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class="social-profile-avatar-container"><img class="profile-avatar u-positionAbsolute" alt="Jane Skippington" border="0" onerror="if (this.src != '//a.academia-assets.com/images/s200_no_pic.png') this.src = '//a.academia-assets.com/images/s200_no_pic.png';" width="200" height="200" src="https://0.academia-photos.com/14260800/10018932/20078454/s200_jane.skippington.jpeg" /></div><div class="title-container"><h1 class="ds2-5-heading-sans-serif-sm">Jane Skippington</h1><div class="affiliations-container fake-truncate js-profile-affiliations"><div><a class="u-tcGrayDarker" href="https://queenslandmuseum.academia.edu/">Queensland Museum</a>, <a class="u-tcGrayDarker" href="https://queenslandmuseum.academia.edu/Departments/Cultures_and_Histories_Program/Documents">Cultures and Histories Program</a>, <span class="u-tcGrayDarker">Faculty Member</span></div><div><a class="u-tcGrayDarker" href="https://uwa.academia.edu/">The University of Western Australia</a>, <a class="u-tcGrayDarker" href="https://uwa.academia.edu/Departments/Faculty_of_Arts_Humanities_and_Social_Sciences/Documents">Faculty of Arts, Humanities and Social Sciences</a>, <span class="u-tcGrayDarker">Graduate Student</span></div></div></div></div><div class="sidebar-cta-container"><button class="ds2-5-button hidden profile-cta-button grow js-profile-follow-button" data-broccoli-component="user-info.follow-button" data-click-track="profile-user-info-follow-button" data-follow-user-fname="Jane" data-follow-user-id="14260800" data-follow-user-source="profile_button" data-has-google="false"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">add</span>Follow</button><button class="ds2-5-button hidden profile-cta-button grow js-profile-unfollow-button" data-broccoli-component="user-info.unfollow-button" data-click-track="profile-user-info-unfollow-button" data-unfollow-user-id="14260800"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">done</span>Following</button></div></div><div class="user-stats-container"><a><div class="stat-container js-profile-followers"><p class="label">Followers</p><p class="data">12</p></div></a><a><div class="stat-container js-profile-followees" data-broccoli-component="user-info.followees-count" data-click-track="profile-expand-user-info-following"><p class="label">Following</p><p class="data">8</p></div></a><a><div class="stat-container js-profile-coauthors" data-broccoli-component="user-info.coauthors-count" data-click-track="profile-expand-user-info-coauthors"><p class="label">Co-authors</p><p class="data">7</p></div></a><span><div class="stat-container"><p class="label"><span class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></div><div class="user-bio-container"><div class="profile-bio fake-truncate js-profile-about" style="margin: 0px;"><b>Address: </b>Brisbane, Queensland<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="14260800" href="https://www.academia.edu/Documents/in/Archaeology"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://queenslandmuseum.academia.edu/JaneSkippington","location":"/JaneSkippington","scheme":"https","host":"queenslandmuseum.academia.edu","port":null,"pathname":"/JaneSkippington","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Archaeology"]}" data-trace="false" 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data-dom-id="Pill-react-component-64ecef63-9bfc-407c-be98-cb703df74557"></div> <div id="Pill-react-component-64ecef63-9bfc-407c-be98-cb703df74557"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="14260800" href="https://www.academia.edu/Documents/in/Philosophy"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Philosophy"]}" data-trace="false" data-dom-id="Pill-react-component-69c28a1b-42ec-4fd8-997a-86fd5dedca13"></div> <div id="Pill-react-component-69c28a1b-42ec-4fd8-997a-86fd5dedca13"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="14260800" href="https://www.academia.edu/Documents/in/Sociology"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Sociology"]}" data-trace="false" data-dom-id="Pill-react-component-bfcbc685-a599-4ecd-9f4d-dddac7ca4707"></div> <div id="Pill-react-component-bfcbc685-a599-4ecd-9f4d-dddac7ca4707"></div> </a></div></div><div class="external-links-container"><ul class="profile-links new-profile js-UserInfo-social"><li class="profile-profiles js-social-profiles-container"><i class="fa fa-spin fa-spinner"></i></li></ul></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="nav-container backbone-profile-documents-nav hidden-xs"><ul class="nav-tablist" role="tablist"><li class="nav-chip active" role="presentation"><a data-section-name="" data-toggle="tab" href="#all" role="tab">all</a></li><li class="nav-chip" role="presentation"><a class="js-profile-docs-nav-section u-textTruncate" data-click-track="profile-works-tab" data-section-name="Conference-Presentations" data-toggle="tab" href="#conferencepresentations" role="tab" title="Conference Presentations"><span>4</span> <span class="ds2-5-body-sm-bold">Conference Presentations</span></a></li><li class="nav-chip" role="presentation"><a class="js-profile-docs-nav-section u-textTruncate" data-click-track="profile-works-tab" data-section-name="Papers" data-toggle="tab" href="#papers" role="tab" title="Papers"><span>8</span> <span class="ds2-5-body-sm-bold">Papers</span></a></li><li class="nav-chip" role="presentation"><a class="js-profile-docs-nav-section u-textTruncate" data-click-track="profile-works-tab" data-section-name="Theses" data-toggle="tab" href="#theses" role="tab" title="Theses"><span>1</span> <span class="ds2-5-body-sm-bold">Theses</span></a></li></ul></div><div class="divider ds-divider-16" style="margin: 0px;"></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Conference Presentations" id="Conference Presentations"><h3 class="profile--tab_heading_container">Conference Presentations by Jane Skippington</h3></div><div class="js-work-strip profile--work_container" data-work-id="34887881"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/34887881/Reconcilable_differences_Integrating_sustainable_heritage_practice_with_commercial_work_programs"><img alt="Research paper thumbnail of Reconcilable differences: Integrating sustainable heritage practice with commercial work programs" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/34887881/Reconcilable_differences_Integrating_sustainable_heritage_practice_with_commercial_work_programs">Reconcilable differences: Integrating sustainable heritage practice with commercial work programs</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Authors - Skippington, J., Strano, A. and D. Bunting Unpublished paper presented at the Aust...</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">Authors - Skippington, J., Strano, A.  and D. 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We present the chemical analysis of five basalt flakes from three sites on Moloka'i, Hawaiian Islands: a well-dated colonisation period stratified coastal mound, a craft specialisation locale and an upland buried habitation. Wavelength dispersive 脳-ray fluorescence (WDXRF) and inductively coupled plasma mass spectrometry (ICP-MS) were used to identify the origin of the artefacts. Radiocarbon dating results indicate that the recently discovered Pu'u P膩pa'i (Moloka'i) quarry was likely utilised from the colonisation period beginning in the 12th century through to the late 1600s, making it one of the oldest, continuously used quarries in the archipelago. Aspects of island colonisation and community networks are discussed including the possible emergence of the elite control of resources.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2eb248f0ad1a931d8db890a42ed1b070" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":103922647,"asset_id":104107666,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/103922647/download_file?st=MTczMzA5MTg0Niw4LjIyMi4yMDguMTQ2&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="104107666"><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="104107666"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 104107666; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=104107666]").text(description); $(".js-view-count[data-work-id=104107666]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 104107666; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='104107666']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 104107666, 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: "2eb248f0ad1a931d8db890a42ed1b070" } } $('.js-work-strip[data-work-id=104107666]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":104107666,"title":"Indirectly Dating one of the Oldest Adze Quarries in the Hawaiian Islands Provides Insights into the Colonisation Process and Community Networks","translated_title":"","metadata":{"abstract":"Chemically characterising stone tools in distant habitation sites and matching artefacts to quarries is some of the strongest evidence archaeologists have to define the spatial and temporal limits of ancient interaction networks. 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Prehistory","url":"https://www.academia.edu/Documents/in/Oceanic_Prehistory"}],"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="74831406"><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/74831406/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia"><img alt="Research paper thumbnail of Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia" class="work-thumbnail" src="https://attachments.academia-assets.com/82842327/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/74831406/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia">Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia</a></div><div class="wp-workCard_item"><span>Molecules</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysi...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b1c4302beb0e3062020bde9e4bd476fe" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":82842327,"asset_id":74831406,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/82842327/download_file?st=MTczMzA5MTg0Niw4LjIyMi4yMDguMTQ2&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="74831406"><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="74831406"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 74831406; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=74831406]").text(description); $(".js-view-count[data-work-id=74831406]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 74831406; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='74831406']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 74831406, 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: "b1c4302beb0e3062020bde9e4bd476fe" } } $('.js-work-strip[data-work-id=74831406]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":74831406,"title":"Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia","translated_title":"","metadata":{"abstract":"This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...","publisher":"MDPI AG","publication_name":"Molecules"},"translated_abstract":"This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...","internal_url":"https://www.academia.edu/74831406/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia","translated_internal_url":"","created_at":"2022-03-28T17:01:14.008-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":14260800,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":82842327,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/82842327/thumbnails/1.jpg","file_name":"pdf.pdf","download_url":"https://www.academia.edu/attachments/82842327/download_file?st=MTczMzA5MTg0Niw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Isotopic_Indications_of_Late_Pleistocene.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/82842327/pdf-libre.pdf?1648514472=\u0026response-content-disposition=attachment%3B+filename%3DIsotopic_Indications_of_Late_Pleistocene.pdf\u0026Expires=1733085678\u0026Signature=cxV81qePHAnZg0axdhH6fsv2LFUpVahIdPZj~~oAmlpBPjn5dh8sallBTfv~kg7zDarkcHB2UkvZt6N-5CSEPF-Yhyw22lHZiwC4G085CSJhhZM2TgT3atmFpdcSR56OOXSAPDbjY~byRttR9THxaeQqFtRlTlm0wiRZ6jom5mQrOYKCwO980GeETgvNeIibwRnQwugH8fPhyR0D~FKO1D1i23XYUnUfCP8bKEFidE7LFwjDHsDU5G7W1WdcugxRdEPPjvcki8QX7nT69j6WsRzTVTGuz8ffI3FAKb3oBLbWSJn2yu534IAGL-bEXjVtlXnjjX6w1PSbyJhgYTaFJw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia","translated_slug":"","page_count":12,"language":"en","content_type":"Work","owner":{"id":14260800,"first_name":"Jane","middle_initials":null,"last_name":"Skippington","page_name":"JaneSkippington","domain_name":"queenslandmuseum","created_at":"2014-07-23T14:34:51.925-07:00","display_name":"Jane Skippington","url":"https://queenslandmuseum.academia.edu/JaneSkippington"},"attachments":[{"id":82842327,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/82842327/thumbnails/1.jpg","file_name":"pdf.pdf","download_url":"https://www.academia.edu/attachments/82842327/download_file?st=MTczMzA5MTg0Niw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Isotopic_Indications_of_Late_Pleistocene.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/82842327/pdf-libre.pdf?1648514472=\u0026response-content-disposition=attachment%3B+filename%3DIsotopic_Indications_of_Late_Pleistocene.pdf\u0026Expires=1733085678\u0026Signature=cxV81qePHAnZg0axdhH6fsv2LFUpVahIdPZj~~oAmlpBPjn5dh8sallBTfv~kg7zDarkcHB2UkvZt6N-5CSEPF-Yhyw22lHZiwC4G085CSJhhZM2TgT3atmFpdcSR56OOXSAPDbjY~byRttR9THxaeQqFtRlTlm0wiRZ6jom5mQrOYKCwO980GeETgvNeIibwRnQwugH8fPhyR0D~FKO1D1i23XYUnUfCP8bKEFidE7LFwjDHsDU5G7W1WdcugxRdEPPjvcki8QX7nT69j6WsRzTVTGuz8ffI3FAKb3oBLbWSJn2yu534IAGL-bEXjVtlXnjjX6w1PSbyJhgYTaFJw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":531,"name":"Organic Chemistry","url":"https://www.academia.edu/Documents/in/Organic_Chemistry"},{"id":328449,"name":"Molecules","url":"https://www.academia.edu/Documents/in/Molecules"}],"urls":[{"id":18895935,"url":"https://www.mdpi.com/1420-3049/26/9/2582/pdf"}]}, 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="74831405"><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/74831405/Early_human_occupation_of_a_maritime_desert_Barrow_Island_North_West_Australia"><img alt="Research paper thumbnail of Early human occupation of a maritime desert, Barrow Island, North-West Australia" class="work-thumbnail" src="https://attachments.academia-assets.com/82842401/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/74831405/Early_human_occupation_of_a_maritime_desert_Barrow_Island_North_West_Australia">Early human occupation of a maritime desert, Barrow Island, North-West Australia</a></div><div class="wp-workCard_item"><span>Quaternary Science Reviews</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6edf511f702e30abc2bcd2ff307c9d8e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":82842401,"asset_id":74831405,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/82842401/download_file?st=MTczMzA5MTg0Niw4LjIyMi4yMDguMTQ2&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="74831405"><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="74831405"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 74831405; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "6edf511f702e30abc2bcd2ff307c9d8e" } } $('.js-work-strip[data-work-id=74831405]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":74831405,"title":"Early human occupation of a maritime desert, Barrow Island, North-West Australia","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"Archaeological deposits from Boodie Cave on Barrow Island, northwest Australia reveal some of the earliest evidence for Aboriginal occupation of Australia, along with demonstrating early systematic use of marine resources by modern peoples outside of Africa. Barrow Island is a large (202 km 2) limestone continental island located on the NorthWest Shelf of Australia, optimally located to sample past use of both the Pleistocene coastline and extensive arid coastal plains. An interdisciplinary team forming the Barrow Island Archaeology Project (BIAP) has addressed questions focusing on the antiquity of occupation of coastal deserts by hunter-gatherers; the use and distribution of marine resources from the coast to the interior; and the productivity of the marine zone with changing sea levels. Boodie Cave is the largest of 20 stratified deposits identified on Barrow Island with 20 m 3 of cultural deposits excavated between 2013 and 2015. In this first major synthesis we focus on the dating and sedimentology of Boodie Cave to establish the framework for ongoing analysis of cultural materials. We present new data on these cultural assemblages-including charcoal, faunal remains and lithics-integrated with micromorphology, sedimentary history and dating by four independent laboratories. First occupation occurs between 51.1 and 46.2 ka, overlapping with the earliest dates for occupation of Australia. Marine resources are incorporated into dietary assemblages by 42.5 ka and continue to be transported to the cave through all periods of occupation, despite fluctuating sea levels and dramatic extensions of the coastal plain. The changing quantities of marine fauna through time reflect the varying distance of the cave from the contemporaneous shoreline. The dietary breadth of both arid zone terrestrial fauna and marine species increases after the Last Glacial Maximum and significantly so by the mid-Holocene. The cave is abandoned by 6.8 ka when the island becomes increasingly distant from the mainland coast.","publication_name":"Quaternary Science 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archaeology","url":"https://www.academia.edu/Documents/in/Island_archaeology"},{"id":14492,"name":"Coastal and Island Archaeology","url":"https://www.academia.edu/Documents/in/Coastal_and_Island_Archaeology"},{"id":28226,"name":"Bayesian Radiocarbon Dating","url":"https://www.academia.edu/Documents/in/Bayesian_Radiocarbon_Dating"},{"id":45999,"name":"Australian archaeology","url":"https://www.academia.edu/Documents/in/Australian_archaeology"},{"id":93755,"name":"History and archaeology","url":"https://www.academia.edu/Documents/in/History_and_archaeology"},{"id":185526,"name":"Last Glacial Maximum","url":"https://www.academia.edu/Documents/in/Last_Glacial_Maximum"},{"id":373417,"name":"Quaternary Science Reviews","url":"https://www.academia.edu/Documents/in/Quaternary_Science_Reviews"},{"id":483062,"name":"Optically Stimulated Luminescence","url":"https://www.academia.edu/Documents/in/Optically_Stimulated_Luminescence"},{"id":993249,"name":"Islands Archaeology","url":"https://www.academia.edu/Documents/in/Islands_Archaeology"},{"id":1288612,"name":"Hunter Gatherer Archaeology","url":"https://www.academia.edu/Documents/in/Hunter_Gatherer_Archaeology"}],"urls":[{"id":18895934,"url":"http://api.elsevier.com/content/article/PII:S0277379117302640?httpAccept=text/xml"}]}, 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="73864676"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/73864676/Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology"><img alt="Research paper thumbnail of Macropods and measurables: A critical review of contemporary isotopic approaches to palaeo-environmental reconstructions in Australian zooarchaeology" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/73864676/Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology">Macropods and measurables: A critical review of contemporary isotopic approaches to palaeo-environmental reconstructions in Australian zooarchaeology</a></div><div class="wp-workCard_item"><span>Journal of Archaeological Science: Reports</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally appli...</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">Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally applied tool for reconstructing past environments and ecological histories from archaeological sites. For Australia, a substantial corpus of foundational literature has competently established the environmental sources of isotopic variation in modern kangaroo and wallaby species. However, despite the pervasive distribution of these kinds of macropods in contemporary and archaeological contexts, isotopic techniques are utilised infrequently. Our review of the history of macropod isotopic analysis identifies and proposes solutions to the complexities that have inhibited its widespread application in Australian archaeology. This includes a description of relevant basic principles including ecology, physiology and isotopic fractionation. To support our claims for the considerable research potential of macropod remains, we present preliminary analyses of tooth enamel carbonates from archaeological deposits at Boodie Cave, Barrow Island, located in Australia&#39;s northwest arid zone.</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="73864676"><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="73864676"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 73864676; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=73864676]").text(description); $(".js-view-count[data-work-id=73864676]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 73864676; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='73864676']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 73864676, 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" } } $('.js-work-strip[data-work-id=73864676]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":73864676,"title":"Macropods and measurables: A critical review of contemporary isotopic approaches to palaeo-environmental reconstructions in Australian zooarchaeology","translated_title":"","metadata":{"abstract":"Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally applied tool for reconstructing past environments and ecological histories from archaeological sites. For Australia, a substantial corpus of foundational literature has competently established the environmental sources of isotopic variation in modern kangaroo and wallaby species. However, despite the pervasive distribution of these kinds of macropods in contemporary and archaeological contexts, isotopic techniques are utilised infrequently. Our review of the history of macropod isotopic analysis identifies and proposes solutions to the complexities that have inhibited its widespread application in Australian archaeology. This includes a description of relevant basic principles including ecology, physiology and isotopic fractionation. To support our claims for the considerable research potential of macropod remains, we present preliminary analyses of tooth enamel carbonates from archaeological deposits at Boodie Cave, Barrow Island, located in Australia\u0026#39;s northwest arid zone.","publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":2018,"errors":{}},"publication_name":"Journal of Archaeological Science: Reports"},"translated_abstract":"Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally applied tool for reconstructing past environments and ecological histories from archaeological sites. For Australia, a substantial corpus of foundational literature has competently established the environmental sources of isotopic variation in modern kangaroo and wallaby species. However, despite the pervasive distribution of these kinds of macropods in contemporary and archaeological contexts, isotopic techniques are utilised infrequently. Our review of the history of macropod isotopic analysis identifies and proposes solutions to the complexities that have inhibited its widespread application in Australian archaeology. This includes a description of relevant basic principles including ecology, physiology and isotopic fractionation. To support our claims for the considerable research potential of macropod remains, we present preliminary analyses of tooth enamel carbonates from archaeological deposits at Boodie Cave, Barrow Island, located in Australia\u0026#39;s northwest arid zone.","internal_url":"https://www.academia.edu/73864676/Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology","translated_internal_url":"","created_at":"2022-03-16T00:20:07.588-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":14260800,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":14260800,"first_name":"Jane","middle_initials":null,"last_name":"Skippington","page_name":"JaneSkippington","domain_name":"queenslandmuseum","created_at":"2014-07-23T14:34:51.925-07:00","display_name":"Jane Skippington","url":"https://queenslandmuseum.academia.edu/JaneSkippington"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"}],"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="70482604"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/70482604/Macropod_Bone_Apatite_Isotopic_Analysis_as_Evidence_for_Recent_Environmental_Change_at_Bandicoot_Bay_Pearling_Camp_Barrow_Island_Australia"><img alt="Research paper thumbnail of Macropod Bone Apatite Isotopic Analysis as Evidence for Recent Environmental Change at Bandicoot Bay Pearling Camp, Barrow Island, Australia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/70482604/Macropod_Bone_Apatite_Isotopic_Analysis_as_Evidence_for_Recent_Environmental_Change_at_Bandicoot_Bay_Pearling_Camp_Barrow_Island_Australia">Macropod Bone Apatite Isotopic Analysis as Evidence for Recent Environmental Change at Bandicoot Bay Pearling Camp, Barrow Island, Australia</a></div><div class="wp-workCard_item"><span>International Journal of Historical Archaeology</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="70482604"><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="70482604"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 70482604; 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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="64370818"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/64370818/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia"><img alt="Research paper thumbnail of Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/64370818/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia">Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia</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://queenslandmuseum.academia.edu/JaneSkippington">Jane Skippington</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://uwa.academia.edu/PeterVeth">Peter Veth</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysi...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...</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="64370818"><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="64370818"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 64370818; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=64370818]").text(description); $(".js-view-count[data-work-id=64370818]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 64370818; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='64370818']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 64370818, 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" } } $('.js-work-strip[data-work-id=64370818]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":64370818,"title":"Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia","translated_title":"","metadata":{"abstract":"This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. 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We present the chemical analysis of five basalt flakes from three sites on Moloka'i, Hawaiian Islands: a well-dated colonisation period stratified coastal mound, a craft specialisation locale and an upland buried habitation. Wavelength dispersive 脳-ray fluorescence (WDXRF) and inductively coupled plasma mass spectrometry (ICP-MS) were used to identify the origin of the artefacts. Radiocarbon dating results indicate that the recently discovered Pu'u P膩pa'i (Moloka'i) quarry was likely utilised from the colonisation period beginning in the 12th century through to the late 1600s, making it one of the oldest, continuously used quarries in the archipelago. Aspects of island colonisation and community networks are discussed including the possible emergence of the elite control of resources.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2eb248f0ad1a931d8db890a42ed1b070" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":103922647,"asset_id":104107666,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/103922647/download_file?st=MTczMzA5MTg0Nyw4LjIyMi4yMDguMTQ2&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="104107666"><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="104107666"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 104107666; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=104107666]").text(description); $(".js-view-count[data-work-id=104107666]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 104107666; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='104107666']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 104107666, 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: "2eb248f0ad1a931d8db890a42ed1b070" } } $('.js-work-strip[data-work-id=104107666]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":104107666,"title":"Indirectly Dating one of the Oldest Adze Quarries in the Hawaiian Islands Provides Insights into the Colonisation Process and Community Networks","translated_title":"","metadata":{"abstract":"Chemically characterising stone tools in distant habitation sites and matching artefacts to quarries is some of the strongest evidence archaeologists have to define the spatial and temporal limits of ancient interaction networks. 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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/74831406/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia">Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia</a></div><div class="wp-workCard_item"><span>Molecules</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysi...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b1c4302beb0e3062020bde9e4bd476fe" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":82842327,"asset_id":74831406,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/82842327/download_file?st=MTczMzA5MTg0Nyw4LjIyMi4yMDguMTQ2&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="74831406"><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="74831406"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 74831406; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=74831406]").text(description); $(".js-view-count[data-work-id=74831406]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 74831406; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='74831406']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 74831406, 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: "b1c4302beb0e3062020bde9e4bd476fe" } } $('.js-work-strip[data-work-id=74831406]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":74831406,"title":"Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia","translated_title":"","metadata":{"abstract":"This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...","publisher":"MDPI AG","publication_name":"Molecules"},"translated_abstract":"This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...","internal_url":"https://www.academia.edu/74831406/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia","translated_internal_url":"","created_at":"2022-03-28T17:01:14.008-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":14260800,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":82842327,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/82842327/thumbnails/1.jpg","file_name":"pdf.pdf","download_url":"https://www.academia.edu/attachments/82842327/download_file?st=MTczMzA5MTg0Nyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Isotopic_Indications_of_Late_Pleistocene.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/82842327/pdf-libre.pdf?1648514472=\u0026response-content-disposition=attachment%3B+filename%3DIsotopic_Indications_of_Late_Pleistocene.pdf\u0026Expires=1733085678\u0026Signature=cxV81qePHAnZg0axdhH6fsv2LFUpVahIdPZj~~oAmlpBPjn5dh8sallBTfv~kg7zDarkcHB2UkvZt6N-5CSEPF-Yhyw22lHZiwC4G085CSJhhZM2TgT3atmFpdcSR56OOXSAPDbjY~byRttR9THxaeQqFtRlTlm0wiRZ6jom5mQrOYKCwO980GeETgvNeIibwRnQwugH8fPhyR0D~FKO1D1i23XYUnUfCP8bKEFidE7LFwjDHsDU5G7W1WdcugxRdEPPjvcki8QX7nT69j6WsRzTVTGuz8ffI3FAKb3oBLbWSJn2yu534IAGL-bEXjVtlXnjjX6w1PSbyJhgYTaFJw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia","translated_slug":"","page_count":12,"language":"en","content_type":"Work","owner":{"id":14260800,"first_name":"Jane","middle_initials":null,"last_name":"Skippington","page_name":"JaneSkippington","domain_name":"queenslandmuseum","created_at":"2014-07-23T14:34:51.925-07:00","display_name":"Jane Skippington","url":"https://queenslandmuseum.academia.edu/JaneSkippington"},"attachments":[{"id":82842327,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/82842327/thumbnails/1.jpg","file_name":"pdf.pdf","download_url":"https://www.academia.edu/attachments/82842327/download_file?st=MTczMzA5MTg0Nyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Isotopic_Indications_of_Late_Pleistocene.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/82842327/pdf-libre.pdf?1648514472=\u0026response-content-disposition=attachment%3B+filename%3DIsotopic_Indications_of_Late_Pleistocene.pdf\u0026Expires=1733085678\u0026Signature=cxV81qePHAnZg0axdhH6fsv2LFUpVahIdPZj~~oAmlpBPjn5dh8sallBTfv~kg7zDarkcHB2UkvZt6N-5CSEPF-Yhyw22lHZiwC4G085CSJhhZM2TgT3atmFpdcSR56OOXSAPDbjY~byRttR9THxaeQqFtRlTlm0wiRZ6jom5mQrOYKCwO980GeETgvNeIibwRnQwugH8fPhyR0D~FKO1D1i23XYUnUfCP8bKEFidE7LFwjDHsDU5G7W1WdcugxRdEPPjvcki8QX7nT69j6WsRzTVTGuz8ffI3FAKb3oBLbWSJn2yu534IAGL-bEXjVtlXnjjX6w1PSbyJhgYTaFJw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":531,"name":"Organic Chemistry","url":"https://www.academia.edu/Documents/in/Organic_Chemistry"},{"id":328449,"name":"Molecules","url":"https://www.academia.edu/Documents/in/Molecules"}],"urls":[{"id":18895935,"url":"https://www.mdpi.com/1420-3049/26/9/2582/pdf"}]}, 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="74831405"><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/74831405/Early_human_occupation_of_a_maritime_desert_Barrow_Island_North_West_Australia"><img alt="Research paper thumbnail of Early human occupation of a maritime desert, Barrow Island, North-West Australia" class="work-thumbnail" src="https://attachments.academia-assets.com/82842401/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/74831405/Early_human_occupation_of_a_maritime_desert_Barrow_Island_North_West_Australia">Early human occupation of a maritime desert, Barrow Island, North-West Australia</a></div><div class="wp-workCard_item"><span>Quaternary Science Reviews</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6edf511f702e30abc2bcd2ff307c9d8e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":82842401,"asset_id":74831405,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/82842401/download_file?st=MTczMzA5MTg0Nyw4LjIyMi4yMDguMTQ2&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="74831405"><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="74831405"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 74831405; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "6edf511f702e30abc2bcd2ff307c9d8e" } } $('.js-work-strip[data-work-id=74831405]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":74831405,"title":"Early human occupation of a maritime desert, Barrow Island, North-West Australia","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"Archaeological deposits from Boodie Cave on Barrow Island, northwest Australia reveal some of the earliest evidence for Aboriginal occupation of Australia, along with demonstrating early systematic use of marine resources by modern peoples outside of Africa. Barrow Island is a large (202 km 2) limestone continental island located on the NorthWest Shelf of Australia, optimally located to sample past use of both the Pleistocene coastline and extensive arid coastal plains. An interdisciplinary team forming the Barrow Island Archaeology Project (BIAP) has addressed questions focusing on the antiquity of occupation of coastal deserts by hunter-gatherers; the use and distribution of marine resources from the coast to the interior; and the productivity of the marine zone with changing sea levels. Boodie Cave is the largest of 20 stratified deposits identified on Barrow Island with 20 m 3 of cultural deposits excavated between 2013 and 2015. In this first major synthesis we focus on the dating and sedimentology of Boodie Cave to establish the framework for ongoing analysis of cultural materials. We present new data on these cultural assemblages-including charcoal, faunal remains and lithics-integrated with micromorphology, sedimentary history and dating by four independent laboratories. First occupation occurs between 51.1 and 46.2 ka, overlapping with the earliest dates for occupation of Australia. Marine resources are incorporated into dietary assemblages by 42.5 ka and continue to be transported to the cave through all periods of occupation, despite fluctuating sea levels and dramatic extensions of the coastal plain. The changing quantities of marine fauna through time reflect the varying distance of the cave from the contemporaneous shoreline. The dietary breadth of both arid zone terrestrial fauna and marine species increases after the Last Glacial Maximum and significantly so by the mid-Holocene. The cave is abandoned by 6.8 ka when the island becomes increasingly distant from the mainland coast.","publication_name":"Quaternary Science 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archaeology","url":"https://www.academia.edu/Documents/in/Island_archaeology"},{"id":14492,"name":"Coastal and Island Archaeology","url":"https://www.academia.edu/Documents/in/Coastal_and_Island_Archaeology"},{"id":28226,"name":"Bayesian Radiocarbon Dating","url":"https://www.academia.edu/Documents/in/Bayesian_Radiocarbon_Dating"},{"id":45999,"name":"Australian archaeology","url":"https://www.academia.edu/Documents/in/Australian_archaeology"},{"id":93755,"name":"History and archaeology","url":"https://www.academia.edu/Documents/in/History_and_archaeology"},{"id":185526,"name":"Last Glacial Maximum","url":"https://www.academia.edu/Documents/in/Last_Glacial_Maximum"},{"id":373417,"name":"Quaternary Science Reviews","url":"https://www.academia.edu/Documents/in/Quaternary_Science_Reviews"},{"id":483062,"name":"Optically Stimulated Luminescence","url":"https://www.academia.edu/Documents/in/Optically_Stimulated_Luminescence"},{"id":993249,"name":"Islands Archaeology","url":"https://www.academia.edu/Documents/in/Islands_Archaeology"},{"id":1288612,"name":"Hunter Gatherer Archaeology","url":"https://www.academia.edu/Documents/in/Hunter_Gatherer_Archaeology"}],"urls":[{"id":18895934,"url":"http://api.elsevier.com/content/article/PII:S0277379117302640?httpAccept=text/xml"}]}, 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="73864676"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/73864676/Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology"><img alt="Research paper thumbnail of Macropods and measurables: A critical review of contemporary isotopic approaches to palaeo-environmental reconstructions in Australian zooarchaeology" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/73864676/Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology">Macropods and measurables: A critical review of contemporary isotopic approaches to palaeo-environmental reconstructions in Australian zooarchaeology</a></div><div class="wp-workCard_item"><span>Journal of Archaeological Science: Reports</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally appli...</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">Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally applied tool for reconstructing past environments and ecological histories from archaeological sites. For Australia, a substantial corpus of foundational literature has competently established the environmental sources of isotopic variation in modern kangaroo and wallaby species. However, despite the pervasive distribution of these kinds of macropods in contemporary and archaeological contexts, isotopic techniques are utilised infrequently. Our review of the history of macropod isotopic analysis identifies and proposes solutions to the complexities that have inhibited its widespread application in Australian archaeology. This includes a description of relevant basic principles including ecology, physiology and isotopic fractionation. To support our claims for the considerable research potential of macropod remains, we present preliminary analyses of tooth enamel carbonates from archaeological deposits at Boodie Cave, Barrow Island, located in Australia&#39;s northwest arid zone.</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="73864676"><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="73864676"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 73864676; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=73864676]").text(description); $(".js-view-count[data-work-id=73864676]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 73864676; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='73864676']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 73864676, 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" } } $('.js-work-strip[data-work-id=73864676]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":73864676,"title":"Macropods and measurables: A critical review of contemporary isotopic approaches to palaeo-environmental reconstructions in Australian zooarchaeology","translated_title":"","metadata":{"abstract":"Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally applied tool for reconstructing past environments and ecological histories from archaeological sites. For Australia, a substantial corpus of foundational literature has competently established the environmental sources of isotopic variation in modern kangaroo and wallaby species. However, despite the pervasive distribution of these kinds of macropods in contemporary and archaeological contexts, isotopic techniques are utilised infrequently. Our review of the history of macropod isotopic analysis identifies and proposes solutions to the complexities that have inhibited its widespread application in Australian archaeology. This includes a description of relevant basic principles including ecology, physiology and isotopic fractionation. To support our claims for the considerable research potential of macropod remains, we present preliminary analyses of tooth enamel carbonates from archaeological deposits at Boodie Cave, Barrow Island, located in Australia\u0026#39;s northwest arid zone.","publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":2018,"errors":{}},"publication_name":"Journal of Archaeological Science: Reports"},"translated_abstract":"Abstract Stable isotopic analyses of herbivorous mammal remains are a powerful and globally applied tool for reconstructing past environments and ecological histories from archaeological sites. For Australia, a substantial corpus of foundational literature has competently established the environmental sources of isotopic variation in modern kangaroo and wallaby species. However, despite the pervasive distribution of these kinds of macropods in contemporary and archaeological contexts, isotopic techniques are utilised infrequently. Our review of the history of macropod isotopic analysis identifies and proposes solutions to the complexities that have inhibited its widespread application in Australian archaeology. This includes a description of relevant basic principles including ecology, physiology and isotopic fractionation. To support our claims for the considerable research potential of macropod remains, we present preliminary analyses of tooth enamel carbonates from archaeological deposits at Boodie Cave, Barrow Island, located in Australia\u0026#39;s northwest arid zone.","internal_url":"https://www.academia.edu/73864676/Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology","translated_internal_url":"","created_at":"2022-03-16T00:20:07.588-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":14260800,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Macropods_and_measurables_A_critical_review_of_contemporary_isotopic_approaches_to_palaeo_environmental_reconstructions_in_Australian_zooarchaeology","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":14260800,"first_name":"Jane","middle_initials":null,"last_name":"Skippington","page_name":"JaneSkippington","domain_name":"queenslandmuseum","created_at":"2014-07-23T14:34:51.925-07:00","display_name":"Jane Skippington","url":"https://queenslandmuseum.academia.edu/JaneSkippington"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"}],"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="70482604"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/70482604/Macropod_Bone_Apatite_Isotopic_Analysis_as_Evidence_for_Recent_Environmental_Change_at_Bandicoot_Bay_Pearling_Camp_Barrow_Island_Australia"><img alt="Research paper thumbnail of Macropod Bone Apatite Isotopic Analysis as Evidence for Recent Environmental Change at Bandicoot Bay Pearling Camp, Barrow Island, Australia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/70482604/Macropod_Bone_Apatite_Isotopic_Analysis_as_Evidence_for_Recent_Environmental_Change_at_Bandicoot_Bay_Pearling_Camp_Barrow_Island_Australia">Macropod Bone Apatite Isotopic Analysis as Evidence for Recent Environmental Change at Bandicoot Bay Pearling Camp, Barrow Island, Australia</a></div><div class="wp-workCard_item"><span>International Journal of Historical Archaeology</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="70482604"><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="70482604"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 70482604; 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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="64370818"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/64370818/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia"><img alt="Research paper thumbnail of Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/64370818/Isotopic_Indications_of_Late_Pleistocene_and_Holocene_Paleoenvironmental_Changes_at_Boodie_Cave_Archaeological_Site_Barrow_Island_Western_Australia">Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia</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://queenslandmuseum.academia.edu/JaneSkippington">Jane Skippington</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://uwa.academia.edu/PeterVeth">Peter Veth</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysi...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. Stable carbon (未13C) and oxygen (未18O) isotope ratios were analyzed from archaeological and modern spectacled hare wallaby (Lagorchestes conspicillatus) and hill kangaroo (Osphranter robustus) tooth enamel carbonates from Boodie Cave on Barrow Island in Western Australia. 未18O results track the dynamic paleoecological history at Boodie Cave including a clear shift towards increasing aridity preceding the onset of the Last Glacial Maximum and a period of increased humidity in the early to mid-Holocene. Enamel 未13C reflects divergent species feeding ecology and may imply a long-term shift toward increasing diversity in vegetation structure. This study contributes new data to the carbonate-isotope record for Australian fauna and demonstrates the significant potent...</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="64370818"><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="64370818"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 64370818; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=64370818]").text(description); $(".js-view-count[data-work-id=64370818]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 64370818; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='64370818']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 64370818, 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" } } $('.js-work-strip[data-work-id=64370818]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":64370818,"title":"Isotopic Indications of Late Pleistocene and Holocene Paleoenvironmental Changes at Boodie Cave Archaeological Site, Barrow Island, Western Australia","translated_title":"","metadata":{"abstract":"This paper presents the first application of mammal tooth enamel carbonate stable isotope analysis for the purpose of investigating late Pleistocene鈥揺arly Holocene environmental change in an Australian archaeological context. 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