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I did intertidal research in Monterey Bay, California and Prince William Sound, Alaska. I was involved in subtidal marine research in all Alaskan seas extending into the Arctic. I am now retired.<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span><a class="ri-more-link js-profile-ri-list-card" data-click-track="profile-user-info-primary-research-interest" data-has-card-for-ri-list="33916837">View All (6)</a></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="33916837" href="https://www.academia.edu/Documents/in/Cyanobacteria"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://uaf.academia.edu/HowardFeder","location":"/HowardFeder","scheme":"https","host":"uaf.academia.edu","port":null,"pathname":"/HowardFeder","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" 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data-component-name="Pill" data-props="{"color":"gray","children":["Coral Reefs"]}" data-trace="false" data-dom-id="Pill-react-component-579a661c-86ce-4aa9-973c-a6dc2f513000"></div> <div id="Pill-react-component-579a661c-86ce-4aa9-973c-a6dc2f513000"></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 Howard Feder</h3></div><div class="js-work-strip profile--work_container" data-work-id="32970526"><div class="profile--work_thumbnail 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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="32930348"><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/32930348/Reproductive_Timing_and_Nutritional_Storage_Cycles_of_Mytilus_trossulus_Gould_1850_in_Port_Vald_ez_Alaska_Site_of_a_Marine_Oil_Terminal"><img alt="Research paper thumbnail of Reproductive Timing and Nutritional Storage Cycles of Mytilus' trossulus Gould, 1850, in Port Vald ez, Alaska, Site of a Marine Oil Terminal" class="work-thumbnail" src="https://attachments.academia-assets.com/53063839/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/32930348/Reproductive_Timing_and_Nutritional_Storage_Cycles_of_Mytilus_trossulus_Gould_1850_in_Port_Vald_ez_Alaska_Site_of_a_Marine_Oil_Terminal">Reproductive Timing and Nutritional Storage Cycles of Mytilus' trossulus Gould, 1850, in Port Vald ez, Alaska, Site of a Marine Oil Terminal</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycle...</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">MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycles for this mussel in Port Yaldez, a fjord within Prince William Sound, Alaska. Three intertidal sites within the boundaries of a marine terminal, and four sites remote from the terminal area were sampled. Mussels from Port Ya|dez exhibit a distinct annual cycle with gametogenic development throughout winter, during periods with freezing air and water temperatures, and demonstrate a summer-long spawning period. Nutritive cells generally decrease throughout late winter as gametogenesis proceeds to spawning, reaching minimal values during early summer. No differences between sites attributable to the proximity of mussels to the terminal area were apparent. The effects of stress, likely related to silt-laden waters derived from a nearby glacier, were observed at one site remote from the marine terminal. Regional differences in the reproductive cycles of MytiLus spp. are discussed.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d4575017202b9160ced8b907918e7083" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063839,"asset_id":32930348,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063839/download_file?st=MTczMjk4MjExNSw4LjIyMi4yMDguMTQ2&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="32930348"><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="32930348"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930348; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930348]").text(description); $(".js-view-count[data-work-id=32930348]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930348; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930348']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930348, 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: "d4575017202b9160ced8b907918e7083" } } $('.js-work-strip[data-work-id=32930348]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930348,"title":"Reproductive Timing and Nutritional Storage Cycles of Mytilus' trossulus Gould, 1850, in Port Vald ez, Alaska, Site of a Marine Oil Terminal","translated_title":"","metadata":{"abstract":"MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycles for this mussel in Port Yaldez, a fjord within Prince William Sound, Alaska. Three intertidal sites within the boundaries of a marine terminal, and four sites remote from the terminal area were sampled. Mussels from Port Ya|dez exhibit a distinct annual cycle with gametogenic development throughout winter, during periods with freezing air and water temperatures, and demonstrate a summer-long spawning period. Nutritive cells generally decrease throughout late winter as gametogenesis proceeds to spawning, reaching minimal values during early summer. No differences between sites attributable to the proximity of mussels to the terminal area were apparent. The effects of stress, likely related to silt-laden waters derived from a nearby glacier, were observed at one site remote from the marine terminal. Regional differences in the reproductive cycles of MytiLus spp. are discussed."},"translated_abstract":"MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycles for this mussel in Port Yaldez, a fjord within Prince William Sound, Alaska. Three intertidal sites within the boundaries of a marine terminal, and four sites remote from the terminal area were sampled. Mussels from Port Ya|dez exhibit a distinct annual cycle with gametogenic development throughout winter, during periods with freezing air and water temperatures, and demonstrate a summer-long spawning period. Nutritive cells generally decrease throughout late winter as gametogenesis proceeds to spawning, reaching minimal values during early summer. No differences between sites attributable to the proximity of mussels to the terminal area were apparent. 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Observations On Fishes Associated With Kelp Beds in Southern California" class="work-thumbnail" src="https://attachments.academia-assets.com/53063834/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/32930345/Title_Fish_Bulletin_160_Observations_On_Fishes_Associated_With_Kelp_Beds_in_Southern_California">Title: Fish Bulletin 160. Observations On Fishes Associated With Kelp Beds in Southern California</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This bulletin is meant to be a guide to the fishes of the west-central coast of North America tha...</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">This bulletin is meant to be a guide to the fishes of the west-central coast of North America that commonly occur in kelp beds and adjacent areas. The fishes described are common species, and this report is not meant to include all species that occur in the kelp environment and adjacent zones. In all, 97 species are described; key identification features are given. Colors listed for each species refer to how that specimen would appear in the live and/or recently captured state; underwater behavioral characteristics are given wherever possible to aid the underwater diving enthusiast. Description of the kelp environment is given, which includes a brief explanation pertaining to the three major ecological zones within the kelp ecosystem. A brief explanation and description of the kelp bed flora is included, along with geographical considerations. The kelp environment as a habitat type for fishes is discussed; three habitat regions in the kelp bed are given special attention, these are: 1) the canopy, 2) intermediate regions, and 3) kelp bottom holdfast region. Accounts of each species of fish then follow which include identification, distribution, size, habitat habits, and life history inclusive of food and reproductive biology whenever available. Four appendix tables include listings of the organisms frequently observed by diving in the various kelp bed habitat regions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a652fbc21c9710323e9c89c75bbfb26f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063834,"asset_id":32930345,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063834/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930345"><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="32930345"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930345; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930345]").text(description); $(".js-view-count[data-work-id=32930345]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930345; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930345']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930345, 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: "a652fbc21c9710323e9c89c75bbfb26f" } } $('.js-work-strip[data-work-id=32930345]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930345,"title":"Title: Fish Bulletin 160. 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The kelp environment as a habitat type for fishes is discussed; three habitat regions in the kelp bed are given special attention, these are: 1) the canopy, 2) intermediate regions, and 3) kelp bottom holdfast region. Accounts of each species of fish then follow which include identification, distribution, size, habitat habits, and life history inclusive of food and reproductive biology whenever available. Four appendix tables include listings of the organisms frequently observed by diving in the various kelp bed habitat regions."},"translated_abstract":"This bulletin is meant to be a guide to the fishes of the west-central coast of North America that commonly occur in kelp beds and adjacent areas. The fishes described are common species, and this report is not meant to include all species that occur in the kelp environment and adjacent zones. In all, 97 species are described; key identification features are given. 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Effects from a magnitude 9.2 earthquake in Prince William Sound, Alaska, 1964, were reflected in recolonization of the basin of the fjord, increased abundance and number of taxa over time, and moderately increased variability in abundance through 1990, stabilizing 26 years after the earthquake. Long-term climatic variability and local physical processes were important sources of spatial and temporal variability. Correlative evidence suggests that indirect effects of juvenile salmon from a shoreline salmon hatchery and deposition of adult salmon carcasses moderately enhanced deep-basin benthic communities. Effects on the deep benthos from a marine oil terminal were negligible. Overall, faunal trends deviated from the stability expected for benthic communities in other fjords. Physical characteristics of the fjord were important in mediating the effects of stressors and in delaying the readjustment process.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b04a4f3cc1ac3c4b7197089a2060e796" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063824,"asset_id":32930332,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063824/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930332"><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="32930332"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930332; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930332]").text(description); $(".js-view-count[data-work-id=32930332]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930332; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930332']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930332, 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: "b04a4f3cc1ac3c4b7197089a2060e796" } } $('.js-work-strip[data-work-id=32930332]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930332,"title":"Temporal variability of benthic communities in an Alaskan glacial fjord, 1971–2007","translated_title":"","metadata":{"abstract":"Temporal trends of deep-subtidal macrofauna in Port Valdez, Alaska, were assessed with respect to multiple environmental stressors. Effects from a magnitude 9.2 earthquake in Prince William Sound, Alaska, 1964, were reflected in recolonization of the basin of the fjord, increased abundance and number of taxa over time, and moderately increased variability in abundance through 1990, stabilizing 26 years after the earthquake. Long-term climatic variability and local physical processes were important sources of spatial and temporal variability. Correlative evidence suggests that indirect effects of juvenile salmon from a shoreline salmon hatchery and deposition of adult salmon carcasses moderately enhanced deep-basin benthic communities. Effects on the deep benthos from a marine oil terminal were negligible. Overall, faunal trends deviated from the stability expected for benthic communities in other fjords. 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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="32930305"><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/32930305/Trace_Element_and_Biotic_Changes_Following_a_Simulated_Oil_Spill_on_a_Mudflat_in_Port_Valdez_Alaska"><img alt="Research paper thumbnail of Trace Element and Biotic Changes Following a Simulated Oil Spill on a Mudflat in Port Valdez, Alaska" class="work-thumbnail" src="https://attachments.academia-assets.com/53063792/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/32930305/Trace_Element_and_Biotic_Changes_Following_a_Simulated_Oil_Spill_on_a_Mudflat_in_Port_Valdez_Alaska">Trace Element and Biotic Changes Following a Simulated Oil Spill on a Mudflat in Port Valdez, Alaska</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of ...</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 mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of Prudhoe Bay crude oil on metal chemistry and harpacticoid copepod abundance. Hydrocarbon concentrations were at background levels 30 days after final addition of oil. The short residence time of oil added to sediments is attributable to physical removal of oil by tides, low sediment permeability, and low affinity of hydrocarbons for peri-glacial clay surfaces. Elemental concentrations, except Si, were lower in oiled than in unoiled sediments. Elemental depletion in oil-impacted sediments is attributable to mobilization of metals from oxide/hydroxide sediment phases or to desorption from clay due to lowering of Eh-pH of sediments subsequent to oil addition. In oiled sediments, abundance of the harpacticoid cope-pods Harpacticus uniremis, Halectinosoma gothiceps, and Heterolaophonte sp. was similar to or higher than values within unoiled plots. The reasons for lack of dele-terious effects of oil on copepods in Port Valdez are not yet understood.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e13a55be6e6dbd07defb655e239b8c0c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063792,"asset_id":32930305,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063792/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930305"><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="32930305"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930305; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930305]").text(description); $(".js-view-count[data-work-id=32930305]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930305; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930305']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930305, 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: "e13a55be6e6dbd07defb655e239b8c0c" } } $('.js-work-strip[data-work-id=32930305]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930305,"title":"Trace Element and Biotic Changes Following a Simulated Oil Spill on a Mudflat in Port Valdez, Alaska","translated_title":"","metadata":{"abstract":"A mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of Prudhoe Bay crude oil on metal chemistry and harpacticoid copepod abundance. 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The reasons for lack of dele-terious effects of oil on copepods in Port Valdez are not yet understood."},"translated_abstract":"A mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of Prudhoe Bay crude oil on metal chemistry and harpacticoid copepod abundance. Hydrocarbon concentrations were at background levels 30 days after final addition of oil. The short residence time of oil added to sediments is attributable to physical removal of oil by tides, low sediment permeability, and low affinity of hydrocarbons for peri-glacial clay surfaces. Elemental concentrations, except Si, were lower in oiled than in unoiled sediments. Elemental depletion in oil-impacted sediments is attributable to mobilization of metals from oxide/hydroxide sediment phases or to desorption from clay due to lowering of Eh-pH of sediments subsequent to oil addition. 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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="32930277"><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/32930277/The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill"><img alt="Research paper thumbnail of The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill" class="work-thumbnail" src="https://attachments.academia-assets.com/53063763/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/32930277/The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill">The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, a...</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 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, an assessment of the benthic macrofauna and associated environmental parameters at 40 and 100 m was made. Assessment of the biota and environmental data demonstrated patterns in deep benthic assemblages reflective of oceanographic conditions, as indicated by sediment differences, rather than EVOS toxicity. Comparison of polynnclear aromatic hydrocarbons (PAH) and 813C values in sediments between stations within the oil trajectory and reference stations outside of the trajectory showed no significant differences. This investigation uncovered no signals of disturbance 16 months after the EVOS. These results agree with conclusions of studies of intertidal and shallow subtidal regions following the EVOS that demonstrated disturbance effects decreasing with depth.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c7f02a93a4d1dde9143fd99f690f2584" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063763,"asset_id":32930277,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063763/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930277"><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="32930277"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930277; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930277]").text(description); $(".js-view-count[data-work-id=32930277]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930277; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930277']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930277, 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: "c7f02a93a4d1dde9143fd99f690f2584" } } $('.js-work-strip[data-work-id=32930277]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930277,"title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill","translated_title":"","metadata":{"abstract":"In 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, an assessment of the benthic macrofauna and associated environmental parameters at 40 and 100 m was made. Assessment of the biota and environmental data demonstrated patterns in deep benthic assemblages reflective of oceanographic conditions, as indicated by sediment differences, rather than EVOS toxicity. Comparison of polynnclear aromatic hydrocarbons (PAH) and 813C values in sediments between stations within the oil trajectory and reference stations outside of the trajectory showed no significant differences. This investigation uncovered no signals of disturbance 16 months after the EVOS. These results agree with conclusions of studies of intertidal and shallow subtidal regions following the EVOS that demonstrated disturbance effects decreasing with depth."},"translated_abstract":"In 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, an assessment of the benthic macrofauna and associated environmental parameters at 40 and 100 m was made. Assessment of the biota and environmental data demonstrated patterns in deep benthic assemblages reflective of oceanographic conditions, as indicated by sediment differences, rather than EVOS toxicity. Comparison of polynnclear aromatic hydrocarbons (PAH) and 813C values in sediments between stations within the oil trajectory and reference stations outside of the trajectory showed no significant differences. This investigation uncovered no signals of disturbance 16 months after the EVOS. These results agree with conclusions of studies of intertidal and shallow subtidal regions following the EVOS that demonstrated disturbance effects decreasing with depth.","internal_url":"https://www.academia.edu/32930277/The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill","translated_internal_url":"","created_at":"2017-05-09T20:00:13.147-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28854583,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":376400,"co_author_invite_id":null,"email":"a***d@alaska.edu","affiliation":"University of Alaska Fairbanks","display_order":1,"name":"Arny Blanchard","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"},{"id":28854584,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":1049512,"email":"f***r@ims.uaf.edu","display_order":2,"name":"Howard Feder","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"},{"id":28854585,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":1296847,"email":"a***b@ims.uaf.edu","display_order":4,"name":"Arny Blanchard","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"},{"id":28854586,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":35006843,"co_author_invite_id":null,"email":"a***k@gmail.com","display_order":5,"name":"Arny Blanchard","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"}],"downloadable_attachments":[{"id":53063763,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063763/thumbnails/1.jpg","file_name":"Feder_and_Blanchard_1998_MPB.pdf","download_url":"https://www.academia.edu/attachments/53063763/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Deep_Benthos_of_Prince_William_Sound.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063763/Feder_and_Blanchard_1998_MPB-libre.pdf?1494385328=\u0026response-content-disposition=attachment%3B+filename%3DThe_Deep_Benthos_of_Prince_William_Sound.pdf\u0026Expires=1732985716\u0026Signature=EYUZTzvAe7GdzIH6qJNcYotOHCKWywWUF~ulHWzv2a0lyXDLfVfYkkJvR8KgF4Ir58uzcb2XKG89ipnfzJ3iTn9e7OE6g213WPey3trLZU8zjw75yzUiXo1zzZ8pQ5Z8oAGFX-xyhP7CtTGtmy7eN33DWf~zYzkcUiV613A64Ul8ntIS0~8KeR~KijSbS172INREr1Tjmlz1vX2RWjjMTfNYznYI50gTkSTjNUKjdqGcpWDkcsvSd2VYFPTlL~IxWNK8mx2zSvm~Tp3xR-XtmQjKEHe3VEsAmCkmzRSbJwxdOpm0PPVyQXXrlXbt9Ahkap5ZINKwzC~IB4kN23-uRw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill","translated_slug":"","page_count":13,"language":"en","content_type":"Work","owner":{"id":33916837,"first_name":"Howard","middle_initials":"","last_name":"Feder","page_name":"HowardFeder","domain_name":"uaf","created_at":"2015-08-14T13:09:52.457-07:00","display_name":"Howard Feder","url":"https://uaf.academia.edu/HowardFeder"},"attachments":[{"id":53063763,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063763/thumbnails/1.jpg","file_name":"Feder_and_Blanchard_1998_MPB.pdf","download_url":"https://www.academia.edu/attachments/53063763/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Deep_Benthos_of_Prince_William_Sound.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063763/Feder_and_Blanchard_1998_MPB-libre.pdf?1494385328=\u0026response-content-disposition=attachment%3B+filename%3DThe_Deep_Benthos_of_Prince_William_Sound.pdf\u0026Expires=1732985716\u0026Signature=EYUZTzvAe7GdzIH6qJNcYotOHCKWywWUF~ulHWzv2a0lyXDLfVfYkkJvR8KgF4Ir58uzcb2XKG89ipnfzJ3iTn9e7OE6g213WPey3trLZU8zjw75yzUiXo1zzZ8pQ5Z8oAGFX-xyhP7CtTGtmy7eN33DWf~zYzkcUiV613A64Ul8ntIS0~8KeR~KijSbS172INREr1Tjmlz1vX2RWjjMTfNYznYI50gTkSTjNUKjdqGcpWDkcsvSd2VYFPTlL~IxWNK8mx2zSvm~Tp3xR-XtmQjKEHe3VEsAmCkmzRSbJwxdOpm0PPVyQXXrlXbt9Ahkap5ZINKwzC~IB4kN23-uRw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, 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="32930268"><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/32930268/The_northeastern_Chukchi_Sea_benthos_environmental_interactions"><img alt="Research paper thumbnail of The northeastern Chukchi Sea: benthos-environmental interactions" class="work-thumbnail" src="https://attachments.academia-assets.com/53063752/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/32930268/The_northeastern_Chukchi_Sea_benthos_environmental_interactions">The northeastern Chukchi Sea: benthos-environmental interactions</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to...</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">Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to determine factors influencing faunal distribution. Four taxon-abundance-based benthic station groups were identified by cluster analysis and ordination techniques. These groups are explained, using stepwise multiple discriminant analysis, by the gravel-sand-mud and water content of bottom sediments, and the organic carbon/nitrogen (OC/N) ratio. In contrast to previous benthic investigations in the northeastern Bering and southeastern Chukchi Seas, faunal diversity between inshore and offshore regions in our study area were not related to differences in sediment sorting. Instead, regional diversity differences in the northeastern Chukchi Sea were related to greater environmental stresses (e.g. ice gouging, wave-current action, marine-mammal feeding activities) inshore than offshore. The presence of a high benthic biomass north of Icy Cape in the vicinity of Point Franklin and seaward of a hydrographic front is presumably related to an enhanced local depositional flux of particulate organic carbon (POC) in the area. We postulate that POC-rich waters derived from the northern Bering and northwestern Chukchi Seas extend to our study area and the flux of the entrained POC provides a persistent source of carbon to sustain the high benthic biomass. Annual POC enrichment of the coastal region north of Icy Cape is reflected by the great abundance of amphipods and other invertebrates present there and the concentration in summer of walrus Odobenus rosmarus djvergens and gray whales Eschrichtius robustus that feed on these invertebrates. This study demonstrates that there can be high standing stocks of benthos in arctic regions with relatively low annual primary production if local carbon is augmented by POC advected from highly productive areas.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="4a1fd1b25a0315943ee32037743206d6" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063752,"asset_id":32930268,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063752/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930268"><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="32930268"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930268; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930268]").text(description); $(".js-view-count[data-work-id=32930268]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930268; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930268']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930268, 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: "4a1fd1b25a0315943ee32037743206d6" } } $('.js-work-strip[data-work-id=32930268]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930268,"title":"The northeastern Chukchi Sea: benthos-environmental interactions","translated_title":"","metadata":{"abstract":"Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to determine factors influencing faunal distribution. Four taxon-abundance-based benthic station groups were identified by cluster analysis and ordination techniques. These groups are explained, using stepwise multiple discriminant analysis, by the gravel-sand-mud and water content of bottom sediments, and the organic carbon/nitrogen (OC/N) ratio. In contrast to previous benthic investigations in the northeastern Bering and southeastern Chukchi Seas, faunal diversity between inshore and offshore regions in our study area were not related to differences in sediment sorting. Instead, regional diversity differences in the northeastern Chukchi Sea were related to greater environmental stresses (e.g. ice gouging, wave-current action, marine-mammal feeding activities) inshore than offshore. The presence of a high benthic biomass north of Icy Cape in the vicinity of Point Franklin and seaward of a hydrographic front is presumably related to an enhanced local depositional flux of particulate organic carbon (POC) in the area. We postulate that POC-rich waters derived from the northern Bering and northwestern Chukchi Seas extend to our study area and the flux of the entrained POC provides a persistent source of carbon to sustain the high benthic biomass. Annual POC enrichment of the coastal region north of Icy Cape is reflected by the great abundance of amphipods and other invertebrates present there and the concentration in summer of walrus Odobenus rosmarus djvergens and gray whales Eschrichtius robustus that feed on these invertebrates. This study demonstrates that there can be high standing stocks of benthos in arctic regions with relatively low annual primary production if local carbon is augmented by POC advected from highly productive areas."},"translated_abstract":"Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to determine factors influencing faunal distribution. Four taxon-abundance-based benthic station groups were identified by cluster analysis and ordination techniques. These groups are explained, using stepwise multiple discriminant analysis, by the gravel-sand-mud and water content of bottom sediments, and the organic carbon/nitrogen (OC/N) ratio. In contrast to previous benthic investigations in the northeastern Bering and southeastern Chukchi Seas, faunal diversity between inshore and offshore regions in our study area were not related to differences in sediment sorting. Instead, regional diversity differences in the northeastern Chukchi Sea were related to greater environmental stresses (e.g. ice gouging, wave-current action, marine-mammal feeding activities) inshore than offshore. The presence of a high benthic biomass north of Icy Cape in the vicinity of Point Franklin and seaward of a hydrographic front is presumably related to an enhanced local depositional flux of particulate organic carbon (POC) in the area. We postulate that POC-rich waters derived from the northern Bering and northwestern Chukchi Seas extend to our study area and the flux of the entrained POC provides a persistent source of carbon to sustain the high benthic biomass. Annual POC enrichment of the coastal region north of Icy Cape is reflected by the great abundance of amphipods and other invertebrates present there and the concentration in summer of walrus Odobenus rosmarus djvergens and gray whales Eschrichtius robustus that feed on these invertebrates. This study demonstrates that there can be high standing stocks of benthos in arctic regions with relatively low annual primary production if local carbon is augmented by POC advected from highly productive areas.","internal_url":"https://www.academia.edu/32930268/The_northeastern_Chukchi_Sea_benthos_environmental_interactions","translated_internal_url":"","created_at":"2017-05-09T19:57:50.828-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28854578,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":32942776,"co_author_invite_id":null,"email":"s***u@alaska.edu","display_order":1,"name":"Sathy Naidu","title":"The northeastern Chukchi Sea: benthos-environmental interactions"},{"id":28854579,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":1049512,"email":"f***r@ims.uaf.edu","display_order":2,"name":"Howard Feder","title":"The northeastern Chukchi Sea: benthos-environmental interactions"},{"id":28854580,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":3706439,"email":"j***t@ims.alaska.edu","display_order":4,"name":"Stephen Jewett","title":"The northeastern Chukchi Sea: benthos-environmental interactions"},{"id":28854581,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":32439470,"co_author_invite_id":null,"email":"S***t@alaska.edu","display_order":5,"name":"Stephen Jewett","title":"The northeastern Chukchi Sea: benthos-environmental interactions"}],"downloadable_attachments":[{"id":53063752,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063752/thumbnails/1.jpg","file_name":"feder_northeast_chucki_sea.pdf","download_url":"https://www.academia.edu/attachments/53063752/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_northeastern_Chukchi_Sea_benthos_env.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063752/feder_northeast_chucki_sea-libre.pdf?1494385178=\u0026response-content-disposition=attachment%3B+filename%3DThe_northeastern_Chukchi_Sea_benthos_env.pdf\u0026Expires=1732985716\u0026Signature=glMiCEKeEMCLyDj36UElJvDIZ0IEFgcJV2Y2t0EJmtRnKR~MVYtQzK0uhapxxv6ygcJztJ9mtvPjOdiuptWWmyEdEBEnh~L7yLJDmLy9SbfCf65pUMiWj--BgsXI6zgbB192lR4ic3r4j~tuO6z8xBAo345nSsDJHZ5B9zBEq15HqWF3qaMgZGaHEWz01GlNb9gUEP8G3uU1q746Mj0ZTKP4mSoVdPAb99dhW-BTUatHGa1v-uaC~o2bMFfoqt7DfapuzEpP-yRU-JQKgiiC7tPyXkMLmCxQFonFWky219Mbv2q6dXB35Tz~6q2IGFucSm1b3fb9a8ZK9w9ZNA0QuA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_northeastern_Chukchi_Sea_benthos_environmental_interactions","translated_slug":"","page_count":20,"language":"en","content_type":"Work","owner":{"id":33916837,"first_name":"Howard","middle_initials":"","last_name":"Feder","page_name":"HowardFeder","domain_name":"uaf","created_at":"2015-08-14T13:09:52.457-07:00","display_name":"Howard Feder","url":"https://uaf.academia.edu/HowardFeder"},"attachments":[{"id":53063752,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063752/thumbnails/1.jpg","file_name":"feder_northeast_chucki_sea.pdf","download_url":"https://www.academia.edu/attachments/53063752/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_northeastern_Chukchi_Sea_benthos_env.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063752/feder_northeast_chucki_sea-libre.pdf?1494385178=\u0026response-content-disposition=attachment%3B+filename%3DThe_northeastern_Chukchi_Sea_benthos_env.pdf\u0026Expires=1732985716\u0026Signature=glMiCEKeEMCLyDj36UElJvDIZ0IEFgcJV2Y2t0EJmtRnKR~MVYtQzK0uhapxxv6ygcJztJ9mtvPjOdiuptWWmyEdEBEnh~L7yLJDmLy9SbfCf65pUMiWj--BgsXI6zgbB192lR4ic3r4j~tuO6z8xBAo345nSsDJHZ5B9zBEq15HqWF3qaMgZGaHEWz01GlNb9gUEP8G3uU1q746Mj0ZTKP4mSoVdPAb99dhW-BTUatHGa1v-uaC~o2bMFfoqt7DfapuzEpP-yRU-JQKgiiC7tPyXkMLmCxQFonFWky219Mbv2q6dXB35Tz~6q2IGFucSm1b3fb9a8ZK9w9ZNA0QuA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, 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="32930264"><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/32930264/Benthic_food_web_structure_in_the_southeastern_Chukchi_Sea_an_assessment_using_d_13_C_and_d_15_N_analyses"><img alt="Research paper thumbnail of Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N analyses" class="work-thumbnail" src="https://attachments.academia-assets.com/53063748/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/32930264/Benthic_food_web_structure_in_the_southeastern_Chukchi_Sea_an_assessment_using_d_13_C_and_d_15_N_analyses">Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N analyses</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://uaf.academia.edu/HowardFeder">Howard Feder</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/StephenJewett">Stephen Jewett</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomas...</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 benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomass resulting from settlement of a large proportion of seasonal phytoplankton under highly nutritious offshore Bering Shelf Anadyr Water (BSAW). In contrast, inshore Alaska Coastal Water (ACW) is much less productive. Yet the Chukchi Bight and Kotzebue Sound, located under ACW in the southeastern Chukchi Sea, contain a substantial faunal abundance and biomass of invertebrates, fishes and marine mammals. We examined food web structure to gain an understanding of how a relatively rich benthic fauna with a high biomass can be supported under ACW with a supposedly low flux of carbon to the benthos. We measured stable isotope (d 13 C and d 15 N) values of selected organisms (from zooplankton to fishes) as markers of food sources and trophic position to compare fauna on the shelf under BSAW with that in the Chukchi Bight and Kotzebue Sound under ACW. Relative isotope position of organisms in all three regions was similar, even though some pelagic species within the Sound were depleted in d 13 C compared to the other regions. We attribute the depletion to the influence of terrestrially derived carbon. We suggest that the hydrodynamics along an oceanic front between the Chuk-chi Shelf and the Chukchi Bight support the advection of nutrient-rich POC into the Bight and Sound as additional food sources to local production. We conclude that local conditions and multiple POC sources in the Bight and Sound support the substantial population of benthic invertebrates and the fishes, seabirds, and marine mammals that feed on them. Keywords Arctic Á Chukchi Sea Á Kotzebue Sound Á Benthos Á POC Á Stable isotopes Á Marine food web</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="25214c0f9eb13a7d8c82b2151ece297b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063748,"asset_id":32930264,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063748/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930264"><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="32930264"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930264; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930264]").text(description); $(".js-view-count[data-work-id=32930264]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930264; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930264']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930264, 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: "25214c0f9eb13a7d8c82b2151ece297b" } } $('.js-work-strip[data-work-id=32930264]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930264,"title":"Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N analyses","translated_title":"","metadata":{"abstract":"The benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomass resulting from settlement of a large proportion of seasonal phytoplankton under highly nutritious offshore Bering Shelf Anadyr Water (BSAW). In contrast, inshore Alaska Coastal Water (ACW) is much less productive. Yet the Chukchi Bight and Kotzebue Sound, located under ACW in the southeastern Chukchi Sea, contain a substantial faunal abundance and biomass of invertebrates, fishes and marine mammals. We examined food web structure to gain an understanding of how a relatively rich benthic fauna with a high biomass can be supported under ACW with a supposedly low flux of carbon to the benthos. We measured stable isotope (d 13 C and d 15 N) values of selected organisms (from zooplankton to fishes) as markers of food sources and trophic position to compare fauna on the shelf under BSAW with that in the Chukchi Bight and Kotzebue Sound under ACW. Relative isotope position of organisms in all three regions was similar, even though some pelagic species within the Sound were depleted in d 13 C compared to the other regions. We attribute the depletion to the influence of terrestrially derived carbon. We suggest that the hydrodynamics along an oceanic front between the Chuk-chi Shelf and the Chukchi Bight support the advection of nutrient-rich POC into the Bight and Sound as additional food sources to local production. We conclude that local conditions and multiple POC sources in the Bight and Sound support the substantial population of benthic invertebrates and the fishes, seabirds, and marine mammals that feed on them. Keywords Arctic Á Chukchi Sea Á Kotzebue Sound Á Benthos Á POC Á Stable isotopes Á Marine food web"},"translated_abstract":"The benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomass resulting from settlement of a large proportion of seasonal phytoplankton under highly nutritious offshore Bering Shelf Anadyr Water (BSAW). In contrast, inshore Alaska Coastal Water (ACW) is much less productive. Yet the Chukchi Bight and Kotzebue Sound, located under ACW in the southeastern Chukchi Sea, contain a substantial faunal abundance and biomass of invertebrates, fishes and marine mammals. We examined food web structure to gain an understanding of how a relatively rich benthic fauna with a high biomass can be supported under ACW with a supposedly low flux of carbon to the benthos. We measured stable isotope (d 13 C and d 15 N) values of selected organisms (from zooplankton to fishes) as markers of food sources and trophic position to compare fauna on the shelf under BSAW with that in the Chukchi Bight and Kotzebue Sound under ACW. Relative isotope position of organisms in all three regions was similar, even though some pelagic species within the Sound were depleted in d 13 C compared to the other regions. We attribute the depletion to the influence of terrestrially derived carbon. We suggest that the hydrodynamics along an oceanic front between the Chuk-chi Shelf and the Chukchi Bight support the advection of nutrient-rich POC into the Bight and Sound as additional food sources to local production. We conclude that local conditions and multiple POC sources in the Bight and Sound support the substantial population of benthic invertebrates and the fishes, seabirds, and marine mammals that feed on them. Keywords Arctic Á Chukchi Sea Á Kotzebue Sound Á Benthos Á POC Á Stable isotopes Á Marine food web","internal_url":"https://www.academia.edu/32930264/Benthic_food_web_structure_in_the_southeastern_Chukchi_Sea_an_assessment_using_d_13_C_and_d_15_N_analyses","translated_internal_url":"","created_at":"2017-05-09T19:56:55.705-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28854566,"work_id":32930264,"tagging_user_id":33916837,"tagged_user_id":376400,"co_author_invite_id":null,"email":"a***d@alaska.edu","affiliation":"University of Alaska Fairbanks","display_order":1,"name":"Arny Blanchard","title":"Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N 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href="https://www.academia.edu/32930259/Abiotic_Biological_Interactions_in_Coastal_Marine_Communities_Insights_from_an_Alaskan_Fjord">Abiotic/Biological Interactions in Coastal Marine Communities: Insights from an Alaskan Fjord</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Interactions among multi-scale coastal marine ecosystem processes can be expected to play large r...</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">Interactions among multi-scale coastal marine ecosystem processes can be expected to play large roles in and interact with biological processes as stresses increase, potentially allowing interfering processes (including biological interactions) to become more prevalent. Retrospective analyses of intertidal (1988–1992) and subtidal (1971–2012) species compositions from a long-term ecological research program in Port Valdez, Alaska evaluated associations between benthic community structure and physical conditions to better understand interactions between regional to local processes on flora and fauna. Low salinity, habitat structure (varying from mudflats to rocky shores over a distance of <18 km), and suspended sediments contributed to intertidal community structure via elimination of predators from low-salinity prey refugia. Subtidal communities demonstrate adjustments by macrofauna to sedi-mentation with smaller, disturbance-tolerant fauna towards the head of the fjord as well as effects from depth-related covari-ates. Shared ecological processes result in comparable community trends in subtidal and intertidal habitats among subarctic and arctic fjords and similarly among coastal environments of the North Pacific. Control exerted by interactions among climatic, oceanographic, and local processes interacting with biota contributes to the direction and length of recovery from disturbance events and environmental changes. Feedbacks, mediation of recovery by additional processes, and strengths of interactions also play important roles in determining interaction outcomes. Interactions among local, regional, and global-scale processes may become critical sources of change as global ecosystem transitions through new climate states.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="316b89a8ac01059d27f48a1a441a1bb1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063744,"asset_id":32930259,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063744/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930259"><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="32930259"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930259; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930259]").text(description); $(".js-view-count[data-work-id=32930259]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930259; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930259']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930259, 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: "316b89a8ac01059d27f48a1a441a1bb1" } } $('.js-work-strip[data-work-id=32930259]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930259,"title":"Abiotic/Biological Interactions in Coastal Marine Communities: Insights from an Alaskan Fjord","translated_title":"","metadata":{"abstract":"Interactions among multi-scale coastal marine ecosystem processes can be expected to play large roles in and interact with biological processes as stresses increase, potentially allowing interfering processes (including biological interactions) to become more prevalent. Retrospective analyses of intertidal (1988–1992) and subtidal (1971–2012) species compositions from a long-term ecological research program in Port Valdez, Alaska evaluated associations between benthic community structure and physical conditions to better understand interactions between regional to local processes on flora and fauna. Low salinity, habitat structure (varying from mudflats to rocky shores over a distance of \u003c18 km), and suspended sediments contributed to intertidal community structure via elimination of predators from low-salinity prey refugia. Subtidal communities demonstrate adjustments by macrofauna to sedi-mentation with smaller, disturbance-tolerant fauna towards the head of the fjord as well as effects from depth-related covari-ates. Shared ecological processes result in comparable community trends in subtidal and intertidal habitats among subarctic and arctic fjords and similarly among coastal environments of the North Pacific. 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Control exerted by interactions among climatic, oceanographic, and local processes interacting with biota contributes to the direction and length of recovery from disturbance events and environmental changes. Feedbacks, mediation of recovery by additional processes, and strengths of interactions also play important roles in determining interaction outcomes. 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Biology of the dominant soft-bottom epifauna and their interaction with the infauna</a></div><div class="wp-workCard_item"><span>Journal of Experimental Marine Biology and Ecology</span><span>, 1988</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... Ecol., 1988, Vol. ... koreni 2 5 Fibres 29 78 Trichobranchidae 1 3 Sediment 28 76 Unidentifie...</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">... Ecol., 1988, Vol. ... koreni 2 5 Fibres 29 78 Trichobranchidae 1 3 Sediment 28 76 Unidentified Polychaeta 18 49 Plant tissue 19 51 Annelida (Oligochaeta) Tubi coides benedeni 1 3 TABLE IVb Total number and per ... 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data-click-track="profile-work-strip-title" href="https://www.academia.edu/32930348/Reproductive_Timing_and_Nutritional_Storage_Cycles_of_Mytilus_trossulus_Gould_1850_in_Port_Vald_ez_Alaska_Site_of_a_Marine_Oil_Terminal">Reproductive Timing and Nutritional Storage Cycles of Mytilus' trossulus Gould, 1850, in Port Vald ez, Alaska, Site of a Marine Oil Terminal</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycle...</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">MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycles for this mussel in Port Yaldez, a fjord within Prince William Sound, Alaska. Three intertidal sites within the boundaries of a marine terminal, and four sites remote from the terminal area were sampled. Mussels from Port Ya|dez exhibit a distinct annual cycle with gametogenic development throughout winter, during periods with freezing air and water temperatures, and demonstrate a summer-long spawning period. Nutritive cells generally decrease throughout late winter as gametogenesis proceeds to spawning, reaching minimal values during early summer. No differences between sites attributable to the proximity of mussels to the terminal area were apparent. The effects of stress, likely related to silt-laden waters derived from a nearby glacier, were observed at one site remote from the marine terminal. Regional differences in the reproductive cycles of MytiLus spp. are discussed.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d4575017202b9160ced8b907918e7083" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063839,"asset_id":32930348,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063839/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNSw4LjIyMi4yMDguMTQ2&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="32930348"><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="32930348"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930348; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930348]").text(description); $(".js-view-count[data-work-id=32930348]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930348; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930348']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930348, 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: "d4575017202b9160ced8b907918e7083" } } $('.js-work-strip[data-work-id=32930348]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930348,"title":"Reproductive Timing and Nutritional Storage Cycles of Mytilus' trossulus Gould, 1850, in Port Vald ez, Alaska, Site of a Marine Oil Terminal","translated_title":"","metadata":{"abstract":"MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycles for this mussel in Port Yaldez, a fjord within Prince William Sound, Alaska. Three intertidal sites within the boundaries of a marine terminal, and four sites remote from the terminal area were sampled. Mussels from Port Ya|dez exhibit a distinct annual cycle with gametogenic development throughout winter, during periods with freezing air and water temperatures, and demonstrate a summer-long spawning period. Nutritive cells generally decrease throughout late winter as gametogenesis proceeds to spawning, reaching minimal values during early summer. No differences between sites attributable to the proximity of mussels to the terminal area were apparent. The effects of stress, likely related to silt-laden waters derived from a nearby glacier, were observed at one site remote from the marine terminal. Regional differences in the reproductive cycles of MytiLus spp. are discussed."},"translated_abstract":"MytiLus trossulus was investigated to determine the reproductive and nutritive cell storage cycles for this mussel in Port Yaldez, a fjord within Prince William Sound, Alaska. Three intertidal sites within the boundaries of a marine terminal, and four sites remote from the terminal area were sampled. Mussels from Port Ya|dez exhibit a distinct annual cycle with gametogenic development throughout winter, during periods with freezing air and water temperatures, and demonstrate a summer-long spawning period. Nutritive cells generally decrease throughout late winter as gametogenesis proceeds to spawning, reaching minimal values during early summer. No differences between sites attributable to the proximity of mussels to the terminal area were apparent. The effects of stress, likely related to silt-laden waters derived from a nearby glacier, were observed at one site remote from the marine terminal. Regional differences in the reproductive cycles of MytiLus spp. are discussed.","internal_url":"https://www.academia.edu/32930348/Reproductive_Timing_and_Nutritional_Storage_Cycles_of_Mytilus_trossulus_Gould_1850_in_Port_Vald_ez_Alaska_Site_of_a_Marine_Oil_Terminal","translated_internal_url":"","created_at":"2017-05-09T20:20:08.100-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28854626,"work_id":32930348,"tagging_user_id":33916837,"tagged_user_id":376400,"co_author_invite_id":null,"email":"a***d@alaska.edu","affiliation":"University of Alaska Fairbanks","display_order":1,"name":"Arny Blanchard","title":"Reproductive Timing and Nutritional Storage Cycles of Mytilus' trossulus Gould, 1850, in Port Vald ez, Alaska, Site of a Marine Oil Terminal"}],"downloadable_attachments":[{"id":53063839,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063839/thumbnails/1.jpg","file_name":"1997_Blanchard_and_Feder_Port_Valdez_mytilus_reproduction.PDF","download_url":"https://www.academia.edu/attachments/53063839/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Reproductive_Timing_and_Nutritional_Stor.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063839/1997_Blanchard_and_Feder_Port_Valdez_mytilus_reproduction-libre.PDF?1494386633=\u0026response-content-disposition=attachment%3B+filename%3DReproductive_Timing_and_Nutritional_Stor.pdf\u0026Expires=1732985715\u0026Signature=fcw6Te47gKbA2p3FtjRDAiR7tA4SQGidjO~CjMIfVO4XdXaUJUbxuNcVtwcFCWDn0xIDOFiPInQtUFnWJ4qXLgISMj1mrQLODQyU27TvE6IKVIwI-hs8vlBlVaIYQ~VbL2k-IB~SF6X-oHgjY2zU6TJa1fLpNw40u0Qn0sxvxW6W~c75ldhehXrbRgb6tx4jlU46PDJF62vGzOWz~NjOwRthoLWmFcfU9xQPt~nNWk9kph7V4Yn-DN~AhPSZO~Z5iFHoDuse4-81ajOg3gKCnrloOtYutTWl5VNxG5obd7CVzaVh6wOM7c-aAlf1vtv9AT4kFR~w~-GG3T554kcM4A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Reproductive_Timing_and_Nutritional_Storage_Cycles_of_Mytilus_trossulus_Gould_1850_in_Port_Vald_ez_Alaska_Site_of_a_Marine_Oil_Terminal","translated_slug":"","page_count":10,"language":"en","content_type":"Work","owner":{"id":33916837,"first_name":"Howard","middle_initials":"","last_name":"Feder","page_name":"HowardFeder","domain_name":"uaf","created_at":"2015-08-14T13:09:52.457-07:00","display_name":"Howard Feder","url":"https://uaf.academia.edu/HowardFeder"},"attachments":[{"id":53063839,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063839/thumbnails/1.jpg","file_name":"1997_Blanchard_and_Feder_Port_Valdez_mytilus_reproduction.PDF","download_url":"https://www.academia.edu/attachments/53063839/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Reproductive_Timing_and_Nutritional_Stor.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063839/1997_Blanchard_and_Feder_Port_Valdez_mytilus_reproduction-libre.PDF?1494386633=\u0026response-content-disposition=attachment%3B+filename%3DReproductive_Timing_and_Nutritional_Stor.pdf\u0026Expires=1732985715\u0026Signature=fcw6Te47gKbA2p3FtjRDAiR7tA4SQGidjO~CjMIfVO4XdXaUJUbxuNcVtwcFCWDn0xIDOFiPInQtUFnWJ4qXLgISMj1mrQLODQyU27TvE6IKVIwI-hs8vlBlVaIYQ~VbL2k-IB~SF6X-oHgjY2zU6TJa1fLpNw40u0Qn0sxvxW6W~c75ldhehXrbRgb6tx4jlU46PDJF62vGzOWz~NjOwRthoLWmFcfU9xQPt~nNWk9kph7V4Yn-DN~AhPSZO~Z5iFHoDuse4-81ajOg3gKCnrloOtYutTWl5VNxG5obd7CVzaVh6wOM7c-aAlf1vtv9AT4kFR~w~-GG3T554kcM4A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, 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="32930345"><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/32930345/Title_Fish_Bulletin_160_Observations_On_Fishes_Associated_With_Kelp_Beds_in_Southern_California"><img alt="Research paper thumbnail of Title: Fish Bulletin 160. Observations On Fishes Associated With Kelp Beds in Southern California" class="work-thumbnail" src="https://attachments.academia-assets.com/53063834/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/32930345/Title_Fish_Bulletin_160_Observations_On_Fishes_Associated_With_Kelp_Beds_in_Southern_California">Title: Fish Bulletin 160. Observations On Fishes Associated With Kelp Beds in Southern California</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This bulletin is meant to be a guide to the fishes of the west-central coast of North America tha...</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">This bulletin is meant to be a guide to the fishes of the west-central coast of North America that commonly occur in kelp beds and adjacent areas. The fishes described are common species, and this report is not meant to include all species that occur in the kelp environment and adjacent zones. In all, 97 species are described; key identification features are given. Colors listed for each species refer to how that specimen would appear in the live and/or recently captured state; underwater behavioral characteristics are given wherever possible to aid the underwater diving enthusiast. Description of the kelp environment is given, which includes a brief explanation pertaining to the three major ecological zones within the kelp ecosystem. A brief explanation and description of the kelp bed flora is included, along with geographical considerations. The kelp environment as a habitat type for fishes is discussed; three habitat regions in the kelp bed are given special attention, these are: 1) the canopy, 2) intermediate regions, and 3) kelp bottom holdfast region. Accounts of each species of fish then follow which include identification, distribution, size, habitat habits, and life history inclusive of food and reproductive biology whenever available. Four appendix tables include listings of the organisms frequently observed by diving in the various kelp bed habitat regions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a652fbc21c9710323e9c89c75bbfb26f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063834,"asset_id":32930345,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063834/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930345"><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="32930345"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930345; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930345]").text(description); $(".js-view-count[data-work-id=32930345]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930345; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930345']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930345, 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: "a652fbc21c9710323e9c89c75bbfb26f" } } $('.js-work-strip[data-work-id=32930345]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930345,"title":"Title: Fish Bulletin 160. Observations On Fishes Associated With Kelp Beds in Southern California","translated_title":"","metadata":{"abstract":"This bulletin is meant to be a guide to the fishes of the west-central coast of North America that commonly occur in kelp beds and adjacent areas. The fishes described are common species, and this report is not meant to include all species that occur in the kelp environment and adjacent zones. In all, 97 species are described; key identification features are given. Colors listed for each species refer to how that specimen would appear in the live and/or recently captured state; underwater behavioral characteristics are given wherever possible to aid the underwater diving enthusiast. Description of the kelp environment is given, which includes a brief explanation pertaining to the three major ecological zones within the kelp ecosystem. A brief explanation and description of the kelp bed flora is included, along with geographical considerations. The kelp environment as a habitat type for fishes is discussed; three habitat regions in the kelp bed are given special attention, these are: 1) the canopy, 2) intermediate regions, and 3) kelp bottom holdfast region. Accounts of each species of fish then follow which include identification, distribution, size, habitat habits, and life history inclusive of food and reproductive biology whenever available. Four appendix tables include listings of the organisms frequently observed by diving in the various kelp bed habitat regions."},"translated_abstract":"This bulletin is meant to be a guide to the fishes of the west-central coast of North America that commonly occur in kelp beds and adjacent areas. The fishes described are common species, and this report is not meant to include all species that occur in the kelp environment and adjacent zones. In all, 97 species are described; key identification features are given. Colors listed for each species refer to how that specimen would appear in the live and/or recently captured state; underwater behavioral characteristics are given wherever possible to aid the underwater diving enthusiast. Description of the kelp environment is given, which includes a brief explanation pertaining to the three major ecological zones within the kelp ecosystem. A brief explanation and description of the kelp bed flora is included, along with geographical considerations. The kelp environment as a habitat type for fishes is discussed; three habitat regions in the kelp bed are given special attention, these are: 1) the canopy, 2) intermediate regions, and 3) kelp bottom holdfast region. Accounts of each species of fish then follow which include identification, distribution, size, habitat habits, and life history inclusive of food and reproductive biology whenever available. Four appendix tables include listings of the organisms frequently observed by diving in the various kelp bed habitat regions.","internal_url":"https://www.academia.edu/32930345/Title_Fish_Bulletin_160_Observations_On_Fishes_Associated_With_Kelp_Beds_in_Southern_California","translated_internal_url":"","created_at":"2017-05-09T20:18:18.719-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":53063834,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063834/thumbnails/1.jpg","file_name":"Fish_Bulletin.pdf","download_url":"https://www.academia.edu/attachments/53063834/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Title_Fish_Bulletin_160_Observations_On.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063834/Fish_Bulletin-libre.pdf?1494386564=\u0026response-content-disposition=attachment%3B+filename%3DTitle_Fish_Bulletin_160_Observations_On.pdf\u0026Expires=1732985716\u0026Signature=WP9IUo5iORefygh-HC1U51tpHj7Uw~9N7CdiQpN4MjUVX~-X5QFLFVvTkNrYbBi1qDH1-nOV404u~8zevupABJ0uzlQs5mLoctCw-6eK4qcAYGn5ju31PvXnVVe67OfBkez8n2gTIiLMWd1TG7YMZfQkciCzcaIf~io~wdLW~cmPJ-NK1wVo63mBGnIrcEuiYUN04iLtEIuvHeKsscEU0dyPgtUhEK7RzH2D-jILcsFc7xeRDUaduJzDhNwKk-v8NbBZ-jQDizQ86CnFV2QoyBplpn5PF3ApUaMi~XILB0dpNBhBZBAHX51XXJGSVf~cJk-~aNmGUt1q3OlWS82KEQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Title_Fish_Bulletin_160_Observations_On_Fishes_Associated_With_Kelp_Beds_in_Southern_California","translated_slug":"","page_count":139,"language":"en","content_type":"Work","owner":{"id":33916837,"first_name":"Howard","middle_initials":"","last_name":"Feder","page_name":"HowardFeder","domain_name":"uaf","created_at":"2015-08-14T13:09:52.457-07:00","display_name":"Howard Feder","url":"https://uaf.academia.edu/HowardFeder"},"attachments":[{"id":53063834,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063834/thumbnails/1.jpg","file_name":"Fish_Bulletin.pdf","download_url":"https://www.academia.edu/attachments/53063834/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Title_Fish_Bulletin_160_Observations_On.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063834/Fish_Bulletin-libre.pdf?1494386564=\u0026response-content-disposition=attachment%3B+filename%3DTitle_Fish_Bulletin_160_Observations_On.pdf\u0026Expires=1732985716\u0026Signature=WP9IUo5iORefygh-HC1U51tpHj7Uw~9N7CdiQpN4MjUVX~-X5QFLFVvTkNrYbBi1qDH1-nOV404u~8zevupABJ0uzlQs5mLoctCw-6eK4qcAYGn5ju31PvXnVVe67OfBkez8n2gTIiLMWd1TG7YMZfQkciCzcaIf~io~wdLW~cmPJ-NK1wVo63mBGnIrcEuiYUN04iLtEIuvHeKsscEU0dyPgtUhEK7RzH2D-jILcsFc7xeRDUaduJzDhNwKk-v8NbBZ-jQDizQ86CnFV2QoyBplpn5PF3ApUaMi~XILB0dpNBhBZBAHX51XXJGSVf~cJk-~aNmGUt1q3OlWS82KEQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, 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="32930332"><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/32930332/Temporal_variability_of_benthic_communities_in_an_Alaskan_glacial_fjord_1971_2007"><img alt="Research paper thumbnail of Temporal variability of benthic communities in an Alaskan glacial fjord, 1971–2007" class="work-thumbnail" src="https://attachments.academia-assets.com/53063824/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/32930332/Temporal_variability_of_benthic_communities_in_an_Alaskan_glacial_fjord_1971_2007">Temporal variability of benthic communities in an Alaskan glacial fjord, 1971–2007</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Temporal trends of deep-subtidal macrofauna in Port Valdez, Alaska, were assessed with respect to...</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">Temporal trends of deep-subtidal macrofauna in Port Valdez, Alaska, were assessed with respect to multiple environmental stressors. Effects from a magnitude 9.2 earthquake in Prince William Sound, Alaska, 1964, were reflected in recolonization of the basin of the fjord, increased abundance and number of taxa over time, and moderately increased variability in abundance through 1990, stabilizing 26 years after the earthquake. Long-term climatic variability and local physical processes were important sources of spatial and temporal variability. Correlative evidence suggests that indirect effects of juvenile salmon from a shoreline salmon hatchery and deposition of adult salmon carcasses moderately enhanced deep-basin benthic communities. Effects on the deep benthos from a marine oil terminal were negligible. Overall, faunal trends deviated from the stability expected for benthic communities in other fjords. Physical characteristics of the fjord were important in mediating the effects of stressors and in delaying the readjustment process.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b04a4f3cc1ac3c4b7197089a2060e796" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063824,"asset_id":32930332,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063824/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930332"><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="32930332"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930332; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930332]").text(description); $(".js-view-count[data-work-id=32930332]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930332; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930332']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930332, 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: "b04a4f3cc1ac3c4b7197089a2060e796" } } $('.js-work-strip[data-work-id=32930332]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930332,"title":"Temporal variability of benthic communities in an Alaskan glacial fjord, 1971–2007","translated_title":"","metadata":{"abstract":"Temporal trends of deep-subtidal macrofauna in Port Valdez, Alaska, were assessed with respect to multiple environmental stressors. Effects from a magnitude 9.2 earthquake in Prince William Sound, Alaska, 1964, were reflected in recolonization of the basin of the fjord, increased abundance and number of taxa over time, and moderately increased variability in abundance through 1990, stabilizing 26 years after the earthquake. Long-term climatic variability and local physical processes were important sources of spatial and temporal variability. Correlative evidence suggests that indirect effects of juvenile salmon from a shoreline salmon hatchery and deposition of adult salmon carcasses moderately enhanced deep-basin benthic communities. Effects on the deep benthos from a marine oil terminal were negligible. Overall, faunal trends deviated from the stability expected for benthic communities in other fjords. Physical characteristics of the fjord were important in mediating the effects of stressors and in delaying the readjustment process."},"translated_abstract":"Temporal trends of deep-subtidal macrofauna in Port Valdez, Alaska, were assessed with respect to multiple environmental stressors. Effects from a magnitude 9.2 earthquake in Prince William Sound, Alaska, 1964, were reflected in recolonization of the basin of the fjord, increased abundance and number of taxa over time, and moderately increased variability in abundance through 1990, stabilizing 26 years after the earthquake. Long-term climatic variability and local physical processes were important sources of spatial and temporal variability. Correlative evidence suggests that indirect effects of juvenile salmon from a shoreline salmon hatchery and deposition of adult salmon carcasses moderately enhanced deep-basin benthic communities. Effects on the deep benthos from a marine oil terminal were negligible. Overall, faunal trends deviated from the stability expected for benthic communities in other fjords. 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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="32930305"><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/32930305/Trace_Element_and_Biotic_Changes_Following_a_Simulated_Oil_Spill_on_a_Mudflat_in_Port_Valdez_Alaska"><img alt="Research paper thumbnail of Trace Element and Biotic Changes Following a Simulated Oil Spill on a Mudflat in Port Valdez, Alaska" class="work-thumbnail" src="https://attachments.academia-assets.com/53063792/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/32930305/Trace_Element_and_Biotic_Changes_Following_a_Simulated_Oil_Spill_on_a_Mudflat_in_Port_Valdez_Alaska">Trace Element and Biotic Changes Following a Simulated Oil Spill on a Mudflat in Port Valdez, Alaska</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of ...</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 mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of Prudhoe Bay crude oil on metal chemistry and harpacticoid copepod abundance. Hydrocarbon concentrations were at background levels 30 days after final addition of oil. The short residence time of oil added to sediments is attributable to physical removal of oil by tides, low sediment permeability, and low affinity of hydrocarbons for peri-glacial clay surfaces. Elemental concentrations, except Si, were lower in oiled than in unoiled sediments. Elemental depletion in oil-impacted sediments is attributable to mobilization of metals from oxide/hydroxide sediment phases or to desorption from clay due to lowering of Eh-pH of sediments subsequent to oil addition. In oiled sediments, abundance of the harpacticoid cope-pods Harpacticus uniremis, Halectinosoma gothiceps, and Heterolaophonte sp. was similar to or higher than values within unoiled plots. The reasons for lack of dele-terious effects of oil on copepods in Port Valdez are not yet understood.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e13a55be6e6dbd07defb655e239b8c0c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063792,"asset_id":32930305,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063792/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930305"><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="32930305"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930305; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930305]").text(description); $(".js-view-count[data-work-id=32930305]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930305; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930305']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930305, 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: "e13a55be6e6dbd07defb655e239b8c0c" } } $('.js-work-strip[data-work-id=32930305]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930305,"title":"Trace Element and Biotic Changes Following a Simulated Oil Spill on a Mudflat in Port Valdez, Alaska","translated_title":"","metadata":{"abstract":"A mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of Prudhoe Bay crude oil on metal chemistry and harpacticoid copepod abundance. 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The reasons for lack of dele-terious effects of oil on copepods in Port Valdez are not yet understood."},"translated_abstract":"A mudflat in Port Valdez, Alaska, was examined to determine effects of experimental additions of Prudhoe Bay crude oil on metal chemistry and harpacticoid copepod abundance. Hydrocarbon concentrations were at background levels 30 days after final addition of oil. The short residence time of oil added to sediments is attributable to physical removal of oil by tides, low sediment permeability, and low affinity of hydrocarbons for peri-glacial clay surfaces. Elemental concentrations, except Si, were lower in oiled than in unoiled sediments. Elemental depletion in oil-impacted sediments is attributable to mobilization of metals from oxide/hydroxide sediment phases or to desorption from clay due to lowering of Eh-pH of sediments subsequent to oil addition. 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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="32930277"><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/32930277/The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill"><img alt="Research paper thumbnail of The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill" class="work-thumbnail" src="https://attachments.academia-assets.com/53063763/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/32930277/The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill">The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, a...</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 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, an assessment of the benthic macrofauna and associated environmental parameters at 40 and 100 m was made. Assessment of the biota and environmental data demonstrated patterns in deep benthic assemblages reflective of oceanographic conditions, as indicated by sediment differences, rather than EVOS toxicity. Comparison of polynnclear aromatic hydrocarbons (PAH) and 813C values in sediments between stations within the oil trajectory and reference stations outside of the trajectory showed no significant differences. This investigation uncovered no signals of disturbance 16 months after the EVOS. These results agree with conclusions of studies of intertidal and shallow subtidal regions following the EVOS that demonstrated disturbance effects decreasing with depth.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c7f02a93a4d1dde9143fd99f690f2584" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063763,"asset_id":32930277,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063763/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930277"><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="32930277"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930277; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930277]").text(description); $(".js-view-count[data-work-id=32930277]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930277; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930277']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930277, 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: "c7f02a93a4d1dde9143fd99f690f2584" } } $('.js-work-strip[data-work-id=32930277]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930277,"title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill","translated_title":"","metadata":{"abstract":"In 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, an assessment of the benthic macrofauna and associated environmental parameters at 40 and 100 m was made. Assessment of the biota and environmental data demonstrated patterns in deep benthic assemblages reflective of oceanographic conditions, as indicated by sediment differences, rather than EVOS toxicity. Comparison of polynnclear aromatic hydrocarbons (PAH) and 813C values in sediments between stations within the oil trajectory and reference stations outside of the trajectory showed no significant differences. This investigation uncovered no signals of disturbance 16 months after the EVOS. These results agree with conclusions of studies of intertidal and shallow subtidal regions following the EVOS that demonstrated disturbance effects decreasing with depth."},"translated_abstract":"In 1990, 16 months after the T/V Exxon Valdez oil spill (EVOS) in Prince William Sound, Alaska, an assessment of the benthic macrofauna and associated environmental parameters at 40 and 100 m was made. Assessment of the biota and environmental data demonstrated patterns in deep benthic assemblages reflective of oceanographic conditions, as indicated by sediment differences, rather than EVOS toxicity. Comparison of polynnclear aromatic hydrocarbons (PAH) and 813C values in sediments between stations within the oil trajectory and reference stations outside of the trajectory showed no significant differences. This investigation uncovered no signals of disturbance 16 months after the EVOS. These results agree with conclusions of studies of intertidal and shallow subtidal regions following the EVOS that demonstrated disturbance effects decreasing with depth.","internal_url":"https://www.academia.edu/32930277/The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill","translated_internal_url":"","created_at":"2017-05-09T20:00:13.147-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28854583,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":376400,"co_author_invite_id":null,"email":"a***d@alaska.edu","affiliation":"University of Alaska Fairbanks","display_order":1,"name":"Arny Blanchard","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"},{"id":28854584,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":1049512,"email":"f***r@ims.uaf.edu","display_order":2,"name":"Howard Feder","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"},{"id":28854585,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":1296847,"email":"a***b@ims.uaf.edu","display_order":4,"name":"Arny Blanchard","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"},{"id":28854586,"work_id":32930277,"tagging_user_id":33916837,"tagged_user_id":35006843,"co_author_invite_id":null,"email":"a***k@gmail.com","display_order":5,"name":"Arny Blanchard","title":"The Deep Benthos of Prince William Sound, Alaska, 16 Months After the Exxon Valdez Oil Spill"}],"downloadable_attachments":[{"id":53063763,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063763/thumbnails/1.jpg","file_name":"Feder_and_Blanchard_1998_MPB.pdf","download_url":"https://www.academia.edu/attachments/53063763/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Deep_Benthos_of_Prince_William_Sound.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063763/Feder_and_Blanchard_1998_MPB-libre.pdf?1494385328=\u0026response-content-disposition=attachment%3B+filename%3DThe_Deep_Benthos_of_Prince_William_Sound.pdf\u0026Expires=1732985716\u0026Signature=EYUZTzvAe7GdzIH6qJNcYotOHCKWywWUF~ulHWzv2a0lyXDLfVfYkkJvR8KgF4Ir58uzcb2XKG89ipnfzJ3iTn9e7OE6g213WPey3trLZU8zjw75yzUiXo1zzZ8pQ5Z8oAGFX-xyhP7CtTGtmy7eN33DWf~zYzkcUiV613A64Ul8ntIS0~8KeR~KijSbS172INREr1Tjmlz1vX2RWjjMTfNYznYI50gTkSTjNUKjdqGcpWDkcsvSd2VYFPTlL~IxWNK8mx2zSvm~Tp3xR-XtmQjKEHe3VEsAmCkmzRSbJwxdOpm0PPVyQXXrlXbt9Ahkap5ZINKwzC~IB4kN23-uRw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_Deep_Benthos_of_Prince_William_Sound_Alaska_16_Months_After_the_Exxon_Valdez_Oil_Spill","translated_slug":"","page_count":13,"language":"en","content_type":"Work","owner":{"id":33916837,"first_name":"Howard","middle_initials":"","last_name":"Feder","page_name":"HowardFeder","domain_name":"uaf","created_at":"2015-08-14T13:09:52.457-07:00","display_name":"Howard Feder","url":"https://uaf.academia.edu/HowardFeder"},"attachments":[{"id":53063763,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063763/thumbnails/1.jpg","file_name":"Feder_and_Blanchard_1998_MPB.pdf","download_url":"https://www.academia.edu/attachments/53063763/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_Deep_Benthos_of_Prince_William_Sound.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063763/Feder_and_Blanchard_1998_MPB-libre.pdf?1494385328=\u0026response-content-disposition=attachment%3B+filename%3DThe_Deep_Benthos_of_Prince_William_Sound.pdf\u0026Expires=1732985716\u0026Signature=EYUZTzvAe7GdzIH6qJNcYotOHCKWywWUF~ulHWzv2a0lyXDLfVfYkkJvR8KgF4Ir58uzcb2XKG89ipnfzJ3iTn9e7OE6g213WPey3trLZU8zjw75yzUiXo1zzZ8pQ5Z8oAGFX-xyhP7CtTGtmy7eN33DWf~zYzkcUiV613A64Ul8ntIS0~8KeR~KijSbS172INREr1Tjmlz1vX2RWjjMTfNYznYI50gTkSTjNUKjdqGcpWDkcsvSd2VYFPTlL~IxWNK8mx2zSvm~Tp3xR-XtmQjKEHe3VEsAmCkmzRSbJwxdOpm0PPVyQXXrlXbt9Ahkap5ZINKwzC~IB4kN23-uRw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, 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="32930268"><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/32930268/The_northeastern_Chukchi_Sea_benthos_environmental_interactions"><img alt="Research paper thumbnail of The northeastern Chukchi Sea: benthos-environmental interactions" class="work-thumbnail" src="https://attachments.academia-assets.com/53063752/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/32930268/The_northeastern_Chukchi_Sea_benthos_environmental_interactions">The northeastern Chukchi Sea: benthos-environmental interactions</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to...</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">Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to determine factors influencing faunal distribution. Four taxon-abundance-based benthic station groups were identified by cluster analysis and ordination techniques. These groups are explained, using stepwise multiple discriminant analysis, by the gravel-sand-mud and water content of bottom sediments, and the organic carbon/nitrogen (OC/N) ratio. In contrast to previous benthic investigations in the northeastern Bering and southeastern Chukchi Seas, faunal diversity between inshore and offshore regions in our study area were not related to differences in sediment sorting. Instead, regional diversity differences in the northeastern Chukchi Sea were related to greater environmental stresses (e.g. ice gouging, wave-current action, marine-mammal feeding activities) inshore than offshore. The presence of a high benthic biomass north of Icy Cape in the vicinity of Point Franklin and seaward of a hydrographic front is presumably related to an enhanced local depositional flux of particulate organic carbon (POC) in the area. We postulate that POC-rich waters derived from the northern Bering and northwestern Chukchi Seas extend to our study area and the flux of the entrained POC provides a persistent source of carbon to sustain the high benthic biomass. Annual POC enrichment of the coastal region north of Icy Cape is reflected by the great abundance of amphipods and other invertebrates present there and the concentration in summer of walrus Odobenus rosmarus djvergens and gray whales Eschrichtius robustus that feed on these invertebrates. This study demonstrates that there can be high standing stocks of benthos in arctic regions with relatively low annual primary production if local carbon is augmented by POC advected from highly productive areas.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="4a1fd1b25a0315943ee32037743206d6" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063752,"asset_id":32930268,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063752/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930268"><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="32930268"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930268; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930268]").text(description); $(".js-view-count[data-work-id=32930268]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930268; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930268']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930268, 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: "4a1fd1b25a0315943ee32037743206d6" } } $('.js-work-strip[data-work-id=32930268]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930268,"title":"The northeastern Chukchi Sea: benthos-environmental interactions","translated_title":"","metadata":{"abstract":"Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to determine factors influencing faunal distribution. Four taxon-abundance-based benthic station groups were identified by cluster analysis and ordination techniques. These groups are explained, using stepwise multiple discriminant analysis, by the gravel-sand-mud and water content of bottom sediments, and the organic carbon/nitrogen (OC/N) ratio. In contrast to previous benthic investigations in the northeastern Bering and southeastern Chukchi Seas, faunal diversity between inshore and offshore regions in our study area were not related to differences in sediment sorting. Instead, regional diversity differences in the northeastern Chukchi Sea were related to greater environmental stresses (e.g. ice gouging, wave-current action, marine-mammal feeding activities) inshore than offshore. The presence of a high benthic biomass north of Icy Cape in the vicinity of Point Franklin and seaward of a hydrographic front is presumably related to an enhanced local depositional flux of particulate organic carbon (POC) in the area. We postulate that POC-rich waters derived from the northern Bering and northwestern Chukchi Seas extend to our study area and the flux of the entrained POC provides a persistent source of carbon to sustain the high benthic biomass. Annual POC enrichment of the coastal region north of Icy Cape is reflected by the great abundance of amphipods and other invertebrates present there and the concentration in summer of walrus Odobenus rosmarus djvergens and gray whales Eschrichtius robustus that feed on these invertebrates. This study demonstrates that there can be high standing stocks of benthos in arctic regions with relatively low annual primary production if local carbon is augmented by POC advected from highly productive areas."},"translated_abstract":"Benthic faunal abundance, diversity, and biomass were examined in the northeastern Chukchi Sea to determine factors influencing faunal distribution. Four taxon-abundance-based benthic station groups were identified by cluster analysis and ordination techniques. These groups are explained, using stepwise multiple discriminant analysis, by the gravel-sand-mud and water content of bottom sediments, and the organic carbon/nitrogen (OC/N) ratio. In contrast to previous benthic investigations in the northeastern Bering and southeastern Chukchi Seas, faunal diversity between inshore and offshore regions in our study area were not related to differences in sediment sorting. Instead, regional diversity differences in the northeastern Chukchi Sea were related to greater environmental stresses (e.g. ice gouging, wave-current action, marine-mammal feeding activities) inshore than offshore. The presence of a high benthic biomass north of Icy Cape in the vicinity of Point Franklin and seaward of a hydrographic front is presumably related to an enhanced local depositional flux of particulate organic carbon (POC) in the area. We postulate that POC-rich waters derived from the northern Bering and northwestern Chukchi Seas extend to our study area and the flux of the entrained POC provides a persistent source of carbon to sustain the high benthic biomass. Annual POC enrichment of the coastal region north of Icy Cape is reflected by the great abundance of amphipods and other invertebrates present there and the concentration in summer of walrus Odobenus rosmarus djvergens and gray whales Eschrichtius robustus that feed on these invertebrates. This study demonstrates that there can be high standing stocks of benthos in arctic regions with relatively low annual primary production if local carbon is augmented by POC advected from highly productive areas.","internal_url":"https://www.academia.edu/32930268/The_northeastern_Chukchi_Sea_benthos_environmental_interactions","translated_internal_url":"","created_at":"2017-05-09T19:57:50.828-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":33916837,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28854578,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":32942776,"co_author_invite_id":null,"email":"s***u@alaska.edu","display_order":1,"name":"Sathy Naidu","title":"The northeastern Chukchi Sea: benthos-environmental interactions"},{"id":28854579,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":1049512,"email":"f***r@ims.uaf.edu","display_order":2,"name":"Howard Feder","title":"The northeastern Chukchi Sea: benthos-environmental interactions"},{"id":28854580,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":null,"co_author_invite_id":3706439,"email":"j***t@ims.alaska.edu","display_order":4,"name":"Stephen Jewett","title":"The northeastern Chukchi Sea: benthos-environmental interactions"},{"id":28854581,"work_id":32930268,"tagging_user_id":33916837,"tagged_user_id":32439470,"co_author_invite_id":null,"email":"S***t@alaska.edu","display_order":5,"name":"Stephen Jewett","title":"The northeastern Chukchi Sea: benthos-environmental interactions"}],"downloadable_attachments":[{"id":53063752,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063752/thumbnails/1.jpg","file_name":"feder_northeast_chucki_sea.pdf","download_url":"https://www.academia.edu/attachments/53063752/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_northeastern_Chukchi_Sea_benthos_env.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063752/feder_northeast_chucki_sea-libre.pdf?1494385178=\u0026response-content-disposition=attachment%3B+filename%3DThe_northeastern_Chukchi_Sea_benthos_env.pdf\u0026Expires=1732985716\u0026Signature=glMiCEKeEMCLyDj36UElJvDIZ0IEFgcJV2Y2t0EJmtRnKR~MVYtQzK0uhapxxv6ygcJztJ9mtvPjOdiuptWWmyEdEBEnh~L7yLJDmLy9SbfCf65pUMiWj--BgsXI6zgbB192lR4ic3r4j~tuO6z8xBAo345nSsDJHZ5B9zBEq15HqWF3qaMgZGaHEWz01GlNb9gUEP8G3uU1q746Mj0ZTKP4mSoVdPAb99dhW-BTUatHGa1v-uaC~o2bMFfoqt7DfapuzEpP-yRU-JQKgiiC7tPyXkMLmCxQFonFWky219Mbv2q6dXB35Tz~6q2IGFucSm1b3fb9a8ZK9w9ZNA0QuA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_northeastern_Chukchi_Sea_benthos_environmental_interactions","translated_slug":"","page_count":20,"language":"en","content_type":"Work","owner":{"id":33916837,"first_name":"Howard","middle_initials":"","last_name":"Feder","page_name":"HowardFeder","domain_name":"uaf","created_at":"2015-08-14T13:09:52.457-07:00","display_name":"Howard Feder","url":"https://uaf.academia.edu/HowardFeder"},"attachments":[{"id":53063752,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53063752/thumbnails/1.jpg","file_name":"feder_northeast_chucki_sea.pdf","download_url":"https://www.academia.edu/attachments/53063752/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_northeastern_Chukchi_Sea_benthos_env.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53063752/feder_northeast_chucki_sea-libre.pdf?1494385178=\u0026response-content-disposition=attachment%3B+filename%3DThe_northeastern_Chukchi_Sea_benthos_env.pdf\u0026Expires=1732985716\u0026Signature=glMiCEKeEMCLyDj36UElJvDIZ0IEFgcJV2Y2t0EJmtRnKR~MVYtQzK0uhapxxv6ygcJztJ9mtvPjOdiuptWWmyEdEBEnh~L7yLJDmLy9SbfCf65pUMiWj--BgsXI6zgbB192lR4ic3r4j~tuO6z8xBAo345nSsDJHZ5B9zBEq15HqWF3qaMgZGaHEWz01GlNb9gUEP8G3uU1q746Mj0ZTKP4mSoVdPAb99dhW-BTUatHGa1v-uaC~o2bMFfoqt7DfapuzEpP-yRU-JQKgiiC7tPyXkMLmCxQFonFWky219Mbv2q6dXB35Tz~6q2IGFucSm1b3fb9a8ZK9w9ZNA0QuA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, 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="32930264"><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/32930264/Benthic_food_web_structure_in_the_southeastern_Chukchi_Sea_an_assessment_using_d_13_C_and_d_15_N_analyses"><img alt="Research paper thumbnail of Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N analyses" class="work-thumbnail" src="https://attachments.academia-assets.com/53063748/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/32930264/Benthic_food_web_structure_in_the_southeastern_Chukchi_Sea_an_assessment_using_d_13_C_and_d_15_N_analyses">Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N analyses</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://uaf.academia.edu/HowardFeder">Howard Feder</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/StephenJewett">Stephen Jewett</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomas...</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 benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomass resulting from settlement of a large proportion of seasonal phytoplankton under highly nutritious offshore Bering Shelf Anadyr Water (BSAW). In contrast, inshore Alaska Coastal Water (ACW) is much less productive. Yet the Chukchi Bight and Kotzebue Sound, located under ACW in the southeastern Chukchi Sea, contain a substantial faunal abundance and biomass of invertebrates, fishes and marine mammals. We examined food web structure to gain an understanding of how a relatively rich benthic fauna with a high biomass can be supported under ACW with a supposedly low flux of carbon to the benthos. We measured stable isotope (d 13 C and d 15 N) values of selected organisms (from zooplankton to fishes) as markers of food sources and trophic position to compare fauna on the shelf under BSAW with that in the Chukchi Bight and Kotzebue Sound under ACW. Relative isotope position of organisms in all three regions was similar, even though some pelagic species within the Sound were depleted in d 13 C compared to the other regions. We attribute the depletion to the influence of terrestrially derived carbon. We suggest that the hydrodynamics along an oceanic front between the Chuk-chi Shelf and the Chukchi Bight support the advection of nutrient-rich POC into the Bight and Sound as additional food sources to local production. We conclude that local conditions and multiple POC sources in the Bight and Sound support the substantial population of benthic invertebrates and the fishes, seabirds, and marine mammals that feed on them. Keywords Arctic Á Chukchi Sea Á Kotzebue Sound Á Benthos Á POC Á Stable isotopes Á Marine food web</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="25214c0f9eb13a7d8c82b2151ece297b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063748,"asset_id":32930264,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063748/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930264"><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="32930264"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930264; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930264]").text(description); $(".js-view-count[data-work-id=32930264]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930264; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930264']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930264, 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: "25214c0f9eb13a7d8c82b2151ece297b" } } $('.js-work-strip[data-work-id=32930264]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930264,"title":"Benthic food web structure in the southeastern Chukchi Sea: an assessment using d 13 C and d 15 N analyses","translated_title":"","metadata":{"abstract":"The benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomass resulting from settlement of a large proportion of seasonal phytoplankton under highly nutritious offshore Bering Shelf Anadyr Water (BSAW). In contrast, inshore Alaska Coastal Water (ACW) is much less productive. Yet the Chukchi Bight and Kotzebue Sound, located under ACW in the southeastern Chukchi Sea, contain a substantial faunal abundance and biomass of invertebrates, fishes and marine mammals. We examined food web structure to gain an understanding of how a relatively rich benthic fauna with a high biomass can be supported under ACW with a supposedly low flux of carbon to the benthos. We measured stable isotope (d 13 C and d 15 N) values of selected organisms (from zooplankton to fishes) as markers of food sources and trophic position to compare fauna on the shelf under BSAW with that in the Chukchi Bight and Kotzebue Sound under ACW. Relative isotope position of organisms in all three regions was similar, even though some pelagic species within the Sound were depleted in d 13 C compared to the other regions. We attribute the depletion to the influence of terrestrially derived carbon. We suggest that the hydrodynamics along an oceanic front between the Chuk-chi Shelf and the Chukchi Bight support the advection of nutrient-rich POC into the Bight and Sound as additional food sources to local production. We conclude that local conditions and multiple POC sources in the Bight and Sound support the substantial population of benthic invertebrates and the fishes, seabirds, and marine mammals that feed on them. Keywords Arctic Á Chukchi Sea Á Kotzebue Sound Á Benthos Á POC Á Stable isotopes Á Marine food web"},"translated_abstract":"The benthos of the southeastern Chukchi Sea shelf is typified by high faunal abundance and biomass resulting from settlement of a large proportion of seasonal phytoplankton under highly nutritious offshore Bering Shelf Anadyr Water (BSAW). In contrast, inshore Alaska Coastal Water (ACW) is much less productive. 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We suggest that the hydrodynamics along an oceanic front between the Chuk-chi Shelf and the Chukchi Bight support the advection of nutrient-rich POC into the Bight and Sound as additional food sources to local production. We conclude that local conditions and multiple POC sources in the Bight and Sound support the substantial population of benthic invertebrates and the fishes, seabirds, and marine mammals that feed on them. 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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="32930259"><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/32930259/Abiotic_Biological_Interactions_in_Coastal_Marine_Communities_Insights_from_an_Alaskan_Fjord"><img alt="Research paper thumbnail of Abiotic/Biological Interactions in Coastal Marine Communities: Insights from an Alaskan Fjord" class="work-thumbnail" src="https://attachments.academia-assets.com/53063744/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/32930259/Abiotic_Biological_Interactions_in_Coastal_Marine_Communities_Insights_from_an_Alaskan_Fjord">Abiotic/Biological Interactions in Coastal Marine Communities: Insights from an Alaskan Fjord</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Interactions among multi-scale coastal marine ecosystem processes can be expected to play large r...</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">Interactions among multi-scale coastal marine ecosystem processes can be expected to play large roles in and interact with biological processes as stresses increase, potentially allowing interfering processes (including biological interactions) to become more prevalent. Retrospective analyses of intertidal (1988–1992) and subtidal (1971–2012) species compositions from a long-term ecological research program in Port Valdez, Alaska evaluated associations between benthic community structure and physical conditions to better understand interactions between regional to local processes on flora and fauna. Low salinity, habitat structure (varying from mudflats to rocky shores over a distance of <18 km), and suspended sediments contributed to intertidal community structure via elimination of predators from low-salinity prey refugia. Subtidal communities demonstrate adjustments by macrofauna to sedi-mentation with smaller, disturbance-tolerant fauna towards the head of the fjord as well as effects from depth-related covari-ates. Shared ecological processes result in comparable community trends in subtidal and intertidal habitats among subarctic and arctic fjords and similarly among coastal environments of the North Pacific. Control exerted by interactions among climatic, oceanographic, and local processes interacting with biota contributes to the direction and length of recovery from disturbance events and environmental changes. Feedbacks, mediation of recovery by additional processes, and strengths of interactions also play important roles in determining interaction outcomes. Interactions among local, regional, and global-scale processes may become critical sources of change as global ecosystem transitions through new climate states.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="316b89a8ac01059d27f48a1a441a1bb1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53063744,"asset_id":32930259,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53063744/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="32930259"><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="32930259"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32930259; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32930259]").text(description); $(".js-view-count[data-work-id=32930259]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32930259; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32930259']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32930259, 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: "316b89a8ac01059d27f48a1a441a1bb1" } } $('.js-work-strip[data-work-id=32930259]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32930259,"title":"Abiotic/Biological Interactions in Coastal Marine Communities: Insights from an Alaskan Fjord","translated_title":"","metadata":{"abstract":"Interactions among multi-scale coastal marine ecosystem processes can be expected to play large roles in and interact with biological processes as stresses increase, potentially allowing interfering processes (including biological interactions) to become more prevalent. Retrospective analyses of intertidal (1988–1992) and subtidal (1971–2012) species compositions from a long-term ecological research program in Port Valdez, Alaska evaluated associations between benthic community structure and physical conditions to better understand interactions between regional to local processes on flora and fauna. Low salinity, habitat structure (varying from mudflats to rocky shores over a distance of \u003c18 km), and suspended sediments contributed to intertidal community structure via elimination of predators from low-salinity prey refugia. Subtidal communities demonstrate adjustments by macrofauna to sedi-mentation with smaller, disturbance-tolerant fauna towards the head of the fjord as well as effects from depth-related covari-ates. Shared ecological processes result in comparable community trends in subtidal and intertidal habitats among subarctic and arctic fjords and similarly among coastal environments of the North Pacific. Control exerted by interactions among climatic, oceanographic, and local processes interacting with biota contributes to the direction and length of recovery from disturbance events and environmental changes. Feedbacks, mediation of recovery by additional processes, and strengths of interactions also play important roles in determining interaction outcomes. Interactions among local, regional, and global-scale processes may become critical sources of change as global ecosystem transitions through new climate states."},"translated_abstract":"Interactions among multi-scale coastal marine ecosystem processes can be expected to play large roles in and interact with biological processes as stresses increase, potentially allowing interfering processes (including biological interactions) to become more prevalent. Retrospective analyses of intertidal (1988–1992) and subtidal (1971–2012) species compositions from a long-term ecological research program in Port Valdez, Alaska evaluated associations between benthic community structure and physical conditions to better understand interactions between regional to local processes on flora and fauna. Low salinity, habitat structure (varying from mudflats to rocky shores over a distance of \u003c18 km), and suspended sediments contributed to intertidal community structure via elimination of predators from low-salinity prey refugia. Subtidal communities demonstrate adjustments by macrofauna to sedi-mentation with smaller, disturbance-tolerant fauna towards the head of the fjord as well as effects from depth-related covari-ates. Shared ecological processes result in comparable community trends in subtidal and intertidal habitats among subarctic and arctic fjords and similarly among coastal environments of the North Pacific. Control exerted by interactions among climatic, oceanographic, and local processes interacting with biota contributes to the direction and length of recovery from disturbance events and environmental changes. Feedbacks, mediation of recovery by additional processes, and strengths of interactions also play important roles in determining interaction outcomes. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="29223827"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/29223827/Growth_and_predation_by_the_ochre_sea_star_Pisaster_ochraceus_Brandt_in_Monterey_Bay_California"><img alt="Research paper thumbnail of Growth and predation by the ochre sea star, Pisaster ochraceus (Brandt), in Monterey Bay, California" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/29223827/Growth_and_predation_by_the_ochre_sea_star_Pisaster_ochraceus_Brandt_in_Monterey_Bay_California">Growth and predation by the ochre sea star, Pisaster ochraceus (Brandt), in Monterey Bay, California</a></div><div class="wp-workCard_item"><span>Ophelia</span><span>, 1970</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="29223827"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="29223827"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 29223827; 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V. Biology of the dominant soft-bottom epifauna and their interaction with the infauna" 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/29223825/The_benthic_ecology_of_Loch_Linnhe_and_Loch_Eil_a_sea_loch_system_on_the_west_coast_of_Scotland_V_Biology_of_the_dominant_soft_bottom_epifauna_and_their_interaction_with_the_infauna">The benthic ecology of Loch Linnhe and Loch Eil, a sea-loch system on the west coast of Scotland. V. Biology of the dominant soft-bottom epifauna and their interaction with the infauna</a></div><div class="wp-workCard_item"><span>Journal of Experimental Marine Biology and Ecology</span><span>, 1988</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... Ecol., 1988, Vol. ... koreni 2 5 Fibres 29 78 Trichobranchidae 1 3 Sediment 28 76 Unidentifie...</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">... Ecol., 1988, Vol. ... koreni 2 5 Fibres 29 78 Trichobranchidae 1 3 Sediment 28 76 Unidentified Polychaeta 18 49 Plant tissue 19 51 Annelida (Oligochaeta) Tubi coides benedeni 1 3 TABLE IVb Total number and per ... 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Foster</a></div><div class="wp-workCard_item"><span>ARCTIC</span><span>, 1992</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="29223824"><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="29223824"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 29223824; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=29223824]").text(description); $(".js-view-count[data-work-id=29223824]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 29223824; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='29223824']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 29223824, 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" } } $('.js-work-strip[data-work-id=29223824]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":29223824,"title":"Intertidal Bivalves. 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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="25707476"><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/25707476/Assessment_of_the_benthic_environment_following_offshore_placer_gold_mining_in_the_northeastern_Bering_Sea"><img alt="Research paper thumbnail of Assessment of the benthic environment following offshore placer gold mining in the northeastern Bering Sea" class="work-thumbnail" src="https://attachments.academia-assets.com/46053005/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/25707476/Assessment_of_the_benthic_environment_following_offshore_placer_gold_mining_in_the_northeastern_Bering_Sea">Assessment of the benthic environment following offshore placer gold mining in the northeastern Bering Sea</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://uaf.academia.edu/HowardFeder">Howard Feder</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/StephenJewett">Stephen Jewett</a></span></div><div class="wp-workCard_item"><span>Marine Environmental Research</span><span>, Aug 1, 1999</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="41d4faed69a67bd9df7a27b33da9fc5e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46053005,"asset_id":25707476,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46053005/download_file?st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&st=MTczMjk4MjExNiw4LjIyMi4yMDguMTQ2&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="25707476"><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="25707476"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 25707476; 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