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Barnes" 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/15974665/18787762/18748072/s200_christopher.barnes.jpg" /></div><div class="title-container"><h1 class="ds2-5-heading-sans-serif-sm">Christopher R . Barnes</h1><div class="affiliations-container fake-truncate js-profile-affiliations"><div><a class="u-tcGrayDarker" href="https://uvic.academia.edu/">University of Victoria</a>, <a class="u-tcGrayDarker" href="https://uvic.academia.edu/Departments/School_of_Earth_and_Ocean_Sciences/Documents">School of Earth and Ocean Sciences</a>, <span class="u-tcGrayDarker">Emeritus</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="Christopher" data-follow-user-id="15974665" 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="15974665"><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">16</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">16</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">4</p></div></a><a href="/ChristopherBarnes/mentions"><div class="stat-container"><p class="label">Mentions</p><p class="data">4,173</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;">Chris Barnes is currently Professor Emeritus in the School of Earth and Ocean Sciences (SEOS), University of Victoria, BC, Canada. Following his B.Sc. from the University of Birmingham, UK (1961) and Ph.D. from the University of Ottawa (1964), and a NATO Research Fellowship at the University of Wales, Chris started his academic career at the University of Waterloo, Ontario in 1965, serving as Chair of Earth Sciences from 1975 to 1981. In a similar position at Memorial University of Newfoundland (1981-87), he merged geology and geophysics and established the Centre of Earth Resources Research. From 1987-1989, as Director General, Sedimentary and Marine Branch, Geological Survey of Canada, he managed four regional offices and also the offshore Frontier Geoscience Program on all three coasts. At the University of Victoria, Chris was Director of the Centre of Earth and Ocean Research (1989-2000), founded the School of Earth and Ocean Sciences (1991-2002), and then served as the founding Director of NEPTUNE Canada (2001-2011), the world’s first regional cabled ocean observatory (800km; $150M).<br />Chris has served on many boards and councils, including as President of the Geological Association of Canada, the Canadian Geoscience Council, and the Academy of Science of the Royal Society of Canada; as Group Chair of both Earth Sciences and Interdisciplinary for the Natural Sciences and Engineering Research Council of Canada (NSERC), and three separate terms as Chair of the Council of Canadian Earth Science Departments. He has been a member of the Canadian Nuclear Safety Commission (14 years), the International Ocean Drilling Program, the International Commission on Stratigraphy and the BC Science Council. <br /><br />He was the first Chair of the United Nations ITU-WMO-UNESCO IOC Joint Task Force on SMART submarine telecommunications cables for ocean climate monitoring and (tsunami) disaster warning (2012-16). He continues to serve on the Science Advisory Committees of both the Canadian Ocean Tracking Network and the Canary Islands Ocean Observatory. <br />Chris’ research focuses on understanding Early Paleozoic oceans, climate and life, principally using conodont micropaleontology, stratigraphy, and isotope geochemistry, with nearly 200 publications and 250 conference abstracts. <br />For his various contributions, he was awarded the J. Willis Ambrose, Elkanah Billings, and Past Presidents medals of the Geological Association of Canada (GAC), the Bancroft Award (Royal Society of Canada), the Pander Society Medal, the Micropalaeontological Society’s Brady Medal, the Queen’s Golden and Diamond Jubilee Medals, and an Honorary D.Sc. from the University of Waterloo and Memorial University of Newfoundland. He is a Fellow of the Royal Society of Canada (RSC), the National Academy of Sciences, Cordoba, Argentina, and was appointed to the Order of Canada.<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span><a class="ri-more-link js-profile-ri-list-card" data-click-track="profile-user-info-primary-research-interest" data-has-card-for-ri-list="15974665">View All (6)</a></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="15974665" href="https://www.academia.edu/Documents/in/Oceanography"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://uvic.academia.edu/ChristopherBarnes","location":"/ChristopherBarnes","scheme":"https","host":"uvic.academia.edu","port":null,"pathname":"/ChristopherBarnes","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":["Oceanography"]}" data-trace="false" data-dom-id="Pill-react-component-8521d9d3-adee-439b-9e6c-7ae444b49f97"></div> <div id="Pill-react-component-8521d9d3-adee-439b-9e6c-7ae444b49f97"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="15974665" href="https://www.academia.edu/Documents/in/Marine_Science"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Marine Science"]}" data-trace="false" data-dom-id="Pill-react-component-6a01310b-2ba2-47b9-9415-c86c34fb0360"></div> <div id="Pill-react-component-6a01310b-2ba2-47b9-9415-c86c34fb0360"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="15974665" href="https://www.academia.edu/Documents/in/Education"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Education"]}" data-trace="false" data-dom-id="Pill-react-component-51714b20-3aea-4ca4-acaa-e449272c4604"></div> <div id="Pill-react-component-51714b20-3aea-4ca4-acaa-e449272c4604"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="15974665" href="https://www.academia.edu/Documents/in/Business"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Business"]}" data-trace="false" data-dom-id="Pill-react-component-362c64b1-530c-43ad-bcca-867232e0f451"></div> <div id="Pill-react-component-362c64b1-530c-43ad-bcca-867232e0f451"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="15974665" 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-43d5dc34-0754-49d2-9110-fdf7843cf4fe"></div> <div id="Pill-react-component-43d5dc34-0754-49d2-9110-fdf7843cf4fe"></div> </a></div></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Christopher R . Barnes</h3></div><div class="js-work-strip profile--work_container" data-work-id="123594971"><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/123594971/Zhang_and_Barnes_C_O_2004_GSL_SP"><img alt="Research paper thumbnail of Zhang&Barnes C-O 2004 GSL SP" class="work-thumbnail" src="https://attachments.academia-assets.com/117990800/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/123594971/Zhang_and_Barnes_C_O_2004_GSL_SP">Zhang&Barnes C-O 2004 GSL SP</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="15020e30eaf342d295074254a4dcd15b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":117990800,"asset_id":123594971,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/117990800/download_file?st=MTczNDE2MDIyNiw4LjIyMi4yMDguMTQ2&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="123594971"><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="123594971"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123594971; 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Dryad Digital Repository" 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/123560072/Data_from_Katian_Upper_Ordovician_conodonts_from_Wales_Dryad_Digital_Repository">Data from: Katian (Upper Ordovician) conodonts from Wales. Dryad Digital Repository</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Middle and upper Katian conodonts were previously known in the British Isles from relatively smal...</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">Middle and upper Katian conodonts were previously known in the British Isles from relatively small collections obtained from a few localities. The present study is mainly based on 17 samples containing more than 17 000 conodont elements from an approximately 14-m-thick succession of the Sholeshook Limestone Formation in a road cut near Whitland, South Wales, that yielded a diverse fauna of more than 40 taxa. It is dominated by representatives of Amorphognathus, Aphelognathus/Plectodina and Eocarniodus along with several coniform taxa. Representatives of Decoriconus, Istorinus and Sagittodontina are reported from the Ordovician of UK for the first time. The fauna is a typical representative of the British Province of the Atlantic Realm and includes a mixture of taxa of North American, Baltoscandic and Mediterranean affinities along with pandemic species. Based on the presence of many elements of Amorphognathus ordovicicus and some morphologically advanced specimens of Amorphognathus superbus, the Sholeshook Limestone Formation is referred to the lower A. ordovicicus Zone. Most of the unit is also coeval with Zone 2 of the Cautleyan Stage in the British regional stage classification, and stage slice Ka3 of the middle Katian Stage in the global stratigraphical classification, an age assignment consistent with data from trilobites, graptolites and chitinozoans. The unusually large collection of M elements of Amorphognathus provides insight into the complex morphological variation in this element of some Katian species of this genus. The Sholeshook conodont fauna is similar to those of the Crug and Birdshill limestones, but differs in several respects from the slightly older ones from the Caradocian type area in the Welsh Borderland. 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It will comprise five main observatory nodes (100m-2700m water depths), an 800km backbone cable delivering 10kV DC power and 10Gbps communications bandwidth to hundreds of sensors, with a design life of 25 years. Infrastructure funding ($100M) and initial operational funding ($20M) have been secured. NC&#39;s wet plant design, manufacture and installation was contracted to Alcatel-Lucent Submarine Networks; junction boxes were designed and built by OceanWorks. UVic leads a consortium of 12 Canadian universities, and hosts the coastal VENUS cabled observatory with Ocean Networks Canada providing management oversight. Experiments will focus on: earthquake dynamics and tsunami hazards; fluid fluxes in both ocean crust and sediments, including gas hydrates; ocean/climate dynamics, including acidification and nutrien...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="123560067"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="123560067"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560067; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560067]").text(description); $(".js-view-count[data-work-id=123560067]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560067; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560067']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560067, 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" } } $('.js-work-strip[data-work-id=123560067]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560067,"title":"Latest developments in building the world's first regional cabled observatory: NEPTUNE Canada","translated_title":"","metadata":{"abstract":"NEPTUNE Canada (NC; www.neptunecanada.ca) plans to complete installation of the world\u0026#39;s first regional cabled ocean observatory in late 2009 off Canada\u0026#39;s west coast. 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UVic leads a consortium of 12 Canadian universities, and hosts the coastal VENUS cabled observatory with Ocean Networks Canada providing management oversight. 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Across the network, high resolution seismic information will elucidate tectonic processes such as earthquakes and strain, and a tsunami system will allow determination of open ocean tsunami amplitude, propagation direction, and speed. 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Installation of the first suite of instruments and connectivity equipment was completed in 2009, so this system now provides the continuous power and bandwidth to collect integrated data on physical, chemical, geological, and biological gradients at temporal resolutions relevant to</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="123560062"><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="123560062"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560062; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560062]").text(description); $(".js-view-count[data-work-id=123560062]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560062; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560062']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560062, 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" } } $('.js-work-strip[data-work-id=123560062]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560062,"title":"Large research infrastructure for Earth-Ocean Science: Challenges of multidisciplinary integration across hardware, software, and people networks","translated_title":"","metadata":{"abstract":"NEPTUNE Canada is operating a regional cabled ocean observatory across the northern Juan de Fuca Plate in the northeastern Pacific. 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This provides continuous power and high bandwidth to collect integrated data on physical, chemical, geological, and biological gradients at temporal resolutions relevant to the dynamics of the earth-ocean system. 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Our recent intense study of Midcontinent conodonts from the St. George Group, Port au Port Peninsula, western Newfoundland, has shown that seven major conodont lineages, involving some 33 multielement species, completely terminate in the late Tremadoc Series, within an interval of a few metres, at a level between the Lower Ordovician conodont Fauna C and Fauna D. The extinction event occurs during the peak of a regressive phase within the deposition of the St. George Group and at a time of apparent global eustatic fall at or slightly below the Tremadoc-Arenig series boundary. This important extinction bioevent has been recognized throughout the Midcontinent Realm in North America. Stratigraphic background Four formations, collectively 550 m thick, occur within the St. George Group, in ascending order the Watts Bight, Boat Harbour, Catoche and Aguathuna formations. The sedimentology and stratigraphy of the St. George Group has been documented well by Pratt and James (1982), Knight and James (1987), James et al. (1989) and</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="597b13270a143a0bf8bd43e9dc5095c4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":117963736,"asset_id":123560059,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/117963736/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="123560059"><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="123560059"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560059; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560059]").text(description); $(".js-view-count[data-work-id=123560059]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560059; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560059']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560059, 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: "597b13270a143a0bf8bd43e9dc5095c4" } } $('.js-work-strip[data-work-id=123560059]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560059,"title":"A major conodont extinction event during the early Ordovician within the Midcontinent realm","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"The major change in the Lower Ordovician conodont faunas of the Midcontinent Realm was recognized by earlier workers. 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Provinces, communities, and the proposed nektobenthic habit of Ordovician conodontophorid...</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">Page 1. Provinces, communities, and the proposed nektobenthic habit of Ordovician conodontophorids CHRISTOPHER R. BARNES AND LARS E. FAHREUS Barnes, C. 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A mobile Internet operated vehicle was used as an instrument platform to monitor and study up to 2000 m2of sediment surface in real‐time. In 2010 the first mission of the robot was to investigate the importance of oscillatory deep ocean currents on methane release at continental margins. Previously, other experimental studies have indicated that methane release from gas hydrate outcrops is diffusion‐controlled and should be much higher than seepage from buried hydrate in semipermeable sediments. Our results show that periods of enhanced bottom currents associated with diurnal shelf waves, internal semidiurnal tides, and also wind‐generated near‐inertial motions ...</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="123560054"><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="123560054"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560054; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560054]").text(description); $(".js-view-count[data-work-id=123560054]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560054; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560054']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560054, 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" } } $('.js-work-strip[data-work-id=123560054]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560054,"title":"Ocean circulation promotes methane release from gas hydrate outcrops at the NEPTUNE Canada Barkley Canyon node","translated_title":"","metadata":{"abstract":"The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and time‐series observations with mobile robots on gas hydrates and benthic community structure on a small plateau of about 1 km2 at a water depth of 870 m in Barkley Canyon, about 100 km offshore Vancouver Island, British Columbia. 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Our results show that periods of enhanced bottom currents associated with diurnal shelf waves, internal semidiurnal tides, and also wind‐generated near‐inertial motions ...","internal_url":"https://www.academia.edu/123560054/Ocean_circulation_promotes_methane_release_from_gas_hydrate_outcrops_at_the_NEPTUNE_Canada_Barkley_Canyon_node","translated_internal_url":"","created_at":"2024-09-04T10:29:37.378-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Ocean_circulation_promotes_methane_release_from_gas_hydrate_outcrops_at_the_NEPTUNE_Canada_Barkley_Canyon_node","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and time‐series observations with mobile robots on gas hydrates and benthic community structure on a small plateau of about 1 km2 at a water depth of 870 m in Barkley Canyon, about 100 km offshore Vancouver Island, British Columbia. 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Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...</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="123560052"><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="123560052"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560052; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560052]").text(description); $(".js-view-count[data-work-id=123560052]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560052; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560052']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560052, 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" } } $('.js-work-strip[data-work-id=123560052]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560052,"title":"Late Cambrian and Early Ordovician conodont communities from platform and slope facies, western Newfoundland: a statistical approach","translated_title":"","metadata":{"abstract":"Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. 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Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...","publisher":"Geological Society of London","publication_date":{"day":null,"month":null,"year":2004,"errors":{}},"publication_name":"Geological Society, London, Special Publications"},"translated_abstract":"Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...","internal_url":"https://www.academia.edu/123560052/Late_Cambrian_and_Early_Ordovician_conodont_communities_from_platform_and_slope_facies_western_Newfoundland_a_statistical_approach","translated_internal_url":"","created_at":"2024-09-04T10:29:36.657-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Late_Cambrian_and_Early_Ordovician_conodont_communities_from_platform_and_slope_facies_western_Newfoundland_a_statistical_approach","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":366440,"name":"Facies","url":"https://www.academia.edu/Documents/in/Facies"}],"urls":[{"id":44467861,"url":"https://syndication.highwire.org/content/doi/10.1144/GSL.SP.2004.230.01.04"}]}, 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="123560050"><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/123560050/Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia"><img alt="Research paper thumbnail of Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia" 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/123560050/Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia">Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia</a></div><div class="wp-workCard_item"><span>Canadian Journal of Earth Sciences</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus...</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 age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...</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="123560050"><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="123560050"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560050; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560050]").text(description); $(".js-view-count[data-work-id=123560050]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560050; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560050']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560050, 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" } } $('.js-work-strip[data-work-id=123560050]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560050,"title":"Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia","translated_title":"","metadata":{"abstract":"The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...","publisher":"Canadian Science Publishing","publication_date":{"day":null,"month":null,"year":2007,"errors":{}},"publication_name":"Canadian Journal of Earth Sciences"},"translated_abstract":"The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...","internal_url":"https://www.academia.edu/123560050/Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia","translated_internal_url":"","created_at":"2024-09-04T10:29:35.868-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10770,"name":"Biostratigraphy","url":"https://www.academia.edu/Documents/in/Biostratigraphy"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":109828,"name":"Fauna","url":"https://www.academia.edu/Documents/in/Fauna"},{"id":198379,"name":"British Columbia","url":"https://www.academia.edu/Documents/in/British_Columbia"}],"urls":[{"id":44467860,"url":"http://www.nrcresearchpress.com/doi/pdf/10.1139/e07-047"}]}, 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="123560048"><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/123560048/Upper_Cambrian_to_Lower_Silurian_stratigraphic_framework_of_platform_to_basin_fades_northeastern_British_Columbia"><img alt="Research paper thumbnail of Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin fades, northeastern British Columbia" class="work-thumbnail" src="https://attachments.academia-assets.com/117963732/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/123560048/Upper_Cambrian_to_Lower_Silurian_stratigraphic_framework_of_platform_to_basin_fades_northeastern_British_Columbia">Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin fades, northeastern British Columbia</a></div><div class="wp-workCard_item"><span>Bulletin of Canadian Petroleum Geology</span><span>, 2000</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passiv...</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 lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passive tectonic evolution of the rifted northern margin of Laurentia. The stratigraphy of the Kechika Formation, Road River Group and Skoki Formation in northern British Columbia has been described previously during reconnaissance mapping. This study provides detailed stratigraphic descriptions of Upper Cambrian to Lower Silurian units from 9 key sections which span an east-west transect from the Macdonald Platform to the Kechika Trough, and 3 sections across the parautochthonous Cassiar Terrane. The transect lies within an interpreted upper plate of an asymmetrically rifted margin. Regionally, renewed phases of extension of the margin throughout the lower Paleozoic are recorded in abrupt lateral and vertical facies changes and pulses of volcanism. The tectono-stratigraphic framework was influenced by eustatic sea-level changes. Revised stratigraphic terminology proposed herein includes the division of the Kechika Formation into 5 formal members: the Lloyd George, Quentin, Grey Peak, Haworth and Mount Sheffield members. The Skoki Formation comprises three distinct, formal members defined as the Sikanni Chief, Keily and Redfern members. The Road River Group is divided into three new formations: the Ospika Formation, the Pesika Formation (formerly the Silurian Limestone) and the Kwadacha Formation (formerly the Silurian Siltstone). The Ospika Formation is further subdivided into five formal members: the Cloudmaker, Finlay Limestone, Chesterfield, Finbow Shale and Ware members. RESUME Les strates du PalEozoique infrrieur du miogdoclinal de la Cordillbre canadienne du Nord documentent l'rvolution tectonique non passive de la marge drrivre du rift du nord de Laurentia.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2efbd2b15c88360eae9d1e5a14fccf19" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":117963732,"asset_id":123560048,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/117963732/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="123560048"><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="123560048"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560048; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560048]").text(description); $(".js-view-count[data-work-id=123560048]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560048; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560048']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560048, 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: "2efbd2b15c88360eae9d1e5a14fccf19" } } $('.js-work-strip[data-work-id=123560048]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560048,"title":"Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin fades, northeastern British Columbia","translated_title":"","metadata":{"publisher":"Canadian Society of Petroleum Geologists","grobid_abstract":"The lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passive tectonic evolution of the rifted northern margin of Laurentia. The stratigraphy of the Kechika Formation, Road River Group and Skoki Formation in northern British Columbia has been described previously during reconnaissance mapping. This study provides detailed stratigraphic descriptions of Upper Cambrian to Lower Silurian units from 9 key sections which span an east-west transect from the Macdonald Platform to the Kechika Trough, and 3 sections across the parautochthonous Cassiar Terrane. The transect lies within an interpreted upper plate of an asymmetrically rifted margin. Regionally, renewed phases of extension of the margin throughout the lower Paleozoic are recorded in abrupt lateral and vertical facies changes and pulses of volcanism. The tectono-stratigraphic framework was influenced by eustatic sea-level changes. Revised stratigraphic terminology proposed herein includes the division of the Kechika Formation into 5 formal members: the Lloyd George, Quentin, Grey Peak, Haworth and Mount Sheffield members. The Skoki Formation comprises three distinct, formal members defined as the Sikanni Chief, Keily and Redfern members. The Road River Group is divided into three new formations: the Ospika Formation, the Pesika Formation (formerly the Silurian Limestone) and the Kwadacha Formation (formerly the Silurian Siltstone). The Ospika Formation is further subdivided into five formal members: the Cloudmaker, Finlay Limestone, Chesterfield, Finbow Shale and Ware members. RESUME Les strates du PalEozoique infrrieur du miogdoclinal de la Cordillbre canadienne du Nord documentent l'rvolution tectonique non passive de la marge drrivre du rift du nord de Laurentia.","publication_date":{"day":null,"month":null,"year":2000,"errors":{}},"publication_name":"Bulletin of Canadian Petroleum Geology","grobid_abstract_attachment_id":117963732},"translated_abstract":null,"internal_url":"https://www.academia.edu/123560048/Upper_Cambrian_to_Lower_Silurian_stratigraphic_framework_of_platform_to_basin_fades_northeastern_British_Columbia","translated_internal_url":"","created_at":"2024-09-04T10:29:35.360-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":117963732,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/117963732/thumbnails/1.jpg","file_name":"48.2.12320240904-1-gifa6i.pdf","download_url":"https://www.academia.edu/attachments/117963732/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Upper_Cambrian_to_Lower_Silurian_stratig.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/117963732/48.2.12320240904-1-gifa6i-libre.pdf?1725473335=\u0026response-content-disposition=attachment%3B+filename%3DUpper_Cambrian_to_Lower_Silurian_stratig.pdf\u0026Expires=1734163827\u0026Signature=OVKLatQcDOipntSiry9BR6OL5XTGaHzD~r-cdlM6nFDqBIMR6hsVC18fK6hIMeDPQBf4-jeqVGR7f67m0734ElSOHTNwtnuC5SdWFXvYIlGKttkFiC5fJ3nt7~kotJxng4X3hKipxQWFwt2qnT4tRESfn04teOMrX02nwph~rXzOhryGR6jRqRSBG4G2o9-QxYX0PXnS~V9soNjGhSmMCV~SF-PniJRACQqTuGYgVj1oolWcud~rV4VrXPaGjC2YceMs3klpsmLc6wpAP1S~83C7W4VvZUTbcjFjAPSIO1VYoE~VKHt60c8M3iNcq81Mpv-64qFJJ17ln8q4S5tcNw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Upper_Cambrian_to_Lower_Silurian_stratigraphic_framework_of_platform_to_basin_fades_northeastern_British_Columbia","translated_slug":"","page_count":27,"language":"en","content_type":"Work","summary":"The lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passive tectonic evolution of the rifted northern margin of Laurentia. The stratigraphy of the Kechika Formation, Road River Group and Skoki Formation in northern British Columbia has been described previously during reconnaissance mapping. This study provides detailed stratigraphic descriptions of Upper Cambrian to Lower Silurian units from 9 key sections which span an east-west transect from the Macdonald Platform to the Kechika Trough, and 3 sections across the parautochthonous Cassiar Terrane. The transect lies within an interpreted upper plate of an asymmetrically rifted margin. Regionally, renewed phases of extension of the margin throughout the lower Paleozoic are recorded in abrupt lateral and vertical facies changes and pulses of volcanism. The tectono-stratigraphic framework was influenced by eustatic sea-level changes. Revised stratigraphic terminology proposed herein includes the division of the Kechika Formation into 5 formal members: the Lloyd George, Quentin, Grey Peak, Haworth and Mount Sheffield members. The Skoki Formation comprises three distinct, formal members defined as the Sikanni Chief, Keily and Redfern members. The Road River Group is divided into three new formations: the Ospika Formation, the Pesika Formation (formerly the Silurian Limestone) and the Kwadacha Formation (formerly the Silurian Siltstone). The Ospika Formation is further subdivided into five formal members: the Cloudmaker, Finlay Limestone, Chesterfield, Finbow Shale and Ware members. RESUME Les strates du PalEozoique infrrieur du miogdoclinal de la Cordillbre canadienne du Nord documentent l'rvolution tectonique non passive de la marge drrivre du rift du nord de Laurentia.","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . 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JOURNAL OF PALEONTOLOGY, V. 47, NO. 4, P. 760-790, 5 PL., 2 TEXT-FIGS., JULY 1973 LOWER A...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Page 1. 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The purpose of SMART Cables is to support climate and ocean observation, sea level monitoring, observations of Earth structure, and tsunami and earthquake early warning and disaster risk reduction, including hazard quantification. Recent advances include regional SMART pilot systems that are the first steps to trans-ocean and global implementation. Examples of pilots include: InSEA wet demonstration project off Sicily at the European Multidisciplinary Seafloor and water column Observatory Western Ionian Facility; New Caledonia and Vanuatu; French Polynesia Natitua South system connecting Tahiti to Tubaui to the south; Indonesia starting with short pilot systems working toward systems for the Sumatra-Java megathrust zone; and the CAM-2...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="41a4d334b94fa19eaca45edbfa0a6611" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113042606,"asset_id":117091515,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113042606/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="117091515"><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="117091515"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117091515; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117091515]").text(description); $(".js-view-count[data-work-id=117091515]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117091515; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117091515']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117091515, 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: "41a4d334b94fa19eaca45edbfa0a6611" } } $('.js-work-strip[data-work-id=117091515]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117091515,"title":"SMART Subsea Cables for Observing the Earth and Ocean, Mitigating Environmental Hazards, and Supporting the Blue Economy","translated_title":"","metadata":{"abstract":"The Joint Task Force, Science Monitoring And Reliable Telecommunications (JTF SMART) Subsea Cables, is working to integrate environmental sensors for ocean bottom temperature, pressure, and seismic acceleration into submarine telecommunications cables. 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Some 220 melted micrometeorites were recovered from the magnetic fraction of six samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from five samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. The micrometeorite-bearing formations span the late Tremadocian to the late Darriliwian (~480-460 Ma), which is consistent with a period of elevated flux of extraterrestrial material, as recorded several thousand kilometres away from coeval horizons in Scotland, Sweden and central China.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d1987e58a617b1d5d96a173a2782cb4d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":108995802,"asset_id":111462385,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/108995802/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="111462385"><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="111462385"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111462385; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111462385]").text(description); $(".js-view-count[data-work-id=111462385]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111462385; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111462385']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111462385, 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: "d1987e58a617b1d5d96a173a2782cb4d" } } $('.js-work-strip[data-work-id=111462385]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111462385,"title":"Cosmic spherules from the Ordovician of Argentina","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Ordovician Micrometeorites: Discovery and Analysis in Argentina","grobid_abstract":"The discovery of magnetic spherules in acid-insoluble residues from conodont samples encouraged a systematic search for Ordovician micrometeorites from northwestern Argentina. Some 220 melted micrometeorites were recovered from the magnetic fraction of six samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from five samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. 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Dryad Digital Repository" 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/123560072/Data_from_Katian_Upper_Ordovician_conodonts_from_Wales_Dryad_Digital_Repository">Data from: Katian (Upper Ordovician) conodonts from Wales. Dryad Digital Repository</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Middle and upper Katian conodonts were previously known in the British Isles from relatively smal...</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">Middle and upper Katian conodonts were previously known in the British Isles from relatively small collections obtained from a few localities. The present study is mainly based on 17 samples containing more than 17 000 conodont elements from an approximately 14-m-thick succession of the Sholeshook Limestone Formation in a road cut near Whitland, South Wales, that yielded a diverse fauna of more than 40 taxa. It is dominated by representatives of Amorphognathus, Aphelognathus/Plectodina and Eocarniodus along with several coniform taxa. Representatives of Decoriconus, Istorinus and Sagittodontina are reported from the Ordovician of UK for the first time. The fauna is a typical representative of the British Province of the Atlantic Realm and includes a mixture of taxa of North American, Baltoscandic and Mediterranean affinities along with pandemic species. Based on the presence of many elements of Amorphognathus ordovicicus and some morphologically advanced specimens of Amorphognathus superbus, the Sholeshook Limestone Formation is referred to the lower A. ordovicicus Zone. Most of the unit is also coeval with Zone 2 of the Cautleyan Stage in the British regional stage classification, and stage slice Ka3 of the middle Katian Stage in the global stratigraphical classification, an age assignment consistent with data from trilobites, graptolites and chitinozoans. The unusually large collection of M elements of Amorphognathus provides insight into the complex morphological variation in this element of some Katian species of this genus. The Sholeshook conodont fauna is similar to those of the Crug and Birdshill limestones, but differs in several respects from the slightly older ones from the Caradocian type area in the Welsh Borderland. Although having some species in common, the Sholeshook conodont fauna clearly differs from coeval Baltoscandic faunas and is even more different in composition compared with equivalent North American Midcontinent faunas</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="123560072"><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="123560072"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560072; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560072]").text(description); $(".js-view-count[data-work-id=123560072]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560072; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560072']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560072, 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" } } $('.js-work-strip[data-work-id=123560072]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560072,"title":"Data from: Katian (Upper Ordovician) conodonts from Wales. 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The present study is mainly based on 17 samples containing more than 17 000 conodont elements from an approximately 14-m-thick succession of the Sholeshook Limestone Formation in a road cut near Whitland, South Wales, that yielded a diverse fauna of more than 40 taxa. It is dominated by representatives of Amorphognathus, Aphelognathus/Plectodina and Eocarniodus along with several coniform taxa. Representatives of Decoriconus, Istorinus and Sagittodontina are reported from the Ordovician of UK for the first time. The fauna is a typical representative of the British Province of the Atlantic Realm and includes a mixture of taxa of North American, Baltoscandic and Mediterranean affinities along with pandemic species. Based on the presence of many elements of Amorphognathus ordovicicus and some morphologically advanced specimens of Amorphognathus superbus, the Sholeshook Limestone Formation is referred to the lower A. ordovicicus Zone. Most of the unit is also coeval with Zone 2 of the Cautleyan Stage in the British regional stage classification, and stage slice Ka3 of the middle Katian Stage in the global stratigraphical classification, an age assignment consistent with data from trilobites, graptolites and chitinozoans. The unusually large collection of M elements of Amorphognathus provides insight into the complex morphological variation in this element of some Katian species of this genus. The Sholeshook conodont fauna is similar to those of the Crug and Birdshill limestones, but differs in several respects from the slightly older ones from the Caradocian type area in the Welsh Borderland. Although having some species in common, the Sholeshook conodont fauna clearly differs from coeval Baltoscandic faunas and is even more different in composition compared with equivalent North American Midcontinent faunas","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . 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Proceedings of a symposium, Waterloo, Ontario, May 1975)</a></div><div class="wp-workCard_item"><span>Science</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="123560069"><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="123560069"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560069; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560069]").text(description); $(".js-view-count[data-work-id=123560069]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560069; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560069']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560069, 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" } } $('.js-work-strip[data-work-id=123560069]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560069,"title":"Microfossils. 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It will comprise five main observatory nodes (100m-2700m water depths), an 800km backbone cable delivering 10kV DC power and 10Gbps communications bandwidth to hundreds of sensors, with a design life of 25 years. Infrastructure funding ($100M) and initial operational funding ($20M) have been secured. NC&#39;s wet plant design, manufacture and installation was contracted to Alcatel-Lucent Submarine Networks; junction boxes were designed and built by OceanWorks. UVic leads a consortium of 12 Canadian universities, and hosts the coastal VENUS cabled observatory with Ocean Networks Canada providing management oversight. Experiments will focus on: earthquake dynamics and tsunami hazards; fluid fluxes in both ocean crust and sediments, including gas hydrates; ocean/climate dynamics, including acidification and nutrien...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="123560067"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="123560067"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560067; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560067]").text(description); $(".js-view-count[data-work-id=123560067]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560067; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560067']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560067, 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" } } $('.js-work-strip[data-work-id=123560067]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560067,"title":"Latest developments in building the world's first regional cabled observatory: NEPTUNE Canada","translated_title":"","metadata":{"abstract":"NEPTUNE Canada (NC; www.neptunecanada.ca) plans to complete installation of the world\u0026#39;s first regional cabled ocean observatory in late 2009 off Canada\u0026#39;s west coast. It will comprise five main observatory nodes (100m-2700m water depths), an 800km backbone cable delivering 10kV DC power and 10Gbps communications bandwidth to hundreds of sensors, with a design life of 25 years. Infrastructure funding ($100M) and initial operational funding ($20M) have been secured. NC\u0026#39;s wet plant design, manufacture and installation was contracted to Alcatel-Lucent Submarine Networks; junction boxes were designed and built by OceanWorks. UVic leads a consortium of 12 Canadian universities, and hosts the coastal VENUS cabled observatory with Ocean Networks Canada providing management oversight. Experiments will focus on: earthquake dynamics and tsunami hazards; fluid fluxes in both ocean crust and sediments, including gas hydrates; ocean/climate dynamics, including acidification and nutrien..."},"translated_abstract":"NEPTUNE Canada (NC; www.neptunecanada.ca) plans to complete installation of the world\u0026#39;s first regional cabled ocean observatory in late 2009 off Canada\u0026#39;s west coast. It will comprise five main observatory nodes (100m-2700m water depths), an 800km backbone cable delivering 10kV DC power and 10Gbps communications bandwidth to hundreds of sensors, with a design life of 25 years. Infrastructure funding ($100M) and initial operational funding ($20M) have been secured. NC\u0026#39;s wet plant design, manufacture and installation was contracted to Alcatel-Lucent Submarine Networks; junction boxes were designed and built by OceanWorks. UVic leads a consortium of 12 Canadian universities, and hosts the coastal VENUS cabled observatory with Ocean Networks Canada providing management oversight. Experiments will focus on: earthquake dynamics and tsunami hazards; fluid fluxes in both ocean crust and sediments, including gas hydrates; ocean/climate dynamics, including acidification and nutrien...","internal_url":"https://www.academia.edu/123560067/Latest_developments_in_building_the_worlds_first_regional_cabled_observatory_NEPTUNE_Canada","translated_internal_url":"","created_at":"2024-09-04T10:29:42.464-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Latest_developments_in_building_the_worlds_first_regional_cabled_observatory_NEPTUNE_Canada","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"NEPTUNE Canada (NC; www.neptunecanada.ca) plans to complete installation of the world\u0026#39;s first regional cabled ocean observatory in late 2009 off Canada\u0026#39;s west coast. It will comprise five main observatory nodes (100m-2700m water depths), an 800km backbone cable delivering 10kV DC power and 10Gbps communications bandwidth to hundreds of sensors, with a design life of 25 years. Infrastructure funding ($100M) and initial operational funding ($20M) have been secured. NC\u0026#39;s wet plant design, manufacture and installation was contracted to Alcatel-Lucent Submarine Networks; junction boxes were designed and built by OceanWorks. UVic leads a consortium of 12 Canadian universities, and hosts the coastal VENUS cabled observatory with Ocean Networks Canada providing management oversight. Experiments will focus on: earthquake dynamics and tsunami hazards; fluid fluxes in both ocean crust and sediments, including gas hydrates; ocean/climate dynamics, including acidification and nutrien...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="123560065"><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/123560065/NEPTUNE_Canada_Regional_Cabled_Observatory_Science_Plan"><img alt="Research paper thumbnail of NEPTUNE Canada Regional Cabled Observatory: Science Plan" 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/123560065/NEPTUNE_Canada_Regional_Cabled_Observatory_Science_Plan">NEPTUNE Canada Regional Cabled Observatory: Science Plan</a></div><div class="wp-workCard_item"><span>Oceans 2007</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Starting in 2007, NEPTUNE Canada will install an 800 km long regional cabled ocean observatory ac...</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">Starting in 2007, NEPTUNE Canada will install an 800 km long regional cabled ocean observatory across the northern Juan de Fuca Plate. Across the network, high resolution seismic information will elucidate tectonic processes such as earthquakes and strain, and a tsunami system will allow determination of open ocean tsunami amplitude, propagation direction, and speed. 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Installation of the first suite of instruments and connectivity equipment was completed in 2009, so this system now provides the continuous power and bandwidth to collect integrated data on physical, chemical, geological, and biological gradients at temporal resolutions relevant to</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="123560062"><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="123560062"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560062; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560062]").text(description); $(".js-view-count[data-work-id=123560062]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560062; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560062']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560062, 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" } } $('.js-work-strip[data-work-id=123560062]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560062,"title":"Large research infrastructure for Earth-Ocean Science: Challenges of multidisciplinary integration across hardware, software, and people networks","translated_title":"","metadata":{"abstract":"NEPTUNE Canada is operating a regional cabled ocean observatory across the northern Juan de Fuca Plate in the northeastern Pacific. 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This provides continuous power and high bandwidth to collect integrated data on physical, chemical, geological, and biological gradients at temporal resolutions relevant to the dynamics of the earth-ocean system. 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Our recent intense study of Midcontinent conodonts from the St. George Group, Port au Port Peninsula, western Newfoundland, has shown that seven major conodont lineages, involving some 33 multielement species, completely terminate in the late Tremadoc Series, within an interval of a few metres, at a level between the Lower Ordovician conodont Fauna C and Fauna D. The extinction event occurs during the peak of a regressive phase within the deposition of the St. George Group and at a time of apparent global eustatic fall at or slightly below the Tremadoc-Arenig series boundary. This important extinction bioevent has been recognized throughout the Midcontinent Realm in North America. Stratigraphic background Four formations, collectively 550 m thick, occur within the St. George Group, in ascending order the Watts Bight, Boat Harbour, Catoche and Aguathuna formations. The sedimentology and stratigraphy of the St. George Group has been documented well by Pratt and James (1982), Knight and James (1987), James et al. (1989) and</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="597b13270a143a0bf8bd43e9dc5095c4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":117963736,"asset_id":123560059,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/117963736/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="123560059"><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="123560059"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560059; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560059]").text(description); $(".js-view-count[data-work-id=123560059]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560059; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560059']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560059, 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: "597b13270a143a0bf8bd43e9dc5095c4" } } $('.js-work-strip[data-work-id=123560059]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560059,"title":"A major conodont extinction event during the early Ordovician within the Midcontinent realm","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"The major change in the Lower Ordovician conodont faunas of the Midcontinent Realm was recognized by earlier workers. 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Provinces, communities, and the proposed nektobenthic habit of Ordovician conodontophorid...</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">Page 1. Provinces, communities, and the proposed nektobenthic habit of Ordovician conodontophorids CHRISTOPHER R. BARNES AND LARS E. FAHREUS Barnes, C. R. &amp; Fdhraeus, LE 19750415: Provinces, communities ...</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="123560057"><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="123560057"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560057; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560057]").text(description); $(".js-view-count[data-work-id=123560057]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560057; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560057']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560057, 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" } } $('.js-work-strip[data-work-id=123560057]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560057,"title":"Provinces, communities, and the proposed nektobenthic habit of Ordovician conodontophorids","translated_title":"","metadata":{"abstract":"Page 1. 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R. \u0026amp; Fdhraeus, LE 19750415: Provinces, communities ...","internal_url":"https://www.academia.edu/123560057/Provinces_communities_and_the_proposed_nektobenthic_habit_of_Ordovician_conodontophorids","translated_internal_url":"","created_at":"2024-09-04T10:29:38.352-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Provinces_communities_and_the_proposed_nektobenthic_habit_of_Ordovician_conodontophorids","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Page 1. Provinces, communities, and the proposed nektobenthic habit of Ordovician conodontophorids CHRISTOPHER R. BARNES AND LARS E. FAHREUS Barnes, C. R. \u0026amp; Fdhraeus, LE 19750415: Provinces, communities ...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes","email":"UUNIUkZ1RGx3ZUREUnlydTF6V1AyeWNNNVREUkJDSUQ3dTc1TkZVanNBaz0tLStDbkdyTTlXNGU5TDZwajFCU2xDRXc9PQ==--ae39c18b66357fd4035e2079acd2eaee8a4c1bf4"},"attachments":[],"research_interests":[{"id":155,"name":"Evolutionary Biology","url":"https://www.academia.edu/Documents/in/Evolutionary_Biology"},{"id":289,"name":"Palaeogeography","url":"https://www.academia.edu/Documents/in/Palaeogeography"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":86151,"name":"Habit","url":"https://www.academia.edu/Documents/in/Habit"},{"id":109828,"name":"Fauna","url":"https://www.academia.edu/Documents/in/Fauna"}],"urls":[{"id":44467865,"url":"https://www.idunn.no/doi/pdf/10.1111/j.1502-3931.1975.tb01308.x"}]}, 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="123560054"><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/123560054/Ocean_circulation_promotes_methane_release_from_gas_hydrate_outcrops_at_the_NEPTUNE_Canada_Barkley_Canyon_node"><img alt="Research paper thumbnail of Ocean circulation promotes methane release from gas hydrate outcrops at the NEPTUNE Canada Barkley Canyon node" 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/123560054/Ocean_circulation_promotes_methane_release_from_gas_hydrate_outcrops_at_the_NEPTUNE_Canada_Barkley_Canyon_node">Ocean circulation promotes methane release from gas hydrate outcrops at the NEPTUNE Canada Barkley Canyon node</a></div><div class="wp-workCard_item"><span>Geophysical Research Letters</span><span>, 2012</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and time‐series observations with mobile robots on gas hydrates and benthic community structure on a small plateau of about 1 km2 at a water depth of 870 m in Barkley Canyon, about 100 km offshore Vancouver Island, British Columbia. A mobile Internet operated vehicle was used as an instrument platform to monitor and study up to 2000 m2of sediment surface in real‐time. In 2010 the first mission of the robot was to investigate the importance of oscillatory deep ocean currents on methane release at continental margins. Previously, other experimental studies have indicated that methane release from gas hydrate outcrops is diffusion‐controlled and should be much higher than seepage from buried hydrate in semipermeable sediments. Our results show that periods of enhanced bottom currents associated with diurnal shelf waves, internal semidiurnal tides, and also wind‐generated near‐inertial motions ...</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="123560054"><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="123560054"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560054; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560054]").text(description); $(".js-view-count[data-work-id=123560054]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560054; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560054']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560054, 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" } } $('.js-work-strip[data-work-id=123560054]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560054,"title":"Ocean circulation promotes methane release from gas hydrate outcrops at the NEPTUNE Canada Barkley Canyon node","translated_title":"","metadata":{"abstract":"The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and time‐series observations with mobile robots on gas hydrates and benthic community structure on a small plateau of about 1 km2 at a water depth of 870 m in Barkley Canyon, about 100 km offshore Vancouver Island, British Columbia. A mobile Internet operated vehicle was used as an instrument platform to monitor and study up to 2000 m2of sediment surface in real‐time. In 2010 the first mission of the robot was to investigate the importance of oscillatory deep ocean currents on methane release at continental margins. Previously, other experimental studies have indicated that methane release from gas hydrate outcrops is diffusion‐controlled and should be much higher than seepage from buried hydrate in semipermeable sediments. Our results show that periods of enhanced bottom currents associated with diurnal shelf waves, internal semidiurnal tides, and also wind‐generated near‐inertial motions ...","publisher":"American Geophysical Union (AGU)","publication_date":{"day":null,"month":null,"year":2012,"errors":{}},"publication_name":"Geophysical Research Letters"},"translated_abstract":"The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and time‐series observations with mobile robots on gas hydrates and benthic community structure on a small plateau of about 1 km2 at a water depth of 870 m in Barkley Canyon, about 100 km offshore Vancouver Island, British Columbia. A mobile Internet operated vehicle was used as an instrument platform to monitor and study up to 2000 m2of sediment surface in real‐time. In 2010 the first mission of the robot was to investigate the importance of oscillatory deep ocean currents on methane release at continental margins. Previously, other experimental studies have indicated that methane release from gas hydrate outcrops is diffusion‐controlled and should be much higher than seepage from buried hydrate in semipermeable sediments. Our results show that periods of enhanced bottom currents associated with diurnal shelf waves, internal semidiurnal tides, and also wind‐generated near‐inertial motions ...","internal_url":"https://www.academia.edu/123560054/Ocean_circulation_promotes_methane_release_from_gas_hydrate_outcrops_at_the_NEPTUNE_Canada_Barkley_Canyon_node","translated_internal_url":"","created_at":"2024-09-04T10:29:37.378-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Ocean_circulation_promotes_methane_release_from_gas_hydrate_outcrops_at_the_NEPTUNE_Canada_Barkley_Canyon_node","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The NEPTUNE Canada cabled observatory network enables non‐destructive, controlled experiments and time‐series observations with mobile robots on gas hydrates and benthic community structure on a small plateau of about 1 km2 at a water depth of 870 m in Barkley Canyon, about 100 km offshore Vancouver Island, British Columbia. A mobile Internet operated vehicle was used as an instrument platform to monitor and study up to 2000 m2of sediment surface in real‐time. In 2010 the first mission of the robot was to investigate the importance of oscillatory deep ocean currents on methane release at continental margins. Previously, other experimental studies have indicated that methane release from gas hydrate outcrops is diffusion‐controlled and should be much higher than seepage from buried hydrate in semipermeable sediments. Our results show that periods of enhanced bottom currents associated with diurnal shelf waves, internal semidiurnal tides, and also wind‐generated near‐inertial motions ...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":28235,"name":"Multidisciplinary","url":"https://www.academia.edu/Documents/in/Multidisciplinary"},{"id":156347,"name":"Methane","url":"https://www.academia.edu/Documents/in/Methane"},{"id":608332,"name":"Neptune","url":"https://www.academia.edu/Documents/in/Neptune"},{"id":1123280,"name":"Hydrate","url":"https://www.academia.edu/Documents/in/Hydrate"},{"id":1730898,"name":"Canyon","url":"https://www.academia.edu/Documents/in/Canyon"}],"urls":[{"id":44467863,"url":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2012GL052462"}]}, 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="123560052"><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/123560052/Late_Cambrian_and_Early_Ordovician_conodont_communities_from_platform_and_slope_facies_western_Newfoundland_a_statistical_approach"><img alt="Research paper thumbnail of Late Cambrian and Early Ordovician conodont communities from platform and slope facies, western Newfoundland: a statistical approach" 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/123560052/Late_Cambrian_and_Early_Ordovician_conodont_communities_from_platform_and_slope_facies_western_Newfoundland_a_statistical_approach">Late Cambrian and Early Ordovician conodont communities from platform and slope facies, western Newfoundland: a statistical approach</a></div><div class="wp-workCard_item"><span>Geological Society, London, Special Publications</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfou...</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">Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...</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="123560052"><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="123560052"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560052; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560052]").text(description); $(".js-view-count[data-work-id=123560052]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560052; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560052']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560052, 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" } } $('.js-work-strip[data-work-id=123560052]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560052,"title":"Late Cambrian and Early Ordovician conodont communities from platform and slope facies, western Newfoundland: a statistical approach","translated_title":"","metadata":{"abstract":"Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...","publisher":"Geological Society of London","publication_date":{"day":null,"month":null,"year":2004,"errors":{}},"publication_name":"Geological Society, London, Special Publications"},"translated_abstract":"Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...","internal_url":"https://www.academia.edu/123560052/Late_Cambrian_and_Early_Ordovician_conodont_communities_from_platform_and_slope_facies_western_Newfoundland_a_statistical_approach","translated_internal_url":"","created_at":"2024-09-04T10:29:36.657-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Late_Cambrian_and_Early_Ordovician_conodont_communities_from_platform_and_slope_facies_western_Newfoundland_a_statistical_approach","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Twelve conodont communities and assemblages in the Cambrian-Ordovician interval of western Newfoundland are recognized by four cluster analyses, which include 18 468 identifiable conodont specimens recovered from 230 conodont-bearing samples from four stratigraphic sections. Each section represents a different facies: platform, upper proximal slope, lower proximal slope, and distal slope. The 12 conodont communities and assemblages were differentiated into pelagic and nektobenthic communities as well as both the assemblages with a mixture of pelagic and nektobenthic communities and transported assemblage. The distribution of conodont communities along the platform-to-slope environmental gradient shows some gradational relationships. Relative sea-level curves derived in part from the distribution pattern of conodont communities reveal a major sea-level drop in the latest Cordylodus proavus Zone time, and two major sea-level rises in the early Iapetognathus fluctivagus Zone time and e...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":366440,"name":"Facies","url":"https://www.academia.edu/Documents/in/Facies"}],"urls":[{"id":44467861,"url":"https://syndication.highwire.org/content/doi/10.1144/GSL.SP.2004.230.01.04"}]}, 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="123560050"><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/123560050/Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia"><img alt="Research paper thumbnail of Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia" 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/123560050/Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia">Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia</a></div><div class="wp-workCard_item"><span>Canadian Journal of Earth Sciences</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus...</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 age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...</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="123560050"><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="123560050"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560050; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560050]").text(description); $(".js-view-count[data-work-id=123560050]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560050; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560050']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560050, 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" } } $('.js-work-strip[data-work-id=123560050]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560050,"title":"Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia","translated_title":"","metadata":{"abstract":"The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...","publisher":"Canadian Science Publishing","publication_date":{"day":null,"month":null,"year":2007,"errors":{}},"publication_name":"Canadian Journal of Earth Sciences"},"translated_abstract":"The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...","internal_url":"https://www.academia.edu/123560050/Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia","translated_internal_url":"","created_at":"2024-09-04T10:29:35.868-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":15974665,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Conodont_biostratigraphy_of_the_latest_Cambrian_Early_Ordovician_upper_McKay_Group_southeastern_British_Columbia","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The age of the upper McKay Group based on conodont biostratigraphy is latest Cambrian (Cordylodus proavus Zone) to late Early Ordovician (middle Floian; Oepikodus communis Zone). A collection of 12 940 conodont elements was recovered from 306 samples of upper McKay Group strata exposed in the Western Main Ranges of the southern Canadian Rocky Mountains, southeastern British Columbia. The conodont fauna is assigned to 53 species representing 30 genera. Twelve zones are recognized, two of which are cosmopolitan: Cordylodus proavus Zone and Iapetognathus Zone. Seven Midcontinent Realm zones, in ascending order, include Polycostatus falsioneotensis, Rossodus tenuis, Rossodus manitouensis, low diversity interval, Scolopodus subrex, and Acodus kechikaensis zones, and Tropodus sweeti Subzone (of the Oepikodus communis Zone). Three Atlantic Realm zones, in ascending order, include Cordylodus angulatus, Acodus deltatus, and Paroistodus proteus zones. The zonation for the upper McKay Group es...","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . Barnes","url":"https://uvic.academia.edu/ChristopherBarnes"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10770,"name":"Biostratigraphy","url":"https://www.academia.edu/Documents/in/Biostratigraphy"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":109828,"name":"Fauna","url":"https://www.academia.edu/Documents/in/Fauna"},{"id":198379,"name":"British Columbia","url":"https://www.academia.edu/Documents/in/British_Columbia"}],"urls":[{"id":44467860,"url":"http://www.nrcresearchpress.com/doi/pdf/10.1139/e07-047"}]}, 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="123560048"><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/123560048/Upper_Cambrian_to_Lower_Silurian_stratigraphic_framework_of_platform_to_basin_fades_northeastern_British_Columbia"><img alt="Research paper thumbnail of Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin fades, northeastern British Columbia" class="work-thumbnail" src="https://attachments.academia-assets.com/117963732/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/123560048/Upper_Cambrian_to_Lower_Silurian_stratigraphic_framework_of_platform_to_basin_fades_northeastern_British_Columbia">Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin fades, northeastern British Columbia</a></div><div class="wp-workCard_item"><span>Bulletin of Canadian Petroleum Geology</span><span>, 2000</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passiv...</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 lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passive tectonic evolution of the rifted northern margin of Laurentia. The stratigraphy of the Kechika Formation, Road River Group and Skoki Formation in northern British Columbia has been described previously during reconnaissance mapping. This study provides detailed stratigraphic descriptions of Upper Cambrian to Lower Silurian units from 9 key sections which span an east-west transect from the Macdonald Platform to the Kechika Trough, and 3 sections across the parautochthonous Cassiar Terrane. The transect lies within an interpreted upper plate of an asymmetrically rifted margin. Regionally, renewed phases of extension of the margin throughout the lower Paleozoic are recorded in abrupt lateral and vertical facies changes and pulses of volcanism. The tectono-stratigraphic framework was influenced by eustatic sea-level changes. Revised stratigraphic terminology proposed herein includes the division of the Kechika Formation into 5 formal members: the Lloyd George, Quentin, Grey Peak, Haworth and Mount Sheffield members. The Skoki Formation comprises three distinct, formal members defined as the Sikanni Chief, Keily and Redfern members. The Road River Group is divided into three new formations: the Ospika Formation, the Pesika Formation (formerly the Silurian Limestone) and the Kwadacha Formation (formerly the Silurian Siltstone). The Ospika Formation is further subdivided into five formal members: the Cloudmaker, Finlay Limestone, Chesterfield, Finbow Shale and Ware members. RESUME Les strates du PalEozoique infrrieur du miogdoclinal de la Cordillbre canadienne du Nord documentent l'rvolution tectonique non passive de la marge drrivre du rift du nord de Laurentia.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2efbd2b15c88360eae9d1e5a14fccf19" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":117963732,"asset_id":123560048,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/117963732/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="123560048"><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="123560048"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 123560048; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=123560048]").text(description); $(".js-view-count[data-work-id=123560048]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 123560048; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='123560048']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 123560048, 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: "2efbd2b15c88360eae9d1e5a14fccf19" } } $('.js-work-strip[data-work-id=123560048]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":123560048,"title":"Upper Cambrian to Lower Silurian stratigraphic framework of platform-to-basin fades, northeastern British Columbia","translated_title":"","metadata":{"publisher":"Canadian Society of Petroleum Geologists","grobid_abstract":"The lower Paleozoic strata of the Northern Canadian Cordilleran Miogeocline document a non-passive tectonic evolution of the rifted northern margin of Laurentia. The stratigraphy of the Kechika Formation, Road River Group and Skoki Formation in northern British Columbia has been described previously during reconnaissance mapping. This study provides detailed stratigraphic descriptions of Upper Cambrian to Lower Silurian units from 9 key sections which span an east-west transect from the Macdonald Platform to the Kechika Trough, and 3 sections across the parautochthonous Cassiar Terrane. The transect lies within an interpreted upper plate of an asymmetrically rifted margin. Regionally, renewed phases of extension of the margin throughout the lower Paleozoic are recorded in abrupt lateral and vertical facies changes and pulses of volcanism. The tectono-stratigraphic framework was influenced by eustatic sea-level changes. Revised stratigraphic terminology proposed herein includes the division of the Kechika Formation into 5 formal members: the Lloyd George, Quentin, Grey Peak, Haworth and Mount Sheffield members. The Skoki Formation comprises three distinct, formal members defined as the Sikanni Chief, Keily and Redfern members. The Road River Group is divided into three new formations: the Ospika Formation, the Pesika Formation (formerly the Silurian Limestone) and the Kwadacha Formation (formerly the Silurian Siltstone). The Ospika Formation is further subdivided into five formal members: the Cloudmaker, Finlay Limestone, Chesterfield, Finbow Shale and Ware members. 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The stratigraphy of the Kechika Formation, Road River Group and Skoki Formation in northern British Columbia has been described previously during reconnaissance mapping. This study provides detailed stratigraphic descriptions of Upper Cambrian to Lower Silurian units from 9 key sections which span an east-west transect from the Macdonald Platform to the Kechika Trough, and 3 sections across the parautochthonous Cassiar Terrane. The transect lies within an interpreted upper plate of an asymmetrically rifted margin. Regionally, renewed phases of extension of the margin throughout the lower Paleozoic are recorded in abrupt lateral and vertical facies changes and pulses of volcanism. The tectono-stratigraphic framework was influenced by eustatic sea-level changes. Revised stratigraphic terminology proposed herein includes the division of the Kechika Formation into 5 formal members: the Lloyd George, Quentin, Grey Peak, Haworth and Mount Sheffield members. The Skoki Formation comprises three distinct, formal members defined as the Sikanni Chief, Keily and Redfern members. The Road River Group is divided into three new formations: the Ospika Formation, the Pesika Formation (formerly the Silurian Limestone) and the Kwadacha Formation (formerly the Silurian Siltstone). The Ospika Formation is further subdivided into five formal members: the Cloudmaker, Finlay Limestone, Chesterfield, Finbow Shale and Ware members. RESUME Les strates du PalEozoique infrrieur du miogdoclinal de la Cordillbre canadienne du Nord documentent l'rvolution tectonique non passive de la marge drrivre du rift du nord de Laurentia.","owner":{"id":15974665,"first_name":"Christopher","middle_initials":"R .","last_name":"Barnes","page_name":"ChristopherBarnes","domain_name":"uvic","created_at":"2014-09-02T10:43:24.420-07:00","display_name":"Christopher R . 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JOURNAL OF PALEONTOLOGY, V. 47, NO. 4, P. 760-790, 5 PL., 2 TEXT-FIGS., JULY 1973 LOWER A...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Page 1. 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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="117091515"><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/117091515/SMART_Subsea_Cables_for_Observing_the_Earth_and_Ocean_Mitigating_Environmental_Hazards_and_Supporting_the_Blue_Economy"><img alt="Research paper thumbnail of SMART Subsea Cables for Observing the Earth and Ocean, Mitigating Environmental Hazards, and Supporting the Blue Economy" class="work-thumbnail" src="https://attachments.academia-assets.com/113042606/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/117091515/SMART_Subsea_Cables_for_Observing_the_Earth_and_Ocean_Mitigating_Environmental_Hazards_and_Supporting_the_Blue_Economy">SMART Subsea Cables for Observing the Earth and Ocean, Mitigating Environmental Hazards, and Supporting the Blue Economy</a></div><div class="wp-workCard_item"><span>Frontiers in Earth Science</span><span>, 2022</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Joint Task Force, Science Monitoring And Reliable Telecommunications (JTF SMART) Subsea Cable...</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 Joint Task Force, Science Monitoring And Reliable Telecommunications (JTF SMART) Subsea Cables, is working to integrate environmental sensors for ocean bottom temperature, pressure, and seismic acceleration into submarine telecommunications cables. The purpose of SMART Cables is to support climate and ocean observation, sea level monitoring, observations of Earth structure, and tsunami and earthquake early warning and disaster risk reduction, including hazard quantification. Recent advances include regional SMART pilot systems that are the first steps to trans-ocean and global implementation. Examples of pilots include: InSEA wet demonstration project off Sicily at the European Multidisciplinary Seafloor and water column Observatory Western Ionian Facility; New Caledonia and Vanuatu; French Polynesia Natitua South system connecting Tahiti to Tubaui to the south; Indonesia starting with short pilot systems working toward systems for the Sumatra-Java megathrust zone; and the CAM-2...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="41a4d334b94fa19eaca45edbfa0a6611" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113042606,"asset_id":117091515,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113042606/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="117091515"><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="117091515"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117091515; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117091515]").text(description); $(".js-view-count[data-work-id=117091515]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117091515; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117091515']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117091515, 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: "41a4d334b94fa19eaca45edbfa0a6611" } } $('.js-work-strip[data-work-id=117091515]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117091515,"title":"SMART Subsea Cables for Observing the Earth and Ocean, Mitigating Environmental Hazards, and Supporting the Blue Economy","translated_title":"","metadata":{"abstract":"The Joint Task Force, Science Monitoring And Reliable Telecommunications (JTF SMART) Subsea Cables, is working to integrate environmental sensors for ocean bottom temperature, pressure, and seismic acceleration into submarine telecommunications cables. 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Some 220 melted micrometeorites were recovered from the magnetic fraction of six samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from five samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. The micrometeorite-bearing formations span the late Tremadocian to the late Darriliwian (~480-460 Ma), which is consistent with a period of elevated flux of extraterrestrial material, as recorded several thousand kilometres away from coeval horizons in Scotland, Sweden and central China.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d1987e58a617b1d5d96a173a2782cb4d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":108995802,"asset_id":111462385,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/108995802/download_file?st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&st=MTczNDE2MDIyNyw4LjIyMi4yMDguMTQ2&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="111462385"><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="111462385"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111462385; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111462385]").text(description); $(".js-view-count[data-work-id=111462385]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111462385; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111462385']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111462385, 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: "d1987e58a617b1d5d96a173a2782cb4d" } } $('.js-work-strip[data-work-id=111462385]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111462385,"title":"Cosmic spherules from the Ordovician of Argentina","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Ordovician Micrometeorites: Discovery and Analysis in Argentina","grobid_abstract":"The discovery of magnetic spherules in acid-insoluble residues from conodont samples encouraged a systematic search for Ordovician micrometeorites from northwestern Argentina. Some 220 melted micrometeorites were recovered from the magnetic fraction of six samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from five samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. 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