Ramos, J. A. del Nevo, A. J.in pressHBNest site selection by Roseate and Common terns in the Azores. Aukin press01VOCONVEX-91: water masses and circulation of the Northeast Atlantic subpolar gyreProgress in Oceanography484461-510Rees, W. J. White, E. 1966<6New records and fauna list of hydroids from the Azores,&Annals and Magazine of Natural History Ser. 13 9271-284 Regan, C. T. 19030)On a collection of fishes from the Azoresy,&Annals and Magazine of Natural History Ser. 79344-348 Regan, C. T 1925voNew ceratioid fishes from the north- Atlantic, the Caribean Sea and the Gulf of Canada, collected by the Danao,&Annals and Magazine of Natural HistorySer. 9, Vol. XV6561-567 Regan, C. T Trewavas, E. e 1929D=The fishes of the families Astronesthidae and ChauliodontidaerZSThe Danish Dana - Expedition 1920-22 in the North Atlantic and the Gulf of Panama No. 51-39 (+ 7 plates) Reiner, F. 19906/Record of marine mammals of the Azorean islandsn&Garcia da Orta, Srie Zoolgicae152r 21-360)Reiner, F. Gonalves, J. M. Santos, R. S.n 1993pjTwo new records of Ziphiidae (Cetacea) for the Azores with an updated checklist of cetacean species. . , , Arquiplago\Life and Marine Sciences 11A113-118 Rey, J. C. 198460 La pesca del pez Espada en el Atlntico Noreste2,Relatrio da IV Semana das Pescas dos Aores 4 113-117$Rey, J. C., E. Alot A. Ramos  1984\USynopsis biologica del Bonito Sarda sarda (Bloch), del Mediterraneo y Atlantico Oeste0)ICCAT, Recueil de Documents Scientifiques 20 (2)469-502TMRibera Maycas, E. Bourdillon, A. Macquart-Molin, C. Passelaigue, F Patriti, G 1999tmDiel Variations of the bathymetric distributio of zooplankton groups and biomass in Cap-Ferret Canyon, FranceDeep-Sea Research II46 2081-2099n*#Rice, A.L. Thurson, M.H. Bett, B.J. 1994The IOSDL DEEPSEAS Programme: introduction and photographic evidence for the presence and absence of a seasonal input of phytodetritus at contrasting abyssal sites in the north-eastern Atlantic.Deep-Sea Research I41 1305-1320  Richard, J. 1910LFLes campagnes scientifiques de S. A. S. le Prince Albert Ier de Monaco<5Exposition Universelle de 1900, Principaut du Monaco9 Imprimerie du Monaco 140 pp Richard, J 1934tmListe gnrale des stations des campagnes scientifiques du Prince Albert de Monaco avec notes et observationszsRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverain du Monaco, Fascicules LXXXIX 1-348  Richard, J.s 1936lfDocuments sur les Ctacs et Pinnipids Provenant des Campagnes du Prince Albert Ier Prince de Monaco.~wRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverin du Monaco, Fascicule XCIV Imprimerie du Monaco 72 ppMMMrrrr|}XXXX~~~sasQ''..ww%%xKz]]]{{{{LLLLLLL888CChhhh^^^^^qqqqqqqMMMMMMMXXXXRRR~~~aQQQQQ''wwwww]]!Io33+CCCCCCChqqqqqqqqqqq~=?4B bC219-224$://A1992KG43200005&Gislason, A. Astthorsson, O. S.RLZooplankton Collected by Sediment Trap Moored in Deep-Water South of Iceland Sarsia>8euthecosomatous pteropods; norwegian sea; flux; swimmersThe seasonal abundance of deep-water zooplankton occurring in a sediment trap moored at 600 m depth south of Iceland was studied from integrated monthly samples during the period November 1986-September 1989. Copepods, ostracods and pteropods usually made up 70-90 % of the animals in the samples. A total of 73 species and other taxa were found in the trap material of which the four most abundant ones were, in declining order of abundance, Limacina retroversa (FLEMMING) which showed peak abundance in January-February, Conchoecia borealis G.O. SARS which reached maximum abundance in July-September, Euchaeta norvegica BOECK with maxima in March or June-July and Calanus finmarchicus (GUNNERUS) which showed maximum numbers in February-March. The following 12 species, which occurred in the sediment trap, are reported as new for Iceland: Nausithoe globifera BROCH (Scyphomedusae); Conchoecia lophura MULLER, C. elegans G.O. SARS, C. ametra MULLER (Ostracoda); Spinocalanus magnus WOLFENDEN, Aetideopsis multiserrata (WOLFENDEN), Candacia elongata (BOECK) (Copepoda); Eurycope murrayi WALKER (Isopoda); Cyphocaris anonyx BOECK, Scina borealis (G.O. SARS), S. tullbergi (BOVALLIUS) (Amphipoda) and Gennadas elegans (SMITH) (Natantia). Sarsia 199277 3-4'MARINE RES INST,SKULAGATA 4,POB 1390,121 REYKJAVIK,ICELAND GISLASON A MARINE RES INST,SKULAGATA 4,POB 1390,121 REYKJAVIK,ICELAND2+Times Cited: 5 English Article KG432 SARSIAISI:A1992KG43200005"Gislason, A Astthorson, O.St 1992RLZooplankton collected by sediment trap moored in deep water south of iceland Sarsia77219-224e 1959-1976r$://A1995TD91600007&Gislason, A. Astthorsson, O. S.82Seasonal Cycle of Zooplankton Southwest of Iceland"Journal of Plankton ResearchZToregon upwelling zone; populations; plankton; calanus; pseudocalanus; migration; sea81Seasonal variations in biomass, abundance and species composition of zooplankton in relation to environmental parameters and chlorophyll a were studied in both the Coastal water [salinity (S) < 35.0 parts per thousand] and the Atlantic water (S > 35.0 parts per thousand) southwest of Iceland. The sampling was carried out at approximately monthly intervals from February to November 1991. The mean temperature of the upper 50m of the water column varied greatly during the year. Lowest temperatures were recorded in March-April (5-7 degrees C) and the highest in July-August (11-12 degrees C). The spring bloom of the phytoplankton probably occurred earlier in the Coastal water (early May) than in the Atlantic water (mid-to late May) and in neither water mass was there an autumn peak in the standing stock of chlorophyll alpha. The seasonal variations in both biomass and abundance of total zooplankton followed more or less those of the most abundant zooplankters, and were characterized by a seasonal low during the winter and two maxima during the summer (May-June) and early autumn (July- September). In the Coastal water, Calanus finmarchicus was the most abundant species (similar to 33% of the total zooplankton), followed by Temora longicornis (similar to 27%), Evadne nordmanni (similar to 17%), Podon leuckarti (similar to 8%) and Pseudocalanus spp. (similar to 6%). On the other hand, in the Atlantic water the plankton were completely dominated by C. fumarchicus (similar to 92%), while euphausiid eggs and larvae ranked second (similar to 3%) and third (similar to 2%), respectively. The annual mean dry weight biomass was about one and a half times greater in the Coastal water (similar to 6 g m(-2)) than in the Atlantic water (similar to 4 g m(-2)). Further, the annual mean abundance was approximately four times higher in the Coastal water (similar to 120 000 individuals m(- 2)) compared to the Atlantic water (similar to 32 000 individuals m(-2)). This is presumably reflecting the higher production of the zooplankton community in Coastal water compared to Atlantic water.J. Plankton Res. 1995 Oct1710'MARINE RES INST,SKULAGATA 4,POB 1390,IS-121 REYKJAVIK,ICELAND GISLASON A MARINE RES INST,SKULAGATA 4,POB 1390,IS-121 REYKJAVIK,ICELAND:4Times Cited: 10 English Article TD916 J PLANKTON RESISI:A1995TD91600007 71-84$://A1996UP52100006&Gislason, A. Astthorsson, O. S.leSeasonal development of Calanus finmarchicus along an inshore- offshore gradient southwest of IcelandOphelia-zooplankton community>7The abundance and development of the copepod Calanus finmarchichus southwest of Iceland was studied in relation to phytoplankton biomass at three stations along a hydrographic gradient during the period February-November 1991. Following increasing stratification nearshore during April, the phytoplankton spring bloom began in the shallow area and culminated in April-May. At greater distances from the shore the stratification did not start until the middle of May and consequently the blooming began later in the deep offshore areas, probably culminating during mid to late May. The number of Calanus finmarchicus was low during the winter months and peaked twice during the summer at all three stations (May-June and July-September), reflecting the two generations of C. finmarchicus which grew up in both shallow and deep water southwest of Iceland. In both waters the spawning of the overwintered generation appeared to begin before the observed phytoplankton spring bloom. However, peak spawning of the overwintered generation approximately coincided with the phytoplankton spring bloom, while also occurring earlier nearshore (April) than farther out from the shore (May). At all three stations there was a second generation of C. finmarchicus which also hatched earlier nearshore (June) than more distant from land (June-July).Ophelia 1996 Apr44 1-3'MARINE RES INST,SKULAGATA 4,POB 1390,REYKJAVIK 121,ICELAND Gislason A MARINE RES INST,SKULAGATA 4,POB 1390,REYKJAVIK 121,ICELAND4-Times Cited: 14 English Article UP521 OPHELIAJISI:A1996UP52100006e811-813$://000076754200030&Gislason, A. Astthorsson, O. S.d]Variability in the population structure of Calanus finmarchicus in Icelandic waters in spring$Ices Journal of Marine ScienceB;Calanus finmarchicus; Icelandic waters; spatial variability0*Since 1961, long-term monitoring of zooplankton has been carried out during spring (May-June) on standard sections around Iceland. An analysis of the onshore-offshore variability in the population structure of Calanus finmarchinus during this time of the year indicates that off the east, south, and west coasts of Iceland reproduction is highest over the banks, while off the Vestirdir Peninsula breeding activities appear to be largely confined to the frontal area between the Atlantic Water close to the land and the cold Polar Water farther out. In the deep waters north-east of Iceland, where the Arctic influence is generally greatest, the percentage of juvenile stages is very low, suggesting little reproduction in these cold water masses. (C) 1998 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 1998 Aug554'Marine Res Inst, Skulagata 4,POB 1390, IS-121 Reykjavik, Iceland Marine Res Inst, IS-121 Reykjavik, Iceland Gislason A Marine Res Inst, Skulagata 4,POB 1390, IS-121 Reykjavik, Iceland:3Times Cited: 2 English Article 134QN ICES J MAR SCIISI:000076754200030@> 66-70$://A1996UC56700010JCVinogradov, M. E. Shushkina, E. A. Vereshchaka, A. L. Nezlin, N. P.bXROn migrations of Calanus finmarchicus sl during the polar day in the Norwegian Sea OkeanologiyajcDetailed observations of diurnal variations of vertical distribution of V and VI Calanus finmarchicus VI copepodites in the upper mixed layer were carried out luring the polar day. The materials were collected on 5 - 15 July 1994 in the single point in the North-Eastern Norwegian Sea (73 degrees 45'N, 13 degrees 30'E). The angle of sun at midnight was 06 degrees 18'. 150-litre bottles were used for sampling, the samples were obtained with 5 m vertical intervals. The series of samples during night hours were collected every 1 - 2 hours. The distribution of the V and VI copepodites appeared to be of a similar type. They formed the layer of high concentration 5 - 15 m thick, where the abundance exceeded 1000, and sometimes 2000 sp/m(3). This layer performed regular diurnal movements, rising before the midnight (22.00) towards surface and descending during the daytime to a depth of 20 - 30 m. The residence time for Calanus in the upper 5-meters layer did not exceed 1 - 2 hours. The rate of illumination changes rather than the absolute value of illumination is belived to be the main stimulator of the movements. Okeanologiya 1996Jan-Feb361'b[PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA Vinogradov ME PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIAe81Times Cited: 3 Russian Article UC567 OKEANOLOGIYAuISI:A1996UC56700010y\UVinogradov, G. M. Vereshchaka, A. L. Shushkina, E. A. Arnautov, G. N. Dyakonov, V. Y.e 1997Vertical distribution of zooplankton above the Broken Spur hydrothermal field in the North-Atlantic Gyre (20 degrees N, 43 degrees W) Okeanologiya374559-570Jul-Aug OkeanologiyaISI:A1997XV83000013tmscattering layer; deep-sea; insitu rates; black-sea; ridge; plume; communities; ocean; vent; macrozooplanktonIn August-September 1996, an expedition on board R/V ''Akademik Mstislav Keldysh'' with two deep-sea manned submersibles ''Mir- 1'' and ''Mir-2'' investigated the vertical distribution of zooplankton above the Broken Spur hydrothermal field in the oligotrophic waters of the North-Atlantic Gyre, Plankton in the water column was sampled with plankton nets, big water bottles (volume 150-1801) and was directly observed and sampled with slurp-gun from the submersibles. The near-bottom (tens and hundreds meteres) layers of water were investigated with significant detailing. No influence of the hydrotherm on the communities in the water column was found, except that some aggregation of planktonic gelatinous animals was found along the borders of hydrothermal plume waters, But in the nearest vicinities of ''black smokers'' (first hundreds of metres) common planktonic animals were replaced by the ones associated with the hydrothermal field (Dirivultidae copepods, shrimps eggs and larvae, etc.). Thus, the hydrothermal community should be regarded as 3-dimensional (''with planktonic hemisphere''), although quasi-closed (with very local influence upon background ecosystems).81Times Cited: 5 Russian Article XV830 OKEANOLOGIYAE$://A1997XV83000013 &a`_^ Ferreira, E. 1940F?A pesca da "Albacora" em 1938 e 1939 e "Pediculados" nos AoresAoreana II (3)129-134i(!Scientific divulgation; fisheries Ferreira, E. 1942,%Peixes luminosos dos mares dos AoresgAoreanaIII (1) [1942-1945]e 6-16(!Checklist; scientific divulgationa FILIN, A. A. 1989NGSome data on distribution of young Notoscopelus kroeyerii (Myctophidae)Voprosy ikhtiologiit  29(6) 1035-1037) in Russian FILIN, A. A  1995\VPeculiarities of feeding and trophic relations of Notoscopelus kroeyerii (Myctophidae)Voprosy ikhtiologiip  35(5)635-641( in Russian FILIN, A. A. 1997PJGrowth and length-age composition of Notoscopelus kroeyerii (Myctophidae)Voprosy ikhtiologiir 37(1)o 33-38) in RussianFilippova, Ju.AY 1973("Distribution and biology of squidsItogi Nauki i Tekhniki$ Zoologiya Bespozvonochnykh, 2 60-101 In RussianFilippova, Ju.Ai 19792+Resources of cephalopods in the World Oceant.'Biological Resources of the World Oceana195-201e In RussianaFilippova, Ju.Ae 1987HBState of the recent squid fishery and prospects of its developmentRK Resources and Perspectives of the Exploitation of Squid in the World Oceanl  VNIRO  4-12 &In English with Russian summaryD=Filippova, Ju.A., Alekseev, D.O., Bizikov, V.A. Khromov, D.N.r 199782Commercial and Mass Cephalopods of the World Ocean 272 pages In RussianFINENKO, Z. Z. 1985pjPrimary production in the areas of rising of the oceanic bottom in the northern part of the Atlantic OceanD= Biological basis of fisheries in the open areas of the ocean184-191  in Russian4*$Fleming, S Furness, R.W. Davies, I.M 2000voContemporary patterns and historical rates of increase of mercury contamination in different marine food chainss:3ICES Annual Science Conference (ICES CM 2000/S:02).)-xo0DBURUKOVSKY, R. N.m 19932+Biology of shrimp Parapasiphae sulcatifronstBiologiya morayR3  45-52 in Russian Bhring,S.I Christiansen,B 2001TNLipids in selected abyssal benthopelagic animals: links to the epipelagic zoneProgress in Oceanography50369-382oCapello, F. de B.s 1871actmPrimeira lista dos peixes da Ilha da Madeira, Aores e das possesses d'Africa que existem no museu de Lisboae:4Jornal de Sciencias Mathematicas Physicas e NaturaesTomo IIINum. XI - Maro de 1871}194-202"Museum collections; catalogs Chaves, A. F. 1924.( Cetceos que aparecem no mar dos AoresA Pesca Martima15 41-44eChavigny, J. Mayaud, N.o 1932B://000083234700003m<5Christiansen, B. Druke, B. Koppelmann, R. Weikert, H.0ztThe near-bottom zooplankton at the abyssal BIOTRANS site, northeast Atlantic: composition, abundance and variability"Journal of Plankton Researchbenthic boundary-layer; central red-sea; cold-core eddy; deep- sea; benthopelagic plankton; vertical-distribution; epibenthic sledge; open ocean; mid-water; communityZSThe near-bottom zooplankton of the abyssal BIOTRANS site (water depth 4500 m) was studied at two stations 11 nautical miles (nm) apart. Stratified sampling was conducted by means of a double MOCNESS at three depth layers 20, 50 and 100 m above bottom. The composition of the zooplankton showed a predominance of copepods, making up >50% of the total zooplankton abundance. Ostracods and chaetognaths were the most important non-copepods, displaying a slight increase towards the bottom. The variability of abundance and biomass was analysed statistically at different scales. Logarithmic coefficients of variation ranged from 29 to 187% for various taxa. Sampling at the two stations added significantly to the total variance for some taxa. By contrast, vertical gradients were mostly weak. Possible reasons for the observed variability are discussed.J. Plankton Res. 1999 Oct2110' Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, Zeiseweg 9, D-22765 Hamburg, Germany Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, D-22765 Hamburg, Germany Christiansen B Univ Hamburg, Inst Hydrobiol & Fischereiwissensch, Zeiseweg 9, D-22765 Hamburg, Germany:3Times Cited: 3 English Article 247RX J PLANKTON RESISI:00008323470000360Christiansen, B Drke,B Koppelmann, R Weikert, H 1999rlThe near-bottom zooplankton at the abyssal BIOTRANS site, NE Atlantic:composition, abundance and variability"Journal of Plankton Research21 (10) 1847-1863BENTHIC BOUNDARY-LAYER, CENTRAL RED-SEA, COLD-CORE EDDY, DEEP-SEA, BENTHOPELAGIC PLANKTON, VERTICAL-DISTRIBUTION, EPIBENTHIC SLEDGE, OPEN OCEAN, MID-WATER, COMMUNITYXRThe near-bottom zooplankton of the abyssal BIOTRANS site (water depth 4500 m) was studied at two stations 11 nautical miles (nm) apart. Stratified sampling was conducted by means of a double MOCNESS at three depth layers 20, 50 and 100 m above bottom. The composition of the zooplankton showed a predominance of copepods, making up >50% of the total zooplankton abundance. Ostracods and chaetognaths were the most important non-copepods, displaying a slight increase towards the bottom. The variability of abundance and biomass was analysed statistically at different scales. Logarithmic coefficients of variation ranged from 29 to 187% for various taxa. Sampling at the two stations added significantly to the total variance for some taxa. By contrast, vertical gradients were mostly weak. Possible reasons for the observed variability are discussed( -,8+*)(* Santos, R. S.i 1992Proteco e conservao do meio marinho nos Aores. in Saldanha, L., R, P. and Martins, A. F. (Eds.). Centenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L'Hirondelle. , ,Aoreana Supl.107-1220)Santos, R. S. P. R A. F. Martins (Eds.) 1992Proteco e conservao do meio marinho nos Aores. Centenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L Hirondelle. Aoreana (Suplemento 1992)107-122m2+Santos, R. S. Nash, R. D. M. Hawkins, S. J.M 1994JDFish assemblages on intertidal shores on the island of Faial, Azores ArquiplagoaLife and Marine Sciences 12A  87-100 Santos, R. S.i 1995,&Allopaternal care in the redlip blennyJournal of Fish Biologyo47in press 4pp "Santos, R. S. Nash, R. D. M. 1995TMSeasonal changes in a sandy beach fish assemblage at Porto Pim, Faial, Azorest*$Estuarine, Coastal and Shelf Science41in press 13pp2+Santos, R. S. Nash, R. D. M. Hawkins, S. J.i 1995bAge, growth and sex ratio of the Azorean rock-pool blenny, Parablennius sanguinolentus parvicornis;HBJournal of the Marine Biological Association of the United Kingdom75in press 4ppB;Santos, R. S. Porteiro, F. M. Barreiros, J. P. Silva, H. M.nin pressJDMarine fishes of the Azores: An annotated checklist and bibliography Arquiplagou,%Life and Marine Sciences (supplement)SAPRONETSKAYA, N. G  1989B8Transactions of the P. P. Sirskov Institut of Oceanololy 104a 26-72. $(in Russian, English summary)S,%Schiebel,R Waniek,J Zeltner,A Alves,M 2000xrImpact of the Azores front on the distribution of planktic foraminifers, shelled gastropods, and coccolithophoridsDeep-Sea Researchpart IIV 1-16 Schmidt, J 19184-Argentinidae, Microstomidae, Opisthoproctidaea Mediterranean Odontostomidae Report of the Dana Oceanographical Expeditions 1908-1910 to the Mediterranean and Adjacent Seas Vol. II. Biology, A.  5. 1-40,&(with 23 figures and 4 charts in text) Schmidt, J 1921HB New studies of Sun-fishes made during the Dana Expedition, 1920 Nature 107 no. 2681 76-79 Schmidt, J 1921XQContributions to the knowledge of the young of the sun-fishes (Mola and Ranzania)tJC Meddlelelser fra Kommissionen for Havunders-gelser, Serie Fiskeril VI (6)16 Schmidt, J 1926PI Further studies of Sun-fishes made during the Dana Expedition, 1921-19223 Nature0 117 No. 2933 80-81rion Candidate of Biological Sciences [cited above] 26 p.  In Russian*$Monaco, S. A. S. le Prince Albert de 1905.'Sur la campagne de la "Princesse-Alice"2+Bulletin du Muse Ocanographique de Monacot39 1-5&Monteiro, L. R. Furness, R. W.s (unpubl.)opSpeciation through temporal segregation of Madeiran storm petrel (Oceanodroma castro) populations in the Azores?BT(unpublished manuscript)ographers themselves make their output more accessible and user-friendly for non-scientists, and take advantage of the new technologies which promise to re-vitalise the field.Prog. Oceanogr. 199434 2-3'UNIV CALIF SANTA BARBARA,INST MARINE SCI,SANTA BARBARA,CA 93106 INST OCEANOG SCI,DEACON LAB,GODALMING GU8 5UB,SURREY,ENGLAND KRAUSE DC UNIV CALIF SANTA BARBARA,INST MARINE SCI,SANTA BARBARA,CA 9310681Times Cited: 1 English Review QB204 PROG OCEANOGRISI:A1994QB20400010 .b*n  29-49$://A1993KY29500002&Schmitz, W. J. McCartney, M. S.(!On the North-Atlantic CirculationReviews of Geophysicsantarctic intermediate water; western boundary current; gulf- stream; sverdrup transports; norwegian-greenland; wind stress; ocean; abaco; east; heatn|A new, speculative, and, we hope, provocative summary of the North Atlantic circulation is described, including both horizontal currents (wind-driven) and the primarily (thermohaline) meridional flows that involve the transformation of warm to cold water at high latitudes. Our picture is based on a synthesis of a variety of independent investigations that are contained in the literature as opposed to a presentation of the results of one technique or the point of view of one author. We describe a thermohaline cell (the so-called thermohaline conveyor belt) that is concentrated within the Atlantic and Southern oceans (rather than essentially global), with the most important upwelling sites being in the circumpolar and the equatorial current regimes. We concentrate on deep water formation and its replacement relative to intermediate-water formation. It has been pointed out recently that the formation of 13 Sv (1 Sv = 10(6) m3 s-1) of southward flowing North Atlantic Deep Water is compensated for in the upper ocean by northward cross-equatorial transport. We suggest that this thermocline layer flow passes through the Straits of Florida. transits the Gulf Stream system on its inshore side, and exits through the North Atlantic Current system after recirculation and modification. There is now a clear observational basis for the structure of recirculating gyres on the southern and northern sides of the Gulf Stream. We suggest a recirculation for the North Atlantic Current as well. We also describe a C-shaped component to the southern Gulf Stream recirculation and identify a roughly 10-Sv circulation in the eastern North Atlantic associated with the Azores Current. Recirculations play an important role in deep boundary current regimes and in water mass formation and modification. The transport of the deep western and northern boundary currents in the North Atlantic Ocean may be boosted (roughly doubled or tripled) by counter-clockwise recirculating gyres and by additions of modified bottom or intermediate water. While the North Atlantic is the most completely observed ocean, there are still significant gaps in our knowledge of its circulation. Rev. Geophys. 1993 Feb311'zWOODS HOLE OCEANOG INST,CLARK LAB 3,WOODS HOLE,MA 02543 SCHMITZ WJ WOODS HOLE OCEANOG INST,CLARK LAB 3,WOODS HOLE,MA 0254381Times Cited: 218 English Review KY295 REV GEOPHYSISI:A1993KY29500002Schroeder, W. C 19402,Some deep sea fishes from the North Atlantic Copeia231-238 Schults, K. Beckmann, W 1995TNNew benthopelagic Tharybdis (Copepoda: Calanoida) from the deep north Atalntic Sarsia80199-211l199-211$://A1995TT71000005SSchulz, K. Beckmann, W.0TNNew benthopelagic tharybids (Copepoda: Calanoida) from the deep North Atlantic Sarsia"zooplankton; community; seaA new genus is proposed to accommodate Rythabis atlantica gen. et sp. n., collected by means of a MOCNESS opening-closing net from 2840 m depth ca 20 m above the seabed in the North Atlantic south of Iceland. The new genus is placed in the family Tharybidae and appears to be closely related to Tharybis, but differs in several characters of prosome, urosome and appendages. In addition, two members of the genus Tharybis, T. angularis sp. n. and T. crenata sp. n., are described and illustrated from the same plankton haul on the basis of adult females. Xanthocalamus groenlandicus TUPITZKY, 1982 is transferred to Tharybis; this brings the number of species attributable to the genus to 13. Sarsia 1995803n2+Times Cited: 5 English Article TT710 SARSIAtISI:A1995TT71000005s.'Schut,E.W Uenzelmann-Neben,G Gersonde,Rr 2002HASeismic evidence for bottom current activity at the Agulhas Ridge "Global and Planetary Changel 721l 1-14Sedberry, G. R 1995ngAspects of the biology and management of wreckfish, Polyprion americanus, in the western north Atlantic4.Relatrio da XIII Semana das Pescas dos Aores 13 (1994)105-116:3Sedberry, G. R. J. L. Carlin R. W. Chapman B. Elebyc 1996Population structure in the pan-oceanic wreckfish, Polyprion americanus (Teleostei: Polyprionidae) as indicated by mtDNA variationJournal of Fish Biology49 (Supplement A)A318-3292B;SENNIKOV, A. M B. P. SHIMKO S. G. MUKHIN T. E. BLIZNICHENKOe 1986rlBiology and distribution of winter spawning group of squid (Todarodes sagittatus) in the North-East AtlanticNH Resources and perspectives of exploitation of squids of the World Ocean  29-37 in RussianB;Sennikov, A.M. Shimko, V.P. Mukhin, S.G. Bliznichenko, T.E,q 1987yBiology and distribution of the winter-spawning grouping of arrow squid Todarodes sagittatus in the northeastern Atlanticib[ Resources and Perspectives of the Exploitation of Squid in the World Ocean. Ed. B.G.Ivanovt 29-37 &In English with Russian summarySEREBROV, L. I 1974jdStudying of behaviour of polar cod and roundnose grenadier with the use of the on-trawl photo cameraRybnoe khozyaistvo  11  6-8s in RussianSEREBROV, L. I 19762,Dependence of schools density on fish sizesVoprosy ikhtiologiiS 16[1(96)]S152-157) in Russian Serpa, J. de 1886. 4-A Industria Piscatoria nas Ilhas Fayal e PiconOpusculos Aorianos, IImprensa AcademicaCoimbrai 1-18 &a`_^ Ferreira, E. 1940F?A pesca da "Albacora" em 1938 e 1939 e "Pediculados" nos AoresAoreana II (3)129-134i(!Scientific divulgation; fisheries Ferreira, E. 1942,%Peixes luminosos dos mares dos AoresgAoreanaIII (1) [1942-1945]e 6-16(!Checklist; scientific divulgationa FILIN, A. A. 1989NGSome data on distribution of young Notoscopelus kroeyerii (Myctophidae)Voprosy ikhtiologiit  29(6) 1035-1037) in Russian FILIN, A. A  1995\VPeculiarities of feeding and trophic relations of Notoscopelus kroeyerii (Myctophidae)Voprosy ikhtiologiip  35(5)635-641( in Russian FILIN, A. A. 1997PJGrowth and length-age composition of Notoscopelus kroeyerii (Myctophidae)Voprosy ikhtiologiir 37(1)o 33-38) in RussianFilippova, Ju.AY 1973("Distribution and biology of squidsItogi Nauki i Tekhniki$ Zoologiya Bespozvonochnykh, 2 60-101 In RussianFilippova, Ju.Ai 19792+Resources of cephalopods in the World Oceant.'Biological Resources of the World Oceana195-201e In RussianaFilippova, Ju.Ae 1987HBState of the recent squid fishery and prospects of its developmentRK Resources and Perspectives of the Exploitation of Squid in the World Oceanl  VNIRO  4-12 &In English with Russian summaryD=Filippova, Ju.A., Alekseev, D.O., Bizikov, V.A. Khromov, D.N.r 199782Commercial and Mass Cephalopods of the World Ocean 272 pages In RussianFINENKO, Z. Z. 1985pjPrimary production in the areas of rising of the oceanic bottom in the northern part of the Atlantic OceanD= Biological basis of fisheries in the open areas of the ocean184-191  in Russian4*$Fleming, S Furness, R.W. Davies, I.M 2000voContemporary patterns and historical rates of increase of mercury contamination in different marine food chainss:3ICES Annual Science Conference (ICES CM 2000/S:02).) =P$ Meeting of Soviet oceanographers0-Memoir - Sears Foundation for Marine ResearchMemrias do Museu do Mar,)Memrias do Museu do Mar- Srie ZoolgicaHEMethods of determination of the age and growth of new commercial fishTNMethods of determination of the age and growth of new commercial marine fishes0+Mmoires de la Socit Acadmique de l'Aube,'Mmoires de la Socit de Biogographie82Mmoires de la Socit Linnenne de Maine et Loire,'Modern Problems of Fisheries Oceanology Molecular Ecology Mol. Ecol.DAMolluscs, their Systematics, Evolution and Significance in NatureXSMolluscs. Main Results of their Study. 6th Meeting on the Investigation of MolluscspjMolluscs. Results and Perspectives of Investigation. 8th Meeting on the Investigation of Molluscs SciencesMorskaya industriyaMoscow. Trudy IOAN0-Moscow: Legkaya i Pishchevaya Promyshlennost' Moscow: Nauka(#Moscow: Pishchevaya Promyshlennost' Murmansk Murmansk. NAFO SCRNAFO SCR Doc. 82/IX/101 NAFO SCR Doc($NAFO SCR Doc 87/91 Serial No. 1395.NAFO SCR Doc. 87/41 Nature NatureNauka Nauka. Naukova Dumka(#Netherlands Journal of Sae Research85Netherlands Journal of Sea Research Neth. J. Sea Res.NOAA Tech. Rep. NMFShcNon-traditional objects of the sea fishery and perspectives of their exploitation. Theses of papers O Telgrafo<7Occasional Papers of the California Academy of SciencesTQOceanographic bases of formation of biological productivity of the North AtlanticTQOceanographic basis of formation of biological productivity of the North Atlantic$Oceanography and Marine Biology41Oceanography and Marine Biology: an Annual Review$Oceanologica Acta Oceanol. Acta OceanologyOecologia Oecologia OkeanologiaOkeanologiya OkeanologiyaOphelia OpheliaOpusculos Aorianos, I OstrichLGOversigt Kongelige Danske Videnskabernes Selskabs Skrifter, KjbenhavenLHOversigt over det Kongelige Danske Videnskabernes Selskabs Forhandlinger Parazitologia4.Pathology and parasitology of marine organisms$Phil. Trans. Roy. Soc. Lond. B<9Philosophical Transactions of the Royal Society of LondonPhilosophical Transactions of the Royal Society of London Series B-Biological Sciences Philos. Trans. R. Soc. Lond. Ser. B-Biol. Sci.@Problems of investigations and exploitation of the World Ocean|wProblems of studying and rational exploitation of biological resources of seas of the European North and North Atlantic<9Problems of the fisheries oceanography of the North Basin<7Problems of the fishery oceanography of the World OceanPMProblems of the Study of Pelagic Fish and Invertebrates of the Atlantic OceanProblems of the Study of Pelagic Fish and Invertebrates of the Atlantic Ocean. Abstracts of Communications of the Young Scientists Conference, AtlantNIRO, Kaliningrad, 1976,(Progress in Oceanography Prog. Oceanogr.Promyshlenno,reybolovstvoPromyslovaya okeanologiya("Publicaes Europa-Amrica, Lisboa`\Rapports et Proces-Verbaux des Reunions. Conseil Internationale pour l'Exploration de la Mer4/Recent Advances in Cephalopod Fisheries Biologyphalaspid opisthobranchs of the AzoresAoreana  Supl.193-215n*$Monaco, S. A. S. le Prince Albert de 1905.'Sur la campagne de la "Princesse-Alice"2+Bulletin du Muse Ocanographique de Monacot39 1-5&Monteiro, L. R. Furness, R. W.s (unpubl.)opSpeciation through temporal segregation of Madeiran storm petrel (Oceanodroma castro) populations in the Azores?BT(unpublished manuscript)=?| 1979-2001$://000074102300012lXQVinogradov, M. E. Shushkina, E. A. Vedernikov, V. I. Nezlin, N. P. Gagarin, V. I.sPrimary production and plankton stocks in the Pacific Ocean and their seasonal variation according to remote sensing and field observations@9Deep-Sea Research Part Ii-Topical Studies in Oceanography waters; sea`ZData collected from 20 years of observations by the P. P. Shirshov Institute of Oceanology (about 250 comprehensive ecosystem stations) are summarized to evaluate the primary production and biomass of the principal groups of plankton in the Pacific Ocean. The stations were classified into geographical regions according to satellite determined criteria. The areas of these regions were evaluated according to CZCS data from 1978 to 1986. The total value of primary production was evaluated as 26.9 Gt C year(-1). Taking the "bottle effect" correction into account, this value may be as high as 45.6 Gt C year(-1). Total biomass values of phytoplankton (134 Mt C), bacteria (86 Mt C), protozoa (26 Mt C) and mesoplankton (184 Mt C) were also calculated. Seasonal variabilities of all these values were remarkably insignificant. (C) 1998 Elsevier Science Ltd.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 199744 9-10'Russian Acad Sci, PP Shirshov Oceanol Inst, 23 Krasikova St, Moscow 117871, Russia Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117871, Russia Vinogradov ME Russian Acad Sci, PP Shirshov Oceanol Inst, 23 Krasikova St, Moscow 117871, RussiaeHBTimes Cited: 7 English Article ZT582 DEEP-SEA RES PT II-TOP ST OCEISI:000074102300012n 85-103$://000072238800005F@Vinogradov, M. E. Shushkina, E. A. Nezlin, N. P. Arnautov, G. N.f`Vertical distribution of zooplankton in the frontal zone of the Gulf Stream and Labrador Current"Journal of Plankton ResearchZooplankton data collected during September 1995 in the North West Atlantic at 41 degrees 39'N, 49 degrees 58'W (the location of the site of the 'Titanic' wreck) were analysed. The region investigated was characterized by a very sharp frontal zone between the Gulf Stream and the main stream of the Labrador Current. The total plankton biomass in the water column was very high. The macroplankton biomass values below the 600 m layer were significantly higher as compared with the similar values measured before in other productive boreal regions of the Atlantic and Pacific oceans. A lot of dead mesoplankton animals occurred in the deep layers. The reason was that the cold-water mesoplankton advected by the Labrador Current died off intensively within the deep layers of the frontal zone and were used as a food resource by the macroplankton carnivores and scavengers that were very abundant there.J. Plankton Res. 1998 Jan201'Russian Acad Sci, PP Shirshov Oceanol Inst, 36 Nakhimovskiy Ave, Moscow 117851, Russia Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117851, Russia Vinogradov ME Russian Acad Sci, PP Shirshov Oceanol Inst, 36 Nakhimovskiy Ave, Moscow 117851, Russia:3Times Cited: 7 English Article YZ282 J PLANKTON RES ISI:000072238800005riphery of the North Atlantic subtropical gyre4.Izvestiya Akademii Nauk Seriya Biologicheskaya\Ulabrador current; frontal zone; gulf-stream; ocean; peculiarities; communities; fieldeVertical distribution of meso- and macroplankton at the north (36 degrees 14' N) and south (14 degrees 45' N, 15 degrees 10' N) periphery of the North Atlantic gyre was considered. The plankton was studied in the net samples (BR 113/140) and by direct visual count from deep-sea manned vessel Mir during five descents. In addition, benthopelagic animals were collected with baited traps. Bimodal structure of macroplankton biomass distribution was observed with peaks in the main picknocline layer at 200-800 and at 1000-1200 m depth. Quantitative distribution of the deep-sea plankton, as well as its species composition were affected by the northward current of intermediate waters from mesotrophic boreal areas (at the north periphery) and southward ultraoligotrophic waters of the central gyre (at the south periphery). Consequently, the plankton at 36 degrees N is enriched at depth below 800-1000 m and a number of deep-sea and benthic species from boreal regions penetrate far to the south. Conversely, biomass of the plankton at 14-15 degrees N sharply decreases at a depth below 1000 m, apparently, due to inflow of deep-sea waters from the central oligotrophic part of the gyre. Izv. Akad. Nauk Ser. Biol. 2000Jul-Aug4>7Times Cited: 0 Russian Article 369AH IZV AKAD NAUK BIOLISI:000090149300013" RG  2345-2381O$://000169098200010 XRDadou, I. Lamy, F. Rabouille, C. Ruiz-Pino, D. Andersen, V. Bianchi, M. Garcon, V.An integrated biological pump model from the euphotic zone to the sediment: a 1-D application in the Northeast tropical Atlantic@9Deep-Sea Research Part Ii-Topical Studies in Oceanographygoceanic primary production; dissolved organic-carbon; particle mixing rates; early diagenesis; central pacific; eumeli program; sargasso sea; mixed-layer; deep-ocean; matterA coupled one-dimensional biogeochemical/physical model is developed to follow the organic matter fluxes from the upper ocean to the sea floor. The biogeochemical model is a nitrogen- based seven-compartment model including nutrients, phytoplankton, zooplankton, two pools of dissolved organic matter, and two size classes of detrital material. Particle dynamics are considered through the water column as well as organic matter deposition and mineralization in the superficial sediments. The model is applied at the EUMELI oligotrophic site (21 degreesN, 31 degreesW) where different seasons were sampled in 1991-1992 and sediment trap data collected continuously over the same period. The model, forced with the reanalyzed ECMWF fluxes for these years, reproduces satisfactorily the weak seasonal variability of phytoplankton concentration as well as the exported nitrogen fluxes. Annual primary production (65 g C/m(2)/yr) is sustained mainly by remineralization of DON and zooplankton excretion. Export production at 150 m is ensured by large particles, the DON export contributing only 31% of the total export. The POC export represents 1.3% of the primary production. Including nutrient horizontal advection in the model to mimic any lateral Ekman transfer from the enriched neighboring subtropical gyre (5.5 mmol N/m(2)/yr over the first 150 m estimated from optimization) induces an annual primary production of 73 g C/m(2)/yr, closer to Morel et al.'s (Deep- Sea Res. I 43(8) (1996) 1273-1304) estimate (110 g C/m(2)/yr). Estimated mean carbon fluxes at 1000 and 4400 m depth compare well with sediment trap data, 2 mg C/m(2)/d and 1 mg C/m(2)/d, respectively. Remineralization and disaggregation are the dominant processes below 150 m, aggregation playing a minor role. Observed continuous particulate organic matter fluxes over both years show a more variable evolution than the modeled one. This could be due to mesoscale circulation in the area, or subduction of water masses from the Mauritania upwelling. The modeled seasonal variability of dissolved matter fluxes at the water-sediment interface is very weak, as expected. (C) 2001 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 20014810'LEGOS, CNRS, UPS, UMR5566, 18 Ave Edouard Berlin, F-31401 Toulouse 4, France LEGOS, CNRS, UPS, UMR5566, F-31401 Toulouse 4, France LMM, CNRS EP2032, F-13288 Marseille, France CEA, UMR CNRS, LSCE, F-91198 Gif Sur Yvette, France Univ Paris 06, LPCM, F-75230 Paris 05, France Observ Oceanol, Stn Zool, ESA 7076, F-06234 Villefranche Sur Mer, France Garcon V LEGOS, CNRS, UPS, UMR5566, 18 Ave Edouard Berlin, F-31401 Toulouse 4, FrancenHBTimes Cited: 2 English Article 439EQ DEEP-SEA RES PT II-TOP ST OCEISI:000169098200010eJDDadou,I Lamy,F Rabouille,C Ruiz-Pino,D Andersen,V Bianchi,M Garcon,V 2001~xAn integrated biological pump model from the euphotic zone to the sediment:a 1-D application in the NE tropical AtlanticDeep-Sea Research part II 48 2345-2381QOCEANIC PRIMARY PRODUCTION, DISSOLVED ORGANIC-CARBON, PARTICLE MIXING RATES, EARLY DIAGENESIS, CENTRAL PACIFIC, EUMELI PROGRAM, SARGASSO SEA, MIXED-LAYER, DEEP-OCEAN, MATTER;A coupled one-dimensional biogeochemical/physical model is developed to follow the organic matter fluxes from the upper ocean to the sea floor. The biogeochemical model is a nitrogen-based seven-compartment model including nutrients, phytoplankton, zooplankton, two pools of dissolved organic matter, and two size classes of detrital material. Particle dynamics are considered through the water column as well as organic matter deposition and mineralization in the superficial sediments. The model is applied at the EUMELI oligotrophic site (21 degreesN, 31 degreesW) where different seasons were sampled in 1991-1992 and sediment trap data collected continuously over the same period. The model, forced with the reanalyzed ECMWF fluxes for these years, reproduces satisfactorily the weak seasonal variability of phytoplankton concentration as well as the exported nitrogen fluxes. Annual primary production (65 g C/m(2)/yr) is sustained mainly by remineralization of DON and zooplankton excretion. Export production at 150 m is ensured by large particles, the DON export contributing only 31% of the total export. The POC export represents 1.3% of the primary production. Including nutrient horizontal advection in the model to mimic any lateral Ekman transfer from the enriched neighboring subtropical gyre (5.5 mmol N/m(2)/yr over the first 150 m estimated from optimization) induces an annual primary production of 73 g C/m(2)/yr, closer to Morel et al.'s (Deep-Sea Res. I 43(8) (1996) 1273-1304) estimate (110 g C/m(2)/yr). Estimated mean carbon fluxes at 1000 and 4400 m depth compare well with sediment trap data, 2 mg C/m(2)/d and 1 mg C/m(2)/d, respectively. Remineralization and disaggregation are the dominant processes below 150 m, aggregation playing a minor role. Observed continuous particulate organic matter fluxes over both years show a more variable evolution than the modeled one. This could be due to mesoscale circulation in the area, or subduction of water masses from the Mauritania upwelling. The modeled seasonal variability of dissolved matter fluxes at the water-sediment interface is very weak, as expected. (C) 2001 Elsevier Science Ltd. All rights reserved.555-585$://A1993MJ37100020oDaly, K. L. Smith, W. O.NGPhysical-Biological Interactions Influencing Marine Plankton Production,.(Annual Review of Ecology and Systematics phytoplankton; zooplankton; turbulent motion; nutrient uptake; grazing marginal ice-zone; subarctic pacific-ocean; small-scale turbulence; euphausia-superba; southern-ocean; el-nino; phytoplankton growth; vertical migration; feeding currents; british-columbiatHBThe interaction of physical and biological processes is extremely important in structuring the biological communities in all marine environments, yet the complexity of this interaction at all scales is just beginning to be appreciated. We review the patterns of plankton biomass and the processes that influence plankton production, and in particular emphasize the importance of different processes at different time and space scales (small-scale, mesoscale, and large-scale). Examples of two different systems (the Southern Ocean and the subarctic North Pacific and North Atlantic Oceans) are given to illustrate the complexity and strength of the interactions. We conclude that biological processes may be more important at smaller scales where behavior such as vertical migration and predation may control the plankton production, whereas physical processes may be more important at larger scales in structuring biological communities. An understanding of both, however, is critical to an understanding of the distribution of plankton and the processes governing production in the ocean.Annu. Rev. Ecol. Syst. 199324>7Times Cited: 12 English Review MJ371 ANNU REV ECOL SYSTISI:A1993MJ37100020  80,Relatrio da IV Semana das Pescas dos Aores0,Relatrio da IX Semana das Pescas dos AoresTPRelatrio da Universidade dos Aores e Royal Society for the Protection of Birds0,Relatrio da VI Semana das Pescas dos Aores0-Relatrio da VII Semana das Pescas dos Aores4.Relatrio da VIII Semana das Pescas dos Aores0+Relatrio da X Semana das Pescas dos Aores0,Relatrio da XI Semana das Pescas dos Aores4.Relatrio da XIII Semana das Pescas dos Aores($Relatrio de Estgio de Licenciatura Relatrio Interno do DOP/UA<6Relatrios e Communicaes do Departamento de BiologiaPLRelatrios e Comunicaes do Departamento de Biologia, Ponta Delgada, AoresRelatrios INIPRelatrios INIP, Lisboa,)Relatrios Tcnicos e Cientficos do INIPd`Rep.Study Group on Biology and Assessment of the Deep-sea Fisheries Resources. ICES Headquarters0-Report of the International Whaling Commision<9Report of the International Whaling Commission (SC/32/01)hdReport of the Scientific Results of the Voyage of the H. M. S. Challenger During the Years 1873-1876\WReport of the study Group on the Biology and assessment of Deep-Sea Fisheries resources84Reports of the Swedish Deep-Sea Expedition 1947-19484.Research SRTM-0839 "Ladoga"/SevrybpromrazvedkaPMResources and perspectives of exploitation of squid stocks of the World OceanLGResources and perspectives of exploitation of squids of the World OceanPJResources and Perspectives of the Exploitation of Squid in the World Ocean`ZResources and Perspectives of the Exploitation of Squid in the World Ocean. Ed. B.G.Ivanov<8Retrospective review and nowadays possibility of fisheryReviews of GeophysicslhRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverain du MonacoxsRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverain du Monaco, Fascicule RuthenicaRuthenica, 2001Rybnoe khozyaistvo Sarsia SarsiaSci. Tot. EnvironScientia Marina Seabird Sevastopol, "Hydronaut" Base Sevrybpromrazvedka. MurmanskPLSix Memoir- Sears Foundation for Marine Research, Yale University, New HavenLHSmithsonian Institution, United States National Museum, Special BulletinLISoviet fisheries investigations in the seas of the European North. Moscow}Spatial and temporal variability of hydrometeorological conditions in the fishing grounds of the Atlantic Ocean. Kaliningrad.41Standford University Press, Standford, CalifornialgState of Biological Resources of Fishery Industry in the Central and South Atlantic and Eastern Pacific|Status of stocks and dynamics of abundance of pelagic fish of the World Ocean. Theses of papers of the scientific conference Steenstrupia0-Studies of bioresources of the North AtlanticD@Studies of bioresources of the North Atlantic. Collected PapersStudying and rational exploitation of biological resources of north seas and North Atlantic. Theses of papers of the conference of young scientists and specialists(%Systematic and ecology of cephalopodsSystematic Zoology0+Systematics and Biogeography of Cephalopods$T.F.H. Publications, New Jersey(#Taxonomy and Ecology of Cephalopods2 Shaboneyev, I. Yee 1973 Materials on the biology of the horsemackerel Trachurus picturatus picturatus (Bowdich) in the eastern part of the central Atlantic Trudyl  93D 91-101"(English translation, mimeo) 75-86$://A1997XZ98100008e Shanks, A. L. Walters, K.rLEHoloplankton, meroplankton, and meiofauna associated with marine snowh$Marine Ecology-Progress Seriesmarine snow; aggregates; nauplii; meroplankton; veligers; holoplankton; copepod; nematode; meiofauna abandoned larvacean houses; deep-sea; vertical flux; populations; dynamics; atlantic; california; detritus; patches; sinkingaThe associations of holoplankton, meroplankton and meiofauna with marine snow, as well as their behavior upon encountering marine snow, were investigated using SCUBA in the field and a vertical flume in the laboratory. Field samples were collected in the Atlantic Ocean off Charleston, South Carolina, USA. (3 dates) and in the Pacific Ocean at 2 locations in the San Juan Islands, Washington, USA (7 dates). Aggregates were present and abundant on all days (range 1 to 63 aggregates l(-1)) but constituted a small percentage of the water column by volume (avg 0.078 %). Holoplanktonic adult calanoid and cyclopoid copepods, larvaceans, and copepod nauplii were found on aggregates. On average <1% of the calanoid and cyclopoid copepods sampled were on aggregates, indicating a weak association with marine snow. In contrast, on average 2.6 % of the larvaceans and 4.8 % of the copepod nauplii sampled resided on aggregates, where they were, respectively, 33 to 62 times more concentrated on marine snow compared to the surrounding water. Percentages of harpacticoid copepods, nematodes, and foraminiferans on aggregates were 12.4, 69.9 and 47.2%, respectively, and all were significantly concentrated on aggregates. Cyprids, bryozoan cyphonautes, and larval echinoderms were either weakly associated with or not found on aggregates. In contrast, bivalve and gastropod veligers and larval anthozoans were significantly concentrated on marine snow, with 5.8, 9.4, and 13.5%, respectively, found on aggregates. Observations in a vertical flume indicated that upon contacting marine snow calanoid and cyclopoid copepods swam away, copepod nauplii swam inside aggregates for several minutes before swimming off, and nematodes were observed to remain in aggregates throughout the observation period adding material from the surrounding water to the 'home' aggregate. These observations suggest that plankters and meiofauna in the water column may spend several hours d(-1) visiting or residing on aggregates, and may visit from 10s to 100s of aggregates d(- 1). The concentration and behavior of organisms on aggregates suggests that marine snow is an important component of the pelagic environment for a variety of both holoplanktonic and meroplanktonic zooplankton.Mar. Ecol.-Prog. Ser. 1997 156'UNIV OREGON,OREGON INST MARINE BIOL,POB 5389,CHARLESTON,OR 97420 MIDDLE TENNESSEE STATE UNIV,DEPT BIOL,MURFREESBORO,TN 37132 Shanks AL UNIV OREGON,OREGON INST MARINE BIOL,POB 5389,CHARLESTON,OR 97420>8Times Cited: 10 English Article XZ981 MAR ECOL-PROGR SERISI:A1997XZ98100008b nN HAHarris, R.P Boyd,P Harbour, D.S Head, R.N Pingree, R.D Pomroy,A.J 1997piPhysical, chemical and biological features of a cyclonic eddy in the region of 61 10'N 19 50' W in the NA8Deep-Sea Research part I 4411 1815-1839 1855-1875$://A1988R606600004Harvey, J. Arhan, M.@9The Water Masses of the Central North-Atlantic in 1983-84& Journal of Physical OceanographyJ. Phys. Oceanogr. 1988 Dec1812'UNIV E ANGLIA,SCH ENVIRONM SCI,NORWICH NR4 7TJ,NORFOLK,ENGLAND INST FRANCAIS RECH EXPLOITAT MER,CTR BREST,BREST,FRANCE HARVEY J UNIV E ANGLIA,SCH ENVIRONM SCI,NORWICH NR4 7TJ,NORFOLK,ENGLAND<5Times Cited: 35 English Article R6066 J PHYS OCEANOGRISI:A1988R606600004Harvey, J. Arhan, M. 1988@:The water masses of the Central North Atlantic in 1983-84.& Journal of Physical Oceanography1812 1855-1875 57-63$://A1995RQ34100007 4.Haury, L. Fey, C. Gal, G. Hobday, A. Genin, A.81Copepod Carcasses in the Ocean .1. Over Seamountsi$Marine Ecology-Progress Seriescopepod; carcass; seamount; predation benthopelagic plankton; migrating zooplankton; new-england; deep-sea; predation; micronekton; community; calanus; pacific; preywPIHigher abundances of copepods with external damage or in various states of internal decay have been found in shallow waters over banks, ridges and seamounts than in the surrounding waters. The increase occurred in 3 of 5 sets of multiple opening-closing net tows taken at Fieberling Guyot, Northeast Bank and Sixtymile Bank, west of San Diego, California, USA. Large numbers of copepod carcasses were also found above the summit of Jasper Seamount. The carcasses are attributed to higher levels of predation over shallow topographic features due to resident organisms that ascend above the summits at night to feed. At Fieberling Guyot (summit depth of about 500 m), this migration was at least 400 m above the summit. Carcasses identical to those collected in the net tows were produced in the laboratory by euphausiids feeding on copepods.Mar. Ecol.-Prog. Ser. 1995 Jul 123 1-3'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,MARINE LIFE RES GRP,LA JOLLA,CA 92093 HEBREW UNIV JERUSALEM,H STEINITZ MARINE BIOL LAB,IL-88103 ELAT,ISRAEL HAURY L UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,MARINE LIFE RES GRP,LA JOLLA,CA 92093>7Times Cited: 6 English Article RQ341 MAR ECOL-PROGR SERISI:A1995RQ34100007 69-105$://000086181200003D.'Haury, L. Fey, C. Newland, C. Genin, A.VJDZooplankton distribution around four eastern North Pacific seamountsProgress in Oceanographyztthermohaline structure; fieberling seamount; copepod carcasses; topography; patchiness; currents; guyot; ocean; flowThe effects of seamounts on the distribution of zooplankton were investigated at four seamounts in the northeastern Pacific. The following hypotheses were tested: (1) mesoscale gaps of reduced abundance of migrating zooplankton develop over seamounts every night; (2) fine-scale patchiness is augmented within these gaps and in the region downstream of seamounts; and (3) increased numbers of crustacean carcasses occur over seamounts. Gaps are expected because most zooplankton that descend over shallow topography at dawn are either eaten by resident predators or are advected off the summit, while fine- scale patchiness should result from lateral shear between the gap and the surrounding zooplankton-rich waters. Copepod carcasses should be more abundant over seamounts than the surrounding water because of the increased predation at seamounts. Zooplankton distributions were determined from net samples and acoustic records. Water column properties were measured with a CTD and hydrocasts, and currents by moored current meters, acoustic current profilers and drifter drogues. Zooplankton gaps were found over three of the four seamounts surveyed, but not on every survey of each seamount. Only three of the surveys provided the information necessary to test the patchiness hypothesis; on two of these increased patchiness and carcass abundance were found associated with gaps. When no gap was observed over a seamount, there was no evidence of increased carcass abundance or enhanced patchiness, indicating that the three phenomena are temporally and spatially linked. Copepod carcasses were found in the intestines of small fish sampled at the same time as the zooplankton. The fish, along with crustacean predators like euphausiids, are the likely source for the carcasses. Seamounts appear to be an important cause of enhanced zooplankton patchiness on scales ranging from 100s of meters to areas larger than the seamounts themselves. (C) 2000 Elsevier Science Ltd. All rights reserved.Prog. Oceanogr. 2000451'VOUniv Calif San Diego, Scripps Inst Oceanog, Marine Life Res Grp, La Jolla, CA 92093 USA Univ Calif San Diego, Scripps Inst Oceanog, Marine Life Res Grp, La Jolla, CA 92093 USA Hebrew Univ, H Steinitz Marine Biol Lab, IL-88103 Eilat, Israel Haury L Univ Calif San Diego, Scripps Inst Oceanog, Marine Life Res Grp, La Jolla, CA 92093 USA81Times Cited: 1 English Review 299DV PROG OCEANOGRISI:000086181200003PJHawkins, S. J. Burnay, L. P. Neto, A. I. Tristo da Cunha, R. Frias, A. F.  1990arkA description of the zonation patterns of molluscs and other biota on the south coast of So Miguel, AzoresoAoreana Supl.  21-38*R|LKHROMOV, D. N. 1986PJPeculiarities of distribution of pelagic Cephalopoda of the North AtlanticTN Resources and perspectives of exploitation of squid stocks of the World Ocean  37-46 in Russian Khromov, D.N.a 1987LEPatterns of distribution of pelagic cephalopods of the North AtlanticlRK Resources and Perspectives of the Exploitation of Squid in the World Oceanr  37-46&In English with Russian summary60KISLITSYN, S. P. A. P. NAGURNY A. S. TSVETUCHIN. 1983Mezo-scale structure of heat flows on the surface of water by observations on the oceanographic fields (August-September, 1977)7 3828119-1232 in Russian$KISLYAKOV, A. G. V. V. ROSSOV. 1973d^Some features of water circulation in the central and northeastern areas of the North Atlantic Trudy PINROR No. 34 10-363 in RussianKlaveren, P. van.e 1992Le Prince Albert I et le Prince Rainier III, un soucis commun: prserver l' environment. in Saldanha, L., R, P. and Martins, A. F. (Eds.). Centenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L'Hirondelle7Aoreana Supl. 83-98"KLENOVA, M. V. V. M. LAVROV. 1975$Geology of the Atlantic Oceana Naukak456 pp.p in Russian&KLIMENKOV, A. I. V. E. KEMENOV.d 1982ngRecommendations on search and fishery in the area of the underwater mountains of the Mid-Atlantic RidgeeXQMaterials on methods of searching for fish and non-fish objects in the open ocean 40-50 in RussianKlyuchnik, T.S.  1975b[Species composition and distribution of the larvae of oceanic squid in the eastern AtlanticHB Molluscs, their Systematics, Evolution and Significance in Nature2,5th Meeting of the Investigation of Molluscs165-166 F?In Russian. English translation: Malacological Review, 11(1978)Knud,S Beckmann,W 1995PINew benthopelagic tharybids (copepoda:calanoida) from the deep N Atlanticu$Institute of Taxonomic Zoology80199-211  Knudsen, J. 1995~wObservations on reproductive strategy and zoogeography of some marine prosobranch gastropods (Mollusca) from the Azores0Aoreana Supl.m135-158  Koefoed, E. 1932`ZFishes from the sea-bottom from the "Michael Sars" north Atlantic deep-sea Expedition 1910f_Report on the Scientific Results of the "Michael Sars" North Atlantic Deep -Sea Expedition 1910 (Bergen Museum)411-148 + 6 plates 19270*Koeve,W Pollehne,F Oschlies,A Zeitzschel,B 2002^XStorm-induced convective export of organic matter during spring in the NE Atlantic oceanDeep-Sea Researche part I 1-14$KOLINKO, A. V. V. N. KISELEV.r 1990Large-scale variability of characteristics of heat exchange between the ocean and the atmosphere in the area of the ocean station C Trudy GOIN  190105-114t in Russian"KOLINKO, A. V. I. V. NAZAROV 1990~Investigation of heat exchange of synoptic vortices between the ocean and atmosphere by data of measurements of ocean stations Trudy GOIN  192  88-94 in RussianA B1113-1120$://000085009000011tB;Bianchi, A. Garcin, J. Gorsky, G. Poulicek, M. Tholosan, O.Stimulation of the potential heterotrophic activity in deep seawater by barotolerant bacteria colonizing faecal pellets produced by migrating zooplanktonZTComptes Rendus De L Academie Des Sciences Serie Iii-Sciences De La Vie-Life Sciencesbacteria; metabolic activity; barophile; hydrostatic pressure; faecal 657-668$://A1995TE36800039&Astthorsson, O. S. Gislason, A.LFLong-Term Changes in Zooplankton Biomass in Icelandic Waters in Spring$Ices Journal of Marine Sciencecod; icelandic waters; long-term changes; zooplankton plankton contact rates; small-scale turbulence; northeast atlantic; sea; trends; larvae Since the early 1960s studies on zooplankton biomass and species composition have been carried out on standard transects during late May and early June in the waters north of Iceland. In the early 1970s the studies were extended to also cover the waters south, west, and east of the island. The present article summarizes these long-term investigations in spring for 62 stations on 9 transects. Calanus finmarchicus usually constituted about 50-80% of the number of animals in the zooplankton samples. Other species/groups of considerable importance in certain areas were C. glacialis, C. hyperboreus, Metridia longa, euphausiid larvae, and cirripede larvae. The horizontal distribution of the zooplankton biomass from shallow to deep water and in different areas was usually relatively uniform (2-4 g m(-2)), except for the frontal area between coastal and Atlantic Water south of Iceland (ca. 10 g m(-2)) and in the waters off the north-east coast beyond the shelf in the Arctic East Icelandic Current (9-11 g m(-2)). North-east of Iceland this is explained by both differences in the state of development and in the composition of the zooplankton. The difference between the highest and lowest biomass on the different transects was 7-24-fold. Principal component analysis (PCA) for the transects in the Atlantic Water south of Iceland revealed maxima in biomass during the mid-1970s, 1980s, and an upward trend since the early 1990s. Lows were observed in the Atlantic Water during the late 1970s and late 1980s. In the transitional waters north-west and north of Iceland (mixed Atlantic/Arctic) PCB demonstrated maxima in the early 1960s, late 1970s and a clear upward trend since the early 1990s. During the minima observed in the intervening periods, slight upward shifts occurred during 1971-1973 and 1984-1986. For the Arctic waters of the north-east and east coasts the PCA showed maxima during the mid-1970s, 1980s, an upward trend since the early 1990s and minima during the late 1970s and late 1980s. Thus, for both the Atlantic and Arctic Waters PCA reveals a period of approximately 10 years between maxima in biomass, while in the transitional waters (mixed Atlantic/Arctic) this period appears to be 16 years. The abundance of 0-group cod in Icelandic waters during 1974-1999 suggests strong interactions with the zooplankton on their spawning grounds and larval drift route to the south and west of Iceland. (C) 1995 International Council for the Exploration of the SeaRICES J. Mar. Sci.3 1995Jun-Aug52 3-4'MARINE RES INST,POB 1390,SKULAGATA 4,IS-121 REYKJAVIK,ICELAND ASTTHORSSON OS MARINE RES INST,POB 1390,SKULAGATA 4,IS-121 REYKJAVIK,ICELAND:3Times Cited: 9 English Article TE368 ICES J MAR SCIaISI:A1995TE36800039ep ^ 2721-2736c$://000085208800003g2,Jaroslow, G. E. Smith, D. K. Tucholke, B. E.{Record of seamount production and off-axis evolution in the western North Atlantic Ocean, 25 degrees 25 '-27 degrees 10 ' Ni2+Journal of Geophysical Research-Solid Earthiridge-transform intersections; east pacific rise; gravity- anomalies; rift-valley; magmatic accretion; spreading ridges; fracture-zone; segmentation; morphology; 26-degrees-n Using multibeam bathymetry, we identified 86 axial and 1290 off-axis seamounts on the western flank of the (near-circular volcanoes with heights greater than or equal to 70 m) in an area of 75,000 km(2) Mid-Atlantic Ridge (MAR), 25 degrees 25'N to 27 degrees 10'N, extending: similar to 400 km from the inner rift valley floor to similar to 29 Ma crust. Our study shows that seamounts are la common morphological feature of the North-Atlantic seafloor. Seamount-producing volcanism: occurs primarily on the inner rift valley floor, and few, if any, seamounts are formed on the rift valley walls or the ridge flank. The high abundance of off-axis seamounts is consistent with 1-3 km wide sections of oceanic crust being transferred intact from the axial valley to the ridge flank; on crust >4 Ma. Significant changes in seamount abundances, sizes, and shapes are attributed to the effects of faulting between similar to 0.6 and 2 m.y. off axis in the lower rift valley walls. Few seamounts are completely destroyed by (inward facing) faults, and population abundances are-similar to those on axis. However, faulting reduces the characteristic height of the seamount-population significantly. In the upper portions of the rift valley, on 2-4 Ma crust, crustal aging processes (sedimentation and mass wasting), together with additional outward facing faults, destroy and degrade a significant number of seamounts. Beyond the crest of the rift mountains (>4 Ma crust) faulting is no longer active, and changes in the off- axis seamount population reflect crustal aging processes as well as temporal changes in seamount production that occurred at the ridge axis. Estimates of population density for off-axis seamounts show a positive correlation to crustal thickness inferred from analysis of gravity,data, suggesting that increased seamount production accompanies increased magma input:at the ridge axis. We find no systematic variations in seamount population density along isochron within individual ridge segments. Possible explanations are that along-axis production of seamounts is uniform or that seamount production is enhanced in some regions (e.g., segment centers), but many seamounts do not meet our counting criteria because they are masked by younger volcanic eruptions and low-relief flows."J. Geophys. Res.-Solid Earth 2000 Feb 10 105B2'Sea Educ Assoc, POB 6, Woods Hole, MA 02543 USA Sea Educ Assoc, Woods Hole, MA 02543 USA Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA Tucholke BE Sea Educ Assoc, POB 6, Woods Hole, MA 02543 USAD>Times Cited: 2 English Article 282GC J GEOPHYS RES-SOLID EARTHISI:000085208800003 Jensen, K. R. 1995mAnatomy and biology of Aplysiopsis formosa Pruvot-Fol (Mollusca, Opisthobranchia, Sacoglossa) from the Azores*Aoreana Supl.217-230D 225-236$://A1992KG43200006&Astthorsson, O. S. Gislason, A.d^Investigations on the Ecology of the Zooplankton Community in Isafjord-Deep, Northwest Iceland Sarsia`Ywestern sweden; northern norway; kosterfjorden; balsfjorden; abundance; dynamics; calanusQuantity and composition of zooplankton at three stations in Isafjord-deep, northwest Iceland, were studied from February 1987 to February 1988 Sampling was made with 335 mum mesh Bongo-net at approximately monthly intervals along with hydrographic measurements and measurements of chlorophyll a concentrations. Spring warming of the water began in early May and maximum temperatures (8-10-degrees-C) were observed during July-September. The phytoplankton bloom started in early April, maximum chlorophyll a levels were observed in late April to the middle of May (c. 8 mg Chl a/m3), and a smaller 'autumn increase' was again observed in July to August (c. 3 mg Chl a/m3). The total zooplankton volume was highest in August (c. 32 ml/100 m3) while it was lowest in February 1987 (< 1 ml/m3). During the winter months euphausiids dominated in terms of volume (> 90 %) while during the summer months the combined volume of fish larvae and 'other zooplankton' (mainly copepods and cirripedes) was similar to that of the euphausiids. The total number of zooplankton stayed small through April. Increasing number through the following months led to a maximum in August (c. 90 000 individuals/100 m3), after which numbers decreased sharply to low winter levels. A total of 40 species and groups was recorded in Isafjord-deep, but only six (Acartia spp., Calanus finmarchicus, Pseudocalanus elongatus, Temora longicornis, Balanus balanoides and Verruca stroemia) usually constituted 80-90 % of the total zooplankton number, The dominant holoplanktonic copepods showed similar changes throughout the year, with a pronounced maximum in August. C. finmarchicus overwintered at copepodite stages IV and V and the overwintering generation spawned during late March and early April. Only a part of the spring generation became mature in June to produce the second generation during the year; the majority remained at younger copepodite stages during The summer and autumn and did not become mature until the following spring. The spring spawning of C. finmarchicus in March-April appeared to be closely linked to the phytoplankton spring bloom, while at that time the temperature in Isafjord-deep was near the annual low. Sarsia 199277 3-4g'MARINE RES INST,SKULAGATA 4,POB 1390,121 REYKJAVIK,ICELAND ASTTHORSSON OS MARINE RES INST,SKULAGATA 4,POB 1390,121 REYKJAVIK,ICELAND2+Times Cited: 5 English Article KG432 SARSIAfISI:A1992KG43200006w  ILIAstronomy & Astrophysics Supplement Series Astron. Astrophys. Suppl. Ser. AtlantNIRO$AtlantNIRO, Zaprybpromrazvedka85Australian. Journal of Marine and Freshwater ResearchTNAutoreferat of the Dissertation Candidate of Biological Sciences [cited above]<9Basin Problems of fisheries oceanography of the Northern BeaufortiaBehavioral Ecology$Behaviour of commercial fishes$ Behaviour of Water Invertebrates<6Berichte zur Polarforschung, Reports on Polar researchBilogical Oceanography0-Biochemical and populational genetics of fish@://000071350200001O"Saltzman, J. Wishner, K. F.ArkZooplankton ecology in the eastern tropical Pacific oxygen minimum zone above a seamount: 1. General trends,<6Deep-Sea Research Part I-Oceanographic Research Paperstnvertical-distribution; ocean; deep; sea; plankton; layer; nitrification; micronekton; temperature; adaptationsThe distribution of zooplankton in the oxygen minimum zone (OMZ) of the eastern tropical Pacific and near a seamount was investigated. The oxygen minimum layer appeared to be an important factor influencing the vertical distribution of zooplankton taxa below the thermocline. The maximum zooplankton in terms of biomass and numbers was in the thermocline zone, with a secondary maximum in the depth zone that included the lower OMZ interface (600-1000 m). Most taxonomic groups showed this secondary peak in abundance in the lower OMZ interface depth zone and minimum abundances above it. The secondary maximum in zooplankton at the lower OMZ interface seems to be unique to OMZ regions. Only larvaceans and mollusks did not appear to be strongly influenced by the minimum concentrations of oxygen. Four vertical distribution patterns characteristic of different taxonomic groups may be indicative of their different tolerances to minimum oxygen concentrations. The physical intrusion of the seamount (summit at 730 m depth) did not cause major changes in the distribution of pelagic zooplankton. Significant biological and physical differences between locations above and away from the seamount were found only within the upper OMZ (100-300 m). Published by Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 Jun446'Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Saltzman J Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USAHBTimes Cited: 8 English Article YQ117 DEEP-SEA RES PT I-OCEANOG RESISI:000071350200001er OMZ interface seems to be unique to OMZ regions. Only larvaceans and mollusks did not appear to be strongly influenced by the minimum concentrations of oxygen. Four vertical distribution patterns characteristic of different taxonomic groups may be indicative of their different tolerances to minimum oxygen concentrations. The physical intrusion of the seamount (summit at 730 m depth) did not cause major changes in the distribution of pelagic zooplankton. Significant biological and physical differences between locations above and away from the seamount were found only within the upper OMZ (100-300 m). Published by Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 Jun446'Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Saltzman J Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USAHBTimes Cited: 8 English Article YQ117 DEEP-SEA RES PT I-OCEANOG RESISI:000071350200001} J 93-115$://A1995QL67100006 rlWishner, K. F. Ashjian, C. J. Gelfman, C. Gowing, M. M. Kann, L. Levin, L. A. Mullineaux, L. S. Saltzman, J.lfPelagic and Benthic Ecology of the Lower Interface of the Eastern Tropical Pacific Oxygen Minimum Zone<6Deep-Sea Research Part I-Oceanographic Research Papersboundary-layer zooplankton; santa-catalina basin; vertical- distribution; upwelling system; arabian sea; seamount; rates; ocean; deep; carbonz The distributions of pelagic and benthic fauna were examined in relation to the lower boundary of the oxygen minimum zone (OMZ) on and near Volcano 7, a seamount that penetrates this feature in the Eastern Tropical Pacific. Although the broad, pronounced OMZ in this region is an effective barrier for most zooplankton, zooplankton abundances, zooplankton feeding rates, and ambient suspended particulate organic carbon (POC) peaked sharply in the lower OMZ (about 740-800 m), in association with the minimum oxygen concentration and the increasing oxygen levels just below it. Zooplankton in the lower OMZ were also larger in size, and the pelagic community included some very abundant, possibly opportunistic, species. Elevated POC and scatter in the light transmission data suggested the existence of a thin, particle-rich, and carbon-rich pelagic layer at the base of the OMZ. Gut contents of planktonic detritivores implied opportunistic ingestion of bacterial aggregates, possibly from this layer. Benthic megafaunal abundances on the seamount, which extended up to 730 m, peaked at about 800 m. There was a consistent vertical progression in the depth of first occurrence of different megafaunal taxa in this depth range, similar to intertidal zonation. Although the vertical gradients of temperature, salinity, and oxygen were gradual at the lower OMZ interface (in contrast to the upper OMZ interface at the thermocline), temporal variability in oxygen levels due to internal wave-induced vertical excursions of the OMZ may produce the distinct zonation in the benthic fauna. The characteristics of the lower OMZ interface result from biological interactions with the chemical and organic matter gradients of the OMZ. Most zooplankton are probably excluded physiologically from pronounced OMZs. The zooplankton abundance peak at the lower interface of the OMZ occurs where oxygen becomes sufficiently high to permit the zooplankton to utilize the high concentrations of organic particles that have descended through the OMZ relatively unaltered because of low metazoan abundance. A similar scenario applies to megabenthic distributions. Plankton layers and a potential short food chain (bacteria to zooplankton) at OMZ interfaces suggest intense utilization and modification of organic material, localized within a thin midwater depth zone. This could be a potentially significant filter for organic material sinking to the deep-sea floor..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1995 Jan421'UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882 UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 95064 UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093 WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543 WISHNER KF UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882JCTimes Cited: 27 English Article QL671 DEEP-SEA RES PT I-OCEANOG RESISI:A1995QL67100006([SI>://A1996VU62300002i*#Llewellyn, C. A. Mantoura, R. F. C.6|Pigment biomarkers and particulate carbon in the upper water column compared to the ocean interior o261-283$://A1992HX79300002o Ottens, J. J.eb[April and August Northeast Atlantic Surface-Water Masses Reflected in Planktic Foraminifera*#Netherlands Journal of Sea Research-}cold-core eddy; phytoplankton growth; azores front; canary basin; eastern; zooplankton; circulation; chlorophyll; shelf; flowF?Northeast Atlantic surface water masses and corresponding frontal zones were alike in April and August, although April frontal zones were enlarged compared to August. The observed water masses and fronts are the Subpolar Water (SW), the Subpolar Front (SF), the North Atlantic Current (NAC), North Atlantic Transitional Water (NATW), the Azores Frontal Zone (AFZ) and the Azores Current (AC). During August, clusters of relative and absolute frequencies of planktic foraminifera corresponded with water masses as conventionally distinguished on oceanic conditions. However, the distinct faunal assemblages deviated from the observed oceanic regime in April, when the transition between the immutable winter and the highly variable spring periods resulted in broad frontal zones. Under those conditions absolute frequencies and information indices prove to be better suited to characterize oceanic conditions than assemblage composition. The highly mixed and migrating fronts strongly influenced the planktic community and affected the horizontal as well as vertical species distribution.-Neth. J. Sea Res.  1992 MarA284L'FREE UNIV AMSTERDAM,INST EARTH SCI,CTR GEOMARINE,DE BOELELAAN 1085,1081 HV AMSTERDAM,NETHERLANDS OTTENS JJ FREE UNIV AMSTERDAM,INST EARTH SCI,CTR GEOMARINE,DE BOELELAAN 1085,1081 HV AMSTERDAM,NETHERLANDSs:3Times Cited: 5 English Article HX793 NETH J SEA RES ISI:A1992HX79300002S Ottens, J.Jc 1992b[April and August northeast Atlantic surface water masses reflected in planktic foraminifera *#Netherlands Journal of Sae Research 28 (4)261-283}COLD-CORE EDDY, PHYTOPLANKTON GROWTH, AZORES FRONT, CANARY BASIN, EASTERN, ZOOPLANKTON, CIRCULATION, CHLOROPHYLL, SHELF, FLOWF?Northeast Atlantic surface water masses and corresponding frontal zones were alike in April and August, although April frontal zones were enlarged compared to August. The observed water masses and fronts are the Subpolar Water (SW), the Subpolar Front (SF), the North Atlantic Current (NAC), North Atlantic Transitional Water (NATW), the Azores Frontal Zone (AFZ) and the Azores Current (AC). During August, clusters of relative and absolute frequencies of planktic foraminifera corresponded with water masses as conventionally distinguished on oceanic conditions. However, the distinct faunal assemblages deviated from the observed oceanic regime in April, when the transition between the immutable winter and the highly variable spring periods resulted in broad frontal zones. Under those conditions absolute frequencies and information indices prove to be better suited to characterize oceanic conditions than assemblage composition. The highly mixed and migrating fronts strongly influenced the planktic community and affected the horizontal as well as vertical species distribution.rPafort- van Iersel, Ta 1981The Sternoptychidae (Pisces: Stomiatoidei) of the Amsterdam mid-north Atlantic expedition, with a note on specimens intermediate between Argyropelecus aculeatus Valenciennes, 1849 and A. olfersi (Cuvier, 1829)a Beaufortia 31 (4) 97-106 Parin, N. V 1970*#Ichthyofauna of the Epipelagic Zone <5Israel Program for Scientific Translations, Jerusalem  205$Parin, N. V S. G. Kobyliansky  1996Diagnoses and distribution of fifteen species recognized in genus Maurolicus Cocco (Sternoptychidae, Stomiiformes) with a key to their identification Cybium 20 (2)185-195S Ferry Rd, Narragansett, RI 02882 USA Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA Univ Calif Santa Cruz, Inst Marine Sci, Santa Cruz, CA 95064 USA Wishner KF Univ Rhode Isl, Grad Sch Oceanog, S Ferry Rd, Narragansett, RI 02882 USA:4Times Cited: 1 English Article 373AW LIMNOL OCEANOGRISI:000165267100012&Zaferman, M. L. Sennikov, A. M. 1991`ZDistribution, biology and behaviour of deepwater crabs in open areas of the North Atlantic VNIRO 1991 69-80tR l  13-25$://A1994MV23900002, Osgood, K. E. Frost, B. W.zsOntogenic Diel Vertical Migration Behaviors of the Marine Planktonic Copepods Calanus-Pacificus and Metridia-LucensC$Marine Ecology-Progress Seriesdiel vertical migration; calanus pacificus; metrida lucens; zooplankton; dabob bay adaptive significance; euphausia-pacifica; feeding-behavior; north pacific; inland sea; zooplankton; ocean; prey; helgolandicus; finmarchicus4.Daytime and nighttime vertically stratified zooplankton samples spanning the entire water column were obtained from Dabob Bay, Washington, USA, during several years. Vertical distributions of all the copepodid stages of Calanus pacificus and Metridia lucens were analyzed from 8 cruises representing the range of seasons, as well as several dates when inferred invertebrate or vertebrate predation pressures on zooplankton were strong or weak. Migration behaviors of similar-sized stages of C. pacificus and M. lucens differed. C. pacificus was closely associated with the surface waters; a large percentage of every stage was always in the surface 50 m at night except when the C5s were in diapause. During the day the different stages of C. pacificus showed varying degrees of avoidance of the surface layers, with the older, larger stages generally being deeper. The C4 and younger stages were particularly tied to the surface waters, with the majority of the population usually in the top 25 m during the day and night. M. lucens was less strongly associated with the surface layers. While the adult females, and usually the C5s, underwent a normal diel vetical migration (DVM), entering the surface 50 m at night, the vast majority of the adult males always stadyed below 75 m. The C4 and younger stages showed more varied behavior. On some dates they underwent a reverse DVM, avoiding the surface 25 m at night, at other times they avoided the surface 10 m particularly during the day, while on still other dates the C3 and younger stages avoided the surface 25 m day and night. On most dates there were significant portions of all the stages in the deepest layers sampled. Differences in the 2 species' migration behavior may be due to differences in their susceptibility to predation, or some additional aspect of their biologies.Mar. Ecol.-Prog. Ser. 1994 Jan 104 1-2'voUNIV WASHINGTON,SCH OCEANOG,WB-10,SEATTLE,WA 98195 OSGOOD KE UNIV WASHINGTON,SCH OCEANOG,WB-10,SEATTLE,WA 98195>8Times Cited: 21 English Article MV239 MAR ECOL-PROGR SERISI:A1994MV23900002 13-28$://A1992HU784000030&Ottens, J. J. Nederbragt, A. J.uJCPlanktic Foraminiferal Diversity as Indicator of Ocean EnvironmentsnMarine Micropaleontology\Unorthern indian-ocean; isotope record; red-sea; atlantic; oxygen; sediments; site-522sThe combination of the number of species (simple diversity), an information function (Shannon diversity) and a measure of equitability is used to characterize modern ocean environments based on planktic foraminiferal faunas. Regional environmental conditions can be recognized as deviations from the global latitudinal trend. Simple diversity (number of species) offers relatively little resolution itself, because it is sensitive to the addition of rare species. Variable conditions, such as the highly productive spring bloom and upwelling, are characterized by relatively low diversity and equitability values. Relatively high diversity and a lesser increase in equitability are found in mixing zones of adjacent water masses. In extreme conditions diversity is low, whereas equitability is intermediate to high. Modern patterns can be applied to fossil sections, to reconstruct regional paleoceanographic conditions. Thus relatively low Shannon diversity with low equitability in Maastrichtian heterohelicid faunas from El Kef, Tunisia, is interpreted as indicating variable conditions. An increase in simple diversity mostly traces evolution of the heterohelicids as a group, which diversified during the Maastrichtian. The number of species through time is a function of available niches and as such related to oceanic circulation on a global scale. Therefore, when applying modern patterns to fossil sections, a distinction has to be made between global diversity trends and regional environmental change. The correlation between Cenozoic stable isotope record and number of planktic foraminiferal species suggest indeed that simple diversity registers changes in global circulation. Maximum number of species occurred in the Maastrichtian, the Middle Eocene and the early Middle Miocene. In these three instances the maxima are found after the start of a cooling trend and are interpreted as transition periods between two modes of ocean circulation, causing the temporary coexistence of old and new species.Mar. Micropaleontol. 1992 Apr19 1-2'FREE UNIV AMSTERDAM,INST EARTH SCI,CTR GEOMARINE,DE BOELELAAN 1085,1081 HV AMSTERDAM,NETHERLANDS OTTENS JJ FREE UNIV AMSTERDAM,INST EARTH SCI,CTR GEOMARINE,DE BOELELAAN 1085,1081 HV AMSTERDAM,NETHERLANDS>7Times Cited: 7 English Article HU784 MAR MICROPALEONTOLISI:A1992HU78400003 yOGANESYAN., S. A. OGANIN, I. A.Ogilvie, K. W. Ohman, M. D. Ohman, M.D Oliveira, P Olsen, K Olsen, K.OMELCHUK., A. V. Onbe, T. Oschlies, A Oschlies, A. Osgood, K Osgood, K. E.Ostapenko, A.A. Ottens, F. Ottens, J. J. Ottens, J.J Owens, W. B.Ozouf-Costaz, C.stvedt, O. J.Paffenhofer, G. A.Pafort- van Iersel, TParfenyuk, A.V. Parin, N. Parin, N. V Parin, N. V. Parr, A. E Pascoe, P.Passelaigue, FPasselaigue, F. Patching, J.Patching, J.W. Patriti, G Patriti, G. Patzner, R. APatzner, R. A. Paula, J. PAVLOV, A. I PAVLOV, A. I.PAVLOV., A. M.Pearre, Jr. S. Pereira, J Pereira, J.Pereira, J. A. G. Pereira, L. C Pereira_JRCPEROVA., L. I.Pershing, A. J. Pettersson, HPetursdottir, HPetursdottir, H. Prez, J. G. Prs, J. MPfannkuche, O. Philbin, L.M Phillips, R.A Pierce, G. J.Pierrot-Bults, A.CPierrot-Bults, A.C. Pietsch, T. WPietsch, T. W.Pinchukov, M.APinchukov, M.A. Pingree, R.Pingree, R. D. Pingree, R.D Pinho, M. R.Piontkovski, S. A. Planque, B.PODRAZHANSKAYA, S. GPODRAZHANSKAYA., S. G.POLETAEV, V. A. Pollehne, FPOLONSKY, A. SPOLOSIN, A. S.POLYANSKAYA., I. B. Pomroy, A. J. Pomroy, A.J Pond, D. W. POPOVA, M. N POPOVA, M. N.Porteiro, F. M.Porteiro, F.M. Post, A Post, A. Poulet, S. A. Poulicek, M.PRISTAVAKINA, E. I.Proctor, C. A.LIProgram., WMO-ICSU Joint Scientific Committee Global Atmospheric Research Prud'homme van Reine, W. F.PSHENICHNY, B. P.PSHENICHNY., B. P. Queiroga, H. Quro, J. C. Quro, J.-C. Rabouille, C Rabouille, C.Rainbow, P. S. Ramalho, A Ramos, A. RAMOS, J. Ramos, J. A. Ramos, J.A Ramos, J.A. Ramos_JA Rannou, M Rannou, M. Read, J. F. Read, J.F Rees, W. J. Regan, C. T Regan, C. T. Reiner, F. Rey, J. C.Rey, J. C., E. Alot R, L. R, P.Ribera Maycas, E. Rice, A.L. Rice, T. L. Rice, T.L Richard, J Richard, J.Richardson, K. Rieck, W. Riemann, F. Ringelberg, JRobertson, D. R. Robins, D.BRobinson, B. H. Rocha, L. A. Roden, G.IRodhouse, P.G. Roe, H.S.J Rogers, A. D. Rogers, A.D. Roman, M.R.Rosenblatt, R. H. Rossby, T Rossby, T.ROSSOV., V. V. Roule, L Rucabado, J Rucabado, J. RUDENKO, M. VRudenko, M. V. Rudenko, M.V. Ruiz-Pino, D Ruiz-Pino, D. Rundle, A. J. Rundle, A.J.RVACHEV, V. D.RVACHEV., V. D.SAFRONOV, A. M.SAGALEVICH, A. MSagalevich, A.M. Saiz, E. Saldanha, L Saldanha, L. Saltzman, J.SAMAREVA, O. I.SAMOKHVALOV, V. VSanders, R. W. Santos, M. B. Santos, R. S. Santos, R.SSAPRONETSKAYA, N. GSAPRONETSKAYA, N. G.Sargent, J. R.Sarradin, P.-S. Savidge, GSAVVATIMSKY, P. ISAVVATIMSKY, P. I.SAVVATIMSKY., P. I. Sazonov, Yu I Schauer, U Schauer, U. Schiebel, R Schmidt, JSchmitz, W. J. Schreiver, G.Schroeder, W. C Schults, K. Schulz, K. Schut, E.WSedberry, G. RSedberry, G. R. Segonzac, M Segonzac, M. Segonzac, N.SENNIKOV, A. MSennikov, A. M.Sennikov, A.M.SENNIKOV., A. M.SEREBROV, L. ISEREBRYAKOV., V. P.SEREBRYANNIKOV, A. I. Serobaba, II Serpa, J. de Serro, E. Serret, P.Shaboneyev, I. YeShachkov, N. L. Shanks, A. L.SHATOBA, O. E.Shcherbachev, Y. N. Sheader, M.Sheberstov, S. V.Shelbourne, J.E Sheldon, R.W.SHESTOPAL, I. PSHESTOPAL, I. P.SHESTOPAL., I. P.Shevtsov, G.A. SHIBANOV, V.SHIBANOV, V. NSHIBANOV, V. N.SHIBANOV., V. N. SHIMKO, B. P. Shimko, B.P.3radov, M. E.Shushkina, E. A.Anokhina, L. L.& Vereshchaka, A.L Vinogradov, G.M 1999Visual observations of the vertical distribution of plankton throughout the water column above Broken Spur vent field, Mild Atlantic RidgeDeep-Sea Research part I 465 1615-1632W~wHYDROTHERMAL PLUME, ENDEAVOR RIDGE, SCATTERING LAYER, ZOOPLANKTON, MACROPLANKTON, SEA, 29-DEGREES-N, COMMUNITIES, OCEANJCVisual observations were made in September 1997 during the 39 cruise of R/V "Akademik Mstislav Keldysh" with 2 deep-sea manned submersibles "Mir" aboard. During 4 dives the following plankton countings were made: 3 vertical throughout the water column during the day, 2 vertical in the upper 1000 m at night, and 1 oblique in the plume area during the day. Biomass profiles are represented for each dive for all abundant animal groups: copepods, euphausiids + decapods + mysids, chaetognaths, medusae, ctenophores, siphonophores, cyclo-thones, myctophides, radiolarians, and the total zooplankton. Plankton distribution shows 2 aggregations, one within the main pycnocline and the other near the plume; Gelatinous animals and radiolarians dominate in both aggregations by biomass and make a significant contribution to the plankton biomass throughout the water column. Oblique counting indicates the presence of aggregations of animals near the upper and lower borders of the plume and biomass depletion within the plume core. (C) 1999 Published by Elsevier Science Ltd. All rights reserved.lg$f<5Bauchot, M.-L. Iwamoto, T. Geistdoefer, P. Rannou, M.w 1971tude critique des rsultats des expditions scientifiques du "Travailleur" et du "Talisman". Nouvel examen des Macrouridae (Tlostens, Gadiformes)iB;Bulletin du Musum National d'Histoire Naturelle, 3e sries14 Zoologie 14653-669tnSystematics; Checklist; scientific expeditions; cruises; stations; museum collection; history; marine research4-Bauchot, M.-L. Desoutter, M. Castle, P. H. J.t 1993Catalogue critique des types de poissons du Musum National d'Histoire Naturelle(suite). Ordres des Anguilliformes et des Saccopharyngiformess Cybium 17(2)l 91-151,&Checklist; museum collection; catalogsFN25 1545-1561$://0001672240000040@9Beare, D. J. Gislason, A. Astthorsson, O. S. McKenzie, E.iXRAssessing long-term changes in early summer zooplankton communities around Iceland$Ices Journal of Marine Sciencelong-term change; summer zooplankton continuous plankton records; calanus-finmarchicus; time-series; abundance; waters; biomass; northA summary of the Icelandic Spring Survey zooplankton data for May and June is presented for the years 1960-1996, along with time-series information on sea surface temperature. Changes in zooplankton abundance are assessed using displacement volumes and simple index numbers modelled as various functions of temporal (gear) and location (latitude and longitude) covariates. Long-term displaced volumes of zooplankton remained fairly stable although there were pronounced short-term fluctuations. Further, the proportion of specimens in each sample belonging to species with affinities of water of Atlantic type has fallen dramatically over the Icelandic Shelf since the 1960s, whereas the proportion of species with Arctic affinities has increased most markedly northeast of Iceland.ICES J. Mar. Sci. 2000 Dec576'}Dept Agr & Fisheries Scotland, Marine Lab, POB 101,Victoria Rd, Aberdeen AB9 8DD, Scotland Dept Agr & Fisheries Scotland, Marine Lab, Aberdeen AB9 8DD, Scotland Marine Res Inst, IS-121 Reykjavik, Iceland Univ Strathclyde, Dept Stat & Modelling Sci, Glasgow G1 1XH, Lanark, Scotland Beare DJ Dept Agr & Fisheries Scotland, Marine Lab, POB 101,Victoria Rd, Aberdeen AB9 8DD, Scotland:3Times Cited: 0 English Article 406PH ICES J MAR SCIISI:000167224000004 Beckmann, Wk 1988The zooplankton community in the deep bathyal and abyssal zones of the eastern North Atalntic. Preliminary results and data lists from MOCNESS hauls during cruise 08 of the RV" Polarstern".<6Berichte zur Polarforschung, Reports on Polar research42 59 pp.0)Berenboim, B.I., Boytsov, V.D. Lysy, A.Yuo 1992piInfluence of hydrometeorological factors on the population dynamics of arrow squid [Todarodes sagittatus]sB;Hydrometeoropogy and Hydrochemistry of the Seas of the USSRWzs1.Barents Sea. Part 2.Hydrochemical Conditions and Oceanological Bases of Forming up of the Biological Productivity134-136 In Russian Bersch, Mi 1995<5On the circulation of the northesatern North AtlanticrDeep-Sea Research5 part I 42e9a 1583-1607af`DRIFTING BUOYS, SLOPE CURRENT, GULF-STREAM, WATER, OCEAN, DEEP, EXTENSION, CHANNEL, FIELD, RIDGE Along a section from Cape Farvel at the southern tip of Greenland to the Porcupine Bank off the Irish coast (WOCE section A1E/AR7E), obtained in September 1991, geostrophic velocities were calculated from CTD measurements and referenced to velocities recorded by an Acoustic Doppler Current Profiler (ADCP) in the upper 500 m. The mean accuracy of the absolute geostrophic velocities is estimated at +/-3.6 cm/s, which is comparable to that resulting from the assumption of a layer of no motion. The derived flow field is essentially columnar without a pronounced layer of no motion. Maximum velocities of 20-30 cm/s occur in the upper 1000 m of the East Greenland Current and the Porcupine slope current and at 2000 m depth in the Denmark Strait overflow. The meandering of the Irminger Current crossing the Reykjanes Ridge and an enhanced mesoscale variability along the Rockall Plateau and in the Rockall Trough are indicated. Compared to Schmitz and McCartney (1993) the estimated volume transports suggest an intensified meridional circulation with an increased supply from the subtropics to the Subpolar Mode Water (SPMW) and an increased entrainment of SPMW into the deeper layers. In the bottom layer with densities sigma(theta) greater than or equal to 27.80 kg/m(3) a reduced circulation of lceland-Scotland Overflow Water (ISOW) in the Irminger Basin and a recirculation of ISOW in the Iceland and West European basins are found. About 12 Sv of bottom water are transported southwards and join the Deep Western Boundary Current.Bersch,M Meincke,J Sy,A 1999PIInterannual thermohaline changes in the northern North Atlantic 1991-1996iDeep-Sea Researchf part II 46 55-75SEA-SURFACE TEMPERATURE, INTERPENTADAL VARIABILITY, WIND STRESS, OCEAN, SALINITY, CLIMATE, WATER, CIRCULATION, HYDROGRAPHY, OSCILLATIONIn the period 1991-1996 the WOCE hydrographic section A1E/AR7E between Greenland and Ireland was repeated five times. The observed thermohaline changes altered the baroclinic structure along the eastern margin of the subpolar gyre significantly, Between June 1995 and August 1996 an overall increase of the temperature and thickness and a decrease of the density of the Subpolar Mode Water (SPMW) layer were observed, accompanied by an increase of its salinity east of the Reykjanes Ridge and a decrease of its salinity in the Irminger Sea. The changes were most pronounced in the Iceland Basin, where the Subarctic Front retreated westwards, coinciding with a strong weakening of the Westerlies as determined by the North Atlantic Oscillation, They are related to a local reduction of the Ekman upwelling and the ocean-to-atmosphere heat flux on the one hand and to the advection of anomalies from the subtropics on the other hand. The eastward spreading of the different Labrador Sea Water (LSW) vintages led to a corresponding cooling of the LSW in the Irminger Sea and in the Iceland Basin in the period 1991-1996. The renewal of the LSW in the Rockall Trough occurred more sporadically, indicating that the North Atlantic Current (NAC) impedes the southward spreading of LSW in the eastern Atlantic. The changes in 1996 seem to have also counteracted this spreading. (C) 1999 Elsevier Science Ltd. All rights reserved."Bersch, M., J. Meincke A. Sy 1999PIInterannual thermohaline changes in the northern North Atlantic 1991-1996PDeep-Sea Research II46 1-24 55-75s Bethoux, N.t 1992f`Ocanographie et mtorologie, de S. A. S. le Prince Albert Ier S. A. S le Prince Rainier III. *#Saldanha, L. R, P. Martins, A. F.iyCentenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L'Hirondelle. Aoreana Supl. 73-82h H T155-161$://A1991FX12200001"Bollens, S. M. Frost, B. W.1voOvigerity, Selective Predation, and Variable Diel Vertical Migration in Euchaeta-Elongata (Copepoda, Calanoida)a Oecologia '2,UNIV WASHINGTON,SCH OCEANOG,SEATTLE,WA 98195ovigerity; selective predation; diel vertical migration; zooplankton; euchaeta-elongata planktonic copepod; marine copepod; lepomis-macrochirus; calanus-pacificus; prey selection; daphnia; eggs; lake; size; reproductionrWe present a statistical analysis of a previously published (Yen, 1983) but heretofore unanalyzed data set on the vertical distributions and diel vertical migration (DVM) of adult females of the marine planktonic copepod Euchaeta elongata in Dabob Bay, Washington, USA. Non-ovigerous females were strongly migratory on all four dates sampled, residing between 75-175 m during the day and at shallower depths during the night, commonly entering the upper 50 m of the water column. In contrast, ovigerous females were non-migratory or weakly migratory, largely remaining between 100-175 m both day and night, and entering the upper 50 m of the water column only rarely. Thus non-ovigerous females always migrated much more strongly, as measured by both amplitude of migration and the proportion of animals migrating, than did ovigerous females. These results led us to hypothesize that differential susceptibility to visually orienting predators was the cause of these differences in DVM behavior in female E. elongata, and we subsequently undertook an experimental study of the feeding selectivity of the copepod's natural predator, Pacific herring (Clupea harengus pallasi). Pacific herring exhibited a highly significant preference for ovigerous over non-ovigerous adult female E. elongata. The demographic consequences of variable DVM in adult female E. elongata were investigated by way of life table analyses. Results indicated that under conditions of thermal stratification of the water column there is a distinct demographic disadvantage (reduced rate of realized population growth) incurred by non-migratory or weakly migratory ovigerous females due to delayed egg development at cooler subsurface temperatures. We conclude that ovigerous female E. elongata remain at depth both day and night to avoid visually orienting predators, and that such behavior must afford the copepod a demographic advantage of no less than a 26% reduction in adult mortality to offset the demographic cost of delayed egg development. Oecologia 19918726/Times Cited: 26 English Article FX122 OECOLOGIAISI:A1991FX12200001.(Bollens,S.M Osgood,K Frost,B.W Watts,S.D 1993Vertical distributions and susceptibilities to vertebrate predation of the marine copepods Metridia lucens and Calanus pacificusLimnol. Oceanogr. 388} 1827-1837s555-564$://A1994NM09500009t0*Bollens, S. M. Frost, B. W. Cordell, J. R.zChemical, Mechanical and Visual Cues in the Vertical Migration Behavior of the Marine Planktonic Copepod Acartia-Hudsonica"Journal of Plankton Researchgasterosteus-aculeatus; 3-spined sticklebacks; calanoid copepods; daphnia-hyalina; 1st antennae; zooplankton; fish; prey; predation; fieldRecent experimental evidence in both marine and freshwater systems indicates that predators can induce vertical migration behavior in individual zooplankters, yet the specific cues by which zooplankters sense their predators appear to vary. In situ manipulation experiments were carried out with enclosed populations of the marine planktonic copepod Acartia hudsonica to re-examine the potential role of chemical cues in the behavior of A.hudsonica, and to test explicitly for the role of mechanical or visual stimuli in triggering vertical migration behavior in this species. Adult female copepods were induced to vertically migrate (descend) when exposed to fish mimics during the day, but no such response occurred when the copepods were exposed to fish mimics during the night. Moreover, copepods exhibited no changes in vertical distribution when exposed to water which, having recently held a natural predator (the threespine stickleback, Gasterosteus aculeatus), was presumed to be laden with predator-produced chemical exudates. Predator- mediated mechanical or visual cues, or a hierarchy of both, are responsible for eliciting vertical migration behavior in adult female A.hudsonica. These results, together with those of other investigations demonstrating the inducing role of chemical exudates. indicate that the stimuli eliciting vertical migration in zooplankton can be expected to vary between species.oJ. Plankton Res. 1994 Maya165a'WOODS HOLE OCEANOG INST,DEPT BIOL,WOODS HOLE,MA 02543 UNIV WASHINGTON,SCH OCEANOG,SEATTLE,WA 98195 UNIV WASHINGTON,FISHERIES RES INST,SEATTLE,WA 98195 BOLLENS SM WOODS HOLE OCEANOG INST,DEPT BIOL,WOODS HOLE,MA 02543o:4Times Cited: 30 English Article NM095 J PLANKTON RESISI:A1994NM09500009l"Bolten, A. B. Martins, H. R. 1990*$Kemp's ridley captured in the AzoresMarine Turtle Newsletter4823HBBolten, A. B. Martins, H. R. Bjorndal, K. A. Cocco, M. Gerosa, G. 1992h8Caretta caretta (loggerhead) pelagic movement and growthHerpetological Review23 116>8Bolten, A. B. Martins, H. R. Bjorndal, K. A. Gordon, J. 1993sSize distribution of pelagic-stage loggerhead sea turtles (Caretta caretta) in the waters around Azores and Madeira;J ArquiplagoLife and Marine Sciences 11A 49-54Borodin, N. A. 1931$North-Atlantic deep-sea fishesD=Bulletin of the Museum of Comparative Zoology, Havard Collegef 72(3)s 55-89ijcSystematics; diagnosis; Checklist; anatomy; meristics; morphometry; scientific expeditions; cruises ji<hgfe zB 485-499$://000088446400011IB;Gebruk, A. V. Southward, E. C. Kennedy, H. Southward, A. J.f`Food sources, behaviour, and distribution of hydrothermal vent shrimps at the Mid-Atlantic RidgeHBJournal of the Marine Biological Association of the United Kingdomrimicaris-exoculata; marine-invertebrates; isotope composition; bresiliid shrimps; caridean shrimp; stable-carbon; fatty-acids; decapoda; field; communities(!Five species of bresilioid shrimp were investigated at seven hydrothermal sites on the Mid-Atlantic Ridge: Menez Gwen, Lucky Strike, Rainbow, Broken Spur, TAG, Snake Pit and Logatchev. Samples were prepared for analysis of stable isotopes, elemental composition and lipids. Shrimp behaviour was observed from the submersible 'Alvin' and in the laboratory aboard RV 'Atlantis'. The distribution and zonation of the shrimp species was recorded. Juvenile shrimp of all species arrive at the vents carrying reserves of photosynthetic origin, built-up in the pelagic larval stages. These reserves are used while the shrimp metamorphose to the adult form and, in Rimicaris exoculata and Chorocaris chacei, while they develop epibiotic bacteria supporting structures, the modified mouthparts and the inside of the carapace. The main food of adult R. exoculata is filamentous bacteria that grow on these structures. The intermediate sizes of C. chacei also feed on such bacteria, but the final stage gets some food by scavenging or predation. Mirocaris species scavenge diverse sources; they are not trophically dependent on either R. exoculata or mussels. Adults of Alvinocaris markensis are predators of other vent animals, including R. exoculata. The dense swarms of R. exoculata, with their exosymbionts, can be compared to endosymbiont-containing animals such as Bathymodiolus and the vestimentiferan tube- worms of the Pacific vents. Such associations, whether endo- or ectosymbiotic, may be necessary for the development of flourishing communities at hydrothermal vents. J. Mar. Biol. Assoc. U.K. 2000 Jun803'Marine Biol Assoc United Kingdom Lab, Citadel Hill, Plymouth PL1 2PB, Devon, England Marine Biol Assoc United Kingdom Lab, Plymouth PL1 2PB, Devon, England Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117851, Russia Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Anglesey, Wales Southward AJ Marine Biol Assoc United Kingdom Lab, Citadel Hill, Plymouth PL1 2PB, Devon, England>7Times Cited: 2 English Article 338WN J MAR BIOL ASSN UKISI:000088446400011Genin, A. Boehlert, G.W. 1985b[Dynamics of temperature and chlorophyll structures above a seamount: an oceanic experiment.h Journal of Marine Research43907-924 151-&$://A1988M800100001("Genin, A. Haury, L. Greenblatt, P.yInteractions of Migrating Zooplankton with Shallow Topography - Predation by Rockfishes and Intensification of Patchiness<6Deep-Sea Research Part a-Oceanographic Research Papers 1988 Feb352'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093 USN,CTR OCEAN SYST,SAN DIEGO,CA 92152 UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093JCTimes Cited: 42 English Article M8001 DEEP-SEA RES PT A-OCEANOG RESISI:A1988M800100001("Genin, A. Haury, L. Greenblatt, P. 1988~xInteractions of migrating zooplankton with shallow topography: predation by rockfishes and intensification of patchinessDeep-Sea Research,352o151-175d]Genin, A. Greene, C. Haury, L. Wiebe, P. H. Gal, G. Kaartvedt, S. Meir, E. Fey, C. Dawson, J. 1994NGZooplankton patch dynamics: daily gap formation over abrupt topography.rDeep-Sea Research I41941-9519&GEORGIEV, V. T., I. I. SVETLOV.r 1989|Peculiarities of thermohaline and dynamic structure of waters of the deepwater eminence Hekate on the North-Atlantic Ridge:4 Problems of fishery oceanography of the North Basin 44-525 in Russian GERBER, E. M.. 1993ngSome data on distribution and biology of blue whiting Micromesistus poutassou on the Mid-Atlantic RidgeVoprosy ikhtiologii- 33(1)d 61-65l in Russian60GEVORKJAN, V. H. T. E. VASILIEVA, R. V. KASABOV. 1982lfProcesses of sedimentation and morphology of underwater mountains and eminencies of the North Atlantic 59 ppp in Russian4.GEVORKJAN, V. H. I. E. LOMAKIN A. V. OMELCHUK. 1986hbGenesis of detrital rocks of the North-West Atlantic and geological position of the Azores PlateauTN Complex investigation of the open part of the Atlantic Ocean. Selected papers 98-1010 in Russian^WGEVORKJAN, V. H. Yu. V. TRETYACHENKO A. I. SEREBRYANNIKOV I. E. LOMAKIN V. N. SHIBANOV.l 1987Studying of relationship between substantial composition of fish otoliths and bottom sediments of some fishing grounds of the north Atlantic(! Meeting of Soviet oceanographerss61 in RussianD>GEVORKJAN, V. H. Yu. G. A. L. SOROKIN G. I. LUKA A. M. PAVLOV. 1990@:Geological aspects of biological productivity of the oceanMurmansk192 pp.p in Russian Girard, A. A. 1892:3Les Cphalopodes des les Aores et de l'le MadrerF@Journal de Sciencias Mathematicas, Physicas e Naturaes, 2 srie2-7i210-221f ~v 2+Nash, R. D. M. Santos, R. S. Hawkins, S. J.  1994NGDiel fluctuations of a sandy beach fish assemblage at Porto Pim, Azores ArquiplagoLife and Marine Sciences 12A 75-86NAZIMOV, V. V. 1972f_Fisheries conditions in dependence on the structure of the northern part of the Reykjanes Ridge6d^Conference of young scientists of PINRO by results of investigations in 1971. Theses of papers 3-4 in Russian NAZIMOV, V. V 1977<5Structure of the northern part of the Reykjanes Ridge"Priroda i khozayistvo Severa 6 96-97 in Russian293-300$://0001660349000054-Negre-Sadargues, G. Castillo, R. Segonzac, M.Carotenoid pigments and trophic behaviour of deep-sea shrimps (Crustacea, Decapoda, Alvinocarididae) from a hydrothermal area of the Mid-Atlantic RidgeTNComparative Biochemistry and Physiology a-Molecular and Integrative Physiologycarotenoid; deep-sea shrimps; hydrothermal site; metabolism; origin; pigments; trophic behaviour rimicaris-exoculata; penaeus-japonicus; vent shrimps; metabolism; prawn; bresiliidae; morphology; eyePigments and trophic behaviour of three species of Alvinocarididae from a Mid-Atlantic hydrothermal site were analysed. Carotenoid pigments are responsible for the more or less marked colouration of these animals. The carotenoid content of whole animals and different tissues were evaluated. Rimicaris exoculata exhibits an increased carotenoid level at the juvenile stage, while Chorocaris chacei and Alvinocaris maskensis contain only few traces of pigment. Free and esterified astaxanthin, reported for most pelagic crustaceans, are present in these deep-sea shrimps. The origin of carotenoids of crustaceans living in the aphotic zone is discussed. (C) 2000 Elsevier Science Inc. All rights reserved.6/Comp. Biochem. Physiol. A-Mol. Integr. Physiol. 2000 Nov 1273',%Univ Montpellier 2, Lab Ecophysiol Invertebres, F-34095 Montpellier 5, France Univ Montpellier 2, Lab Ecophysiol Invertebres, F-34095 Montpellier 5, France IFREMER, CENTOB, F-29280 Plouzane, France Negre-Sadargues G Univ Montpellier 2, Lab Ecophysiol Invertebres, F-34095 Montpellier 5, FranceD>Times Cited: 0 English Article 385ZK COMP BIOCHEM PHYSIOL PT AISI:000166034900005 Neill,W.E 1992^XPopulation variation in the ontogeny of prtedator-induced vertical migration of copepods Nature 3569 54-57- Nesis, K.N. 1973XQTaxonomy, phylogeny and evolution of squids of the family Gonatidae (Cephalopoda)lZoologichesky Zhurnalp 52(11) 1626-1638r&In Russian with English summary Nesis, K.N.p 1973<5Ecological classification (life forms) of cephalopodseItogi Nauki i Tekhniki Nesis, K.N.  1979>7Squid larvae of the family Ommastrephidae (Cephalopoda)o"Zoologichesky Zhurnal, 58(l) Nesis, K.N. 1982<5Abridged Manual to the Cephalopods of the World Ocean4-Moscow: Legkaya i Pishchevaya Promyshlennost' 356 p) In Russian"Nesis, K.N. Sagalevich, A.M. 1983<6Deep-water octopods from the porthole of a submersible Priroda, 19838 No. 11"Nesis, K.N. Sagalevich, A.M. 1983<6Deep-water octopods from the porthole of a submersiblePriroda No. 11 23-25 In Russian Nesis, K.N.p 1984 Cephalopods$ Field Card Manual of PlanktonNGPart 3. Leningrad: Zoological Institute of the USSR Academy of Sciences 182 pages. In Russiannd an evaluation of its systematic positionn"Journal of Zoology of London 190225-239W Markle, D. F J.-C. Quro  1986>7Fishes of the North-east Atlantic and the Mediterranean UNESCO Vol. I228-253T Marshall, N. B T. Iwamoto  1973*$Fishes of the Western North AtlanticRLSix Memoir- Sears Foundation for Marine Research, Yale University, New Haven Number One446-665"Martin, A. R. Melo, A. M. A. 1983B$Journal of Crustacean Biology52294-305<0400010 Krause, D. C. Angel, M. V.<6Marine Biogeography, Climate-Change and Societal NeedsProgress in Oceanography:4doppler current profiler; abundance; patterns; waterPelagic biogeography deals with the large scale distributional patterns of pelagic organisms in the woKoppelmann,R Weikert, Hl 1999|vTemporal changes of deep-sea mesozooplankton abundance in the temperate NE Atlantic and estimates of the carbon budget$Marine Ecology Progress Series 179 27-40NE Atlantic, deep-sea zooplankton, temporal changes, carbon requireme BIOGENIC PARTICLE FLUXES, BENTHIC BOUNDARY-LAYER, SPATIAL VARIABILITY, OXYGEN-CONSUMPTION, NORTH-ATLANTIC, SEDIMENT TRAP, INSITU RATES, PHOTOGRAPHIC EVIDENCE, CALANUS-FINMARCHICUS, MARINE PHYTOPLANKTONFull-depth spring and summer vertical profiles of mesozooplankton numbers and biomass were obtained with a 1 m(2) multiple opening/closing net and environmental sensing system (MOCNESS) from the BIOTRANS (biological vertical transport and energetics in the benthic boundary layer of the deep sea) study area (47 degrees N, 20 degrees W) in the temperate NE Atlantic in 1992. Mesozooplankton abundance was high in spring and less in summer in the upper 750 m. Between 750 and 1050 m differences between these seasons could not be detected. In the upper bathypelagic zone, between 1050 and 2250 m, where abiotic fluctuations are minor, both mesozooplankton biomass and numbers were significantly higher in summer compared to spring. Samples from summer 1989 fitted this pattern. Calanoid copepods of the genus Metridia were the main contributors; most of the major zooplankton groups, though playing a subsidiary role, also showed a significant increase in summer in the upper bathypelagic zone. The increase probably was due to the large transient input of detrital material, which regularly occurred in the course of the phytoplankton spring bloom in the area investigated and may have stimulated the onset of reproduction in the bathypelagic zone. Temporal changes in mesozooplankton abundance could not be detected below 2250 m depth. Metabolic carbon requirements of mesozooplankton, calculated from ETS (electron transport system) data, increased in the bathypelagic zone (1000 to 4250 m) from 1.61 mg C m(-2) d(-1) in spring to 4.12 mg C m(-2) d(-1) in summer. The carbon respired by the bathypelagic micro- and mesozooplankton in summer, based on an assumed spring bloom area of 50 000 km(2), was 893 t C d(-1) as a minimum estimate, which was higher than in spring by a factor of 2.6.i KOPTEV, A. V.e 1984PJSome data on sound scattering layers in the area of the Mid-Atlantic Ridge~x Problems of studying and rational exploitation of biological resources of seas of the European North and North Atlantic 8-9 in Russian Korzun, Yu.V 1976<6Teuthofauna of northern part of the Mid-Atlantic RidgeUnpublished MS ThesisuTNKaliningrad, Kaliningrad Technical Institute of Fishery and Fishery Management 72 p In Russian Korzun, Yu.V.  1976<6Teuthofauna of northern part of the Mid-Atlantic RidgeleUnpublished MS Thesis. Kaliningrad, Kaliningrad Technical Institute of Fishery and Fishery Management4 72 p.E In RussianRKKorzun, Yu.V. Nesis, K.N. Nigmatullin, Ch.M. Ostapenko, A.A. Pinchukov, M.Ao 1979XQNew data on the distribution of squids, family Ommastrephidae, in the World Ocean Okeanologiya 19(4)p729-733i&In Russian with English summaryVOKoslow, J.A. Boehlert, G.W. Gordon, J.D.M. Haedrich, R.L. Lorance, P. Parin, N. 1999JCThe impact of fishing on Continental slope and Deep-sea ecosystems.:3SCOR Symposium on the Ecosystem Impacts of Fishing. Montpellier, France$ICES Journal of Marine Science16-19 March, 1999KOTENEV, B. N. 1968>7Marine geological investigations in the area of Icelandf Okeanologiya  8(6)o 1049-1052p in Russian zNn*$Lloris, D. Rucabado, J. Figueroa, H. 1991{Biogeography of the Macaronesian ichthyofauna (The Azores, Madeira, the Canary islands, Cape Verde and the African enclave)a,%Boletim do Museu Municipal do Funchal43 234:191-241JDLOGVINENKO, B. M. G. N. NEFEDOV L. M. MASSALSKAYA I. B. POLYANSKAYA. 1983f`Populational analysis of grenadier by genetic polymorphism of non-specific esterases and myogens Genetics of commercial fishes and objects of aquaculture. Materials of the union conference on genetics, selection and hybridization of fishese 29-343 in RussianLOKTIONOV, Yu. A.S 1981Some features of mezo-scaled variability of hydrological characteristics south of the subpolar front above the North-Atlantic Ridge}Spatial and temporal variability of hydrometeorological conditions in the fishing grounds of the Atlantic Ocean. Kaliningrad.e  21-27 in RussianLOKTIONOV, Yu. A.S 1984Fluctuations of temperature as a factor of changeability of flows of the intermediate layer of water in the fishing grounds above the North-Atlantic Ridge$Abstract of the Doctor Thesisa  22 pp in RussianLOKTIONOV, Yu. A.E 1986The North-Atlantic Ridge(" Fisheries oceanography. 286-287 in RussianB://A1994PZ967000111>7Hays, G. C. Proctor, C. A. John, A. W. G. Warner, A. J.1}Interspecific Differences in the Diel Vertical Migration of Marine Copepods - the Implications of Size, Color, and Morphologyr Limnology and Oceanography'LFSIR ALISTER HARDY FDN OCEAN SCI,THE LAB,PLYMOUTH PL1 2PB,DEVON,ENGLAND"zooplankton; predation; fishSamples collected by continuous plankton recorders (CPRs) between 1948 and 1992 were used to describe the diel vertical migration (DVM) behavior of 41 copepod taxa in the northeast Atlantic between 45 and 55 degrees N and 11 and 31 degrees W. A total of 13,622 samples, each representing similar to 18.5 km (10 nm) of tow, were analyzed. Since CPRs are towed in near- surface waters, taxa that exhibit DVM occur predominantly in samples taken at night. Larger taxa showed significantly stronger DVM, with body size explaining 47% of the intertaxa variation in DVM. For small taxa (<1 mm wide) the residual variation in DVM was correlated with carotenoid pigment levels but not with body morphology, with more heavily pigmented taxa exhibiting DVM. For larger taxa (>1 mm wide) the residual variation in DVM was correlated with body morphology but not with carotenoid pigment levels, with more elongate copepods not exhibiting DVM.Limnol. Oceanogr. 1994 Nov397<5Times Cited: 23 English Article PZ967 LIMNOL OCEANOGRISI:A1994PZ96700011469-475$://A1995RE86200002a.(Hays, G. C. Warner, A. J. Proctor, C. A.Spatiotemporal Patterns in the Diel Vertical Migration of the Copepod Metridia-Lucens in the Northeast Atlantic Derived from the Continuous Plankton Recorder Survey Limnology and Oceanography'TMSIR ALISTER HARDY FDN OCEAN SCI,THE LABORATORY,PLYMOUTH PL1 2PB,DEVON,ENGLANDb>8calanus-finmarchicus; zooplankton; predation; bloom; seanhThe archived data set collected over a 45-yr period (1948-1992) by Continuous Plankton Recorders (CPRs) towed in near-surface waters was used to investigate the diel vertical migration of the copepod Metridia lucens in the northeast Atlantic (47-63 degrees N and 10-30 degrees W). Although the CPR sampling intensity was uniform during the day and the night, M. lucens was caught predominantly in samples collected at night, consistent with a normal diel vertical migration pattern involving movement from greater depth during the day to shallower depths at night. The length of time spent near the surface varied seasonally and was closely correlated (r(2) = 0.80) with seasonal change in length of night. The residual variation in length of time spent at the surface was nonrandom, with more time being spent at the surface in spring before the onset of the spring bloom, and less time being spent at the surface in autumn, than that predicted from the length of night at these periods. The timing of this enhanced near-surface occupation in spring varied with latitude, occurring a mean of 3.4 d later per degree of latitude.Limnol. Oceanogr.  1995 Mayf403t:4Times Cited: 6 English Article RE862 LIMNOL OCEANOGRISI:A1995RE86200002a 1601-1615$://A1996WD66700003 Hays, G. C.LELarge-scale patterns of diel vertical migration in the north Atlantic <6Deep-Sea Research Part I-Oceanographic Research Paperscontinuous plankton recorder; filtration efficiency; adaptive significance; nitrogen flux; upper ocean; copepod; zooplankton; variability; avoidance; speed ,%Samples historically collected and analysed by the Continuous Plankton Recorder (CPR) survey in the North Atlantic were used to examine large-scale spatial patterns in both the normal diel vertical migration (normal DVM) behaviour and the mean body size within epi-pelagic copepod communities. Normal DVM was most marked in the northwest Atlantic and less marked in the northeast Atlantic and in shallow coastal areas such as around the U.K. and on the Grand Banks of Newfoundland. These patterns of normal DVM were strongly correlated with patterns of mean body size, with normal DVM being more marked in those areas where larger species predominated. In both the northwest and northeast Atlantic, marked seasonal changes occurred in the migrating biomass. In the northwest Atlantic, Euchaeta norvegica and Calanus finmarchicus were the most important contributors to the total migrating biomass, while in the northeast Atlantic the most important contributors were E. norvegica, Metridia lucens and Pleuromamma robusta. Copyright (C) 1996 Elsevier Science Ltd.(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1996 Oct4310HBTimes Cited: 6 English Article WD667 DEEP-SEA RES PT I-OCEANOG RESISI:A1996WD66700003 85-92$://000071269300007n,%Hays, G. C. Warner, A. J. Tranter, P.tzWhy do the two most abundant copepods in the North Atlantic differ so markedly in their diel vertical migration behaviour?Journal of Sea Research North Atlantic; diel vertical migration; copepod; Metridia; Calanus; CPR plankton recorder survey; calanus-pacificus; marine copepods; metridia-lucens; zooplankton; predation; fish; distributions; population; selection A total of 55 113 plankton samples, collected between 1948 and 1992 in the North Atlantic by the Continuous Plankton Recorder (CPR) survey, were used to show that normal diel vertical migration (NDVM) behaviour was far more marked in the copepod Metridia lucens than in the copepod Calanus finmarchicus. These two species are of similar size and pigmentation, but differ in morphology, with C. finmarchicus being the more elongate. To examine whether this variation in morphology might be linked to the observed difference in NDVM behaviour, both body morphology and NDVM behaviour were quantified for a further five similar sized copepod species (Pleuromamma robusta, P. abdominalis, C. helgolandicus, C. glacialis and Neocalanus gracilis). NDVM behaviour was significantly less marked in the more elongate species. It is suggested that the more elongate species have a faster avoidance speed from predators, which leads to a lower susceptibility to predation and consequently these species do not need to exhibit marked NDVM behaviour.l J. Sea Res. 1997 Dec38 1-24.Times Cited: 4 English Article YP362 J SEA RESISI:000071269300007951-961$://000166204500015a:3Hays, G. C. Clark, D. R. Walne, A. W. Warner, A. J.J\VLarge-scale patterns of zooplankton abundance in the NE Atlantic in June and July 1996@9Deep-Sea Research Part Ii-Topical Studies in Oceanography|ueastern north-atlantic; plankton distribution; c-helgolandicus; frontal area; finmarchicus; calanus; sea; environmenttThe abundance of various mesozooplankon taxa was measured in the NE Atlantic (36-64 degreesN and 15-24 degreesW) during June and July 1996 using a high-speed plankton sampler, the U-Tow. A total of 225 plankton samples were collected, each representing about 16.5 km of tow. The abundance of mesozooplankton during 1996 was compared to the data that have been collected historically in this region by the Continuous Plankton Recorder (CPR) survey. The abundance of Calanus in 1996 was well below the long-term mean. For fish larvae, euphausiids and amphipods there was a distinct peak in abundance around 49-50 degreesN associated with frontal features, but elsewhere levels of abundance were again generally below the long-term mean. (C) 2001 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 200148 4-5HBTimes Cited: 2 English Article 388VV DEEP-SEA RES PT II-TOP ST OCEISI:000166204500015 h; B`.'Hays,G.C Clark,D.R Walne,A.W Warner,A.Je 2001\VLarge-scale patterns of zooplankton abundance in the NE Atlantic in June and July 1996Deep-Sea Research, part II 48951-961}|uEASTERN NORTH-ATLANTIC, PLANKTON DISTRIBUTION, C-HELGOLANDICUS, FRONTAL AREA, FINMARCHICUS, CALANUS, SEA, ENVIRONMENTThe abundance of various mesozooplankon taxa was measured in the NE Atlantic (36-64 degreesN and 15-24 degreesW) during June and July 1996 using a high-speed plankton sampler, the U-Tow. A total of 225 plankton samples were collected, each representing about 16.5 km of tow. The abundance of mesozooplankton during 1996 was compared to the data that have been collected historically in this region by the Continuous Plankton Recorder (CPR) survey. The abundance of Calanus in 1996 was well below the long-term mean. For fish larvae, euphausiids and amphipods there was a distinct peak in abundance around 49-50 degreesN associated with frontal features, but elsewhere levels of abundance were again generally below the long-term mean. (C) 2001 Elsevier Science Ltd. All rights reserved. 53-73$://0000861154000062,Head, E. J. H. Harris, L. R. Campbell, R. W.Investigations on the ecology of Calanus spp. in the Labrador Sea. I. Relationship between the phytoplankton bloom and reproduction and development of Calanus finmarchicus in spring$Marine Ecology-Progress SeriesCalanus finmarchicus; reproduction; spring bloom; Labrador sea seasonal development; egg-production; st-lawrence; zooplankton; waters; abundance; copepod; iceland; cycle; stratification yDuring mid-May-early June 1997 observations of hydrography, phytoplankton and nitrate concentrations, and abundance and stage distribution of Calanus finmarchicus populations were made in the Labrador Sea and south of Greenland. Egg production rates were also measured for isolated C. finmarchicus females. Surface nitrate and integrated phytoplankton concentrations indicated that, in the deep water, the phytoplankton bloom had ended in the north and east, was in progress in the north central Labrador Sea and near the basin margins, and had not yet become established in an area stretching from the central Labrador Sea to the south of Greenland. C. finmarchicus egg production rates and stage distributions at stations in the 3 areas designated as early, mid- and late/post-bloom zones, suggested that development rates of the overwintered GO generation into mature adults (females and males) were probably low before the bloom, but accelerated during its development. Individual and areal rates of egg production were highest in the early bloom zone, whereas nauplii were more abundant in the bloom and late/post-bloom zones. Differences in naupliar abundance may have been related to food Limitation, or predation. Following development through to the young copepodite stages (CI-III), which were most abundant in the late/post-bloom zone, morality rates were apparently lower and growth rates less dependent on high phytoplankton concentrations and perhaps more dependent on temperature. In the Labrador Sea, where the annual growth season is relatively short and C, finmarchicus produces only 1 generation per year, the timing of the spring bloom may have a significant impact on recruitment of the new year's generation. In areas where the bloom is early and intense, maturation of the overwintered adults will be rapid and egg-laying will occur when phytoplankton concentrations are high. Subsequent survival success of eggs through to later stages will also probably be relatively high and individuals from the new year's generation will have ample time to reach stages capable of overwintering. By contrast, if the bloom is late or of low intensity, adult maturation will be delayed and egg-laying may occur when phytoplankton concentrations are low. Under these conditions relatively few eggs may survive and individuals that do survive will have a shorter period in which to attain stages which can overwinter.Mar. Ecol.-Prog. Ser. 2000 193'60Bedford Inst Oceanog, Ocean Sci Div, Dept Fisheries & Oceans, POB 1006, Dartmouth, NS B2Y 4A2, Canada Bedford Inst Oceanog, Ocean Sci Div, Dept Fisheries & Oceans, Dartmouth, NS B2Y 4A2, Canada Head EJH Bedford Inst Oceanog, Ocean Sci Div, Dept Fisheries & Oceans, POB 1006, Dartmouth, NS B2Y 4A2, Canada>7Times Cited: 2 English Article 298AA MAR ECOL-PROGR SERISI:000086115400006("Head,E.J.H Harris,L.R Campbell,R.W 2000Investigations on the ecology of Calanus spp. in the Labrador Sea.I.Relationship between the phytoplankton bloom and reproduction and development of Calanus Finmarchicus in springW$Marine Ecology Progress Series 193 53-.73Calanus finmarchicus, reproduction, spring bloom, Labrador sea SEASONAL DEVELOPMENT, EGG-PRODUCTION, ST-LAWRENCE, ZOOPLANKTON, WATERS, ABUNDANCE, COPEPOD, ICELAND, CYCLE, STRATIFICATION  yDuring mid-May-early June 1997 observations of hydrography, phytoplankton and nitrate concentrations, and abundance and stage distribution of Calanus finmarchicus populations were made in the Labrador Sea and south of Greenland. Egg production rates were also measured for isolated C. finmarchicus females. Surface nitrate and integrated phytoplankton concentrations indicated that, in the deep water, the phytoplankton bloom had ended in the north and east, was in progress in the north central Labrador Sea and near the basin margins, and had not yet become established in an area stretching from the central Labrador Sea to the south of Greenland. C. finmarchicus egg production rates and stage distributions at stations in the 3 areas designated as early, mid- and late/post-bloom zones, suggested that development rates of the overwintered GO generation into mature adults (females and males) were probably low before the bloom, but accelerated during its development. Individual and areal rates of egg production were highest in the early bloom zone, whereas nauplii were more abundant in the bloom and late/post-bloom zones. Differences in naupliar abundance may have been related to food Limitation, or predation. Following development through to the young copepodite stages (CI-III), which were most abundant in the late/post-bloom zone, morality rates were apparently lower and growth rates less dependent on high phytoplankton concentrations and perhaps more dependent on temperature. In the Labrador Sea, where the annual growth season is relatively short and C, finmarchicus produces only 1 generation per year, the timing of the spring bloom may have a significant impact on recruitment of the new year's generation. In areas where the bloom is early and intense, maturation of the overwintered adults will be rapid and egg-laying will occur when phytoplankton concentrations are high. Subsequent survival success of eggs through to later stages will also probably be relatively high and individuals from the new year's generation will have ample time to reach stages capable of overwintering. By contrast, if the bloom is late or of low intensity, adult maturation will be delayed and egg-laying may occur when phytoplankton concentrations are low. Under these conditions relatively few eggs may survive and individuals that do survive will have a shorter period in which to attain stages which can overwinter.v0391-400$://A1992JJ78700007r Huang, C. Uye, S. Onbe, T.Ontogenic Diel Vertical Migration of the Planktonic Copepod Calanus-Sinicus in the Inland Sea of Japan .2. Late Fall and Early SpringZMarine Biology*$celtic sea; pacificus; helgolandicusThe ontogenetic diel vertical migration of the planktonic copepod Calanus sinicus was investigated in the Inland Sea of Japan in November 1988 and March 1989, when the water temperature was weakly stratified in a reversed manner. In both investigations a pronounced ontogenetic difference in vertical distribution was found. Spawning always occurred during nighttime, being confined to the upper 40 m water column in November but to the layer below 35 m in March. The distribution of pre-feeding nauplius stages, NI and NII, was more or less similar to that of the eggs. The first-feeding NIII performed a marked upward migration, and late nauplius stages (NIV to NVI) and early copepodite stages (CI and CII) continuously aggregated in the upper water column where phytoplankton was abundant. CIII to CVI (adult female and male) tended to disperse in the whole water column. In November, however, they avoided the upper 10 m strata during daytime and some individuals migrated upward to the surface during nighttime. In March, CV and CVI aggregated in the layer between 5 and 15 m deep in the daytime and migrated both upward and downward at dusk, resulting in homogeneous distributions during the nighttime.a Mar. Biol. 1992 Julr 113i3 'xqHIROSHIMA UNIV,FAC APPL BIOL SCI,HIROSHIMA 724,JAPAN HUANG C HIROSHIMA UNIV,FAC APPL BIOL SCI,HIROSHIMA 724,JAPAN 4.Times Cited: 10 English Article JJ787 MAR BIOLISI:A1992JJ78700007r609-653$://A1996UP20500001 Humes, A. G.|vDeep-sea Copepoda (Siphonostomatoida) from hydrothermal sites on the Mid-Atlantic Ridge at 23 degrees and 37 degrees N Bulletin of Marine Sciencevent; pacific; genusvoEleven species of Dirivultidae (Copepoda: Siphonostomatoida) have been found at deep-sea vent areas on the Mid-Atlantic Ridge at the Snake Pit site, 23 degrees 23'N, 44 degrees 56'W, depth 3,500 m, and near the Azores at the Lucky Strike site, 37 degrees N, 32 degrees N, depth 1,620 m. Rimipontius mediospinifer new genus, new species, is characterized by the formula 0-0; I for the endopod of leg 4 and by the presence of five setae on each caudal ramus. Aphotopontius atlanteus new species is distinguished by the length of the caudal ramus and by details of the genital double-somite in the female. Stygiopontius cladarus new species is noted for its small subdrate caudal ramus; S. serratus new species for the serrate nature of posterior margin of the antennule; S. teres new species in the female for its smooth expansions of the genital double-somite and the angular margin on leg 5; S. regius new species for its large broad undivided leg 5 in the female and its irregularly shaped spermatophore; S. bulbisetiger new species for the bulbous setae on the antenna; S. mirus new species for the prolongation of the coxa of the maxilliped with a terminal clawlike process; and S. latulus new species for the unusually broad prosome. Two copepods show a disjunct distribution: Aphotopontius forcipatus Humes, 1987, previously known only from the northeastern Pacific, is reported for the first time in the Atlantic; Stygiopontius pectinatus flumes, 1987, reported originally from the Mid-Atlantic Ridge and known also from the Mariana Back-Are Basin, is recorded in large numbers from the hydrothermal site at 23 degrees 23'N, 44 degrees 56'W.Bull. Mar. Sci. 1996 May583'BOSTON UNIV,MARINE PROGRAM,MARINE BIOL LAB,WOODS HOLE,WOODS HOLE,MA 02543 Humes AG BOSTON UNIV,MARINE PROGRAM,MARINE BIOL LAB,WOODS HOLE,WOODS HOLE,MA 0254381Times Cited: 7 English Article UP205 BULL MAR SCIISI:A1996UP20500001 Humes, A.G 1996XRDeep-sea copepoda from hydrothermal sites on the Mid-Atlantic Ridge at 23 and 37 N"Bulletin of Marine Researchn583 609-653t 51-62$://000074318700006e Humes, A. G. Segonzac, M.}Copepoda from deep-sea hydrothermal sites and cold seeps: description of a new species of Aphotopontius from the East Pacific Rise and general distribution Cahiers De Biologie MarineCopepoda; Poecilostomatoida; Siphonostomatoida; Aphotopontius; hydrothermal vents mid-atlantic ridge; vent communities; siphonostomatoida; erebonasteridae; genus; poecilostomatoida; ecology; water; areasuTwenty-four poecilostomatoid and siphonostomatoid copepods are reported from hydrothermal sites in the eastern Pacific and on the Mid-Atlantic Ridge. These include two siphonostomatoids from the East Pacific Rise: Aphotopontius rapunculus, new species, and Stygiopontius mirus, a, species previously known only from the Mid-Atlantic Ridge. Ecological remarks and a synoptic table of 67 species of copepods known at this time from hydrothermal sites and cold seeps are presented.Cah. Biol. Mar. 1998391'Boston Univ, Marine Program, Marine Biol Lab, Woods Hole, MA 02543 USA Boston Univ, Marine Program, Marine Biol Lab, Woods Hole, MA 02543 USA Humes AG Boston Univ, Marine Program, Marine Biol Lab, Woods Hole, MA 02543 USA81Times Cited: 4 English Article ZV574 CAH BIOL MARISI:000074318700006Humes,A.G Segonzac,M 1998Copepoda from deep-sea hydrothermal sites and cold seeps:description of a new species of Aphotopontius from the East Pacific Rise and general distributionBiology Marine39 51-626/Huskin,I Anadon,R Medina,G Head,R.N Harris, R.Pi 2001{Mesoplankton distribution and copepod grazing in the Subtropical Antlantic near the Azores:Influence of mesocale structures"Journal of Plankton Research237671-691NORTH-EAST ATLANTIC, WARM-CORE EDDY, FRONT SOUTHEAST, INGESTION RATE, CYCLONIC EDDY, ZOOPLANKTON, OCEAN, CHLOROPHYLL, PHYTOPLANKTON, REGION5ztMesozooplankton distribution and copepod grazing were investigated in the Subtropical Atlantic Ocean near the Azores during the AZORES I (August) and II (April-May) cruises. Mesozooplankton biomass and abundance remained low throughout the region, but significant increases were found related to the presence of the Azores Front. The Azores Front also exhibited maximum values of copepod community ingestion, reaching 250 mg C m(-2) ingested daily. This increase in ingestion was related to increases in copepod abundance, but not in copepod gut contents. Alb relationship was found between gut contents, or ingestion, and phytoplankton biomass or production. Daily cycles were found in copepod gut contents, being higher during the night, but not in copepod abundance. Multidimensional scaling analysis revealed differences in copepod taxonomic composition between both sides of the front. During spring, daily copepod ingestion represents an average of 6% of the integrated chlorophyll (Chl) a concentration and 22% of the primary production. These percentages increase to 15% of Chl and 61% of production if we only consider large (>2 mum) phytoplankton. No clear influence of the cyclonic eddy LETICIA was found in mesozooplankton biomass or grazing. A significant effect of the Great Meteor Tablemount was found in copepod abundance and grazing, with higher values located west of the mount. ILJIN, A. V. 19760*Geomorphology of the Atlantic Ocean bottom  Nauka 232 pp in Russian INIP 1985aF@Programa de apoio 0224 s pescas nos Aores. Cruzeiros 020150479Relatrios INIPLisboa (40) 1985 26ppPJFisheries; cruises; technology; checklist; Fisheries biology; Oceanography rDKASATKIN, V. I.P 1979 Conditions of fishery for roundnose grenadier in the area of the Mid-Atlantic Ridge. Materials of meeting on further development of fishery in the open World Ocean  20-26 in RussianKASHKIN, N. I.P 1977^WFauna of the echosounding layers. Biology of ocean. V. 1. Biological structure of oceann 299-318 in Russian KELLER, N. B.P 1985rkMadreporarian corals of the Reykjanes Ridge and Platon Mountains (the northern part of the Atlantic Ocean).\ Trudy IOAN 120e 39-51n in RussianKEMENOV, V. E. 1979The influence of water dynamics on the effectiveness of the midwater fishery in the zone of local rising of the World Ocean bottom (on the example of underwater mountains of the Mid-Atlantic Ridge)V:3Problems of fishery oceanography of the World Ocean  55-56 in RussianKEMENOV, V. E. 1982|vForecast of horizontal migrations of grenadier on banks of the Mid-Atlantic Ridge as a basis of the systematic fishery*#The union meeting of oceanographers 5(2)  65-66 in Russian633-656$://000171207400006fjdKhripounoff, A. Vangriesheim, A. Crassous, P. Segonzac, M. Colaco, A. Desbruyeres, D. Barthelemy, R.~xParticle flux in the Rainbow hydrothermal vent field (Mid- Atlantic Ridge): Dynamics, mineral and biological composition Journal of Marine Researchvplucky-strike segment; endeavor ridge; water column; time- series; sea; plume; ocean; sediments; plankton; larvae < 5In order to provide information about the export and the distribution of hydrothermal particulate material to the surrounding deep ocean, four moorings were deployed in the vicinity of the hydrothermal Rainbow vent field (Mid-Atlantic Ridge, 36 degrees 14'N, 2250 m depth). The first mooring was a sediment trap with a current meter deployed at 2 m from a chimney of the Rainbow vent field and 1.5 m above the bottom (a.b.) for 16 days. It represented the reference for the initial composition of particles produced by the vent. The total mean mass particle flux (6.9 g m(-2) d(-1)) was distinctly higher than the flux measured at the shallower hydrothermal vents on the MAR segment. This particulate flux showed a high temporal variation at the scale of a few days and was characterized by a high concentration of sulphur (17.2%) and copper (3.5%) and a very low concentration of organic carbon (0.14%). Several hundred bivalve larvae belonging to the hydrothermal mytilid Bathymodiohis azoricus were collected in this trap at the beginning of the experiment. The density of larvae decreased strongly at the end, indicating a patchiness distribution or a discontinuous reproduction of this species. The other three moorings, including sediment traps, current- meters and thermistor chains, were deployed for 304 days at different distances and altitudes from the Rainbow vent field. The mean speed of the current in the rift valley was low (6 cm s(-1)) and was oriented toward the north. The total mean particle mass flux measured with the five sediment traps varied little, from 10.6 to 25.0 mg m m(-2) d(-1), and displayed temporal variations which are typical of deep-sea environments with seasonal changes in the overlying production. However, in the trap at 500 m from the vents 150 m a.b., the presence of the hydrothermal plume can be observed: the sulphur, iron and copper concentrations of particles were significantly higher compared to the particles sampled in the pelagic reference trap. The plume composition was about 50% hydrothermal particles and 50% pelagic particles and its upper limit reached 300 m a.b. at this distance. In the traps at 1000 m from the vents, the elemental composition of particles was similar to the pelagic particles and we assume that these traps were not in the plume during the experiment. The zooplankton obtained in the long-term trap samples revealed high density variations in relation to the distance from the vent site. The nutrient enrichment around the hydrothermal area and the abundance of free living bacteria explain these variations in zooplankton density. J. Mar. Res. 2001 Jul5944.Times Cited: 1 English Article 476BY J MAR RESISI:000171207400006 G<6Technical Report of Fisheries Research Board of Canada Technology of fish productsXRTese de Aptido Cientfica e Capacidade Pedaggica, Universidade dos Aores, HortaXSThe Danish Dana - Expedition 1920-22 in the North Atlantic and the Gulf of Panama<7The IXth union conference on the fisheries oceanographyThe meeting of specialists of the union associations of the USSR Ministry for Fisheries, fish searching fleets and basins institutes on the problem of widening of fisheries for valuable fish species and sea productsPKThe Study Group on the Biology and Assessment Deep-Sea Fisheries ResourcesXUThe Study Group on the biol. and assessment of deep-sea fish. resources .Working docPMThe Study Group on the Biology and Assessment of Deep-sea Fisheries ResourceshcThe union conference Reserve food and biological resources of the open ocean and seas of the USSRd_The union conference Reserve food biological resources of the open ocean and seas of the USSRHBThe union conference of commercial invertebrates. Theses of papers82The union conference of oceanographers. Sevastopold_The union conference on biochemical genetics, karyological polymorphism and mutagenesis in fish,&The union conference on marine biology85The union conference on the early ontogenesis of fishplThe union conference on theory of formation of abundance and rational exploitation of commercial fish stockslgThe union conference on theory of formation of abundance and rational exploitation of commercial stocks(#The union meeting of oceanographersHEThe union meeting on parasites and diseases of fish. Theses of papersTOThe Working Group on the Biology and Assessment of Deep-sea Fisheries ResourcesTheses of papershdTheses of papers of the conference of young scientists of PINRO by results of investigations in 1971TPTheses of papers of the VIIth Russian conference on problems of fishery forecast\WTheses of Reports of the 4th All-Union Conference on problems of commercial forecasting<8Transactions of the P. P. Sirskov Institut of OceanololyTrudy Trudy AANIITrudy AtlantNIRO Trudy GOIN Trudy IOAN,&Trudy molodykh uchenykh i specialistov Trudy PINROTrudy PINRO, No. 28 Trudy VNIROXRUnderwater investigations from the bio-oceanological and fisheries points of view(#Underwater fisheries investigations$!Underwater Fishery InvestigationsHDUnderwater Investigations for Bio-Oceanological and Fishery Purposes@Larvae of the Nettastomatid eels: Systematics and Distribution Dana-Report  90l 1-44 Smith, D. G J. G. Nielsen 1989|vFamily Nemichthyidae. Fishes of the Western North Atlantic. Volume One: Orders Anguilliformes and Saccopharyngiformes.4-Memoir - Sears Foundation for Marine ResearchNumber One, Part Nine441-459659-685$://A1992HR30900016.@:Smith, K. L. Kaufmann, R. S. Edelman, J. L. Baldwin, R. J.Abyssopelagic Fauna in the Central North Pacific - Comparison of Acoustic Detection and Trawl and Baited Trap Collections to 5800-Mr<6Deep-Sea Research Part a-Oceanographic Research Papersdeep-sea; necrophagous amphipod; eurythenes-gryllus; atlantic- ocean; vertical-distribution; scavenging amphipods; temporal variation; target strength; abyssal-plain; zooplanktonAn integrated study using an acoustic array, opening-closing trawl and baited traps was conducted at an abyssal station in the central North Pacific (31-degrees-N, 159-degrees-W) to further characterize the near-bottom community. Two split-beam line arrays with beam patterns narrow in the vertical and omnidirectional in the horizontal were moored at 100 and 600 m above bottom (mab), sampling an insonified volume of 7855 m3 each. In addition, a multiple opening-closing trawl (10 m2 mouth opening) and baited traps were used to sample the fauna up to 1800 mab. Fourteen deployments of the acoustic arrays during two cruises detected 26 targets, with twice as many at 100 mab as at 600 mab (2.10 vs 0.97 targets h-1). Backscatter strengths for acoustic targets ranged from -57.2 to -26.8 dB. A total of 31 species, at least eight previously undescribed, were identified from trawl and trap collections within 1800 m of the sea floor. Of these new species, four of the decapod genus Hymenodora and one eel, Monognathus rosenblatti, were the most abundant animals collected by trawl. Other species commonly collected in baited traps included Acanthephyra quadrispinosa (Crustacea, Decapoda), Eurythenes gryllus (Crustacea, Amphipoda), and Coryphaenoides yaquinae (Osteichthyes, Macrouridae). Acoustic target abundances ranged from 0 to 1.6 animals per 10(5) m3 per deployment, while values measured with the trawl ranged from 1.4 to 11.9 animals per 10(5) m3. Biomass of the acoustic targets, estimated using a tentative identification based on size, and a series of regressions based on target strength and animal length and weight, ranged form 0 to 72.3 g wet weight per 10(5) m3. Biomass estimates from the trawl samples ranged form 0.2 to 6.7 g wet weight per 10(5) m3. The large number of new species collected during this study and the variability in sampling sparse populations using three different sampling techniques illustrate how little we know about the abyssopelagic community. 1992Mar-Apr39 3-4A'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,DIV MARINE BIOL RES,0202,LA JOLLA,CA 92093 SMITH KL UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,DIV MARINE BIOL RES,0202,LA JOLLA,CA 92093HBTimes Cited: 7 English Article HR309 DEEP-SEA RES PT A-OCEANOG RESISI:A1992HR30900016"SOPOV, Yu. N V. N. SHIBANOV  1980B://A1994QB20400004R Sournia, A..&Pelagic Biogeography and FrontsTProgress in Oceanographymediterranean-sea; gulf-stream; river plume; phytoplankton distribution; zooplankton populations; spatial-distribution; english-channel; north-sea; summer; oceanztFronts, in their world-wide occurrence in the oceans at all space and time scales, exert a wide range of effects on the distribution of pelagic organisms including boundary effects, mixing, concentration, taxonomic and ontogenetic selection, enhanced production, initiation of successions, vertical export, and horizontal transport; a list which is not exhaustive. Moreover, at any given time two or more may be interacting to determine distribution patterns. Thus fronts are hydrological structures which have to be given full consideration in biogeographical studies, even if some of their effects are still poorly understood.Prog. Oceanogr. 199434 2-3'MUSEUM NATL HIST NAT,GEOL LAB,OBSERV OCEANOL ROSCOFF,CNRS INSU,43 RUE BUFFON,F-75005 PARIS,FRANCE SOURNIA A MUSEUM NATL HIST NAT,GEOL LAB,OBSERV OCEANOL ROSCOFF,CNRS INSU,43 RUE BUFFON,F-75005 PARIS,FRANCE82Times Cited: 10 English Review QB204 PROG OCEANOGRISI:A1994QB20400004on; english-channel; north-sea; summer; oceanztFronts, in their world-wide occurrence in the oceans at all space and time scales, exert a wide range of effects on the distribution of pelagic organisms including boundary effects, mixing, concentration, taxonomic and ontogenetic selection, enhanced production, initiation of successions, vertical export, and horizontal transport; a list which is not exhaustive. Moreover, at any given time two or more may be interacting to determine distribution patterns. Thus fronts are hydrological structures which have to be given full consideration in biogeographical studies, even if some of their effects are still poorly understood.Prog. Oceanogr. 199434 2-3'MUSEUM NATL HIST NAT,GEOL LAB,OBSERV OCEANOL ROSCOFF,CNRS INSU,43 RUE BUFFON,F-75005 PARIS,FRANCE SOURNIA A MUSEUM NATL HIST NAT,GEOL LAB,OBSERV OCEANOL ROSCOFF,CNRS INSU,43 RUE BUFFON,F-75005 PARIS,FRANCE82Times Cited: 10 English Review QB204 PROG OCEANOGRISI:A1994QB20400004C:j4$://000166204500013e Wade, I. P. Heywood, K. J.Acoustic backscatter observations of zooplankton abundance and behaviour and the 52-55$://000085834300006jcVinogradov, M. E. Shushkina, E. A. Anokhina, L. L. Vostokov, S. V. Kucheruk, N. V. Lukashova, T. A.piDense aggregations of the ctenophore Beroe ovata (Eschscholtz) near the north-east shore of the Black Sea Okeanologiyamnemiopsis-leidyiDuring the autumn 1999, dense aggregations of the mediterranean ctenophore Beroe ovata has been recorded near the north-east shore of the Black Sea. this specialised carnivorous animal feeds on other ctenophores, including Mnemiopsis. At the end of August-beginning of Septermer, the biomass of Beroe in the Golubaja Bay reached 130 g/m(2) of wet weight in average and 300 g/m(2) in aggregations. This was resulted in the decrease of the biomass of Mnemiopsis and, consequently, in the increase of the biomass of the mesosooplankton and planktophagous fishes. If the high biomass of Beroe will take place in the future, the press of Mnemiopsis will probably decline, while both the biomass of the mesoplankton and the catches of economically important planktophagous fishes will increase. Okeanologiya 2000Jan-Feb401'PP Shirshov Oceanol Inst, Moscow, Russia PP Shirshov Oceanol Inst, Moscow, Russia Vinogradov ME PP Shirshov Oceanol Inst, Moscow, Russia81Times Cited: 6 Russian Article 293CQ OKEANOLOGIYAISI:000085834300006B;Vinogradov, M.E Vereshchaka,A.L Vinogradov, G.M Musaeva,E.IC 2000b\Vertical distribution of zooplankton at the periphery of the North Atlantic subtropical gyre Deep-Sea Water circulation4496-510V\ULABRADOR CURRENT, FRONTAL ZONE, GULF-STREAM, OCEAN, PECULIARITIES, COMMUNITIES, FIELDfVertical distribution of meso- and macroplankton at the north (36 degrees 14' N) and south (14 degrees 45' N, 15 degrees 10' N) periphery of the North Atlantic gyre was considered. The plankton was studied in the net samples (BR 113/140) and by direct visual count from deep-sea manned vessel Mir during five descents. In addition, benthopelagic animals were collected with baited traps. Bimodal structure of macroplankton biomass distribution was observed with peaks in the main picknocline layer at 200-800 and at 1000-1200 m depth. Quantitative distribution of the deep-sea plankton, as well as its species composition were affected by the northward current of intermediate waters from mesotrophic boreal areas (at the north periphery) and southward ultraoligotrophic waters of the central gyre (at the south periphery). Consequently, the plankton at 36 degrees N is enriched at depth below 800-1000 m and a number of deep-sea and benthic species from boreal regions penetrate far to the south. Conversely, biomass of the plankton at 14-15 degrees N sharply decreases at a depth below 1000 m, apparently, due to inflow of deep-sea waters from the central oligotrophic part of the gyre. 7 6DY ("Speer, K. G. Gould, J. LaCasce, J. 1999`ZYear-long float trajectories in the Labrador Sea Water of the eastern North Atlantic Ocean@9Deep-Sea Research Part II-Topical Studies in Oceanography46 1-2^165-1790*Deep-Sea Res. Part II-Top. Stud. Oceanogr.ISI:000079477500009HBmediterranean salt tongue; circulation; variability; driven; modelYear-long Lagrangian trajectories within the Labrador Sea Water of the eastern North Atlantic Ocean are analysed for basic flow statistics. Root-mean-square velocities at 1750 m depth are about 2 cm/s, except within the North Atlantic Current, where they are twice as large. These values are consistent with previous Eulerian measurements and extend those results to a much larger domain of the eastern basin. Mean flow estimates in boxes large enough to contain about 1 float-year of data indicate that Labrador Sea Water, having crossed the Mid- Atlantic Ridge (not resolved) near 50-55 degrees N, presumably with the North Atlantic Current, partially recirculates to the north in the subpolar gyre, as well as entering the subtropical gyre and continuing south and west. The circulation of this water mass, as defined by the 1 yr average velocities, is stronger than traditional models of deep circulation would suggest, with an interior flow of roughly 1 cm/s. Mean speeds up to 3 cm/s were observed, with the highest values near the Azores Plateau. North of 45 degrees N-55 degrees N, mean eastward speeds closer to 0.2 cm/s were observed. Wind- generated barotropic fluctuations may be responsible for some part of the transport at this depth. (C) 1999 Elsevier Science Ltd. All rights reserved.6HBTimes Cited: 3 English Article 182AZ DEEP-SEA RES PT II-TOP ST OCE$://000079477500009a'IFREMER, CNRS, Lab Phys Oceans, BP 70, F-29280 Plouzane, France IFREMER, CNRS, Lab Phys Oceans, F-29280 Plouzane, France Southampton Oceanog Ctr, Southampton, Hants, England Speer KG IFREMER, CNRS, Lab Phys Oceans, BP 70, F-29280 Plouzane, France(!Speer, K. G., J. Gould J. LaCasce  1999b[Year-long float trajectories in the Labrador Sea Water of the eastern North Atlantic Ocean.Deep-Sea Research II46 1-2-165-1792 Stearns,D.E Forward,R.B.Jr 1984vpCopepod photobehavior in a stimulated natural light environment and its relation to nocturnal vertical migrationMarine Biology82 91-100 Steenstrup, J Ltken, Chr  1898RKSpolia Atlantica. Bidrag til Kundskab om Klump-eller Maanefiskene (Molidae)D>Kongelige Danske Videnskabernes Selskabs Skrifter, Kjbenhaven Afd IX. 6  51-544,%Stefanescu, C. D. Lloris J. Rucabado s 1991tn propos de la prsence de Lepidion guentheri (Giglioli, 1880) (Moridae) en Mditerrane occidentale Ibrique Cybium 15 (2)139-146 *$Stefanescu, C D. Lloris J. Rucabado  1994Revalidation of Lampanyctus gemmifer (Goode & Bean, 1879), a junior synonym of Lampanyctus crocodilus (Risso, 1810) in the Atlantic Ocean (Myctophidae) Cybium 18 (3)315-323 Stehmann, M. 1971 Raja (Leucoraja) leucosticta spec. nov. (Pisces, Batoidei, Rajidae), eine neue Rochenart aus dem Seegebiet des tropischen Westafrika; gleichzeitig zur Frage des Vorkommens von Raja ackleyi Garman, 1881 im mittleren Ostatlantikg&Archiv fr Fishereiwissenschaftv 22 (1) 1-16 Steiner, L. Gordon, J. 1990HBCetacea sightseeing's made between 1987 and 1990 in Azorean waters:3Report of the International Fund for Animal Welfared  Cambridgeo 16 pp Steiner, L.m 1995kRough-toothed dolphin, Steno brenadensis: a new species record for the Azores, with some notes on behavioure( ArquiplagoLife and Marine Sciencesin press8179-189$://A1995RC87500013.'Turley, C. M. Lochte, K. Lampitt, R. S.u^WTransformations of Biogenic Particles During Sedimentation in the Northeastern Atlantica\VPhilosophical Transactions of the Royal Society of London Series B-Biological Sciencesparticulate organic-matter; diel migrant biota; deep-sea floor; marine snow; north-atlantic; seasonal deposition; bloom experiment; pacific-ocean; vertical flux; carbon fluxp The vertical flux and transformation of biogenic particles are important processes in the oceanic carbon cycle. Changes in the magnitude of the biological pump can occur in the north eastern Atlantic on both a seasonal and interannual basis. For example, seasonal Variations in vertical flux at 47 degrees N 20 degrees W are linked to seasonal ocean productivity variations such as the spring bloom. The size and organic and inorganic content of phytoplankton species, their development and succession also play a role in the scale and composition of the biological pump. The majority of flux is in the form of fast sinking aggregates. Bacteria and transparent exopolymer particle production by phytoplankton have been implicated in aggregate production and mass flux events. Zooplankton grazing and faecal pellet production, their size and composition and extent of their vertical migration also influence the magnitude of vertical flux. Aggregates are formed in the upper ocean, often reaching a maximum concentration just below the seasonal thermocline and can be a food resource to mesozooplankton as well as to the high concentrations of attached bacteria and protozoa. Attached bacteria remineralize and solubilize the aggregate particulate organic carbon. The degree of particle solubilization is likely to be affected by factors controlling enzyme activity and production, for example temperature, pressure or concentration of specific organic molecules, all of which may change during sinking. Attached bacterial growth is greatest on particulate organic matter collected at 500 m which is the depth where studies of(210)po reveal that there is greatest break-up of rapidly sinking particles. Break-up of particles by feeding zooplankton can also occur. The fraction of sinking poc lost between 150-3100 m at one station in the north eastern Atlantic could supply about 90 % of the bacterial carbon demand. Some larger, faster sinking aggregates escape solubilization and disaggregation in the upper 1000 m and arrive in the deep ocean and on the deep-sea bed. Seasonally varying rates of sedimentation are reflected at the deep-sea floor by deposition of phytodetrital material in summer. Approximately 2-4 % of surface water primary production reaches the sea floor in 4500 m depth at 47 degrees N 20 degrees W after a sedimentation time of about 4-6 weeks. In this region, concentrations of chloroplastic pigments increased in summer by an order of magnitude, whereas seasonal changes in activity or biomass parameters were smaller. Breakdown of the generally strongly degraded organic matter deposited on deep-sea sediments is mainly accomplished by bacteria. Rates of degradation and efficiency of biomass production depend largely on the proportion of biologically labile material which decreases with advancing decay. It is likely that different levels of organic matter deposition influence the bioturbation rates of larger benthos, which has an effect on transport processes within the sediment and presumably also on microbial degradation rates.4.Philos. Trans. R. Soc. Lond. Ser. B-Biol. Sci. 1995 May 30 348 1324' PLYMOUTH MARINE LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLAND ALFRED WEGENER INST POLAR & MARINE RES,W-2850 BREMERHAVEN,GERMANY INST OCEANOG SCI,DEACON LAB,WORMLEY GU8 5UB,SURREY,ENGLAND TURLEY CM PLYMOUTH MARINE LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLANDHATimes Cited: 25 English Article RC875 PHIL TRANS ROY SOC LONDON BISI:A1995RC87500013ab Phys Oceans, F-29280 Plouzane, France Southampton Oceanog Ctr, Southampton, Hants, England Speer KG IFREMER, CNRS, Lab Phys Oceans, BP 70, F-29280 Plouzane, France(!Speer, K. G., J. Gould J. LaCasce  1999b[Year-long float trajectories in the Labrador Sea Water of the eastern North Atlantic Ocean.Deep-Sea Research II46 1-2-165-1792 Stearns,D.E Forward,R.B.Jr 1984vpCopepod photobehavior in a stimulated natural light environment and its relation to nocturnal vertical migrationMarine Biology82 91-100 Steenstrup, J Ltken, Chr  1898RKSpolia Atlantica. Bidrag til Kundskab om Klump-eller Maanefiskene (Molidae)D>Kongelige Danske Videnskabernes Selskabs Skrifter, Kjbenhaven Afd IX. 6  51-544,%Stefanescu, C. D. Lloris J. Rucabado s 1991tn propos de la prsence de Lepidion guentheri (Giglioli, 1880) (Moridae) en Mditerrane occidentale Ibrique Cybium 15 (2)139-146 *$Stefanescu, C D. Lloris J. Rucabado  1994Revalidation of Lampanyctus gemmifer (Goode & Bean, 1879), a junior synonym of Lampanyctus crocodilus (Risso, 1810) in the Atlantic Ocean (Myctophidae) Cybium 18 (3)315-323 Stehmann, M. 1971 Raja (Leucoraja) leucosticta spec. nov. (Pisces, Batoidei, Rajidae), eine neue Rochenart aus dem Seegebiet des tropischen Westafrika; gleichzeitig zur Frage des Vorkommens von Raja ackleyi Garman, 1881 im mittleren Ostatlantikg&Archiv fr Fishereiwissenschaftv 22 (1) 1-16 Steiner, L. Gordon, J. 1990HBCetacea sightseeing's made between 1987 and 1990 in Azorean waters:3Report of the International Fund for Animal Welfared  Cambridgeo 16 pp Steiner, L.m 1995kRough-toothed dolphin, Steno brenadensis: a new species record for the Azores, with some notes on behavioure( ArquiplagoLife and Marine Sciencesin press682-689$://A1990DW76000024$Galkin, S. V. Moskalev, L. I.VOStudy of Abyssal Fauna of the North-Atlantic Using Deep-Sea Inhabited Apparatus Okeanologiya Okeanologiya 1990Jul-Aug304L'ZSPP SHIRSHOV OCEANOL INST,MOSCOW,USSR GALKIN SV PP SHIRSHOV OCEANOL INST,MOSCOW,USSRS81Times Cited: 3 Russian Article DW760 OKEANOLOGIYAYISI:A1990DW76000024V0)Gallienne,G.P Robins,D.B Woodd-Walker,R.S  2001}Abundance distribution and size structure of zooplankton along a 20 west meridional transect of the NE Atlantic Ocean in JulyDeep-Sea Research part II 48925-9496.'OPTICAL PLANKTON COUNTER, HELGOLANDICUSZooplankton distribution, abundance and size structure were characterised on leg 2 of the PRIME cruise in the northeast Atlantic during July 1996. Latitudinal sampling was carried out from 60 degreesN to 37 degreesN along a meridian at approximately 20 degreesW. Zooplankton were characterised using an Optical Plankton Counter (OPC), and from traditional depth-integrated net hauls for taxonomy and carbon. The former method allows zooplankton to be described in terms of biovolume and size. There was good agreement between the two methods for abundance and a good correlation between OPC biovolume and carbon analysis. These data also showed compatibility with concurrent acoustic measurements of zooplankton. Results for the cruise compared to recent studies in the region, show that, overall abundance was generally low, although most of the previous studies were closer to spring bloom conditions. The size structure over latitude shows that mean size fluctuated, but there was a general trend of decreasing mean size from the north of the transect to about 47 degreesN. Further statistical treatment of the OPC data, using principal component analysis, showed that zooplankton size structure changed at five positions along the transect. Three of these coincided with changes in physical structure, one each side of the front at 48 degreesN and the third on the outer edge of an eddy. The other two occurred in regions of high-surface chlorophyll concentration. (C) 2001 Published by Elsevier Science Ltd. Gardner, W.D.t Gardner, D 1975HBObservations on the distribution of dissolved mercury in the ocean Marine Pollution Bulletino6  43-46r Gardner, W.D.A 1977B://000080498700002VOGebruk, A. V. Galkin, S. V. Vereshchaka, A. L. Moskalev, L. I. Southward, A. J.HXQEcology and biogeography of the hydrothermal vent fauna of the Mid-Atlantic Ridgee("Advances in Marine Biology, Vol 32 ACADEMIC PRESS LTDshrimp rimicaris-exoculata; azores triple-junction; caridean shrimp; seep communities; methane seep; tube-worms; north-sea; genus; bresiliidae; field  Advances in Marine Biology 199732*$Times Cited: 16 English Review BN05A London'jdGebruk AV Russian Acad Sci, PP Shirshov Oceanol Inst, Nakhimovsky Prospekt 36, Moscow 117851, RussiaISI:000080498700002sZ Quro1986~ Quro1989 Quro1991G Rabouille2001 Rabouille2001 Rainbow1995= Rainbow1995 Ramalho1929 Ramos1984l Ramos1996 RAMOS19968 Ramos1996: Ramos1996> Ramos1998Ramosin pressRamosin pressCRamos_JA19999f Rannou1971 Rannou1974 Rannou1976 Read2001U Read2001 Rees1966 Regan1903 Regan1925 Regan1929 Reiner19855 Reiner1990 Reiner1993 Rey1984 Rey1984 R19921$ R1992a R19921 Ribera Maycas1999 Rice1994W Rice19966  Richard1910 Richard1934! Richard19369 Richardson20000S Rieck1992 Riemann1989 Ringelberg1995 Robertson2002 Robins20010bRobinson1977 Rocha2002 Roden1987Rodhouse1998 Roe1984w Rogers1994 Rogers1994u Rogers2000 Roman1995a Rosenblatt1984 Rossby1996_ Rossby1999  Rossby1999W Rossby1999X Rossby2000 ROSSOV.1973 Roule1915Rucabado1991Rucabado19919Rucabado19949 RUDENKO1973 RUDENKO1982 RUDENKO1986  Rudenko1992  Rudenko1992G Ruiz-Pino2001 Ruiz-Pino2001 Rundle19949 Rundle19949 RVACHEV1984RVACHEV.1974GSAFRONOV1998 Sagalevich1983 Sagalevich1983 SAGALEVICH1987  Saiz1993 SaldanhaSaldanha1977Saldanha1977Saldanha1980"Saldanha1991Saldanha1991#Saldanha1992$Saldanha1992Saldanha19949Saldanha1994Saldanha1995Saldanha19966}Saltzman19959dSaltzman1997eSaltzman1997SAMAREVA1980 SAMOKHVALOV1982I Sanders1996 Santos19855 Santos19877% Santos1987 Santos19888& Santos1989' Santos1990 Santos19900 Santos19911 Santos1991 Santos19922 Santos19922( Santos1992 Santos1992 Santos1993 Santos19933 Santos19939 Santos19949 Santos1994) Santos1994 Santos1994* Santos1995+ Santos1995, Santos1995m Santos199669 Santos19966-Santosin press SAPRONETSKAYA1979 SAPRONETSKAYA1979 SAPRONETSKAYA1989+ Sargent2000Sarradin19949 Savidge2001 SAVVATIMSKY1982 SAVVATIMSKY1982 SAVVATIMSKY1984 SAVVATIMSKY1987 SAVVATIMSKY1987U SAVVATIMSKY.1987 Sazonov1976 Schauer1992Z Schauer1992 Schiebel2000 Schmidt1918 Schmidt1921 Schmidt1921 Schmidt1926 Schmitz1993 Schreiver1989 Schroeder1940 Schults1995 Schulz1995 Schut2002Sedberry1995Sedberry1996Segonzac19969Segonzac1998Segonzac1998Segonzac2000eSegonzac20012SENNIKOV1986SENNIKOV1986Sennikov1987BSennikov1991SENNIKOV1991k SENNIKOV.1981SEREBROV1974SEREBROV1976v SEREBRYAKOV.1983iSEREBRYANNIKOV1987;Serobaba19955. Serpa1886. Serro19929o Serret20010 Shaboneyev1973<Shachkov199112 Shanks1997 SHATOBA1984 Shcherbachev1976 Shcherbachev1985 Sheader1996 Sheberstov1995 Shelbourne1962 Sheldon1987 SHESTOPAL1991 SHESTOPAL1993 SHESTOPAL1996 SHESTOPAL1997 SHESTOPAL.1990Shevtsov19855SHIBANOV1980SHIBANOV1984SHIBANOV1985SHIBANOV19879SHIBANOV1987SHIBANOV1988SHIBANOV1988SHIBANOV1988SHIBANOV1988SHIBANOV1989SHIBANOV1989SHIBANOV1989SHIBANOV1990SHIBANOV1991SHIBANOV1991SHIBANOV1991SHIBANOV1991SHIBANOV1992oSHIBANOV19949SHIBANOV19941SHIBANOV19969SHIBANOV1998SHIBANOV1999m SHIBANOV.1983i SHIBANOV.1987 SHIBANOV.1989 SHIBANOV.1991 Shimko1984 Shimko1984 SHIMKO19868 Shimko19878 Shimko1987 Shimko1989 Shimko1990 Shimko1990 Shimko1990 SHISHLO1984 Shlibanov1985 SHLIBANOV1987a Shores19707SHUBENKO198337 Shushkina1989< Shushkina1991 Shushkina19928 Shushkina1992 Shushkina1995; Shushkina19955 Shushkina1996@ Shushkina1996 Shushkina1997? Shushkina1997 Shushkina1998= Shushkina1998 Shushkina1999 Shushkina1999> Shushkina1999 Shushkina2000: Shushkina20009 Shushkina2002#Sieracki1993 SIGAEV19828 Silva1983/ Silva1986a0 Silva1986b1 Silva1987a1 Silva1987a Silva1987a1 Silva1987a1 Silva1987ab1 Silva1987aa86b1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a Silva1987ab1 Silva1987ab1 Silva1987ab1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a Silva1987a Silva1987ab1 Silva1987a Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987ab1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987ab1 Silva1987a1 Silva1987a1 Silva1987a1 Silva1987ab1 Silva1987ab1 Silva1987a1 Silva1987antos1995, Santos1995m Santos19966-Santosin press SAPRONETSKAYA1979 SAPRONETSKAYA1979+ Sargent2000Sarradin19949 Savidge2001U SAVVATIMSKY.1987̧ Sazonov1976 Schauer1992 Schiebel2000̨ Schmidt1918 Schmidt1921 Schmidt1921 Schmidt1926 Schmitz1993 Schreiver1989 Schroeder1940 Schults1995 Schulz1995 Schut2002Sedberry1995̮Sedberry1996Segonzac19969Segonzac1998Segonzac1998Segonzac2000eSegonzac20012Sennikov1987BSennikov1991k SENNIKOV.1981v SEREBRYAKOV.1983iSEREBRYANNIKOV1987;Serobaba19955. Serpa1886. Serro19929o Serret20010 Shaboneyev1973<Shachkov199112 Shanks1997̰ Shcherbachev1976̱ Shcherbachev1985̫ Sheader1996 Sheberstov1995 Shelbourne1962 Sheldon1987 SHESTOPAL.1990Shevtsov19855oSHIBANOV19949m SHIBANOV.1983i SHIBANOV.1987 SHIBANOV.1989 SHIBANOV.1991 Shimko1984 Shimko1984 Shimko19878 Shimko1987 Shimko1989 Shimko1990 Shimko1990 Shimko1990̱ Shlibanov1985 SHLIBANOV1987a Shores197077 Shushkina1989< Shushkina1991 Shushkina19928 Shushkina1992 Shushkina1995; Shushkina19955 Shushkina1996@ Shushkina1996 Shushkina1997? Shushkina1997 Shushkina1998= Shushkina1998 Shushkina1999 Shushkina1999> Shushkina1999 Shushkina2000: Shushkina20009 Shushkina2002#Sieracki1993̲ Silva1983/ Silva1986a0 Silva1986b1 Silva1987anPKAIH>7Wiebe,P.H Madin,L.P Haury, L.R Harbison,G.R Philbin,L.Ms 1979~Diel Vertical Migration by Salpa aspera and Its Potential for Large-Scale Particulate Organic Matter Transport to the Deep-seaMarine Biology53249-255224-233$://A1996UK850000040F?Williamson, C. E. Sanders, R. W. Moeller, R. E. Stutzman, P. L.|vUtilization of subsurface food resources for zooplankton reproduction: Implications for diel vertical migration theory Limnology and Oceanographylife-history parameters; adaptive significance; eutrophic lake; fresh-water; daphnia; predation; bacteria; temperature; nanoplankton; chlorophyll~xThe water columns of lakes and oceans provide a diverse habitat gradient in which light, temperature, food, and predation risk all change with depth. Many planktonic organisms exhibit diel vertical migrations (DVM) in response to daily oscillations in many of these variables. DVM theory often assumes that surface waters are more food-rich than deeper, subsurface layers and proceeds to try to explain why zooplankton migrate out of these beneficial surface layers during the day. Here, we test the assumption that food is best in surface waters by feeding two common crustacean zooplankton with natural epilimnetic and metalimnetic food assemblages from a eutrophic lake and examining their egg production rates. Both Diaptomus and Daphnia showed greater reproductive rates in the metalimnetic water and significant food limitation in the epilimnetic water. Mass-specific ingestion rates were approximately three times higher in the metalimnion than in the epilimnion. In spite of the poorer food in the surface waters, these two crustaceans migrated into the epilimnion at night. These observations are contrary to the assumption that food is best in the surface water, and a review of the literature suggests that food frequently is not best in surface waters. The upward migrations at night are best explained by the warmer temperatures and reduced predation risk in the surface waters at night.Limnol. Oceanogr. 1996 Mar412'LEHIGH UNIV,DEPT EARTH & ENVIRONM SCI,BETHLEHEM,PA 18015 ACAD NAT SCI PHILADELPHIA,DIV ENVIRONM RES,PHILADELPHIA,PA 19103 Williamson CE LEHIGH UNIV,DEPT EARTH & ENVIRONM SCI,BETHLEHEM,PA 18015<5Times Cited: 25 English Article UK850 LIMNOL OCEANOGRISI:A1996UK85000004Wirtz, P. Martins, H. R. 1993}Notes on some rare and little known marine invertebrates from the Azores, with a discussion of the zoogeography of the region ArquiplagofLife and Marine Sciences 11A 55-63 Wishner, K.F 198082The biomass of the deep-sea benthopelagic planktonDeep-Sea Researcho 27 A203-216"Wishner, K.F Meise-Munns,C.J 1984JDIn situ grazing rates of deep-sea benthic boumdary-layer zooplanktonMarine Biology84 65-74357-366$://A1987G973000005"Wishner, K. F. Gowing, M. M.voInsitu Filtering and Ingestion Rates of Deep-Sea Benthic Boundary-Layer Zooplankton in the Santa-Catalina BasinMarine Biology Mar. Biol. 1987943S'UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882 UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 95064 WISHNER KF UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 028824.Times Cited: 20 English Article G9730 MAR BIOLISI:A1987G973000005 57-59$://A1990DM39600059Y6/Wishner, K. Levin, L. Gowing, M. Mullineaux, L.eNHInvolvement of the Oxygen Minimum in Benthic Zonation on a Deep Seamount Nature Nature 1990 Jul 5z 346 6279'*$UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882 N CAROLINA STATE UNIV,DEPT MARINE EARTH & ATMOSPHER SCI,RALEIGH,NC 27695 UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 95064 WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543 WISHNER K UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 028822,Times Cited: 44 English Article DM396 NATUREISI:A1990DM396000592f0Vereshchaka, A.L 1995PJMacroplankton in the near-bottom layer of continental slopes and seamountsDeep-Sea Researchs part I 429\ 1639-1668BENTHIC BOUNDARY-LAYER, HYPERBENTHIC MYSIDS CRUSTACEA, NORTHEAST ATLANTIC-OCEAN, WESTERN INDIAN-OCEAN, DEEP-SEA, VERTICAL-DISTRIBUTION, BENTHOPELAGIC PLANKTON, BIOMASS, ZOOPLANKTON, ZONATIONDistributions of mysids, euphausiids, shrimps and bottom-dwelling decapod larvae have been studied to reveal their relation to the sea bottom. A total of about 200,000 specimens belonging to 178 species and closer unidentified taxa has been examined. The material has been taken by R.V. Professor Shtokman in the Southeast Pacific (1987-1988) and by R.V. Vityaz in the western Indian Ocean (1989-1990) by sampling at depths of 1500 m and less over seamounts and continental slopes. In addition, aquarium observations on five species and analyses of the gut contents of 14 species have been carried out. Two principal groups of animals have proved to live in the near-bottom layer: pelagic (independent of the bottom) and benthopelagic (related to the bottom). They appear to differ in all studied aspects: distribution, behaviour and feeding. The benthopelagic animals are divided into three subgroups with finer ecological differences: hypo-, epi-, and amphibenthopelagic. The patterns of their distribution and migrations, the near-bottom biological zonation and its relation to the benthic boundary and benthic nepheloid layers are discussed, with (re)definitions of the terms used.r 1905-1921O$://000072322200007 Vereshchaka, A. L.zsComparative morphological studies on four populations of the shrimp Rimicaris exoculata from the Mid-Atlantic RidgeV<6Deep-Sea Research Part I-Oceanographic Research Papersriftia-pachyptila populations; sea hydrothermal vents; deep- sea; eastern pacific; gene flow; decapoda; alvinocarididae; bresiliidae; crustacea; ecology81Four populations (a total of 677 specimens) of the hydrothermal shrimp species Rimicaris exoculata from three Mid-Atlantic Ridge vent fields were studied: Broken Spur (29 degrees N), TAG (26 degrees N), and "14-45" (14 degrees N). Five morphological characters were analysed: number of dorsolateral spines on telson, relative carapace width, relative abdominal length, presence of "abnormal telson", and fat content. Dependences of each character upon shrimp size were analysed. Division of the shrimp ontogenesis on the basis of general morphology is proposed. Phenotypic analysis based upon five selected characters revealed statistically significant divergence between two populations within the same vent field TAG. Probable causes of observed divergence are discussed. (C) 1998 Published by Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 Nov4411'Russian Acad Sci, Inst Oceanol, Krasikova St 23, Moscow 117851, Russia Russian Acad Sci, Inst Oceanol, Moscow 117851, Russia Vereshchaka AL Russian Acad Sci, Inst Oceanol, Krasikova St 23, Moscow 117851, RussiaHBTimes Cited: 1 English Article ZA037 DEEP-SEA RES PT I-OCEANOG RESISI:000072322200007d 1615-1632N$://000081843700006i*$Vereshchaka, A. L. Vinogradov, G. M.Visual observations of the vertical distribution of plankton throughout the water column above Broken Spur vent field, Mid- Atlantic Ridge<6Deep-Sea Research Part I-Oceanographic Research Papers~whydrothermal plume; endeavor ridge; scattering layer; zooplankton; macroplankton; sea; 29-degrees-n; communities; oceaneJDVisual observations were made in September 1997 during the 39 cruise of R/V "Akademik Mstislav Keldysh" with 2 deep-sea manned submersibles "Mir" aboard. During 4 dives the following plankton countings were made: 3 vertical throughout the water column during the day, 2 vertical in the upper 1000 m at night, and 1 oblique in the plume area during the day. Biomass profiles are represented for each dive for all abundant animal groups: copepods, euphausiids + decapods + mysids, chaetognaths, medusae, ctenophores, siphonophores, cyclo- thones, myctophides, radiolarians, and the total zooplankton. Plankton distribution shows 2 aggregations, one within the main pycnocline and the other near the plume; Gelatinous animals and radiolarians dominate in both aggregations by biomass and make a significant contribution to the plankton biomass throughout the water column. Oblique counting indicates the presence of aggregations of animals near the upper and lower borders of the plume and biomass depletion within the plume core. (C) 1999 Published by Elsevier Science Ltd. All rights reserved..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1999 Sepc469sHBTimes Cited: 4 English Article 223LZ DEEP-SEA RES PT I-OCEANOG RESISI:000081843700006o >H555-566$://000083507000009 LEVinogradov, M. E. Vereshchaka, A. L. Shushkina, E. A. Arnautov, G. N.Vd^Structure of zooplanktonic communities in the frontal zone of Gulf Stream and Labrador Current Okeanologiyavertical-distributionVertical distribution of meso- and macroplankton was studied in the area of the sharpest climatic frontal zone between Gulf Stream and Labrador Current at the site 41 degrees 39'N, 49 degrees 58'W. Plankton nets BR 113/140 and direct visual observations from manned submersibles "Mir" were used. In the frontal zone, arctoboreal communities and North Atlantic subtropical gyre communities contract. In more "mature" communities (in terms of succession) of anticyclone gyre, macroplanktonic carnivorous and detritophagous animals (mainly shrimps Acanthephyra) develop and create "living net" feeding on the rich arctoboreal plankton brought from, the North, Resulting shrimp biomass appears much higher than that of their prey. Patterns of vertical distribution and population structure: of shrimps were analysed. The data on quantitative vertical distribution of the total biomass of meso- and macroplankton as well as of the most important groups including gelatinous animals (ctenophores, medusae, syphonophores) were obtained. Vertical change in the role of various planktonic groups were traced; they gave evidence for the frontal changes in the community structure from the surface to a depth of about 2000 m. Okeanologiya 1999Jul-AugG394R'PP Shirshov Oceanol Inst, Moscow, Russia PP Shirshov Oceanol Inst, Moscow, Russia Vinogradov ME PP Shirshov Oceanol Inst, Moscow, Russia81Times Cited: 2 Russian Article 252NF OKEANOLOGIYAJISI:000083507000009e 64-74$://000079729200009XQVinogradov, M. E. Shushkina, E. A. Nezlin, N. P. Vedernikov, V. I. Gagarin, V. I.^WCorrelation between different parameters of ecosystem of epipelagial of the World Ocean Okeanologiyaphotosynthetic primary production; pacific-ocean; quantitative characteristics; satellite; communities; waters; layer; phytoplankton; algorithms; planktonThe quantitative characteristics of planktonic communities of the productive ocean layer (0-200 m) were studied in ecosystem expeditions of SIO RAS in different regions of the World Ocean (295 stations). Unified methodology was used. The correlations were estimated between the chlorophyll concentration in the surface layer and different parameters of communities: total chlorophyll content in 0-200-m layer, primary production, the biomasses of phytoplankton, small (less than or equal to 3 mm), large (>3 mm), and total mesoplankton. The correlations between these parameters and water transparency (Secchi disk) were also estimated. The regression equations are significantly different in cold-water (polarmore from 40 degrees N and 40 degrees S) and warm-water regions. The possibility of using these equations for arbitrary evaluation of structural characteristics of planktonic communities is discussed. Okeanologiya 1999Jan-Feb391'PP Shirshov Oceanol Inst, Moscow, Russia PP Shirshov Oceanol Inst, Moscow, Russia Vinogradov ME PP Shirshov Oceanol Inst, Moscow, Russia81Times Cited: 4 Russian Article 186KV OKEANOLOGIYAtISI:000079729200009h496-510$://000090149300013eLEVinogradov, M. E. Vereshchaka, A. L. Vinogradov, G. M. Musaeva, E. I.nb\Vertical distribution of zooplankton at the periphery of the North Atlantic subtropical gyre4.Izvestiya Akademii Nauk Seriya Biologicheskaya\Ulabrador current; frontal zone; gulf-stream; ocean; peculiarities; communities; fieldeVertical distribution of meso- and macroplankton at the north (36 degrees 14' N) and south (14 degrees 45' N, 15 degrees 10' N) periphery of the North Atlantic gyre was considered. The plankton was studied in the net samples (BR 113/140) and by direct visual count from deep-sea manned vessel Mir during five descents. In addition, benthopelagic animals were collected with baited traps. Bimodal structure of macroplankton biomass distribution was observed with peaks in the main picknocline layer at 200-800 and at 1000-1200 m depth. Quantitative distribution of the deep-sea plankton, as well as its species composition were affected by the northward current of intermediate waters from mesotrophic boreal areas (at the north periphery) and southward ultraoligotrophic waters of the central gyre (at the south periphery). Consequently, the plankton at 36 degrees N is enriched at depth below 800-1000 m and a number of deep-sea and benthic species from boreal regions penetrate far to the south. Conversely, biomass of the plankton at 14-15 degrees N sharply decreases at a depth below 1000 m, apparently, due to inflow of deep-sea waters from the central oligotrophic part of the gyre. Izv. Akad. Nauk Ser. Biol. 2000Jul-Aug4>7Times Cited: 0 Russian Article 369AH IZV AKAD NAUK BIOLISI:000090149300013 " 9295-303$://000175729100007("Vinogradov, M. E. Shushkina, E. A.|vVertical distribution of gelatinous macroplankton in the North Pacific observed by manned submersibles Mir-1 and Mir-2Journal of OceanographyMedusa; vertical distribution; North Pacific; submersibles; abundance; biodiversity zooplankton; sea; jellyfish; medusae; insitu; region$The vertical distribution of several medusa species in the Kurile-Kamtehatka region of the Pacific Ocean is described. Animals were observed in the light cone from deep-sea submersibles Mir-1 and Mir-2 throughout the water column, from the surface to 5000-6000 m at four different sites. Bathy- and abyssopelagic species are noted along with the species living in an extremely wide depth range. A faunistic border is re vealed at a depth of 3000 m. The contribution of gelatinous animals (medusae, submersibles, siphonophores, salps) to the total deep-sea plankton biomass was estimated using a abundance, biodiversity. wire reference cube during nine dives in the highly productive areas of the northwest Pacific, eastern Pacific (California, Costa-Rica Dome), and subtropical oligotrophic areas. J. Oceanogr. 2002 Apr582'PP Shirshov Oceanol Inst, Nakhimovsky Prosp 36, Moscow 117851, Russia PP Shirshov Oceanol Inst, Moscow 117851, Russia Vinogradov ME PP Shirshov Oceanol Inst, Nakhimovsky Prosp 36, Moscow 117851, Russia4.Times Cited: 0 English Review 554HE J OCEANOGRISI:000175729100007$VINOGRADOVA, L. A L. N. GRUZOV 1990\UOn biocenotical division of epipelagic layer of the North Atlantic and adjacent areaso Trudy GOIN82112-1333 in Russian,%Voss, N.A. Nesis, K.N. Rodhouse, P.G.C 1998b[Systematics, Biology and Biogeography of the Cephalopod Family Histioteuthidae (Oegopsida),\2, Systematics and Biogeography of Cephalopods82Smithsonian Contributions to Zoology, 586, part II293-372I In English899-924$://000166204500013e Wade, I. P. Heywood, K. J.Acoustic backscatter observations of zooplankton abundance and behaviour and the influence of oceanic fronts in the northeast Atlantic@9Deep-Sea Research Part Ii-Topical Studies in OceanographydNGdoppler current profiler; patterns; water; distributions; winter; ridgeuAcoustic Doppler Current Profiler-derived acoustic backscatter data were compared with physical and biological data collected during leg 2 of the PRIME cruise in the northeastern Atlantic during July 1996. The leg 2 transect from 59 to 37 degreesN ran approximately along the 20 degreesW meridian and crossed a range of hydrographic conditions from near subarctic in the north to subtropical in the south. A front at 52.5 degreesN was an extension of a southern branch of the North Atlantic Current system. A stronger frontal feature was observed at 48 degreesN and was considered to be the northern limit of Eastern North Atlantic Water that had been ventilated at the eastern boundary. At 37 degreesN a Lagrangian time-series study was performed. High acoustic backscatter was observed within the PRIME eddy at 59 degreesN and at the southern site. Other changes in backscatter intensity, or more correctly, in 'mean volume backscattering strength' (MVBS), coincided with two main fronts crossed during the transect and upon arrival at the southern site. An increased MVBS in the surface 100 m in the north was not present south of 52.5 degreesN. Between 48 and 37 degreesN the MVBS approached its lowest of the transect. At 37 degreesN marked changes in the backscatter were observed, with a strong signal seen in the top 75 m. As well as changes in the MVBS there were differences in the diel migratory patterns observed in the backscatter. Scattering at 37 degreesN was concentrated above a strong pycnocline at 75 m. In the north the scattering signal was generally noisier and less well defined than in the south. Biomass has been estimated from the MVBS by comparing it with biomass estimates derived from Optical Plankton Counter data and carbon/nitrogen measurements. Although such calibrations have their limitations, the results give important information concerning net sampling strategies and are a good test of the representativeness of such sampling. (C) 2001 Elsevier Science Ltd. All rights reserved.0*Deep-Sea Res. Part II-Top. Stud. Oceanogr. 200148 4-5HBTimes Cited: 8 English Article 388VV DEEP-SEA RES PT II-TOP ST OCEISI:000166204500013 H P   %$#"!  H@9ZAFERMAN, M. L V. N. SHIBANOV A. N. KALUGIN A. S. YAROVOYr 1991Investigations of behaviour and distribution of roundnose grenadier in the area of the Mid-Atlantic Ridge with the use of underwater device Sever-2D=Biological resources of thalassic bathyal of the World Ocean 62-69 in Russian$ZAFERMAN, M. L I. P. SHESTOPAL 1996Assessment of tusk abundance on the underwater eminencies of the North Atlantic by data of underwater observations and long lining6/ Instrumental methods of fishery investigationsn 65-797 in Russian$ZAFERMAN, M. L I. P. SHESTOPAL 1997XQNon-traditional fishery objects on the underwater mountains of the North AtlanticNjd Non-traditional objects of the sea fishery and perspectives of their exploitation. Theses of papers  49-51 in Russian ZEZINA, O. N 1985nhOn the usage of bottom sestonophages for evaluation of the productivity on the middle-oceanic eminencies Trudy IOAN  120 65-69 in Russian"ZILANOV, V. K S. J. BOGDANOV 1969RLResults research on Scomberesox saurus in the north-eastern Atlantic in 1968 Annals. Biolog. (1968) 25252-255. in Russian ZILANOV, V. KO 1970XQInvestigations on the biology of Scomberesox saurus in the North Atlantic in 1969tAnnals. Biolog. (1969)  26e263-265. in RussianZILANOV, V. K. 1975BMercury levels in seabirds from the Azores, mid-North Atlantic<6Archives of Environmental Contamination and Toxicology28304-309:"Monteiro, L.R. Furness, R.W  1995@9Seabirds as monitors of mercury in the marine environment$Water, Air and Soil Pollution  80 851-8700)Monteiro, L.R. Furness, R.W del Nevo, A.JP 1995JDMercury levels in seabirds from the Azores, mid-North Atlantic Ocean& Arch. Environ. Contam. Toxicol  28 304-309.V"Monteiro, L.R. Furness, R.Wn 1995@9Seabirds as monitors of mercury in the marine environment} pp. 851-870"Monteiro, L.R. Furness, R.W  19950*Fea's petrel Pterodroma feae in the Azores Bull. Brit. Orn. Cl  115  9-14.e proportion observed at the MAR), while area B has 83% smooth seamounts. On the basis of these results, we present a conceptual model for building the shallow crust at the slow spreading Reykjanes Ridge that takes into account the possible influence of the Iceland hot spot on the crustal melt delivery system and its influence on variables that control seamount abundances, sizes, shapes, and surface morphologies. In this model we suggest that the increased seamount production and proliferation of smooth seamounts in area B may be associated with a pulse of hot spot material, in the form of asthenosphere of higher temperature, that has recently affected area B."J. Geophys. Res.-Solid Earth 1995 May 10 100B5'WOODS HOLE OCEANOG INST,DEPT GEOL & GEOPHYS,WOODS HOLE,MA 02543 MIT,WHOI,JOINT PROGRAM OCEANOG,WOODS HOLE,MA MADGE LS WOODS HOLE OCEANOG INST,DEPT GEOL & GEOPHYS,WOODS HOLE,MA 02543D>Times Cited: 1 English Article QX769 J GEOPHYS RES-SOLID EARTHISI:A1995QX769000281 fedcbMauchline,J Gordon,J.D.M 1991jcOceanic pelagic prey of benthopelagic fish in the benthic boundary layer of marginal oceanic region0$Marine Ecology Progress Series74109-115NORTHEASTERN ATLANTIC-OCEAN, SANTA-CATALINA BASIN, DEEP-SEA FISH, ROCKALL TROUGH, NEAR-BOTTOM, MIDWATER, WATER, FLOOR, HYDROGRAPHY, ZOOPLANKTONhbThe availability of oceanic plankton and micronekton to the benthopelagic fish assemblages on the slopes of the Rockall Trough, a marginal region of the northeast Atlantic deep-sea environment, is examined. The vertical distribution of pelagic species predated by the fish was determined in the off-slope water column, as were the depths at which they are predated by the fish in the benthic boundary layer of the slope. The benthopelagic fish predated pelagic species at depths on the slope corresponding to the daytime depths of the pelagic prey. The occurrence of these pelagic species at the benthic boundary layer is primarily through truncation of their pelagic vertical distributions rather than horizontal impingement, although this does occur: this applies not only to epi- and mesopelagic but also to the bathypelagic species which can even reach abyssal sediments. Diel vertical migration of the pelagic species did not make them available to slope fishes in shallower depths presumably because vertical migration is strictly upwards within the pelagic water column and not up the contours of the slope sediment Maul, G. E 1951^WMonografia dos Peixes do Museu Municipal do Funchal: Famlias Macrouridae e Merluciidae,%Boletim do Museu Municipal do Funchal12 5-55 Maul, G. E 1952^WMonografia dos Peixes do Museu Municipal do Funchal: Famlias Gadidae e Bregmacerotidae,%Boletim do Museu Municipal do Funchal15 5-51 Maul, G. E 1959B;Aulostomus, a recent spontaneous settler in Madeiran waters,%Bocagiana, Museu Municipal do Funchal1 1- 18 Maul, G. E 1972|uOn a new species of the genus Callionymus from the Great Meteor seamount (Percomorphi, Callionymoidea, Callionymidae),%Bocagiana, Museu Municipal do Funchal30 1-8 Maul, G. E 1976tnThe fishes taken in bottom trawls by R. V. Meteor during the 1967 Seamount Cruises in the Northeast Atlantic$ Meteor Forschungsergebnisse No. 22  1-690RLMaycas, E. R. Bourdillon, A. Macquart-Moulin, C. Passelaigue, F. Patriti, G. 1999tnDiel variations of the bathymetric distribution of zooplankton groups and biomass in Cap-Ferret Canyon, France@9Deep-Sea Research Part Ii-Topical Studies in Oceanography4610 2081-20990*Deep-Sea Res. Part II-Top. Stud. Oceanogr.ISI:000082200300007TFnorthwestern mediterranean-sea; vertical nitrogen flux; submarine canyons; respiratory carbon; calanus-pacificus; migrant biota; near-bottom; migration; copepod; shelfaThe bathymetric distribution, abundance and diel vertical migrations (DVM) of zooplankton were investigated along the axis of the Cap-Ferret Canyon (Bay of Biscay, French Atlantic coast) by a consecutive series of synchronous net hauls that sampled the whole water column (0-2000 m in depth) during a diel cycle. The distribution of appendicularians (maximum 189 individuals m(-3)), cladocerans (maximum 287 individuals m(- 3)), copepods (copepods < 4 mm, maximum 773 individuals m(-3), copepods > 4 mm, maximum 13 individuals m(-3)), ostracods (maximum 8 individuals m(-3)), siphonophores (maximum > 2 individuals m(-3)) and peracarids (maximum > 600 individuals 1000 m(-3)) were analysed and represented by isoline diagrams. The biomass of total zooplankton (maximum 18419 mu g C m(-3), 3780 mu g N m(-3)) and large copepods ( > 4 mm maximum 2256 mu g C m(-3), 425 mu g N m(-3)) also were determined. Vertical migration was absent or affected only the epipelagic zone for appendicularians, cladocerans, small copepods and siphonophores. Average amplitude of vertical migration was about 400-500 m for ostracods, some hyperiids and mysids, and large copepods, which were often present in the epipelagic, mesopelagic, and bathypelagic zones. Large copepods can constitute more than 80% of the biomass corresponding to total zooplankton. They may play an important role in the active vertical transfer of carbon and nitrogen. (C) 1999 Elsevier Science Ltd. All rights reserved.HBTimes Cited: 1 English Article 229NH DEEP-SEA RES PT II-TOP ST OCE$://0000822003000073'hbUniv Mediterrannee, Ctr Oceanol Marseille, OSU, CNRS,UMR 6540,DIMAR, Campus de Luminy,Case 901, F-13288 Marseille 9, France Univ Mediterrannee, Ctr Oceanol Marseille, OSU, CNRS,UMR 6540,DIMAR, F-13288 Marseille 9, France Maycas ER Univ Mediterrannee, Ctr Oceanol Marseille, OSU, CNRS,UMR 6540,DIMAR, Campus de Luminy,Case 901, F-13288 Marseille 9, France W h2JT2350000660Atkinson, A. Ward, P. Williams, R. Poulet, S. A.vpFeeding Rates and Di915-926$://A1996VY72900001Angel, M. V. Rice, T. L.PJThe ecology of the deep ocean and its relevance to global waste management Journal of Applied Ecologylong-term problems; waste management; human population growth; deepsea; criteria north-atlantic ocean; hoplostethus-atlanticus; orange roughy; sea; marine; biodiversity; diversity; communities; population; pacificn1. As global human populations continue to grow uncontrollably, there is a foreseeable medium to long-term need for the utilization of deep ocean environments for disposal of waste materials to maintain sustainability of global environmental resources. 2. The assimilative capacity of deep ocean ecosystems is likely to be high relative to the quantities of waste that cannot be dealt with through alternative options such as waste minimization, recycling and incineration. 3. Deep ocean disposal may not be an acceptable option for the disposal of industrial organic compounds, which are persistent in the environment but for which alternative destructive procedures are available. 4. The choice of either a dispersive or accumulative regime for a disposal will need be based on the characteristics of the waste. Waste that is biologically or chemically degradable may best be dispersed. 5. Present knowledge of deep ocean ecosystems would suggest that disposal of inert, metal-rich, or even organic-rich wastes into accumulative regimes on the floor of the abyssal ocean would not create major deleterious impacts on living resources or other uses by Mankind of the oceans. Thus, under the present definition adopted by the Law of the Sea Convention this would not constitute large-scale pollution. 6. These tentative conclusions need to be evaluated by appropriately scaled experiments. Results from small-scale experimental procedures, based on the disposal of a few tonnes of waste and effecting a few square metres of sea-bed, cannot be extrapolated to predict confidently the impact of industrial scale disposal. Experiments approaching a tenth the size and extent of a full industrial exercise will be needed, but conducting such an experiment will not, in itself, carry significant environmental risk. 7. There are also some basic biological questions, mostly concerning the diversity of benthic assemblages and the processes that maintain their diversity, that will need to be resolved before deep-ocean disposal could be adopted. 8. There are major socio-economic problems about the global management of the abyssal ocean as a non-living resource which will have to be addressed internationally.J. Appl. Ecol. 1996 Oct335'SOUTHAMPTON OCEANOG CTR,EMPRESS DOCK,SOUTHAMPTON SO14 3ZH,HANTS,ENGLAND Angel MV SOUTHAMPTON OCEANOG CTR,EMPRESS DOCK,SOUTHAMPTON SO14 3ZH,HANTS,ENGLAND6/Times Cited: 5 English Review VY729 J APPL ECOLISI:A1996VY72900001ANIKEEV, V. S. LEBEDEV 2001LFGrenadier of the Middle-Atlantic Ridge is a perspective fishing objectMorskaya industriyay 2 10-12n in Russian ANON 1977hbBioresources of the open part of the Atlantic Ocean and methods of their studying and exploitationManual of methodsE 294 pp in Russian ANON.S 1974Brief description of results of the cruise of research BMRT-121 "Kivach" to the area of Reykjanes and Mid-Atlantic Ridges from 14 January to 30 June, 1974"Sevrybpromrazvedka. Murmansk 36 ppW in Russian ANON.S 1974Information on results of searching and catching of grenadier by BMRT-0421 "Polyarnoe Siyanie" on the Reykjanes Ridge in June, July and October, 1973"Sevrybpromrazvedka. Murmansk 31 ppW in Russian ANON.X 1975ZTOrganization of searching and fishery for deepwater fishes on the Mid-Atlantic Ridge<6PINRO,AtlantNIRO,Sevrybpromrazvedka,Zaprybpromrazvedka 205 pp in Russianpean Communities DG XIV/C/1 - Study contract 95/095 160pp Merrett, N. Re 1980Bathytyphlops sewelli (Pisces: Chlorophthamidae): a senior synonym of B. azorensis, from the eastern North Atlantic with notes on its biology.(Journal of the Linnean Society of London 68 (2) 99-109 Merrett, N. Rd 19860)Macrouridae of the eastern-north Atlantics0*Fiches dIdentification du Plancton (ICES) 173/174/17514Mikkelsen, P. M. 1995.(Cephalaspid opisthobranchs of the AzoresAoreana  Supl.193-215n*$Monaco, S. A. S. le Prince Albert de 1905.'Sur la campagne de la "Princesse-Alice"2+Bulletin du Muse Ocanographique de Monacot39 1-5&Monteiro, L. R. Furness, R. W.s (unpubl.)opSpeciation through temporal segregation of Madeiran storm petrel (Oceanodroma castro) populations in the Azores?BT(unpublished manuscript)dGosliner1990& Goulart1989 Gould1985 Gould1999 Gowing19877 Gowing19900 Gowing1992} Gowing19955| Gowing20000 Granadeiro1995, Granadeiro1998- Granadeiro1998. Granadeiro1998? Granadeiro1998/ Granadeiro1999@ Granadeiro19990 Granadeiro2000+ Grant1983a Grant1991z Greenblatt1988 Greenblatt1988 Greene1994 Greene2000 Grice1965 Grice1971Griffies1997s GRIGORJEV1972t GRIGORJEV1972u GRIGORJEV1982v GRIGORJEV1983w GRIGORJEV1988x GRIGORJEV1989 Grobecker1987 Gros20010C Groz_MP1999 GRUZOV1990y GRUZOV1997 Gudfinnson20000  Gudfinnsson2000 Guerra1998 Guerra1998 Guimares1882 Guimares1882 Guimares1884 Guimares1884Guinehut2002% Gunkel19933 Gunson19996 Gurney20000 Gurney20000GURVICH.1990zGUSHCHIN1981{GUSHCHIN1982|GUSHCHIN1982}GUSHCHIN1982~GUSHCHIN1982Gushchin1983GUSHCHIN1983GUSHCHIN1984Haedrich1964gHaedrich1965aHaedrich1970bHaedrich1977Haedrich1999 Hamer 1989 Hamer1994 Hamer1994SHamilton19922HHarbison1979 Harbour1997 Harbour1997o Harbour2001 Harding1987 Hardy1954o HAREIDE1994 HAREIDE1998Hargrave1987 Hargreaves1991 Hargreaves1999 Harris19911 Harris1997 Harris1997; Harris2000 Harris2000 Harris2001Harrison19888Harrison19899 Hartog1984 Harvey1988 Harvey1988 Hastie1994H Haury1979z Haury1988 Haury1988 Haury1994n Haury1995b Haury2000Hawkins 1990a Hawkins1987' Hawkins1990 Hawkins1992 Hawkins1994) Hawkins1994, Hawkins19959 Hay2000 Hays1994 Hays1995 Hays1996 Hays1997 Hays19979  Hays2001 Hays2001 Head19979 Head19979; Head2000 Head2000 Head20010: Heath19946 Heath20009 Heath2000 Heath2000[Heemstra1991]Heemstra1992_Heemstra1995Heemstra1995Hemleben19899 Henrich20026 Heptner1996 Herring1998>Hewitson1998( Heyman1983e Heywood2001E Heywood2001 Hilgendorf1888b* Hilton200001 Hilton2000CHilton_G199992 Hilton_GM20006 Hind20000 Hind20000r Hjort1912n Hobday1995 Hogg1980S Hollweg19921 Houston2000 Huang1992 Huber2002 Hughes19879 Hulsemann1965 Humes1996 Humes1996 Humes1998 Humes1998 Hureau19744 Hureau19799{ Hureau19800 Hureau19899 Huskin2001 Ibanez19977 Ibanez19977 ILJIN1976 INIP1985a INIP1985b INIP1985cS Ipavich19926Irigoien20000Irogoien20000 Isidro1987 Isidro1987a Isidro1987b Isidro1988 Isidro1989 Isidro1990a Isidro1990a Isidro1990b Isidro19919k Isidro19919 Isidro1996 IVANOV19888 IVANOV.1988f Iwamoto1971[ Iwamoto1973J1998 J.19919 J.19989pJaroslow2000 Jensen1995 John199490 Johnsen1998 Johnsen1999) Johnsen2001 Joint2001$ Jonasdottir19939 Jonasdottir2000 Jones1997 Jonsson1993S Joos19929y Juniper1992 Kaartvedt1989 Kaartvedt1994 Kaartvedt1994 Kaartvedt1996 KALUGIN1988 KALUGIN1989 KALUGIN1989 KALUGIN1989 KALUGIN1989 KALUGIN1990 KALUGIN1991 KALUGIN1991 KALUGIN1991} Kann19959 KAPRALOVA1983CKARASEV.1986KARASEVA2000 KASABOV1977 KASABOV1984I KASABOV1985gKASABOV.1982VKASATKIN1979 KASHKIN1977YKaufmann1992 Kaupp1991 KELLER1985 KEMENOV1979 KEMENOV1982 KEMENOV1987KEMENOV.19822 Kennedy2000 Kerdoncuff19949\ KHARZOVA.1981] KHARZOVA.1981 KHLIVNOY20010 Khripounoff2001 KHROMOV1986 Khromov1987 Khromov1997 Kiefer19979 Kikawa19707 Kirby1987KISELEV.1990 KISLITSYN1983 KISLYAKOV1973 Kissel2002o KJERSTAD.1994Klaveren1992 KLENOVA1975 KLIMENKOV1982 Klomp 19898 Klyuchnik1975: Knauer1992 Knud1995 Knudsen1995 Kobyliansky1996 Koefoed1932 Koeve2000 Koeve2002 Kolber19911G KOLCHIN1998 KOLESNIKOV1984 KOLESNIKOV1984 KOLESNIKOV1987 KOLESNIKOV1987 KOLESNIKOV19884 KOLESNIKOV.1977I KOLESNIKOV.1985 KOLESNIKOV.1988 KOLINKO1990 KOLINKO1990Kolmakov1990L KOLODNITSKY1985M KOLODNITSKY1986 KONOVALENKO.1988[ KONSTANTINOVA1981\ KONSTANTINOVA1981] KONSTANTINOVA1981XKONSTANTINOVA.1977YKONSTANTINOVA.1978 Koppelmann1992 Koppelmann1999- Koppelmann19999 Koppelmann19999 Koppelmann1999 KOPTEV1984L KOPTEV.1985M KOPTEV.1986N KOPTEV.1991 Korytov1989 Korytov1990 Korzun1976 Korzun1976 Korzun1979 Koslow1999 KOTENEV1968 KOTENEV1974 KOTENEV1976 KOTENEV1986 KOTLYAR1986 KOTLYAR1988 KOTLYAR1996KOVALEVA1981X Krause1994S Krauss1986 Krug1989w Krug1990 Krug1990 Krug19904 Krug199225 Krug19944 Krug19977 Krug19989:Kucheruk20000z KUKUEV19818 KUKUEV1984 Kukuev1985v KUKUEV1985 KUKUEV1985 KUKUEV1988 KUKUEV1988 KUKUEV1991 KUKUEV1998 KUKUEV2000 KUKUEV.1990 KUSMORSKAYA1960n KUZMICHEV.1984\ KUZMINA1981] KUZMINA1981[KUZMINA.1981 KUZNETSOV1985 KUZNETSOVA1985\L. V. PASHKOVA1981]L. V. PASHKOVA1981 LaCasce1999Y LaCasce1999 Laj2002 Lallier1994 Lampert1981 Lampert19899 Lampitt1993 Lampitt19938 Lampitt1995G Lamy20011 Lamy20011 Lance1962LANGEDAL1998 Languir1996 Laptikhovsky1994 Laptikhovsky1999C Laranjo_M1999Larnicol2002- Latif2000 LAVROV1979 LAVROV.1975 Lazzaro1987Le Fevre1986Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand19816Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand19816Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981 Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand1981Le Grand19816Le Grand1981Le Grand1981Le Grand1981   @v\utsrf ` 745-&$://A1997XD90300002i$Mullineaux, L. S. Mills, S. W.LEA test of the larval retention hypothesis in seamount-generated flowst<6Deep-Sea Research Part I-Oceanographic Research Paperstall isolated seamount; thermohaline structure; fieberling- guyot; deep-sea; invertebrate larvae; cobb-seamount; north pacific; ocean; currents; zooplanktonDistributions of larvae of benthic invertebrates in the water column near Fieberling Guyot, a tall seamount in the eastern tropical Pacific, were compared with studies of physical oceanographic processes in an effort to test the hypothesis that larvae are retained in seamount-generated flows. Field measurements of currents during 1990 and 1991 had shown that flows near the seamount were driven by tidal rectification, resulting in anticyclonic circulation over the summit and a vertical-radial circulation cell characterized by downwelling at the seamount center, outwelling at the level of the rim, and inward return flows above the level of the rim. No persistent, bottom-trapped, stagnant region was detected on the seamount, but the tidally rectified vertical-radial circulation could theoretically retain larvae. Larval abundances quantified in net samples collected near the seamount in September of 1989 and 1990 were slightly higher near the seamount center than over the flank or base (far field), but did not show the distinct, bottom-trapped aggregation expected from retention in a classic Taylor cap. Larval abundance patterns over the broad region of the seamount (even at the far field sampling locations) were, however, consistent with retention in the tidally rectified circulation. Hydroid colonization on settlement plates suspended on moorings for 6-and 13-month periods (an indirect measure of hydroid larval abundance) was concentrated over a narrow depth range (450-650 m) but extended radially over 40 km away from the seamount center, a pattern also consistent with larval transport and retention in the. tidally-rectified circulation cell. (C) 1997 Elsevier Science Ltd..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1997 May445'yWOODS HOLE OCEANOG INST,DEPT BIOL,WOODS HOLE,MA 02543 Mullineaux LS WOODS HOLE OCEANOG INST,DEPT BIOL,WOODS HOLE,MA 02543JCTimes Cited: 10 English Article XD903 DEEP-SEA RES PT I-OCEANOG RESISI:A1997XD90300002MUROMTSEV, A. Mi 196381Main features of hydrology of the Atlantic OceanrGidrometeoizdati 838 in RussianMurray, John Johan Hjort 1912The Depths of the Ocean - A general account of the modern science of oceanography based largely on the scientific researches of the norwegian steamer Michael Sars in the north Atlantic- Macmillan and Co  821Nafpaktitis, B. G 1968le Taxonomy and distribution of the lanternfishes, genera Lobianchia and Diaphus, in the north Atlantic Dana-Reportn  73n 1-131eNafpaktitis, B. Gi 1975tmReview of the lanternfish genus Notoscopelus (Family Myctophidae) in the North Atlantic and the Mediterranean0 Bulletin of Marine Science 25(1) Nakamura, Ie 1985Billfishes of the World: An annotated and illustrated catalogue of marlins, sailfishes, spearfishes and sword. fishes known to dateo FAO Fisheries Synopsis 125, Vol. 5  65Nakamura, I N. V. Parin  1993Snake mackerels and cutlassfishes of the World: An annotated and illustrated catalogue of the snake mackerels, snoeks, escolars, gemfishes, sackfishes, domine, oilfishes, cutlassfishes, scabbardfishes, hairtails and frostfishes known to datehFAO Fisheries Synopsis 125, Vol. 15o  1360)Nash, R. D. M. Geffen A. J. Santos, R. S. 1991uThe wyde-flounder, Bothus podas Delaroche, a singular flat fish in varied shallow-water habitats of the Azores. , (),*#Netherlands Journal of Sea Research27 3/4f367-3730"Nash, R. D. M. Santos, R. S. 1993UThe occurrence of the lesser weever (Echiichthys vipera) (Cuvier, 1829) in the Azores%7Journal of Fish Biology432317-319  j|NIZOVTSEV, G. PV 1989haNew data on distribution of Greenland halibut Reinhardtius hippoglossoides in the North AtlanticsVoprosy ikhtiologiiS  29(5)856-860 in Russian Nobre, A. 1924,%Contribuies para a fauna dos Aorese>7Anais do Instituto de Zoologia da Universidade do Portoc Vol. I 41-90f Nobre, A. 19304.Materiais para o Estudo da Fauna dos Aores. . Companhia Editora do Minho 108 pp Noji, T.T. 1991F?The influence of macrozooplankton on vertical particulate flux. sarsia76 1-9o Norman, J. R.e 1930:4Oceanic fishes and flatfishes collected in 1925-1927Discovery Reports1II271-370 (+ 2 plates) Nunn, P. D 1994Oceanic islands& Blackwell Publishers, Oxford, UKxv  413 Nybelin, O 1951\UIntroduction and station list.Reports of the Swedish Deep-Sea Expedition 1947-1948 IIZoology 1 1-28 Nybelin, O 1957^WDeep-sea bottom fishes. Reports of the Swedish Deep-Sea Expedition 1947-1948, Volume IIZoology  20250-345("Ohman,M.D Theilacker,G.H Kaupp,S.E 1991tmImmunochemical detection of predation on ciliate protists by larvae of the Northern Anchovy(engraulis mordax)d Biol. Bull.\ 181550-504Z499-523$://000085808900034(!Oschlies, A. Koeve, W. Garcon, V.tAn eddy-permitting coupled physical-biological model of the North Atlantic 2. Ecosystem dynamics and comparison with satellite and JGOFS local studies dataa"Global Biogeochemical Cyclesgeneral-circulation model; cold-core eddy; northwestern sargasso sea; euphotic zone; plankton community; tropical atlantic; pelagic ecosystem; bloom experiment; organic-carbon; spring bloomyf`A model of biological production in the euphotic zone of the North Atlantic has been developed by coupling a Nitrate, Phytoplankton, Zooplankton, Detritus (NPZD) nitrogen-based ecosystem model with an eddy-permitting circulation model. The upper ocean physical and biological results are presented for an experiment with monthly climatological forcing. A comparison with satellite ocean color data shows that the model is capable of a realistic description of the main seasonal and regional patterns of surface chlorophyll. Agreement is also good for primary production except in the subtropical gyre where the model produces values more than an order of magnitude smaller than derived from satellite observations. In situ data available at Joint Global Ocean Flux Study (JGOFS) time series and local study sites (Bermuda Atlantic Time-series Study (BATS), 32 degrees N, 65 degrees W; North Atlantic Bloom Experiment (NABE), 47 degrees N, 20 degrees W; EUMELI oligotrophic, 21 degrees N, 31 degrees W) are used for a more detailed analysis of the model's capability to simultaneously reproduce seasonal ecosystem dynamics in different biological provinces of the North Atlantic Ocean. The seasonal cycle of phytoplankton biomass and nitrate is simulated quite realistically at all sites. Main discrepancies between model and observations are a large zooplankton peak, required by the model to end the phytoplankton spring bloom at the 47 degrees N, 20 degrees W site, and the underestimation of primary production at EUMELI and under oligotrophic summer conditions at BATS. The former model deficiency can be related to the neglect of phytoplankton aggregation; the latter is caused by too inefficient recycling of nutrients within the euphotic zone. Model improvements are suggested for further steps toward a realistic basin-wide multiprovinces simulation with a single ecosystem model.Glob. Biogeochem. Cycle 2000 Mar141BW4-Relatrio da VII Semana das Pescas dos Aores7(1986)183-189ZTBiology; age; reproduction; growth; Geographical distribution; fisheries; statistics Isidro, E. J. 1987avContribuio para o estudo da biologia e pesca de boca-negra, Helicolenus dactylopterus (De la Roche, 1809) dos Aores>W4-Relatrio da VII Semana das Pescas dos Aores7 (1986)183-189 Isidro, E. J.i 1987bajAge and growth of the bluemouth Helicolenus dactylopterus dactylopterus (De la Roche, 1809) off the Azores HICES, CM 1989/G:63 6 pp + figs Isidro, H. A. 19880)A pesca dos pequenos pelgicos nos Aoresi4.Relatrio da VIII Semana das Pescas dos Aores8 (1987)183-186sFisheries; statisticst  Isidro, E. 1989Cresimento e reproduo de Helicolenus dactylopterus (De la Roche, 1809). Provas de Acesso Categoria de Assistente de Investigao4 Horta D>Departamento de Oceanografia e Pescas, Universidade dos Aores 40pp+2 anexos ("Biology; age; growth; reproduction Isidro, H. A.t 1990asDAge and growth of Trachurus picturus (Bowdich, 1825) from the Azores$ Arquiplagot Life and Earth Sciences, 8 45-54PJBiology; age; growth; fisheries; statistics; fisheries biology; parameters Isidro, H. A.p 1990asFAge and growth of Trachurus picturatus (Bowdich, 1825) from the Azores& Arquiplagol Life and Earth Sciences8  45-54  Isidro, H. A. 1990bsEstudo do Chicharro (Trachurus picturatus Bowdich, 1825) (Teleostei, Carangidae) dos Aores Provas de Acesso Categoria de Assistente de Investigac) Horta D>Departamento de Oceanografia e Pescas, Universidade dos Aores 64pp + anexos@9Fisheries; statistics; biology; age; growth; reproduction Isidro, E. 1996b[Biology and population dynamics of selected demersal fish species of the Azores Archipelagot:4Department of Environmental and Evolutionary Biology University of Liverpooly vi +m249pp (+3 appendices) PhD}<5Fisheries biology; biology; age; growth; reproductionn PT A-OCEANOG RESISI:A1992JY326000042+TSYGANOV, V.F I. K. SIGAEV Yu. A. LOKTIONOVe 1982Distribution of Available Potential Energy, Geostrophic Circulation and Biological Productivity Indices in Two Areas of the North AtlanticNAFO SCR Doc. 82/IX/101Serial No 610. in Russian Tucker, G. M. Heath, M. F. 19940*Birds in Europe: their conservation statusBirdLife International  Cambridgea"BirdLife Conservation Series No. 3n  600pp  B RtQ alley, L. D. McCartney, M. S.LEAn Eastern Atlantic Section from Iceland Southward across the Equator<6Deep-Sea Research Part a-Oceanographic Research Paperspolar mode water; north-atlantic; mediterranean water; norwegian-greenland;  Wohlleben,T.M.H Weaver,A.J 1995F?Interdecadal climate variability in the subpolar North AtlanticClimate Dynamics118t459-4671SEA-SURFACE TEMPERATURE, INTERPENTADAL VARIABILITY, THERMOHALINE CIRCULATION, GENERAL-CIRCULATION, FRESH-WATER, OCEAN, SALINITY, ICE, MODEL, FLUCTUATIONSThe statistical relationships between various components of the subpolar North Atlantic air-sea-ice climate system are reexamined in order to investigate potential processes involved in interdecadal climate variability. It is found that sea surface temperature anomalies concentrated in the Labrador Sea region have a strong impact upon atmospheric sea level pressure anomalies over Greenland, which in turn influence the transport of freshwater and ice anomalies out of the Arctic Ocean, via Fram Strait. These freshwater and ice anomalies are advected around the subpolar gyre into the Labrador Sea affecting convection and the formation of Labrador Sea Water. This has an impact upon the transport of North Atlantic Current water into the subpolar gyre and thus, also upon sea surface temperatures in the region. An interdecadal negative feedback loop is therefore proposed as an internal source of climate variability within the subpolar North Atlantic. Through the lags associated with the correlations between different climatic components, observed horizontal advection time scales, and the use of Boolean delay equation models, the time scale for one cycle of this feedback loop is determined to have a period of about 21 years. Woods, L. P. 1957,&Beryx splendens Lowe in Gulf of Mexico Copeia, 1957  (4)298-299Wroblewski,J.S 1982{Interaction of currents and vertical migration in maintaining calanus marshallae in the oregon upwelling zone-a stimulationsDeep Sea Researchl296A665-686ZAFERMAN, M. L 1977@9On behaviour of roundnose grenadier in the fishing groundRybnoe khozyaistvo 4 19-21t in RussianZAFERMAN, M. L 1986LFOn behaviour of roundnose grenadier by data of underwater observations(" Underwater fishery investigations 5-14 in Russian$ZAFERMAN, M. L A. M. SENNIKOVK 1986RKBiology and peculiarities of behaviour of deepwater crab Geryon quinquedens\HBThe union conference of commercial invertebrates. Theses of papers  43-45 in Russian"ZAFERMAN, M. L V. E. KEMENOV 1987PJDynamics of waters and behaviour of fish. Meeting of Soviet oceanographersTheses of papersPart II. Leningrad  16-17 in Russian&Zaferman, M. L. Sennikov, A. M. 1991`ZDistribution, biology and behaviour of deepwater crabs in open areas of the North Atlantic VNIRO 1991 69-80tZAFERMAN, M. L 1991haOn behaviour of roundnose grenadier Coryphaenoides rupestris (by data of underwater observations)NVoprosy ikhtiologii  31(6) in Russian$ZAFERMAN, M. L A. M. SENNIKOVK 1991hbDistribution, peculiarities of biology and behaviour of deepwater crabs in the open North AtlanticHB Biological resources of the thalassic bathyal of the World Ocean 69-80s in Russian$ZAFERMAN, M. L I. P. SHESTOPAL 1991tnUnderwater search for fish and deepwater longlining in the areas of underwater mountains of the North Atlantic PINROR  50-77 in Russian2,ZAFERMAN, M. L. V. N. SHIBANOV A. N. KALUGIN 1991Studies of behavior and distribution of round-nose grenadier in the Mid-Atlantic Ridge region with using of submersible Sever-22>7Biological resources of the World Ocean thalassobathyala 62-696 in Russian20171207400006fjdKhripounoff, A. Vangriesheim, A. Crassous, P. Segonzac, M. Colaco, A. Desbruyeres, D. Barthelemy, R.~xParticle flux in the Rainbow hydrother179-195$://A1994NA80700010SRKKaartvedt, S. Vandover, C. L. Mullineaux, L. S. Wiebe, P. H. Bollens, S. M.,4.Amphipods on a Deep-Sea Hydrothermal Treadmill<6Deep-Sea Research Part I-Oceanographic Research Papers'<5WOODS HOLE OCEANOG INST,DEPT BIOL,WOODS HOLE,MA 02543mid-atlantic ridge; oxygen-consumption; euphausia-superba; vent field; ocean; macrozooplankton; communities; swarms; rates; size$Conspicuous swarms of a pardaliscid amphipod were observed at about 2520 and 2580 m depth in the East Pacific Rise vent field during dives with the submersible Alvin. Swarms occurred in association with mussels, clams and tubeworms, and were located above, and immediately downstream of cracks with emanating hydrothermal water. Numerical density sometimes exceeded 1000 individuals l-1, which is 3 orders of magnitude greater than and previous report on pelagic crustaceans from the deep sea. The amphipods, however, were not obligatory swarmers, and thin- layered shoals and scattered individuals were observed. Orientation of individuals was often polarized as they headed into the venting flow, swimming vigorously at 5-10 cm s-1 to maintain their position in the current. Retention within the preferred habitat requires an average swimming speed corresponding to the average current speed, suggesting a sustained swimming of >10 body lengths s-1. These observations contrast with the general concept of low swimming activity in deep-sea crustaceans..(Deep-Sea Res. Part I-Oceanogr. Res. Pap. 1994 JanD411nHBTimes Cited: 8 English Article NA807 DEEP-SEA RES PT I-OCEANOG RESISI:A1994NA80700010n145-156$://A1996UP52100010t Kaartvedt, S.rpiHabitat preference during overwintering and timing of seasonal vertical migration of Calanus finmarchicusOpheliaUnova-scotia shelf; fish benthosema-glaciale; western norway; life-history; winter distribution; st-lawrence; zooplankton; copepod; micronekton; variabilityCalanus finmarchicus (Copepoda) appears to be very flexible with respect to physical characteristics of the overwintering habitat. Data from the literature document successful overwintering at depths ranging from about 2000 m to near the surface, and temperatures ranging from -1 to +11 degrees C. I argue that reducing encounters with predators may be a major driving force for C. finmarchicus to select their overwintering habitat. Preliminary analyses from Norwegian fjords suggest that overwintering C. finmarchicus may distribute vertically so as to reduce danger of predation by mesopelagic fish. Episodic presence of planktivorous fish may influence timing of seasonal vertical migrations of Calanus populations.Ophelia 1996 Apr44 1-3'rkUNIV OSLO,INST BIOL,POB 1064,N-0316 OSLO,NORWAY Kaartvedt S UNIV OSLO,INST BIOL,POB 1064,N-0316 OSLO,NORWAY4-Times Cited: 20 English Article UP521 OPHELIAISI:A1996UP52100010$KALUGIN, A. N. V. N. SHIBANOV. 1989^XOn ecology of roundnose grenadier of some underwater mountains of the Mid-Atlantic Ridge4. Complex studying of the Atlantic Ocean nature 146-147 in Russian2,KALUGIN, A. N. I. E. LOMAKIN V. N. SHIBANOV. 1991d]Relief of underwater mountains, local dynamics of waters and distribution of marine organisms1B://A1990EH36700022$Galkin, S. V. Moskalev, L. I.2,Fauna of the Mid-Atlantic Ridge Hydrothermal Okeanologiya Okeanologiya 1990Sep-Oct305'ZSPP SHIRSHOV OCEANOL INST,MOSCOW,USSR GALKIN SV PP SHIRSHOV OCEANOL INST,MOSCOW,USSR81Times Cited: 8 Russian Article EH367 OKEANOLOGIYAISI:A1990EH36700022X rx2+KOTENEV, B. N. V. V. NAZIMOV V. D. RVACHEV.  1974*$Geomorphology of the Reykjanes Ridge Trudy VNIROn  98o 98-109 in RussianKOTENEV, B. N. 1976pjUnderwater canyons of the Atlantic Ocean and their influence on the biological productivity of deep waters Fisheries oceanography 2 1-49 in RussianKOTENEV, B. N. 1986@:Topogenic areas of the increased bioproductivity of waters0*Biological resources of the Atlantic Ocean 35-51O in RussianKOTLYAR, A. N. 1988~wAtlantic roughy Hoplostethus atlanticus Collett (Trachichthyidae, Beryciformes): distribution and commercial importance0Biological resources of the thalassobathyal zone of the World Ocean. Abstracts of the All-Union Conference on studies of fishes of the World Ocean thalassobathyal. (Pybnoye, November 1988)32 in RussianKOTLYAR, A. N. 1996*$Oceanic fish of the Berycidae family VNIRO  368pN in Russian& KOVALEVA, A. A. A. V. GAEVSKAYA. 1981^WOn new findings of Microsporidia of Parvicapsula genera in fish of the Atlantic OceanaZoologichesky zhurnala LX() in Russian221-235$://A1994QB20400010 Krause, D. C. Angel, M. V.<6Marine Biogeography, Climate-Change and Societal NeedsProgress in Oceanography:4doppler current profiler; abundance; patterns; waterPelagic biogeography deals with the large scale distributional patterns of pelagic organisms in the world's oceans, their origins through evolution and the changes in ocean morphology during the geological past, and the factors which currently control and maintain them. The knowledge it generates has a wide variety of uses in science, both basic and applied, and in socio-economics. Its products include: (1) Distributional data compiled in data bases, maps and atlases; (2) Explanatory scientific and non-scientific publications on the distributions and their implications; (3) Standardisation of methodologies; (4) Trained specialists; (5) Advice to society on oceanic aspects of global resource management; and (6) Assessments of oceanic biodiversity in relation to the Biodiversity Convention. The immediate users of this knowledge include oceanographers in other disciplines, ecologists, applied scientists and engineers, resource managers, fishermen, environmentalists, teachers, international lawyers and policy- makers. At present the largest users are the natural resource managers seeking to optimise and to sustain the resource for which they are responsible. There is a considerable body of national and international legislation which is underpinned by biogeographical information. Similarly much of our understanding about past climate which is being used to predict future trends, is based on applying information on present-day distributional patterns to the interpretation of the fossil record in marine sediments. Global change, in the ocean, the atmosphere and on land, is strongly modulated by the feedback between marine organisms, nutrients and greenhouse gases, The marked coherence observed between the distributions of physical, chemical and biological patterns suggest that the processes involved in this feedback are linked with pelagic community structure. Remote sensing of sea-surface properties and the heat content of the mixed-layer, offer considerable potential for linking ecological and biogeographical processes to large scale features of ocean circulation and climatology. The long-term monitoring of the ocean in the Global Ocean Observing System will need to integrate physical, chemical and ecological data, if the models used to predict future change are to achieve adequate precision. The future use and resource management of the oceans has to involve biogeographical information. Traditional sampling methods, even when supplemented by large scale surveys such as CALCOFI and the Continuous Plankton Recorder surveys,will never provide sufficient data, so new techniques for intensive sampling and monitoring are being sought. Some surrogate measures such as chlorophyll fluorescence are already well established as standard oceanographic methodology; others involving acoustics and optical properties have the potential for sampling the biological characteristics at the same time/space scales as the physicochemical properties of the oceans are being studied. However, the calibration of these new techniques against traditional sampling and observational methods remains problematic. Information technology is beginning to be used, not only to unify the systematics of many taxonomic groups, but also to improve information exchange. Improvements in digital data bases will lead to freer exchange of information, and also facilitate the production of maps and interpretations customized for other users. The scientific resources being devoted to pelagic biogeography are declining with potentially serious consequences. This trend can only be reversed if the biogeographers themselves make their output more accessible and user-friendly for non-scientists, and take advantage of the new technologies which promise to re-vitalise the field.Prog. Oceanogr. 199434 2-3'UNIV CALIF SANTA BARBARA,INST MARINE SCI,SANTA BARBARA,CA 93106 INST OCEANOG SCI,DEACON LAB,GODALMING GU8 5UB,SURREY,ENGLAND KRAUSE DC UNIV CALIF SANTA BARBARA,INST MARINE SCI,SANTA BARBARA,CA 9310681Times Cited: 1 English Review QB204 PROG OCEANOGRISI:A1994QB20400010 KJZ`hI|-,@:New views of the Atlantic. Topical studies in oceanography Deep-Sea Research Part II 46 1-2p. 1990@9Check-list of the Fishes of the Eastern Tropical Atlantice B;Quro, J. C. Hureau, J. C. Karrer, C. Post, A. Saldanha, L. Lisboa  UNESCO, JNICT6Vol. I, II, III. pp. 1-1492 Expedio Aores/89 1990PIEcologia e Taxonomia do Litoral Marinho dos Aores: Relatrio Preliminar,p  Horta, Aores ,%Departamento de Oceanografia e Pescas\<6Parte I, Vol. 1, 1-177, Vol. 2, 178-371 Parte II, 1-44$AGAFONOVA, T. B. E. I. KUKUEV. 1990@9New data on distribution of Cubiceps gracialis Lowe, 1843nVoprosy ikhtiologii, 30(6)t 1028-1031t in Russian.r Agostinho, J. 1954 Notas ornitolgicasAoreanaV  (2)184-1868Aguiar, A. Pereira, J. 1982uPhysiculus dalwigki Kaup, 1858 and Gadella maraldi (Risso, 1810) newly recorded in Azorean waters (Pisces: Moridae).#3 Cybium63 35-38B;Geographical distribution; new records;anatomy; morphometry Aken, H. M. C. J. De Boer 1995\VOn the synoptic hydrography of intermediate and deep water masses in the Iceland BasinDeep-Sea Research I422165-189Aken, H. M. van Becker 1996b[Hydrography and through-flow in the north-eastern North Atlantic Ocean: the NANSEN project.Progress in Oceanography38?297-3463 7-28$://A1996UP52100002r"Aksnes, D. L. Blindheim, J.tmCirculation patterns in the North Atlantic and possible impact on population dynamics of Calanus finmarchicus1Ophelia|diel vertical migration; western norway; winter distribution; zooplankton; masfjorden; lindaspollene; micronekton; fish; sea& Due to advective impact few consistent time-series describing the population development of the copepod C. finmarchicus exist. Quantitatively, the spring generation seems to be the most important, and especially in the northern areas one generation per year seems to prevail. A fecundity of 10(2)- 10(3) eggs female(-1) and a sex ratio 1:1 then give a maximal reproductive rate of 3.9-6.2 year(-1). This low rate seems to be compensated by low mortality due to effective predator avoidance in terms of diurnal and seasonal vertical migrations. We have calculated that the advective renewal of the habitats of C. finmarchicus in the subpolar gyre and in the Nordic Seas are 0.13 and 0.29 year(-1) respectively while the birth and death rates of C.finmarchicus typically are above 3.9 year(-1). This means that the biological rates are likely to dominate over the advective rates in the two ocean areas, and that the C.finmarchicus development is facilitated by Ic cal production in both areas. Rough calculations for the Nordic Seas indicate that our of a total annual production of 74 mill. tonnes, 3.6 mill. tonnes are lost to adjacent seas by advection. Due to the flow of deep and cold waters southward and the seasonal migration of C. finmarchicus it is likely that the loss of individuals from the Nordic Seas southward to the North Atlantic is dominated by copepodite V, and that a higher proportion of younger life stages are carried in the south- north (Barents Sea) and west-east (Norwegian coast and the North Sea) directions with the warmer, Atlantic Water.Ophelia: 1996 Apr244 1-3 4-Times Cited: 25 English Article UP521 OPHELIARISI:A1996UP521000020}|{zyxwl2@  Nesis, K.N.t 1984<6Deep-sea cirrate octopuses observed from a submersibleDeep-Sea NewsletterNo. 9: 7 In English Nesis, K.N., 1985>8Oceanic cephalopods: Distribution, life forms, evolution Moscow: Nauka 287 p In RussianB;Nesis, K.N. Amelekhina, A.M. Boltachev, A.R. Shevtsov, G.A.t 1985`YRecords of giant squids of the genus Architeuthis in the North Pacific and South AtlanticZoologichesky Zhurnalr 64(4)W518-528&In Russian with English summary Nesis, K.N., 1987LECephalopods of the World. Squids, Cuttlefishes, Octopuses, and Allies&T.F.H. Publications, New Jersey 351 pages Nesis, K.N.s 19910)Underwater cephalopod studies in the USSRAn anotated bibliography"Cephalopod Newsletter, N 14 11-18  In English Nesis, K.N., 19922,Cephalopods of underwater rises in the ocean$Doklady Akademii Nauk, 322(5) 322(5) 1003-1006 In Russian Nesis, K.N. 19934.Cephalopods of seamounts and submarine ridges,60 Recent Advances in Cephalopod Fisheries Biology$Tokyo: Tokai University Pressi365-373 Nesis, K.N.i 1996B;Mating, spawning and death in oceanic cephalopods: a review  Ruthenicad 6(1) 23-64 &In English with Russian summaryi Nesis, K.N.i 2000LESquid family Onychoteuthidae: phylogeny, biogeography and way of lifea"Zoologicheskii Zhurnal, 2000  79(3)272-281m&In Russian with English summaryNHNesis, K.N. Arkhipkin, A.I. Nikitina, I.V. Middleton, D.A.J. Brickle, P. 2001A new subspecies of the bathyal sepiolid cephalopod Neorossia caroli (Joubin, 1902) from the southwestern Atlantic off the Falkland IslandsRuthenica, 20010 10(1)1 51-565&In English with Russian summaryNHNesis, K.N. Arkhipkin, A.I. Nikitina, I.V. Middleton, D.A.J. Brickle, P. 2001A new subspecies of the bathyal sepiolid cephalopod Neorossia caroli (Joubin, 1902) from the southwestern Atlantic off the Falkland IslandsRuthenica, 2001, 10(1) 51-565In English with Russiann Neto, A. I.f 1992XQContribution to the taxonomy and ecology of the Azorean benthic marine Algae. , ,70)Biological Journal of the Linnean Society346163-176  Neto, A. I.  1994:3Checklist of the benthic marine algae of the Azoresr ArquiplagoeLife and Marine Sciences 12A2 15-34  Neumann, G. 1968Ocean currents "Amsterdam, London, New Yorkl Elsevier 352r Neuville, HV 1897leRemarques anatomiques sur les Squales observs pendant la dernire campagnes du yacht Princesse Alice.'Bulletin du Musum dHistoire Naturellec 35 Neuville, H. 1900PJLintestin valvulaire de la Chimre monstrueuse (Chimaera monstrosa Linn)$Bulletin de la Socit Philoms 9e sr., t.III59 Nielsen, J. G 1968XQRedescription and reassigment of Parabrotula and Leucobrotula (Pisces: Zoarcidae)NHVidenskabelige Meddelelserfra Dansk Naturhistorisk Forening i kjbenhavn 131225-249Nielsen, J. G Smith, D s 1978<6 The eel family Nemichthyidae (Pisces: Anguilliformes) Dana-Reporte  88  1-71"Nielsen, J. G J.- C. Hureau  1980Revision of the ophidiid genus Spectrunculus Jordan & Thompson 1914, a senior synonym of Parabassogigas Nybelin, 1957 (Pisces: Ophidiiformes) Steenstrupia6149-169"Nielsen, J. G E. Bertelsen e 1985F?The gulper-ell family Saccopharyngidae (Pisces: Anguilliformes)  Steenstrupia 11 (6)157-206m.'Nielsen, J. G J. Baddock N. R. Merrett  1990^XNew data elucidating the taxonomy and ecology of the Parabrotulidae (Pisces: Zoarcoidei)Journal of Fish Biology37437-448 ~>TH\2*#Nierop, M. M. van Hartog, J. C. den 1984A study on the gut contents of five juvenile loggerhead turtles, Caretta caretta (Linnaeus) (Reptilia, Cheloniidae), from the South-Eastern part of the North Atlantic Ocean, with emphasis on coelenterate identificationAPZoologische Mededelingen594 35-53Nigmatullin, Ch.M. 1976:3Ecological groupings of squid family OmmastrephidaetTN Problems of the Study of Pelagic Fish and Invertebrates of the Atlantic Oceand]Abstracts of Communications of the Young Scientists Conference, AtlantNIRO, Kaliningrad, 1976 14-15  In Russian("Nigmatullin, Ch.M. Pinchukov, M.A. 1976\VFeeding of the squid Ommastrephes bartrami in the Atlantic Ocean and Mediterranean Sea Problems of the Study of Pelagic Fish and Invertebrates of the Atlantic Ocean. Abstracts of Communications of the Young Scientists Conference, AtlantNIRO, Kaliningrad, 1976720 In RussianNigmatullin, Ch.M. 1977RKTaxonomic relations and ecological structure of squid family Ommastrephidaentn All-USSR Scientific Conference on the Use of Commercial Invertebrates for Food, Fodder and Technical PurposesB://A1993MP15800006F Angel, M. V.(!Biodiversity of the Pelagic OceanTConservation BiologyThis paper reviews knowledge of biodiversity in open ocean pelagic communities and discusses the possible causal factors for the patterns. The oceanic pelagic ecosystem is by far the largest on Earth and, although locally its assemblages may be as rich as many terrestrial ecosystems, its global diversity (at both a species and an ecosystem level) is low. There are latitudinal trends in pelagic species diversity similar to those in many terrestrial taxa. High species richness in the oceans, however, tends to be associated with regions of low productivity that lack strong seasonality in the production cycle. The richest zones occur at the boundaries between different types of oceanic water where different faunas are mixed together, but the geographical locations of these boundaries are unstable and shift seasonally by hundreds of kilometers. If high diversity is emphasized in the development of protocols for conservation, then not only will the oceans receive low priority in conservation and resource management, but the regions most important in terms of process will also be overlooked. The scales of oceanic systems are so large that the methodologies developed for terrestrial conservation and resource management are inapplicable Biodiversity may be regarded as the principal criterion for developing management strategies, yet the links (if any) between the ecological processes in the ocean that play such an important role in global homeostasis remain poorly characterized. The basis for a predictive understanding of the interaction between diversity and ecological process can be greatly enhanced relatively inexpensively by systematically collating existing data and working up extant collections of materialConserv. Biol. 1993 Dec74'INST OCEANOG SCI,DEACON LAB,WORMLEY GODALMING GU8 5UB,SURREY,ENGLAND ANGEL MV INST OCEANOG SCI,DEACON LAB,WORMLEY GODALMING GU8 5UB,SURREY,ENGLAND81Times Cited: 17 English Review MP158 CONSERV BIOL ISI:A1993MP15800006i\@[  <H808-810$://000076754200029&Astthorsson, O. S. Gislason, A.XQEnvironmental conditions, zooplankton, and capelin in the waters north of Iceland$Ices Journal of Marine Science>7capelin; environment; Icelandic waters; zooplankton codThe waters north of Iceland are characterized by large hydrographic fluctuations. Warm and cold years are distinguished on the basis of the hydrography. Time-series data reveal that zooplankton biomass, capelin biomass, and capelin weight-at-age are ail greater during warm years than during cold years. The chain of events that links hydrographic conditions with the observed ecological variations is discussed. (C) 1998 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 1998 Aug554'Marine Res Inst, Skulagata 4,POB 1390, IS-121 Reykjavik, Iceland Marine Res Inst, IS-121 Reykjavik, Iceland Astthorsson OS Marine Res Inst, Skulagata 4,POB 1390, IS-121 Reykjavik, Iceland:3Times Cited: 3 English Article 134QN ICES J MAR SCIISI:000076754200029 49-56$://A1992JT2350000660Atkinson, A. Ward, P. Williams, R. Poulet, S. A.vpFeeding Rates and Diel Vertical Migration of Copepods near South Georgia - Comparison of Shelf and Oceanic SitesMarine Biologycalanus-propinquus; calanoides-acutus; weddell sea; adaptive significance; rhincalanus-gigas; life-cycles; zooplankton; phytoplankton; patterns; behaviorSeventeen Longhurst Hardy Plankton Recorder profiles were taken over a diel cycle in January 1990 to study the feeding of four major copepods over the South Georgia shelf. Ontogenetic changes in vertical migration were followed and feeding cycles determined by gut fluorometry for Calanoides acutus Stage CV, Calanus simillimus CV and CVI female, C. propinquus CV and Rhincalanus gigas CV and CVI female. In common with a neighbouring oceanic site visited two weeks later and reported elsewhere, all four species had a diel cycle of feeding and migration. The vertical distributions of C. simillimus (all stages), R. gigas (nauplii) and Euphausia frigida (postlarvae) were similar at both sites, the night being spent within the chlorophyll maximum at 15 to 30 m. However, the biomass dominants, C. acutus and R. gigas, dwelt below the chlorophyll maximum, about 30 m deeper than their oceanic counterparts. Unlike the oceanic site, feeding at the shelf site was not restricted to darkness, but increased 6 to 10 h before nightfall and finished at dawn, the intervening period coincided with sinking and digestion. Daylight feeding may have been induced by the shorter night, lower light levels or greater food requirements at the shelf site, despite planktonic predators being over three times more abundant. Daily ration estimates for R. gigas at both sites were only approximately 2% body carbon per day. These low values contrast with its smaller competitors, whose rations were in the range 5.6 to 27%. Mar. Biol. 1992 Sep 1141'NERC,BRITISH ANTARCT SURVEY,HIGH CROSS,MADINGLEY RD,CAMBRIDGE CB3 0ET,ENGLAND PLYMOUTH MARINE LAB,PLYMOUTH PL1 3DH,DEVON,ENGLAND CNRS,BIOL STN,F-29680 ROSCOFF,FRANCE ATKINSON A NERC,BRITISH ANTARCT SURVEY,HIGH CROSS,MADINGLEY RD,CAMBRIDGE CB3 0ET,ENGLAND4.Times Cited: 39 English Article JT235 MAR BIOLISI:A1992JT23500006B;Azevedo, J. M. N. Neto, A. I. Heemstra, P. C. Arruda, L. M.t 1991$Peixes marinhos de Santa Maria<6Relatrios e Communicaes do Departamento de Biologia19 49-51nHAEcology; demography; vertical distribution; feeding; biology; age7Azevedo, J. M. N. 1992`Nota sbre os meros, Epinephelus marginatus (Lowe, 1834) (Pisces: Serranidae), nas Lajes do Pico.*<6Relatrios e Communicaes do Departamento de Biologia20 35-37(!Ecology; demography; biology; age    % - 5[   , .n /)  6 Z  K<  k t#l 2 ? @W3  B ~ bI #":XRQN gM mU ~ p xf<  |F I    0  \Mtq N    >z _9L  y`V:X     V {^   g !rZ Rl B ER 6J[Rhx;:9876,54Mba `:_^F]B;Azevedo, J. M. N. Heemstra, P. C. Arruda, L. M. Neto, A. I.o 199281Peixes marinhos litorais da ilha do Pica (Aores)t<6Relatrios e Communicaes do Departamento de Biologia20 27-33 ChecklistoAzevedo, J. M. 1992`Nota sobre os meros, Epinephelus marginatus (Lowe, 1834) (Pisces, Serranidae), nas Lajes do Pico,RLRelatrios e Comunicaes do Departamento de Biologia, Ponta Delgada, Aores$PICO/91: Expedio Cientficat 35-37 Azevedo, J. M. N. 1995`ZFood web of the Azorean shallow water marine ichthyological communities: a guild approach.,%Boletin do Musea Municipal do FunchalnSuplemento no. 4 29-53 "Checklist; ecology; feeding(!Azevedo, J. M. N. Heemstra, P. C.y 19952,New records of marine fishes from the Azores ArquiplagoLife and Marine Sciences 13A 1-10rkSystematics; diagnosis; anatomy; morphology; meristics; morphometry; geographical distribution; new recordsr2+Azevedo, J. M. Heemstra, P. C. Brum, J. M.t 19952+New records of fishes known from the Azores.,%Arquiplago, Life and Marine Sciences 13A6$Azevedo, J. M. N. Brum, J. M.in pressqFirst record of the Sailfin Roughshark Oxynotus paradoxus Frade, 1929 (Chondrychthyes, Oxynatidae) for the Azoresc'9 CybiumD>Systematics; diagnosis; Geographical distribution; new recordsB7Problems of the fishery oceanography of the World Ocean 71-72 in Russian&BAIDALINOV, A. P. L. I. PEROVA.  1979^XOn weight and chemical composition of liver of roundnose grenadier of the North AtlanticTrudy AtlantNIRO No. 79 32-36 in Russian BAKAY, Yu. I.s 1984rkData on fauna of parasites of deep-sea redfish (Sebastes mentella) from various areas of the North Atlantic~wProblems of studying and rational exploitation of biological resources of seas of the European North and North Atlantic  40-41 in Russian"BAKAY, Yu.I. A.V. Zubchenko. 1984lfParasites of roundnose grenadier (Coryphaenoides rupestris) in two areas of the North Atlantic in 1981Annales Biologiquesi38200-201. BAKAY, Yu.I. 1988Application of results from parasitological investigations in redfish (Sebastes mentella Travin) populational structure studies. ICES C.M. 1988/G:35. BAKAY, Yu. I.s 1992On interrelation between alfoncino (Beryx splendens Love) concentrations from different areas of the North Atlantic by data of parasitological investigations4.Pathology and parasitology of marine organisms 6-7S in Russian BAKAY, Yu. I. 1997NGParasites of sea redfishes of the Sebastes genera of the North AtlanticMurmansk 43 ppp in RussianBALABANOVA, L. G.  1981jcYear-to-year and seasonal variability of water masses borders in the area of the Mid-Atlantic RidgeRLBiological Resources of Deep Water and Pelagic Layer of the Open World Ocean 47-499 in Russian("Bannerman, D. A. Bannerman, W. M. 1966RLBirds of the Atlantic Islands, Vol. 3 - A History of the Birds of the Azores Oliver and Boyd, Edinburgh 262 pp B,ED@ Steiner, L 1995tn Rough-toothed dolphin, Steno bredanensis: a new species recorded for the Azores, with some notes on behaviour,&Arquiplago - Life and Marine Sciences 13A125-128 21-37$://A1993LR15800002& Stewart, K. M. Sutherland, J. W.:4Zooplankton Migration in 3 Lakes of Western New-York6/Internationale Revue Der Gesamten HydrobiologieVzooplankton migration; chaoborus; restricted dispersal; chaos diel vertical migration; fresh-water zooplankton; chaoborus; predation; larvae; distributions; communities; cladocera; advantageWe examined the diel vertical migration (DVM) of zooplankton in three lakes of western New York; Lakes Conesus, Lime, and McCargo. In all three lakes, the dipteran predator Chaoborus was a more dramatic migrator than any of the cladocerans or copepods. In contrast, another invertebrate predator, Leptodora, seemed to have the least vertical dispersal. In Conesus Lake, following the evening ascent and upper-water night-positioning of Chaoborus flavicans, Daphnia pulicaria expanded its own vertical range of dispersal thereby decreasing its degree of overlap with Chaoborus. The vertical distribution of Diaptomus sicilis was mostly below that of Daphnia pulicaria, thus reducing possible competition for food resources. Poor oxygen conditions in the lower waters of Lakes Lime and McCargo restricted all zooplankton (except Chaoborus) to an epilimnetic zone where the regions of niche overlap and predation were narrowed. Such annually-induced restrictions on vertical dispersal are probably common features of numerous stratified lakes with hypolimnetic reducing conditions. No fixed pattern of vertical dispersal or migration is likely in lakes where stratification and non-stratification follow each other seasonally. Vertical migration does provide some flexibility in niche separation, but the potential for chaotic behavior in interacting predators and prey may confound simple explanations of DVM.$Int. Rev. Gesamten Hydrobiol. 1993781'SUNY,DEPT BIOL SCI,BUFFALO,NY 14260 NEW YORK STATE DEPT ENVIRONM CONSERVAT,ALBANY,NY 12233 STEWART KM SUNY,DEPT BIOL SCI,BUFFALO,NY 14260F?Times Cited: 3 English Article LR158 INT REV GESAMTEN HYDROBIOLISI:A1993LR158000020)Stewart, F.M. R.W. Furness L.R. Monteiro  1996Relationships Between Heavy Metal and Metallothionein Concentrations in Lesser Black-Backed Gulls, Larus fuscus and Cory's Shearwater, Calonectris diomedea& Arch. Environ. Contam. ToxicolM  30L299-305.0)Stewart, F.M. Monteiro, L.R Furness, R.W  1997piHeavy metal concentrations in Corys shearwater Calonectris diomedea fledglings from the Azores, Portugal$Bull. Environ. Contam. Toxicol58 115-122.4Stich,H-B Lampert,W 1981VOPredator evasion as an explanation of diurnal vertical migration by zooplankton  Nature 2932396-397l Sulak, K. Jc 1974f_Morphological and ecological observations on Atlantic ipnopid fishes of the genus Bathytyphlops Copeia 570-5734.SVETLOV, I. I. V. N. SHIBANOV V. V. KOLESNIKOV 1984The influence of oceanographic factors on the distribution and behaviour of roundnose grenadier on banks of the Mid-Atlantic RidgeF?Inter-university conference of young scientists and specialistst106-1070 in Russian 6527-6547D$://A1995QT22200002ed]Swift, E. Sullivan, J. M. Batchelder, H. P. Vankeuren, J. Vaillancourt, R. D. Bidigare, R. R.sBioluminescent Organisms and Bioluminescence Measurements in the North-Atlantic Ocean near Latitude 59.5-Degrees-N, Longitude 21-Degrees-W,&Journal of Geophysical Research-OceansVPcontinuous plankton records; sargasso sea; zooplankton; abundance; waters; fjordWe investigated mixed-layer bioluminescence from early April to late September (in April 1989, May 1991, July 1983 and 1990, August 1991, September 1988 and 1989) at stations near the Marine-Light - Mixed Layers (MLML) bio-optical moorings site. Volume-specific bioluminescence potential (BPOT, photons per unit volume) from epipelagic organisms was estimated directly with a pump-through bioluminescence photometer (BP) in 1983, 1988, and 1991. For all cruises, BPOT was also estimated by summing for a volume of seawater, the measurements of each species' total stimulable bioluminescence multiplied by each species'numerical abundance in the volume. The abundance data were taken from bottle casts, net tows, and BP effluent nets. After the onset of the spring bloom, from May through September, mixed layer BPOT was fairly constant, (similar to) 1-4 X 10(14) photons m(-3). On one early April cruise (1989) before the spring bloom, BPOT was two orders of magnitude lower. Heterotrophic dinoflagellates in the genus Protoperidinium generally produced most (90% or more) of the mixed Layer BPOT in the spring, summer, and fall. On one cruise in September (1988), the autotrophic dinoflagellate Ceratium fusus produced the bulk of the mixed layer BPOT (more than about 4 X 10(14) photons m(-3)). Other autotrophic dinoflagellates in the genus Gonyaulax and mesozooplankton produced a minor part of BPOT at most stations. The relative contribution of all autotrophic dinoflagellates to BPOT increased from a few percent during the May-June-July period to (similar to) 10% during the August-September period. In situ mechanically stimulable bioluminescence was reduced when underwater scalar irradiance (wavelengths 400-700 nm) was greater than 0.1 mu mol photons m(-2) s(-1).J. Geophys. Res.-Oceans 1995 Apr 15 100C4@9Times Cited: 8 English Article QT222 J GEOPHYS RES-OCEANSISI:A1995QT22200002 \ Lazzaro, X. Le Fevre, J. Le Grand, G. Le Traon, P.Y Leal, J. H. Leaper, L. Leaper, R. LEBEDEV, S.Lebedeva, L. P. LeGrand, G. Lenz, J.Lescrauwert, A. C. Levin, A.B. Levin, L. Levin, L. A. Levy, D. A. Lewis, S. A.Lilliendahl, K. Lima, S.LLISITSYN, A. P.LISOVSKY, S. F. LITVIN, V. M. Livi, S.Llewellyn, C. A. Lloris, D. Lochte, K. Lodha, VLOGVINENKO, B. M.Lohrenz, S. E. Lohrenz, S.ELOKTIONOV, Yu. A.LOKTIONOV., Yu. A.LOMAKIN, I. E.Longhurst, A.R. Lopes, H. D.Lopes, M. F. R.Lopukhin, A.S. Lorance, P. Lough, R.G Lovell, P.Lozier, M., S. Lozier, M.S LUKA, G. I.LUKASHEVICH, I. P.LUKASHINA., N. P.Lukashova, T. A. Lundgren, R. Ltken, Chr Lysy, A.Yu M, Nunes M.C, Silva Mackas, D. L. Mackas, L.D.Macquart-Molin, C.Macquart-Moulin, CMacquart-Moulin, C. Madge, L. S. Madge, L.S Madin, L.PMagalhes, M. J. MAKAROV, AMAKOVOZENKO, T. VMALAKHOV, V. A. Mall, U. MAMAEV, Yu. LMantoura, R. F. C.Mantoura, R.F.G. Markle Markle, D. FMarques, J. C.Marshall, N. B Martin, A. Martin, A. R Martin, A. R.Martins, A. F.Martins, A. F. M. -Ed. Martins, H. Martins, H. RMartins, H. R. Martins, H.R.Martins, J. A. Martins, RMASSALSKAYA, L. M. Matsui, TMatsumoto, G. I. MATUL, A. G Mauchline, J Mauchline, J. Maul, G. E Mayaud, N. Maycas, E. R. Maycas, E.R Mazaud, A.MAZHIRINA, G. PMcCartney, M. S. McKenzie, C McKenzie, E.McKenzie, J. F. Mead, G. WMedeiros, F. M. Medina, G Mees, J Meggers, H Meincke, J Meincke, J. Meir, E.Meise-Munns, C.J melle, W Melle, W.MELNIKOV, S. PMelo, A. M. A. Menard, F. Menard, H.W. Menezes, G.Menezes, G. M. Merrett, N. RMerrett, N. R. Michel, E.Middleton, D.A.J.Middleton, J. H.Mikkelsen, P. M. Miller, C. A. Mills, S. W.Moeller, R. E. MOISEEV, S. IMOISEEV, S. I. Moiseev, S.I. MOKANU, O. V.($Monaco, S. A. S. le Prince Albert deMonteiro, L. RMonteiro, L. R. Monteiro, L.RMonteiro, L.R.Monteiro, M. C. Monteiro, P. Monteiro_LR Monteiro_PR Moore, C. C. Moore, P. G. Morales, A.Morales, C. E.Morales, J. S. Morato, T Moreno, J. A Morin, C MOROVA, N. A.MOROZENKO, V. P. Morn, J. Morton, B.Moseley, H. N.Moskalenko, V.PMoskalev, L. I. Moss, D. L. Mourino, B.Mukhacheva, V. A. MUKHIN, S. G. Mukhin, S.G.Mullineaux, L.Mullineaux, L. S.MUROMTSEV, A. M Murray, J. Murray, John Murton, B. J.Musaeva, E. I. Musaeva, E.I Muscheler, R. Mnnich, MN, KHLIVNOY V.Nafpaktitis, B. GNAGURNY, A. P. Nakamura, INash, R. D. M.NAZAROV, I. V. NAZIMOV, V. VNAZIMOV, V. V.Nederbragt, A. J.NEFEDOV, G. N.Negre-Sadargues, G. Neill, W.ENeilson, D. J. Nelson, J. R. Nesis, K.N.Nespereira, J. L. Neto, A. I. Neumann, G. Neuville, H Neuville, H. Neves, V Neves_VCNevo, A. J. Del Newland, C. Nezlin, N. P. Niehoff, B Niehoff, B. Nielsen, J. Nielsen, J. GNielsen, J. G.Nierop, M. M. vanNigmatullin, Ch.MNigmatullin, Ch.M.Nikitina, I.V.Nikolsky, V.N. Ninni, E Nishikawa, Y. NITS, G. S.NIZOVTSEV, G. P Nobre, A. Noji, T.T. Norman, J. R. Norris, J.Novikova, N. S. Nunes, M Nunn, P. D Nybelin, O .X+nmlk S 267-289$://A1992HA43700004C,%Gloeckler, G. Geiss, J. Balsiger, H. Bedini, P. Cain, J. C. Fischer, J. Fisk, L. A. Galvin, A. B. Gliem, F. Hamilton, D. C. Hollweg, J. V. Ipavich, F. M. Joos, R. Livi, S. Lundgren, R. Mall, U. McKenzie, J. F. Ogilvie, K. W. Ottens, F. Rieck, W. Tums, E. O. Vonsteiger, R. Weiss, W. Wilken, B.2+The Solar-Wind Ion Composition Spectrometerd0*Astronomy & Astrophysics Supplement Seriesinterplanetary medium; jupiter; artificial satellites space probes; sun; solar wind earths bow shock; voyager-2; upstream; plasma; origin The Solar Wind Ion Composition Spectrometer (SWICS) on Ulysses is designed to determine uniquely the elemental and ionic- charge composition, and the temperatures and mean speeds of all major solar-wind ions, from H through Fe, at solar wind speeds ranging from 175 km/s (protons) to 1280 km/s (Fe8+). The instrument, which covers an energy per charge range from 0.16 to 59.6 keV/e in approximately 13 min, combines an electrostatic analyzer with post-acceleration, followed by a time-of-flight and energy measurement. The measurements made by SWICS will have an impact on many areas of solar and heliospheric physics, in particular providing essential and unique information on: (i) conditions and processes in the region of the corona where the solar wind is accelerated; (ii) the location of the source regions of the solar wind in the corona; (iii) coronal heating processes; (iv) the extent and causes of variations in the composition of the solar atmosphere; (v) plasma processes in the solar wind; (vi) the acceleration of energetic particles in the solar wind; (vii) the thermalization and acceleration of interstellar ions in the solar wind, and their composition; and (viii) the composition, charge states and behavior of the plasma in various regions of the Jovian magnetosphere.$Astron. Astrophys. Suppl. Ser. 1992 Jan922'UNIV MARYLAND,DEPT PHYS,COLLEGE PK,MD 20742 UNIV BERN,INST PHYS,CH-3000 BERN,SWITZERLAND UNIV MARYLAND,DEPT PHYS,COLLEGE PK,MD 20742 TECH UNIV BRAUNSCHWEIG,INST DATENVERARBEITENDE ANLAGEN,W-3300 BRAUNSCHWEIG,GERMANY UNIV NEW HAMPSHIRE,DEPT PHYS,DURHAM,NH 03824 NASA,GODDARD SPACE FLIGHT CTR,GREENBELT,MD 20771 NASA,OFF SPACE SCI & APPLICAT,WASHINGTON,DC 20546 MAX PLANCK INST AERON,W-3411 KATLENBURG DUHM,GERMANY GLOECKLER G UNIV MARYLAND,DEPT PHYS,COLLEGE PK,MD 20742JDTimes Cited: 104 English Article HA437 ASTRON ASTROPHYS SUPPL SERIESISI:A1992HA43700004$GLUKHOV, A. A. A. M. SENNIKOV. 1981Status and perspectives of studying and exploitation of biological resources in the open North Atlantic. Biological resources of deep and pelagic waters of open World Ocean Murmansk.k  3-4 in Russian$GLUKHOV, A. A. M. L. ZAFERMAN. 1982PIObservations of behaviour of Poliprion americanus (Schneider)(Serranidae)eVoprosy ikhtiologiii 22(2)2334-3363 in Russian0*GLUKHOV, A.A. A. I. PAVLOV V. N. SHIBANOV. 1983f_Investigations on the a ecology deep-water fishes from the Hatton Plateau and George Bligh Bank Annales Biol 37. in Russian&GLUKHOV, A. A. A. P. KUZMICHEV.s 1984New locations of Squalus laticaudus Smith et Radcliffe (Squalidae) and Neocyttus helgae Holt et Byrne (Zeidae) in the North-East AtlanticVoprosy ikhtiologii  24(4)669-671 in Russian82Godley, B.J Thompson, D.R Waldron, S Furness, R.W  1998TMThe trophic status of marine turtles as determined by stable isotope analysisMar. Ecol. Prog. Ser 166 277-284.Godman, F. du C. 1866 On the birds of the Azores Ibis 88-109 Gofas, S. 1990D=The littoral Rissoidae and Anabathridae of So Miguel, AzoresAAoreana Supl.a 97-134Gonalves, J. M.  1993JMOctopus vulgaris Cuvier, 1797 (polvo comum): sinopse da biologia e exploraooXRTese de Aptido Cientfica e Capacidade Pedaggica, Universidade dos Aores, Horta 470 ppGonalves, J. M. 1991ah82The Octopoda (Mollusca, Cephalopoda) of the Azores ArquiplagorLife and Earth Sciencest9S 75-91Gonalves, J. M. 1991bheBiology and exploitation of Octopus vulgaris Cuvier, 1791 (Mollusca, Cephalopoda) in the Azores. : ,, ICES CM 1991/K11 1-13F?Gonalves, J. M. Porteiro, F. M. Menezes, G. M. Fonseca, L. C. 1993Relatrio preliminar de execuo do projecto de investigao "Estudo pontual das condies fsico-qumicas e biolgicas, com especial incidncia na populao de amijoas (Ruditapes decussatus), na Lagoa de Sto. Cristoe"Relatrio Interno do DOP/UA 13 pp 263-272$://A1992JW40600006 Koppelmann, R. Weikert, H.NHFull-Depth Zooplankton Profiles over the Deep Bathyal of the Ne Atlantic$Marine Ecology-Progress SeriesVOsea-floor; rates; sedimentation; copepods; surface; fluxes; water; salps; zones,&Vertical profiles of zooplankton (size range less than 5 mm) were taken with a 1 m2 MOCNESS (333 mum mesh aperture) from the > 4000 m water column at 2 sites in the NE Atlantic. In the upper 1000 m, the profiles tended to exhibit high variability and were influenced by diurnal migrations, but below, the distributions were nearly similar. The standing crop in the upper 400 m was remarkably low, possibly due to a bloom of salps and their grazing pressure on the phytoplankton crop. The nonlinear decrease of the normalized zooplankton abundance and biomass below 1000 m in the area investigated could be approximated by a power function. The improved regression 'model' revealed no differences between the slopes when compared to biomass data from other marine locations given by various authors. This indicates that the processes of vertical material flux seem to be similar in many bathypelagic systems of the open sea. The y-intercepts, however, showed differences due to either a higher surface productivity in some ocean areas or differences in sampling methods and evaluation of the material. Possible causes which may have led to less of a decrease in zooplankton abundance at greater.depths (below 2500 m) such as food supply, resuspension, upward flux, faunal changes and trophic interactions are discussed.Mar. Ecol.-Prog. Ser. 1992 Sep863'INST HYDROBIOL & FISCHEREIWISSENSCH,ZEISEWEG 9,W-2000 HAMBURG 50,GERMANY KOPPELMANN R INST HYDROBIOL & FISCHEREIWISSENSCH,ZEISEWEG 9,W-2000 HAMBURG 50,GERMANY>8Times Cited: 14 English Article JW406 MAR ECOL-PROGR SERISI:A1992JW40600006 27-40$://000080261400003 Koppelmann, R. Weikert, H.|vTemporal changes of deep-sea mesozooplankton abundance in the temperate NE Atlantic and estimates of the carbon budget$Marine Ecology-Progress SeriesNE Atlantic; deep-sea zooplankton; temporal changes; carbon requirements biogenic particle fluxes; benthic boundary-layer; spatial variability; oxygen-consumption; north-atlantic; sediment trap; insitu rates; photographic evidence; calanus-finmarchicus; marine phytoplanktonFull-depth spring and summer vertical profiles of mesozooplankton numbers and biomass were obtained with a 1 m(2) multiple opening/closing net and environmental sensing system (MOCNESS) from the BIOTRANS (biological vertical transport and energetics in the benthic boundary layer of the deep sea) study area (47 degrees N, 20 degrees W) in the temperate NE Atlantic in 1992. Mesozooplankton abundance was high in spring and less in summer in the upper 750 m. Between 750 and 1050 m differences between these seasons could not be detected. In the upper bathypelagic zone, between 1050 and 2250 m, where abiotic fluctuations are minor, both mesozooplankton biomass and numbers were significantly higher in summer compared to spring. Samples from summer 1989 fitted this pattern. Calanoid copepods of the genus Metridia were the main contributors; most of the major zooplankton groups, though playing a subsidiary role, also showed a significant increase in summer in the upper bathypelagic zone. The increase probably was due to the large transient input of detrital material, which regularly occurred in the course of the phytoplankton spring bloom in the area investigated and may have stimulated the onset of reproduction in the bathypelagic zone. Temporal changes in mesozooplankton abundance could not be detected below 2250 m depth. Metabolic carbon requirements of mesozooplankton, calculated from ETS (electron transport system) data, increased in the bathypelagic zone (1000 to 4250 m) from 1.61 mg C m(-2) d(-1) in spring to 4.12 mg C m(-2) d(-1) in summer. The carbon respired by the bathypelagic micro- and mesozooplankton in summer, based on an assumed spring bloom area of 50 000 km(2), was 893 t C d(-1) as a minimum estimate, which was higher than in spring by a factor of 2.6.rMar. Ecol.-Prog. Ser.o 1999 179 >7Times Cited: 4 English Article 195PW MAR ECOL-PROGR SER9ISI:000080261400003a q0po  on 0)Morato, T Sola, E. Gros, M.P. Menezes, G. 2001Feeding habits of two congener species of seabreams, Pagellus bogaraveo and Pagellus acarne, off the Azores (Northeastern Atlantic) during spring of 1996 and 1997.5GL[ Bulletin of Marine Science693 1073-1087Moreno, J. A J. Morn  1992Comparative study of the Genus Isurus (Rafinesque, 1810) and description of a form (Marrajo Criollo) apparently endemic to the Azores<5Australian. Journal of Marine and Freshwater Research  43109-122rMorin, C 1992 Les Aores, cl de la biologie du germon en Atlantique Nord? Centenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L Hirondelle.  Aoreana (Suplemento 1992)155-192 Morton, B. 1995kThe biology and functional morphology of Trichomusculus semigranatus (Bivalvia: Mytiloidea) from the Azores)DAoreana Supl.279-295Moskalenko, V.PC 1981PJInformation about biology of arrow squid and prospects of its exploitation60Unpublished report, Murmansk, Sevrybpromrazvedka 16 p In Russian Moss, D. L. 1992JCA summary of the porifera collectec during "Expedition Azores 1989"a ArquiplagomLife and Earth Sciencesr10 45-53b167-185$://0001691945000062LFMourino, B. Fernandez, E. Serret, P. Harbour, D. Sinha, B. Pingree, R.|vVariability and seasonality of physical and biological fields at the Great Meteor Tablemount (subtropical NE Atlantic)Oceanologica Actaphysical variability; phytoplankton; primary production; seamount; subtropical Atlantic seamount-trapped waves; north-atlantic; tidal currents; cobb seamount; thermohaline structure; fieberling-seamount; sargasso sea; ocean; flow; circulationFive oceanographic surveys were conducted at the Great Meteor Tablemount (subtropical NE Atlantic; 30.0 degreesN, 28.5 degreesW) throughout the 1992-1999 period tc, investigate temporal variability in the relationship between the physical structure of the water column associated with the seamount and phytoplankton biomass and/or production rates. Local increases in chlorophyll a, enhanced carbon incorporation rates and changes in phytoplankton species composition were associated with the seamount. These effects were subjected to a large degree of temporal and spatial variability both at seasonal and shorter time scales. (C) 2001 Ifremer/CNRS/LRD/Editions scientifiques et medicales Elsevier SAS. Oceanol. Acta 2001Mar-Apr242'|uUniv Vigo, Dept Ecol & Biol Anim, Campus Lagoas Marcosende, Vigo 36200, Spain Univ Vigo, Dept Ecol & Biol Anim, Vigo 36200, Spain SAHFOS, Plymouth PL1 3BN, Devon, England Southampton Ocean Ctr, Southampton SO14 3ZH, Hants, England MBA Citadel Hill Lab, Plymouth PL1 2PB, Devon, England Mourino B Univ Vigo, Dept Ecol & Biol Anim, Campus Lagoas Marcosende, Vigo 36200, Spain81Times Cited: 0 English Article 440VD OCEANOL ACTAISI:000169194500006Mukhacheva, V. A.  1976ySystematics and distribution of Bonapartia Goode & Bean and Margrethia Jespersen et Tning (Gonostomatidae, Osteichthyes) >8Transactions of the P. P. Sirskov Institut of Oceanololy 1041 73-91 $(in Russian, English summary)Mukhacheva, V. A.  1981pjGeographical distribution and variability of Maurolicus muelleri (Gmelin) (Sternoptychidae, Osteichthyes).nhFishes of the Open Ocean. Academy of Sciences of the USSR, P. P. Shirshov Institut of Oceanology, Moscow 119p$(in Russian, English summary).raphique du Prince Albert de Monaco aux Aores bord de L Hirondelle.  Aoreana (Suplemento 1992)155-192 Morton, B. 1995kThe biology and functional morphology of Trichomusculus semigranatus (Bivalvia: Mytiloidea) from the Azores)DAoreana Supl.279-295Moskalenko, V.PC 1981PJInformation about biology of arrow squid and prospects of its exploitation60Unpublished report, Murmansk, Sevrybpromrazvedka 16 p In Russian Moss, D. L. 1992JCA summary of the porifera collectec during "Expedition Azores 1989"a ArquiplagomLife and Earth Sciencesr10 45-53b167-185$://0001691945000062LFMourino, B. Fernandez, E. Serret, P. Harbour, D. Sinha, B. Pingree, R.|vVariability and seasonality of physical and biological fields at the Great Meteor Tablemount (subtropical NE Atlantic)Oceanologica Actaphysical variability; phytoplankton; primary production; seamount; subtropical Atlantic seamount-trapped waves; north-atlantic; tidal currents; cobb seamount; thermohaline structure; fieberling-seamount; sargasso sea; ocean; flow; circulationFive oceanographic surveys were conducted at the Great Meteor Tablemount (subtropical NE Atlantic; 30.0 degreesN, 28.5 degreesW) throughout the 1992-1999 period tc, investigate temporal variability in the relationship between the physical structure of the water column associated with the seamount and phytoplankton biomass and/or production rates. Local increases in chlorophyll a, enhanced carbon incorporation rates and changes in phytoplankton species composition were associated with the seamount. These effects were subjected to a large degree of temporal and spatial variability both at seasonal and shorter time scales. (C) 2001 Ifremer/CNRS/LRD/Editions scientifiques et medicales Elsevier SAS. Oceanol. Acta 2001Mar-Apr242'|uUniv Vigo, Dept Ecol & Biol Anim, Campus Lagoas Marcosende, Vigo 36200, Spain Univ Vigo, Dept Ecol & Biol Anim, Vigo 36200, Spain SAHFOS, Plymouth PL1 3BN, Devon, England Southampton Ocean Ctr, Southampton SO14 3ZH, Hants, England MBA Citadel Hill Lab, Plymouth PL1 2PB, Devon, England Mourino B Univ Vigo, Dept Ecol & Biol Anim, Campus Lagoas Marcosende, Vigo 36200, Spain81Times Cited: 0 English Article 440VD OCEANOL ACTAISI:000169194500006Mukhacheva, V. A.  1976ySystematics and distribution of Bonapartia Goode & Bean and Margrethia Jespersen et Tning (Gonostomatidae, Osteichthyes) >8Transactions of the P. P. Sirskov Institut of Oceanololy 1041 73-91 $(in Russian, English summary)Mukhacheva, V. A.  1981pjGeographical distribution and variability of Maurolicus muelleri (Gmelin) (Sternoptychidae, Osteichthyes).nhFishes of the Open Ocean. Academy of Sciences of the USSR, P. P. Shirshov Institut of Oceanology, Moscow 119p$(in Russian, English summary).+ . PODRAZHANSKAYA, S. G 1969jdFeeding of roundnose grenadier in some areas of the North-West Atlantic and in the waters of Iceland.' Trudy molodykh uchenykh i specialistova 1 54-73  in RussianPODRAZHANSKAYA, S. G 1975Feeding of commercial species of Macruridae of the North Atlantic: roundnose grenadier (Macrurus rupestris) and roughhead grenadier (Macrurus berglax) Abstract of Doctor Thesis  30 in RussianB;POLETAEV, V. A. K. V. GORCHINSKY A. A. FILIN A. K. CHUMAKOVh 1991XQPreliminary results of studying of lanternfishes of the Atlantic and South Oceansu\VComplex fisheries investigations of PINRO on the North Basin: results and perspectives 118-129 in RussianPOLONSKY, A. S 1979>7Fish resources of the bathyal waters of the World OceanA.'Biological resources of the World Ocean 138-149 in Russian171-179$://000088100100016hhbPond, D. W. Gebruk, A. Southward, E. C. Southward, A. J. Fallick, A. E. Bell, M. V. Sargent, J. R.Unusual fatty acid composition of storage lipids in the bresilioid shrimp Rimicaris exoculata couples the photic zone with MAR hydrothermal vent sites$Marine Ecology-Progress Serieshydrothermal vent shrimp; nutrition; lipid metabolism; wax ester; PUFA mid-atlantic ridge; stable-carbon; isotope composition; decapoda; zooplankton; copepods; animals; ecologyLipid and stable carbon isotope analyses of Rimicaris exoculata, the dominant bresilioid shrimp found at the MAR (Mid-Atlantic Ridge) vent sites, have indicated that these animals possess a highly unusual storage lipid composition. The dominant neutral Lipid classes, triacylglycerols and wax esters, contained very high levels of polyunsaturated fatty acids (PUFA, up to 89% of neutral lipid fatty acids). Gas chromatography isotope ratio mass spectrometry (GC-IRMS) analysis of the PUFA from neutral lipid gave delta(13)C (v-PDB) values of -17.6 to -27.1 parts per thousand, which is within the range expected for a photosynthetic origin for these compounds. Fatty acid analyses of bacterial/detrital material collected from the vent sites contained only very low amounts of PUFA. It is clear from these findings that R. exoculata has evolved a highly specialized lipid metabolism which allows it to store substantial amounts of PUFA during its early planktotrophic life stages. These PUFA reserves will be subsequently mobilized to enable growth and maturation of the shrimp on return to a suitable vent site and are therefore an important factor allowing R. exoculata to inhabit deep sea vent ecosystems.Mar. Ecol.-Prog. Ser. 2000 198'Southampton Oceanog Ctr, Empress Dock, Southampton SO14 3ZH, Hants, England Southampton Oceanog Ctr, Southampton SO14 3ZH, Hants, England Marine Biol Assoc, Plymouth PL1 2PB, Devon, England Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117851, Russia Scottish Univ Res & Reactor Ctr, Glasgow G75 OQF, Lanark, Scotland Univ Stirling, Inst Aquaculture, Stirling FK9 4LA, Scotland Pond DW Southampton Oceanog Ctr, Empress Dock, Southampton SO14 3ZH, Hants, England>7Times Cited: 4 English Article 332XR MAR ECOL-PROGR SERISI:0000881001000169  V2+KUKUEV, E. I. E. I. KARASEVA V. N. FELDMAN.c 2000PIOn mezopelagic ichthyofauna of the boreal zone of the North-East AtlanticfVoprosy ikhtiologii0 40(3)2391-396A in RussianKUSMORSKAYA, A. P. 1960LEZooplankton of the frontal zone of the North Atlantic in spring, 1958 PJ Soviet fisheries investigations in the seas of the European North. Moscow 139-153 in RussianKUZNETSOV, A. P. 1985tnBottom fauna of the reef zone of the Reykjanes Ridge (distribution of quantity, trophic structure, communities Trudy IOAN 120 6-20 in Russian*#KUZNETSOVA, L. N. Yu. A. LOKTIONOV.n 1985Investigation of changeability of three-dimensional water circulation above peaks of the North-Atlantic Ridge with the use of diagnostic method of currents calculation.Complex fishery and oceanographic investigations in the Atlantic Ocean AtlantNIRO 11-18W in Russian177-190$://0001763411000144F?Laj, C. Kissel, C. Mazaud, A. Michel, E. Muscheler, R. Beer, J.aztGeomagnetic field intensity, North Atlantic Deep Water circulation and atmospheric Delta C-14 during the last 50 kyr*#Earth and Planetary Science Letterscmagnetic intensity; North Atlantic Deep Water; circulation; C- 14/C-12 earths magnetic-field; radiocarbon calibration; thermohaline circulation; glacial maximum; laschamp excursion; c-14 calibration; nordic seas; time-scale; cal bp; oceanWe present simulated records of past changes in the atmospheric Delta(14)C for the last 50 kyr due to changes in geomagnetic field intensity and in the strength of the North Atlantic Deep Water (NADW). A new geomagnetic record was used, largely based on the NAPIS-75 record [Laj et al., Phil. Trans. R. Soc. London A 358 (2000) 10091025] which has been extended for the 0-20 kyr interval using archeomagnetic and volcanic data. Past changes of the NADW were derived from a mineral magnetic study of the cores used in the construction of NAPIS-75. Two box models of different complexity (4 and 17 boxes) were used to simulate the carbon cycle. Calculated records of Delta(14)C are consistent with experimental determinations for the last 24 kyr. For older ages, the records calculated with variable oceanic circulation conditions reach values as high as 600% (with an average of 500%) between 20 and 40 kyr with maxima around 21, 30 and 38 kyr (GISP2 age model), while low values are observed prior to 42 kyr. Although large inconsistencies in experimental data preclude precise comparison, the average record simulated with the 17-box model is overall consistent with the Icelandic Sea record [Voelker et al., Radiocarbon 40 (1998) 517-534; 42 (2000) 437-452], except for the extremely high peak observed in this record at 40.5 kyr. On the other hand, the results recently reported from a stalagmite recovered from a submerged cave in the Bahamas [Beck et al., Science 292 (2001) 2453-2458] are inconsistent with all our model simulations. In the 20-45 kyr interval, the improved geomagnetic record combined with the new NADW profile allows us to give a modeled evaluation of the relative contribution of these factors to changes in atmospheric Delta(14)C. The average simulation provides a first order modeled correction for conventional radiocarbon ages older than 25 kyr for which no calibration curve is available as yet. (C) 2002 Elsevier Science B.V. All rights reserved.Earth Planet. Sci. Lett. 2002 Jun 20 200 1-2' CEA, CNRS, Lab Sci Climat Environm, F-91198 Gif Sur Yvette, France CEA, CNRS, Lab Sci Climat Environm, F-91198 Gif Sur Yvette, France EAWAG, Dept Surface Waters, CH-8600 Dubendorf, Switzerland Laj C CEA, CNRS, Lab Sci Climat Environm, F-91198 Gif Sur Yvette, France@:Times Cited: 0 English Article 564YL EARTH PLANET SCI LETTISI:000176341100014 Lampert, W 1989HBThe adaptive signifiance of diel vertical migration of zooplanktonFunctional Ecology3  21-27o689-702$://A1993LR57300017i>8Lampitt, R. S. Wishner, K. F. Turley, C. M. Angel, M. V.Marine Snow Studies in the Northeast Atlantic-Ocean - Distribution, Composition and Role as a Food Source for Migrating PlanktonMarine Biologyvertical nitrogen flux; diel migrant biota; deep-sea; chroococcoid cyanobacteria; coastal waters; potential role; sinking rates; fecal pellets; zooplankton; particles zDuring a 25 d Lagrangian study in May and June 1990 in the Northeast Atlantic Ocean, marine snow aggregates were collected using a novel water bottle, and the composition was determined microscopically. The aggregates contained a characteristic signature of a matrix of bacteria, cyanobacteria and autotrophic picoplankton with inter alia inclusions of the tintiniid Dictyocysta elegans and large pennate diatoms. The concentration of bacteria and cyanobacteria was much greater on the aggregates than when free-living by factors of 100 to 6000 and 3000 to 2500000, respectively, depending on depth. Various species of crustacean plankton and micronekton were collected, and the faecal pellets produced after capture were examined. These often contained the marine snow signature, indicating that these organisms had been consuming marine snow. In some cases, marine snow material appeared to dominate the diet. This implies a food-chain short cut whereby material, normally too small to be consumed by the mesozooplankton, and considered to constitute the diet of the microplankton can become part of the diet of organisms higher in the food-chain. The micronekton was dominated by the amphipod Themisto compressa, whose pellets also contained the marine snow signature. Shipboard incubation experiments with this species indicated that (1) it does consume marine snow, and (2) its gut-passage time is sufficiently long for material it has eaten in the upper water to be defecated at its day-time depth of several hundred meters. Plankton and micronekton were collected with nets to examine their vertical distribution and diel migration and to put into context the significance of the flux of material in the guts of migrants. ''Gut flux'' for the T compressa population was calculated to be up to 2% of the flux measured simultaneously by drifting sediment traps and < 5% when all migrants are considered. The in situ abundance and distribution of marine snow aggregates (> 0.6 mm) was examined photographically. A sharp concentration peak was usually encountered in the depth range 40 to 80 m which was not associated with peaks of in situ fluorescence or attenuation but was just below or at the base of the upper mixed layer. The feeding behaviour of zooplankton and nekton may influence these concentration gradients to a considerable extent, and hence affect the flux due to passive settling of marine snow aggregates. Mar. Biol. 1993 Aug 1164'INST OCEANOG SCI,DEACON LAB,GODALMING GU8 5UB,SURREY,ENGLAND UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882 PLYMOUTH MARINE LAB,PLYMOUTH PL1 2PB,DEVON,ENGLAND LAMPITT RS INST OCEANOG SCI,DEACON LAB,GODALMING GU8 5UB,SURREY,ENGLAND4.Times Cited: 63 English Article LR573 MAR BIOLISI:A1993LR57300017 &xih Menezes, G. M. 1991bpUmbraculum mediterraneum (Lamarck, 1819) (Mollusca, Opistobranchia, Umbraculomorpha), a new record for the littoral fauna of the Azores ArquiplagoLife and Earth Sciences9101-102Menezes, G. Silva, H. M. Krug, H. Balguerias, E. Delgado,J. Prez, J. G. Soldevilla, I. L. Nespereira, J. L. Carvalho, D. Morales, J. S. 1997piDesign optimization and implementation of demersal surveys in the Macaronesian archipelagos. FINAL REPORT.PICommission of the European Communities DG X1V/C/1 - Study contract 94/034&Arquivos do DOP. Sries Estudos 3/1998 162ppNGMenezes, G. Delgado, J. Krug, H. Pinho, M. R. Silva, H. M. Carvalho, D. 1998`ZDesign and implementation of demersal cruise surveys in the Macaronesian archipelagos - IIPICommission of the european Communities DG XIV/C/1 - Study contract 95/095 160pp Merrett, N. Re 1980Bathytyphlops sewelli (Pisces: Chlorophthamidae): a senior synonym of B. azorensis, from the eastern North Atlantic with notes on its biology.(Journal of the Linnean Society of London 68 (2) 99-109 Merrett, N. Rd 19860)Macrouridae of the eastern-north Atlantics0*Fiches dIdentification du Plancton (ICES) 173/174/17514Mikkelsen, P. M. 1995.(Cephalaspid opisthobranchs of the AzoresAoreana  Supl.193-215n MOISEEV, S. Ie 1986b\Underwater observations of squids of the North Atlantic from the underwater device Sever-2*#Underwater fisheries investigations in Russian Moiseev, S.I.i 1987\VUnderwater observations of North Atlantic squids from the manned submersible "Sever 2"(" Underwater Fishery Investigations&Collection of Scientific Papersc  71-78 Moiseev, S.I.S 1988Materials on the distribution and behavior of bathyal octopod Chunioteuthis sp. (Cephalopoda, Cirroteuthidae) in the area of the Mid-Atlantic Ridge, North Atlanticc Abstracts of Communications on III Scientific-Practical Conference of the Crimea "Young Scientists' and Specialists' Contribution to the Decision of the Modern Problems of Oceanology and Hydrobiology", Sevastopol  88-89 In Russian Moiseev, S.I.S 1989~xVertical distribution and behavior of the squid, Gonatus fabricii (Cephalopoda, Gonatidae), in the northeastern AtlanticLE Underwater Investigations for Bio-Oceanological and Fishery PurposesW vol? 53-60.&In Russian with English summary Moiseev, S.I.. 1989:3Vertical Distribution and Behavior of Oceanic Squidn"Sevastopol, "Hydronaut" Base vol?70 In RussianMOISEEV, S. I. 1989xqVertical distribution and behaviour of squid Gonatus fabricii (Cephalopoda, Gonatidae) in the North-East AtlanticlZS Underwater investigations from the bio-oceanological and fisheries points of view 53-60 in Russian Moiseev, S.I. 1992hbObservation of the vertical distribution and behavior of nektonic squids using manned submersibles Bulletin of Marine Science49(1-2)s446-456  In English Moiseev, S.I.r 2001voVertical Distribution and Behavior of Nektonic Squid Family Ommastrephidae and Some Other Groups of Cephalopods@:Unpublished Dissertation, Candidate of Biological Sciences Moiseev, S.I.p 2001voVertical Distribution and Behavior of Nektonic Squid Family Ommastrephidae and Some Other Groups of Cephalopods5TNAutoreferat of the Dissertation Candidate of Biological Sciences [cited above] 26 p.  In Russian*$Monaco, S. A. S. le Prince Albert de 1905.'Sur la campagne de la "Princesse-Alice"2+Bulletin du Muse Ocanographique de Monacot39 1-5&Monteiro, L. R. Furness, R. W.s (unpubl.)opSpeciation through temporal segregation of Madeiran storm petrel (Oceanodroma castro) populations in the Azores?BT(unpublished manuscript) Nesis1971 Nesis1973 Nesis1973 Nesis1975 Nesis1976 Nesis1979 Nesis1979 Nesis1982 Nesis1983 Nesis1983 Nesis1984 Nesis1984 Nesis1985 Nesis1985 Nesis1987 Nesis1991 Nesis1992 Nesis1993 Nesis1996 Nesis1998 Nesis1998 Nesis1998 Nesis2000 Nesis2001 Nesis2001 Nespereira1997 Neto 1990a0[ Neto19919] Neto19929 Neto19929 Neto1992 Neto19949 Neto19949 Neumann1968wNeuville1897xNeuville1900> Neves1998CNeves_VC19999l Nevo19969b Newland2000 Nezlin19951@ Nezlin1996? Nezlin19971= Nezlin19989 Nezlin19999> Nezlin199996 Niehoff2000 Niehoff2000y Nielsen1968 Nielsen1974z Nielsen1978{ Nielsen1980| Nielsen1985 Nielsen1989 Nielsen1989} Nielsen1990 Nierop1984  Nigmatullin1975  Nigmatullin1975  Nigmatullin1975 Nigmatullin1976 Nigmatullin1976 Nigmatullin1976  Nigmatullin1976 Nigmatullin1977 Nigmatullin1977  Nigmatullin1977 Nigmatullin1979 Nigmatullin1979 Nigmatullin1987 Nigmatullin1989 Nigmatullin1991 Nigmatullin1994 Nigmatullin1997 Nigmatullin1999Nikitina20011Nikitina20011Nikolsky19911~ Ninni1933 Nishikawa1970 NITS1974 NIZOVTSEV1989 Nobre1924 Nobre1930 Noji1991 Norman1930 Norris19929Novikova19761, Nunes1998 Nunn1994 Nybelin1951 Nybelin1957w OGANESYAN.1988x OGANESYAN.1989 OGANIN19888 OGANIN19919S Ogilvie1992 Ohman1991 Ohman1998@Oliveira19999u Olsen19766 Olsen2000 Olsen2000h OMELCHUK.1986 Onbe19922Oschlies1999Oschlies2000Oschlies2002 Osgood19933 Osgood1994 Ostapenko1979R Ottens1992S Ottens19922[ Ottens1992 Ottens1992T Owens1995~ Ozouf-Costaz1989u stvedt1976  Paffenhofer1993Pafort- van Iersel1981 Parfenyuk1991 Parin1970v Parin1993 Parin1996 Parin1999 Parr1960 Pascoe199331 Passelaigue1999 Passelaigue1999 Passelaigue1999Patching19899Patching199491 Patriti1999 Patriti1999 Patriti1999 Patzner1990 Patzner1990 Patzner1992 Patzner1993 Paula1992 PAVLOV1980m PAVLOV19833 PAVLOV1988 PAVLOV19888 PAVLOV1991 PAVLOV1991 PAVLOV1991j PAVLOV.1990 Pearre19877 Pereira1977Z Pereira1982 Pereira1983 Pereira1994> Pereira1998C Pereira_JRC19995 PEROVA.1979Pershing2000 Pettersson1957  Petursdottir2000 Petursdottir2000 Prez1997 Prs1992 Pfannkuche1989H Philbin1979HPhillips19999 Pierce1994 Pierrot-Bults1975) Pierrot-Bults1979 Pietsch1972 Pietsch1972 Pietsch1975 Pietsch1979 Pietsch1986 Pietsch1987 Pinchukov1975 Pinchukov1976 Pinchukov1977 Pinchukov1979 Pingree1997 Pingree1997o Pingree2001 Pinho1994 Pinho1998 Piontkovski1997 Planque1997 Planque1997 Planque2000PODRAZHANSKAYA1969PODRAZHANSKAYA1975PODRAZHANSKAYA.1984POLETAEV1991Pollehne2002POLONSKY1979 POLOSIN1974 POLYANSKAYA.1983 Pomroy19977 Pomroy19977+ Pond2000 POPOVA1975 POPOVA19777 POPOVA1977 POPOVA1978 POPOVA19799 POPOVA1979 POPOVA1981Porteiro1992Porteiro1992Porteiro19933Porteiro1994-Porteiroin press Post1982 Post1985 Post1991 Poulet19929,Poulicek1999 PRISTAVAKINA1982 Proctor1994 Proctor1995Prud'homme van Reine1988 PSHENICHNY1986O PSHENICHNY.1979Queiroga19922 Quro1980ga19922 Quro198022 Quro1980 Quro1980 Quro1980 Quro198022 Quro19808022 Quro19809922 Quro1980 Quro198022 Quro198022 Quro198022 Quro1980 Quro1980 Quro198022 Quro1980 Quro1980 Quro19809922 Quro198019922 Quro1980 Quro1980 Quro198022 Quro19809922 Quro1980 Quro198022 Quro19809922 Quro198022 Quro1980 Quro1980$*0*Shimko, B.P. Korytov, V.G. Daulmetov, A.A. 1989RKSome patterns of long-term variations in abundance of nerito-oceanic squidsn{ Abstracts of Communications of 4th All-USSR Scientific Conference on Problems of Fisheries Forecasting (Long-Term Aspects)s 1939 In Russian Shimko, B.P. 1990~Mechanisms of the effect of space-geophysical factors on long-term fluctuations of abundance of some common cephalopod species.'Modern Problems of Fisheries Oceanologyf192-193  In Russian Shimko, B.P. 1990NGPeriodicity of growth rings deposition on the statoliths of Cephalopoda F@ Abstracts of Scientific Papers of ICES 1990 Shellfish Symposium  814 In English@:Shimko, B.P. Kolmakov, Yu.A. Korytov, V.G. Daulmetov, A.A. 1990hbThe effect of cosmic and geophysic forces on long-term variations in abundance of some cephalopodsF@ Abstracts of Scientific Papers of ICES 1990 Shellfish Symposium80 In English4881-887$://A1992JY35000012g("Shushkina, E. A. Vinogradov, M. E.TNVertical-Distribution of Zooplankton in the Guaymas Basin (Gulf of California) Okeanologiya sea; oceanVertical distribution of various taxonomic groups and different size fractions of meso- and macroplankton was studied in the water column in the vicinity of the Guyamas Basin hydrothermal fields. Plankton numbers were estimated with the aid of 150 l water bottles (lowerd to 750 m), BP 113/140 plankton nets (up to 1800 m) and by direct counting in a registration cube of the <> deep manned submersible (to the bottom - 2053 m). The plankton distribution is essentially influenced by oxygen minimum (less than 0.1 ml/l) in the intermediate layers. However the depletion of zooplankton biomass in the oxygen minimum layer is much less pronounced than other areas with such a minimum. The reasons for this phenomenon are not clear. In the near-bottom layer there is a slight increase of biomass due to Ctenophora, large copepods and to a lesser extent, decapods and amphipods. This enrichment does not seem to be related to the effects of hydrothermal fields. Okeanologiya 1992Sep-Oct325'\VPP SHIRSHOV OCEANOL INST,MOSCOW,USSR SHUSHKINA EA PP SHIRSHOV OCEANOL INST,MOSCOW,USSR81Times Cited: 3 Russian Article JY350 OKEANOLOGIYAISI:A1992JY35000012705-712$://A1995TF08200009XQShushkina, E. A. Vinogradov, M. E. Sheberstov, S. V. Nezlin, N. P. Gagarin, V. I.hThe Characteristics of Epipelagic Ecosystems of the Pacific- Ocean on the Base of Both Satellite and Field Observations - the Stock of Plankton in the Epipelagial OkeanologiyaTMquantitative characteristics; southern-ocean; phytoplankton; community; spaceThe area of the Pacific Ocean was divided into regions according to the surface chlorophyll concentration determined by the satellite Nimbus-7. The areas occupied by the waters of 7 distinguished chlorophyll concentration levels were calculated. The information obtained on about 300 ecosystemic stations of IO RAS ships i upper 200-m layer was taken into account. Both geometric mean biomasses and stock values of phytoplankton, bacteria, protozoa and mesoplankton for every climatologic season and average for year were calculated for every chlorophyll concentration level. The year average stock values for all Pacific were the following: phytoplankton - 134 x 10(6), bacteria - 86 x 10(6), protozoa - 26 x 10(6), mesoplankton - 185 x 10(6) t C. The seasonal stack variations of all the listed groups were shown to be insignificant. The reason is that in winter the stocks in the temperate regions decrease but the areas occupied by oligotrophic waters reduce, the opposite pattern taking place in spring and summer. The seasonal stability of the plankton stocks and, consequently, the metabolic process influence by far the peculiarities of the carbon cycle it the ocean.o Okeanologiya 1995Sep-Oct2355e'`ZPP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA SHUSHKINA EA PP SHIRSHOV OCEANOL INST,MOSCOW,RUSSIA81Times Cited: 7 Russian Article TF082 OKEANOLOGIYAISI:A1995TF08200009&F((4$$SHATOBA, O. E. Yu. V. SHISHLOe 1984pjHydroacoustic search for fish at large depths (manual for navigators working in the open part of Atlantic)72 in Russian("Shcherbachev, Y. N. N. S. Novikova 1976vpMaterials on the distribution and systematics of the mesopelagic fishes of the family Stomiatidae (Osteichthyes)>8Transactions of the P. P. Sirskov Institut of Oceanololy  10492-112.2$(in Russian, English summary)6/Shcherbachev, Y. N. E.I. Kukuev V.I. Shlibanov  1985Composition of the benthic and demersal ichthyocenoses of the submarine mountains in the southern part of the North Atlantic RangeJournal of Ichthyology 25 (1)110-1252Shelbourne,J.E 1962PIA predator-prey size relationship for plaice larvae feeding on OIKOPLEURAyJournal marine biology42243-252\$SHESTOPAL, I. P S. F. LISOVSKY 1993ZTOn perspectives of fishery for sharks on the underwater mounts of the North Atlantic 63-646 in RussianSHIBANOV, V. N 1985PJPeculiarities of reproduction of roundnose grenadier of the North Atlantic Studying and rational exploitation of biological resources of north seas and North Atlantic. Theses of papers of the conference of young scientists and specialists  71 in Russian& SHIBANOV, V. N P. I. SAVVATIMSKY 1987Method of conversion of Roundnose Grenadier (Coryphaenoides rupestris Gunnerus, Macrouridae) Ante-Anal Distance into Zoological Length*$NAFO SCR Doc 87/91 Serial No. 1395. in RussianSHIBANOV, V. N 1988tmSome peculiarities of seasonal and daily dynamics of feeding of roundnose grenadier of the Mid-Atlantic Ridge6^W Feeding of marine fishes and exploitation of food base as elements of fishery forecast112-113  in Russian"SHIBANOV, V. N A. S. YAROVOY 1988}Measurement of reflection ability of roundnose grenadier and microplankton with the use of the underwater apparatus Sever-2Rybnoe khozyaistvo 3 74-76t in Russian2+SHIBANOV, V. N A. N. KALUGIN V. V. BONDAREVo 1988Assessment of biomass of the bottom ichthyocenosis on the underwater mounts of the Azores area with the use of underwater apparatus Sever-2:4Instrumental methods of commercial stocks assessment  65-74 in Russian0)SHIBANOV, V. N. A. I. PAVLOV I. A. OGANINg 1988TMPerspectives of national fisheries in thalassic bathyal of the North Atlantic1 The meeting of specialists of the union associations of the USSR Ministry for Fisheries, fish searching fleets and basins institutes on the problem of widening of fisheries for valuable fish species and sea products  87-89 in Russian"SHIBANOV, V. N A. N. KALUGIN 1989Results of fish assessment done with the use of the underwater apparatus Sever-2 on the underwater mounts of the Mid-Atlantic Ridge6PI Bioresources of mezo- and bathypelagic waters of the open North Atalntici199-2152 in Russian2+SHIBANOV, V. N. A. N. KALUGIN A. S. YAROVOYn 1989rkOn the method of stock assessment of roundnose grenadier on the underwater mounts of the Mid-Atlantic Ridge2156-1655 in Russian2+SHIBANOV, V. N. I. E. LOMAKIN A. N. KALUGINe 1989rlResults of investigations of thalassic bathyal of the North Atlantic in the 12th cruise of RPS IchthyandrtnAdvanced industrial experience and scientific and technical achievements recommended for introduction. Moscow 5 1-11 in Russian"SHIBANOV, V. N A. N. KALUGIN 1990d^Vertical distribution of demersal fishes on the underwater mountains of the Mid-Atlantic RidgejcThe union conference Reserve food and biological resources of the open ocean and seas of the USSRR176-1777 in RussianSHIBANOV, V. N 1992^WSeasonal and daily dynamics of feeding of roundnose grenadier of the Mid-Atlantic Ridgeo:4 Investigation of bioresources of the North Atlantic  31-44 in RussianSHIBANOV, V. N 1998zsBiological basis of fishery for roundnose grenadier (Coryphaenoides rupestris Gubberus, 1765) in the North Atlanticp Abstract of Doctor Thesist  244 in RussianSHIBANOV, V. N 1999d^Populational structure of roundnose grenadier (Coryphaenoides rupestris) of the North Atlantic>7The IXth union conference on the fisheries oceanography2  102 in Russian Shimko, B.P. 1984\VMethodological Recommendations for Age Determination of Northeast Atlantic Cephalopods  24 p. In Russian Shimko, B.P. 1984LEAgeing and biological peculiarities of Todarodes sagittatus (Lamarck) 12 p.  In Englishl Shimko, B.P. 1987xqOceanological prerequisites of forming up of the macroscale groupings of cephalopods in the northeastern Atlanticnrk Abstracts of Communications of 7th All-USSR Conference on Fisheries Oceanology, Astrakhan, 19-21 May, 1987S142-143  In Russian @ IZJKYW !"#$%&'()*+,-./0123L:DA<\^`_][baM45689:7;<cd=>?e!gf5N,@ABChOijklmn&Do(-EFpqrscG"$GHxtywvuIJKzygLMN{|}O~PQRSTVWUZ\][XY^_`a&QP'Q(*)bcdzefjhgiCB?=>: Snmkl+opqr0-/.,astuwxvy{|}~znb ;69612p0)XS9%4TTUVqYWXZ[\]`_a3;bcdef13ghim9>467;<=AB5?@kj:8lCno  opqfrstuv   wxy}|{z~[R+U !wu_ WX   "#$de(*&%'+),- .2/012345Y3Y76DE ZGFH89 [:8!;"#$%&2'()*+<r,-./7023#   46789:;<=>?@5 C  EFG=>?@HIAKL}|PQR B!"# $%     ܿ1vy@Qma0/.-,82Granadeiro, J.P Nunes, M Silva, M.C. Furness, R.W  1998lfFlexible foraging strategy of Cory's shearwater, Calonectris diomedea, during the chick-rearing period Animal Behaviour56 1169-1176..(Granadeiro, J.P Burns, M.D Furness, R.W  1998}Patterns of activity and burrow attendance in Cory's Shearwater Calonectris diomedea as revealed by a novel logging techniqueh Ibis 1405458-466.2,Granadeiro, J.P Monteiro, L.R. Furness, R.W  1998leDiet and feeding ecology of Corys shearwater Calonectris diomedea in the Azores, north-east AtlanticMar. Ecol. Prog. Ser. 166 267-276..'Granadeiro, J.P Burns, M.D Furness, R.Ws 1999\UFood provisioning to nestling shearwaters: why parental behaviour should be monitoreds Anim. Behav  57663-671.@9Granadeiro, J.P. Bolton, M Silva M.C Nunes M Furness, R.W 2000rlResponses of breeding Cory's shearwater Calonectris diomedea to experimental manipulation of chick conditionBehavioral Ecology  111274-281. 33-40$://A1991FE84000004 Grant, G. C.Chaetognatha from the Central and Southern Middle Atlantic Bight - Species Composition, Temperature-Salinity Relationships, and Interspecific AssociationsFishery BulletinTNtemporal abundance patterns; western north-atlantic; oceanic chaetognaths; bay&Eighteen species of chaetognaths were identified from shelf waters in the Middle Atlantic Bight. Species composition in the water column and the hyponeuston was nearly identical, but the percent frequencies of the more common cold-temperate species were generally lower in surface collections. Mean surface salinity, weighted for abundance of individual chaetognath species in the hyponeuston collections, varied from 32.6 and 32.8 parts per thousand for the coastal- and estuarine-inhabiting Sagitta tenuis and Parasagitta elegans, to 34.8 and 34.9 for the offshore Pterosagitta draco and Krohnitta pacifica. Weighted mean temperatures ranged from below 14- degrees-C for Mesosagitta minima, P. elegans, and Serratosagitta tasmanica to over 24-degrees-C for K. pacifica. Overall association among Middle Atlantic Bight chaetognaths, measured for the 15 most frequent species in 716 collections by variance ratio, was significantly positive. Association between pairs of species was therefore also largely positive, with the important exception of Parasagitta elegans. This species, with a unique regional niche in low salinities and temperatures, was negatively associated (p < 0.01) with five warm-water species (Krohnitta pacifica, Ferosagitta hispida, Sagitta tenuis, Sagitta helenae, and Flaccisagitta enflata). Most species reached maximum abundance at the surface near midnight. Exceptions included Sagitta helenae, with daylight maxima, and Krohnitta pacifica, Ferosagitta hispida and Serratosagitta serratodentata, showing crepuscular increases in abundance. Fish. Bull. 1991 Jan891'VIRGINIA INST MARINE SCI,GLOUCESTER POINT,VA 23062 COLL WILLIAM & MARY,SCH MARINE SCI,GLOUCESTER POINT,VA 23062 GRANT GC VIRGINIA INST MARINE SCI,GLOUCESTER POINT,VA 230624.Times Cited: 4 English Article FE840 FISH BULLISI:A1991FE84000004 1536-1544d$://000167224000003r$Greene, C. H. Pershing, A. J.The response of Calanus finmarchicus populations to climate variability in the Northwest Atlantic: basin-scale forcing associated with the North Atlantic Oscillationi$Ices Journal of Marine ScienceCalanus finmarchicus; climate variability; North Atlantic Oscillation; shelf ecosystems nova-scotia shelf; c-helgolandicus; el-nino; zooplankton; sea; ocean; gulf; environment; temperature; atmosphere The North Atlantic Oscillation (NAO) is associated with decadal-scale forcing of climate and physical oceanography throughout the North Atlantic. Oceanographers have recently established correlations between the NAG and various processes at work in the shelf ecosystems of the NE Atlantic, correlations that have led them to suggest several hypotheses explaining the mechanistic basis of ecosystem and population responses to the NAG. Here, we incorporate these ideas into a new. conceptual framework for interpreting the responses of shelf ecosystems to climate variability on both sides of the North Atlantic. This conceptual framework, contrasting the relative importance of internal ecological dynamics versus advective exchange processes, is used to examine the trans- Atlantic responses of Calanus finmarchicus populations to the NAG. We conclude by proposing an NAG-based explanation for the trends in C. finmarchicus abundance observed from 1961 to 1989 on the NW Atlantic Shelf. (C) 2000 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 2000 Dec576:3Times Cited: 0 English Article 406PH ICES J MAR SCIISI:000167224000003ntly established correlations between the NAG and various processes at work in the shelf ecosystems of the NE Atlantic, correlations that have led them to suggest several hypotheses explaining the mechanistic basis of ecosystem and population responses to the NAG. Here, we incorporate these ideas into a new. conceptual framework for interpreting the responses of shelf ecosystems to climate variability on both sides of the North Atlantic. This conceptual framework, contrasting the relative importance of internal ecological dynamics versus advective exchange processes, is used to examine the trans- Atlantic responses of Calanus finmarchicus populations to the NAG. We conclude by proposing an NAG-based explanation for the trends in C. finmarchicus abundance observed from 1961 to 1989 on the NW Atlantic Shelf. (C) 2000 International Council for the Exploration of the Sea.ICES J. Mar. Sci. 2000 Dec576:3Times Cited: 0 English Article 406PH ICES J MAR SCIISI:000167224000003 dcb*)(Q'PQD 1975-1991t$://000071634800010G Frank, T. M. Widder, E. A.The correlation of downwelling irradiance and staggered vertical migration patterns of zooplankton in Wilkinson Basin, Gulf of Maine"Journal of Plankton Researchchaoborus-punctipennis larvae; deep-sea crustaceans; diel migrations; mesopelagic community; northeast atlantic; light- intensity; behavioral sensitivity; uv-light; near-uv; distributionsn"Field studies on the characteristics of light that influence vertical migrations in the mesopelagic realm are sparse, due to the difficulty in simultaneously monitoring changes in species distributions with changes in downwelling irradiance. Using the Johnson-Sea-Link submersible as a platform, in situ measurements of the changes in downwelling irradiance at sunset were made simultaneously with observations on changes in animal distribution patterns in Wilkinson Basin, Gulf of Maine. The results indicate that the vertical migrations for several species of large zooplankton are staggered, with euphausiids (Meganyctiphanes norvegica) migrating first, cydippid ctenophores (Euplokamus) migrating next, and two species of caridean shrimp (Dichelopandalus leptocerus and Pasiphaea multidentata) migrating last. Data collected on daytime dives indicate that the daytime depth distribution is not solely responsible for the migration order, and that different species may be responding to different cues, or have different thresholds for the same cue.J. Plankton Res. 1997 Dec,1912'Harbor Branch Oceanog Inst Inc, 5600 US 1 N, Ft Pierce, FL 34946 USA Harbor Branch Oceanog Inst Inc, Ft Pierce, FL 34946 USA Frank TM Harbor Branch Oceanog Inst Inc, 5600 US 1 N, Ft Pierce, FL 34946 USA:3Times Cited: 4 English Article YT705 J PLANKTON RES7ISI:000071634800010oFrank, T.M Widder, E.A 1997The correlation of downelling irradiance and staggered vertical migration patterns of zooplankton in Wilkinson basin, Gulf of Mainei"Journal of Plankton Research 19(12) 1975-1991Frank,T.M Widder,E.A 2002{Effects of a decrease in downelling irradiance on the daytime vertical distribution patterns of zooplankton and micronektonlMarine Biology22Fransen, C. H. J. M. 1991rkLysmata olavoi, a new shrimp of the family Hippolytidae (Decapoda, Caridae) from the eastern Atlantic Ocean ArquiplagoLife and Earth Sciences9 63-73Fratantoni, D. M.i 2001d]North Atlantic surface circulation during the 1990s observed with satellite-tracked drifters.&Journal of Geophysical Research 106 C10- 22067-220943*$Fredericq, S. Serro, E. Norris, J. 19926/New records of marine red algae from the Azores} ArquiplagozLife and Earth Sciencess10 1-4r:3Friesen, V.L. Lodha, V Monteiro, L.R. Furness, R.W  1998ZTEvidence for sympatric speciation in the band-rumped storm-petrel Oceanodroma castroOstrich69400-401.Fuglister, F. C. 1960|vAtlantic Ocean Atlas, temperature and salinity profiles and data from the international Geophysical Year of 1957-1958.81Woods Hole Oceanographic Institution contribution 1108 Furness, R.Ws 1994voAn estimate of the quantity of squid consumed by seabirds in the eastern North Atlantic and adjoining seas\ Fisheries Res  21165-177. Furness, R.W Monteiro, L.R 1995^XRed-billed tropicbird Phaethon aethereus in the Azores: first breeding record for Europe Bull. Brit. Orn. Cl 1151 6-8.,&Furness, R.W G.M. Hilton L.R. Monteiro 2000Influences of coastal habitat characteristics on the distribution of Corys Shearwater Calonectris diomedea in the Azores archipelago Bird StudyV47257-265.(!Gaevskaya, A.V. Nigmatullin, Ch.Ma 1976Biotic connections of Ommastrephes bartrami (Cephalopoda, Ommastrephidae) in the northern and southern parts of the Atlantic Ocean$Zoologichesky Zhurnal, 55(12)i 1800-1810&In Russian with English summaryGALAKTIONOV, G. Z. 1984~xPeculiarities of behaviour of Alfonsino Beryx splendens Lowe (Berycidae) schools in the Atlantic Ocean thalassic bathyal Vopr. Ikhtiola 24 (5)863-865  in RussianGALAKTIONOVA, A. I.o 1978zIntraspecies structure of roundnose grenadier (Coryphaenoides rupestris G.) in the northern part of the Mid-Atlantic Ridge Abstract of Doctor Thesis  24  in Russian,&GALAKTIONOVA, A. I. G. Z. GALAKTIONOV. 1990Structure of encephalon and peculiarities of behaviour of roundnose grenadier Coryphaenoides rupestris of the Mid-Atlantic RidgeVoprosy ikhtiologiii 30(2)2342-3474 in RussianGalhardo, M. L. 1990yCetceos que ocorrem nos Aores (Biologia, Ecologia e Taxonomia) e estudos sobre a histria da baleao nos Aores. , , ,4*$Relatrio de Estgio de Licenciatura  Ponta Delgada Universidade dos Aores 330 pp842-847$://A1990EH36700022$Galkin, S. V. Moskalev, L. I.2,Fauna of the Mid-Atlantic Ridge Hydrothermal Okeanologiya Okeanologiya 1990Sep-Oct305'ZSPP SHIRSHOV OCEANOL INST,MOSCOW,USSR GALKIN SV PP SHIRSHOV OCEANOL INST,MOSCOW,USSR81Times Cited: 8 Russian Article EH367 OKEANOLOGIYAISI:A1990EH36700022CZBA@ ?>=<;:98ml>8Monteiro, L. R. J. A. Ramos R. W. Furness A. J. Del Nevo 1996RLMovements, morphology, breeding, molt, and feeding of seabirds in the AzoresColonial Waterbirds- 19 (1) 82-97S:3Monteiro, L. R. V. Costa R. W. Furness R. S. Santos. 1996haMercury concentrations in prey fish indicate enhanced bioaccumulation in mesopelagic environmentss.(Marine Ecology Progress Series, in press<5Monteiro, L.R. Ramos, J.A Furness, R.W. del Nevo, A.J 1996XQMovements, Morphology, Breeding, Molt, Diet and Feeding of Seabirds in the AzoreszColonial Waterbirdst19 82-97.6/Monteiro, L.R Costa, V Furness, R.W Santos, R.Sa 1996haMercury concentrations in prey fish indicate enhanced bioaccumulation in mesopelagic environmentsn$Marine Ecology Progress Series 141 21-25.W,%Monteiro, L.R Ramos, J.A Furness, R.W 1996b[Past and present status and conservation of the seabirds breeding in the Azores archipelagoh Biological Conservation  78V319-328. Monteiro, L.R Furness, R.W 1996ZSMoult of Cory's Shearwater Calonectris diomedea borealis during the breeding seasont Condor  981 216-221.1 Monteiro, L.R Furness, R.W 1997Accelerated increase in mercury contamination in North Atlantic mesopelagic food chains as indicated by time series of seabird feathers.Environ. Toxicol. Chem16 2489-2493."Monteiro, L.R Furness, R.W n 1998voSpeciation through temporal segregation of Madeiran Storm Petrel (Oceanodroma castro) populations in the AzoresB& Phil. Trans. Roy. Soc. Lond. Bi 353n945-953.|Monteiro, L.R. Feio, R Wilson, L Hewitson, L. Pereira, J Ramos, J.A. Sola, E. Monteiro, P. Furness, R.W Tavares, A Neves, V  1998HBUsing raft counts to census Corys shearwater Calonectris diomedeaOstrich  69 347.2+Monteiro, L.R. Granadeiro, J.P Furness, R.Wr 1998JDThe relationship between mercury burdens and diet in Azores seabirdsMar Ecol Prog Sern  166 259-265.6>8Monteiro, L.R. Granadeiro, J.P Furness, R.W. Oliveira, P 1999Contemporary patterns of mercury contamination in the Portuguese Atlantic inferred from mercury concentrations in seabird tissuesV$Marine Environmental ResearchW47137-156."Monteiro, L.R Furness, R.W  2001piKinetics, dose-response, excretion, and toxicity of methylmercury in free-living Corys shearwater chicksEnviron. Toxicol. Chem20 1816-1823. Monteiro, L.R Furness, R.W 2001f_Kinetics, dose-response, and excretion of methylmercury in free-living adult Corys shearwatersp Environ. Sci. Technol  355739-746.4.Monteiro, L. R. Furness, R. W. del Nevo, A .J.in pressJDMercury levels in seabirds from the Azores, north-mid Atlantic Ocean:4Archives of Environment, Contaminants and Toxicology0*Monteiro, L.R. Ramos, J. A. Furness, R. W.in pressb[Past and present status and conservation of the seabirds breeding in the Azores ArchipelagoeBiological Conservation in pressMonteiro_LR Ramos_JA Pereira_JRC Monteiro_PR Feio_RS Thompson_DR Bearhop_S Furness_RW Laranjo_M Hilton_G Neves_VC Groz_MP Thompson_KRi 1999Status and distribution of Fea's petrel, Bulwer's petrel, Manx shearwater, little shearwater and band-rumped storm-petrel in the Azores archipelagoT Waterbirds  22358-366. Moore, C. C. 1994HBPelagic seabird transects through Azorean waters, autumn 1990-1992 ArquiplagohLife and Marine Sciences 12A111-116 Moore, P. G. 1995XQFaunistic notes on a small collection of marine amphipods from So Miguel, AzoresAoreana Supl.o313-316E Moore, P. G. Weeks, J. M. 1995rlObservations on the natural history of some supralittoral and terrestrial talitrid amphipods from the AzoresAoreana Supl. 79-91. C. 1994HBPelagic seabird transects through Azorean waters, autumn 1990-1992 ArquiplagohLife and Marine Sciences 12A111-116 Moore, P. G. 1995XQFaunistic notes on a small collection of marine amphipods from So Miguel, AzoresAoreana Supl.o313-316E Moore, P. G. Weeks, J. M. 1995rlObservations on the natural history of some supralittoral and terrestrial talitrid amphipods from the AzoresAoreana Supl. 79-91rq>po>N$Gonalves, J.M. Pinho, M. R.  1994Relatrio de Campanha N 17/94 do N/I "Arquiplago" (Ensaio de pesca de crustceos de profundidade com covos, manuteno do DCP da Graciosa e arrsatos com Bongo'2& Arquivos do DOP, Srie Cruzeiros 2/94 8 pp$Gonalves, J.M. Santos, R. S.  1994Relatrio de Campanha N 14/94 do N/I "Arquiplago" (Ensaio preliminar de pesca de profundidade com armadilhas dirigidas a crustceos e peixes)d'2& Arquivos do DOP, Srie Cruzeiros 1/94 7 pp Goode, G. B. Bean, T. H. 1895Oceanic Ichthyology - A treatise on the deep-sea and pelagic fishes of the World, based chiefly upon the collections made by the steamers Blake, Albatross, and Fish hawk in the northwestern AtlanticNHSmithsonian Institution, United States National Museum, Special BulletinVol. I, Vol. II<6Vol. I, xxxv + 553 pp. Vol. II, xxiii + cxxiii platesGoodman, F. du C.A 187060Natural history of the Azores or western islands London & John Van Voorst, Paternoster Row v+258 60Natural history; history; scientific expeditionsLEGORCHINSKY, K. V. SHIBANOV V. VINNICHENKO N.-R. HAREIDE M. KJERSTAD. l 1994Northern Mid-Atlantic Ridge (42- 48 N) ichthyofauna characteristics. Some results from the Russian-Norwegian deep-water expedition in September-October 1993. ICES CM 1994/G: 25.iGORDINA, A. D. 1985TMDistribution of ichthyoplankton in areas of the Atlantic Ocean bottom arising81 Complex studying of nature of the Atlantic OceanPart II in RussianGORDINA, A. D. 1988Structure and distributional pattern of ichthyoplankton near rises of oceanic floor.Biological resources of the thalassobathyal zone of the World Oceanfd]Abstracts of the All-Union Conference on studies of fishes of the World Ocean thalassobathyala 13-14- in RussianGORDINA, A. D. 1991HAchthyoplankton of oceanic rises of the Atlantic and Indian Oceanse Naukova Dumka. 113 p. in Russian:[ h9HGF8*T Tning, . V 1932B< Myctophum hygomi. Faune Ichthyologique de lAtlantique Nord@:Conseil Permanent pour lExploration de la Mer, Copenhague  1-18 (cards not numbered) Templeman, W 1970Additional tabular details of distributional, meristic and morphometric data for the paper: A review of the Morid fish genus Lepidion of the North Atlantic with first records of Lepidion eques from the Western North Atlantic<6Technical Report of Fisheries Research Board of Canada 160 30pp Templeman, W 1970 A review of the Morid fish genus Lepidion of the North Atlantic with first records of Lepidion eques from the Western North Atlantic4-Journal of Fisheries Research Board of Canada27457-498Thiel, H. Pfannkuche, O. Schreiver, G. Lochte, K. Gooday, A.J. Hemleben, C.H. Mantoura, R.F.G. Turley, C.M. Patching, J.W. Riemann, F. 1989`YPhytodetritus on the deep-sea floor in a central oceanic region of the Northeast AtlanticBilogical Oceanography6203-239Thompson, G. B.S 1979YDistribution and population dynamics of the limpet Patella aspera (Lamarck) in Bantry Baym3B82Journal of Experimental Marine Biology and Ecology40115-135.'Thompson, D.R. Furness, R.W Walsh, P.Mn 1992Historical changes in mercury concentrations in the marine ecosystem of the north and north-east Atlantic Ocean as indicated by seabird feathersb J. Appl. Ecolp  29 79-84.0)Thompson, D.R Furness, R.W Monteiro, L.R . 1998`ZSeabirds as biomonitors of mercury inputs to epipelagic and mesopelagic marine food chainsSci. Tot. Environ  213299-305.ZTThompson, D.R. Lilliendahl, K. Solmundsson, J Furness, R.W Waldron, S. Phillips, R.A 1999rkTrophic relationships among six species of Icelandic seabirds as determined through stable isotope analysis Condor 101 898-903. TITOVA, N. V 1981~Differentiation of Beryx splendens Lowe of the thalassic bathyal of the Atlantic Ocean by frequency of esterase locus alleles4. Genetics, selection and hybridization of fish135-137 in RussianTittley, I Neto, A. I.) 1994^WMarine algae collected during "Expedition Azores 1989", with discussion of biogeographyr ArquiplagonLife and Marine Sciences 12A 1-13:3Tizard, T. H H. N. Moseley J. Y. Buchanan J. Murraya 1885xr Narrative of the cruise of H. M. S. Challenger with a general account of the scientific results of the expeditionjdReport of the Scientific Results of the Voyage of the H. M. S. Challenger During the Years 1873-1876"Narrative Vol. I, First Part  508 (+ 19 plates) Tortonese, E J. C. Hureau  1979  Les Presses de l UNESCO 2+ Clofnam, supplment 1978, Cybium, 3e sriei  (5)5 [333] - 66 [394]&TROYANOVSKY, F.M S. F. LISOVSKYV 1995\URussian (USSR) fisheries research in deep waters (below 500 m.) in the North Atlantic@: Deep-Water Fisheries of the North Atlantic Oceanic Slope 357-365.3 in Russian 1885-1917 $://A1992JY326000042+Tsuchiya, M. Talley, L. D. McCartney, M. S.LEAn Eastern Atlantic Section from Iceland Southward across the Equator<6Deep-Sea Research Part a-Oceanographic Research Paperspolar mode water; north-atlantic; mediterranean water; norwegian-greenland; intermediate water; ocean; circulation; sea; deep; flowt A long CTD/hydrographic section with closely-spaced stations was occupied in July-August 1988 from Iceland southward to 3- degrees-S along a nominal longitude of 20-degrees-W. The section extends from the surface down to the bottom, and spans the entire mid-ocean circulation regime of the North Atlantic from the subpolar gyre through the subtropical gyre and the equatorial currents. Vertical sections of potential temperature, salinity and potential density from CTD measurements and of oxygen, silica, phosphate and nitrate, based on discrete water-sample measurements are presented and discussed in the context of the large-scale circulation of the North Atlantic Ocean. The close spacing of high-quality stations reveals some features not described previously. The more important findings include: (1) possible recirculation of the lightest Subpolar Mode Water into the tropics; (2) a thermostad at temperatures of 8-9-degrees-C, lying below that of the Equatorial 13-degrees-C Water; (3) the nutrient distribution in the low-salinity water above the Mediterranean Outflow Water that supports the previous conjecture of northern influence of the Antarctic Intermediate Water; (4) a great deal of lateral structure of the Mediterranean Outflow Water, with a number of lobes of high salinity; (5) an abrupt southern boundary of the Labrador Sea Water at the Azores-Biscay Rise and a vertically well-mixed region to its south; (6) a sharp demarcation in the central Iceland Basin between the newest Iceland-Scotland Overflow Water and older bottom water, which has a significant component of southern water; (7) evidence that the Northeast Atlantic Deep Water is a mixture of the Mediterranean Outflow Water and the Northwest Atlantic Bottom Water with very little input from the Iceland-Scotland Overflow Water; (8) an isolated core of the high-salinity, low-silica Upper North Atlantic Deep Water at the equator; (9) a core of the high-oxygen, low-nutrient Lower North Atlantic Deep Water pressed against the southern flank of the Mid-Atlantic Ridge just south of the equator; (10) a weak minimum of salinity, and well-defined maxima of nutrients associated with the oxygen minimum that separates the Middle and Lower North Atlantic Deep Waters south of the equator; (11) a large body of nearly homogeneous water beneath the Middle North Atlantic Deep Water between 20-degrees-N and the Azores-Biscay Rise; and (12) a deep westward boundary undercurrent on the southern slope of the Rockall Plateau. 1992Nov-Dec39 11-12A'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093 WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543 TSUCHIYA M UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093JCTimes Cited: 66 English Article JY326 DEEP-SEA RES PT A-OCEANOG RESISI:A1992JY326000040)Tsuchiya, M. L. D. Talley M. S. McCartney9 1992LFAn eastern Atlantic section from Iceland southward across the equator.Deep-Sea Research39 11/12A 1885-19182+TSYGANOV, V.F I. K. SIGAEV Yu. A. LOKTIONOVe 1982Distribution of Available Potential Energy, Geostrophic Circulation and Biological Productivity Indices in Two Areas of the North AtlanticNAFO SCR Doc. 82/IX/101Serial No 610. in Russian Tucker, G. M. Heath, M. F. 19940*Birds in Europe: their conservation statusBirdLife International  Cambridgea"BirdLife Conservation Series No. 3n  600pp-C, lying below that of the Equatorial 13-degrees-C Water; (3) the nutrient distribution in the low-salinity water above the Mediterranean Outflow Water that supports the previous conjecture of northern influence of the Antarctic Intermediate Water; (4) a great deal of lateral structure of the Mediterranean Outflow Water, with a number of lobes of high salinity; (5) an abrupt southern boundary of the Labrador Sea Water at the Azores-Biscay Rise and a vertically well-mixed region to its south; (6) a sharp demarcation in the central Iceland Basin between the newest Iceland-Scotland Overflow Water and older bottom water, which has a significant component of southern water; (7) evidence that the Northeast Atlantic Deep Water is a mixture of the Mediterranean Outflow Water and the Northwest Atlantic Bottom Water with very little input from the Iceland-Scotland Overflow Water; (8) an isolated core of the high-salinity, low-silica Upper North Atlantic Deep Water at the equator; (9) a core of the high-oxygen, low-nutrient Lower North Atlantic Deep Water pressed against the southern flank of the Mid-Atlantic Ridge just south of the equator; (10) a weak minimum of salinity, and well-defined maxima of nutrients associated with the oxygen minimum that separates the Middle and Lower North Atlantic Deep Waters south of the equator; (11) a large body of nearly homogeneous water beneath the Middle North Atlantic Deep Water between 20-degrees-N and the Azores-Biscay Rise; and (12) a deep westward boundary undercurrent on the southern slope of the Rockall Plateau. 1992Nov-Dec39 11-12A'UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093 WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543 TSUCHIYA M UNIV CALIF SAN DIEGO,SCRIPPS INST OCEANOG,LA JOLLA,CA 92093JCTimes Cited: 66 English Article JY326 DEEP-SEA RES PT A-OCEANOG RESISI:A1992JY326000040)Tsuchiya, M. L. D. Talley M. S. McCartney9 1992LFAn eastern Atlantic section from Iceland southward across the equator.Deep-Sea Research39 11/12A 1885-19182+TSYGANOV, V.F I. K. SIGAEV Yu. A. LOKTIONOVe 1982Distribution of Available Potential Energy, Geostrophic Circulation and Biological Productivity Indices in Two Areas of the North AtlanticNAFO SCR Doc. 82/IX/101Serial No 610. in Russian Tucker, G. M. Heath, M. F. 19940*Birds in Europe: their conservation statusBirdLife International  Cambridgea"BirdLife Conservation Series No. 3n  600ppq PVBU TTLopukhin, A.S. 1986NGDistribution of ATP Concentration Above Seamounts in the Atlantic Oceanc Oceanology263361-365{F@Seamount, ATP, Atlantic Ocean, microplankton, Mid Atlantic Ridge The distribution of microplankton ATP consentrations near seamount in the Atlantic was studied. The maximum consentration proved to occur in euphotic areas above the slopes of the seamounts, while the microplankton concentration was considerably smaller directly above the summits.,%Lozier,M.S Brechner Owens,W Curry,R.G 1995,%The climatology of the North AtlanticProgress in Oceanography36 1-44,&Lozier, M., S. W. B. Owens R. G. Curry 1995,&The climatology of the North Atlantic.Progress in Oceanography361h 1-44<5LUKASHEVICH, I. P. E. I. PRISTAVAKINA O. G. SOROKHTIN  1982hbRole of dynamics and static in formation of the relief of the northern part the Mid-Atlantic Ridge Okeanologiaf  22(5)781-788e in Russian Ltken, Chrt 1877(!To sjaeldnere pelagiske BeryciderNHOversigt over det Kongelige Danske Videnskabernes Selskabs Forhandlinger 175-194.e Ltken, Chrt 1880Spolia Atlantica. Bidrag til Kundskab om Formforandringer hos Fiske under deres Vxt og Udvikling srligt hos nogle af Atlanterhavets HjsfiskeD>Kongelige Danske Videnskabernes Selskabs Skrifter, Kjbenhaven Afd XII. 6410-613 + 5 plates Ltken, Chrt 1892Spolia Atlantica. Scopelini Musei Zoologici Universitatis Hauniensis. Bidrag til Kundskab om det aabne Havs Laxesild eller Scopeliner. Med et tillaeg om en anden pelagisk fiskeslaegtNGOversigt Kongelige Danske Videnskabernes Selskabs Skrifter, Kjbenhaven  (6) 7221-297. 8449-8468N$://A1995QX76900028I Madge, L. S. Smith, D. K.iVPSeamount Volcanism at the Reykjanes Ridge - Relationship to the Iceland Hot-Spot2+Journal of Geophysical Research-Solid EarthTMmid-atlantic ridge; east pacific rise; lava flows; segmentation; plume; oceana The axial zone of the Reykjanes Ridge is covered with small (0.5-3 lan in diameter) volcanoes that pile together to form larger axial volcanic ridges. This style of volcanism is similar to that at the Mid-Atlantic Ridge (MAR) and may be common to slow spreading ridges despite proximity of the Reykjanes Ridge to the Iceland hot spot. In this study we quantitatively investigate the population of seamounts in three study areas at the Reykjanes Ridge. Areas A and B are centered at 62 degrees N and 60 degrees N, respectively. Area C is centered at 58 degrees N and is located south of the transition in ridge morphology from an axial high to an axial graben. Using multibeam bathymetry data, 541 seamounts (summit height H > 50 m) were identified in the three areas, and their size and shape statistics were compiled. Additionally, 105 seamounts in areas B and C were recognized in deep-towed side scan images, and their surface morphologies (hummocky or smooth) were recorded. On the basis of estimated population parameters, we find that seamounts at the Reykjanes Ridge are more abundant (310 +/- 20 per 10(3) km(2)), on average, than at the MAR between 24 degrees and 30 degrees N (200 +/- 10 per 10(3) km(2)). Significant along-axis variations exist at the Reykjanes Ridge, however, which are not simply related to distance from the hot spot: area B has nearly twice the abundance of seamounts as either area A or area C. Variation in the characteristic height of the seamount population is also observed between the Reykjanes Ridge (68 +/- 2 m) and the MAR (58 +/- 2 m), but no significant variation is found between our three study areas. A dramatic change in seamount surface morphology occurs between areas B and C (there are no side scan data from area A). Area C has 78% hummocky seamounts (similar to the proportion observed at the MAR), while area B has 83% smooth seamounts. On the basis of these results, we present a conceptual model for building the shallow crust at the slow spreading Reykjanes Ridge that takes into account the possible influence of the Iceland hot spot on the crustal melt delivery system and its influence on variables that control seamount abundances, sizes, shapes, and surface morphologies. In this model we suggest that the increased seamount production and proliferation of smooth seamounts in area B may be associated with a pulse of hot spot material, in the form of asthenosphere of higher temperature, that has recently affected area B."J. Geophys. Res.-Solid Earth 1995 May 10 100B5'WOODS HOLE OCEANOG INST,DEPT GEOL & GEOPHYS,WOODS HOLE,MA 02543 MIT,WHOI,JOINT PROGRAM OCEANOG,WOODS HOLE,MA MADGE LS WOODS HOLE OCEANOG INST,DEPT GEOL & GEOPHYS,WOODS HOLE,MA 02543D>Times Cited: 1 English Article QX769 J GEOPHYS RES-SOLID EARTHISI:A1995QX76900028` 2 yGordon, J. Arnbom, T. Brum, J. M. Coxson, C. Cunha, R. Gillespie, D. Gordon, T. Hughes, K. Kirby, T. Storey, K. Walsh, V.t 1987The first cruise of "Song of the Whale" and cetacean research carried out in the Azores by the International Fund for Animal Welfare  Cambridge7 11 pp7 jcGordon, J. Arnbom, T. Gillespie, D. Gordon, T. Leaper, R. Lescrauwert, A. C. Lovell, P. Steiner, L.b 1988Preliminary report on cetacean research being conducted in the waters around the Azores by the International Fund for Animal Welfare  Cambridge 95pp LEGordon, J. Goddard, A. Leaper, R. Leaper, L. Steiner, L. Whitmore, C.e 1989.'Cetacean research program in the Azoress  Cambridged :3Report of the International Fund for Animal Welfare59Gosliner, T. M. 1990XQOpisthobranch mollusks from the Azores Islands. I. Runcinidae and Chromodorididae Aoreana Supl.d135-166d Gould, W. J. 19850)Physical oceanography of the Azores front\Progress in Oceanography14(1-4)o167-190a451-467$://A1992HJ52200013"Gowing, M. M. Wishner, K. F.ZTFeeding Ecology of Benthopelagic Zooplankton on an Eastern Tropical Pacific SeamountMarine Biologybenthic boundary-layer; santa-catalina basin; midwater food web; deep-sea; phaeodarian radiolarians; northeast pacific; sediment traps; marine snow; bacteria; water"The gut contents of dominant deep-sea benthic boundary layer zooplankton (primarily copepods and mysids) and the vacuole contents of phaeodarians collected and preserved in situ at four depths (from 724 to 3112 m) on an eastern tropical Pacific seamount (Volcano 7; 13-degrees 23'N, 102-degrees 27'W) between 23 November and 4 December 1988 were analyzed using transmission electron microscopy (TEM). Suspended, and sinking plus resuspended particles, were quantitatively sampled to characterize potential food sources. The broad oxygen minimum characteristic of this region intersects the summit of the seamount and affects the feeding ecology of these organisms. Several copepods and mysids and an amphipod contained guts packed with what appeared to be grain-positive bacteria, an unusual finding. We hypothesize that the source of these bacteria-like bodies was a mat or aggregate that originated in the oxygen minimum or at its upper or lower interface. The presence of the bacteria-like bodies in 43 to 100% of the particle-feeding zooplankton that were sectioned and that had gut contents, suggests that the bacteria-like bodies are an important food source. The diverse gut and vacuole contents of other detritivores were similar among depths. Particles and microorganisms from the depths were also similar. This finding can be explained by the rapid sinking of particles and aggregates from surface waters and their relatively intact transit through the broad oxygen minimum with its reduced populations of zooplankton. The presence of algal cells in guts and vacuoles of benthic boundary-layer zooplankton suggests that these zooplankton select particles of recent surface origin for consumption. The presence of the guts filled with bacteria-like bodies shows that some deep-sea copepods and mysids that are normally generalist feeders can specialize opportunistically. The similarity of gut contents of crustaceans and vacuole contents or phaeodarians suggests that these two very different groups of particle feeders utilize similar food sources in the deep sea. Mar. Biol. 1992 Mar 1123'UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 95064 UNIV RHODE ISL,GRAD SCH OCEANOG,NARRAGANSETT,RI 02882 GOWING MM UNIV CALIF SANTA CRUZ,INST MARINE SCI,SANTA CRUZ,CA 950644.Times Cited: 30 English Article HJ522 MAR BIOLISI:A1992HJ52200013D=Granadeiro, J. P. Monteiro, L. R. Furness, R. W. Silva, M. C.l 1995z5The food of common terns Sterna hirundo in the Azoresw'PIAbstracts of papers presented at the 5th International Seabird Conference Glasgow 20-2124-26 March 1995Ecology; feeding2 Silva1987bw Silva1990 Silva19903 Silva19924 Silva19925 Silva1994q Silva1995 Silva1995 Silva1995 Silva1995 Silva1995 Silva1996 SILVA1996 Silva1997 Silva1998, Silva1998 Silva1999-Silvain press Simes19955o Sinha2001ESIROTIN.1975FSIROTIN.19756Skreslet20000Skreslet20000 Smale1996 SMIRNOV1983 SMIRNOV1998z Smith1978 Smith1982 Smith1982 Smith1989F Smith1990Y Smith1992" Smith1993 Smith1995q Smith1995 Smith1995p Smith2000 Smolenack2000 Smoot1989 Smoot1989> Sola19988 Sola20010 Soldevilla1997H Solmundsson19991 Solmundsson2000 SOPOV1980 SOROKHTIN1982 SOROKIN1984I SOROKIN1985 SOROKIN1987 SOROKIN1987j SOROKIN19903 Sournia1994 Southward1997+ Southward2000+ Southward2000 Southward2000 Southward2000 Speer1999Y Speer1999 Stearns1984 Steenstrup1898 Stefanescu1991 Stefanescu1994Stehmann1971 Steiner1988 Steiner19896 Steiner19907 Steiner1995 Steiner1995Stewart 1989 Stewart1993 Stewart1994 Stewart1994D Stewart1996E Stewart1997 Stich1981#Stoecker1993 Storey19879IStutzman19969 SUKHOVERSHIN.1985 Sulak1974 Sullivan1995 Sutherland1993 SVETLOV1984eSVETLOV.1989  Swift1995! Swift1995 Sy1988 Sy1992Z Sy1992 Sy1999N Sy19991 T. Comtet1996gT. E. VASILIEVA1982 Talley19929[ Talley199296 Tande2000 Tande2000 TARNOPOLSKY1983> Tavares1998 Taylor1996 Tning1932 Templeman1970 Templeman1970 Theilacker1991 Thiel1989,Tholosan1999Thompson 19898Thompson1979FThompson1992Thompson1994Thompson1994+Thompson1998GThompson1998HThompson1999C Thompson_DR1999C Thompson_KR1999 Thurson1994  TIMOSHENKO20011 Tiselius1993 TITOVA19789 TITOVA19799 TITOVA19819 Tittley1994 Tizard1885 Tokarev1997Toporova19777 Tortonese1979 Tortonese1989 Tranter1991 Tranter1997i TRETYACHENKO1987Trewavas1929Tristo da Cunha 1990a TROYANOVSKY1995 TRUNOV19879 Tsuchiya1992[Tsuchiya1992 TSVETUCHIN.1983TSYGANOV1982pTucholke2000: Tucker1994S Tums19922 Turley198989 Turley19933 Turley199338 Turley1995! Tyler1988 Tyler1996Uenzelmann-Neben2002Ueyanagi1970UFINTSEV1973 UKRAINSKY1983 Uto1970 Uye1992 V.GORCHINSKY1994  Vaillancourt1995! Vaillancourt1995Vaillant1887;Vaillant1888#Van Aken1995"Van Aken1996) Van Der Spoel1979( Van Der Spoel1983$ Van Der Spoel1985% Van Der Spoel1994& Van Der Spoel19942 Van der Spoel1997' Van Der Spoel1997 Van Dover1996* Van Soest1979Vandover19944 Vangriesheim2001  Vankeuren1995! Vankeuren1995 Vass19871+ Vecchione1983< Vedel1995? Vedernikov1997> Vedernikov1999r Venrick1991, Venrick1991- Venzke2000. Vereshchaka1990/ Vereshchaka19947 Vereshchaka19950 Vereshchaka19955 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996aka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka19965 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996aka19955 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996 Vereshchaka1996  Comtet19949 Copley1996 Cordell1994 Cornec19949 Cornelius1992 a Cornelius1992bm Costa19969 Costa1996c Coutis1999 Cowles1995 Coxson1987aCraddock1970bCraddock1977Crassous19949Crassous20012 Cunha1987 Curry1995T Curry1995G Dadou2001 Dadou2001" Daly1993$ Dam1993 Dam1995 Dando1994 Daulmetov1989 Daulmetov1990 Dautzenberg1889& Davies20000 Dawson19949 De Stasio1993del Nevo1990del Nevo1991del Nevo1993del Nevo19955del Nevo19958del Nevo1996del Nevoin pressdel Nevoin press Delgado1997 Delgado1998G DEMENIN1998<Depledge1995=Depledge1995 Desbruyeres2001 Desbruyres1994 Desbruyres1996g Desoutter1993HDETINOVA1985: Deuser1992t Dias1971u Dias1976v Dias1986w Dias1990x Dias1991y Dias1991 Dill1989 Dinter2001 Dixon1998I DMITRIENKO1985 Dodson1988JDOLGANOV1985Domanski1986K DONDUA1982z DOP1993y Dower1992g Dower1996 Dower1996L DROBYSHEVA1985M DROBYSHEVA1986N DROBYSHEVA1991{ Drout1858 Drout1858 Drout1861| Drout1861a} Drout1861b- Druke1999O DRUZHININ1979 Drke1999~ Du Buit1989 Duarte1999 Dunn19901 Dunn199316 Dunn2000o Dunn2000o Duron1980PDUSHENKO1980QDUSHENKO1982RDUSHENKO1983SDUSHENKO1985TDUSHENKO1987UDUSHENKO1987VDUSHENKO1988WDUSHENKO1989X DVININ1977Y DVININ1978Z DVININ1981[ DVININ1981\ DVININ1981] DVININ1981Dyakonov19977Dyakonov19999Y Edelman1992 Ehrich1977 Eiane1998 Eleby19966 Ellertsen2000 Ellertsen2000 Ellis1985Emmerson1984 Epp1989 Epp1989 Eschmeyer1969 Esteves1984 Esteves1995 ESTEVES1996F.-Tesch1982 Fabri1994 Falkowski1991+ Fallick2000 Fasham1975 Fasham1979> Feio19981C Feio_RS1999 Felbeck1994FELDMAN.2000Feldmann1946 Fernandes1984o Fernandez2001Ferreira1937aFerreira1938Ferreira1939Ferreira1939Ferreira1940Ferreira1942 Fessenden1995 Fey1994n Fey1995b Fey2000 Fiala-Mdioni1994 Fiala-Mdioni1996Figueroa1991^ FILIN1989 FILIN1991 FILIN1992_ FILIN1995` FILIN1997 Filippova1973 Filippova1979 Filippova1987 Filippova1997a FINENKO1985S Fischer1992S Fisk19929& Fleming2000 Fonseca1993 Forward1984 Foxton1979Q Frank1997 Frank1997 Frank2002 Fransen19919 Fraser2000P Fratantoni2001 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq19921992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq199292 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq1992 Fredericq199292 Fredericq199292 Fredericq199292 Fredericq1992ansen19919 Fraser2000P Fratantoni2001 Fredericq1992 Fredericq1992 Fredericq1992Dp82Moore, P. G. Rainbow, P. S. Weeks, J. M. Smith, B. 1995~xObservations on copper and zinc in an ecological series of talitroidean amphipods (Crustacea: Amphipoda) from the AzoresAoreana Supl. 93-102455-472$://A1991EZ43500013>7Morales, C. E. Bedo, A. Harris, R. P. Tranter, P. R. G.leGrazing of Copepod Assemblages in the North-East Atlantic - the Importance of the Small Size Fraction"Journal of Plankton Researchcontinuous plankton records; vertical-distribution; calanus- finmarchicus; pigment destruction; temora-longicornis; feeding patterns; gut clearance; acartia-tonsa; phytoplankton; ratesThe North Atlantic was the site for the 1989 JGOFS Pilot Study, an international study of ocean fluxes in relation to the carbon cycle. In this paper we present preliminary estimates of the grazing pressure by copepod assemblages at four stations: 60, 56, 52 and 47-degrees-N, along the JGOFS 20- degrees-W transect, during June-July. Three major size fractions of mesoplanktonic copepods were considered: small (200-500-mu-m), medium (500-1000-mu-m) and large (1000-2000-mu- m). At each station, copepod composition and abundance were analysed and the gut fluorescence method was used to estimate ingestion rates. The results support the importance of the small size fraction relative to the other fractions, in terms of numerical abundance and their grazing impact. However, the total grazing pressure of copepods on phytoplankton was relatively minor during the period of sampling since the fraction of phytoplankton standing stock and primary production consumed by the copepods was on average < 1 and 2% respectively. The implications of these results as well as the potential sources of bias involved in these types of measurements and estimations are discussed.J. Plankton Res. 1991 MarT132S'PLYMOUTH MARINE LAB,PROSPECT PL,W HOE,PLYMOUTH PL1 3DH,ENGLAND MORALES CE PLYMOUTH MARINE LAB,PROSPECT PL,W HOE,PLYMOUTH PL1 3DH,ENGLAND:4Times Cited: 89 English Article EZ435 J PLANKTON RESISI:A1991EZ43500013 1799-1808t$://000082691600013aMorales, C. E.Carbon and nitrogen fluxes in the oceans: the contribution by zooplankton migrants to active transport in the North Atlantic during the Joint Global Ocean Flux Studyh"Journal of Plankton Researchdiel vertical migration; wax esters; respiratory carbon; calanoid copepods; bloom experiment; marine copepods; eastern gulf; metabolism; mesozooplankton; phytoplanktonaThe role of vertical migrant zooplankton, with both seasonal/ontogenetic and daily strategies, in the active transport of carbon and nitrogen out of the surface layer in the North Atlantic is analysed. The data used were obtained mainly during the Joint Global Ocean Flux Study (JGOFS)-North Atlantic Bloom Experiment (NABE) (1989-1990) in the North Atlantic and from published information on the biochemical composition of the dominant genera/species. The resulting estimates of active transport are compared with the values of sedimentation rates at the JGOFS-NABE stations and other sites in the North Atlantic. The estimates obtained support previous findings indicating that active transport, especially by interzonal diel migrants, should be taken into account in the estimation of total carbon and nitrogen export Aux. The contribution of seasonal migrants to carbon export flux, however, has been considerably underestimated before, although it appears to be significantly lower compared to that of diel migrants. Biomass estimates and biochemical composition, together with mortality and metabolic rates, should be investigated in further detail for some of the dominant species in oceanic areas in order to evaluate active transport more precisely.J. Plankton Res. 1999 Sep219r:3Times Cited: 2 English Article 238BT J PLANKTON RESuISI:000082691600013id$]\[ZYXW Madge,L.S Smith,D.Kc 1995TNSeamount volcanism at the Reykjanes Ridge:relationship to the Iceland hot spot&Journal of Geophysical Research 1009B5 8449-8468TMMID-ATLANTIC RIDGE, EAST PACIFIC RISE, LAVA FLOWS, SEGMENTATION, PLUME, OCEAN5 The axial zone of the Reykjanes Ridge is covered with small (0.5-3 lan in diameter) volcanoes that pile together to form larger axial volcanic ridges. This style of volcanism is similar to that at the Mid-Atlantic Ridge (MAR) and may be common to slow spreading ridges despite proximity of the Reykjanes Ridge to the Iceland hot spot. In this study we quantitatively investigate the population of seamounts in three study areas at the Reykjanes Ridge. Areas A and B are centered at 62 degrees N and 60 degrees N, respectively. Area C is centered at 58 degrees N and is located south of the transition in ridge morphology from an axial high to an axial graben. Using multibeam bathymetry data, 541 seamounts (summit height H > 50 m) were identified in the three areas, and their size and shape statistics were compiled. Additionally, 105 seamounts in areas B and C were recognized in deep-towed side scan images, and their surface morphologies (hummocky or smooth) were recorded. On the basis of estimated population parameters, we find that seamounts at the Reykjanes Ridge are more abundant (310 +/- 20 per 10(3) km(2)), on average, than at the MAR between 24 degrees and 30 degrees N (200 +/- 10 per 10(3) km(2)). Significant along-axis variations exist at the Reykjanes Ridge, however, which are not simply related to distance from the hot spot: area B has nearly twice the abundance of seamounts as either area A or area C. Variation in the characteristic height of the seamount population is also observed between the Reykjanes Ridge (68 +/- 2 m) and the MAR (58 +/- 2 m), but no significant variation is found between our three study areas. A dramatic change in seamount surface morphology occurs between areas B and C (there are no side scan data from area A). Area C has 78% hummocky seamounts (similar to the proportion observed at the MAR), while area B has 83% smooth seamounts. On the basis of these results, we present a conceptual model for building the shallow crust at the slow spreading Reykjanes Ridge that takes into account the possible influence of the Iceland hot spot on the crustal melt delivery system and its influence on variables that control seamount abundances, sizes, shapes, and surface morphologies. In this model we suggest that the increased seamount production and proliferation of smooth seamounts in area B may be associated with a pulse of hot spot material, in the form of asthenosphere of higher temperature, that has recently affected area B.$Magalhes, M. J. Barros, M. C. 1987piThe contamination of fish with chlorinated hidrocarbons in Portugal: continental coast and Azores islands3.'Environmental Monitoring and Assessmentd8r 37-57 MAKAROV, A V. VINNICHENKOn 1998Elusive alfoncinol Fishing News International 37, No. 7 8-99 in RussianMAKOVOZENKO, T. Vt 1983VPCalculation of thickness of the active layer in some areas of the North Atlantic Trudy GOINo  164 79-85 in Russian$MAMAEV, Yu. L A. V. ZUBCHENKOo 1978:4Two new genera of monogenies from the North AtlanticZoologichesky zhurnal LVII(8) 1131-1139o in Russian Markle, D. F 1976Preliminary studies on the systematics of the deep-sea Alepocephalidae (Pisces: Salmoniformes). A dissertation presented to the Faculty of the School of Marine Science. The College of William and Mary in Virginia(not published) 225pp Markle, D. F 1978f_Taxonomy and distribution of Rouleina attrita and Rouleina maderensis (Pisces: Alepocephalidae)eFishery Bulletin 76 (1) 78-87lMarkle N. R. Merrettt 1980The abyssal alepocephalid, Rinoctes nasutus (Pisces, Salmoniformes), a redescription and an evaluation of its systematic positionn"Journal of Zoology of London 190225-239W Markle, D. F J.-C. Quro  1986>7Fishes of the North-east Atlantic and the Mediterranean UNESCO Vol. I228-253T Marshall, N. B T. Iwamoto  1973*$Fishes of the Western North AtlanticRLSix Memoir- Sears Foundation for Marine Research, Yale University, New Haven Number One446-665"Martin, A. R. Melo, A. M. A. 1983B$Journal of Crustacean Biology52294-305wX  Ringelberg,J 1995D=Is diel vertical migration possible without a rythmic signal?"Journal of Plankton Research173h653-655243-252$://000173726200008<6Rocha, L. A. Bass, A. L. Robertson, D. R. Bowen, B. W.Adult habitat preferences, larval dispersal, and the comparative phylogeography of three Atlantic surgeonfishes (Teleostei : Acanthuridae)Molecular EcologytAcanthurus; biogeography; Brazil; Caribbean; central Atlantic islands; dispersal; reef fishes coral-reef fishes; mitochondrial-dna; patternsAlthough many reef fishes of the tropical Atlantic are widely distributed, there are large discontinuities that may strongly influence phylogeographical patterns. The freshwater outflow of the Amazon basin is recognized as a major barrier that produces a break between Brazilian and Caribbean faunas. The vast oceanic distances between Brazil and the mid-Atlantic ridge islands represent another formidable barrier. To assess the relative importance of these barriers, we compared a fragment of the mitochondrial DNA (mtDNA) cytochrome b gene among populations of three species of Atlantic surgeonfishes:Acanthurus bahianus, A. chirurgus and A. coeruleus. These species have similar life histories but different adult habitat preferences. The mtDNA data show no population structure between Brazil and the mid-Atlantic islands, indicating that this oceanic barrier is readily traversed by the pelagic larval stage of all three surgeonfishes, which spend similar to45-70 days in the pelagic environment. The Amazon is a strong barrier to dispersal of A. bahianus (d = 0.024, Phi(ST) = 0.724), a modest barrier for A. coeruleus (Phi(ST) = 0.356), and has no discernible effect as a barrier for A. chirurgus. The later species has been collected on soft bottoms with sponge habitats under the Amazon outflow, indicating that relaxed adult habitat requirements enable it to readily cross that barrier. A limited ability to use soft bottom habitats may also explain the low (but significant) population structure in A. coeruleus. In contrast, A. bahianus has not been collected over deep sponge bottoms, and rarely settles outside shallow reefs. Overall, adult habitat preferences seem to be the factor that differentiates phylogeographical patterns in these reef-associated species. Mol. Ecol. 2002 Feb112'jdUniv Florida, Dept Fisheries & Aquat Sci, 7922 NW 71st St, Gainesville, FL 32653 USA Univ Florida, Dept Fisheries & Aquat Sci, Gainesville, FL 32653 USA Univ S Florida, Dept Biol, Tampa, FL 33620 USA Smithsonian Trop Res Inst Panama, Unit 0948, APO, AA 34002 USA Rocha LA Univ Florida, Dept Fisheries & Aquat Sci, 7922 NW 71st St, Gainesville, FL 32653 USA4-Times Cited: 0 English Article 519KV MOL ECOLISI:000173726200008 Roden, G.I 1987PJEffect of seamount chains on ocean circulation and thermohaline structure. 60Keating, B.H. Fryer, P. Batiza, R Boehlert, G.W.Geophysical monograph 43  Washington DC American Geophysical Union335-354. Roe,H.S.J 1984lfThe diel migrations and distributions within a mesopelagic community in the NE Atlantic 4 the copepodsProgress in Oceanography13353-388s305-350 $://A1994BB98Q00005 Rogers, A. D.The Biology of Seamounts("Advances in Marine Biology, Vol 30 ACADEMIC PRESS LTDroughy hoplostethus-atlanticus; north pacific seamounts; deep- sea; orange roughy; genetic-variability; new-zealand; thermohaline structure; hydrothermal activity; uncharted seamount; mitochondrial-dna Advances in Marine Biology 199430*$Times Cited: 32 English Review BB98Q London'`ZROGERS AD MARINE BIOL ASSOC UNITED KINGDOM LAB,CITADEL HILL,PLYMOUTH PL1 2PB,DEVON,ENGLANDISI:A1994BB98Q00005!." 0U,&Rannou, M. J. G. Nielsen J. C. Hureau  1974RL A note on several Aphyonidae of the north Atlantic (Teleostei: Ophidioidei)F@Bulletin Museum National d Histoire Naturelle, Paris (Zoologie)  171 1249-1257$Rannou, M M. Gaborit-Rezzouk e 1976d^Contribution lՎtude des Batypteroidea (Pisces: Iniomi) de l Atlantique e de la MditrranPIBulletin Museum National d Histoire Naturelle, Paris, Srie 3 (Zoologie) (375) 263453-466Read,J.F 2001LFCONVEX-91: wter masses and circulation of the NE Atlantic supolar gyreProgress in Oceanography48461-510s Read, J. F.r 2001VOCONVEX-91: water masses and circulation of the Northeast Atlantic subpolar gyreProgress in Oceanography484461-510Rees, W. J. White, E. 1966<6New records and fauna list of hydroids from the Azores,&Annals and Magazine of Natural History Ser. 13 9271-284 Regan, C. T. 19030)On a collection of fishes from the Azoresy,&Annals and Magazine of Natural History Ser. 79344-348 Regan, C. T 1925voNew ceratioid fishes from the north- Atlantic, the Caribean Sea and the Gulf of Canada, collected by the Danao,&Annals and Magazine of Natural HistorySer. 9, Vol. XV6561-567 Regan, C. T Trewavas, E. e 1929D=The fishes of the families Astronesthidae and ChauliodontidaerZSThe Danish Dana - Expedition 1920-22 in the North Atlantic and the Gulf of Panama No. 51-39 (+ 7 plates) Reiner, F. 19906/Record of marine mammals of the Azorean islandsn&Garcia da Orta, Srie Zoolgicae152r 21-360)Reiner, F. Gonalves, J. M. Santos, R. S.n 1993pjTwo new records of Ziphiidae (Cetacea) for the Azores with an updated checklist of cetacean species. . , , Arquiplago\Life and Marine Sciences 11A113-118 Rey, J. C. 198460 La pesca del pez Espada en el Atlntico Noreste2,Relatrio da IV Semana das Pescas dos Aores 4 113-117$Rey, J. C., E. Alot A. Ramos  1984\USynopsis biologica del Bonito Sarda sarda (Bloch), del Mediterraneo y Atlantico Oeste0)ICCAT, Recueil de Documents Scientifiques 20 (2)469-502TMRibera Maycas, E. Bourdillon, A. Macquart-Molin, C. Passelaigue, F Patriti, G 1999tmDiel Variations of the bathymetric distributio of zooplankton groups and biomass in Cap-Ferret Canyon, FranceDeep-Sea Research II46 2081-2099n*#Rice, A.L. Thurson, M.H. Bett, B.J. 1994The IOSDL DEEPSEAS Programme: introduction and photographic evidence for the presence and absence of a seasonal input of phytodetritus at contrasting abyssal sites in the north-eastern Atlantic.Deep-Sea Research I41 1305-1320  Richard, J. 1910LFLes campagnes scientifiques de S. A. S. le Prince Albert Ier de Monaco<5Exposition Universelle de 1900, Principaut du Monaco9 Imprimerie du Monaco 140 pp Richard, J 1934tmListe gnrale des stations des campagnes scientifiques du Prince Albert de Monaco avec notes et observationszsRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverain du Monaco, Fascicules LXXXIX 1-348  Richard, J.s 1936lfDocuments sur les Ctacs et Pinnipids Provenant des Campagnes du Prince Albert Ier Prince de Monaco.~wRsultats des Campagnes Scientifiques Accomplies sur son Yacht par Albert Ier Prince Souverin du Monaco, Fascicule XCIV Imprimerie du Monaco 72 pp pLe Grand1983Le Grand1984Le Grand1993Le Traon2002 Leal1991 Leaper19889 Leaper19899 Leaper19899 LEBEDEV2001Lebedeva19989Lebedeva20000 LeGrand1990% Lenz1993 Lescrauwert1988 Levin1988 Levin1990} Levin1995 Levy19888 Lewis 19898 Lewis1994 Lewis1994H Lilliendahl19991 Lilliendahl2000 Lima1989LISITSYN1990LISOVSKY1990LISOVSKY19933LISOVSKY19959 LITVIN1966 LITVIN19737 LITVIN1978 LITVIN1980S Livi199294 Llewellyn1996 Lloris1991 Lloris19911 Lloris19941 Lochte198998 Lochte1995' Lodha1998 LOGVINENKO1983: Lohrenz1992 LOKTIONOV1981 LOKTIONOV1982 LOKTIONOV1984 LOKTIONOV1986 LOKTIONOV.1985h LOMAKIN1986i LOMAKIN1987 LOMAKIN1987 LOMAKIN1987 LOMAKIN1988 LOMAKIN1988 LOMAKIN1989 LOMAKIN1991 Longhurst1988 Longhurst1989 Lopes1990j Lopes1990 Lopes1991k Lopes1991 Lopes1993Lopukhin1986 Lorance1999 Lough1983 Lovell1988 Lozier1995T Lozier1995j LUKA19909 LUKASHEVICH1982@ LUKASHINA.19868: Lukashova2000SLundgren19922T Ltken1877U Ltken1880V Ltken1892 Ltken18981 Lysy19920M20000 M.C2000g Mackas1996 Mackas1996Macquart-Molin19991Macquart-Moulin1999Macquart-Moulin1999q Madge1995 Madge1995H Madin1979 Magalhes1987 MAKAROV1998 MAKOVOZENKO1983MALAKHOV19878S Mall19921 MAMAEV1978Mantoura198994Mantoura19966W Markle1976X Markle1978Y Markle1980Z Markle1986 Marques1993[Marshall1973 Martin1983 Martin19848 Martin1986\ Martin1986] Martins1977 Martins1982 Martins1985Martins1985aMartins1985b Martins1986 Martins1987% Martins1987 Martins1988 Martins1990 Martins1990 Martins1990' Martins1990_ Martins1990 Martins1991 Martins1991 Martins1992 Martins1992 Martins1992$ Martins1992` Martins1992 Martins1993 Martins1993A Martins1993 Martins1994p Martins1995q Martins1995 Martins1995 Martins1996 MASSALSKAYA1983a Matsui19843 Matsumoto1997 MATUL1994 MATUL1999; Mauchline1991 Mauchline1991b Maul1951c Maul1952d Maul1959e Maul1972f Maul1976 Mayaud193231 Maycas1999 Maycas1999 Mazaud2002 MAZHIRINA1992 MAZHIRINA1992  McCartney1992[ McCartney1992 McCartney1993 McCartney1993 McCartney1993 McCartney199393 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney199392 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 McCartney1993 54 3210/183-191$://00008897890000682Shushkina, E. A. Vinogradov, M. E. Lebedeva, L. P.tnProcesses of detritus production and fluxes of organic matter from epipelagic zones in different ocean regions Oceanologycommunities; layerThe processes of detritus production in epipelagic communities were analyzed on the basis of the ecosystem data collected in the expeditions of the Shirshov Institute of Oceanology, Russian Academy of Sciences in different regions of the World Ocean (about 300 stations). The developed algorithm was used to estimate the detritus production and the part of it that was not consumed in the upper 200-m layer and sank to the deeper layers. The roles of different organisms of plankton in the process of detritus production and consumption are evaluated. The maximum contribution to the detritus production value is made by small mesozooplankton (0.2-3 mm)-60-80%; dying large phytoplankton (>15 mu m)-10-30%; large mesozooplankton (>3- 5 mm)-4-20%. The major part of the detritus production (60-80%) is produced from food, which was not assimilated by the mesoplanktonic animals. In the epipelagic zones, this detritus is mainly grazed by bacteria (50-90%), protozoa ( 10-35%), and zooplankton (1-15%). The possibility of approximate estimation of the flux of organic matter from the biomass values of large and total mesozooplankton in the waters of different productivity is discussed. Oceanology 2000Mar-Apr402'Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia Shushkina EA Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia6/Times Cited: 0 English Article 348HF OCEANOLOGYISI:000088978900006 Silva, H. M. 1983vpPreliminary studies of the exploited stock of kitefin shark, Scymnorhinus licha (Bonnaterre, 1788) in the Azores:4International Council for the Exploration of the Sea1813 Silva, H. M. 1986a JDBiologia e avaliao das principais espcies de demersais dos Aores2,Relatrio da VI Semana das Pescas dos Aores6e105-113r Silva, H. M. 1986bpHReproduction of the forkbeard Phycis phycis (L., 1766) in Azorean waters+ ICES CM 1986/G-60 13 pp Silva, H. M. 1987ahPAn assessment of the azorean stock of kitefin shark, Dalatias licha (Bonn. 1788)5C ICES CM 1987/G-66 10 pp Silva, H. M. 1987bo*$Estado dos stocks de goraz e abrtea4-Relatrio da VII Semana das Pescas dos AoresV7a197-199\ Silva, H. M. 1992Potencialidades pesqueiras dos Aores. in Centenaire de la Dernire Campagne Ocanographique du Prince Albert de Monaco aux Aores bord de L'Hirondelle *#Saldanha, L. R, L. Martins, A. F.Aoreana Supl.199-215Silva, H. M. Krug, H. M. 1992[Virtual population analysis of the forkbeard, Phycis phycis (Linnaeus, 1766), in the Azores.< ArquiplagoLife and Earth Sciences10 5-12.'Silva, H. M. Krug, H. M. Menezes, G. M.  1994B