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  • 1995-1999  (19)
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  • 1
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The trachymedusa Ptychogastria polaris Allman, 1878 has been identified in seabed photographs from high-Arctic shelves and upper continental slopes off Northeast Greenland and in the northern Barents Sea. It was found to be a common epifaunal element, being present at 34 of 57 stations in 40- to 495-m depth and at 7 of 11 stations in 70- to 330-m depth, respectively. All specimens recorded in the photographs either sat directly at, or hovered very closely (≤ about 1 cm) over, the sea bed, indicating a primarily epibenthic life style of this hydrozoan species. The small-scale (i.e. within-station) distribution of medusae was rather patchy, with frequencies along photographic transects – consisting of 35–73 pictures distributed over seabed strips of 150- to 300-m length – varying from 1 to 58% off Northeast Greenland and from 1 to 34% in the Barents Sea. Absolute maximum density was 6 ind m−2, and station mean abundances ranged from 0.01 to 0.91 ind m−2 and from 0.01 to 0.52 ind m−2, respectively. Values tended to decrease with water depth, albeit significantly only off Northeast Greenland. Otherwise, no clear relationships to environmental conditions, such as geomorphology or near-bottom water hydrography, were detected. Circumstantial evidence suggests that seabed granulometry and potential food supply are important distribution determinants. However, further investigations are required to identify more stringently the key factors controlling the distribution of P. polaris.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Little is known about the biology and feeding ecology of Arctogadus glacialis (Peters, 1874), an endemic gadid fish species occurring circumpolarly in both ice-free and ice-covered Arctic seas. In this study we analysed specimens sampled from bottom trawl and Agassiz trawl catches conducted at eight stations in water depths from 115 to 490 m in the Northeast Water Polynya off Greenland in August 1990. Size composition and sex ratios were assessed for 585 fish with standard lengths ranging from 7.8 to 34.5 cm. Median fish sizes at the stations ranged between 8.6 and 18.8 cm. Quantitative stomach content analyses of a subsample of 175 specimens revealed that in the Northeast Water A. glacialis fed almost exclusively on pelagic prey. Truly benthic organisms were not found in the stomachs, and sympagic species were rarely recorded. Overall, calanoid copepods were the major prey in terms of numbers. However, stomach contents varied considerably between fish size groups. In terms of prey biomass, copepods dominated the diet of small fish (〈12 cm), primarily occurring at shallow stations (115–250 m), whereas amphipods and mysids were relatively more important for larger fish (〉16 cm), which dominated the catches at deep stations (360–480 m). The broad variety of diet composition indicated an opportunistic pelagic feeding pattern.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The regular sea urchin, Strongylocentrotus pallidus (G.O. Sars, 1871), is a widespread epibenthic species in high-Arctic waters. However, little is known about its distribution, standing stock, population dynamics and production. In the northern Barents Sea, S. pallidus was recorded on seabed still photographs at 10 out of 11 stations in water depths of 80–360 m. Mean abundances along photographic transects of 150–300 m length ranged between 〈0.1 and 14.7 ind. m−2 yielding a grand average of 3.6 ind. m−2. The small-scale distribution along the transects was patchy, with densities varying from nil to an overall maximum of 25.5 ind. m−2, and exhibited a significant relation to the number of stones present. Sea urchin test diameters, measured on scaled photographs, extended from 7 to 90 mm. Median values at single stations varied from 14 to 46 mm, showing a significant inverse relationship to water depth. Biomass, estimated by combining photographic abundances, size frequencies and a size-mass function established with trawled specimens, ranged between 〈0.1 and 3.0 g ash-free dry mass m−2, averaging about 1.0 g ash free dry mass m−2. An analysis of skeletal growth bands in genital plates was carried out with 143 trawled individuals ranging in test diameter (D) from 4 to 48 mm. Assuming these bands to represent annual growth marks, the ages of the specimens analysed ranged between 3 and 42 years. A von Bertalanffy function was fitted to size-at-age data to model individual growth pattern (D∞ = 102.3 mm, k = 0.011 year−1, t0 = 0.633 year). The annual mortality rate Z of the population in the northern Barents Sea was estimated from a size-converted catch curve to be 0.08 year−1. Applying the weight-specific growth rate method, the average P/B ratio and the mean annual production of this population were estimated as 0.07 year−1 and 0.076 g AFDM m−2 year−1, respectively. In conclusion, S. pallidus is characterized by slow growth, low mortality, high longevity and low productivity. Because of its relatively high biomass, it is considered to contribute significantly to total benthic standing stock and carbon flux in the study area.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Composition and distribution of asteroid and ophiuroid assemblages were investigated by means of Agassiz trawl catches at 34 stations in 220- to 1,200-m depth in the Weddell Sea and at 17 stations in 90- and 830-m depth off Northeast Greenland. A total of 86 species (48 sea stars, 38 brittle stars) were identified in the Weddell Sea whereas off Northeast Greenland a total of 26 species (16 sea stars, 10 brittle stars) were recorded. In both study areas, brittle stars were numerically more important than sea stars, and abundances generally decreased with water depths. Multivariate analyses revealed a conspicuous depth zonation of sea and brittle stars off Greenland. Very high abundances of Ophiocten sericeum and Ophiura robusta characterized the assemblages on shallow shelf banks whereas in greater depths Ophiopleura borealis, Ophioscolex glacialis and Ophiacantha bidentata became dominant, albeit at significantly lower densities. Mass occurrences of brittle stars, such as those recorded on Greenlandic shelf banks, have not been discovered in the Weddell Sea, where distinct assemblages were discriminated in deep shelf trenches as well as on the eastern and southern shelf. Ophioplocus incipiens, Ophiurolepis martensi and Ophiurolepis brevirima were the most prominent species on the eastern shelf. Ophiacantha antarctica, Ophiurolepis gelida and Ophionotus victoriae on the southern shelf, and Ophiosparte gigas as well as the asteriod Hymenaster sp., in the shelf trenches. Overall, the Weddell Sea housed conspicuously more asterozoan species than the waters off Greenland. Higher species diversity was also evident at both a regional and local scale, especially for the eastern Weddell Sea shelf. However, because many species from the Weddell Sea are closely related, the Weddell Sea assemblages were not significantly different from the Greenland ones in terms of taxonomic diversity and distinctness.
    Type of Medium: Electronic Resource
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  • 5
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    Alfred-Wegener-Institut für Polarforschung
    In:  Berichte zur Polarforschung, 174 . Alfred-Wegener-Institut für Polarforschung, Bremerhaven, 6 ungez., XI, 387 pp.
    Publication Date: 2019-09-23
    Description: PREFACE : The Laptev Sea System The Arctic Ocean, in particular the wide Eurasian shelf seas comprise some of the most sensitive elements of the global environment which are believed to respond at a very early time to Global Change. The renewed interest in the Arctic, the large scale international research efforts devoted to the Arctic, as well as the presently available new technology to carry out research in ice-infested areas, have opened many new avenues to conduct investigations On the variability of the depositional environments of the Eurasian shelf seas. The Laptev Sea is of particular importance in the string of the Eurasian shelf seas because feeding the Transpolar Drift of the Arctic sea-ice Cover it exports relatively the largest amounts of sea ice into the Open Arctic Ocean, because it is farthest away from the influence of the Atlantic and Pacific waters, and because it is under the influence of rapidly changing fresh water fluxes from the Siberian hinterland (Fig. 1, Sea ice drift paths in the Arctic Ocean). The morphology of the seafloor, the rapidly changing coast lines of the fragil Lena Delta Island frame work as well as the presence of submarine permafrost are examples for the dynamics of the entire Laptev Sea System. - Fig. 1 - In order to address the natural properties of the Laptev Sea System a joint research project is carried out between a number of Russian and German research institutions under the framework of the "Laptev Sea System Project" (Fig. 2, Research institutions under the framework of the "Laptev Sea System Project"). Every year expeditions are carried out in the area on Russian or German research vessels where multi-disciplinary and binational working groups are addressing some of the identified scientific themes. Results from these joint investigations are then discussed in a series of RussianIGerman workshops which are held alternatively in Russia or Germany. The second workshop 'Russian-German Cooperation: Laptev Sea System' was held in November 1994 in St. Petersburg in order to assess (1) the state of knowledge of the Laptev Sea and the adjacent continental margin of the deep Arctic, and (2) to develop a research strategy for the marine geosciences in the Laptev Sea and terrestrial werk in East Siberia. The workshop brought together more than 100 scientists, among them meteorologists, sea ice physicists, oceanographers, biologists, chemists, geologists and geophysicists from various Russian and German research institutions. The main goal of the workshop was to promote and coordinate scientific collaboration among scientists from Russia and Germany. Main emphasis have laid on first scientific results of the expeditions within the scope of the interdisciplinary Russian-German research project 'Laptev Sea System', that is present and past oceanography, ecology, and climatology of the Laptev Sea. The workshop was organized into serveral sessions which followed various themes of the environment of the Laptev Sea from their present situation to their geological record: (I) Ciimate and Ice (11) Modern Environment of the Laptev Sea (111) Environmental History of the Laptev Sea (IV) From Siberia to the Arctic Ocean: Land-Sea Connection (V) Strategy and Plans for Future Work (VI) Mid-long Term Perspectives The scientific content of this workshop is documented in this report containing most of the results and discussions. The publication of this volume serves various purposes. It is primarily a forum for scientists working in the Siberian shelf seas, in which the results of many years of research and preliminary shipboard results can be presented. In order to provide all the participants in the workshop with the opportunity for reporting their results, a speedy way of publication was chosen. Thus, each individual author has presented his opinions and views as he or she sees them, reflecting the diversity and complexity of the Laptev Sea system. On the other hand, this volume offers many researchers the possibility of acquainting themselves with methods and results of research into the East Siberian seas as carried out in other parts of the world. Finally, it is hoped that this collection of papers will function as another step toward joint research projects and are base for the expeditions to be carried out in 1995 and the following years. Many of the papers published identify major scientific problems, thus offering new perspectives for future scientific research in polar regions. The nature of the papers, the discussions and the disciplines of the attendees clearly demonstrate that the study of the Laptev Sea System is a multidisciplinary one in an interesting key area involving all branches of the natural sciences, such as ice physics, oceanography, biology and geology, in particular. It thus remains an important example for GLOBAL CHANGE and CLIMATE IMPACT research within international research efforts, e.g. International Arctic Science Committee (IASC), Arctic Ocean Sciences Board (AOSB) or the Nansen Arctic Drilling Programme (NAD). - Fig. 2 - The editors also made an effort, probably not wholly successful, to edit manuscripts by non-English-speaking authors to make them easier to understand. In this process, we hope we have not changed the meanings of the original papers. Above all we thank Bettina Rohr and Daniel Krüger who kindly assisted in editing the papers. The workshop has been sponsored by the German and Russian Ministries for Research and Technology and the meeting was held from the 21st to the 14th of November in 1994 in the Arctic and Antarctic Research Institute in St. Petersburg. We wish to thank these organizations for their financial and logistic support.
    Type: Report , NonPeerReviewed
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  • 6
    Publication Date: 2017-03-17
    Type: Article , NonPeerReviewed
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  • 7
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    PANGAEA
    In:  Supplement to: Piepenburg, Dieter; Chernova, Natalia V; von Dorrien, Christian F; Gutt, Julian; Neyelov, Alexei V; Rachor, Eike; Saldanha, Luiz; Schmid, Michael K (1996): Megabenthic communities in the waters around Svalbard. Polar Biology, 16(6), 431-446, https://doi.org/10.1007/BF02390425
    Publication Date: 2023-08-19
    Description: Composition and distribution of megabenthic communities around Svalbard were investigated in June/July 1991 with 20 Agassiz trawl and 5 bottom trawl hauls in depths between 100 and 2100 m. About 370 species, ranging from sponges to fish, were identified in the catches. Species numbers per station ranged from 21 to 86. Brittle stars, such as Ophiacantha bidentata, Ophiura sarsi and Ophiocten sericeum, were most important in terms of constancy and relative abundance in the catches. Other prominent faunal elements were eunephthyid alcyonarians, bivalves, shrimps, sea stars and fish (Gadidae, Zoarcidae, Cottidae). Multivariate analyses of the species and environmental data sets showed that the spatial distribution of the megabenthos was characterized by a pronounced depth zonation: abyssal, bathyal, off-shore shelf and fjordic communities were discriminated. However, a gradient in sediment properties, especially the organic carbon content, seemed to superimpose on the bathymetric pattern. Both main factors are interpreted as proxies of the average food availability, which is, hence, suggested to have the strongest influence in structuring megabenthic communities off Svalbard.
    Keywords: EPOS; European Polarstern Study
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 8
    Publication Date: 2023-08-19
    Keywords: Agassiz Trawl; AGT; Arctic Ocean; ARK-VIII/2; Barents Sea; Bottom trawl; BT; Date/Time of event; Date/Time of event 2; Elevation of event; Elevation of event 2; EPOS; European Polarstern Study; Event label; Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; Method/Device of event; North Greenland Sea; Norwegian Sea; Polarstern; PS19/040-2; PS19/042-1; PS19/045-2; PS19/050-2; PS19/055-2; PS19/070-2; PS19/076-2; PS19/077-2; PS19/078-2; PS19/082-2; PS19/084-2; PS19/086-2; PS19/090-3; PS19/100-2; PS19/101-2; PS19/104-2; PS19/105-2; PS19/107-2; PS19/108-2; PS19/112-2; PS19/119A-1; PS19/125-1; PS19/134-2; PS19/136-2; PS19/141-2; PS19 EPOS II; South Atlantic Ocean; Station label; Topography
    Type: Dataset
    Format: text/tab-separated-values, 50 data points
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  • 9
    Publication Date: 2023-08-19
    Keywords: Abietinaria abietina; Acanthostepheia sp.; Aceroides latipes; Acryptolaria borealis; Admete viridula; Agassiz Trawl; Aglaophamus sp.; AGT; Alcyonidium gelatinosum anderssoni; Alcyonidium mamillatum; Alcyonidium radicellatum; Allantactis parasitica; Amathillopsis spinosa; Ampelisca eschrichti; Ampharete sp.; Amphianthus aff. margaritaceus; Amphicteis gunneri; Amphicteis sundevalli; Amphilochus sp.; Amphitrite cirrata; Amphiura sundevalli; Anarhichas minor; Anisarchus medius; Anomalosipho altus; Anonyx nugax; Apomatus globifer; Arctic Ocean; Arctinula greenlandicus; ARK-VIII/2; Artacama proboscidea; Artediellus atlanticus; Ascidiacea sp.; Astarte acuticostata; Astarte borealis placenta; Astarte crenata crenata; Astarte montagui striata; Austrosyrrhoe fimbriatus; Balanus balanus; Barents Sea; Bathyarca glacialis; Bathyarca pectunculoides; Bathybiaster vexillifer; Bathycrinus carpenterii; Bathypolypus arcticus; Bispira sp.; Boreogadus saida; Boreonymphon abyssorum; Boreonymphon ossiansarsi; Boreotrophon truncatus; Bottom trawl; Brada cf. villosa; Brada inhabilis; BT; Buccinum hydrophanum; Buccinum nivale; Byblis gaimardi; Byblis longicornis; Bythocaris leucopis; Cactosoma abyssorum; Calathura brachiata; Careproctus reinhardti; Careproctus spp.; Caulophacus arcticus; Cellepora canaliculata; Cellepora nodulosa; Cellepora pumicosa; Ceramaster granularis; Chitonidae sp.; Chlamys islandica; Ciliatocardium ciliatum; Cladorhiza gelida; Cleippides quadricuspis; Colossendeis angusta; Colossendeis proboscidea; Colus islandicus; Colus latericeus; Colus sabini; Colus turgidulus; Cottunculus microps; Cribrilina watersi; Crisia eburneo-denticulata; Crisiella sp.; Cryptonatica clausa; Ctenodiscus crispatus; Cucumaria cf. frondosa; Curtitoma trevelliana; Cuspidaria arctica; Cuspidaria subtorta; Cyclopecten imbrifer; Cylichna sp.; Cystisella saccata; Dacrydium vitreum; Date/Time of event; Date/Time of event 2; Defrancia lucernaria; Diastylis goodsiri; Diastylis lepechini; Diastylis spinulosa; Diplosolen intricarius; Diplosolen obelia arctica; Disporella hispida; Dulichia macera; Edwardsia sp.; Ekmania sp.; Elevation of event; Elevation of event 2; Elpidia glacialis; Epimeria loricata; Epizoanthus incrustatus; EPOS; Escharoides jacksoni; Eucratea loricata; Eudendrium capillare; Eudendrium ramosum; Eumicrotremus spinosus; Eupyrgus scaber; European Polarstern Study; Eusirus cuspidatus; Eusirus longipes; Event label; Frigidoalvania janmayeni; Gadus morhua; Gattyana cirrosa; Geodia sp.; Glandulactis spetsbergensis; Glyphanostomum sp.; Gnathia stygia; Gorgonocephalus spp.; Grammaria abietina; Gymnelus retrodorsalis; Gymnocanthus tricuspis; Halecium beanii; Halecium labrosum; Halecium muricatum; Haploops cf. sibirica; Haploops tubicola; Harmothoe (Eunoe) nodosa; Heliometra glacialis; Henricia spp.; Hiatella arctica; Hippasteria phrygiana; Hippoglossoides platessoides; Hippoglossus hippoglossus; Hormathia digitata; Hormathia nodosa; Hornera lichenoides; Hyas sp.; Hydractinia carica; Hymenaster pellucidus; Hymenodora glacialis; Icasterias panopla; Icelus bicornis; Idmidronea atlantica gracillima; Idunella cf. aequicornis; Ischyrocerus sp.; Kadosactis rosea; Kinetoskias smitti; Korethraster hispidus; Lafoea dumosa; Lafoea grandis; Laonice cf. sarsi; Laonice spirata; Latitude of event; Latitude of event 2; Lebbeus polaris; Leionucula belloti; Leionucula corticata; Lepeta coeca; Lepidepecreum umbo; Leptagonus decagonus; Leptasterias sp.; Leptoclinus maculatus; Leptychaster arcticus; Lichenopora verrucaria; Liljeborgia fissicornis; Liljeborgia sp.; Liparis fabricii; Liparis gibbus; Liponema multicornis; Lissodendoryx spp.; Longitude of event; Longitude of event 2; Lophaster furcifer; Lumbrineris fragilis; Lumbrineris sp.; Lumpenus lampretaeformis; Lunatia pallida; Lycenchelys kolthoffi; Lycodes esmarkii; Lycodes eudipleurostictus; Lycodes frigidus; Lycodes pallidus; Lycodes reticulatus; Lycodes rossi; Lycodes seminudus; Lycodes squamiventer; Lycodes vahlii gracilis; Lycodonus flagellicauda; Lycodonus sp.; Macandrevia cranium; Macoma calcarea; Macrourus berglax; Maldane sarsi; Mallotus villosus; Margarites costalis sordida; Margarites sp.; Melanogrammus aeglefinus; Melinna cristata; Melinnopsis arctica; Melita dentata; Method/Device of event; Metopa cf. borealis; Modeeria plicatile; Modeeria rotunda; Mohnia parva; Molpadia sp.; Munnopsurus giganteus; Musculus niger; Mya truncata; Myriapora coarctata; Myriapora subgracilis; Myriochele sp.; Myriotrochus rinkii; Neoamphitrite affinis; Neohela monstrosa; Nephtys caeca; Nereis zonata; Nicomache lumbricalis; Nolella dilatata; North Greenland Sea; Norwegian Sea; Notoplites sibirica; Nuculana pernula; Nymphon cf. gracile; Nymphon elegans; Nymphon grossipes; Nymphon hirtipes; Nymphon sluiteri; Nymphon stroemi; Oenopota cinerea; Oenopota pyramidalis; Onchidiopsis sp.; Onogadus argentatus; Onuphis conchylega; Ophelia cf. rathkei; Ophelina acuminata; Ophiacantha bidentata; Ophiocten sericeum; Ophiopholis aculeata; Ophiopleura borealis; Ophiopus arcticus; Ophioscolex glacialis; Ophiura robusta; Ophiura sarsi; Owenia fusiformis; Pagurus pubescens; Palmicellaria skenei bicornis; Pandalus borealis; Panomya arctica; Paraliparis bathybius; Paramphithoe hystrix; Parasmittina jeffreysi; Pardaliscidae; Parerythrops spectabilis; Pasiphaea tarda; Phascolion strombi; Pherusa plumosa; Phoxocephalidae sp.; Phylactella labiata; Phyllodoce groenlandica; Pista maculata; Podoceridae sp.; Polarstern; Poliometra prolixa; Polycirrus medusa; Polymastia mamillaris; Pontaster tenuispinus; Poraniomorpha bidens; Poraniomorpha hispida; Poraniomorpha tumida; Porella minuta; Pourtalesia sp.; Priapulus bicaudatus; Prionospio cf. malmgreni; Protula tubularia; PS19/040-2; PS19/042-1; PS19/045-2; PS19/050-2; PS19/055-2; PS19/070-2; PS19/076-2; PS19/077-2; PS19/078-2; PS19/082-2; PS19/084-2; PS19/086-2; PS19/090-3; PS19/100-2; PS19/101-2; PS19/104-2; PS19/105-2; PS19/107-2; PS19/108-2; PS19/112-2; PS19/119A-1; PS19/125-1; PS19/134-2; PS19/136-2; PS19/141-2; PS19 EPOS II; Pseudoflustra birulai; Pseudoflustra hincksi; Pseudoflustra sinuosa; Pseudoflustra solida; Pseudomma roseum; Psolus sp.; Pteraster obscurus; Ptychogastria polaris; Pycnanthus densus; Radiella sol; Ragionula rosacea; Raja hyperborea; Raja radiata; Reinhardtius hippoglossoides; Retepora beaniana; Rhachotropis aculeata; Rhizocaulus verticillatus; Rozinante fragilis; Sabellidae sp.; Sabinea septemcarinata; Saduria megalura; Saduria sabini; Sagartia splendens; Sample code/label; Sarsiflustra abyssicola; Scalpellum sp.; Sclerocrangon cf. boreas; Sclerocrangon ferox; Sebastes mentella; Securiflustra securifrons; Serpulidae sp.; Sertularella tenella; Sertularia tenera; Siphonodentalium lobatum; Smittina glaciata; Socarnes bidenticulatus; Solaster spp.; South Atlantic Ocean; Spiochaetopterus typicus; Spirontocaris spinus; Staurophora mertensii; Stegocephalopsis ampulla; Stegocephalus inflatus; Stomphia coccinea; Strongylocentrotus pallidus; Tachyrhynchus erosus; Tealia felina lofotensis; Tentorium semisuberites; Terebellidae sp.; Terebratulina retusa; Tetilla polyura; Thelepus cincinnatus; Thracia myopsis; Tiron spiniferum; Tmetonyx cicada; Tremaster mirabilis; Tricellaria gracilis; Tricellaria ternata; Trichobranchidae sp.; Triglops murrayi; Triglops nybelini; Tubulipora fruticosa; Turrisipho voeringi; Umbellula encrinus; Unciola cf. planipes; Unciola leucopis; Urasterias lincki; Velutina sp.; Volutopsius norwegicus; Yoldia hyperborea; Yoldiella intermedia; Yoldiella lenticula; Yoldiella lucida; Zygophylax pinnatus
    Type: Dataset
    Format: text/tab-separated-values, 8425 data points
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  • 10
    Publication Date: 2023-08-19
    Keywords: Area/locality; ARK-VIII/2; Carbon, organic, total; DEPTH, sediment/rock; Element analyser CHN, LECO; Elevation of event; EPOS; European Polarstern Study; Event label; Grain size, sieving/settling tube; Latitude of event; Longitude of event; MULT; Multiple investigations; Polarstern; PS19/040; PS19/045; PS19/050; PS19/055; PS19/070; PS19/078; PS19/082; PS19/084; PS19/086; PS19/090; PS19/100; PS19/101; PS19/104; PS19/105; PS19/108; PS19/112; PS19/119A; PS19/134; PS19/136; PS19 EPOS II; Size fraction 〈 0.063 mm, mud, silt+clay; Topography
    Type: Dataset
    Format: text/tab-separated-values, 76 data points
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