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class="label"><span class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="245506432" href="https://www.academia.edu/Documents/in/Kentsel_Muhalefet"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://independent.academia.edu/BergmannMelanie","location":"/BergmannMelanie","scheme":"https","host":"independent.academia.edu","port":null,"pathname":"/BergmannMelanie","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Kentsel Muhalefet"]}" data-trace="false" 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data-dom-id="Pill-react-component-c418d61d-d794-435e-87cd-6a6b60b10193"></div> <div id="Pill-react-component-c418d61d-d794-435e-87cd-6a6b60b10193"></div> </a></div></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Melanie Bergmann</h3></div><div class="js-work-strip profile--work_container" data-work-id="90832620"><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/90832620/Review_report_on_and_8221_Atmospheric_dry_deposition_of_microplastics_and_mesoplastics_in_an_Antarctic_glacier_The_case_of_the_expanded_polystyrene_and_8221_tc_2020_261_"><img alt="Research paper thumbnail of Review report on &#8221;Atmospheric dry deposition of microplastics and mesoplastics in an Antarctic glacier: The case of the expanded polystyrene&#8221; (tc-2020-261)" class="work-thumbnail" src="https://attachments.academia-assets.com/94286548/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/90832620/Review_report_on_and_8221_Atmospheric_dry_deposition_of_microplastics_and_mesoplastics_in_an_Antarctic_glacier_The_case_of_the_expanded_polystyrene_and_8221_tc_2020_261_">Review report on &#8221;Atmospheric dry deposition of microplastics and mesoplastics in an Antarctic glacier: The case of the expanded polystyrene&#8221; (tc-2020-261)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6f8e3f36ccbb1f9df1e39132311cd956" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94286548,"asset_id":90832620,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94286548/download_file?st=MTczMjQwMDUzNSw4LjIyMi4yMDguMTQ2&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="90832620"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span 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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/90832619/A_global_plastic_treaty_must_cap_production">A global plastic treaty must cap production</a></div><div class="wp-workCard_item"><span>Science</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="90832619"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832619"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832619; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90832619]").text(description); $(".js-view-count[data-work-id=90832619]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90832619; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90832619']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 90832619, container: "", }); });</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-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.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" } } $('.js-work-strip[data-work-id=90832619]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90832619,"title":"A global plastic treaty must cap production","translated_title":"","metadata":{"publisher":"American Association for the Advancement of Science (AAAS)","publication_name":"Science"},"translated_abstract":null,"internal_url":"https://www.academia.edu/90832619/A_global_plastic_treaty_must_cap_production","translated_internal_url":"","created_at":"2022-11-15T06:10:31.895-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":245506432,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"A_global_plastic_treaty_must_cap_production","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":245506432,"first_name":"Melanie","middle_initials":null,"last_name":"Bergmann","page_name":"BergmannMelanie","domain_name":"independent","created_at":"2022-11-15T06:04:53.074-08:00","display_name":"Melanie 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href="https://www.academia.edu/90832618/Monitoring_microplastics_in_the_atmosphere_and_cryosphere_in_the_circumpolar_North_A_case_for_multi_compartment_monitoring"><img alt="Research paper thumbnail of Monitoring microplastics in the atmosphere and cryosphere in the circumpolar North: A case for multi-compartment monitoring" class="work-thumbnail" src="https://attachments.academia-assets.com/94286461/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/90832618/Monitoring_microplastics_in_the_atmosphere_and_cryosphere_in_the_circumpolar_North_A_case_for_multi_compartment_monitoring">Monitoring microplastics in the atmosphere and cryosphere in the circumpolar North: A case for multi-compartment monitoring</a></div><div class="wp-workCard_item"><span>Arctic Science</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The atmosphere and cryosphere have recently garnered considerable attention due to their role in ...</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 atmosphere and cryosphere have recently garnered considerable attention due to their role in transporting microplastics to and within the Arctic, and between freshwater, marine, and terrestrial environments. While investigating either in isolation provides valuable insight on the fate of microplastics in the Arctic, monitoring both provides a more holistic view. Nonetheless, despite the recent scientific interest, fundamental knowledge on microplastic abundance, and consistent monitoring efforts, are lacking for these compartments. Here, we build upon the work of the Arctic Monitoring and Assessment Programme’s Monitoring Guidelines for Litter and Microplastic to provide a roadmap for multi-compartment monitoring of the atmosphere and cryosphere to support our understanding of the sources, pathways, and sinks of plastic pollution across the Arctic. Overall, we recommend the use of existing standard techniques for ice and atmospheric sampling and to build upon existing monitoring...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9d4ce2b857defedae7fae8305936bf01" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94286461,"asset_id":90832618,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94286461/download_file?st=MTczMjQwMDUzNiw4LjIyMi4yMDguMTQ2&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="90832618"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832618"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832618; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90832618]").text(description); $(".js-view-count[data-work-id=90832618]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90832618; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90832618']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 90832618, container: "", }); });</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-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.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: "9d4ce2b857defedae7fae8305936bf01" } } $('.js-work-strip[data-work-id=90832618]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90832618,"title":"Monitoring microplastics in the atmosphere and cryosphere in the circumpolar North: A case for multi-compartment monitoring","translated_title":"","metadata":{"abstract":"The atmosphere and cryosphere have recently garnered considerable attention due to their role in transporting microplastics to and within the Arctic, and between freshwater, marine, and terrestrial environments. 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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="90832617"><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/90832617/Megafauna_at_the_Haakon_Mosby_mud_volcano_the_Barents_Sea_based_on_image_analysis"><img alt="Research paper thumbnail of Megafauna at the Haakon Mosby mud volcano (the Barents Sea) based on image analysis" 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" href="https://www.academia.edu/90832617/Megafauna_at_the_Haakon_Mosby_mud_volcano_the_Barents_Sea_based_on_image_analysis">Megafauna at the Haakon Mosby mud volcano (the Barents Sea) based on image analysis</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreak...</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">A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreaker R/V Polarstern in August 2002 to the Haakon Mosby Mud Volcano (HMMV). Different habitats inside the volcano caldera and outside were photographed using a towed camera system (Ocean Floor Observation System, OFOS). Four OFOS transects were carried out in total: three across the caldera (I-III) and one outside the caldera (IV) to the south of volcano. The length of each transect was ca. 2 km. 1045 images were used for statistical analyses. Among the analysed images, 894 were taken along the three transects across the caldera and 151 images along the transect outside the volcano. All images within the volcano were taken in the soft-sediment environment. Part of images along the transect outside the volcano were taken on hard substrata (boulders, carbonate rocks and crust). Those images were excluded from the analysis because the aim of our study was to compare fauna from similar sediment...</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="90832617"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832617"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832617; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90832617]").text(description); $(".js-view-count[data-work-id=90832617]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90832617; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90832617']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 90832617, container: "", }); });</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-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.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" } } $('.js-work-strip[data-work-id=90832617]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90832617,"title":"Megafauna at the Haakon Mosby mud volcano (the Barents Sea) based on image analysis","translated_title":"","metadata":{"abstract":"A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreaker R/V Polarstern in August 2002 to the Haakon Mosby Mud Volcano (HMMV). 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All images within the volcano were taken in the soft-sediment environment. Part of images along the transect outside the volcano were taken on hard substrata (boulders, carbonate rocks and crust). 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90832607"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/90832607/Belfast_UK"><img alt="Research paper thumbnail of Belfast; UK" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/90832607/Belfast_UK">Belfast; UK</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Despite over a century of exploitation of fish in European waters, scientists know surprisingly l...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Despite over a century of exploitation of fish in European waters, scientists know surprisingly little about the precise distribution of the major commercially exploited fish species, and their habitat requirements. 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$(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="90832604"><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/90832604/From_the_sea_surface_to_the_deep_seafloor_Microplastics_prevail_at_all_ocean_depths_of_the_HAUSGARTEN_observatory_Arctic_"><img alt="Research paper thumbnail of From the sea surface to the deep seafloor: Microplastics prevail at all ocean depths of the HAUSGARTEN observatory (Arctic)" 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" href="https://www.academia.edu/90832604/From_the_sea_surface_to_the_deep_seafloor_Microplastics_prevail_at_all_ocean_depths_of_the_HAUSGARTEN_observatory_Arctic_">From the sea surface to the deep seafloor: Microplastics prevail at all ocean depths of the HAUSGARTEN observatory (Arctic)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Although recent research indicates that microplastic (MP) has spread to all marine ecosystem comp...</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">Although recent research indicates that microplastic (MP) has spread to all marine ecosystem compartments from the sea surface to the deep sea, our understanding of transport pathways is still limited. Currently, our knowledge of MP concentrations throughout the water column is largely based on model runs. To fill this gap, we deployed in-situ pumps at four different depths (sea surface, ~300m, ~1000m, near seafloor) at five stations of the HAUSGARTEN observatory (west of Svalbard). These pumps filtered 218–560 litres of seawater (&gt; 10µm). Our analyses using µFTIR spectroscopy resulted in 16–8,750 MP m-3, comprising 15 different polymer types. Of the four deep stations (2500m depth), the northernmost station, which is located in the marginal ice zone, harboured the highest concentration (1,373 MP m-3) throughout the water column, and polyamide accounted for the largest proportion (28%). 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90832603"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/90832603/Discards_from_the_Nephrops_norvegicus_fishery_in_the_Clyde_Sea_area_composition_damage_survival_and_utilization_by_benthic_scavengers"><img alt="Research paper thumbnail of Discards from the Nephrops norvegicus fishery in the Clyde Sea area: composition, damage, survival and utilization by benthic scavengers" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/90832603/Discards_from_the_Nephrops_norvegicus_fishery_in_the_Clyde_Sea_area_composition_damage_survival_and_utilization_by_benthic_scavengers">Discards from the Nephrops norvegicus fishery in the Clyde Sea area: composition, damage, survival and utilization by benthic scavengers</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90832603"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832603"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832603; 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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="90832602"><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/90832602/_Table_2_Species_density_and_composition_of_an_inshore_and_offshore_station_in_Kongsfjord_Svalbard"><img alt="Research paper thumbnail of (Table 2) Species density and composition of an inshore and offshore station in Kongsfjord, Svalbard" 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" href="https://www.academia.edu/90832602/_Table_2_Species_density_and_composition_of_an_inshore_and_offshore_station_in_Kongsfjord_Svalbard">(Table 2) Species density and composition of an inshore and offshore station in Kongsfjord, Svalbard</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Megafauna plays an important role in benthic ecosystems and contributes significantly to benthic ...</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">Megafauna plays an important role in benthic ecosystems and contributes significantly to benthic biomass in the Arctic. The distribution is mostly studied using towed cameras. Here, we compare the megafauna from two sites located at different distances from the Kongsfjord: one station at the entrance to the fjord, another on the outer shelf. Although they are only located 25 km apart and at comparable depth, there were significant differences in their species composition. While the inshore station was characterized by shrimps (2.57 +/- 2.18 ind./m**2) and brittlestars (3.21 +/- 3.21 ind./m**2), the offshore site harboured even higher brittlestar densities (15.23 +/- 9.32 ind./m**2) and high numbers of the sea urchin Strongylocentrotus pallidus (1.23 +/- 1.09 ind./m**2). Phytodetrital concentrations of the upper sediment centimetres were significantly higher inshore compared with offshore. At a smaller scale, there were also differences in the composition of different transect sections. Several taxa were characterized by a patchy distribution along transects. We conclude that these differences were caused primarily by habitat characteristics. The seafloor inshore was characterized by glacial soft sediments, whereas the station offshore harboured large quantities of stones. Although the use of a new web-2.0-based tool, BIIGLE (<a href="http://www.BIIGLE.de" rel="nofollow">http://www.BIIGLE.de</a>), allowed us to analyse more images (~90) than could have been achieved by hand, taxon area curves indicated that the number of images analysed was not sufficient to capture the species inventory fully. New automated image analysis tools would enable a rapid analysis of larger quantities of camera footage.</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="90832602"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832602"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832602; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90832602]").text(description); $(".js-view-count[data-work-id=90832602]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90832602; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90832602']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 90832602, container: "", }); });</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-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.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" } } $('.js-work-strip[data-work-id=90832602]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90832602,"title":"(Table 2) Species density and composition of an inshore and offshore station in Kongsfjord, Svalbard","translated_title":"","metadata":{"abstract":"Megafauna plays an important role in benthic ecosystems and contributes significantly to benthic biomass in the Arctic. The distribution is mostly studied using towed cameras. Here, we compare the megafauna from two sites located at different distances from the Kongsfjord: one station at the entrance to the fjord, another on the outer shelf. Although they are only located 25 km apart and at comparable depth, there were significant differences in their species composition. While the inshore station was characterized by shrimps (2.57 +/- 2.18 ind./m**2) and brittlestars (3.21 +/- 3.21 ind./m**2), the offshore site harboured even higher brittlestar densities (15.23 +/- 9.32 ind./m**2) and high numbers of the sea urchin Strongylocentrotus pallidus (1.23 +/- 1.09 ind./m**2). Phytodetrital concentrations of the upper sediment centimetres were significantly higher inshore compared with offshore. At a smaller scale, there were also differences in the composition of different transect sections. Several taxa were characterized by a patchy distribution along transects. We conclude that these differences were caused primarily by habitat characteristics. The seafloor inshore was characterized by glacial soft sediments, whereas the station offshore harboured large quantities of stones. Although the use of a new web-2.0-based tool, BIIGLE (http://www.BIIGLE.de), allowed us to analyse more images (~90) than could have been achieved by hand, taxon area curves indicated that the number of images analysed was not sufficient to capture the species inventory fully. New automated image analysis tools would enable a rapid analysis of larger quantities of camera footage.","publication_date":{"day":null,"month":null,"year":2011,"errors":{}}},"translated_abstract":"Megafauna plays an important role in benthic ecosystems and contributes significantly to benthic biomass in the Arctic. The distribution is mostly studied using towed cameras. 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While investigating either in isolation provides valuable insight on the fate of microplastics in the Arctic, monitoring both provides a more holistic view. Nonetheless, despite the recent scientific interest, fundamental knowledge on microplastic abundance, and consistent monitoring efforts, are lacking for these compartments. Here, we build upon the work of the Arctic Monitoring and Assessment Programme’s Monitoring Guidelines for Litter and Microplastic to provide a roadmap for multi-compartment monitoring of the atmosphere and cryosphere to support our understanding of the sources, pathways, and sinks of plastic pollution across the Arctic. Overall, we recommend the use of existing standard techniques for ice and atmospheric sampling and to build upon existing monitoring...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9d4ce2b857defedae7fae8305936bf01" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94286461,"asset_id":90832618,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94286461/download_file?st=MTczMjQwMDUzNiw4LjIyMi4yMDguMTQ2&st=MTczMjQwMDUzNiw4LjIyMi4yMDguMTQ2&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="90832618"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832618"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832618; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90832618]").text(description); $(".js-view-count[data-work-id=90832618]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90832618; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90832618']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 90832618, container: "", }); });</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-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.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: "9d4ce2b857defedae7fae8305936bf01" } } $('.js-work-strip[data-work-id=90832618]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90832618,"title":"Monitoring microplastics in the atmosphere and cryosphere in the circumpolar North: A case for multi-compartment monitoring","translated_title":"","metadata":{"abstract":"The atmosphere and cryosphere have recently garnered considerable attention due to their role in transporting microplastics to and within the Arctic, and between freshwater, marine, and terrestrial environments. While investigating either in isolation provides valuable insight on the fate of microplastics in the Arctic, monitoring both provides a more holistic view. Nonetheless, despite the recent scientific interest, fundamental knowledge on microplastic abundance, and consistent monitoring efforts, are lacking for these compartments. Here, we build upon the work of the Arctic Monitoring and Assessment Programme’s Monitoring Guidelines for Litter and Microplastic to provide a roadmap for multi-compartment monitoring of the atmosphere and cryosphere to support our understanding of the sources, pathways, and sinks of plastic pollution across the Arctic. Overall, we recommend the use of existing standard techniques for ice and atmospheric sampling and to build upon existing monitoring...","publisher":"Canadian Science Publishing","publication_name":"Arctic Science"},"translated_abstract":"The atmosphere and cryosphere have recently garnered considerable attention due to their role in transporting microplastics to and within the Arctic, and between freshwater, marine, and terrestrial environments. While investigating either in isolation provides valuable insight on the fate of microplastics in the Arctic, monitoring both provides a more holistic view. Nonetheless, despite the recent scientific interest, fundamental knowledge on microplastic abundance, and consistent monitoring efforts, are lacking for these compartments. 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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="90832617"><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/90832617/Megafauna_at_the_Haakon_Mosby_mud_volcano_the_Barents_Sea_based_on_image_analysis"><img alt="Research paper thumbnail of Megafauna at the Haakon Mosby mud volcano (the Barents Sea) based on image analysis" 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" href="https://www.academia.edu/90832617/Megafauna_at_the_Haakon_Mosby_mud_volcano_the_Barents_Sea_based_on_image_analysis">Megafauna at the Haakon Mosby mud volcano (the Barents Sea) based on image analysis</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreak...</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">A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreaker R/V Polarstern in August 2002 to the Haakon Mosby Mud Volcano (HMMV). Different habitats inside the volcano caldera and outside were photographed using a towed camera system (Ocean Floor Observation System, OFOS). Four OFOS transects were carried out in total: three across the caldera (I-III) and one outside the caldera (IV) to the south of volcano. The length of each transect was ca. 2 km. 1045 images were used for statistical analyses. Among the analysed images, 894 were taken along the three transects across the caldera and 151 images along the transect outside the volcano. All images within the volcano were taken in the soft-sediment environment. Part of images along the transect outside the volcano were taken on hard substrata (boulders, carbonate rocks and crust). Those images were excluded from the analysis because the aim of our study was to compare fauna from similar sediment...</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="90832617"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90832617"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90832617; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90832617]").text(description); $(".js-view-count[data-work-id=90832617]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90832617; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90832617']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 90832617, container: "", }); });</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-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.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" } } $('.js-work-strip[data-work-id=90832617]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90832617,"title":"Megafauna at the Haakon Mosby mud volcano (the Barents Sea) based on image analysis","translated_title":"","metadata":{"abstract":"A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreaker R/V Polarstern in August 2002 to the Haakon Mosby Mud Volcano (HMMV). Different habitats inside the volcano caldera and outside were photographed using a towed camera system (Ocean Floor Observation System, OFOS). Four OFOS transects were carried out in total: three across the caldera (I-III) and one outside the caldera (IV) to the south of volcano. The length of each transect was ca. 2 km. 1045 images were used for statistical analyses. Among the analysed images, 894 were taken along the three transects across the caldera and 151 images along the transect outside the volcano. All images within the volcano were taken in the soft-sediment environment. Part of images along the transect outside the volcano were taken on hard substrata (boulders, carbonate rocks and crust). Those images were excluded from the analysis because the aim of our study was to compare fauna from similar sediment...","publisher":"Shirshov Institute of Oceanology, Russian Academy of Sciences","publication_date":{"day":29,"month":5,"year":2021,"errors":{}}},"translated_abstract":"A photographic survey was carried out during the expedition ARK-XVIII/1b of the research icebreaker R/V Polarstern in August 2002 to the Haakon Mosby Mud Volcano (HMMV). Different habitats inside the volcano caldera and outside were photographed using a towed camera system (Ocean Floor Observation System, OFOS). Four OFOS transects were carried out in total: three across the caldera (I-III) and one outside the caldera (IV) to the south of volcano. The length of each transect was ca. 2 km. 1045 images were used for statistical analyses. Among the analysed images, 894 were taken along the three transects across the caldera and 151 images along the transect outside the volcano. All images within the volcano were taken in the soft-sediment environment. Part of images along the transect outside the volcano were taken on hard substrata (boulders, carbonate rocks and crust). Those images were excluded from the analysis because the aim of our study was to compare fauna from similar sediment...","internal_url":"https://www.academia.edu/90832617/Megafauna_at_the_Haakon_Mosby_mud_volcano_the_Barents_Sea_based_on_image_analysis","translated_internal_url":"","created_at":"2022-11-15T06:10:31.544-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":245506432,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Megafauna_at_the_Haakon_Mosby_mud_volcano_the_Barents_Sea_based_on_image_analysis","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":245506432,"first_name":"Melanie","middle_initials":null,"last_name":"Bergmann","page_name":"BergmannMelanie","domain_name":"independent","created_at":"2022-11-15T06:04:53.074-08:00","display_name":"Melanie Bergmann","url":"https://independent.academia.edu/BergmannMelanie"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); 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The distribution is mostly studied using towed cameras. Here, we compare the megafauna from two sites located at different distances from the Kongsfjord: one station at the entrance to the fjord, another on the outer shelf. Although they are only located 25 km apart and at comparable depth, there were significant differences in their species composition. While the inshore station was characterized by shrimps (2.57 +/- 2.18 ind./m**2) and brittlestars (3.21 +/- 3.21 ind./m**2), the offshore site harboured even higher brittlestar densities (15.23 +/- 9.32 ind./m**2) and high numbers of the sea urchin Strongylocentrotus pallidus (1.23 +/- 1.09 ind./m**2). Phytodetrital concentrations of the upper sediment centimetres were significantly higher inshore compared with offshore. At a smaller scale, there were also differences in the composition of different transect sections. Several taxa were characterized by a patchy distribution along transects. 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