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data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647060/Approaching_the_diversity_and_density_dilemma_of_the_lebensspuren_tracemaker_tandem_a_study_case_from_abyssal_Northwest_Pacific"><img alt="Research paper thumbnail of Approaching the diversity and density dilemma of the lebensspuren-tracemaker tandem: a study case from abyssal Northwest Pacific" class="work-thumbnail" src="https://attachments.academia-assets.com/121350427/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647060/Approaching_the_diversity_and_density_dilemma_of_the_lebensspuren_tracemaker_tandem_a_study_case_from_abyssal_Northwest_Pacific">Approaching the diversity and density dilemma of the lebensspuren-tracemaker tandem: a study case from abyssal Northwest Pacific</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the deep-sea, the interaction between benthic fauna and substrate mainly occurs through biotur...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the deep-sea, the interaction between benthic fauna and substrate mainly occurs through bioturbational processes which can be preserved as traces (i.e., lebensspuren). Lebensspuren are common features of deep seafloor landscapes and usually more abundant than the organism that produce them (i.e., tracemakers), rendering them promising proxies to infer biodiversity. The density and diversity relationships between lebensspuren and benthic fauna are to the present day unclear and contradicting hypotheses have been proposed suggesting negative, positive, or even null correlations. To test these hypotheses, in this study lebensspuren, tracemakers (specific epibenthic fauna that produce these traces), degrading fauna (benthic fauna that can erase lebensspuren), and fauna in general were characterized taxonomically at eight deep-sea stations in the Kuril Kamchatka Trench area. No general correlation (over-all study area) could be observed between diversities of lebensspuren, tracemakers, degrading fauna and fauna. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647059"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647059/Peracarid_fauna_Crustacea_Malacostraca_of_the_Northeast_Water_Polynya_off_Greenland_documenting_close_benthic_pelagic_coupling_in_the_Westwind_Trough"><img alt="Research paper thumbnail of Peracarid fauna (Crustacea, Malacostraca) of the Northeast Water Polynya off Greenland:documenting close benthic-pelagic coupling in the Westwind Trough" class="work-thumbnail" src="https://attachments.academia-assets.com/121350424/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647059/Peracarid_fauna_Crustacea_Malacostraca_of_the_Northeast_Water_Polynya_off_Greenland_documenting_close_benthic_pelagic_coupling_in_the_Westwind_Trough">Peracarid fauna (Crustacea, Malacostraca) of the Northeast Water Polynya off Greenland:documenting close benthic-pelagic coupling in the Westwind Trough</a></div><div class="wp-workCard_item"><span>Marine Ecology Progress Series</span><span>, 1995</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Composition, abundance, and diversity of peracarids (Crustacea) were investigated over a period o...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Composition, abundance, and diversity of peracarids (Crustacea) were investigated over a period of 3 mo in the Northeast Water Polynya (NEW), off Greenland. Samples were collected from May to July 1993 during expeditions ARK IX/2 and 3 using an epibenthic sledge on RV 'Polarstern' Within the macrobenthic community peracarids were an important component of the shelf fauna and occurred in high abundance in this area together with polychaetes, molluscs and brittle stars. A total of 38322 specimens were sampled from 22 stations. Cumacea attained the highest total abundance and Amphipoda the highest d~versity. Isopoda were of medium abundance, Mysidacea less abundant, and Tanaidacea least abundant. In total 229 species were found. Differences in composition, abundance and diversity do not reflect bathymetric gradients, but mainly the availability of food (phytoplankton and especially ice algae) and, hence, the temporal and spatial opening of the polynya. Thus primary production and hydrographic condit~ons (lateral advection due to the ant~cyclonic gyre around Belgica Bank) are the main biological and physical parameters influencing the peracarid crustacean community, documenting a close coupling between primary production and the benthic community in the eastern Westwind Trough. The high abundance of Peracarida, which are also capable of burrowing in the upper sediment layers, indicates their importance for benthic carbon cycling.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="79b44a60fbad0fd1be5d98dba0d9c6b1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350424,"asset_id":127647059,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350424/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647059"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647059"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647059; 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Several strategic groups (SGs) have been established under the KDM umbrella to address overarching marine scientific topics with a high societal relevance, including observing systems, coastal and climate research, biodiversity, and marine biological as well as mineral resources.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bce6845c3deae54438b125dcda18ca22" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350422,"asset_id":127647058,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350422/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647058"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647058"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647058; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647056"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647056/A_new_species_of_Cirolana_Leach_1818_Crustacea_Isopoda_Cirolanidae_from_the_western_Ross_Sea_Antarctica_the_first_record_of_the_genus_from_polar_waters"><img alt="Research paper thumbnail of A new species of Cirolana Leach, 1818 (Crustacea, Isopoda, Cirolanidae) from the western Ross Sea, Antarctica, the first record of the genus from polar waters" class="work-thumbnail" src="https://attachments.academia-assets.com/121350420/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647056/A_new_species_of_Cirolana_Leach_1818_Crustacea_Isopoda_Cirolanidae_from_the_western_Ross_Sea_Antarctica_the_first_record_of_the_genus_from_polar_waters">A new species of Cirolana Leach, 1818 (Crustacea, Isopoda, Cirolanidae) from the western Ross Sea, Antarctica, the first record of the genus from polar waters</a></div><div class="wp-workCard_item"><span>Zenodo (CERN European Organization for Nuclear Research)</span><span>, Dec 31, 2006</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cirolana mclaughlinae n. sp. is described from specimens collected in the Ross Sea, Antarctica. T...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Cirolana mclaughlinae n. sp. is described from specimens collected in the Ross Sea, Antarctica. Th e species is characterised by the head having a prominent anterior marginal ridge, lacking a rostrum, and being dorsally depressed; the posterior submarginal surfaces of pereonites 5-7 and the pleonites are nodulose and pitted; the pleotelson has weakly concave lateral margins converging to a narrowly rounded apex, the dorsal surface is provided with a low, longitudinal median ridge. Th e genus has a world-wide distribution, but has hitherto not been recorded from polar waters, the previous most southerly record being at about 44°S. Une nouvelle espèce de Cirolana Leach, 1818 (Crustacea, Isopoda, Cirolanidae) provenant de la mer de Ross occidentale dans l'Antarctique, première récolte du genre dans les eaux polaires. Cirolana mclaughlinae n. sp. est décrite d'après des spécimens récoltés dans l'Antarctique, en mer de Ross. L'espèce se caractérise par la tête dépourvue de ZOOSYSTEMA • 2006 • 28 (2)</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b5cd8a83c7a9d27dd549b59a24247f81" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350420,"asset_id":127647056,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350420/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647056"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647056"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647056; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647054"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647054/Climate_change_and_fisheries_affect_benthic_composition_and_diversity_in_the_North_Sea_Investigations_at_the_Dogger_Bank_during_three_decades_1991_2021_"><img alt="Research paper thumbnail of Climate change and fisheries affect benthic composition and diversity in the North Sea - Investigations at the Dogger Bank during three decades (1991-2021)" class="work-thumbnail" src="https://attachments.academia-assets.com/121350417/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647054/Climate_change_and_fisheries_affect_benthic_composition_and_diversity_in_the_North_Sea_Investigations_at_the_Dogger_Bank_during_three_decades_1991_2021_">Climate change and fisheries affect benthic composition and diversity in the North Sea - Investigations at the Dogger Bank during three decades (1991-2021)</a></div><div class="wp-workCard_item"><span>Research Square (Research Square)</span><span>, Jul 27, 2023</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Over a period of 30 years benthic fauna was monitored at a long-term sampling station at the NATU...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Over a period of 30 years benthic fauna was monitored at a long-term sampling station at the NATURA2000 marine protected area Dogger Bank and at a reference station in Dutch waters, using a ring dredge and a 2 m beam trawl. Changes of benthic diversity of 127 species were detected in 238 temporally distributed samples and correlated with temperature and intensity of bottom shing. Our results provide a solid benchmark for future research in the German Exclusive Economic Zone. During the timeframe of our study, the temperature at depths below 30 m remarkably increased by 4°C, while shing pressure in the studied ICES rectangles decreased over the past 30 years from over 100.000 h of trawling per year to about 20.000 h. The numbers of benthic individuals sampled each year show a negative trend, while the number from 1991 to 2001 is rst more in uenced by shing, later by temperature. An analysis of the benthic fauna at some stations adjacent to the long-term sampled station, sampled in 2021, showed that species composition is comparatively uniform over space and that therefore long-term sampling of one station can be used as a proxy for its surroundings in this area.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0b48e16ebbff11f67238de853a74645c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350417,"asset_id":127647054,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350417/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647054"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647054"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647054; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647053"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647053/Abundance_of_benthic_peracarids_sampled_in_the_Atlantic_Sector_of_the_Southern_Ocean_and_Weddell_Sea_during_expeditions_JR15005_JR275_JR17003a_PS118"><img alt="Research paper thumbnail of Abundance of benthic peracarids sampled in the Atlantic Sector of the Southern Ocean and Weddell Sea during expeditions JR15005, JR275, JR17003a, PS118" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647053/Abundance_of_benthic_peracarids_sampled_in_the_Atlantic_Sector_of_the_Southern_Ocean_and_Weddell_Sea_during_expeditions_JR15005_JR275_JR17003a_PS118">Abundance of benthic peracarids sampled in the Atlantic Sector of the Southern Ocean and Weddell Sea during expeditions JR15005, JR275, JR17003a, PS118</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Peracarid abundance and composition were studied in the Atlantic Sector of the Southern Ocean and...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Peracarid abundance and composition were studied in the Atlantic Sector of the Southern Ocean and the Weddell Sea at a depth range of 403-2021 m. Samples were collected using an epibenthic sledge (EBS) during expeditions on board the RRS James Clarke Ross in the Filchner Trough (JR275), the South Orkney Islands (JR15005), the Prince Gustav Channel (JR17003a) and on board the RV Polarstern in the Eastern Antarctic Peninsula (PS118). Expeditions took place in February-March 2012, 2016, 2018 and 2019 respectively. Since the trawling distance between stations was not always the same, in order to make data comparable between different stations, numbers of individuals were standardized to 1000 m haul distances.In total 64766 peracarids were found and sorted into five different orders (Amphipoda, Cumacea, Isopoda, Mysidacea and Tanaidacea). Amphipods were the most abundant group representing the 32% of the total abundances. The Filchner Trough had the highest abundance of peracarids, while...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647053"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647053"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647053; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647053]").text(description); $(".js-view-count[data-work-id=127647053]").attr('title', description).tooltip(); 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} }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647052"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647052/Zooplankton_sampled_under_ice_during_POLARSTERN_cruise_PS81_ANT_XXIX_7_"><img alt="Research paper thumbnail of Zooplankton sampled under-ice during POLARSTERN cruise PS81 (ANT-XXIX/7)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647052/Zooplankton_sampled_under_ice_during_POLARSTERN_cruise_PS81_ANT_XXIX_7_">Zooplankton sampled under-ice during POLARSTERN cruise PS81 (ANT-XXIX/7)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647052"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647052"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647052; 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Peters, Janna; Flores, Hauke; Brandt, Angelika (2011): Demersal fishes from the Antarctic shelf and deep sea: A diet study based on fatty acid ..." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647051/Gut_filling_gut_content_and_fatty_acid_composition_of_demersal_fish_species_sampled_during_POLARSTERN_cruise_ANT_XXIV_2_supplement_to_W%C3%BCrzberg_Laura_Peters_Janna_Flores_Hauke_Brandt_Angelika_2011_Demersal_fishes_from_the_Antarctic_shelf_and_deep_sea_A_diet_study_based_on_fatty_acid_">Gut filling, gut content and fatty acid composition of demersal fish species sampled during POLARSTERN cruise ANT-XXIV/2, supplement to: Würzberg, Laura; Peters, Janna; Flores, Hauke; Brandt, Angelika (2011): Demersal fishes from the Antarctic shelf and deep sea: A diet study based on fatty acid ...</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The gut contents and fatty acid composition of 49 fish belonging to five Antarctic demersal famil...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The gut contents and fatty acid composition of 49 fish belonging to five Antarctic demersal families (Nototheniidae, Macrouridae, Channichtyidae, Bathydraconidae and Artedidraconidae) sampled at two stations at the Southern Ocean shelf and deep sea (600 and 2150 m) were analysed in order to identify their main food resource by linking trophic biomarkers with the dietary items found in the fish guts. Main food items of most fish analysed were amphipod crustaceans (e.g. in 63% of Trematomus bernachii guts) and polychaetes (e.g. in 80% of Bathydraco sp. guts), but other food items including fish, other crustaceans and gastropods were also ingested. The most prominent fatty acids found were 20:5(n-3), 16:0, 22:6(n-3) and 18:1(n-9). The results of gut content and fatty acid analyses indicate that all fish except the Channichthyidae share similar food resources irrespective of their depth distribution, i.e. benthic amphipods and polychaetes. A difference of the dietary spectrum can be obs...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647051"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647051"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647051; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647051]").text(description); $(".js-view-count[data-work-id=127647051]").attr('title', description).tooltip(); 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</script> <div class="js-work-strip profile--work_container" data-work-id="127647046"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647046/Macrofauna_abundance_and_biomass_at_the_LTER_observatory_HAUSGARTEN_in_2016_supplement_to_K%C3%A4%C3%9F_Melissa_Vedenin_Andrey_Hasemann_Christiane_Brandt_Angelika_Soltwedel_Thomas_2019_Community_structure_of_macrofauna_in_the_deep_Fram_Strait_A_comparison_between_two_bathymetric_gradients_in_"><img alt="Research paper thumbnail of Macrofauna abundance and biomass at the LTER observatory HAUSGARTEN in 2016, supplement to: Käß, Melissa; Vedenin, Andrey; Hasemann, Christiane; Brandt, Angelika; Soltwedel, Thomas (2019): Community structure of macrofauna in the deep Fram Strait: A comparison between two bathymetric gradients in..." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647046/Macrofauna_abundance_and_biomass_at_the_LTER_observatory_HAUSGARTEN_in_2016_supplement_to_K%C3%A4%C3%9F_Melissa_Vedenin_Andrey_Hasemann_Christiane_Brandt_Angelika_Soltwedel_Thomas_2019_Community_structure_of_macrofauna_in_the_deep_Fram_Strait_A_comparison_between_two_bathymetric_gradients_in_">Macrofauna abundance and biomass at the LTER observatory HAUSGARTEN in 2016, supplement to: Käß, Melissa; Vedenin, Andrey; Hasemann, Christiane; Brandt, Angelika; Soltwedel, Thomas (2019): Community structure of macrofauna in the deep Fram Strait: A comparison between two bathymetric gradients in...</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Macrofauna data was collected using a box corer (0.25m² sampling area). The sampled sediment from...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Macrofauna data was collected using a box corer (0.25m² sampling area). The sampled sediment from each box corer was divided into eight subsamples (pseudoreplicates). The uppermost 12 cm of these subsamples were analyzed. Each subsample was processed through a 500-µm mesh size sieve. After sieving, residuals were fixed with 100% ethanol and stored at room temperature. Macrofaunal organisms were identified to the lowest possible taxonomical level. Whenever identification to species level was not possible, the sample was identified to the next identifiable taxonomical category and assigned a putative species name (e.g., &#39;Hesionidae genus sp. 1&#39;, &#39;Hesionidae genus sp. 2&#39;). Posterior fragments, exuviae, xenobionts, meiofauna taxa (Nematoda, Ostracoda, Harpacticoida) and empty tubes were excluded from the analysis. Biomass (blotted wet weight, ww) was determined by weighing each specimen. Shelled organisms, such as mollusks, were weight in their shells.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647046"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647046"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647046; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647046]").text(description); $(".js-view-count[data-work-id=127647046]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647046; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647046']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647044"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647044/_Table_I_II_Station_details_and_isopoda_abundance_of_samples_taken_during_POLARSTERN_cruise_ANT_XV_3_to_the_eastern_Weddell_Sea_and_King_George_Island_supplement_to_Brandt_Angelika_2004_Abundance_diversity_and_community_patterns_of_Isopoda_Crustacea_in_the_Weddell_Sea_and_in_the_Bransf_"><img alt="Research paper thumbnail of (Table I-II) Station details and isopoda abundance of samples taken during POLARSTERN cruise ANT-XV/3 to the eastern Weddell Sea and King George Island, supplement to: Brandt, Angelika (2004): Abundance, diversity, and community patterns of Isopoda (Crustacea) in the Weddell Sea and in the Bransf..." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647044/_Table_I_II_Station_details_and_isopoda_abundance_of_samples_taken_during_POLARSTERN_cruise_ANT_XV_3_to_the_eastern_Weddell_Sea_and_King_George_Island_supplement_to_Brandt_Angelika_2004_Abundance_diversity_and_community_patterns_of_Isopoda_Crustacea_in_the_Weddell_Sea_and_in_the_Bransf_">(Table I-II) Station details and isopoda abundance of samples taken during POLARSTERN cruise ANT-XV/3 to the eastern Weddell Sea and King George Island, supplement to: Brandt, Angelika (2004): Abundance, diversity, and community patterns of Isopoda (Crustacea) in the Weddell Sea and in the Bransf...</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abundance, diversity, and distribution of suprabenthic Isopoda caught from a water layer between ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Abundance, diversity, and distribution of suprabenthic Isopoda caught from a water layer between 0.27 to 0.60 m above the seafloor were analysed. The samples were taken during the ANT XV/3 cruise on RV Polarstern by means of an epibenthic sledge along two transects in the southern Weddell Sea (Vestkapp and Halley Bay) and another one east of King George Island. At each of these three bathymetric transects, five to six stations were sampled between 200 and 2000 m. In total, 4258 specimens of isopods were sampled at 14 stations standardized to 1000 m2 hauls. 114 species were identified from 49 genera and 23 higher taxa (families and suborders) of Isopoda. Most of them belonged to the suborder Asellota. Dominant families are Munnopsididae (Eurycopinae, Ilyarachninae), Joeropsidae, Munnidae, Paramunnidae, Ischnomesidae and Desmosomatidae. No striking differences were found between areas (Vestkapp, Halley Bay, Kapp Norvegia, and Bransfield Strait). Overall isopod abundances were highest ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647044"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647044"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647044; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647044]").text(description); $(".js-view-count[data-work-id=127647044]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647044; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647044']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=127647044]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":127647044,"title":"(Table I-II) Station details and isopoda abundance of samples taken during POLARSTERN cruise ANT-XV/3 to the eastern Weddell Sea and King George Island, supplement to: Brandt, Angelika (2004): Abundance, diversity, and community patterns of Isopoda (Crustacea) in the Weddell Sea and in the Bransf...","internal_url":"https://www.academia.edu/127647044/_Table_I_II_Station_details_and_isopoda_abundance_of_samples_taken_during_POLARSTERN_cruise_ANT_XV_3_to_the_eastern_Weddell_Sea_and_King_George_Island_supplement_to_Brandt_Angelika_2004_Abundance_diversity_and_community_patterns_of_Isopoda_Crustacea_in_the_Weddell_Sea_and_in_the_Bransf_","owner_id":226089093,"coauthors_can_edit":true,"owner":{"id":226089093,"first_name":"Angelika","middle_initials":null,"last_name":"Brandt","page_name":"BrandtAngelika","domain_name":"independent","created_at":"2022-06-09T03:39:28.948-07:00","display_name":"Angelika Brandt","url":"https://independent.academia.edu/BrandtAngelika"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647042"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647042/Sea_ice_meiofauna_10_%CE%BCm_abundance_in_Arctic_pack_ice_north_of_Svalbard_during_the_Polarstern_expedition_PS92_in_2015"><img alt="Research paper thumbnail of Sea-ice meiofauna (>10 µm) abundance in Arctic pack ice north of Svalbard during the Polarstern expedition PS92 in 2015" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647042/Sea_ice_meiofauna_10_%CE%BCm_abundance_in_Arctic_pack_ice_north_of_Svalbard_during_the_Polarstern_expedition_PS92_in_2015">Sea-ice meiofauna (>10 µm) abundance in Arctic pack ice north of Svalbard during the Polarstern expedition PS92 in 2015</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">We investigated the taxonomic composition and abundance of sea-ice meiofauna (here heterotrophs &...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">We investigated the taxonomic composition and abundance of sea-ice meiofauna (here heterotrophs &gt;10 µm) at eight ice stations on Arctic pack ice north of Svalbard. Sampling was conducted during spring in 2015 by sea-ice coring. The bottom 10 cm of each ice core was investigated for sea-ice meiofauna and abundances of individuals/m² were calculated from counting numbers.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647042"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647042"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647042; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647042]").text(description); $(".js-view-count[data-work-id=127647042]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647042; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647042']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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</script> <div class="js-work-strip profile--work_container" data-work-id="127647038"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647038/Proportion_of_bryozoa_isopoda_and_ostracoda_and_bryozoan_species_richness_on_the_Antarctic_continental_shelf_slope_and_abyss"><img alt="Research paper thumbnail of Proportion of bryozoa, isopoda and ostracoda, and bryozoan species richness on the Antarctic continental shelf, slope and abyss" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647038/Proportion_of_bryozoa_isopoda_and_ostracoda_and_bryozoan_species_richness_on_the_Antarctic_continental_shelf_slope_and_abyss">Proportion of bryozoa, isopoda and ostracoda, and bryozoan species richness on the Antarctic continental shelf, slope and abyss</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Antarctic continental slope spans the depths from the shelf break (usually between 500 and 10...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Antarctic continental slope spans the depths from the shelf break (usually between 500 and 1000 m) to ~3000 m, is very steep, overlain by &#39;warm&#39; (2-2.5 °C) Circumpolar Deep Water (CDW), and life there is poorly studied. This study investigates whether life on Antarctica&#39;s continental slope is essentially an extension of the shelf or the abyssal fauna, a transition zone between these or clearly distinct in its own right. Using data from several cruises to the Weddell Sea and Scotia Sea, including the ANDEEP (ANtarctic benthic DEEP-sea biodiversity, colonisation history and recent community patterns) I-III, BIOPEARL (Biodiversity, Phylogeny, Evolution and Adaptive Radiation of Life in Antarctica) 1 and EASIZ (Ecology of the Antarctic Sea Ice Zone) II cruises as well as current databases (SOMBASE, SCAR-MarBIN), four different taxa were selected (i.e. cheilostome bryozoans, isopod and ostracod crustaceans and echinoid echinoderms) and two areas, the Weddell Sea and the Scotia Sea, to examine faunal composition, richness and affinities. The answer has important ramifications to the link between physical oceanography and ecology, and the potential of the slope to act as a refuge and resupply zone to the shelf during glaciations. Benthic samples were collected using Agassiz trawl, epibenthic sledge and Rauschert sled. By bathymetric definition, these data suggest that despite eurybathy in some of the groups examined and apparent similarity of physical conditions in the Antarctic, the shelf, slope and abyssal faunas were clearly separated in the Weddell Sea. However, no such separation of faunas was apparent in the Scotia Sea (except in echinoids). Using a geomorphological definition of the slope, shelf-slope-abyss similarity only changed significantly in the bryozoans. Our results did not support the presence of a homogenous and unique Antarctic slope fauna despite a high number of species being restricted to the slope. However, it remains the case that there may be a unique Antarctic slope fauna, but the paucity of [...]</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647038"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647038"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647038; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647038]").text(description); 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window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647036]").text(description); $(".js-view-count[data-work-id=127647036]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647036; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647036']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=127647036]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":127647036,"title":"(Table 2) Phytoplankton composition of the surface layer of Station PS71/039 on Maud Rise","internal_url":"https://www.academia.edu/127647036/_Table_2_Phytoplankton_composition_of_the_surface_layer_of_Station_PS71_039_on_Maud_Rise","owner_id":226089093,"coauthors_can_edit":true,"owner":{"id":226089093,"first_name":"Angelika","middle_initials":null,"last_name":"Brandt","page_name":"BrandtAngelika","domain_name":"independent","created_at":"2022-06-09T03:39:28.948-07:00","display_name":"Angelika Brandt","url":"https://independent.academia.edu/BrandtAngelika"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647034"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647034/First_insights_into_the_solenogaster_diversity_of_the_Sea_of_Okhotsk_with_the_description_of_a_new_species_of_Kruppomenia_Simrothiellidae_Cavibelonia_"><img alt="Research paper thumbnail of First insights into the solenogaster diversity of the Sea of Okhotsk with the description of a new species of Kruppomenia (Simrothiellidae, Cavibelonia)" class="work-thumbnail" src="https://attachments.academia-assets.com/121350434/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647034/First_insights_into_the_solenogaster_diversity_of_the_Sea_of_Okhotsk_with_the_description_of_a_new_species_of_Kruppomenia_Simrothiellidae_Cavibelonia_">First insights into the solenogaster diversity of the Sea of Okhotsk with the description of a new species of Kruppomenia (Simrothiellidae, Cavibelonia)</a></div><div class="wp-workCard_item"><span>Deep Sea Research Part II: Topical Studies in Oceanography</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Solenogastres form a small clade of worm-shaped molluscs distributed world-wide with most of the ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Solenogastres form a small clade of worm-shaped molluscs distributed world-wide with most of the approx. 300 species occurring in the deep sea. A recent diversity study from the abyssal plain in the Northwest Pacific has revealed a wealth of new abyssal solenogaster lineages highlighting the need for further alpha-taxonomic work. During the 'Sea of Okhotsk Biodiversity Studies' (SokhoBio) expedition, 93 specimens were collected at overall eight stations ranging from depths of 1696 m to 3377 m. Preliminary investigations revealed twelve clearly distinguishable morphospecies, including one relatively common species present at six of eleven stations. All morphospecies are characterized externally via light microscopy and identified to the best possible taxonomic level via scleritome characters. Molecular barcodes (16S rRNA) are provided as a first step towards establishment of a barcoding library to enable fast and accurate re-identification of these taxonomically challenging molluscs in future studies. The most wide-spread and abundant cavibelonian Solenogastres Kruppomenia genslerae sp. nov. (Simrothiellidae) is exemplarily described in full microanatomical detail based on 3D-reconstructions from histological semithin section series and scanning electron microscopy. We discuss our results in comparison to the solenogaster diversity of the neighbouring abyssal plain of the Northwest Pacific, which is connected with the Kuril Basin via two straits. Our initial characterization of the diversity boosts the hitherto poorly known diversity of Solenogastres in the Far Eastern Seas, but also underlines the taxonomic impediment for proper taxonomic descriptions of the wealth of new discovered material.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ddc685747da4cbb7ac02618b7502520f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350434,"asset_id":127647034,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350434/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647034"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647034"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647034; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647032"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647032/Peracarid_crustacean_assemblages_of_the_Kolbeinsey_Ridge_north_of_Iceland"><img alt="Research paper thumbnail of Peracarid crustacean assemblages of the Kolbeinsey Ridge, north of Iceland" class="work-thumbnail" src="https://attachments.academia-assets.com/121350431/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647032/Peracarid_crustacean_assemblages_of_the_Kolbeinsey_Ridge_north_of_Iceland">Peracarid crustacean assemblages of the Kolbeinsey Ridge, north of Iceland</a></div><div class="wp-workCard_item"><span>Polar Biology</span><span>, 1994</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">On the Kolbeinsey Ridge, north of Iceland, 92 species of peracarid crustaceans were sampled using...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">On the Kolbeinsey Ridge, north of Iceland, 92 species of peracarid crustaceans were sampled using the epibenthic sledge. For an analysis of the multispecies distribution pattern across the ridge, a total of 46 species have been considered, which occurred at least at two stations and with at least 5% relative abundance at any one station. The analysis revealed four assemblages: a deep species assemblage, an eastern slope assemblage, an ubiquitous species assemblage and a western slope assemblage. The western slope assemblage consists mainly of Amphipoda, which were most abundant and diverse on the western slope. The ubiquitous and eastern slope assemblages, however, are dominated by Isopoda, which also comprised most species and individuals on the eastern slope. Cumaceans were the most representative species of the deep species assemblage. These differences in species composition and abundance can probably be attributed to food supply and sediment composition, rather than to salinity or bottom water temperature.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="fa60a1bf5382894a493d4cf932b42823" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350431,"asset_id":127647032,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350431/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647032"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647032"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647032; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647029"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647029/Seasonal_occurrence_of_planktic_Crustacea_in_sediment_trap_samples_at_three_depth_horizons_in_the_Greenland_Sea"><img alt="Research paper thumbnail of Seasonal occurrence of planktic Crustacea in sediment trap samples at three depth horizons in the Greenland Sea" class="work-thumbnail" src="https://attachments.academia-assets.com/121350428/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647029/Seasonal_occurrence_of_planktic_Crustacea_in_sediment_trap_samples_at_three_depth_horizons_in_the_Greenland_Sea">Seasonal occurrence of planktic Crustacea in sediment trap samples at three depth horizons in the Greenland Sea</a></div><div class="wp-workCard_item"><span>Polar Biology</span><span>, 1997</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Zooplankton were quantitatively investigated in sediment trap samples deployed in the Greenland S...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Zooplankton were quantitatively investigated in sediment trap samples deployed in the Greenland Sea at three locations (72°00.7N, 7°02.5W, 72°23.0N, 7°42.7W and 72°22.9N, 7°42.7W). Overall samples covered a period of three annual cycles (July 1989 to July 1992). The investigation of zooplankton, consisting almost exclusively of Crustacea ('99%), shows that the majority of the species must be regarded as ''swimmers'', which actively invaded the traps. Crustacea were composed of 45 species, mainly Copepoda, Amphipoda and Ostracoda. Each depth level showed a characteristic species composition. Diversity decreased with depth. The samples were dominated by Copepoda in terms of abundance and by Amphipoda with respect to biomass. The seasonal occurrence of Crustacea showed a maximum during winter and a minimum during summer. Carnivores were regularly found in the collected material, indicating that they had been actively attracted by the organic matter emanating from the traps. Omnivores showed a distinct seasonal occurrence. During winter, when primary production is low, omnivores change to a predatory way of life and they were consequently also found in increasing numbers. Herbivores were always rare. Due to the high number of ''swimmers'' found in winter, when particle flux is at its minimum, particle flux measurements may be severely biased at this time of the year.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ca653da057ee9c062b3238f4b8b6d1a1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350428,"asset_id":127647029,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350428/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647029"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647029"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647029; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647029]").text(description); $(".js-view-count[data-work-id=127647029]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647029; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647029']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="15373089" id="papers"><div class="js-work-strip profile--work_container" data-work-id="127647060"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647060/Approaching_the_diversity_and_density_dilemma_of_the_lebensspuren_tracemaker_tandem_a_study_case_from_abyssal_Northwest_Pacific"><img alt="Research paper thumbnail of Approaching the diversity and density dilemma of the lebensspuren-tracemaker tandem: a study case from abyssal Northwest Pacific" class="work-thumbnail" src="https://attachments.academia-assets.com/121350427/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647060/Approaching_the_diversity_and_density_dilemma_of_the_lebensspuren_tracemaker_tandem_a_study_case_from_abyssal_Northwest_Pacific">Approaching the diversity and density dilemma of the lebensspuren-tracemaker tandem: a study case from abyssal Northwest Pacific</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the deep-sea, the interaction between benthic fauna and substrate mainly occurs through biotur...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the deep-sea, the interaction between benthic fauna and substrate mainly occurs through bioturbational processes which can be preserved as traces (i.e., lebensspuren). Lebensspuren are common features of deep seafloor landscapes and usually more abundant than the organism that produce them (i.e., tracemakers), rendering them promising proxies to infer biodiversity. The density and diversity relationships between lebensspuren and benthic fauna are to the present day unclear and contradicting hypotheses have been proposed suggesting negative, positive, or even null correlations. To test these hypotheses, in this study lebensspuren, tracemakers (specific epibenthic fauna that produce these traces), degrading fauna (benthic fauna that can erase lebensspuren), and fauna in general were characterized taxonomically at eight deep-sea stations in the Kuril Kamchatka Trench area. No general correlation (over-all study area) could be observed between diversities of lebensspuren, tracemakers, degrading fauna and fauna. However, a diversity correlation was observed between specific stations, showing both negative and positive correlations depending on: 1) the number of unknown</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a647de549c449e0d1878e4b4b5c2e9fe" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350427,"asset_id":127647060,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350427/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647060"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647060"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647060; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647060]").text(description); $(".js-view-count[data-work-id=127647060]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647060; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647060']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "a647de549c449e0d1878e4b4b5c2e9fe" } } $('.js-work-strip[data-work-id=127647060]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":127647060,"title":"Approaching the diversity and density dilemma of the lebensspuren-tracemaker tandem: a study case from abyssal Northwest Pacific","internal_url":"https://www.academia.edu/127647060/Approaching_the_diversity_and_density_dilemma_of_the_lebensspuren_tracemaker_tandem_a_study_case_from_abyssal_Northwest_Pacific","owner_id":226089093,"coauthors_can_edit":true,"owner":{"id":226089093,"first_name":"Angelika","middle_initials":null,"last_name":"Brandt","page_name":"BrandtAngelika","domain_name":"independent","created_at":"2022-06-09T03:39:28.948-07:00","display_name":"Angelika Brandt","url":"https://independent.academia.edu/BrandtAngelika"},"attachments":[{"id":121350427,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/121350427/thumbnails/1.jpg","file_name":"bg-2023-81.pdf","download_url":"https://www.academia.edu/attachments/121350427/download_file","bulk_download_file_name":"Approaching_the_diversity_and_density_di.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/121350427/bg-2023-81-libre.pdf?1739539672=\u0026response-content-disposition=attachment%3B+filename%3DApproaching_the_diversity_and_density_di.pdf\u0026Expires=1740021786\u0026Signature=f6wapMf4hMNJJXZh9wNzgybvrw7Gr0ovoz3B8Eys3ts3bUi9RVaY6~WIl1oF3KOpfKJmAOxMT7SVzTHMfS4yeYNN2bA7N71X9SdvBB~ZG0JcWseX-equXVjvKg7WnQW~Cmp26D69OdZL~nbTwljbeVT4A2kZoDF7t-AzauDmOk1-mgby4sywQLc3Pd-uzfUJoZgbEcGrrJKE5PgZa7zu~ICag-Vki4gl2VSGMtVK2kPnU4MZ4Vmi6o0nlYlSfPkXAJ~EoCk81Bj45v~Go4A5iQ3mv5TaWSoq5FJ2T2jEDXb~zggEP8tLjmVpkliIB~N3dWKFdeZMKqdmQSn3M2ZxDg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647059"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647059/Peracarid_fauna_Crustacea_Malacostraca_of_the_Northeast_Water_Polynya_off_Greenland_documenting_close_benthic_pelagic_coupling_in_the_Westwind_Trough"><img alt="Research paper thumbnail of Peracarid fauna (Crustacea, Malacostraca) of the Northeast Water Polynya off Greenland:documenting close benthic-pelagic coupling in the Westwind Trough" class="work-thumbnail" src="https://attachments.academia-assets.com/121350424/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647059/Peracarid_fauna_Crustacea_Malacostraca_of_the_Northeast_Water_Polynya_off_Greenland_documenting_close_benthic_pelagic_coupling_in_the_Westwind_Trough">Peracarid fauna (Crustacea, Malacostraca) of the Northeast Water Polynya off Greenland:documenting close benthic-pelagic coupling in the Westwind Trough</a></div><div class="wp-workCard_item"><span>Marine Ecology Progress Series</span><span>, 1995</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Composition, abundance, and diversity of peracarids (Crustacea) were investigated over a period o...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Composition, abundance, and diversity of peracarids (Crustacea) were investigated over a period of 3 mo in the Northeast Water Polynya (NEW), off Greenland. Samples were collected from May to July 1993 during expeditions ARK IX/2 and 3 using an epibenthic sledge on RV 'Polarstern' Within the macrobenthic community peracarids were an important component of the shelf fauna and occurred in high abundance in this area together with polychaetes, molluscs and brittle stars. A total of 38322 specimens were sampled from 22 stations. Cumacea attained the highest total abundance and Amphipoda the highest d~versity. Isopoda were of medium abundance, Mysidacea less abundant, and Tanaidacea least abundant. In total 229 species were found. Differences in composition, abundance and diversity do not reflect bathymetric gradients, but mainly the availability of food (phytoplankton and especially ice algae) and, hence, the temporal and spatial opening of the polynya. Thus primary production and hydrographic condit~ons (lateral advection due to the ant~cyclonic gyre around Belgica Bank) are the main biological and physical parameters influencing the peracarid crustacean community, documenting a close coupling between primary production and the benthic community in the eastern Westwind Trough. The high abundance of Peracarida, which are also capable of burrowing in the upper sediment layers, indicates their importance for benthic carbon cycling.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="79b44a60fbad0fd1be5d98dba0d9c6b1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350424,"asset_id":127647059,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350424/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647059"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647059"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647059; 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Several strategic groups (SGs) have been established under the KDM umbrella to address overarching marine scientific topics with a high societal relevance, including observing systems, coastal and climate research, biodiversity, and marine biological as well as mineral resources.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bce6845c3deae54438b125dcda18ca22" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350422,"asset_id":127647058,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350422/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647058"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647058"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647058; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647056"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647056/A_new_species_of_Cirolana_Leach_1818_Crustacea_Isopoda_Cirolanidae_from_the_western_Ross_Sea_Antarctica_the_first_record_of_the_genus_from_polar_waters"><img alt="Research paper thumbnail of A new species of Cirolana Leach, 1818 (Crustacea, Isopoda, Cirolanidae) from the western Ross Sea, Antarctica, the first record of the genus from polar waters" class="work-thumbnail" src="https://attachments.academia-assets.com/121350420/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647056/A_new_species_of_Cirolana_Leach_1818_Crustacea_Isopoda_Cirolanidae_from_the_western_Ross_Sea_Antarctica_the_first_record_of_the_genus_from_polar_waters">A new species of Cirolana Leach, 1818 (Crustacea, Isopoda, Cirolanidae) from the western Ross Sea, Antarctica, the first record of the genus from polar waters</a></div><div class="wp-workCard_item"><span>Zenodo (CERN European Organization for Nuclear Research)</span><span>, Dec 31, 2006</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cirolana mclaughlinae n. sp. is described from specimens collected in the Ross Sea, Antarctica. T...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Cirolana mclaughlinae n. sp. is described from specimens collected in the Ross Sea, Antarctica. Th e species is characterised by the head having a prominent anterior marginal ridge, lacking a rostrum, and being dorsally depressed; the posterior submarginal surfaces of pereonites 5-7 and the pleonites are nodulose and pitted; the pleotelson has weakly concave lateral margins converging to a narrowly rounded apex, the dorsal surface is provided with a low, longitudinal median ridge. Th e genus has a world-wide distribution, but has hitherto not been recorded from polar waters, the previous most southerly record being at about 44°S. Une nouvelle espèce de Cirolana Leach, 1818 (Crustacea, Isopoda, Cirolanidae) provenant de la mer de Ross occidentale dans l'Antarctique, première récolte du genre dans les eaux polaires. Cirolana mclaughlinae n. sp. est décrite d'après des spécimens récoltés dans l'Antarctique, en mer de Ross. L'espèce se caractérise par la tête dépourvue de ZOOSYSTEMA • 2006 • 28 (2)</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b5cd8a83c7a9d27dd549b59a24247f81" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350420,"asset_id":127647056,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350420/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647056"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647056"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647056; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647054"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647054/Climate_change_and_fisheries_affect_benthic_composition_and_diversity_in_the_North_Sea_Investigations_at_the_Dogger_Bank_during_three_decades_1991_2021_"><img alt="Research paper thumbnail of Climate change and fisheries affect benthic composition and diversity in the North Sea - Investigations at the Dogger Bank during three decades (1991-2021)" class="work-thumbnail" src="https://attachments.academia-assets.com/121350417/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647054/Climate_change_and_fisheries_affect_benthic_composition_and_diversity_in_the_North_Sea_Investigations_at_the_Dogger_Bank_during_three_decades_1991_2021_">Climate change and fisheries affect benthic composition and diversity in the North Sea - Investigations at the Dogger Bank during three decades (1991-2021)</a></div><div class="wp-workCard_item"><span>Research Square (Research Square)</span><span>, Jul 27, 2023</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Over a period of 30 years benthic fauna was monitored at a long-term sampling station at the NATU...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Over a period of 30 years benthic fauna was monitored at a long-term sampling station at the NATURA2000 marine protected area Dogger Bank and at a reference station in Dutch waters, using a ring dredge and a 2 m beam trawl. Changes of benthic diversity of 127 species were detected in 238 temporally distributed samples and correlated with temperature and intensity of bottom shing. Our results provide a solid benchmark for future research in the German Exclusive Economic Zone. During the timeframe of our study, the temperature at depths below 30 m remarkably increased by 4°C, while shing pressure in the studied ICES rectangles decreased over the past 30 years from over 100.000 h of trawling per year to about 20.000 h. The numbers of benthic individuals sampled each year show a negative trend, while the number from 1991 to 2001 is rst more in uenced by shing, later by temperature. An analysis of the benthic fauna at some stations adjacent to the long-term sampled station, sampled in 2021, showed that species composition is comparatively uniform over space and that therefore long-term sampling of one station can be used as a proxy for its surroundings in this area.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0b48e16ebbff11f67238de853a74645c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350417,"asset_id":127647054,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350417/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647054"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647054"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647054; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647053"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647053/Abundance_of_benthic_peracarids_sampled_in_the_Atlantic_Sector_of_the_Southern_Ocean_and_Weddell_Sea_during_expeditions_JR15005_JR275_JR17003a_PS118"><img alt="Research paper thumbnail of Abundance of benthic peracarids sampled in the Atlantic Sector of the Southern Ocean and Weddell Sea during expeditions JR15005, JR275, JR17003a, PS118" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647053/Abundance_of_benthic_peracarids_sampled_in_the_Atlantic_Sector_of_the_Southern_Ocean_and_Weddell_Sea_during_expeditions_JR15005_JR275_JR17003a_PS118">Abundance of benthic peracarids sampled in the Atlantic Sector of the Southern Ocean and Weddell Sea during expeditions JR15005, JR275, JR17003a, PS118</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Peracarid abundance and composition were studied in the Atlantic Sector of the Southern Ocean and...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Peracarid abundance and composition were studied in the Atlantic Sector of the Southern Ocean and the Weddell Sea at a depth range of 403-2021 m. Samples were collected using an epibenthic sledge (EBS) during expeditions on board the RRS James Clarke Ross in the Filchner Trough (JR275), the South Orkney Islands (JR15005), the Prince Gustav Channel (JR17003a) and on board the RV Polarstern in the Eastern Antarctic Peninsula (PS118). Expeditions took place in February-March 2012, 2016, 2018 and 2019 respectively. Since the trawling distance between stations was not always the same, in order to make data comparable between different stations, numbers of individuals were standardized to 1000 m haul distances.In total 64766 peracarids were found and sorted into five different orders (Amphipoda, Cumacea, Isopoda, Mysidacea and Tanaidacea). Amphipods were the most abundant group representing the 32% of the total abundances. The Filchner Trough had the highest abundance of peracarids, while...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647053"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647053"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647053; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647053]").text(description); $(".js-view-count[data-work-id=127647053]").attr('title', description).tooltip(); 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} }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647052"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647052/Zooplankton_sampled_under_ice_during_POLARSTERN_cruise_PS81_ANT_XXIX_7_"><img alt="Research paper thumbnail of Zooplankton sampled under-ice during POLARSTERN cruise PS81 (ANT-XXIX/7)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647052/Zooplankton_sampled_under_ice_during_POLARSTERN_cruise_PS81_ANT_XXIX_7_">Zooplankton sampled under-ice during POLARSTERN cruise PS81 (ANT-XXIX/7)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647052"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647052"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647052; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647052]").text(description); $(".js-view-count[data-work-id=127647052]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647052; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647052']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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Peters, Janna; Flores, Hauke; Brandt, Angelika (2011): Demersal fishes from the Antarctic shelf and deep sea: A diet study based on fatty acid ..." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647051/Gut_filling_gut_content_and_fatty_acid_composition_of_demersal_fish_species_sampled_during_POLARSTERN_cruise_ANT_XXIV_2_supplement_to_W%C3%BCrzberg_Laura_Peters_Janna_Flores_Hauke_Brandt_Angelika_2011_Demersal_fishes_from_the_Antarctic_shelf_and_deep_sea_A_diet_study_based_on_fatty_acid_">Gut filling, gut content and fatty acid composition of demersal fish species sampled during POLARSTERN cruise ANT-XXIV/2, supplement to: Würzberg, Laura; Peters, Janna; Flores, Hauke; Brandt, Angelika (2011): Demersal fishes from the Antarctic shelf and deep sea: A diet study based on fatty acid ...</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The gut contents and fatty acid composition of 49 fish belonging to five Antarctic demersal famil...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The gut contents and fatty acid composition of 49 fish belonging to five Antarctic demersal families (Nototheniidae, Macrouridae, Channichtyidae, Bathydraconidae and Artedidraconidae) sampled at two stations at the Southern Ocean shelf and deep sea (600 and 2150 m) were analysed in order to identify their main food resource by linking trophic biomarkers with the dietary items found in the fish guts. Main food items of most fish analysed were amphipod crustaceans (e.g. in 63% of Trematomus bernachii guts) and polychaetes (e.g. in 80% of Bathydraco sp. guts), but other food items including fish, other crustaceans and gastropods were also ingested. The most prominent fatty acids found were 20:5(n-3), 16:0, 22:6(n-3) and 18:1(n-9). The results of gut content and fatty acid analyses indicate that all fish except the Channichthyidae share similar food resources irrespective of their depth distribution, i.e. benthic amphipods and polychaetes. A difference of the dietary spectrum can be obs...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647051"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647051"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647051; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647051]").text(description); $(".js-view-count[data-work-id=127647051]").attr('title', description).tooltip(); 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</script> <div class="js-work-strip profile--work_container" data-work-id="127647046"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647046/Macrofauna_abundance_and_biomass_at_the_LTER_observatory_HAUSGARTEN_in_2016_supplement_to_K%C3%A4%C3%9F_Melissa_Vedenin_Andrey_Hasemann_Christiane_Brandt_Angelika_Soltwedel_Thomas_2019_Community_structure_of_macrofauna_in_the_deep_Fram_Strait_A_comparison_between_two_bathymetric_gradients_in_"><img alt="Research paper thumbnail of Macrofauna abundance and biomass at the LTER observatory HAUSGARTEN in 2016, supplement to: Käß, Melissa; Vedenin, Andrey; Hasemann, Christiane; Brandt, Angelika; Soltwedel, Thomas (2019): Community structure of macrofauna in the deep Fram Strait: A comparison between two bathymetric gradients in..." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647046/Macrofauna_abundance_and_biomass_at_the_LTER_observatory_HAUSGARTEN_in_2016_supplement_to_K%C3%A4%C3%9F_Melissa_Vedenin_Andrey_Hasemann_Christiane_Brandt_Angelika_Soltwedel_Thomas_2019_Community_structure_of_macrofauna_in_the_deep_Fram_Strait_A_comparison_between_two_bathymetric_gradients_in_">Macrofauna abundance and biomass at the LTER observatory HAUSGARTEN in 2016, supplement to: Käß, Melissa; Vedenin, Andrey; Hasemann, Christiane; Brandt, Angelika; Soltwedel, Thomas (2019): Community structure of macrofauna in the deep Fram Strait: A comparison between two bathymetric gradients in...</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Macrofauna data was collected using a box corer (0.25m² sampling area). The sampled sediment from...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Macrofauna data was collected using a box corer (0.25m² sampling area). The sampled sediment from each box corer was divided into eight subsamples (pseudoreplicates). The uppermost 12 cm of these subsamples were analyzed. Each subsample was processed through a 500-µm mesh size sieve. After sieving, residuals were fixed with 100% ethanol and stored at room temperature. Macrofaunal organisms were identified to the lowest possible taxonomical level. Whenever identification to species level was not possible, the sample was identified to the next identifiable taxonomical category and assigned a putative species name (e.g., &#39;Hesionidae genus sp. 1&#39;, &#39;Hesionidae genus sp. 2&#39;). Posterior fragments, exuviae, xenobionts, meiofauna taxa (Nematoda, Ostracoda, Harpacticoida) and empty tubes were excluded from the analysis. Biomass (blotted wet weight, ww) was determined by weighing each specimen. Shelled organisms, such as mollusks, were weight in their shells.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647046"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647046"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647046; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647046]").text(description); $(".js-view-count[data-work-id=127647046]").attr('title', description).tooltip(); 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647044"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647044/_Table_I_II_Station_details_and_isopoda_abundance_of_samples_taken_during_POLARSTERN_cruise_ANT_XV_3_to_the_eastern_Weddell_Sea_and_King_George_Island_supplement_to_Brandt_Angelika_2004_Abundance_diversity_and_community_patterns_of_Isopoda_Crustacea_in_the_Weddell_Sea_and_in_the_Bransf_"><img alt="Research paper thumbnail of (Table I-II) Station details and isopoda abundance of samples taken during POLARSTERN cruise ANT-XV/3 to the eastern Weddell Sea and King George Island, supplement to: Brandt, Angelika (2004): Abundance, diversity, and community patterns of Isopoda (Crustacea) in the Weddell Sea and in the Bransf..." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647044/_Table_I_II_Station_details_and_isopoda_abundance_of_samples_taken_during_POLARSTERN_cruise_ANT_XV_3_to_the_eastern_Weddell_Sea_and_King_George_Island_supplement_to_Brandt_Angelika_2004_Abundance_diversity_and_community_patterns_of_Isopoda_Crustacea_in_the_Weddell_Sea_and_in_the_Bransf_">(Table I-II) Station details and isopoda abundance of samples taken during POLARSTERN cruise ANT-XV/3 to the eastern Weddell Sea and King George Island, supplement to: Brandt, Angelika (2004): Abundance, diversity, and community patterns of Isopoda (Crustacea) in the Weddell Sea and in the Bransf...</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abundance, diversity, and distribution of suprabenthic Isopoda caught from a water layer between ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Abundance, diversity, and distribution of suprabenthic Isopoda caught from a water layer between 0.27 to 0.60 m above the seafloor were analysed. The samples were taken during the ANT XV/3 cruise on RV Polarstern by means of an epibenthic sledge along two transects in the southern Weddell Sea (Vestkapp and Halley Bay) and another one east of King George Island. At each of these three bathymetric transects, five to six stations were sampled between 200 and 2000 m. In total, 4258 specimens of isopods were sampled at 14 stations standardized to 1000 m2 hauls. 114 species were identified from 49 genera and 23 higher taxa (families and suborders) of Isopoda. Most of them belonged to the suborder Asellota. Dominant families are Munnopsididae (Eurycopinae, Ilyarachninae), Joeropsidae, Munnidae, Paramunnidae, Ischnomesidae and Desmosomatidae. No striking differences were found between areas (Vestkapp, Halley Bay, Kapp Norvegia, and Bransfield Strait). Overall isopod abundances were highest ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647044"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647044"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647044; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647044]").text(description); $(".js-view-count[data-work-id=127647044]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647044; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647044']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647042"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647042/Sea_ice_meiofauna_10_%CE%BCm_abundance_in_Arctic_pack_ice_north_of_Svalbard_during_the_Polarstern_expedition_PS92_in_2015"><img alt="Research paper thumbnail of Sea-ice meiofauna (>10 µm) abundance in Arctic pack ice north of Svalbard during the Polarstern expedition PS92 in 2015" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647042/Sea_ice_meiofauna_10_%CE%BCm_abundance_in_Arctic_pack_ice_north_of_Svalbard_during_the_Polarstern_expedition_PS92_in_2015">Sea-ice meiofauna (>10 µm) abundance in Arctic pack ice north of Svalbard during the Polarstern expedition PS92 in 2015</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">We investigated the taxonomic composition and abundance of sea-ice meiofauna (here heterotrophs &...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">We investigated the taxonomic composition and abundance of sea-ice meiofauna (here heterotrophs &gt;10 µm) at eight ice stations on Arctic pack ice north of Svalbard. Sampling was conducted during spring in 2015 by sea-ice coring. The bottom 10 cm of each ice core was investigated for sea-ice meiofauna and abundances of individuals/m² were calculated from counting numbers.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647042"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647042"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647042; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647042]").text(description); $(".js-view-count[data-work-id=127647042]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 127647042; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='127647042']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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</script> <div class="js-work-strip profile--work_container" data-work-id="127647038"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/127647038/Proportion_of_bryozoa_isopoda_and_ostracoda_and_bryozoan_species_richness_on_the_Antarctic_continental_shelf_slope_and_abyss"><img alt="Research paper thumbnail of Proportion of bryozoa, isopoda and ostracoda, and bryozoan species richness on the Antarctic continental shelf, slope and abyss" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/127647038/Proportion_of_bryozoa_isopoda_and_ostracoda_and_bryozoan_species_richness_on_the_Antarctic_continental_shelf_slope_and_abyss">Proportion of bryozoa, isopoda and ostracoda, and bryozoan species richness on the Antarctic continental shelf, slope and abyss</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Antarctic continental slope spans the depths from the shelf break (usually between 500 and 10...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Antarctic continental slope spans the depths from the shelf break (usually between 500 and 1000 m) to ~3000 m, is very steep, overlain by &#39;warm&#39; (2-2.5 °C) Circumpolar Deep Water (CDW), and life there is poorly studied. This study investigates whether life on Antarctica&#39;s continental slope is essentially an extension of the shelf or the abyssal fauna, a transition zone between these or clearly distinct in its own right. Using data from several cruises to the Weddell Sea and Scotia Sea, including the ANDEEP (ANtarctic benthic DEEP-sea biodiversity, colonisation history and recent community patterns) I-III, BIOPEARL (Biodiversity, Phylogeny, Evolution and Adaptive Radiation of Life in Antarctica) 1 and EASIZ (Ecology of the Antarctic Sea Ice Zone) II cruises as well as current databases (SOMBASE, SCAR-MarBIN), four different taxa were selected (i.e. cheilostome bryozoans, isopod and ostracod crustaceans and echinoid echinoderms) and two areas, the Weddell Sea and the Scotia Sea, to examine faunal composition, richness and affinities. The answer has important ramifications to the link between physical oceanography and ecology, and the potential of the slope to act as a refuge and resupply zone to the shelf during glaciations. Benthic samples were collected using Agassiz trawl, epibenthic sledge and Rauschert sled. By bathymetric definition, these data suggest that despite eurybathy in some of the groups examined and apparent similarity of physical conditions in the Antarctic, the shelf, slope and abyssal faunas were clearly separated in the Weddell Sea. However, no such separation of faunas was apparent in the Scotia Sea (except in echinoids). Using a geomorphological definition of the slope, shelf-slope-abyss similarity only changed significantly in the bryozoans. Our results did not support the presence of a homogenous and unique Antarctic slope fauna despite a high number of species being restricted to the slope. However, it remains the case that there may be a unique Antarctic slope fauna, but the paucity of [...]</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647038"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647038"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647038; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=127647038]").text(description); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=127647036]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":127647036,"title":"(Table 2) Phytoplankton composition of the surface layer of Station PS71/039 on Maud Rise","internal_url":"https://www.academia.edu/127647036/_Table_2_Phytoplankton_composition_of_the_surface_layer_of_Station_PS71_039_on_Maud_Rise","owner_id":226089093,"coauthors_can_edit":true,"owner":{"id":226089093,"first_name":"Angelika","middle_initials":null,"last_name":"Brandt","page_name":"BrandtAngelika","domain_name":"independent","created_at":"2022-06-09T03:39:28.948-07:00","display_name":"Angelika Brandt","url":"https://independent.academia.edu/BrandtAngelika"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647034"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647034/First_insights_into_the_solenogaster_diversity_of_the_Sea_of_Okhotsk_with_the_description_of_a_new_species_of_Kruppomenia_Simrothiellidae_Cavibelonia_"><img alt="Research paper thumbnail of First insights into the solenogaster diversity of the Sea of Okhotsk with the description of a new species of Kruppomenia (Simrothiellidae, Cavibelonia)" class="work-thumbnail" src="https://attachments.academia-assets.com/121350434/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647034/First_insights_into_the_solenogaster_diversity_of_the_Sea_of_Okhotsk_with_the_description_of_a_new_species_of_Kruppomenia_Simrothiellidae_Cavibelonia_">First insights into the solenogaster diversity of the Sea of Okhotsk with the description of a new species of Kruppomenia (Simrothiellidae, Cavibelonia)</a></div><div class="wp-workCard_item"><span>Deep Sea Research Part II: Topical Studies in Oceanography</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Solenogastres form a small clade of worm-shaped molluscs distributed world-wide with most of the ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Solenogastres form a small clade of worm-shaped molluscs distributed world-wide with most of the approx. 300 species occurring in the deep sea. A recent diversity study from the abyssal plain in the Northwest Pacific has revealed a wealth of new abyssal solenogaster lineages highlighting the need for further alpha-taxonomic work. During the 'Sea of Okhotsk Biodiversity Studies' (SokhoBio) expedition, 93 specimens were collected at overall eight stations ranging from depths of 1696 m to 3377 m. Preliminary investigations revealed twelve clearly distinguishable morphospecies, including one relatively common species present at six of eleven stations. All morphospecies are characterized externally via light microscopy and identified to the best possible taxonomic level via scleritome characters. Molecular barcodes (16S rRNA) are provided as a first step towards establishment of a barcoding library to enable fast and accurate re-identification of these taxonomically challenging molluscs in future studies. The most wide-spread and abundant cavibelonian Solenogastres Kruppomenia genslerae sp. nov. (Simrothiellidae) is exemplarily described in full microanatomical detail based on 3D-reconstructions from histological semithin section series and scanning electron microscopy. We discuss our results in comparison to the solenogaster diversity of the neighbouring abyssal plain of the Northwest Pacific, which is connected with the Kuril Basin via two straits. Our initial characterization of the diversity boosts the hitherto poorly known diversity of Solenogastres in the Far Eastern Seas, but also underlines the taxonomic impediment for proper taxonomic descriptions of the wealth of new discovered material.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ddc685747da4cbb7ac02618b7502520f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350434,"asset_id":127647034,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350434/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647034"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647034"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647034; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647032"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647032/Peracarid_crustacean_assemblages_of_the_Kolbeinsey_Ridge_north_of_Iceland"><img alt="Research paper thumbnail of Peracarid crustacean assemblages of the Kolbeinsey Ridge, north of Iceland" class="work-thumbnail" src="https://attachments.academia-assets.com/121350431/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647032/Peracarid_crustacean_assemblages_of_the_Kolbeinsey_Ridge_north_of_Iceland">Peracarid crustacean assemblages of the Kolbeinsey Ridge, north of Iceland</a></div><div class="wp-workCard_item"><span>Polar Biology</span><span>, 1994</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">On the Kolbeinsey Ridge, north of Iceland, 92 species of peracarid crustaceans were sampled using...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">On the Kolbeinsey Ridge, north of Iceland, 92 species of peracarid crustaceans were sampled using the epibenthic sledge. For an analysis of the multispecies distribution pattern across the ridge, a total of 46 species have been considered, which occurred at least at two stations and with at least 5% relative abundance at any one station. The analysis revealed four assemblages: a deep species assemblage, an eastern slope assemblage, an ubiquitous species assemblage and a western slope assemblage. The western slope assemblage consists mainly of Amphipoda, which were most abundant and diverse on the western slope. The ubiquitous and eastern slope assemblages, however, are dominated by Isopoda, which also comprised most species and individuals on the eastern slope. Cumaceans were the most representative species of the deep species assemblage. These differences in species composition and abundance can probably be attributed to food supply and sediment composition, rather than to salinity or bottom water temperature.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="fa60a1bf5382894a493d4cf932b42823" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":121350431,"asset_id":127647032,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/121350431/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="127647032"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127647032"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127647032; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="127647029"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/127647029/Seasonal_occurrence_of_planktic_Crustacea_in_sediment_trap_samples_at_three_depth_horizons_in_the_Greenland_Sea"><img alt="Research paper thumbnail of Seasonal occurrence of planktic Crustacea in sediment trap samples at three depth horizons in the Greenland Sea" class="work-thumbnail" src="https://attachments.academia-assets.com/121350428/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/127647029/Seasonal_occurrence_of_planktic_Crustacea_in_sediment_trap_samples_at_three_depth_horizons_in_the_Greenland_Sea">Seasonal occurrence of planktic Crustacea in sediment trap samples at three depth horizons in the Greenland Sea</a></div><div class="wp-workCard_item"><span>Polar Biology</span><span>, 1997</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Zooplankton were quantitatively investigated in sediment trap samples deployed in the Greenland S...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Zooplankton were quantitatively investigated in sediment trap samples deployed in the Greenland Sea at three locations (72°00.7N, 7°02.5W, 72°23.0N, 7°42.7W and 72°22.9N, 7°42.7W). Overall samples covered a period of three annual cycles (July 1989 to July 1992). The investigation of zooplankton, consisting almost exclusively of Crustacea ('99%), shows that the majority of the species must be regarded as ''swimmers'', which actively invaded the traps. Crustacea were composed of 45 species, mainly Copepoda, Amphipoda and Ostracoda. Each depth level showed a characteristic species composition. Diversity decreased with depth. The samples were dominated by Copepoda in terms of abundance and by Amphipoda with respect to biomass. The seasonal occurrence of Crustacea showed a maximum during winter and a minimum during summer. Carnivores were regularly found in the collected material, indicating that they had been actively attracted by the organic matter emanating from the traps. Omnivores showed a distinct seasonal occurrence. During winter, when primary production is low, omnivores change to a predatory way of life and they were consequently also found in increasing numbers. Herbivores were always rare. 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