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$('body').addClass('profile-viewed-by-owner'); } $socialProfiles = []</script><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://sevin.academia.edu/OlgaKrylovich","location":"/OlgaKrylovich","scheme":"https","host":"sevin.academia.edu","port":null,"pathname":"/OlgaKrylovich","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="ProfileCheckPaperUpdate" data-props="{}" data-trace="false" data-dom-id="ProfileCheckPaperUpdate-react-component-2b08664b-c13b-4d3d-8518-b581aac0302d"></div> <div id="ProfileCheckPaperUpdate-react-component-2b08664b-c13b-4d3d-8518-b581aac0302d"></div> <div class="DesignSystem"><div class="onsite-ping" id="onsite-ping"></div></div><div class="profile-user-info DesignSystem"><div class="social-profile-container"><div class="left-panel-container"><div 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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 Olga Krylovich</h3></div><div class="js-work-strip profile--work_container" data-work-id="44611111"><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/44611111/Holocene_Dynamics_of_Invertebrate_Fauna_in_the_Littoral_Zone_of_Adak_the_Aleutian_Islands_According_to_Archaeozoological_Data"><img alt="Research paper thumbnail of Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data" class="work-thumbnail" src="https://attachments.academia-assets.com/65075874/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/44611111/Holocene_Dynamics_of_Invertebrate_Fauna_in_the_Littoral_Zone_of_Adak_the_Aleutian_Islands_According_to_Archaeozoological_Data">Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data</a></div><div class="wp-workCard_item"><span>Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data</span><span>, 2009</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak Is...</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">Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak<br />Island have shown that the faunistic composition of invertebrates in the study area had not changed significantly<br />during the Late Holocene. The traditional mode of natural resource use by the ancient Aleuts had no impact on<br />the abundance of valuable species and biodiversity in general. Changes in the temperature regime were found<br />to have taken place in the history of deposit formation. The period from the 8th to the mid-11th century was<br />relatively cold. Climate warming took place between the mid-11th and the mid-12th centuries and between the<br />mid-16th and the 19th centuries, with an intervening cooling period (from the mid-12th to the mid-16th century).<br />This cooling was most distinct between the 15th and the mid-16th centuries.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a830e8bc4838574cc1b545a2bce4cb7e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":65075874,"asset_id":44611111,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/65075874/download_file?st=MTczMjUyOTk3Nyw4LjIyMi4yMDguMTQ2&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="44611111"><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="44611111"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 44611111; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=44611111]").text(description); $(".js-view-count[data-work-id=44611111]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 44611111; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='44611111']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 44611111, 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: "a830e8bc4838574cc1b545a2bce4cb7e" } } $('.js-work-strip[data-work-id=44611111]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":44611111,"title":"Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data","translated_title":"","metadata":{"doi":"10.1134/s106741360902009x","abstract":"Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak\nIsland have shown that the faunistic composition of invertebrates in the study area had not changed significantly\nduring the Late Holocene. 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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="32946266"><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/32946266/The_Marine_Radiocarbon_Reservoir_Effect_on_Adak_Island_Central_Aleutian_Islands_Alaska"><img alt="Research paper thumbnail of The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32946266/The_Marine_Radiocarbon_Reservoir_Effect_on_Adak_Island_Central_Aleutian_Islands_Alaska">The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska</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://fukuoka-u.academia.edu/MitsuruOkuno">Mitsuru Okuno</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/ArkadySavinetsky">Arkady Savinetsky</a></span></div><div class="wp-workCard_item"><span>Radiocarbon</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed ...</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">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.</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="32946266"><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="32946266"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32946266; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32946266]").text(description); $(".js-view-count[data-work-id=32946266]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32946266; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32946266']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32946266, 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" } } $('.js-work-strip[data-work-id=32946266]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32946266,"title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska","translated_title":"","metadata":{"abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Radiocarbon"},"translated_abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. 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Results of Preliminary Stable Isotopes Analysis" class="work-thumbnail" src="https://attachments.academia-assets.com/42669601/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/21946219/Hunting_Impacts_on_the_Sea_Otter_Enhydra_lutris_Population_in_Clam_Lagoon_Adak_Island_Aleutian_Islands_7_000_Years_Ago_Results_of_Preliminary_Stable_Isotopes_Analysis">Hunting Impacts on the Sea Otter ( Enhydra lutris ) Population in Clam Lagoon (Adak Island, Aleutian Islands) 7,000 Years Ago? Results of Preliminary Stable Isotopes Analysis</a></div><div class="wp-workCard_item"><span>The Journal of Island and Coastal Archaeology</span><span>, 2011</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="dfd8ca2122de9d9536ecd86cf4b2b3d4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":42669601,"asset_id":21946219,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/42669601/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="21946219"><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="21946219"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 21946219; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=21946219]").text(description); $(".js-view-count[data-work-id=21946219]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 21946219; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='21946219']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 21946219, 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: "dfd8ca2122de9d9536ecd86cf4b2b3d4" } } $('.js-work-strip[data-work-id=21946219]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":21946219,"title":"Hunting Impacts on the Sea Otter ( Enhydra lutris ) Population in Clam Lagoon (Adak Island, Aleutian Islands) 7,000 Years Ago? 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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="18149495"><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/18149495/Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material"><img alt="Research paper thumbnail of Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material" class="work-thumbnail" src="https://attachments.academia-assets.com/39901302/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/18149495/Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material">Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material</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://sevin.academia.edu/ArkadySavinetsky">Arkady Savinetsky</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MityaVasyukov">Mitya Vasyukov</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/BulatKhasanov">Bulat Khasanov</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and ni...</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 paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and nitrogen isotope composition (ratio of 15N/14N) for taxonomic diagnostics of animal bone remains from archaeological sites and other ancient deposits. The world literature pertaining to the use of stable-isotope analysis (SIA) in animal trophic ecology and methodological difficulties of work with subfossil material are reviewed. Several particular cases show a successful application of SIA for taxonomic identification of the archaeozoological remains, especially bones of brown and polar bears, large sea mammals and a few species of Anseriformes.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bfeb4d7c4f831eed00b727894e95ae2c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39901302,"asset_id":18149495,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39901302/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="18149495"><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="18149495"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 18149495; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=18149495]").text(description); $(".js-view-count[data-work-id=18149495]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 18149495; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='18149495']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 18149495, 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: "bfeb4d7c4f831eed00b727894e95ae2c" } } $('.js-work-strip[data-work-id=18149495]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":18149495,"title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material","translated_title":"","metadata":{"abstract":"The paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and nitrogen isotope composition (ratio of 15N/14N) for taxonomic diagnostics of animal bone remains from archaeological sites and other ancient deposits. The world literature pertaining to the use of stable-isotope analysis (SIA) in animal trophic ecology and methodological difficulties of work with subfossil material are reviewed. Several particular cases show a successful application of SIA for taxonomic identification of the archaeozoological remains, especially bones of brown and polar bears, large sea mammals and a few species of Anseriformes."},"translated_abstract":"The paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and nitrogen isotope composition (ratio of 15N/14N) for taxonomic diagnostics of animal bone remains from archaeological sites and other ancient deposits. The world literature pertaining to the use of stable-isotope analysis (SIA) in animal trophic ecology and methodological difficulties of work with subfossil material are reviewed. Several particular cases show a successful application of SIA for taxonomic identification of the archaeozoological remains, especially bones of brown and polar bears, large sea mammals and a few species of Anseriformes.","internal_url":"https://www.academia.edu/18149495/Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material","translated_internal_url":"","created_at":"2015-11-11T06:34:33.170-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":9465427,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":0,"name":"Arkady Savinetsky","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465428,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":38248084,"co_author_invite_id":2154372,"email":"t***6@gmail.com","display_order":4194304,"name":"Mitya Vasyukov","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465429,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":4753710,"co_author_invite_id":null,"email":"b***k@gmail.com","affiliation":"Severtsov Institute of ecology and evolution","display_order":6291456,"name":"Bulat Khasanov","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465430,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":null,"co_author_invite_id":1187273,"email":"a***v@mail.ru","display_order":7340032,"name":"Alexei Tiunov","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465431,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":null,"co_author_invite_id":2154373,"email":"g***k@gmail.com","display_order":7864320,"name":"Ekaterina Gorlova","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"}],"downloadable_attachments":[{"id":39901302,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39901302/thumbnails/1.jpg","file_name":"Gorlova_et_al-2015.pdf","download_url":"https://www.academia.edu/attachments/39901302/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stable_Isotope_Analysis_as_a_Method_of_T.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39901302/Gorlova_et_al-2015-libre.pdf?1447253359=\u0026response-content-disposition=attachment%3B+filename%3DStable_Isotope_Analysis_as_a_Method_of_T.pdf\u0026Expires=1732533578\u0026Signature=X-VlwbBra4j7S828BcQbxlh1296SjQVh7~0TXdaWlmpmJnLZTsaIxUZuhaqTKFh4cEOewDwzbGe42jAFjoQwZRvagHDj24dtl-7u3R7potxUDr5DPgdeWLjD4GA~oNNcRwl-lm~xugi3Ny3Y1F0fG8KqExCCKBrWcGj~M5JSQZ8nn0DumJGA2TesN4V2t9yEAGdVq3OWDwX4rAwNQ05PNECmWShZusOBKMqoIYMjEmQovsoASvQzV7iuq-TZ5FXo5TVgD3hG10eaDqeoBHJEWv0gZ7YFUcyvPgfAAnC0pvITefTut5WsHS87M-xklvzrU7~ti4GG-nPOq6lVulyfbQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material","translated_slug":"","page_count":12,"language":"en","content_type":"Work","owner":{"id":36817796,"first_name":"Olga","middle_initials":null,"last_name":"Krylovich","page_name":"OlgaKrylovich","domain_name":"sevin","created_at":"2015-10-23T07:14:19.517-07:00","display_name":"Olga Krylovich","url":"https://sevin.academia.edu/OlgaKrylovich"},"attachments":[{"id":39901302,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39901302/thumbnails/1.jpg","file_name":"Gorlova_et_al-2015.pdf","download_url":"https://www.academia.edu/attachments/39901302/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stable_Isotope_Analysis_as_a_Method_of_T.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39901302/Gorlova_et_al-2015-libre.pdf?1447253359=\u0026response-content-disposition=attachment%3B+filename%3DStable_Isotope_Analysis_as_a_Method_of_T.pdf\u0026Expires=1732533578\u0026Signature=X-VlwbBra4j7S828BcQbxlh1296SjQVh7~0TXdaWlmpmJnLZTsaIxUZuhaqTKFh4cEOewDwzbGe42jAFjoQwZRvagHDj24dtl-7u3R7potxUDr5DPgdeWLjD4GA~oNNcRwl-lm~xugi3Ny3Y1F0fG8KqExCCKBrWcGj~M5JSQZ8nn0DumJGA2TesN4V2t9yEAGdVq3OWDwX4rAwNQ05PNECmWShZusOBKMqoIYMjEmQovsoASvQzV7iuq-TZ5FXo5TVgD3hG10eaDqeoBHJEWv0gZ7YFUcyvPgfAAnC0pvITefTut5WsHS87M-xklvzrU7~ti4GG-nPOq6lVulyfbQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1421,"name":"Stable isotope ecology","url":"https://www.academia.edu/Documents/in/Stable_isotope_ecology"}],"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="17793399"><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/17793399/Holocene_hyrax_dung_deposits_in_the"><img alt="Research paper thumbnail of Holocene hyrax dung deposits in the" class="work-thumbnail" src="https://attachments.academia-assets.com/39713918/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/17793399/Holocene_hyrax_dung_deposits_in_the">Holocene hyrax dung deposits in the</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits f...</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 results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock<br />shelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits<br />accumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays,<br />respectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP)<br />correlate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP)<br />(15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas<br />event (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid<br />communities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000<br />(cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was<br />interrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000<br />years was observed. Presumably the first traces of human activities in this area can be shown for up<br />about 2500 (cal) years BP.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7c93a49439af1526ec5d6473580b2b56" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39713918,"asset_id":17793399,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39713918/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="17793399"><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="17793399"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17793399; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17793399]").text(description); $(".js-view-count[data-work-id=17793399]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17793399; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17793399']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17793399, 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: "7c93a49439af1526ec5d6473580b2b56" } } $('.js-work-strip[data-work-id=17793399]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17793399,"title":"Holocene hyrax dung deposits in the","translated_title":"","metadata":{"abstract":"The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock\nshelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits\naccumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays,\nrespectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP)\ncorrelate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP)\n(15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas\nevent (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid\ncommunities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000\n(cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was\ninterrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000\nyears was observed. Presumably the first traces of human activities in this area can be shown for up\nabout 2500 (cal) years BP."},"translated_abstract":"The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock\nshelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits\naccumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays,\nrespectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP)\ncorrelate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP)\n(15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas\nevent (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid\ncommunities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000\n(cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was\ninterrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000\nyears was observed. Presumably the first traces of human activities in this area can be shown for up\nabout 2500 (cal) years BP.","internal_url":"https://www.academia.edu/17793399/Holocene_hyrax_dung_deposits_in_the","translated_internal_url":"","created_at":"2015-11-05T06:25:06.778-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":8803548,"work_id":17793399,"tagging_user_id":36817796,"tagged_user_id":10920347,"co_author_invite_id":null,"email":"k***a@gmail.com","affiliation":"Severtsov Institute of ecology and evolution","display_order":0,"name":"Evgeniya Kuzmicheva","title":"Holocene hyrax dung deposits in the"},{"id":8803551,"work_id":17793399,"tagging_user_id":36817796,"tagged_user_id":4090888,"co_author_invite_id":null,"email":"h***a@gmail.com","affiliation":"Addis Ababa University","display_order":4194304,"name":"Habte Debella","title":"Holocene hyrax dung deposits in the"},{"id":8803555,"work_id":17793399,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":6291456,"name":"Arkady Savinetsky","title":"Holocene hyrax dung deposits in the"}],"downloadable_attachments":[{"id":39713918,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39713918/thumbnails/1.jpg","file_name":"10731-Kuzmicheva_2013.pdf","download_url":"https://www.academia.edu/attachments/39713918/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Holocene_hyrax_dung_deposits_in_the.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39713918/10731-Kuzmicheva_2013-libre.pdf?1446735197=\u0026response-content-disposition=attachment%3B+filename%3DHolocene_hyrax_dung_deposits_in_the.pdf\u0026Expires=1732533578\u0026Signature=GHQsv~HoOwYdX5foCHG7OyqnJnnLOdwt6gQJltoKkKIKqqpc0Xp5vh2iQqwa9QJDzlEuZb6rs8jxrdwfVT3bI1YWEzjavsef3aUC3JBobnmyFXKJbwbQ4CULJ9-VwgeSHYXRjHkzSHcnW0b9bJ5f~khxlPKnv4AHVL5GOLRm2IDRS-Me5IV04TKHg2IJMpVZxn3dok8rTw3RPAzNVtWZCQdX4c-D91BD7p0mYhm9SmkWsM-qr0uHbHixEn46ioKl5TVapCk3qPHcF1GucTMtytTP48gjjQR7dOxCPalDmEFadd1F-OV6Hy4Z1noZwIMFRkLno~IM4L0szDf-vCQApg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Holocene_hyrax_dung_deposits_in_the","translated_slug":"","page_count":10,"language":"en","content_type":"Work","owner":{"id":36817796,"first_name":"Olga","middle_initials":null,"last_name":"Krylovich","page_name":"OlgaKrylovich","domain_name":"sevin","created_at":"2015-10-23T07:14:19.517-07:00","display_name":"Olga Krylovich","url":"https://sevin.academia.edu/OlgaKrylovich"},"attachments":[{"id":39713918,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39713918/thumbnails/1.jpg","file_name":"10731-Kuzmicheva_2013.pdf","download_url":"https://www.academia.edu/attachments/39713918/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Holocene_hyrax_dung_deposits_in_the.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39713918/10731-Kuzmicheva_2013-libre.pdf?1446735197=\u0026response-content-disposition=attachment%3B+filename%3DHolocene_hyrax_dung_deposits_in_the.pdf\u0026Expires=1732533578\u0026Signature=GHQsv~HoOwYdX5foCHG7OyqnJnnLOdwt6gQJltoKkKIKqqpc0Xp5vh2iQqwa9QJDzlEuZb6rs8jxrdwfVT3bI1YWEzjavsef3aUC3JBobnmyFXKJbwbQ4CULJ9-VwgeSHYXRjHkzSHcnW0b9bJ5f~khxlPKnv4AHVL5GOLRm2IDRS-Me5IV04TKHg2IJMpVZxn3dok8rTw3RPAzNVtWZCQdX4c-D91BD7p0mYhm9SmkWsM-qr0uHbHixEn46ioKl5TVapCk3qPHcF1GucTMtytTP48gjjQR7dOxCPalDmEFadd1F-OV6Hy4Z1noZwIMFRkLno~IM4L0szDf-vCQApg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":44390,"name":"Vegetation History and Archaeobotany","url":"https://www.academia.edu/Documents/in/Vegetation_History_and_Archaeobotany"}],"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="17792201"><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/17792201/THE_MARINE_RADIOCARBON_RESERVOIR_EFFECT_ON_ADAK_ISLAND_CENTRAL_ALEUTIAN_ISLANDS_ALASKA"><img alt="Research paper thumbnail of THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA" class="work-thumbnail" src="https://attachments.academia-assets.com/39713113/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/17792201/THE_MARINE_RADIOCARBON_RESERVOIR_EFFECT_ON_ADAK_ISLAND_CENTRAL_ALEUTIAN_ISLANDS_ALASKA">THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA</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://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/BulatKhasanov">Bulat Khasanov</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/DixieWest">Dixie West</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed ...</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">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand<br />the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6c06cdd46d60ccb14fcdb2c3d2bd7b08" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39713113,"asset_id":17792201,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39713113/download_file?st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="17792201"><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="17792201"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17792201; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17792201]").text(description); $(".js-view-count[data-work-id=17792201]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17792201; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17792201']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17792201, 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: "6c06cdd46d60ccb14fcdb2c3d2bd7b08" } } $('.js-work-strip[data-work-id=17792201]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17792201,"title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA","translated_title":"","metadata":{"abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand\nthe marine reservoir offset. 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The burying of the remains dates to the twelfth to thirteenth centu ries. 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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="17403430"><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/17403430/Nitrogen_Isotope_Composition_of_Peat_Samples_as_a_Proxy_for_Determining_Human_Colonization_of_Islands"><img alt="Research paper thumbnail of Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands" class="work-thumbnail" src="https://attachments.academia-assets.com/39486192/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/17403430/Nitrogen_Isotope_Composition_of_Peat_Samples_as_a_Proxy_for_Determining_Human_Colonization_of_Islands">Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands</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://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/ArkadySavinetsky">Arkady Savinetsky</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/BulatKhasanov">Bulat Khasanov</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/DixieWest">Dixie West</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more ...</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 Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more than ten million seabirds. No doubt their numbers were even larger prior to the introduction of foxes and rats, invasive species that have shaped the current population sizes and distributions of bird-breeding colonies. Here we present evidence that the peopling of the Aleutian Islands had the same dramatic effect on seabird populations. Analyses of nitrogen stable isotopes in Shemya Island peat deposits revealed significant 15N enrichment of layers formed cal. 4,700.2,800 yrs BP suggesting high seabird guano input at that time. Following this period there was a sharp decline in ƒÂ15N that coincides with the first appearance of human settlement and reflects drastic reduction in seabird abundance. The isotope signature of marine-derived nitrogen vectored by seabirds is specific only for coastal peat deposits; neither 15N enrichment nor decline was detected in inland peat deposits.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="38cf43ad565d84c83bd3a5b2cbd1d0b3" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39486192,"asset_id":17403430,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39486192/download_file?st=MTczMjUyOTk3OSw4LjIyMi4yMDguMTQ2&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="17403430"><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="17403430"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17403430; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17403430]").text(description); $(".js-view-count[data-work-id=17403430]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17403430; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17403430']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17403430, 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: "38cf43ad565d84c83bd3a5b2cbd1d0b3" } } $('.js-work-strip[data-work-id=17403430]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17403430,"title":"Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands","translated_title":"","metadata":{"abstract":"The Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more than ten million seabirds. No doubt their numbers were even larger prior to the introduction of foxes and rats, invasive species that have shaped the current population sizes and distributions of bird-breeding colonies. Here we present evidence that the peopling of the Aleutian Islands had the same dramatic effect on seabird populations. Analyses of nitrogen stable isotopes in Shemya Island peat deposits revealed significant 15N enrichment of layers formed cal. 4,700.2,800 yrs BP suggesting high seabird guano input at that time. Following this period there was a sharp decline in ƒÂ15N that coincides with the first appearance of human settlement and reflects drastic reduction in seabird abundance. The isotope signature of marine-derived nitrogen vectored by seabirds is specific only for coastal peat deposits; neither 15N enrichment nor decline was detected in inland peat deposits."},"translated_abstract":"The Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more than ten million seabirds. No doubt their numbers were even larger prior to the introduction of foxes and rats, invasive species that have shaped the current population sizes and distributions of bird-breeding colonies. Here we present evidence that the peopling of the Aleutian Islands had the same dramatic effect on seabird populations. Analyses of nitrogen stable isotopes in Shemya Island peat deposits revealed significant 15N enrichment of layers formed cal. 4,700.2,800 yrs BP suggesting high seabird guano input at that time. Following this period there was a sharp decline in ƒÂ15N that coincides with the first appearance of human settlement and reflects drastic reduction in seabird abundance. 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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="15720756"><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/15720756/FISHING_THROUGH_TIME_Archaeoichthyology_Biodiversity_Ecology_and_Human_Impact_on_Aquatic_Environments_PROGRAM_AND_ABSTRACTS_OF_THE_18TH_INTERNATIONAL_COUNCIL_FOR_ARCHAEOZOOLOGY_FISH_REMAINS_WORKING_GROUP"><img alt="Research paper thumbnail of FISHING THROUGH TIME. Archaeoichthyology, Biodiversity, Ecology and Human Impact on Aquatic Environments. PROGRAM AND ABSTRACTS OF THE 18TH INTERNATIONAL COUNCIL FOR ARCHAEOZOOLOGY - FISH REMAINS WORKING GROUP." class="work-thumbnail" src="https://attachments.academia-assets.com/38775352/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/15720756/FISHING_THROUGH_TIME_Archaeoichthyology_Biodiversity_Ecology_and_Human_Impact_on_Aquatic_Environments_PROGRAM_AND_ABSTRACTS_OF_THE_18TH_INTERNATIONAL_COUNCIL_FOR_ARCHAEOZOOLOGY_FISH_REMAINS_WORKING_GROUP">FISHING THROUGH TIME. Archaeoichthyology, Biodiversity, Ecology and Human Impact on Aquatic Environments. PROGRAM AND ABSTRACTS OF THE 18TH INTERNATIONAL COUNCIL FOR ARCHAEOZOOLOGY - FISH REMAINS WORKING GROUP.</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://patrimoniocultural.academia.edu/S%C3%B3niaGabriel">Sonia Gabriel</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ntnu-no.academia.edu/James_H_Barrett">James H Barrett</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/TatianaTheodoropoulou">Tatiana Theodoropoulou</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/ArleneFradkin">Arlene Fradkin</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://yorku.academia.edu/RichardHoffmann">Richard Hoffmann</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://urv.academia.edu/Mar%C3%ADaMart%C3%ADnezPolanco">María Fernanda Martínez-Polanco</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uniss.academia.edu/GabrieleCarenti">Gabriele Carenti</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://us.academia.edu/AntonioSaezRomero">Antonio Saez Romero</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://moesmus.academia.edu/KenRitchie">Kenneth Ritchie</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uhi.academia.edu/JenHarland">Jen Harland</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/YingZhang69">Ying Zhang</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/AnaCosta121">Ana Costa</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sfu.academia.edu/ThomasCARoyle">Thomas Royle</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ut-ee.academia.edu/EveRannam%C3%A4e">Eve Rannamäe</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/Ga%C3%ABlPiqu%C3%A8s">Gaël Piquès</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://helsinki.academia.edu/KatariinaNurminen">Katariina Nurminen</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://naturalsciences-be.academia.edu/WimWouters">Wim Wouters</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uva.academia.edu/JanBakker">Jan Bakker</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://nku.academia.edu/SharynJones">Sharyn Jones</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://instapstudycenter.academia.edu/DimitraMylona">Dimitra Mylona</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://reading.academia.edu/SallyGrainger">Sally Grainger</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MTensen">Marrie Tensen</a></span></div><div class="wp-workCard_item"><span>TRABALHOS DO LARC</span><span>, Sep 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this volume of Trabalhos do LARC we present the Program and Abstracts of the 18th biennial mee...</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 this volume of Trabalhos do LARC we present the Program and Abstracts of the 18th biennial meeting of <br />the International Council for Archaeozoology - Fish Remains Working Group (ICAZ-FRWG), hosted by the <br />Directorate-General for Cultural Heritage - Archaeosciences Laboratory (DGPC - LARC) and the Research <br />Centre in Biodiversity and Genetic Resources – Environmental Archaeology Research Group (CIBIO - <br />EnvArch). <br />The meeting is aimed primarily for archaeozoologists interested in the systematic study of fish bones <br />retrieved from archaeological sites around the world, and also to archaeologists, ichthyologists, historians, <br />ethnographers, and fishery biologists. To this end the conference is structured to encompass a multiplicity <br />of approaches to the study of fish remains and their contribution to our understanding of how fishing, fish <br />trade, fish consumption, biodiversity, ecology and human impact on aquatic environments have changed <br />through time.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b047bc9f480233d9db0e464213f68b31" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38775352,"asset_id":15720756,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38775352/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&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="15720756"><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="15720756"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 15720756; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=15720756]").text(description); $(".js-view-count[data-work-id=15720756]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 15720756; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='15720756']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 15720756, 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: "b047bc9f480233d9db0e464213f68b31" } } $('.js-work-strip[data-work-id=15720756]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":15720756,"title":"FISHING THROUGH TIME. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="3825505" id="papers"><div class="js-work-strip profile--work_container" data-work-id="44611111"><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/44611111/Holocene_Dynamics_of_Invertebrate_Fauna_in_the_Littoral_Zone_of_Adak_the_Aleutian_Islands_According_to_Archaeozoological_Data"><img alt="Research paper thumbnail of Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data" class="work-thumbnail" src="https://attachments.academia-assets.com/65075874/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/44611111/Holocene_Dynamics_of_Invertebrate_Fauna_in_the_Littoral_Zone_of_Adak_the_Aleutian_Islands_According_to_Archaeozoological_Data">Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data</a></div><div class="wp-workCard_item"><span>Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data</span><span>, 2009</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak Is...</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">Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak<br />Island have shown that the faunistic composition of invertebrates in the study area had not changed significantly<br />during the Late Holocene. The traditional mode of natural resource use by the ancient Aleuts had no impact on<br />the abundance of valuable species and biodiversity in general. Changes in the temperature regime were found<br />to have taken place in the history of deposit formation. The period from the 8th to the mid-11th century was<br />relatively cold. Climate warming took place between the mid-11th and the mid-12th centuries and between the<br />mid-16th and the 19th centuries, with an intervening cooling period (from the mid-12th to the mid-16th century).<br />This cooling was most distinct between the 15th and the mid-16th centuries.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a830e8bc4838574cc1b545a2bce4cb7e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":65075874,"asset_id":44611111,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/65075874/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3Nyw4LjIyMi4yMDguMTQ2&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="44611111"><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="44611111"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 44611111; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=44611111]").text(description); $(".js-view-count[data-work-id=44611111]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 44611111; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='44611111']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 44611111, 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: "a830e8bc4838574cc1b545a2bce4cb7e" } } $('.js-work-strip[data-work-id=44611111]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":44611111,"title":"Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data","translated_title":"","metadata":{"doi":"10.1134/s106741360902009x","abstract":"Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak\nIsland have shown that the faunistic composition of invertebrates in the study area had not changed significantly\nduring the Late Holocene. The traditional mode of natural resource use by the ancient Aleuts had no impact on\nthe abundance of valuable species and biodiversity in general. Changes in the temperature regime were found\nto have taken place in the history of deposit formation. The period from the 8th to the mid-11th century was\nrelatively cold. Climate warming took place between the mid-11th and the mid-12th centuries and between the\nmid-16th and the 19th centuries, with an intervening cooling period (from the mid-12th to the mid-16th century).\nThis cooling was most distinct between the 15th and the mid-16th centuries.","publication_date":{"day":null,"month":null,"year":2009,"errors":{}},"publication_name":"Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data"},"translated_abstract":"Studies on invertebrate remains from the cultural layer of an ancient Aleut settlement on Adak\nIsland have shown that the faunistic composition of invertebrates in the study area had not changed significantly\nduring the Late Holocene. The traditional mode of natural resource use by the ancient Aleuts had no impact on\nthe abundance of valuable species and biodiversity in general. Changes in the temperature regime were found\nto have taken place in the history of deposit formation. The period from the 8th to the mid-11th century was\nrelatively cold. Climate warming took place between the mid-11th and the mid-12th centuries and between the\nmid-16th and the 19th centuries, with an intervening cooling period (from the mid-12th to the mid-16th century).\nThis cooling was most distinct between the 15th and the mid-16th centuries.","internal_url":"https://www.academia.edu/44611111/Holocene_Dynamics_of_Invertebrate_Fauna_in_the_Littoral_Zone_of_Adak_the_Aleutian_Islands_According_to_Archaeozoological_Data","translated_internal_url":"","created_at":"2020-12-01T01:03:21.557-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":36007534,"work_id":44611111,"tagging_user_id":36817796,"tagged_user_id":null,"co_author_invite_id":7152590,"email":"z***a@mail.ru","display_order":1,"name":"Zhanna Antipushina","title":"Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data"},{"id":36007535,"work_id":44611111,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":2,"name":"Arkady Savinetsky","title":"Holocene Dynamics of Invertebrate Fauna in the Littoral Zone of Adak, the Aleutian Islands, According to Archaeozoological Data"}],"downloadable_attachments":[{"id":65075874,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/65075874/thumbnails/1.jpg","file_name":"6229_Antipushina_2009.pdf","download_url":"https://www.academia.edu/attachments/65075874/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3Nyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Holocene_Dynamics_of_Invertebrate_Fauna.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/65075874/6229_Antipushina_2009-libre.pdf?1606818792=\u0026response-content-disposition=attachment%3B+filename%3DHolocene_Dynamics_of_Invertebrate_Fauna.pdf\u0026Expires=1732533577\u0026Signature=OaWsfrAbC2vrpT6ACtz9quRcW8ZYOaZ5tUBvORiUtgu~iQ19XwmnYy8ig~JZgG61aq-YFRqqAzlvPLxDoddCwFnXpg6cC8hMnrNleIlZbmBfgd00hVSCsl174V55Tu7BS8rEL5Iq1lS~5JxZtbLuZgpUfHgy2YS5C6-HM8YhIfRa2IEfUwarnXT3hTv5u6i~WhC0UAgpdwpSYFCbqv8fyy~Q3A5uZGqk7j3oILTDGn5BXgWGJHxf7zpMdoVG-XeaMXLwzDqBaheNI7j5q5ZZfBSsQwcgarSj~nPfpxQ0cdCmK0R~k1NtwjAl-NYwopzIbsL4LkxtqAkf7BDlSkyf4w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Holocene_Dynamics_of_Invertebrate_Fauna_in_the_Littoral_Zone_of_Adak_the_Aleutian_Islands_According_to_Archaeozoological_Data","translated_slug":"","page_count":9,"language":"en","content_type":"Work","owner":{"id":36817796,"first_name":"Olga","middle_initials":null,"last_name":"Krylovich","page_name":"OlgaKrylovich","domain_name":"sevin","created_at":"2015-10-23T07:14:19.517-07:00","display_name":"Olga Krylovich","url":"https://sevin.academia.edu/OlgaKrylovich"},"attachments":[{"id":65075874,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/65075874/thumbnails/1.jpg","file_name":"6229_Antipushina_2009.pdf","download_url":"https://www.academia.edu/attachments/65075874/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3Nyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Holocene_Dynamics_of_Invertebrate_Fauna.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/65075874/6229_Antipushina_2009-libre.pdf?1606818792=\u0026response-content-disposition=attachment%3B+filename%3DHolocene_Dynamics_of_Invertebrate_Fauna.pdf\u0026Expires=1732533577\u0026Signature=OaWsfrAbC2vrpT6ACtz9quRcW8ZYOaZ5tUBvORiUtgu~iQ19XwmnYy8ig~JZgG61aq-YFRqqAzlvPLxDoddCwFnXpg6cC8hMnrNleIlZbmBfgd00hVSCsl174V55Tu7BS8rEL5Iq1lS~5JxZtbLuZgpUfHgy2YS5C6-HM8YhIfRa2IEfUwarnXT3hTv5u6i~WhC0UAgpdwpSYFCbqv8fyy~Q3A5uZGqk7j3oILTDGn5BXgWGJHxf7zpMdoVG-XeaMXLwzDqBaheNI7j5q5ZZfBSsQwcgarSj~nPfpxQ0cdCmK0R~k1NtwjAl-NYwopzIbsL4LkxtqAkf7BDlSkyf4w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":70250,"name":"Archaeology of shell middens","url":"https://www.academia.edu/Documents/in/Archaeology_of_shell_middens"},{"id":78965,"name":"Holocene","url":"https://www.academia.edu/Documents/in/Holocene"},{"id":155263,"name":"Aleutian islands","url":"https://www.academia.edu/Documents/in/Aleutian_islands"}],"urls":[]}, dispatcherData: dispatcherData }); 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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="32946266"><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/32946266/The_Marine_Radiocarbon_Reservoir_Effect_on_Adak_Island_Central_Aleutian_Islands_Alaska"><img alt="Research paper thumbnail of The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32946266/The_Marine_Radiocarbon_Reservoir_Effect_on_Adak_Island_Central_Aleutian_Islands_Alaska">The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska</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://fukuoka-u.academia.edu/MitsuruOkuno">Mitsuru Okuno</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/ArkadySavinetsky">Arkady Savinetsky</a></span></div><div class="wp-workCard_item"><span>Radiocarbon</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed ...</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">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.</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="32946266"><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="32946266"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32946266; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32946266]").text(description); $(".js-view-count[data-work-id=32946266]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32946266; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32946266']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32946266, 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" } } $('.js-work-strip[data-work-id=32946266]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32946266,"title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska","translated_title":"","metadata":{"abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Radiocarbon"},"translated_abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.","internal_url":"https://www.academia.edu/32946266/The_Marine_Radiocarbon_Reservoir_Effect_on_Adak_Island_Central_Aleutian_Islands_Alaska","translated_internal_url":"","created_at":"2017-05-10T22:43:52.782-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":40765015,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":28872254,"work_id":32946266,"tagging_user_id":40765015,"tagged_user_id":4541045,"co_author_invite_id":null,"email":"d***t@ksu.edu","display_order":0,"name":"Dixie West","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"},{"id":28872255,"work_id":32946266,"tagging_user_id":40765015,"tagged_user_id":36817796,"co_author_invite_id":null,"email":"c***r@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":4194304,"name":"Olga Krylovich","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"},{"id":28872256,"work_id":32946266,"tagging_user_id":40765015,"tagged_user_id":4753710,"co_author_invite_id":null,"email":"b***k@gmail.com","affiliation":"Severtsov Institute of ecology and evolution","display_order":6291456,"name":"Bulat Khasanov","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"},{"id":28872289,"work_id":32946266,"tagging_user_id":40765015,"tagged_user_id":null,"co_author_invite_id":6287202,"email":"t***a@po.rd.taisho.co.jp","display_order":7340032,"name":"Toshio Nakamura","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"},{"id":29976125,"work_id":32946266,"tagging_user_id":36817796,"tagged_user_id":510122,"co_author_invite_id":null,"email":"v***d@hotmail.com","display_order":7864320,"name":"Virginia Hatfield","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"},{"id":29976126,"work_id":32946266,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":8126464,"name":"Arkady Savinetsky","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"},{"id":29976128,"work_id":32946266,"tagging_user_id":36817796,"tagged_user_id":2711778,"co_author_invite_id":null,"email":"k***v@rambler.ru","affiliation":"Institute of Archaeology of Ukrainian National Academy of Sciences","display_order":8257536,"name":"Ekaterina Gorlova","title":"The Marine Radiocarbon Reservoir Effect on Adak Island (Central Aleutian Islands), Alaska"}],"downloadable_attachments":[],"slug":"The_Marine_Radiocarbon_Reservoir_Effect_on_Adak_Island_Central_Aleutian_Islands_Alaska","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":40765015,"first_name":"Mitsuru","middle_initials":"","last_name":"Okuno","page_name":"MitsuruOkuno","domain_name":"fukuoka-u","created_at":"2015-12-30T15:47:36.246-08:00","display_name":"Mitsuru Okuno","url":"https://fukuoka-u.academia.edu/MitsuruOkuno"},"attachments":[],"research_interests":[{"id":14717,"name":"Radiocarbon","url":"https://www.academia.edu/Documents/in/Radiocarbon"},{"id":19758,"name":"Radiocarbon Dating (Earth Sciences)","url":"https://www.academia.edu/Documents/in/Radiocarbon_Dating_Earth_Sciences_"},{"id":112668,"name":"Radiocarbon Dating (Archaeology)","url":"https://www.academia.edu/Documents/in/Radiocarbon_Dating_Archaeology_"}],"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="21946219"><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/21946219/Hunting_Impacts_on_the_Sea_Otter_Enhydra_lutris_Population_in_Clam_Lagoon_Adak_Island_Aleutian_Islands_7_000_Years_Ago_Results_of_Preliminary_Stable_Isotopes_Analysis"><img alt="Research paper thumbnail of Hunting Impacts on the Sea Otter ( Enhydra lutris ) Population in Clam Lagoon (Adak Island, Aleutian Islands) 7,000 Years Ago? Results of Preliminary Stable Isotopes Analysis" class="work-thumbnail" src="https://attachments.academia-assets.com/42669601/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/21946219/Hunting_Impacts_on_the_Sea_Otter_Enhydra_lutris_Population_in_Clam_Lagoon_Adak_Island_Aleutian_Islands_7_000_Years_Ago_Results_of_Preliminary_Stable_Isotopes_Analysis">Hunting Impacts on the Sea Otter ( Enhydra lutris ) Population in Clam Lagoon (Adak Island, Aleutian Islands) 7,000 Years Ago? Results of Preliminary Stable Isotopes Analysis</a></div><div class="wp-workCard_item"><span>The Journal of Island and Coastal Archaeology</span><span>, 2011</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="dfd8ca2122de9d9536ecd86cf4b2b3d4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":42669601,"asset_id":21946219,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/42669601/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="21946219"><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="21946219"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 21946219; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=21946219]").text(description); $(".js-view-count[data-work-id=21946219]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 21946219; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='21946219']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 21946219, 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: "dfd8ca2122de9d9536ecd86cf4b2b3d4" } } $('.js-work-strip[data-work-id=21946219]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":21946219,"title":"Hunting Impacts on the Sea Otter ( Enhydra lutris ) Population in Clam Lagoon (Adak Island, Aleutian Islands) 7,000 Years Ago? 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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="18149495"><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/18149495/Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material"><img alt="Research paper thumbnail of Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material" class="work-thumbnail" src="https://attachments.academia-assets.com/39901302/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/18149495/Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material">Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material</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://sevin.academia.edu/ArkadySavinetsky">Arkady Savinetsky</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MityaVasyukov">Mitya Vasyukov</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/BulatKhasanov">Bulat Khasanov</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and ni...</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 paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and nitrogen isotope composition (ratio of 15N/14N) for taxonomic diagnostics of animal bone remains from archaeological sites and other ancient deposits. The world literature pertaining to the use of stable-isotope analysis (SIA) in animal trophic ecology and methodological difficulties of work with subfossil material are reviewed. Several particular cases show a successful application of SIA for taxonomic identification of the archaeozoological remains, especially bones of brown and polar bears, large sea mammals and a few species of Anseriformes.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bfeb4d7c4f831eed00b727894e95ae2c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39901302,"asset_id":18149495,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39901302/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="18149495"><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="18149495"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 18149495; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=18149495]").text(description); $(".js-view-count[data-work-id=18149495]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 18149495; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='18149495']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 18149495, 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: "bfeb4d7c4f831eed00b727894e95ae2c" } } $('.js-work-strip[data-work-id=18149495]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":18149495,"title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material","translated_title":"","metadata":{"abstract":"The paper discusses the possibility of using carbon isotope composition (ratio of 13C/12C) and nitrogen isotope composition (ratio of 15N/14N) for taxonomic diagnostics of animal bone remains from archaeological sites and other ancient deposits. 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Several particular cases show a successful application of SIA for taxonomic identification of the archaeozoological remains, especially bones of brown and polar bears, large sea mammals and a few species of Anseriformes.","internal_url":"https://www.academia.edu/18149495/Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material","translated_internal_url":"","created_at":"2015-11-11T06:34:33.170-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":9465427,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":0,"name":"Arkady Savinetsky","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465428,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":38248084,"co_author_invite_id":2154372,"email":"t***6@gmail.com","display_order":4194304,"name":"Mitya Vasyukov","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465429,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":4753710,"co_author_invite_id":null,"email":"b***k@gmail.com","affiliation":"Severtsov Institute of ecology and evolution","display_order":6291456,"name":"Bulat Khasanov","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465430,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":null,"co_author_invite_id":1187273,"email":"a***v@mail.ru","display_order":7340032,"name":"Alexei Tiunov","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"},{"id":9465431,"work_id":18149495,"tagging_user_id":36817796,"tagged_user_id":null,"co_author_invite_id":2154373,"email":"g***k@gmail.com","display_order":7864320,"name":"Ekaterina Gorlova","title":"Stable-Isotope Analysis as a Method of Taxonomical Identification of Archaeozoological Material"}],"downloadable_attachments":[{"id":39901302,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39901302/thumbnails/1.jpg","file_name":"Gorlova_et_al-2015.pdf","download_url":"https://www.academia.edu/attachments/39901302/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stable_Isotope_Analysis_as_a_Method_of_T.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39901302/Gorlova_et_al-2015-libre.pdf?1447253359=\u0026response-content-disposition=attachment%3B+filename%3DStable_Isotope_Analysis_as_a_Method_of_T.pdf\u0026Expires=1732533578\u0026Signature=X-VlwbBra4j7S828BcQbxlh1296SjQVh7~0TXdaWlmpmJnLZTsaIxUZuhaqTKFh4cEOewDwzbGe42jAFjoQwZRvagHDj24dtl-7u3R7potxUDr5DPgdeWLjD4GA~oNNcRwl-lm~xugi3Ny3Y1F0fG8KqExCCKBrWcGj~M5JSQZ8nn0DumJGA2TesN4V2t9yEAGdVq3OWDwX4rAwNQ05PNECmWShZusOBKMqoIYMjEmQovsoASvQzV7iuq-TZ5FXo5TVgD3hG10eaDqeoBHJEWv0gZ7YFUcyvPgfAAnC0pvITefTut5WsHS87M-xklvzrU7~ti4GG-nPOq6lVulyfbQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Stable_Isotope_Analysis_as_a_Method_of_Taxonomical_Identification_of_Archaeozoological_Material","translated_slug":"","page_count":12,"language":"en","content_type":"Work","owner":{"id":36817796,"first_name":"Olga","middle_initials":null,"last_name":"Krylovich","page_name":"OlgaKrylovich","domain_name":"sevin","created_at":"2015-10-23T07:14:19.517-07:00","display_name":"Olga Krylovich","url":"https://sevin.academia.edu/OlgaKrylovich"},"attachments":[{"id":39901302,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39901302/thumbnails/1.jpg","file_name":"Gorlova_et_al-2015.pdf","download_url":"https://www.academia.edu/attachments/39901302/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stable_Isotope_Analysis_as_a_Method_of_T.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39901302/Gorlova_et_al-2015-libre.pdf?1447253359=\u0026response-content-disposition=attachment%3B+filename%3DStable_Isotope_Analysis_as_a_Method_of_T.pdf\u0026Expires=1732533578\u0026Signature=X-VlwbBra4j7S828BcQbxlh1296SjQVh7~0TXdaWlmpmJnLZTsaIxUZuhaqTKFh4cEOewDwzbGe42jAFjoQwZRvagHDj24dtl-7u3R7potxUDr5DPgdeWLjD4GA~oNNcRwl-lm~xugi3Ny3Y1F0fG8KqExCCKBrWcGj~M5JSQZ8nn0DumJGA2TesN4V2t9yEAGdVq3OWDwX4rAwNQ05PNECmWShZusOBKMqoIYMjEmQovsoASvQzV7iuq-TZ5FXo5TVgD3hG10eaDqeoBHJEWv0gZ7YFUcyvPgfAAnC0pvITefTut5WsHS87M-xklvzrU7~ti4GG-nPOq6lVulyfbQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1421,"name":"Stable isotope ecology","url":"https://www.academia.edu/Documents/in/Stable_isotope_ecology"}],"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="17793399"><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/17793399/Holocene_hyrax_dung_deposits_in_the"><img alt="Research paper thumbnail of Holocene hyrax dung deposits in the" class="work-thumbnail" src="https://attachments.academia-assets.com/39713918/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/17793399/Holocene_hyrax_dung_deposits_in_the">Holocene hyrax dung deposits in the</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits f...</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 results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock<br />shelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits<br />accumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays,<br />respectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP)<br />correlate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP)<br />(15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas<br />event (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid<br />communities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000<br />(cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was<br />interrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000<br />years was observed. Presumably the first traces of human activities in this area can be shown for up<br />about 2500 (cal) years BP.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7c93a49439af1526ec5d6473580b2b56" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39713918,"asset_id":17793399,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39713918/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OCw4LjIyMi4yMDguMTQ2&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="17793399"><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="17793399"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17793399; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17793399]").text(description); $(".js-view-count[data-work-id=17793399]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17793399; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17793399']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17793399, 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: "7c93a49439af1526ec5d6473580b2b56" } } $('.js-work-strip[data-work-id=17793399]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17793399,"title":"Holocene hyrax dung deposits in the","translated_title":"","metadata":{"abstract":"The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock\nshelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits\naccumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays,\nrespectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP)\ncorrelate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP)\n(15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas\nevent (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid\ncommunities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000\n(cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was\ninterrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000\nyears was observed. Presumably the first traces of human activities in this area can be shown for up\nabout 2500 (cal) years BP."},"translated_abstract":"The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock\nshelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits\naccumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays,\nrespectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP)\ncorrelate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP)\n(15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas\nevent (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid\ncommunities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000\n(cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was\ninterrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000\nyears was observed. 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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="17792201"><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/17792201/THE_MARINE_RADIOCARBON_RESERVOIR_EFFECT_ON_ADAK_ISLAND_CENTRAL_ALEUTIAN_ISLANDS_ALASKA"><img alt="Research paper thumbnail of THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA" class="work-thumbnail" src="https://attachments.academia-assets.com/39713113/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/17792201/THE_MARINE_RADIOCARBON_RESERVOIR_EFFECT_ON_ADAK_ISLAND_CENTRAL_ALEUTIAN_ISLANDS_ALASKA">THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA</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://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/BulatKhasanov">Bulat Khasanov</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/DixieWest">Dixie West</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed ...</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">Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand<br />the marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6c06cdd46d60ccb14fcdb2c3d2bd7b08" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39713113,"asset_id":17792201,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39713113/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&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="17792201"><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="17792201"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17792201; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17792201]").text(description); $(".js-view-count[data-work-id=17792201]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17792201; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17792201']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17792201, 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: "6c06cdd46d60ccb14fcdb2c3d2bd7b08" } } $('.js-work-strip[data-work-id=17792201]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17792201,"title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA","translated_title":"","metadata":{"abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand\nthe marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians."},"translated_abstract":"Radiocarbon dates (n = 18) from three archaeological sites on Adak Island, Alaska, were analyzed to understand\nthe marine reservoir offset. Samples of marine and terrestrial origins recovered from the same archaeological context were compiled in nine pairs. The mean ΔR value calculated for them totaled 545 ± 10 yr. This value can be regarded as a sound estimate of the marine reservoir offset in the central Aleutians.","internal_url":"https://www.academia.edu/17792201/THE_MARINE_RADIOCARBON_RESERVOIR_EFFECT_ON_ADAK_ISLAND_CENTRAL_ALEUTIAN_ISLANDS_ALASKA","translated_internal_url":"","created_at":"2015-11-05T06:19:10.122-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":8801100,"work_id":17792201,"tagging_user_id":36817796,"tagged_user_id":4753710,"co_author_invite_id":null,"email":"b***k@gmail.com","affiliation":"Severtsov Institute of ecology and evolution","display_order":0,"name":"Bulat Khasanov","title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA"},{"id":8801108,"work_id":17792201,"tagging_user_id":36817796,"tagged_user_id":4541045,"co_author_invite_id":null,"email":"d***t@ksu.edu","display_order":4194304,"name":"Dixie West","title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA"},{"id":8801117,"work_id":17792201,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":6291456,"name":"Arkady Savinetsky","title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA"},{"id":8801119,"work_id":17792201,"tagging_user_id":36817796,"tagged_user_id":510122,"co_author_invite_id":null,"email":"v***d@hotmail.com","display_order":7340032,"name":"Virginia Hatfield","title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA"},{"id":8801121,"work_id":17792201,"tagging_user_id":36817796,"tagged_user_id":2711778,"co_author_invite_id":null,"email":"k***v@rambler.ru","affiliation":"Institute of Archaeology of Ukrainian National Academy of Sciences","display_order":7864320,"name":"Ekaterina Gorlova","title":"THE MARINE RADIOCARBON RESERVOIR EFFECT ON ADAK ISLAND (CENTRAL ALEUTIAN ISLANDS), ALASKA"},{"id":25599537,"work_id":17792201,"tagging_user_id":4753710,"tagged_user_id":229738012,"co_author_invite_id":1358273,"email":"t***a@sunysb.edu","display_order":8126464,"name":"T. 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The burying of the remains dates to the twelfth to thirteenth centu ries. It is assumed that the spread of the black rat in the European part of Russia in the Middle Ages was asso ciated first of all with the development of trade.","grobid_abstract_attachment_id":39486234},"translated_abstract":null,"internal_url":"https://www.academia.edu/17403487/On_the_History_of_the_Spread_of_the_Black_Rat_Rattus_rattus_L_1758_in_Northwestern_Russia","translated_internal_url":"","created_at":"2015-10-28T02:48:19.072-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":8132363,"work_id":17403487,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":0,"name":"Arkady Savinetsky","title":"On the History of the Spread of the Black Rat (Rattus rattus L., 1758) in Northwestern Russia"}],"downloadable_attachments":[{"id":39486234,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39486234/thumbnails/1.jpg","file_name":"8466-Savinetsky-2011.pdf","download_url":"https://www.academia.edu/attachments/39486234/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"On_the_History_of_the_Spread_of_the_Blac.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39486234/8466-Savinetsky-2011-libre.pdf?1446032904=\u0026response-content-disposition=attachment%3B+filename%3DOn_the_History_of_the_Spread_of_the_Blac.pdf\u0026Expires=1732533579\u0026Signature=OVZPJrOPGKcZAZxTHTCSZad1gs6GEgEOXEQxJ7fgHfSY23zbzZw2saJ76CdTh3gtPq7OAVof7-hppHHX9t8pCa7qeo~FkBDaepiKVo2NAxQsNbY9wZYgN5AI1LqITPjP5h5RmQIyw1gWD3XlF411ukbFy-2JaId8l6JagAZJGZs3IdqNCc-vSlWS7Erd5yc0V-7KhWjYHGTZeusX-cKlzLCg~4hHLk2z6Qp7iXRihZ41ejj78dT1OkLvmWpJcTYCwg20zew0OonEka4J8ffrj07WpKrJH5cfmOrCLZPYvafWU1IRm-cuVBXloGhn1h5ZD2gdeSEWT8XRGwu2uahmZw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"On_the_History_of_the_Spread_of_the_Black_Rat_Rattus_rattus_L_1758_in_Northwestern_Russia","translated_slug":"","page_count":5,"language":"en","content_type":"Work","owner":{"id":36817796,"first_name":"Olga","middle_initials":null,"last_name":"Krylovich","page_name":"OlgaKrylovich","domain_name":"sevin","created_at":"2015-10-23T07:14:19.517-07:00","display_name":"Olga Krylovich","url":"https://sevin.academia.edu/OlgaKrylovich"},"attachments":[{"id":39486234,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39486234/thumbnails/1.jpg","file_name":"8466-Savinetsky-2011.pdf","download_url":"https://www.academia.edu/attachments/39486234/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk3OSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"On_the_History_of_the_Spread_of_the_Blac.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39486234/8466-Savinetsky-2011-libre.pdf?1446032904=\u0026response-content-disposition=attachment%3B+filename%3DOn_the_History_of_the_Spread_of_the_Blac.pdf\u0026Expires=1732533579\u0026Signature=OVZPJrOPGKcZAZxTHTCSZad1gs6GEgEOXEQxJ7fgHfSY23zbzZw2saJ76CdTh3gtPq7OAVof7-hppHHX9t8pCa7qeo~FkBDaepiKVo2NAxQsNbY9wZYgN5AI1LqITPjP5h5RmQIyw1gWD3XlF411ukbFy-2JaId8l6JagAZJGZs3IdqNCc-vSlWS7Erd5yc0V-7KhWjYHGTZeusX-cKlzLCg~4hHLk2z6Qp7iXRihZ41ejj78dT1OkLvmWpJcTYCwg20zew0OonEka4J8ffrj07WpKrJH5cfmOrCLZPYvafWU1IRm-cuVBXloGhn1h5ZD2gdeSEWT8XRGwu2uahmZw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1912107,"name":"Black rat","url":"https://www.academia.edu/Documents/in/Black_rat"}],"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="17403430"><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/17403430/Nitrogen_Isotope_Composition_of_Peat_Samples_as_a_Proxy_for_Determining_Human_Colonization_of_Islands"><img alt="Research paper thumbnail of Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands" class="work-thumbnail" src="https://attachments.academia-assets.com/39486192/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/17403430/Nitrogen_Isotope_Composition_of_Peat_Samples_as_a_Proxy_for_Determining_Human_Colonization_of_Islands">Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands</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://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/ArkadySavinetsky">Arkady Savinetsky</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/BulatKhasanov">Bulat Khasanov</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/DixieWest">Dixie West</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more ...</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 Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more than ten million seabirds. No doubt their numbers were even larger prior to the introduction of foxes and rats, invasive species that have shaped the current population sizes and distributions of bird-breeding colonies. Here we present evidence that the peopling of the Aleutian Islands had the same dramatic effect on seabird populations. Analyses of nitrogen stable isotopes in Shemya Island peat deposits revealed significant 15N enrichment of layers formed cal. 4,700.2,800 yrs BP suggesting high seabird guano input at that time. Following this period there was a sharp decline in ƒÂ15N that coincides with the first appearance of human settlement and reflects drastic reduction in seabird abundance. The isotope signature of marine-derived nitrogen vectored by seabirds is specific only for coastal peat deposits; neither 15N enrichment nor decline was detected in inland peat deposits.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="38cf43ad565d84c83bd3a5b2cbd1d0b3" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39486192,"asset_id":17403430,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39486192/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&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="17403430"><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="17403430"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17403430; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17403430]").text(description); $(".js-view-count[data-work-id=17403430]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17403430; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17403430']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 17403430, 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: "38cf43ad565d84c83bd3a5b2cbd1d0b3" } } $('.js-work-strip[data-work-id=17403430]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17403430,"title":"Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands","translated_title":"","metadata":{"abstract":"The Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more than ten million seabirds. No doubt their numbers were even larger prior to the introduction of foxes and rats, invasive species that have shaped the current population sizes and distributions of bird-breeding colonies. Here we present evidence that the peopling of the Aleutian Islands had the same dramatic effect on seabird populations. Analyses of nitrogen stable isotopes in Shemya Island peat deposits revealed significant 15N enrichment of layers formed cal. 4,700.2,800 yrs BP suggesting high seabird guano input at that time. Following this period there was a sharp decline in ƒÂ15N that coincides with the first appearance of human settlement and reflects drastic reduction in seabird abundance. The isotope signature of marine-derived nitrogen vectored by seabirds is specific only for coastal peat deposits; neither 15N enrichment nor decline was detected in inland peat deposits."},"translated_abstract":"The Aleutian Islands comprise a unique ecosystem, providing nesting grounds and habitat for more than ten million seabirds. No doubt their numbers were even larger prior to the introduction of foxes and rats, invasive species that have shaped the current population sizes and distributions of bird-breeding colonies. Here we present evidence that the peopling of the Aleutian Islands had the same dramatic effect on seabird populations. Analyses of nitrogen stable isotopes in Shemya Island peat deposits revealed significant 15N enrichment of layers formed cal. 4,700.2,800 yrs BP suggesting high seabird guano input at that time. Following this period there was a sharp decline in ƒÂ15N that coincides with the first appearance of human settlement and reflects drastic reduction in seabird abundance. The isotope signature of marine-derived nitrogen vectored by seabirds is specific only for coastal peat deposits; neither 15N enrichment nor decline was detected in inland peat deposits.","internal_url":"https://www.academia.edu/17403430/Nitrogen_Isotope_Composition_of_Peat_Samples_as_a_Proxy_for_Determining_Human_Colonization_of_Islands","translated_internal_url":"","created_at":"2015-10-28T02:45:53.362-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":36817796,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":8132196,"work_id":17403430,"tagging_user_id":36817796,"tagged_user_id":988242,"co_author_invite_id":null,"email":"a***s@rambler.ru","affiliation":"Severtsov Institute of ecology and evolution","display_order":0,"name":"Arkady Savinetsky","title":"Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands"},{"id":8132198,"work_id":17403430,"tagging_user_id":36817796,"tagged_user_id":4753710,"co_author_invite_id":null,"email":"b***k@gmail.com","affiliation":"Severtsov Institute of ecology and evolution","display_order":4194304,"name":"Bulat Khasanov","title":"Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands"},{"id":8132200,"work_id":17403430,"tagging_user_id":36817796,"tagged_user_id":4541045,"co_author_invite_id":null,"email":"d***t@ksu.edu","display_order":6291456,"name":"Dixie West","title":"Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands"},{"id":8132202,"work_id":17403430,"tagging_user_id":36817796,"tagged_user_id":3512406,"co_author_invite_id":null,"email":"n***s@rambler.ru","affiliation":"Institute of Archaeology of Ukrainian National Academy of Sciences","display_order":7340032,"name":"Nina Kiseleva","title":"Nitrogen Isotope Composition of Peat Samples as a Proxy for Determining Human Colonization of Islands"}],"downloadable_attachments":[{"id":39486192,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39486192/thumbnails/1.jpg","file_name":"11927-Savinetsky-2014.pdf","download_url":"https://www.academia.edu/attachments/39486192/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Nitrogen_Isotope_Composition_of_Peat_Sam.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39486192/11927-Savinetsky-2014-libre.pdf?1446029546=\u0026response-content-disposition=attachment%3B+filename%3DNitrogen_Isotope_Composition_of_Peat_Sam.pdf\u0026Expires=1732506697\u0026Signature=ZgfziA3nT-zy8hE4Nan7rbuBsWTFwPHpCwolXpVE3CdyO84bSg32AMGuZn6Hhd84ieKpbPE6Wwmp5jUvkjzxEYD3s5V25ADumIZW8FBWLCqIItLv~qwsWhyikdllQZ5mUvEqc4vQMm1388D1L6NsGacovyiZ9FSmLNV2RQHzuS7s0dnLVFirOBdLZyHe8XMJl7MuUHaHGLENd5SORFhjwxM8bwDwqSNezr8lwLX1sdEoQ5qMH1rSawBLmPjqGRxc4uSAN5L7FFK3hd-ZNc0I2PP5~DBEaGEMPK2jdxJRTKybK9gm3I1YziC5CFpFpOSX~TJHAgyC50eHOTArLMWPuQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Nitrogen_Isotope_Composition_of_Peat_Samples_as_a_Proxy_for_Determining_Human_Colonization_of_Islands","translated_slug":"","page_count":9,"language":"en","content_type":"Work","owner":{"id":36817796,"first_name":"Olga","middle_initials":null,"last_name":"Krylovich","page_name":"OlgaKrylovich","domain_name":"sevin","created_at":"2015-10-23T07:14:19.517-07:00","display_name":"Olga Krylovich","url":"https://sevin.academia.edu/OlgaKrylovich"},"attachments":[{"id":39486192,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39486192/thumbnails/1.jpg","file_name":"11927-Savinetsky-2014.pdf","download_url":"https://www.academia.edu/attachments/39486192/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Nitrogen_Isotope_Composition_of_Peat_Sam.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39486192/11927-Savinetsky-2014-libre.pdf?1446029546=\u0026response-content-disposition=attachment%3B+filename%3DNitrogen_Isotope_Composition_of_Peat_Sam.pdf\u0026Expires=1732506697\u0026Signature=ZgfziA3nT-zy8hE4Nan7rbuBsWTFwPHpCwolXpVE3CdyO84bSg32AMGuZn6Hhd84ieKpbPE6Wwmp5jUvkjzxEYD3s5V25ADumIZW8FBWLCqIItLv~qwsWhyikdllQZ5mUvEqc4vQMm1388D1L6NsGacovyiZ9FSmLNV2RQHzuS7s0dnLVFirOBdLZyHe8XMJl7MuUHaHGLENd5SORFhjwxM8bwDwqSNezr8lwLX1sdEoQ5qMH1rSawBLmPjqGRxc4uSAN5L7FFK3hd-ZNc0I2PP5~DBEaGEMPK2jdxJRTKybK9gm3I1YziC5CFpFpOSX~TJHAgyC50eHOTArLMWPuQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":155263,"name":"Aleutian islands","url":"https://www.academia.edu/Documents/in/Aleutian_islands"},{"id":912534,"name":"Aleutian Archaeology","url":"https://www.academia.edu/Documents/in/Aleutian_Archaeology"}],"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="15720756"><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/15720756/FISHING_THROUGH_TIME_Archaeoichthyology_Biodiversity_Ecology_and_Human_Impact_on_Aquatic_Environments_PROGRAM_AND_ABSTRACTS_OF_THE_18TH_INTERNATIONAL_COUNCIL_FOR_ARCHAEOZOOLOGY_FISH_REMAINS_WORKING_GROUP"><img alt="Research paper thumbnail of FISHING THROUGH TIME. Archaeoichthyology, Biodiversity, Ecology and Human Impact on Aquatic Environments. PROGRAM AND ABSTRACTS OF THE 18TH INTERNATIONAL COUNCIL FOR ARCHAEOZOOLOGY - FISH REMAINS WORKING GROUP." class="work-thumbnail" src="https://attachments.academia-assets.com/38775352/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/15720756/FISHING_THROUGH_TIME_Archaeoichthyology_Biodiversity_Ecology_and_Human_Impact_on_Aquatic_Environments_PROGRAM_AND_ABSTRACTS_OF_THE_18TH_INTERNATIONAL_COUNCIL_FOR_ARCHAEOZOOLOGY_FISH_REMAINS_WORKING_GROUP">FISHING THROUGH TIME. Archaeoichthyology, Biodiversity, Ecology and Human Impact on Aquatic Environments. PROGRAM AND ABSTRACTS OF THE 18TH INTERNATIONAL COUNCIL FOR ARCHAEOZOOLOGY - FISH REMAINS WORKING GROUP.</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://patrimoniocultural.academia.edu/S%C3%B3niaGabriel">Sonia Gabriel</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ntnu-no.academia.edu/James_H_Barrett">James H Barrett</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/TatianaTheodoropoulou">Tatiana Theodoropoulou</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/ArleneFradkin">Arlene Fradkin</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://yorku.academia.edu/RichardHoffmann">Richard Hoffmann</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://urv.academia.edu/Mar%C3%ADaMart%C3%ADnezPolanco">María Fernanda Martínez-Polanco</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uniss.academia.edu/GabrieleCarenti">Gabriele Carenti</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://us.academia.edu/AntonioSaezRomero">Antonio Saez Romero</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://moesmus.academia.edu/KenRitchie">Kenneth Ritchie</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uhi.academia.edu/JenHarland">Jen Harland</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/YingZhang69">Ying Zhang</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/AnaCosta121">Ana Costa</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sfu.academia.edu/ThomasCARoyle">Thomas Royle</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ut-ee.academia.edu/EveRannam%C3%A4e">Eve Rannamäe</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/Ga%C3%ABlPiqu%C3%A8s">Gaël Piquès</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://helsinki.academia.edu/KatariinaNurminen">Katariina Nurminen</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://naturalsciences-be.academia.edu/WimWouters">Wim Wouters</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uva.academia.edu/JanBakker">Jan Bakker</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://nku.academia.edu/SharynJones">Sharyn Jones</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://sevin.academia.edu/OlgaKrylovich">Olga Krylovich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://instapstudycenter.academia.edu/DimitraMylona">Dimitra Mylona</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://reading.academia.edu/SallyGrainger">Sally Grainger</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MTensen">Marrie Tensen</a></span></div><div class="wp-workCard_item"><span>TRABALHOS DO LARC</span><span>, Sep 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this volume of Trabalhos do LARC we present the Program and Abstracts of the 18th biennial mee...</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 this volume of Trabalhos do LARC we present the Program and Abstracts of the 18th biennial meeting of <br />the International Council for Archaeozoology - Fish Remains Working Group (ICAZ-FRWG), hosted by the <br />Directorate-General for Cultural Heritage - Archaeosciences Laboratory (DGPC - LARC) and the Research <br />Centre in Biodiversity and Genetic Resources – Environmental Archaeology Research Group (CIBIO - <br />EnvArch). <br />The meeting is aimed primarily for archaeozoologists interested in the systematic study of fish bones <br />retrieved from archaeological sites around the world, and also to archaeologists, ichthyologists, historians, <br />ethnographers, and fishery biologists. To this end the conference is structured to encompass a multiplicity <br />of approaches to the study of fish remains and their contribution to our understanding of how fishing, fish <br />trade, fish consumption, biodiversity, ecology and human impact on aquatic environments have changed <br />through time.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b047bc9f480233d9db0e464213f68b31" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38775352,"asset_id":15720756,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38775352/download_file?st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&st=MTczMjUyOTk4Miw4LjIyMi4yMDguMTQ2&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="15720756"><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="15720756"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 15720756; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=15720756]").text(description); $(".js-view-count[data-work-id=15720756]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 15720756; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='15720756']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 15720756, 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: "b047bc9f480233d9db0e464213f68b31" } } $('.js-work-strip[data-work-id=15720756]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":15720756,"title":"FISHING THROUGH TIME. 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