CINXE.COM

<!DOCTYPE html> <html lang="en" xmlns:fb="http://www.facebook.com/2008/fbml" class="wf-loading"> <head prefix="og: https://ogp.me/ns# fb: https://ogp.me/ns/fb# academia: https://ogp.me/ns/fb/academia#"> <meta charset="utf-8"> <meta name=viewport content="width=device-width, initial-scale=1"> <meta rel="search" type="application/opensearchdescription+xml" href="/open_search.xml" title="Academia.edu"> <title>Jimmy Van Itterbeeck - Academia.edu</title>  <link href="//a.academia-assets.com/images/favicons/favicon-production.ico" rel="shortcut icon" type="image/vnd.microsoft.icon"> <link rel="apple-touch-icon" sizes="57x57" href="//a.academia-assets.com/images/favicons/apple-touch-icon-57x57.png"> <link rel="apple-touch-icon" sizes="60x60" href="//a.academia-assets.com/images/favicons/apple-touch-icon-60x60.png"> <link rel="apple-touch-icon" sizes="72x72" href="//a.academia-assets.com/images/favicons/apple-touch-icon-72x72.png"> <link rel="apple-touch-icon" sizes="76x76" href="//a.academia-assets.com/images/favicons/apple-touch-icon-76x76.png"> <link rel="apple-touch-icon" sizes="114x114" href="//a.academia-assets.com/images/favicons/apple-touch-icon-114x114.png"> <link rel="apple-touch-icon" sizes="120x120" href="//a.academia-assets.com/images/favicons/apple-touch-icon-120x120.png"> <link rel="apple-touch-icon" sizes="144x144" href="//a.academia-assets.com/images/favicons/apple-touch-icon-144x144.png"> <link rel="apple-touch-icon" sizes="152x152" href="//a.academia-assets.com/images/favicons/apple-touch-icon-152x152.png"> <link rel="apple-touch-icon" sizes="180x180" href="//a.academia-assets.com/images/favicons/apple-touch-icon-180x180.png"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-32x32.png" sizes="32x32"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-194x194.png" sizes="194x194"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-96x96.png" sizes="96x96"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/android-chrome-192x192.png" sizes="192x192"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-16x16.png" sizes="16x16"> <link rel="manifest" href="//a.academia-assets.com/images/favicons/manifest.json"> <meta name="msapplication-TileColor" content="#2b5797"> <meta name="msapplication-TileImage" content="//a.academia-assets.com/images/favicons/mstile-144x144.png"> <meta name="theme-color" content="#ffffff"> <script> window.performance && window.performance.measure && window.performance.measure("Time To First Byte", "requestStart", "responseStart"); </script> <script> (function() { if (!window.URLSearchParams || !window.history || !window.history.replaceState) { return; } var searchParams = new URLSearchParams(window.location.search); var paramsToDelete = [ 'fs', 'sm', 'swp', 'iid', 'nbs', 'rcc', // related content category 'rcpos', // related content carousel position 'rcpg', // related carousel page 'rchid', // related content hit id 'f_ri', // research interest id, for SEO tracking 'f_fri', // featured research interest, for SEO tracking (param key without value) 'f_rid', // from research interest directory for SEO tracking 'f_loswp', // from research interest pills on LOSWP sidebar for SEO tracking 'rhid', // referrring hit id ]; if (paramsToDelete.every((key) => searchParams.get(key) === null)) { return; } paramsToDelete.forEach((key) => { searchParams.delete(key); }); var cleanUrl = new URL(window.location.href); cleanUrl.search = searchParams.toString(); history.replaceState({}, document.title, cleanUrl); })(); </script> <script async src="https://www.googletagmanager.com/gtag/js?id=G-5VKX33P2DS"></script> <script> window.dataLayer = window.dataLayer || []; function gtag(){dataLayer.push(arguments);} gtag('js', new Date()); gtag('config', 'G-5VKX33P2DS', { cookie_domain: 'academia.edu', send_page_view: false, }); gtag('event', 'page_view', { 'controller': "profiles/works", 'action': "summary", 'controller_action': 'profiles/works#summary', 'logged_in': 'false', 'edge': 'unknown', // Send nil if there is no A/B test bucket, in case some records get logged // with missing data - that way we can distinguish between the two cases. // ab_test_bucket should be of the form <ab_test_name>:<bucket> 'ab_test_bucket': null, }) </script> <script type="text/javascript"> window.sendUserTiming = function(timingName) { if (!(window.performance && window.performance.measure)) return; var entries = window.performance.getEntriesByName(timingName, "measure"); if (entries.length !== 1) return; var timingValue = Math.round(entries[0].duration); gtag('event', 'timing_complete', { name: timingName, value: timingValue, event_category: 'User-centric', }); }; window.sendUserTiming("Time To First Byte"); </script> <meta name="csrf-param" content="authenticity_token" /> <meta name="csrf-token" content="7XfHZ30gXo893EZnJn9DTRooLExJ7GTCSAubHkH9zmvZ47XvPt7Za4OAULVIWMq1oZ70-AIwmgn30EOvKnfN9w" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/wow-3d36c19b4875b226bfed0fcba1dcea3f2fe61148383d97c0465c016b8c969290.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/social/home-79e78ce59bef0a338eb6540ec3d93b4a7952115b56c57f1760943128f4544d42.css" /><script type="application/ld+json">{"@context":"https://schema.org","@type":"ProfilePage","mainEntity":{"@context":"https://schema.org","@type":"Person","name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck","image":"https://0.academia-photos.com/4746200/2011708/2372873/s200_jimmy.van_itterbeeck.jpg","sameAs":[]},"dateCreated":"2013-07-04T12:06:58-07:00","dateModified":"2023-01-31T01:47:06-08:00","name":"Jimmy Van Itterbeeck","description":"","image":"https://0.academia-photos.com/4746200/2011708/2372873/s200_jimmy.van_itterbeeck.jpg","thumbnailUrl":"https://0.academia-photos.com/4746200/2011708/2372873/s65_jimmy.van_itterbeeck.jpg","primaryImageOfPage":{"@type":"ImageObject","url":"https://0.academia-photos.com/4746200/2011708/2372873/s200_jimmy.van_itterbeeck.jpg","width":200},"sameAs":[],"relatedLink":"https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea"}</script><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/heading-95367dc03b794f6737f30123738a886cf53b7a65cdef98a922a98591d60063e3.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/button-8c9ae4b5c8a2531640c354d92a1f3579c8ff103277ef74913e34c8a76d4e6c00.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/body-170d1319f0e354621e81ca17054bb147da2856ec0702fe440a99af314a6338c5.css" /><link crossorigin="" href="https://fonts.gstatic.com/" rel="preconnect" /><link href="https://fonts.googleapis.com/css2?family=DM+Sans:ital,opsz,wght@0,9..40,100..1000;1,9..40,100..1000&family=Gupter:wght@400;500;700&family=IBM+Plex+Mono:wght@300;400&family=Material+Symbols+Outlined:opsz,wght,FILL,GRAD@20,400,0,0&display=swap" rel="stylesheet" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/common-2b6f90dbd75f5941bc38f4ad716615f3ac449e7398313bb3bc225fba451cd9fa.css" /> <meta name="author" content="jimmy van itterbeeck" /> <meta name="description" content="Jimmy Van Itterbeeck: 24 Followers, 7 Following, 24 Research papers. Research interests: Tectonics, Geochronology, and Tectonics & Sedimentation." /> <meta name="google-site-verification" content="bKJMBZA7E43xhDOopFZkssMMkBRjvYERV-NaN4R6mrs" /> <script> var $controller_name = 'works'; var $action_name = "summary"; var $rails_env = 'production'; var $app_rev = '107520bac59918e2ceae62eaadd15bff3d1e7904'; var $domain = 'academia.edu'; var $app_host = "academia.edu"; var $asset_host = "academia-assets.com"; var $start_time = new Date().getTime(); var $recaptcha_key = "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB"; var $recaptcha_invisible_key = "6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj"; var $disableClientRecordHit = false; </script> <script> window.Aedu = { hit_data: null }; window.Aedu.SiteStats = {"premium_universities_count":13997,"monthly_visitors":"111 million","monthly_visitor_count":111388986,"monthly_visitor_count_in_millions":111,"user_count":284024380,"paper_count":55203019,"paper_count_in_millions":55,"page_count":432000000,"page_count_in_millions":432,"pdf_count":16500000,"pdf_count_in_millions":16}; window.Aedu.serverRenderTime = new Date(1740881946000); window.Aedu.timeDifference = new Date().getTime() - 1740881946000; window.Aedu.isUsingCssV1 = false; window.Aedu.enableLocalization = true; window.Aedu.activateFullstory = false; window.Aedu.serviceAvailability = { status: {"attention_db":"on","bibliography_db":"on","contacts_db":"on","email_db":"on","indexability_db":"on","mentions_db":"on","news_db":"on","notifications_db":"on","offsite_mentions_db":"on","redshift":"on","redshift_exports_db":"on","related_works_db":"on","ring_db":"on","user_tests_db":"on"}, serviceEnabled: function(service) { return this.status[service] === "on"; }, readEnabled: function(service) { return this.serviceEnabled(service) || this.status[service] === "read_only"; }, }; window.Aedu.viewApmTrace = function() { // Check if x-apm-trace-id meta tag is set, and open the trace in APM // in a new window if it is. var apmTraceId = document.head.querySelector('meta[name="x-apm-trace-id"]'); if (apmTraceId) { var traceId = apmTraceId.content; // Use trace ID to construct URL, an example URL looks like: // https://app.datadoghq.com/apm/traces?query=trace_id%31298410148923562634 var apmUrl = 'https://app.datadoghq.com/apm/traces?query=trace_id%3A' + traceId; window.open(apmUrl, '_blank'); } }; </script>  <link href="https://fonts.googleapis.com/css?family=Roboto:100,100i,300,300i,400,400i,500,500i,700,700i,900,900i" rel="stylesheet"> <link rel="preload" href="//maxcdn.bootstrapcdn.com/font-awesome/4.3.0/css/font-awesome.min.css" as="style" onload="this.rel='stylesheet'"> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/libraries-a9675dcb01ec4ef6aa807ba772c7a5a00c1820d3ff661c1038a20f80d06bb4e4.css" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/academia-1eb081e01ca8bc0c1b1d866df79d9eb4dd2c484e4beecf76e79a7806c72fee08.css" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system_legacy-056a9113b9a0f5343d013b29ee1929d5a18be35fdcdceb616600b4db8bd20054.css" /> <script src="//a.academia-assets.com/assets/webpack_bundles/runtime-bundle-005434038af4252ca37c527588411a3d6a0eabb5f727fac83f8bbe7fd88d93bb.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/webpack_libraries_and_infrequently_changed.wjs-bundle-a7f06b7b91deb14294c0fd04acc3d1303a356edfef84048171548420b79efa13.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/core_webpack.wjs-bundle-caa56a0f54c25da9fc0ce496a02fe99f5ff17476fd61737267d5dfef010828de.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/sentry.wjs-bundle-5fe03fddca915c8ba0f7edbe64c194308e8ce5abaed7bffe1255ff37549c4808.js"></script> <script> jade = window.jade || {}; jade.helpers = window.$h; jade._ = window._; </script>  <script id="tag-manager-head-root">(function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start': new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0], j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src= 'https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f); })(window,document,'script','dataLayer_old','GTM-5G9JF7Z');</script>  <script> window.gptadslots = []; window.googletag = window.googletag || {}; window.googletag.cmd = window.googletag.cmd || []; </script> <script type="text/javascript"> // TODO(jacob): This should be defined, may be rare load order problem. // Checking if null is just a quick fix, will default to en if unset. // Better fix is to run this immedietely after I18n is set. if (window.I18n != null) { I18n.defaultLocale = "en"; I18n.locale = "en"; I18n.fallbacks = true; } </script> <link rel="canonical" href="https://independent.academia.edu/JimmyVanItterbeeck" /> </head>   <body class='c-profiles/works a-summary logged_out'>  <div id="fb-root"></div><script>window.fbAsyncInit = function() { FB.init({ appId: "2369844204", version: "v8.0", status: true, cookie: true, xfbml: true }); // Additional initialization code. if (window.InitFacebook) { // facebook.ts already loaded, set it up. window.InitFacebook(); } else { // Set a flag for facebook.ts to find when it loads. window.academiaAuthReadyFacebook = true; } };</script><script>window.fbAsyncLoad = function() { // Protection against double calling of this function if (window.FB) { return; } (function(d, s, id){ var js, fjs = d.getElementsByTagName(s)[0]; if (d.getElementById(id)) {return;} js = d.createElement(s); js.id = id; js.src = "//connect.facebook.net/en_US/sdk.js"; fjs.parentNode.insertBefore(js, fjs); }(document, 'script', 'facebook-jssdk')); } if (!window.defer_facebook) { // Autoload if not deferred window.fbAsyncLoad(); } else { // Defer loading by 5 seconds setTimeout(function() { window.fbAsyncLoad(); }, 5000); }</script> <div id="google-root"></div><script>window.loadGoogle = function() { if (window.InitGoogle) { // google.ts already loaded, set it up. window.InitGoogle("331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b"); } else { // Set a flag for google.ts to use when it loads. window.GoogleClientID = "331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b"; } };</script><script>window.googleAsyncLoad = function() { // Protection against double calling of this function (function(d) { var js; var id = 'google-jssdk'; var ref = d.getElementsByTagName('script')[0]; if (d.getElementById(id)) { return; } js = d.createElement('script'); js.id = id; js.async = true; js.onload = loadGoogle; js.src = "https://accounts.google.com/gsi/client" ref.parentNode.insertBefore(js, ref); }(document)); } if (!window.defer_google) { // Autoload if not deferred window.googleAsyncLoad(); } else { // Defer loading by 5 seconds setTimeout(function() { window.googleAsyncLoad(); }, 5000); }</script> <div id="tag-manager-body-root">  <noscript><iframe src="https://www.googletagmanager.com/ns.html?id=GTM-5G9JF7Z" height="0" width="0" style="display:none;visibility:hidden"></iframe></noscript>   <script> window.addEventListener('load', function() { if (document.querySelector('input[name="commit"]')) { document.querySelector('input[name="commit"]').addEventListener('click', function() { gtag('event', 'click', { event_category: 'button', event_label: 'Log In' }) }) } }); </script> </div> <script>var _comscore = _comscore || []; _comscore.push({ c1: "2", c2: "26766707" }); (function() { var s = document.createElement("script"), el = document.getElementsByTagName("script")[0]; s.async = true; s.src = (document.location.protocol == "https:" ? "https://sb" : "http://b") + ".scorecardresearch.com/beacon.js"; el.parentNode.insertBefore(s, el); })();</script><img src="https://sb.scorecardresearch.com/p?c1=2&c2=26766707&cv=2.0&cj=1" style="position: absolute; visibility: hidden" /> <div id='react-modal'></div> <div class='DesignSystem'> <a class='u-showOnFocus' href='#site'> Skip to main content </a> </div> <div id="upgrade_ie_banner" style="display: none;"><p>Academia.edu no longer supports Internet Explorer.</p><p>To browse Academia.edu and the wider internet faster and more securely, please take a few seconds to <a href="https://www.academia.edu/upgrade-browser">upgrade your browser</a>.</p></div><script>// Show this banner for all versions of IE if (!!window.MSInputMethodContext || /(MSIE)/.test(navigator.userAgent)) { document.getElementById('upgrade_ie_banner').style.display = 'block'; }</script> <div class="DesignSystem bootstrap ShrinkableNav"><div class="navbar navbar-default main-header"><div class="container-wrapper" id="main-header-container"><div class="container"><div class="navbar-header"><div class="nav-left-wrapper u-mt0x"><div class="nav-logo"><a data-main-header-link-target="logo_home" href="https://www.academia.edu/"><img class="visible-xs-inline-block" style="height: 24px;" alt="Academia.edu" src="//a.academia-assets.com/images/academia-logo-redesign-2015-A.svg" width="24" height="24" /><img width="145.2" height="18" class="hidden-xs" style="height: 24px;" alt="Academia.edu" src="//a.academia-assets.com/images/academia-logo-redesign-2015.svg" /></a></div><div class="nav-search"><div class="SiteSearch-wrapper select2-no-default-pills"><form class="js-SiteSearch-form DesignSystem" action="https://www.academia.edu/search" accept-charset="UTF-8" method="get"><i class="SiteSearch-icon fa fa-search u-fw700 u-positionAbsolute u-tcGrayDark"></i><input class="js-SiteSearch-form-input SiteSearch-form-input form-control" data-main-header-click-target="search_input" name="q" placeholder="Search" type="text" value="" /></form></div></div></div><div class="nav-right-wrapper pull-right"><ul class="NavLinks js-main-nav list-unstyled"><li class="NavLinks-link"><a class="js-header-login-url Button Button--inverseGray Button--sm u-mb4x" id="nav_log_in" rel="nofollow" href="https://www.academia.edu/login">Log In</a></li><li class="NavLinks-link u-p0x"><a class="Button Button--inverseGray Button--sm u-mb4x" rel="nofollow" href="https://www.academia.edu/signup">Sign Up</a></li></ul><button class="hidden-lg hidden-md hidden-sm u-ml4x navbar-toggle collapsed" data-target=".js-mobile-header-links" data-toggle="collapse" type="button"><span class="icon-bar"></span><span class="icon-bar"></span><span class="icon-bar"></span></button></div></div><div class="collapse navbar-collapse js-mobile-header-links"><ul class="nav navbar-nav"><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/login">Log In</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/signup">Sign Up</a></li><li class="u-borderColorGrayLight u-borderBottom1 js-mobile-nav-expand-trigger"><a href="#">more&nbsp<span class="caret"></span></a></li><li><ul class="js-mobile-nav-expand-section nav navbar-nav u-m0x collapse"><li class="u-borderColorGrayLight u-borderBottom1"><a rel="false" href="https://www.academia.edu/about">About</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/press">Press</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="false" href="https://www.academia.edu/documents">Papers</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/terms">Terms</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/privacy">Privacy</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/copyright">Copyright</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/hiring"><i class="fa fa-briefcase"></i> We're Hiring!</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://support.academia.edu/hc/en-us"><i class="fa fa-question-circle"></i> Help Center</a></li><li class="js-mobile-nav-collapse-trigger u-borderColorGrayLight u-borderBottom1 dropup" style="display:none"><a href="#">less&nbsp<span class="caret"></span></a></li></ul></li></ul></div></div></div><script>(function(){ var $moreLink = $(".js-mobile-nav-expand-trigger"); var $lessLink = $(".js-mobile-nav-collapse-trigger"); var $section = $('.js-mobile-nav-expand-section'); $moreLink.click(function(ev){ ev.preventDefault(); $moreLink.hide(); $lessLink.show(); $section.collapse('show'); }); $lessLink.click(function(ev){ ev.preventDefault(); $moreLink.show(); $lessLink.hide(); $section.collapse('hide'); }); })() if ($a.is_logged_in() || false) { new Aedu.NavigationController({ el: '.js-main-nav', showHighlightedNotification: false }); } else { $(".js-header-login-url").attr("href", $a.loginUrlWithRedirect()); } Aedu.autocompleteSearch = new AutocompleteSearch({el: '.js-SiteSearch-form'});</script></div></div> <div id='site' class='fixed'> <div id="content" class="clearfix"> <script>document.addEventListener('DOMContentLoaded', function(){ var $dismissible = $(".dismissible_banner"); $dismissible.click(function(ev) { $dismissible.hide(); }); });</script> <script src="//a.academia-assets.com/assets/webpack_bundles/profile.wjs-bundle-0ceb3be4b43a1e81bd83edaf59acf60dd046a0a3ef0d3b827386b5556dbaf5c2.js" defer="defer"></script><script>$viewedUser = Aedu.User.set_viewed( {"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck","photo":"https://0.academia-photos.com/4746200/2011708/2372873/s65_jimmy.van_itterbeeck.jpg","has_photo":true,"is_analytics_public":false,"interests":[{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":13087,"name":"Tectonics \u0026 Sedimentation","url":"https://www.academia.edu/Documents/in/Tectonics_and_Sedimentation"},{"id":19524,"name":"Mountain Building","url":"https://www.academia.edu/Documents/in/Mountain_Building"}]} ); if ($a.is_logged_in() && $viewedUser.is_current_user()) { $('body').addClass('profile-viewed-by-owner'); } $socialProfiles = []</script><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://independent.academia.edu/JimmyVanItterbeeck","location":"/JimmyVanItterbeeck","scheme":"https","host":"independent.academia.edu","port":null,"pathname":"/JimmyVanItterbeeck","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="ProfileCheckPaperUpdate" data-props="{}" data-trace="false" data-dom-id="ProfileCheckPaperUpdate-react-component-bb46fa61-368a-43bc-ad20-ce6115643f3d"></div> <div id="ProfileCheckPaperUpdate-react-component-bb46fa61-368a-43bc-ad20-ce6115643f3d"></div> <div class="DesignSystem"><div class="onsite-ping" id="onsite-ping"></div></div><div class="profile-user-info DesignSystem"><div class="social-profile-container"><div class="left-panel-container"><div class="user-info-component-wrapper"><div class="user-summary-cta-container"><div class="user-summary-container"><div class="social-profile-avatar-container"><img class="profile-avatar u-positionAbsolute" alt="Jimmy Van Itterbeeck" 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/4746200/2011708/2372873/s200_jimmy.van_itterbeeck.jpg" /></div><div class="title-container"><h1 class="ds2-5-heading-sans-serif-sm">Jimmy Van Itterbeeck</h1><div class="affiliations-container fake-truncate js-profile-affiliations"></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="Jimmy" data-follow-user-id="4746200" 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="4746200"><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">24</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">7</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">2</p></div></a><div class="js-mentions-count-container" style="display: none;"><a href="/JimmyVanItterbeeck/mentions"><div class="stat-container"><p class="label">Mentions</p><p class="data"></p></div></a></div><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="suggested-academics-container"><div class="suggested-academics--header"><p class="ds2-5-body-md-bold">Related Authors</p></div><ul class="suggested-user-card-list"><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://uu.academia.edu/KimCohen"><img class="profile-avatar u-positionAbsolute" alt="Kim M Cohen" 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/31840/10277/9694/s200_kim.cohen.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://uu.academia.edu/KimCohen">Kim M Cohen</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Utrecht University</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://bergbaumuseum.academia.edu/NimaNezafati"><img class="profile-avatar u-positionAbsolute" alt="Nima Nezafati" 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/58779/17089/2005499/s200_nima.nezafati_.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://bergbaumuseum.academia.edu/NimaNezafati">Nima Nezafati</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Deutsches Bergbau-Museum, Bochum</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://ens.academia.edu/NicolasColtice"><img class="profile-avatar u-positionAbsolute" alt="Nicolas Coltice" 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/76505/21165/1097058/s200_nicolas.coltice.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://ens.academia.edu/NicolasColtice">Nicolas Coltice</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">École Normale Supérieure</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://bgs.academia.edu/NickRoberts"><img class="profile-avatar u-positionAbsolute" alt="Nick Roberts" 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/77572/21510/276482/s200_nick.roberts.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://bgs.academia.edu/NickRoberts">Nick Roberts</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">British Geological Survey</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://iasbs.academia.edu/MahnazRezaeian"><img class="profile-avatar u-positionAbsolute" alt="Mahnaz Rezaeian" 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/97147/26862/24760/s200_mahnaz.rezaeian.jpeg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://iasbs.academia.edu/MahnazRezaeian">Mahnaz Rezaeian</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Institute for Advanced Studies in Basic Sciences</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://uppsala.academia.edu/HeminKoyi"><img class="profile-avatar u-positionAbsolute" alt="Hemin Koyi" 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/102248/28141/11213115/s200_hemin.koyi.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://uppsala.academia.edu/HeminKoyi">Hemin Koyi</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Uppsala University</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://bucknell.academia.edu/ChristopherDaniel"><img class="profile-avatar u-positionAbsolute" alt="Christopher Daniel" 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/155269/1083127/1350891/s200_christopher.daniel.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://bucknell.academia.edu/ChristopherDaniel">Christopher Daniel</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Bucknell University</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://columbia.academia.edu/httpswwwldeocolumbiaedupolsennbcppeocv1html"><img class="profile-avatar u-positionAbsolute" alt="Paul E. Olsen" 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/155497/4465541/5174914/s200_paul_e..olsen.jpg_oh_fb87dfb614eed6275d02ea5a2a4905a5_oe_54955aff___gda___1422878224_5543797cac79301afd5ddd6d627fb26d" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://columbia.academia.edu/httpswwwldeocolumbiaedupolsennbcppeocv1html">Paul E. Olsen</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Columbia University</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://usal.academia.edu/GabrielGutierrezAlonso"><img class="profile-avatar u-positionAbsolute" alt="Gabriel Gutierrez-Alonso" 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/175637/822125/1022101/s200_gabriel.gutierrez-alonso.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://usal.academia.edu/GabrielGutierrezAlonso">Gabriel Gutierrez-Alonso</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">University of Salamanca</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a href="https://lisboa.academia.edu/PauloEmanuelFonseca"><img class="profile-avatar u-positionAbsolute" alt="Paulo Emanuel T F Fonseca" 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/342117/877289/19902064/s200_paulo_emanuel.fonseca.png" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://lisboa.academia.edu/PauloEmanuelFonseca">Paulo Emanuel T F Fonseca</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Universidade de Lisboa</p></div></div></ul></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="4746200" href="https://www.academia.edu/Documents/in/Tectonics"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://independent.academia.edu/JimmyVanItterbeeck","location":"/JimmyVanItterbeeck","scheme":"https","host":"independent.academia.edu","port":null,"pathname":"/JimmyVanItterbeeck","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":["Tectonics"]}" data-trace="false" data-dom-id="Pill-react-component-5b90dd1e-8ea1-4bd6-b922-02015e3aa8f5"></div> <div id="Pill-react-component-5b90dd1e-8ea1-4bd6-b922-02015e3aa8f5"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="4746200" href="https://www.academia.edu/Documents/in/Geochronology"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Geochronology"]}" data-trace="false" data-dom-id="Pill-react-component-3be274b5-72e5-48a4-b210-c3d36ee70d1d"></div> <div id="Pill-react-component-3be274b5-72e5-48a4-b210-c3d36ee70d1d"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="4746200" href="https://www.academia.edu/Documents/in/Tectonics_and_Sedimentation"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Tectonics \u0026 Sedimentation"]}" data-trace="false" data-dom-id="Pill-react-component-8cdc6ebe-dc45-4831-b4f4-458e0ce07986"></div> <div id="Pill-react-component-8cdc6ebe-dc45-4831-b4f4-458e0ce07986"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="4746200" href="https://www.academia.edu/Documents/in/Mountain_Building"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Mountain Building"]}" data-trace="false" data-dom-id="Pill-react-component-257b79ee-aad2-46b1-bfce-9f0260c6603d"></div> <div id="Pill-react-component-257b79ee-aad2-46b1-bfce-9f0260c6603d"></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 Jimmy Van Itterbeeck</h3></div><div class="js-work-strip profile--work_container" data-work-id="95406183"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea"><img alt="Research paper thumbnail of A new model for the evolution of oceanic transform faults based on 3D PSDM Seismic observations from São Tomé and Príncipe, eastern Gulf of Guinea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea">A new model for the evolution of oceanic transform faults based on 3D PSDM Seismic observations from São Tomé and Príncipe, eastern Gulf of Guinea</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&amp;amp;lt;p&amp;amp;gt;Oceanic Transform faults are one of the three major tectonic plate bound...</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">&amp;amp;lt;p&amp;amp;gt;Oceanic Transform faults are one of the three major tectonic plate boundaries and yet their evolution and deformational mechanism is not well understood. They are broadly considered to be dominated by strike-slip displacement along simple planar vertical faults and to be conservative in nature with no magmatic addition. Observations from Pre-Stack depth-migrated (PSDM) 3D seismic of Cretaceous-aged transforms in the eastern Gulf of Guinea allow complex internal architectures to be described, including crustal scale detachments and rotated packages of volcanics.&amp;amp;lt;/p&amp;amp;gt;&amp;amp;lt;p&amp;amp;gt;These insights demonstrate additional complexity previously only predicted in numerical simulations of spreading ridge-transform interaction, namely intra-transform extension at a high angle to the spreading orientation, and the addition of significant extrusive volcanic material. In the study area of S&amp;amp;amp;#227;o Tom&amp;amp;amp;#233; and Pr&amp;amp;amp;#237;ncipe, several Oceanic Fracture Zones (OFZ) are identified, consisting of a broad deformational zones that can be described from top to base crust. OFZ scarps are observed to connect at depth with zones of low angle reflectivity which dip into the OFZ and perpendicular to the spreading orientation. At depth they detach onto the Moho below, necking the adjacent crust along the length of the OFZ in the manner of extensional shear zones. Thickly stacked and tilted reflectors, interpreted as extrusive lava flows, are common above the shear zones and infill up to 75% of the crustal thickness. The entire OFZ stratigraphy is overlain and sealed by late-stage lavas that are continuous from the abyssal hills of the trailing spreading ridge. This constrains a process of oblique extension at a high angle to the spreading orientation along a low angle shear zone which also acts as a conduit for decompression related melt.&amp;amp;lt;/p&amp;amp;gt;&amp;amp;lt;p&amp;amp;gt;We demonstrate that transforms in S&amp;amp;amp;#227;o Tom&amp;amp;amp;#233; and Pr&amp;amp;amp;#237;ncipe were both non-conservative and not a simple strike slip fault zone, contradicting the current understanding of modern systems. This style of deformation has similarities with anomalously deep and smooth nodal basins which form at slow spreading inside-corner crust. Our model adds strong observational constraints to complement recent numerical models that predict oblique extension within transform zones.&amp;amp;lt;/p&amp;amp;gt;</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="95406183"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406183"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406183; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406183]").text(description); $(".js-view-count[data-work-id=95406183]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406183; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406183']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406183]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406183,"title":"A new model for the evolution of oceanic transform faults based on 3D PSDM Seismic observations from São Tomé and Príncipe, eastern Gulf of Guinea","internal_url":"https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406182"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406182/Detailed_lithostratigraphic_description_of_the_Wealden_facies_found_in_the_BER3_borehole_Bernissart_Belgium_Preliminary_comparison_with_the_subsequent_deposits_of_the_Hautrage_and_Thieu_facies_Mons_Basin_Belgium_"><img alt="Research paper thumbnail of Detailed lithostratigraphic description of the Wealden facies found in the BER3 borehole (Bernissart, Belgium). Preliminary comparison with the subsequent deposits of the Hautrage and Thieu facies (Mons Basin, Belgium)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406182/Detailed_lithostratigraphic_description_of_the_Wealden_facies_found_in_the_BER3_borehole_Bernissart_Belgium_Preliminary_comparison_with_the_subsequent_deposits_of_the_Hautrage_and_Thieu_facies_Mons_Basin_Belgium_">Detailed lithostratigraphic description of the Wealden facies found in the BER3 borehole (Bernissart, Belgium). Preliminary comparison with the subsequent deposits of the Hautrage and Thieu facies (Mons Basin, Belgium)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406182"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406182"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406182; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406182]").text(description); $(".js-view-count[data-work-id=95406182]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406182; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406182']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406182]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406182,"title":"Detailed lithostratigraphic description of the Wealden facies found in the BER3 borehole (Bernissart, Belgium). Preliminary comparison with the subsequent deposits of the Hautrage and Thieu facies (Mons Basin, Belgium)","internal_url":"https://www.academia.edu/95406182/Detailed_lithostratigraphic_description_of_the_Wealden_facies_found_in_the_BER3_borehole_Bernissart_Belgium_Preliminary_comparison_with_the_subsequent_deposits_of_the_Hautrage_and_Thieu_facies_Mons_Basin_Belgium_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406181"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406181/Stable_isotope_d13C_d18O_analyses_on_marine_ostracod_shells_from_the_Danian_Selandian_boundary_Paleocene_of_Tunisia"><img alt="Research paper thumbnail of Stable isotope (d13C, d18O) analyses on marine ostracod shells from the Danian/Selandian boundary (Paleocene) of Tunisia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406181/Stable_isotope_d13C_d18O_analyses_on_marine_ostracod_shells_from_the_Danian_Selandian_boundary_Paleocene_of_Tunisia">Stable isotope (d13C, d18O) analyses on marine ostracod shells from the Danian/Selandian boundary (Paleocene) of Tunisia</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406181"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406181"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406181; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406181]").text(description); $(".js-view-count[data-work-id=95406181]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406181; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406181']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406181]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406181,"title":"Stable isotope (d13C, d18O) analyses on marine ostracod shells from the Danian/Selandian boundary (Paleocene) of Tunisia","internal_url":"https://www.academia.edu/95406181/Stable_isotope_d13C_d18O_analyses_on_marine_ostracod_shells_from_the_Danian_Selandian_boundary_Paleocene_of_Tunisia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406180"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406180/Sea_level_and_paleoenvironment_of_the_Danian_Selandian_transition_in_Tunisia"><img alt="Research paper thumbnail of Sea level and paleoenvironment of the Danian/Selandian transition in Tunisia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406180/Sea_level_and_paleoenvironment_of_the_Danian_Selandian_transition_in_Tunisia">Sea level and paleoenvironment of the Danian/Selandian transition in Tunisia</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406180"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406180"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406180; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406180]").text(description); $(".js-view-count[data-work-id=95406180]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406180; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406180']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406180]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406180,"title":"Sea level and paleoenvironment of the Danian/Selandian transition in Tunisia","internal_url":"https://www.academia.edu/95406180/Sea_level_and_paleoenvironment_of_the_Danian_Selandian_transition_in_Tunisia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406179"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406179/Latest_Cretaceous_hadrosaurid_dinosaurs_from_Heilongjiang_Province_P_R_China_and_the_Amur_Region_Far_Eastern_Asia_"><img alt="Research paper thumbnail of Latest Cretaceous hadrosaurid dinosaurs from Heilongjiang Province (P. R. China) and the Amur Region (Far Eastern Asia)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406179/Latest_Cretaceous_hadrosaurid_dinosaurs_from_Heilongjiang_Province_P_R_China_and_the_Amur_Region_Far_Eastern_Asia_">Latest Cretaceous hadrosaurid dinosaurs from Heilongjiang Province (P. R. China) and the Amur Region (Far Eastern Asia)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406179"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406179"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406179; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406179]").text(description); $(".js-view-count[data-work-id=95406179]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406179; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406179']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406179]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406179,"title":"Latest Cretaceous hadrosaurid dinosaurs from Heilongjiang Province (P. R. China) and the Amur Region (Far Eastern Asia)","internal_url":"https://www.academia.edu/95406179/Latest_Cretaceous_hadrosaurid_dinosaurs_from_Heilongjiang_Province_P_R_China_and_the_Amur_Region_Far_Eastern_Asia_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406178"><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/95406178/Nonmarine_ostracods_from_the_Paleocene_Subeng_mammal_site_inner_Mongolia_P_R_China_taxonomy_and_biostratigraphy"><img alt="Research paper thumbnail of Nonmarine ostracods from the Paleocene Subeng mammal site, inner Mongolia, P.R. China, taxonomy and biostratigraphy" class="work-thumbnail" src="https://attachments.academia-assets.com/97598175/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/95406178/Nonmarine_ostracods_from_the_Paleocene_Subeng_mammal_site_inner_Mongolia_P_R_China_taxonomy_and_biostratigraphy">Nonmarine ostracods from the Paleocene Subeng mammal site, inner Mongolia, P.R. China, taxonomy and biostratigraphy</a></div><div class="wp-workCard_item"><span>Bulletin Institut Royal Des Sciences Naturelles De Belgique Sciences De La Terre</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Nine species, belonging to six genera, of nonmarine ostracods of the mammal-bearing horizons of t...</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">Nine species, belonging to six genera, of nonmarine ostracods of the mammal-bearing horizons of the Subeng locality are described and figured. One species is new: Timiriasevia subengensis sp. nov. Seven species are in common with the Paleocene White Beds (Naran Member) of the Naran Bulak Formation, Nemegt Basin, Mongolia. The two other species are known from the Paleocene of China. Based on the ostracod fauna, the mammalbearing horizons of the Subeng site (Bayan Ulan Beds, Nomogen Formation) are late Paleocene in age and can be correlated with the Naran Member of the Naran Bulak Formation.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="142f03056aed20167cb333513ea22875" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":97598175,"asset_id":95406178,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/97598175/download_file?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="95406178"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406178"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406178; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406178]").text(description); $(".js-view-count[data-work-id=95406178]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406178; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406178']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "142f03056aed20167cb333513ea22875" } } $('.js-work-strip[data-work-id=95406178]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406178,"title":"Nonmarine ostracods from the Paleocene Subeng mammal site, inner Mongolia, P.R. China, taxonomy and biostratigraphy","internal_url":"https://www.academia.edu/95406178/Nonmarine_ostracods_from_the_Paleocene_Subeng_mammal_site_inner_Mongolia_P_R_China_taxonomy_and_biostratigraphy","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":97598175,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97598175/thumbnails/1.jpg","file_name":"irscnb_p4087_022b9dx_74-2_bulletin-11.pdf","download_url":"https://www.academia.edu/attachments/97598175/download_file","bulk_download_file_name":"Nonmarine_ostracods_from_the_Paleocene_S.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97598175/irscnb_p4087_022b9dx_74-2_bulletin-11-libre.pdf?1674302121=\u0026response-content-disposition=attachment%3B+filename%3DNonmarine_ostracods_from_the_Paleocene_S.pdf\u0026Expires=1740873910\u0026Signature=MZdNBxhZnrpLuLAi0VcOPrKN2ifT~HVV9C41hFesHb6hQ8MOJ6MO04FobnooOKg7wNx-k7s2qfgpWHkJu8~PqnOJeGqElOpfmpLC7SPklv5ia6cqe-v5dn5Sp3umdlQE3hmexyWvMqPhRLs77X59lobJQ2bmxdWN~vf6FcE0rrcIpsKUlwN8GUWrZIMY72vXxD0qSOCq3YTG5key2p1tT7Oo3XTniX-39A0Or21PJcCdNvmZecYFoPIxqSePW3WO9TlntbAwE3XxYmjCMtQpuouglGARoioIOW26uT90FmeS1wEYNTIuXMKswyCTLwTmapUxGGyU6K-grKl36vZ3Jg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="95406177"><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/95406177/Cenozoic_deformation_and_exhumation_of_the_Kampot_Fold_Belt_and_implications_for_south_Indochina_tectonics"><img alt="Research paper thumbnail of Cenozoic deformation and exhumation of the Kampot Fold Belt and implications for south Indochina tectonics" class="work-thumbnail" src="https://attachments.academia-assets.com/97598162/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/95406177/Cenozoic_deformation_and_exhumation_of_the_Kampot_Fold_Belt_and_implications_for_south_Indochina_tectonics">Cenozoic deformation and exhumation of the Kampot Fold Belt and implications for south Indochina tectonics</a></div><div class="wp-workCard_item"><span>Journal of Geophysical Research: Solid Earth</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Latest Mesozoic to earliest Cenozoic deformation affected SE Asia's Sundaland-core. The deformati...</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">Latest Mesozoic to earliest Cenozoic deformation affected SE Asia's Sundaland-core. The deformation event bridges the Mesozoic SE Asian fusion with the Cenozoic era of rifting, translation, basin formation and the creation of modern SE Asian oceans. Southern Cambodia and Vietnam are central to this shift, but geological investigations of the region are in their infancy. Based on apatite and zircon fission track analyses (AFTA and ZFTA), stratigraphic and structural observations, seismic data, thermal maturity and igneous rock dating the geological evolution of southern Cambodia and Vietnam is investigated. Diverse depositional styles, igneous activity, structural deformation and sub-surface unconformities testify to a highly variable Phanerozoic tectonic setting. Major latest Cretaceous to Paleocene thrusting and uplift affected the Kampot Fold Belt and surrounding regions and the associated up to ~11 km exhumation probably exceeds earlier denudation events since at least Permian time. The present relief of the Bokor Mountains rising high above the Kampot Fold Belt represents an artifact after differential erosion and only 2.5-4.5 km of erosion affected this area. The latest Cretaceous to Paleocene orogenesis affected much of greater Indochina probably owing to plate collision along eastern Sundaland or a combination of collisions along both east and west Sundaland. AFTA and ZFTA data document protracted cooling of Cretaceous granites and locally elevated thermal gradients persisting a few tens of million years after their emplacement. The thermal gradient had stabilized by early Miocene time, and Miocene cooling probably reflects a renewed denudation pulse driven by either regional tectonism or climate-enhanced erosion.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b4223d8a4bdaff8364a09687572fd1a6" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":97598162,"asset_id":95406177,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/97598162/download_file?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="95406177"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406177"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406177; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406177]").text(description); $(".js-view-count[data-work-id=95406177]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406177; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406177']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "b4223d8a4bdaff8364a09687572fd1a6" } } $('.js-work-strip[data-work-id=95406177]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406177,"title":"Cenozoic deformation and exhumation of the Kampot Fold Belt and implications for south Indochina tectonics","internal_url":"https://www.academia.edu/95406177/Cenozoic_deformation_and_exhumation_of_the_Kampot_Fold_Belt_and_implications_for_south_Indochina_tectonics","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":97598162,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97598162/thumbnails/1.jpg","file_name":"2016jb01284720230121-1-1ehdx2l.pdf","download_url":"https://www.academia.edu/attachments/97598162/download_file","bulk_download_file_name":"Cenozoic_deformation_and_exhumation_of_t.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97598162/2016jb01284720230121-1-1ehdx2l-libre.pdf?1674302024=\u0026response-content-disposition=attachment%3B+filename%3DCenozoic_deformation_and_exhumation_of_t.pdf\u0026Expires=1740840026\u0026Signature=WWIa~rEdTrKdikPz2oPYNCg5sktLX2w9tlbvkz3WZb9gvqGSUexSHQVAglio8kQxpm7Cqh63q1pZUXUNBQY-RyyeZGe5LRoIY2iSl1lTMo17t-2ejXcOHi~Xq9SDqkjUbmC89OogfogmxViinmBCn5k9kK5sTzLhCOaMKKa02JjYpOe6Yt7tg1noNZJdBzRFMMuXFLBqb5Aha18n70lfgiJF5U35I~PY-70mOJSBqdc2uKzChk~GVHxhkzwhxR1YwuF6PtwLPciBozJKy9fy8KhhosgUt~IJIh~fDCnlqNJrVlH8OCTqW4GuMkwDDAEHCsFj1lMTfNsdrNHMcyuBjA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="95406176"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406176/Climatic_changes_and_sea_level_fluctuations_in_the_Danian_Selandian_boundary_interval_of_Tunesia_an_ostracod_perspective"><img alt="Research paper thumbnail of Climatic changes and sea-level fluctuations in the Danian/Selandian boundary interval of Tunesia: an ostracod perspective" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406176/Climatic_changes_and_sea_level_fluctuations_in_the_Danian_Selandian_boundary_interval_of_Tunesia_an_ostracod_perspective">Climatic changes and sea-level fluctuations in the Danian/Selandian boundary interval of Tunesia: an ostracod perspective</a></div><div class="wp-workCard_item"><span>… and Abstracts Berlin …</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Most research efforts on the Paleocene epoch have been invested in both its lower and upper bound...</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">Most research efforts on the Paleocene epoch have been invested in both its lower and upper boundaries: the Cretaceous/Paleogene and Paleocene/Eocene boundaries respectively. Compared to its boundaries, the remainder of the Paleocene epoch has ...</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="95406176"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406176"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406176; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406176]").text(description); $(".js-view-count[data-work-id=95406176]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406176; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406176']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406176]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406176,"title":"Climatic changes and sea-level fluctuations in the Danian/Selandian boundary interval of Tunesia: an ostracod perspective","internal_url":"https://www.academia.edu/95406176/Climatic_changes_and_sea_level_fluctuations_in_the_Danian_Selandian_boundary_interval_of_Tunesia_an_ostracod_perspective","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406175"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406175/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_"><img alt="Research paper thumbnail of A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406175/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_">A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)</a></div><div class="wp-workCard_item"><span>Studia Universitatis …</span><span>, 2002</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... Title: A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania...</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">... Title: A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania). Authors: Smith, Th × Codrea, V Sasaran, E Van Itterbeeck, Jimmy Bultynck, Pierre Csiki, Z Dica, P Farcas, C Folie, A Garcia, G Godefroit, P. Issue Date: 2002. ...</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="95406175"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406175"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406175; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406175]").text(description); $(".js-view-count[data-work-id=95406175]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406175; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406175']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406175]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406175,"title":"A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)","internal_url":"https://www.academia.edu/95406175/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406174"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406174/Palynostratigraphy_of_the_Maastrichtian_dinosaur_and_mammal_sites_of_the_R%C3%A2ul_Mare_and_Barbat_Valleys_Ha%C5%A3eg_Basin_Romania_"><img alt="Research paper thumbnail of Palynostratigraphy of the Maastrichtian dinosaur-and mammal sites of the Râul Mare and Barbat Valleys (Haţeg Basin, Romania)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406174/Palynostratigraphy_of_the_Maastrichtian_dinosaur_and_mammal_sites_of_the_R%C3%A2ul_Mare_and_Barbat_Valleys_Ha%C5%A3eg_Basin_Romania_">Palynostratigraphy of the Maastrichtian dinosaur-and mammal sites of the Râul Mare and Barbat Valleys (Haţeg Basin, Romania)</a></div><div class="wp-workCard_item"><span>Geologica Carpathica</span><span>, 2005</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406174"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406174"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406174; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406174]").text(description); $(".js-view-count[data-work-id=95406174]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406174; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406174']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406174]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406174,"title":"Palynostratigraphy of the Maastrichtian dinosaur-and mammal sites of the Râul Mare and Barbat Valleys (Haţeg Basin, Romania)","internal_url":"https://www.academia.edu/95406174/Palynostratigraphy_of_the_Maastrichtian_dinosaur_and_mammal_sites_of_the_R%C3%A2ul_Mare_and_Barbat_Valleys_Ha%C5%A3eg_Basin_Romania_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406162"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406162/A_New_Model_for_the_Evolution_of_Oceanic_Transform_Faults_Based_on_3D_Broadband_Seismic_Observations_From_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_in_the_Eastern_Gulf_of_Guinea"><img alt="Research paper thumbnail of A New Model for the Evolution of Oceanic Transform Faults Based on 3D Broadband Seismic Observations From São Tomé and Príncipe in the Eastern Gulf of Guinea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406162/A_New_Model_for_the_Evolution_of_Oceanic_Transform_Faults_Based_on_3D_Broadband_Seismic_Observations_From_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_in_the_Eastern_Gulf_of_Guinea">A New Model for the Evolution of Oceanic Transform Faults Based on 3D Broadband Seismic Observations From São Tomé and Príncipe in the Eastern Gulf of Guinea</a></div><div class="wp-workCard_item"><span>Geochemistry, Geophysics, Geosystems</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="95406162"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406162"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406162; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406162]").text(description); $(".js-view-count[data-work-id=95406162]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406162; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406162']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406162]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406162,"title":"A New Model for the Evolution of Oceanic Transform Faults Based on 3D Broadband Seismic Observations From São Tomé and Príncipe in the Eastern Gulf of Guinea","internal_url":"https://www.academia.edu/95406162/A_New_Model_for_the_Evolution_of_Oceanic_Transform_Faults_Based_on_3D_Broadband_Seismic_Observations_From_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_in_the_Eastern_Gulf_of_Guinea","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="17390882"><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/17390882/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_"><img alt="Research paper thumbnail of A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)" class="work-thumbnail" src="https://attachments.academia-assets.com/39482307/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/17390882/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_">A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ubbcluj.academia.edu/EmanoilSasaran">Emanoil Sasaran</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/JimmyVanItterbeeck">Jimmy Van Itterbeeck</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://ubbcluj.academia.edu/VladACodrea">Vlad A. Codrea</a></span></div><div class="wp-workCard_item"><span>Studia Universitatis …</span><span>, 2002</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Three exceptional fossiliferous marl pockets yielding respectively micro-vertebrate, ornithopod 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">Three exceptional fossiliferous marl pockets yielding respectively micro-vertebrate, ornithopod and sauropod concentrated remains have been discovered in the new Maastrichtian Nălaţ-Vad locality (Haţeg Basin, Romania). The facies assemblage indicates a fluvial palaeoenvironment with sandy channel infills and silty and clayey floodplain deposits containing well-developed calcretes. Large megaloolithid-type dinosaur eggs have been found in association with these calcretic palaeosols. In the ornithopod pocket the disconnected bones are abundant and apparently belong to a single specimen referred to as Iguanodontia indet. The most remarkable collected micro-remains are teeth and jaws of multituberculate mammals representing the richest concentration of mammal remains from the Late Cretaceous of Europe.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b20d2a27cd2dd99d62ab2c316634e1f7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39482307,"asset_id":17390882,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39482307/download_file?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="17390882"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="17390882"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17390882; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17390882]").text(description); $(".js-view-count[data-work-id=17390882]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17390882; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17390882']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "b20d2a27cd2dd99d62ab2c316634e1f7" } } $('.js-work-strip[data-work-id=17390882]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17390882,"title":"A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)","internal_url":"https://www.academia.edu/17390882/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_","owner_id":164345,"coauthors_can_edit":true,"owner":{"id":164345,"first_name":"Emanoil","middle_initials":null,"last_name":"Sasaran","page_name":"EmanoilSasaran","domain_name":"ubbcluj","created_at":"2010-04-07T04:24:44.927-07:00","display_name":"Emanoil Sasaran","url":"https://ubbcluj.academia.edu/EmanoilSasaran"},"attachments":[{"id":39482307,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39482307/thumbnails/1.jpg","file_name":"A_new_exceptional_vertebrate_site_from_t20151027-13450-9zntul.pdf","download_url":"https://www.academia.edu/attachments/39482307/download_file","bulk_download_file_name":"A_new_exceptional_vertebrate_site_from_t.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39482307/A_new_exceptional_vertebrate_site_from_t20151027-13450-9zntul-libre.pdf?1446014172=\u0026response-content-disposition=attachment%3B+filename%3DA_new_exceptional_vertebrate_site_from_t.pdf\u0026Expires=1740873910\u0026Signature=W8NUBX469UMJT8DddoNax6sUSBmFNRLLb6Y9OfknQTj-FQ0u6Uj4eKk6ZjZFATWoEM1Nffji9qjoV5knw7fWZoHV-ivnN2ZnnKvIBBwDM7BNTs0nUc5cx9uPzisJBUvA52ybtVz2h3CcJrAFead6fFHo63N1zvx5CT010n3fRn6A3IUQZ-~Whhuq2JFCzrw1n6nM1pEz9UerfI6l8YL3Rk1bZBFja7GEmN~1Zh~L6eEJwr99HF7nR9iZmPNK5qIQB2n~vN3Z7DKWN0F6xYfThUW~mfbE4n16AtkNgVYfpBJyNZElXu1UIcQkh7JV9mqqCzftwekiuouyb84W76dYMQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856260"><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/3856260/Oldest_Plesiadapiform_Mammalia_Proprimates_from_Asia_and_its_palaeobiogeographical_implications_for_faunal_interchange_with_North_America"><img alt="Research paper thumbnail of Oldest Plesiadapiform (Mammalia, Proprimates) from Asia and its palaeobiogeographical implications for faunal interchange with North America" class="work-thumbnail" src="https://attachments.academia-assets.com/50114322/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/3856260/Oldest_Plesiadapiform_Mammalia_Proprimates_from_Asia_and_its_palaeobiogeographical_implications_for_faunal_interchange_with_North_America">Oldest Plesiadapiform (Mammalia, Proprimates) from Asia and its palaeobiogeographical implications for faunal interchange with North America</a></div><div class="wp-workCard_item"><span>Comptes Rendus Palevol</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Carpolestid plesiadapiforms are well known in several lineages from the North American Palaeocene...</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">Carpolestid plesiadapiforms are well known in several lineages from the North American Palaeocene, but they are absent from Europe and known, until now, by only two taxa from the Early Eocene of Asia. Here we describe a new genus of Carpolestinae from the Late Palaeocene locality of Subeng in Inner Mongolia (China). In its morphological characteristics,</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f956c0854d88cd09c0f53406c40cd522" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114322,"asset_id":3856260,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114322/download_file?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="3856260"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856260"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856260; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856260]").text(description); $(".js-view-count[data-work-id=3856260]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856260; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856260']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "f956c0854d88cd09c0f53406c40cd522" } } $('.js-work-strip[data-work-id=3856260]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856260,"title":"Oldest Plesiadapiform (Mammalia, Proprimates) from Asia and its palaeobiogeographical implications for faunal interchange with North America","internal_url":"https://www.academia.edu/3856260/Oldest_Plesiadapiform_Mammalia_Proprimates_from_Asia_and_its_palaeobiogeographical_implications_for_faunal_interchange_with_North_America","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114322,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114322/thumbnails/1.jpg","file_name":"Oldest_Plesiadapiform_Mammalia_Proprima20161104-26169-k7esk9.pdf","download_url":"https://www.academia.edu/attachments/50114322/download_file","bulk_download_file_name":"Oldest_Plesiadapiform_Mammalia_Proprimat.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114322/Oldest_Plesiadapiform_Mammalia_Proprima20161104-26169-k7esk9-libre.pdf?1478319534=\u0026response-content-disposition=attachment%3B+filename%3DOldest_Plesiadapiform_Mammalia_Proprimat.pdf\u0026Expires=1740873910\u0026Signature=KAe1L~C8tvBfLUaqsxcgbc6q1sc0m-Z9l15aXA2x7yZH29ypgD0OmOW5zm7ZRSJGXUrrOV9hX33uFU2agIJmAR7AhUm2FarYyfpHv0y~sxrKJFntOIg9tmgka3yJqRsJpXml5HH1gbfBFvR9TnHqWSgVq5pRmgq-xzZr3zMJ-rXXW5EvnS0hRjMiHdkPhTP3XrYgwsGfMvHsC-FSkGjNmNmwP3S6-EZ5yCH8hjlasekd2XxXSnRnC5x8cmFjdmONfjfdGB9C33QE7QDTzI~jnL4Nkd7OvJ~gKP-KdfKIUsR~j2okUO2RtB4wsUUvq56CnzQErm1nWI6oiKmJiutGBw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856259"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/3856259/Taphonomy_and_Age_Profile_of_a_Latest_Cretaceous_Dinosaur_Bone_Bed_in_Far_Eastern_Russia"><img alt="Research paper thumbnail of Taphonomy and Age Profile of a Latest Cretaceous Dinosaur Bone Bed in Far Eastern Russia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/3856259/Taphonomy_and_Age_Profile_of_a_Latest_Cretaceous_Dinosaur_Bone_Bed_in_Far_Eastern_Russia">Taphonomy and Age Profile of a Latest Cretaceous Dinosaur Bone Bed in Far Eastern Russia</a></div><div class="wp-workCard_item"><span>Palaios</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A large dinosaur bone bed has been investigated in the Udurchukan Formation (?late Maastrichtian)...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A large dinosaur bone bed has been investigated in the Udurchukan Formation (?late Maastrichtian) at Blagoveschensk, Far Eastern Russia. The observed mixture of unstratified fine and coarse sediments in the bone bed is typical for sediment-gravity-flow deposits. It is ...</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="3856259"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856259"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856259; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856259]").text(description); $(".js-view-count[data-work-id=3856259]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856259; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856259']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=3856259]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856259,"title":"Taphonomy and Age Profile of a Latest Cretaceous Dinosaur Bone Bed in Far Eastern Russia","internal_url":"https://www.academia.edu/3856259/Taphonomy_and_Age_Profile_of_a_Latest_Cretaceous_Dinosaur_Bone_Bed_in_Far_Eastern_Russia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="3856258"><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/3856258/Woodland_in_a_fluvio_lacustrine_environment_on_the_dry_Mongolian_Plateau_during_the_late_Paleocene_Evidence_from_the_mammal_bearing_Subeng_section_Inner_Mongolia_P_R_China"><img alt="Research paper thumbnail of Woodland in a fluvio-lacustrine environment on the dry Mongolian Plateau during the late Paleocene: Evidence from the mammal bearing Subeng section (Inner Mongolia, P.R. China" class="work-thumbnail" src="https://attachments.academia-assets.com/50114318/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/3856258/Woodland_in_a_fluvio_lacustrine_environment_on_the_dry_Mongolian_Plateau_during_the_late_Paleocene_Evidence_from_the_mammal_bearing_Subeng_section_Inner_Mongolia_P_R_China">Woodland in a fluvio-lacustrine environment on the dry Mongolian Plateau during the late Paleocene: Evidence from the mammal bearing Subeng section (Inner Mongolia, P.R. China</a></div><div class="wp-workCard_item"><span>Palaeogeography Palaeoclimatology Palaeoecology</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the understanding of the global faunal turnover during the Paleocene–Eocene transition, an imp...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the understanding of the global faunal turnover during the Paleocene–Eocene transition, an important role has been attributed to the Asian continent, although the Asian fossil record for this period is still incomplete. Here we present a multidisciplinary study of the Subeng section (Inner Mongolia, P.R. China), integrating sedimentological, stratigraphical and diverse palaeontological data, in order to reconstruct the palaeoenvironment and to enhance the understanding of the late Paleocene communities that once thrived on the Mongolian Plateau. The Subeng section starts with the Maastrichtian Iren Dabasu Formation directly covered by the late Paleocene Nomogen Formation. This Nomogen Formation is composed of typical lacustrine deposits at the base, covered by fluvio-lacustrine deposits at the top. Both types of deposits provided rich ostracod and charophyte assemblages, closest to those of the Naran Member, Naran Bulak Formation of Mongolia. Palynomorphs from the lake sediments suggest a local flora at Subeng more wooded and closed than reported from elsewhere in this region. The fluvio-lacustrine deposits of the Nomogen Formation have yielded a vertebrate fauna especially rich in mammals. The mammal fauna from Subeng is close to that from Bayan Ulan and typical for the Gashatan Asian Land Mammal Age. The presence of reworked pedogenic carbonate nodules and mud aggregates suggests an at least seasonally dry regional climate. Combined sedimentological and palaeontological data suggest the late Paleocene Nomogen Formation at Subeng was an isolated woodland in a fluvio-lacustrine environment, representing a locally humid environment on the semi-arid Mongolian Plateau. The mammal fauna reflects these differences and shows a number of relatives to mammals from the more humid northeastern Chinese biotic province as well as some North American immigrants.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a2da55ca3039f61c23dd87a38ad10f14" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114318,"asset_id":3856258,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114318/download_file?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="3856258"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856258"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856258; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856258]").text(description); $(".js-view-count[data-work-id=3856258]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856258; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856258']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "a2da55ca3039f61c23dd87a38ad10f14" } } $('.js-work-strip[data-work-id=3856258]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856258,"title":"Woodland in a fluvio-lacustrine environment on the dry Mongolian Plateau during the late Paleocene: Evidence from the mammal bearing Subeng section (Inner Mongolia, P.R. China","internal_url":"https://www.academia.edu/3856258/Woodland_in_a_fluvio_lacustrine_environment_on_the_dry_Mongolian_Plateau_during_the_late_Paleocene_Evidence_from_the_mammal_bearing_Subeng_section_Inner_Mongolia_P_R_China","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114318,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114318/thumbnails/1.jpg","file_name":"Woodland_in_a_fluvio-lacustrine_environm20161104-26169-wew6g0.pdf","download_url":"https://www.academia.edu/attachments/50114318/download_file","bulk_download_file_name":"Woodland_in_a_fluvio_lacustrine_environm.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114318/Woodland_in_a_fluvio-lacustrine_environm20161104-26169-wew6g0-libre.pdf?1478319542=\u0026response-content-disposition=attachment%3B+filename%3DWoodland_in_a_fluvio_lacustrine_environm.pdf\u0026Expires=1740780277\u0026Signature=XPGrJjT7W~WV4qAppMfWAczqjKARyCG22NxU3RRPUkAHK-5zBYi4IOuS7hYE9iLr94gxW9hnHd9Sgj~aIIM6I5KI1T0d0bXsbaXNKwqQnYQLWddeUDU9GNFFFcXpZyH8GTOGlmthAVsVC5aBU-V3Rz9wbm6sRPXTeKSE~yt1w~bCFHf6fGZOQ66wjyldB9TxMAtQ~5HyB3aXDxRVMNUbOLEUhJDZhYRMMUyksNBs41JSQrAlz0WF~lC1kdKQArWyZNptHU0eYN5rrKKL1DVLa2RFTV4FqOuQWbmc-TMryTt7drPGGe7CU7OCygD0ODGRWuDLPfBUZJaAoplumkeLiQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856257"><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/3856257/The_age_of_the_dinosaur_bearing_Cretaceous_sediments_at_Dashuiguo_Inner_Mongolia_P_R_China_based_on_charophytes_ostracods_and_palynomorphs"><img alt="Research paper thumbnail of The age of the dinosaur-bearing Cretaceous sediments at Dashuiguo, Inner Mongolia, P.R. China based on charophytes, ostracods and palynomorphs" class="work-thumbnail" src="https://attachments.academia-assets.com/50114320/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/3856257/The_age_of_the_dinosaur_bearing_Cretaceous_sediments_at_Dashuiguo_Inner_Mongolia_P_R_China_based_on_charophytes_ostracods_and_palynomorphs">The age of the dinosaur-bearing Cretaceous sediments at Dashuiguo, Inner Mongolia, P.R. China based on charophytes, ostracods and palynomorphs</a></div><div class="wp-workCard_item"><span>Cretaceous Research</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Dashuiguo Formation has yielded numerous fossils of Probactrosaurus, a dinosaur with both igu...</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 Dashuiguo Formation has yielded numerous fossils of Probactrosaurus, a dinosaur with both iguanodontid and hadrosaurid characteristics. Based on the evolutionary position of Probactrosaurus, the dinosaur-bearing sediments have been considered to be Aptian–Albian, but new micropalaeontological data (charophytes, ostracods and palynomorphs) indicate that they may be as old as Barremian. The three charophyte species recovered are indicative of a Barremian–Aptian age. A rich fauna of non-marine Ostracoda (13 species in nine genera) includes two species described as new, Cypridea pseudomodica sp. nov. and C. dashuiguoensis sp. nov., while the remaining eleven species have been described previously from Lower Cretaceous sediments of the Gobi Basin and adjacent areas in China. Based on the ostracod assemblage, the Dashuiguo Formation can be correlated with the Dzun Bayn suite of the Gobi Basin and can therefore be regarded as Barremian–Albian in age. The palynomorph assemblage is very similar to that described from the nearby Tebch site with an estimated Barremian–Early Aptian age and is radiometrically calibrated on the basis of an overlying basalt layer.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8c88e1fd8d5960bf81f4aeae5e969187" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114320,"asset_id":3856257,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114320/download_file?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="3856257"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856257"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856257; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856257]").text(description); $(".js-view-count[data-work-id=3856257]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856257; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856257']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "8c88e1fd8d5960bf81f4aeae5e969187" } } $('.js-work-strip[data-work-id=3856257]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856257,"title":"The age of the dinosaur-bearing Cretaceous sediments at Dashuiguo, Inner Mongolia, P.R. China based on charophytes, ostracods and palynomorphs","internal_url":"https://www.academia.edu/3856257/The_age_of_the_dinosaur_bearing_Cretaceous_sediments_at_Dashuiguo_Inner_Mongolia_P_R_China_based_on_charophytes_ostracods_and_palynomorphs","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114320,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114320/thumbnails/1.jpg","file_name":"j.cretres.2004.02.00120161104-26173-1r97nb.pdf","download_url":"https://www.academia.edu/attachments/50114320/download_file","bulk_download_file_name":"The_age_of_the_dinosaur_bearing_Cretaceo.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114320/j.cretres.2004.02.00120161104-26173-1r97nb-libre.pdf?1478319540=\u0026response-content-disposition=attachment%3B+filename%3DThe_age_of_the_dinosaur_bearing_Cretaceo.pdf\u0026Expires=1740873910\u0026Signature=OA0vdl5EMNBZw8KGLorOg3gVTWEbq2KzUtwOgoT8YMQGeE2WjrX0aDQPcIvsq1MUcf12U1wwrXGU5LtSVvH4UGIOgSx8-Bu9~SsLwnVPZgip8~uBb~Zv9e1084BBIr~kLh5bOWkObD7rt0jm3oOb92dpcyFw7iygx7GmEnz6MX6ANV7wjnpzl0j1nDhCeM-pHKkJ-MAOW-VaTRLont2-ZkXvIyR-pEkh9v8opFj5weDCZuJGgeNpC~lkIK-X0~rNIBLcBYminb-hBVcJSyKFRMkoLD~AI1nbwI0JJwgN5boMHYrZv4PT-~h55FZq6fzTOPlEmeE0lqZZ88vbvIvvDQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856256"><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/3856256/Sedimentology_of_the_Upper_Cretaceous_mammal_and_dinosaur_bearing_sites_along_the_R%C3%A2ul_Mare_and_Barbat_rivers_Ha_t_eg_Basin_Romania"><img alt="Research paper thumbnail of Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Barbat rivers, Ha t ̧ eg Basin, Romania" class="work-thumbnail" src="https://attachments.academia-assets.com/50114316/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/3856256/Sedimentology_of_the_Upper_Cretaceous_mammal_and_dinosaur_bearing_sites_along_the_R%C3%A2ul_Mare_and_Barbat_rivers_Ha_t_eg_Basin_Romania">Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Barbat rivers, Ha t ̧ eg Basin, Romania</a></div><div class="wp-workCard_item"><span>Cretaceous Research</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Mammal and dinosaur localities in the Haeg Basin belonging to the Upper Cretaceous Sânpetru and D...</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">Mammal and dinosaur localities in the Haeg Basin belonging to the Upper Cretaceous Sânpetru and Densuş-Ciula formations have been known since the beginning of the last century. Recently, two new exposures with a comparable fauna have been discovered in the Râul Mare valley. The sediments at these new sites, Toteşti-baraj and Năla-Vad, have been compared with the sediments at the previously known Pui site. At all three sites the deposits reflect a fluvial environment with coarse-grained channel deposits channelized in fine-grained floodplain deposits with calcrete palaeosols. However, the nature of the calcrete palaeosols is different at the three sites. At Toteşti-baraj and Năla-Vad, hydromorphic calcic vertisols have been observed, and locally these grade into groundwater calcretes. At Pui, the calcretes are associated with redbed deposits. Considering the similar palaeogeographical situation and age of the deposits at the three sites, the difference in soil type should not be interpreted as a climatic difference but rather as a difference in the height of the palaeogroundwater table. The soils at Pui are indicative of a general semi-arid climate. Those at Toteşti-baraj and Năla-Vad do not directly reflect the climate, but rather the high seasonal groundwater table. Differences in palaeohydrology between the sites are reflected in the fossil content with humidity-loving species only occurring at the Râul Mare sites.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a6cd1f01ef4efb40f412b9f9d090427b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114316,"asset_id":3856256,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114316/download_file?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="3856256"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856256"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856256; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856256]").text(description); $(".js-view-count[data-work-id=3856256]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856256; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856256']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "a6cd1f01ef4efb40f412b9f9d090427b" } } $('.js-work-strip[data-work-id=3856256]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856256,"title":"Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Barbat rivers, Ha t ̧ eg Basin, Romania","internal_url":"https://www.academia.edu/3856256/Sedimentology_of_the_Upper_Cretaceous_mammal_and_dinosaur_bearing_sites_along_the_R%C3%A2ul_Mare_and_Barbat_rivers_Ha_t_eg_Basin_Romania","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114316,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114316/thumbnails/1.jpg","file_name":"Itterbeeck-KRes-2004.pdf","download_url":"https://www.academia.edu/attachments/50114316/download_file","bulk_download_file_name":"Sedimentology_of_the_Upper_Cretaceous_ma.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114316/Itterbeeck-KRes-2004-libre.pdf?1478319548=\u0026response-content-disposition=attachment%3B+filename%3DSedimentology_of_the_Upper_Cretaceous_ma.pdf\u0026Expires=1740873910\u0026Signature=ZmTol9gZRGXA6id~skik2T9blWcheIcK5NcRlcjQx2gYuxajP2r9AOnPmtnUXoiaFnXdLqPzSt3eiM4CxovTnktjn5PpfJVe5oJtfc5wm2-kqTQ8nzUV-4R-MSsZ89ouut5SBlWZPV73gbhGVYqUrefPv6esxKHLPwJz~c9Z1WhFiksErt2iLsKC73UmM8cZkoE5Y58aPFRQIGzCk07y47I4c3T1Umj97qYoM1PrYwMSsidbFp6Q1Jhm5PckVqio9g9oth7oikd7~YBjJ7j8OqrEywN8kl1l1m5WmXGEMEJOgi9b3S~ZBSIxTm~IXcaK2hf2fDt~oWFrdrSuxZXDSg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856255"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/3856255/Stratigraphy_sedimentology_and_palaeoecology_of_the_dinosaur_bearing_Kundur_section_Zeya_Bureya_Basin_Amur_Region_Far_Eastern_Russia"><img alt="Research paper thumbnail of Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/3856255/Stratigraphy_sedimentology_and_palaeoecology_of_the_dinosaur_bearing_Kundur_section_Zeya_Bureya_Basin_Amur_Region_Far_Eastern_Russia">Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia</a></div><div class="wp-workCard_item"><span>Geological Magazine</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... In North America, the same floristic changes as those observed at the end of the Asian W. spi...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... In North America, the same floristic changes as those observed at the end of the Asian W. spinataA. subtilis palynozone coincide with the K/P boundary (Braman &amp;amp;amp;amp; Sweet, 1999; Nichols, 1990; Nichols, 2002; Nichols &amp;amp;amp;amp; Sweet, 1993; Sweet, Braman &amp;amp;amp;amp; Lerbekmo, 1999; Tschudy ...</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="3856255"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856255"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856255; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856255]").text(description); $(".js-view-count[data-work-id=3856255]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856255; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856255']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=3856255]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856255,"title":"Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia","internal_url":"https://www.academia.edu/3856255/Stratigraphy_sedimentology_and_palaeoecology_of_the_dinosaur_bearing_Kundur_section_Zeya_Bureya_Basin_Amur_Region_Far_Eastern_Russia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="3856254"><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/3856254/Stratigraphy_and_palaeoenvironment_of_the_dinosaur_bearing_Upper_Cretaceous_Iren_Dabasu_Formation_Inner_Mongolia_Peoples_Republic_of_China"><img alt="Research paper thumbnail of Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China" class="work-thumbnail" src="https://attachments.academia-assets.com/50114324/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/3856254/Stratigraphy_and_palaeoenvironment_of_the_dinosaur_bearing_Upper_Cretaceous_Iren_Dabasu_Formation_Inner_Mongolia_Peoples_Republic_of_China">Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China</a></div><div class="wp-workCard_item"><span>Cretaceous Research</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">New field observations and sedimentological analyses of the dinosaur-bearing Upper Cretaceous Ire...</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">New field observations and sedimentological analyses of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation in the Iren Nor region of Inner Mongolia (People's Republic of China) have led to a better understanding of its palaeoenvironment. The fluvial deposits represent a braided river that, due to the large amount of fines, does not fit the classical model for braided rivers. The study area is divided into two parts: in the northern part, sediments of the main channel belt of the ancient braided river system are exposed along a dry river valley on the northern edge of the Iren Nor salt lake, while in the southern part, comprising all other studied exposures, different facies of the ancient floodplain are represented, including minor channels, temporary ponds, and palaeosols. The difference between the northern and southern parts is also reflected in the fossil content; only the southern exposures have yielded dinosaur remains. The ancient braided river had a broad, vegetated floodplain populated by a diverse dinosaur fauna. Four species of charophytes are described and illustrated from the Iren Nor site, together with eight species of ostracods, one of which (Cypridea irennorensis sp. nov.) is new. Contrary to the vertebrate data, both groups of microfossils indicate a latest Cretaceous age (Campanian–Maastrichtian) for the Iren Dabasu Formation, and suggest a possible correlation with the Nemegt Formation, which would allow the age estimation to be refined to latest Campanian–Early Maastrichtian.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a3a3f3939fd02ef7355ad703dabf2765" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114324,"asset_id":3856254,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114324/download_file?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="3856254"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856254"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856254; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856254]").text(description); $(".js-view-count[data-work-id=3856254]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856254; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856254']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "a3a3f3939fd02ef7355ad703dabf2765" } } $('.js-work-strip[data-work-id=3856254]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856254,"title":"Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China","internal_url":"https://www.academia.edu/3856254/Stratigraphy_and_palaeoenvironment_of_the_dinosaur_bearing_Upper_Cretaceous_Iren_Dabasu_Formation_Inner_Mongolia_Peoples_Republic_of_China","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114324,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114324/thumbnails/1.jpg","file_name":"j.cretres.2005.03.00420161104-26167-sxh407.pdf","download_url":"https://www.academia.edu/attachments/50114324/download_file","bulk_download_file_name":"Stratigraphy_and_palaeoenvironment_of_th.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114324/j.cretres.2005.03.00420161104-26167-sxh407-libre.pdf?1478319540=\u0026response-content-disposition=attachment%3B+filename%3DStratigraphy_and_palaeoenvironment_of_th.pdf\u0026Expires=1740873910\u0026Signature=E7jGrjieeKZMF4ppnUzJE1RZ0FJLJippxU5zOBQp~ft-4n~P54oqWNjhBbMPh4-cqXvtfLR2dQ1pWAjmJNAxeSfZGLnUpXBzAlZWytA7-BLp0BPSdKM7TayPd5KhC6Meu~Q7iagFR-INOVARnpglpMl-xUXDnJppKqfjXTjJp4PbS4lxWdwZfvbMlmOhCDDfmd78307iEWEVdtriiiSllZeasWuX9hfSzJTU6jR5tHWxgC0Uur9-853a9ovF0SYWhz~WPMtgE80neHk1jYE7fDOmHKz-wTsqWNLiqtQxTfnfiuuy0WpiRicYJJfcVCQuZu7oElXEe3PaHvN6opi8MQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856253"><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/3856253/The_lambeosaurine_dinosaur_Amurosaurus_riabinini_from_the_Maastrichtian_of_Far_Eastern_Russia"><img alt="Research paper thumbnail of The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia" class="work-thumbnail" src="https://attachments.academia-assets.com/31498382/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/3856253/The_lambeosaurine_dinosaur_Amurosaurus_riabinini_from_the_Maastrichtian_of_Far_Eastern_Russia">The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Itterbeeck, J. 2004. The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Itterbeeck, J. 2004. The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia. Acta Palaeontologica Polonica 49 (4): 585-618.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6e0ad6f8775c90e2dfe38bfedffa2614" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":31498382,"asset_id":3856253,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/31498382/download_file?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="3856253"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856253"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856253; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856253]").text(description); $(".js-view-count[data-work-id=3856253]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856253; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856253']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "6e0ad6f8775c90e2dfe38bfedffa2614" } } $('.js-work-strip[data-work-id=3856253]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856253,"title":"The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia","internal_url":"https://www.academia.edu/3856253/The_lambeosaurine_dinosaur_Amurosaurus_riabinini_from_the_Maastrichtian_of_Far_Eastern_Russia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":31498382,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/31498382/thumbnails/1.jpg","file_name":"2004_godefroit_amurosaurus.pdf","download_url":"https://www.academia.edu/attachments/31498382/download_file","bulk_download_file_name":"The_lambeosaurine_dinosaur_Amurosaurus_r.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/31498382/2004_godefroit_amurosaurus-libre.pdf?1392348708=\u0026response-content-disposition=attachment%3B+filename%3DThe_lambeosaurine_dinosaur_Amurosaurus_r.pdf\u0026Expires=1740840026\u0026Signature=VIbuNl0LTRUDepXfur004y3Nr~bsrnk5b5UUBdnNww58Hzn3wrz-AuVJ8OY~uvCUEspXPmVHFutbTsfUr7LJezrVH0kV9Qew3TZlMKQE7q-7jVd1IqXaxF0QG9NYwRh8YJG9zL89w~6Dr4a8HKBJeTe6H3Y9qet3Zc6GjQQmXdonsfrzoFlCJLBBmlypsuL8pJa3RKmAEU7qi3lYUHcsJ3xsURORu6x~kKHpevAHjkw6dQNOZMWm42fsgC0aywzvRgedm8gjbd8oMmKNf13gAMosonCStaOg~9wi60VfnPUyVimSx7L9TS9hej7PLHj8aU9wf6IJuZ2LOcyIoNAaMQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="604555" id="papers"><div class="js-work-strip profile--work_container" data-work-id="95406183"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea"><img alt="Research paper thumbnail of A new model for the evolution of oceanic transform faults based on 3D PSDM Seismic observations from São Tomé and Príncipe, eastern Gulf of Guinea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea">A new model for the evolution of oceanic transform faults based on 3D PSDM Seismic observations from São Tomé and Príncipe, eastern Gulf of Guinea</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&amp;amp;lt;p&amp;amp;gt;Oceanic Transform faults are one of the three major tectonic plate bound...</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">&amp;amp;lt;p&amp;amp;gt;Oceanic Transform faults are one of the three major tectonic plate boundaries and yet their evolution and deformational mechanism is not well understood. They are broadly considered to be dominated by strike-slip displacement along simple planar vertical faults and to be conservative in nature with no magmatic addition. Observations from Pre-Stack depth-migrated (PSDM) 3D seismic of Cretaceous-aged transforms in the eastern Gulf of Guinea allow complex internal architectures to be described, including crustal scale detachments and rotated packages of volcanics.&amp;amp;lt;/p&amp;amp;gt;&amp;amp;lt;p&amp;amp;gt;These insights demonstrate additional complexity previously only predicted in numerical simulations of spreading ridge-transform interaction, namely intra-transform extension at a high angle to the spreading orientation, and the addition of significant extrusive volcanic material. In the study area of S&amp;amp;amp;#227;o Tom&amp;amp;amp;#233; and Pr&amp;amp;amp;#237;ncipe, several Oceanic Fracture Zones (OFZ) are identified, consisting of a broad deformational zones that can be described from top to base crust. OFZ scarps are observed to connect at depth with zones of low angle reflectivity which dip into the OFZ and perpendicular to the spreading orientation. At depth they detach onto the Moho below, necking the adjacent crust along the length of the OFZ in the manner of extensional shear zones. Thickly stacked and tilted reflectors, interpreted as extrusive lava flows, are common above the shear zones and infill up to 75% of the crustal thickness. The entire OFZ stratigraphy is overlain and sealed by late-stage lavas that are continuous from the abyssal hills of the trailing spreading ridge. This constrains a process of oblique extension at a high angle to the spreading orientation along a low angle shear zone which also acts as a conduit for decompression related melt.&amp;amp;lt;/p&amp;amp;gt;&amp;amp;lt;p&amp;amp;gt;We demonstrate that transforms in S&amp;amp;amp;#227;o Tom&amp;amp;amp;#233; and Pr&amp;amp;amp;#237;ncipe were both non-conservative and not a simple strike slip fault zone, contradicting the current understanding of modern systems. This style of deformation has similarities with anomalously deep and smooth nodal basins which form at slow spreading inside-corner crust. Our model adds strong observational constraints to complement recent numerical models that predict oblique extension within transform zones.&amp;amp;lt;/p&amp;amp;gt;</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="95406183"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406183"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406183; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406183]").text(description); $(".js-view-count[data-work-id=95406183]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406183; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406183']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406183]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406183,"title":"A new model for the evolution of oceanic transform faults based on 3D PSDM Seismic observations from São Tomé and Príncipe, eastern Gulf of Guinea","internal_url":"https://www.academia.edu/95406183/A_new_model_for_the_evolution_of_oceanic_transform_faults_based_on_3D_PSDM_Seismic_observations_from_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_eastern_Gulf_of_Guinea","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406182"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406182/Detailed_lithostratigraphic_description_of_the_Wealden_facies_found_in_the_BER3_borehole_Bernissart_Belgium_Preliminary_comparison_with_the_subsequent_deposits_of_the_Hautrage_and_Thieu_facies_Mons_Basin_Belgium_"><img alt="Research paper thumbnail of Detailed lithostratigraphic description of the Wealden facies found in the BER3 borehole (Bernissart, Belgium). Preliminary comparison with the subsequent deposits of the Hautrage and Thieu facies (Mons Basin, Belgium)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406182/Detailed_lithostratigraphic_description_of_the_Wealden_facies_found_in_the_BER3_borehole_Bernissart_Belgium_Preliminary_comparison_with_the_subsequent_deposits_of_the_Hautrage_and_Thieu_facies_Mons_Basin_Belgium_">Detailed lithostratigraphic description of the Wealden facies found in the BER3 borehole (Bernissart, Belgium). Preliminary comparison with the subsequent deposits of the Hautrage and Thieu facies (Mons Basin, Belgium)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406182"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406182"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406182; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406182]").text(description); $(".js-view-count[data-work-id=95406182]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406182; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406182']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406182]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406182,"title":"Detailed lithostratigraphic description of the Wealden facies found in the BER3 borehole (Bernissart, Belgium). Preliminary comparison with the subsequent deposits of the Hautrage and Thieu facies (Mons Basin, Belgium)","internal_url":"https://www.academia.edu/95406182/Detailed_lithostratigraphic_description_of_the_Wealden_facies_found_in_the_BER3_borehole_Bernissart_Belgium_Preliminary_comparison_with_the_subsequent_deposits_of_the_Hautrage_and_Thieu_facies_Mons_Basin_Belgium_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406181"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406181/Stable_isotope_d13C_d18O_analyses_on_marine_ostracod_shells_from_the_Danian_Selandian_boundary_Paleocene_of_Tunisia"><img alt="Research paper thumbnail of Stable isotope (d13C, d18O) analyses on marine ostracod shells from the Danian/Selandian boundary (Paleocene) of Tunisia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406181/Stable_isotope_d13C_d18O_analyses_on_marine_ostracod_shells_from_the_Danian_Selandian_boundary_Paleocene_of_Tunisia">Stable isotope (d13C, d18O) analyses on marine ostracod shells from the Danian/Selandian boundary (Paleocene) of Tunisia</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406181"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406181"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406181; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406181]").text(description); $(".js-view-count[data-work-id=95406181]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406181; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406181']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406181]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406181,"title":"Stable isotope (d13C, d18O) analyses on marine ostracod shells from the Danian/Selandian boundary (Paleocene) of Tunisia","internal_url":"https://www.academia.edu/95406181/Stable_isotope_d13C_d18O_analyses_on_marine_ostracod_shells_from_the_Danian_Selandian_boundary_Paleocene_of_Tunisia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406180"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406180/Sea_level_and_paleoenvironment_of_the_Danian_Selandian_transition_in_Tunisia"><img alt="Research paper thumbnail of Sea level and paleoenvironment of the Danian/Selandian transition in Tunisia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406180/Sea_level_and_paleoenvironment_of_the_Danian_Selandian_transition_in_Tunisia">Sea level and paleoenvironment of the Danian/Selandian transition in Tunisia</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406180"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406180"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406180; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406180]").text(description); $(".js-view-count[data-work-id=95406180]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406180; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406180']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406180]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406180,"title":"Sea level and paleoenvironment of the Danian/Selandian transition in Tunisia","internal_url":"https://www.academia.edu/95406180/Sea_level_and_paleoenvironment_of_the_Danian_Selandian_transition_in_Tunisia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406179"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406179/Latest_Cretaceous_hadrosaurid_dinosaurs_from_Heilongjiang_Province_P_R_China_and_the_Amur_Region_Far_Eastern_Asia_"><img alt="Research paper thumbnail of Latest Cretaceous hadrosaurid dinosaurs from Heilongjiang Province (P. R. China) and the Amur Region (Far Eastern Asia)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406179/Latest_Cretaceous_hadrosaurid_dinosaurs_from_Heilongjiang_Province_P_R_China_and_the_Amur_Region_Far_Eastern_Asia_">Latest Cretaceous hadrosaurid dinosaurs from Heilongjiang Province (P. R. China) and the Amur Region (Far Eastern Asia)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406179"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406179"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406179; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406179]").text(description); $(".js-view-count[data-work-id=95406179]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406179; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406179']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406179]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406179,"title":"Latest Cretaceous hadrosaurid dinosaurs from Heilongjiang Province (P. R. China) and the Amur Region (Far Eastern Asia)","internal_url":"https://www.academia.edu/95406179/Latest_Cretaceous_hadrosaurid_dinosaurs_from_Heilongjiang_Province_P_R_China_and_the_Amur_Region_Far_Eastern_Asia_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406178"><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/95406178/Nonmarine_ostracods_from_the_Paleocene_Subeng_mammal_site_inner_Mongolia_P_R_China_taxonomy_and_biostratigraphy"><img alt="Research paper thumbnail of Nonmarine ostracods from the Paleocene Subeng mammal site, inner Mongolia, P.R. China, taxonomy and biostratigraphy" class="work-thumbnail" src="https://attachments.academia-assets.com/97598175/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/95406178/Nonmarine_ostracods_from_the_Paleocene_Subeng_mammal_site_inner_Mongolia_P_R_China_taxonomy_and_biostratigraphy">Nonmarine ostracods from the Paleocene Subeng mammal site, inner Mongolia, P.R. China, taxonomy and biostratigraphy</a></div><div class="wp-workCard_item"><span>Bulletin Institut Royal Des Sciences Naturelles De Belgique Sciences De La Terre</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Nine species, belonging to six genera, of nonmarine ostracods of the mammal-bearing horizons of t...</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">Nine species, belonging to six genera, of nonmarine ostracods of the mammal-bearing horizons of the Subeng locality are described and figured. One species is new: Timiriasevia subengensis sp. nov. Seven species are in common with the Paleocene White Beds (Naran Member) of the Naran Bulak Formation, Nemegt Basin, Mongolia. The two other species are known from the Paleocene of China. Based on the ostracod fauna, the mammalbearing horizons of the Subeng site (Bayan Ulan Beds, Nomogen Formation) are late Paleocene in age and can be correlated with the Naran Member of the Naran Bulak Formation.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="142f03056aed20167cb333513ea22875" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":97598175,"asset_id":95406178,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/97598175/download_file?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="95406178"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406178"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406178; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406178]").text(description); $(".js-view-count[data-work-id=95406178]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406178; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406178']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "142f03056aed20167cb333513ea22875" } } $('.js-work-strip[data-work-id=95406178]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406178,"title":"Nonmarine ostracods from the Paleocene Subeng mammal site, inner Mongolia, P.R. China, taxonomy and biostratigraphy","internal_url":"https://www.academia.edu/95406178/Nonmarine_ostracods_from_the_Paleocene_Subeng_mammal_site_inner_Mongolia_P_R_China_taxonomy_and_biostratigraphy","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":97598175,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97598175/thumbnails/1.jpg","file_name":"irscnb_p4087_022b9dx_74-2_bulletin-11.pdf","download_url":"https://www.academia.edu/attachments/97598175/download_file","bulk_download_file_name":"Nonmarine_ostracods_from_the_Paleocene_S.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97598175/irscnb_p4087_022b9dx_74-2_bulletin-11-libre.pdf?1674302121=\u0026response-content-disposition=attachment%3B+filename%3DNonmarine_ostracods_from_the_Paleocene_S.pdf\u0026Expires=1740873910\u0026Signature=MZdNBxhZnrpLuLAi0VcOPrKN2ifT~HVV9C41hFesHb6hQ8MOJ6MO04FobnooOKg7wNx-k7s2qfgpWHkJu8~PqnOJeGqElOpfmpLC7SPklv5ia6cqe-v5dn5Sp3umdlQE3hmexyWvMqPhRLs77X59lobJQ2bmxdWN~vf6FcE0rrcIpsKUlwN8GUWrZIMY72vXxD0qSOCq3YTG5key2p1tT7Oo3XTniX-39A0Or21PJcCdNvmZecYFoPIxqSePW3WO9TlntbAwE3XxYmjCMtQpuouglGARoioIOW26uT90FmeS1wEYNTIuXMKswyCTLwTmapUxGGyU6K-grKl36vZ3Jg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="95406177"><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/95406177/Cenozoic_deformation_and_exhumation_of_the_Kampot_Fold_Belt_and_implications_for_south_Indochina_tectonics"><img alt="Research paper thumbnail of Cenozoic deformation and exhumation of the Kampot Fold Belt and implications for south Indochina tectonics" class="work-thumbnail" src="https://attachments.academia-assets.com/97598162/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/95406177/Cenozoic_deformation_and_exhumation_of_the_Kampot_Fold_Belt_and_implications_for_south_Indochina_tectonics">Cenozoic deformation and exhumation of the Kampot Fold Belt and implications for south Indochina tectonics</a></div><div class="wp-workCard_item"><span>Journal of Geophysical Research: Solid Earth</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Latest Mesozoic to earliest Cenozoic deformation affected SE Asia's Sundaland-core. The deformati...</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">Latest Mesozoic to earliest Cenozoic deformation affected SE Asia's Sundaland-core. The deformation event bridges the Mesozoic SE Asian fusion with the Cenozoic era of rifting, translation, basin formation and the creation of modern SE Asian oceans. Southern Cambodia and Vietnam are central to this shift, but geological investigations of the region are in their infancy. Based on apatite and zircon fission track analyses (AFTA and ZFTA), stratigraphic and structural observations, seismic data, thermal maturity and igneous rock dating the geological evolution of southern Cambodia and Vietnam is investigated. Diverse depositional styles, igneous activity, structural deformation and sub-surface unconformities testify to a highly variable Phanerozoic tectonic setting. Major latest Cretaceous to Paleocene thrusting and uplift affected the Kampot Fold Belt and surrounding regions and the associated up to ~11 km exhumation probably exceeds earlier denudation events since at least Permian time. The present relief of the Bokor Mountains rising high above the Kampot Fold Belt represents an artifact after differential erosion and only 2.5-4.5 km of erosion affected this area. The latest Cretaceous to Paleocene orogenesis affected much of greater Indochina probably owing to plate collision along eastern Sundaland or a combination of collisions along both east and west Sundaland. AFTA and ZFTA data document protracted cooling of Cretaceous granites and locally elevated thermal gradients persisting a few tens of million years after their emplacement. The thermal gradient had stabilized by early Miocene time, and Miocene cooling probably reflects a renewed denudation pulse driven by either regional tectonism or climate-enhanced erosion.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b4223d8a4bdaff8364a09687572fd1a6" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":97598162,"asset_id":95406177,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/97598162/download_file?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="95406177"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406177"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406177; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406177]").text(description); $(".js-view-count[data-work-id=95406177]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406177; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406177']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "b4223d8a4bdaff8364a09687572fd1a6" } } $('.js-work-strip[data-work-id=95406177]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406177,"title":"Cenozoic deformation and exhumation of the Kampot Fold Belt and implications for south Indochina tectonics","internal_url":"https://www.academia.edu/95406177/Cenozoic_deformation_and_exhumation_of_the_Kampot_Fold_Belt_and_implications_for_south_Indochina_tectonics","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":97598162,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97598162/thumbnails/1.jpg","file_name":"2016jb01284720230121-1-1ehdx2l.pdf","download_url":"https://www.academia.edu/attachments/97598162/download_file","bulk_download_file_name":"Cenozoic_deformation_and_exhumation_of_t.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97598162/2016jb01284720230121-1-1ehdx2l-libre.pdf?1674302024=\u0026response-content-disposition=attachment%3B+filename%3DCenozoic_deformation_and_exhumation_of_t.pdf\u0026Expires=1740840026\u0026Signature=WWIa~rEdTrKdikPz2oPYNCg5sktLX2w9tlbvkz3WZb9gvqGSUexSHQVAglio8kQxpm7Cqh63q1pZUXUNBQY-RyyeZGe5LRoIY2iSl1lTMo17t-2ejXcOHi~Xq9SDqkjUbmC89OogfogmxViinmBCn5k9kK5sTzLhCOaMKKa02JjYpOe6Yt7tg1noNZJdBzRFMMuXFLBqb5Aha18n70lfgiJF5U35I~PY-70mOJSBqdc2uKzChk~GVHxhkzwhxR1YwuF6PtwLPciBozJKy9fy8KhhosgUt~IJIh~fDCnlqNJrVlH8OCTqW4GuMkwDDAEHCsFj1lMTfNsdrNHMcyuBjA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="95406176"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406176/Climatic_changes_and_sea_level_fluctuations_in_the_Danian_Selandian_boundary_interval_of_Tunesia_an_ostracod_perspective"><img alt="Research paper thumbnail of Climatic changes and sea-level fluctuations in the Danian/Selandian boundary interval of Tunesia: an ostracod perspective" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406176/Climatic_changes_and_sea_level_fluctuations_in_the_Danian_Selandian_boundary_interval_of_Tunesia_an_ostracod_perspective">Climatic changes and sea-level fluctuations in the Danian/Selandian boundary interval of Tunesia: an ostracod perspective</a></div><div class="wp-workCard_item"><span>… and Abstracts Berlin …</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Most research efforts on the Paleocene epoch have been invested in both its lower and upper bound...</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">Most research efforts on the Paleocene epoch have been invested in both its lower and upper boundaries: the Cretaceous/Paleogene and Paleocene/Eocene boundaries respectively. Compared to its boundaries, the remainder of the Paleocene epoch has ...</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="95406176"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406176"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406176; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406176]").text(description); $(".js-view-count[data-work-id=95406176]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406176; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406176']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406176]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406176,"title":"Climatic changes and sea-level fluctuations in the Danian/Selandian boundary interval of Tunesia: an ostracod perspective","internal_url":"https://www.academia.edu/95406176/Climatic_changes_and_sea_level_fluctuations_in_the_Danian_Selandian_boundary_interval_of_Tunesia_an_ostracod_perspective","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406175"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406175/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_"><img alt="Research paper thumbnail of A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406175/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_">A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)</a></div><div class="wp-workCard_item"><span>Studia Universitatis …</span><span>, 2002</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... Title: A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania...</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">... Title: A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania). Authors: Smith, Th × Codrea, V Sasaran, E Van Itterbeeck, Jimmy Bultynck, Pierre Csiki, Z Dica, P Farcas, C Folie, A Garcia, G Godefroit, P. Issue Date: 2002. ...</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="95406175"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406175"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406175; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406175]").text(description); $(".js-view-count[data-work-id=95406175]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406175; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406175']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406175]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406175,"title":"A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)","internal_url":"https://www.academia.edu/95406175/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="95406174"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406174/Palynostratigraphy_of_the_Maastrichtian_dinosaur_and_mammal_sites_of_the_R%C3%A2ul_Mare_and_Barbat_Valleys_Ha%C5%A3eg_Basin_Romania_"><img alt="Research paper thumbnail of Palynostratigraphy of the Maastrichtian dinosaur-and mammal sites of the Râul Mare and Barbat Valleys (Haţeg Basin, Romania)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406174/Palynostratigraphy_of_the_Maastrichtian_dinosaur_and_mammal_sites_of_the_R%C3%A2ul_Mare_and_Barbat_Valleys_Ha%C5%A3eg_Basin_Romania_">Palynostratigraphy of the Maastrichtian dinosaur-and mammal sites of the Râul Mare and Barbat Valleys (Haţeg Basin, Romania)</a></div><div class="wp-workCard_item"><span>Geologica Carpathica</span><span>, 2005</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95406174"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406174"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406174; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406174]").text(description); $(".js-view-count[data-work-id=95406174]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406174; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406174']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406174]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406174,"title":"Palynostratigraphy of the Maastrichtian dinosaur-and mammal sites of the Râul Mare and Barbat Valleys (Haţeg Basin, Romania)","internal_url":"https://www.academia.edu/95406174/Palynostratigraphy_of_the_Maastrichtian_dinosaur_and_mammal_sites_of_the_R%C3%A2ul_Mare_and_Barbat_Valleys_Ha%C5%A3eg_Basin_Romania_","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="95406162"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95406162/A_New_Model_for_the_Evolution_of_Oceanic_Transform_Faults_Based_on_3D_Broadband_Seismic_Observations_From_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_in_the_Eastern_Gulf_of_Guinea"><img alt="Research paper thumbnail of A New Model for the Evolution of Oceanic Transform Faults Based on 3D Broadband Seismic Observations From São Tomé and Príncipe in the Eastern Gulf of Guinea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/95406162/A_New_Model_for_the_Evolution_of_Oceanic_Transform_Faults_Based_on_3D_Broadband_Seismic_Observations_From_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_in_the_Eastern_Gulf_of_Guinea">A New Model for the Evolution of Oceanic Transform Faults Based on 3D Broadband Seismic Observations From São Tomé and Príncipe in the Eastern Gulf of Guinea</a></div><div class="wp-workCard_item"><span>Geochemistry, Geophysics, Geosystems</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="95406162"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95406162"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95406162; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95406162]").text(description); $(".js-view-count[data-work-id=95406162]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95406162; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95406162']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=95406162]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95406162,"title":"A New Model for the Evolution of Oceanic Transform Faults Based on 3D Broadband Seismic Observations From São Tomé and Príncipe in the Eastern Gulf of Guinea","internal_url":"https://www.academia.edu/95406162/A_New_Model_for_the_Evolution_of_Oceanic_Transform_Faults_Based_on_3D_Broadband_Seismic_Observations_From_S%C3%A3o_Tom%C3%A9_and_Pr%C3%ADncipe_in_the_Eastern_Gulf_of_Guinea","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="17390882"><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/17390882/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_"><img alt="Research paper thumbnail of A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)" class="work-thumbnail" src="https://attachments.academia-assets.com/39482307/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/17390882/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_">A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ubbcluj.academia.edu/EmanoilSasaran">Emanoil Sasaran</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/JimmyVanItterbeeck">Jimmy Van Itterbeeck</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://ubbcluj.academia.edu/VladACodrea">Vlad A. Codrea</a></span></div><div class="wp-workCard_item"><span>Studia Universitatis …</span><span>, 2002</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Three exceptional fossiliferous marl pockets yielding respectively micro-vertebrate, ornithopod 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">Three exceptional fossiliferous marl pockets yielding respectively micro-vertebrate, ornithopod and sauropod concentrated remains have been discovered in the new Maastrichtian Nălaţ-Vad locality (Haţeg Basin, Romania). The facies assemblage indicates a fluvial palaeoenvironment with sandy channel infills and silty and clayey floodplain deposits containing well-developed calcretes. Large megaloolithid-type dinosaur eggs have been found in association with these calcretic palaeosols. In the ornithopod pocket the disconnected bones are abundant and apparently belong to a single specimen referred to as Iguanodontia indet. The most remarkable collected micro-remains are teeth and jaws of multituberculate mammals representing the richest concentration of mammal remains from the Late Cretaceous of Europe.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b20d2a27cd2dd99d62ab2c316634e1f7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39482307,"asset_id":17390882,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39482307/download_file?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="17390882"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="17390882"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 17390882; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=17390882]").text(description); $(".js-view-count[data-work-id=17390882]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 17390882; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='17390882']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "b20d2a27cd2dd99d62ab2c316634e1f7" } } $('.js-work-strip[data-work-id=17390882]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":17390882,"title":"A new exceptional vertebrate site from the Late Cretaceous of the Hateg Basin (Romania)","internal_url":"https://www.academia.edu/17390882/A_new_exceptional_vertebrate_site_from_the_Late_Cretaceous_of_the_Hateg_Basin_Romania_","owner_id":164345,"coauthors_can_edit":true,"owner":{"id":164345,"first_name":"Emanoil","middle_initials":null,"last_name":"Sasaran","page_name":"EmanoilSasaran","domain_name":"ubbcluj","created_at":"2010-04-07T04:24:44.927-07:00","display_name":"Emanoil Sasaran","url":"https://ubbcluj.academia.edu/EmanoilSasaran"},"attachments":[{"id":39482307,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/39482307/thumbnails/1.jpg","file_name":"A_new_exceptional_vertebrate_site_from_t20151027-13450-9zntul.pdf","download_url":"https://www.academia.edu/attachments/39482307/download_file","bulk_download_file_name":"A_new_exceptional_vertebrate_site_from_t.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/39482307/A_new_exceptional_vertebrate_site_from_t20151027-13450-9zntul-libre.pdf?1446014172=\u0026response-content-disposition=attachment%3B+filename%3DA_new_exceptional_vertebrate_site_from_t.pdf\u0026Expires=1740873910\u0026Signature=W8NUBX469UMJT8DddoNax6sUSBmFNRLLb6Y9OfknQTj-FQ0u6Uj4eKk6ZjZFATWoEM1Nffji9qjoV5knw7fWZoHV-ivnN2ZnnKvIBBwDM7BNTs0nUc5cx9uPzisJBUvA52ybtVz2h3CcJrAFead6fFHo63N1zvx5CT010n3fRn6A3IUQZ-~Whhuq2JFCzrw1n6nM1pEz9UerfI6l8YL3Rk1bZBFja7GEmN~1Zh~L6eEJwr99HF7nR9iZmPNK5qIQB2n~vN3Z7DKWN0F6xYfThUW~mfbE4n16AtkNgVYfpBJyNZElXu1UIcQkh7JV9mqqCzftwekiuouyb84W76dYMQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856260"><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/3856260/Oldest_Plesiadapiform_Mammalia_Proprimates_from_Asia_and_its_palaeobiogeographical_implications_for_faunal_interchange_with_North_America"><img alt="Research paper thumbnail of Oldest Plesiadapiform (Mammalia, Proprimates) from Asia and its palaeobiogeographical implications for faunal interchange with North America" class="work-thumbnail" src="https://attachments.academia-assets.com/50114322/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/3856260/Oldest_Plesiadapiform_Mammalia_Proprimates_from_Asia_and_its_palaeobiogeographical_implications_for_faunal_interchange_with_North_America">Oldest Plesiadapiform (Mammalia, Proprimates) from Asia and its palaeobiogeographical implications for faunal interchange with North America</a></div><div class="wp-workCard_item"><span>Comptes Rendus Palevol</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Carpolestid plesiadapiforms are well known in several lineages from the North American Palaeocene...</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">Carpolestid plesiadapiforms are well known in several lineages from the North American Palaeocene, but they are absent from Europe and known, until now, by only two taxa from the Early Eocene of Asia. Here we describe a new genus of Carpolestinae from the Late Palaeocene locality of Subeng in Inner Mongolia (China). In its morphological characteristics,</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f956c0854d88cd09c0f53406c40cd522" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114322,"asset_id":3856260,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114322/download_file?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="3856260"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856260"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856260; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856260]").text(description); $(".js-view-count[data-work-id=3856260]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856260; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856260']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "f956c0854d88cd09c0f53406c40cd522" } } $('.js-work-strip[data-work-id=3856260]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856260,"title":"Oldest Plesiadapiform (Mammalia, Proprimates) from Asia and its palaeobiogeographical implications for faunal interchange with North America","internal_url":"https://www.academia.edu/3856260/Oldest_Plesiadapiform_Mammalia_Proprimates_from_Asia_and_its_palaeobiogeographical_implications_for_faunal_interchange_with_North_America","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114322,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114322/thumbnails/1.jpg","file_name":"Oldest_Plesiadapiform_Mammalia_Proprima20161104-26169-k7esk9.pdf","download_url":"https://www.academia.edu/attachments/50114322/download_file","bulk_download_file_name":"Oldest_Plesiadapiform_Mammalia_Proprimat.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114322/Oldest_Plesiadapiform_Mammalia_Proprima20161104-26169-k7esk9-libre.pdf?1478319534=\u0026response-content-disposition=attachment%3B+filename%3DOldest_Plesiadapiform_Mammalia_Proprimat.pdf\u0026Expires=1740873910\u0026Signature=KAe1L~C8tvBfLUaqsxcgbc6q1sc0m-Z9l15aXA2x7yZH29ypgD0OmOW5zm7ZRSJGXUrrOV9hX33uFU2agIJmAR7AhUm2FarYyfpHv0y~sxrKJFntOIg9tmgka3yJqRsJpXml5HH1gbfBFvR9TnHqWSgVq5pRmgq-xzZr3zMJ-rXXW5EvnS0hRjMiHdkPhTP3XrYgwsGfMvHsC-FSkGjNmNmwP3S6-EZ5yCH8hjlasekd2XxXSnRnC5x8cmFjdmONfjfdGB9C33QE7QDTzI~jnL4Nkd7OvJ~gKP-KdfKIUsR~j2okUO2RtB4wsUUvq56CnzQErm1nWI6oiKmJiutGBw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856259"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/3856259/Taphonomy_and_Age_Profile_of_a_Latest_Cretaceous_Dinosaur_Bone_Bed_in_Far_Eastern_Russia"><img alt="Research paper thumbnail of Taphonomy and Age Profile of a Latest Cretaceous Dinosaur Bone Bed in Far Eastern Russia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/3856259/Taphonomy_and_Age_Profile_of_a_Latest_Cretaceous_Dinosaur_Bone_Bed_in_Far_Eastern_Russia">Taphonomy and Age Profile of a Latest Cretaceous Dinosaur Bone Bed in Far Eastern Russia</a></div><div class="wp-workCard_item"><span>Palaios</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A large dinosaur bone bed has been investigated in the Udurchukan Formation (?late Maastrichtian)...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A large dinosaur bone bed has been investigated in the Udurchukan Formation (?late Maastrichtian) at Blagoveschensk, Far Eastern Russia. The observed mixture of unstratified fine and coarse sediments in the bone bed is typical for sediment-gravity-flow deposits. It is ...</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="3856259"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856259"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856259; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856259]").text(description); $(".js-view-count[data-work-id=3856259]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856259; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856259']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=3856259]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856259,"title":"Taphonomy and Age Profile of a Latest Cretaceous Dinosaur Bone Bed in Far Eastern Russia","internal_url":"https://www.academia.edu/3856259/Taphonomy_and_Age_Profile_of_a_Latest_Cretaceous_Dinosaur_Bone_Bed_in_Far_Eastern_Russia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="3856258"><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/3856258/Woodland_in_a_fluvio_lacustrine_environment_on_the_dry_Mongolian_Plateau_during_the_late_Paleocene_Evidence_from_the_mammal_bearing_Subeng_section_Inner_Mongolia_P_R_China"><img alt="Research paper thumbnail of Woodland in a fluvio-lacustrine environment on the dry Mongolian Plateau during the late Paleocene: Evidence from the mammal bearing Subeng section (Inner Mongolia, P.R. China" class="work-thumbnail" src="https://attachments.academia-assets.com/50114318/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/3856258/Woodland_in_a_fluvio_lacustrine_environment_on_the_dry_Mongolian_Plateau_during_the_late_Paleocene_Evidence_from_the_mammal_bearing_Subeng_section_Inner_Mongolia_P_R_China">Woodland in a fluvio-lacustrine environment on the dry Mongolian Plateau during the late Paleocene: Evidence from the mammal bearing Subeng section (Inner Mongolia, P.R. China</a></div><div class="wp-workCard_item"><span>Palaeogeography Palaeoclimatology Palaeoecology</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the understanding of the global faunal turnover during the Paleocene–Eocene transition, an imp...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the understanding of the global faunal turnover during the Paleocene–Eocene transition, an important role has been attributed to the Asian continent, although the Asian fossil record for this period is still incomplete. Here we present a multidisciplinary study of the Subeng section (Inner Mongolia, P.R. China), integrating sedimentological, stratigraphical and diverse palaeontological data, in order to reconstruct the palaeoenvironment and to enhance the understanding of the late Paleocene communities that once thrived on the Mongolian Plateau. The Subeng section starts with the Maastrichtian Iren Dabasu Formation directly covered by the late Paleocene Nomogen Formation. This Nomogen Formation is composed of typical lacustrine deposits at the base, covered by fluvio-lacustrine deposits at the top. Both types of deposits provided rich ostracod and charophyte assemblages, closest to those of the Naran Member, Naran Bulak Formation of Mongolia. Palynomorphs from the lake sediments suggest a local flora at Subeng more wooded and closed than reported from elsewhere in this region. The fluvio-lacustrine deposits of the Nomogen Formation have yielded a vertebrate fauna especially rich in mammals. The mammal fauna from Subeng is close to that from Bayan Ulan and typical for the Gashatan Asian Land Mammal Age. The presence of reworked pedogenic carbonate nodules and mud aggregates suggests an at least seasonally dry regional climate. Combined sedimentological and palaeontological data suggest the late Paleocene Nomogen Formation at Subeng was an isolated woodland in a fluvio-lacustrine environment, representing a locally humid environment on the semi-arid Mongolian Plateau. The mammal fauna reflects these differences and shows a number of relatives to mammals from the more humid northeastern Chinese biotic province as well as some North American immigrants.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a2da55ca3039f61c23dd87a38ad10f14" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114318,"asset_id":3856258,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114318/download_file?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="3856258"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856258"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856258; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856258]").text(description); $(".js-view-count[data-work-id=3856258]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856258; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856258']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "a2da55ca3039f61c23dd87a38ad10f14" } } $('.js-work-strip[data-work-id=3856258]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856258,"title":"Woodland in a fluvio-lacustrine environment on the dry Mongolian Plateau during the late Paleocene: Evidence from the mammal bearing Subeng section (Inner Mongolia, P.R. China","internal_url":"https://www.academia.edu/3856258/Woodland_in_a_fluvio_lacustrine_environment_on_the_dry_Mongolian_Plateau_during_the_late_Paleocene_Evidence_from_the_mammal_bearing_Subeng_section_Inner_Mongolia_P_R_China","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114318,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114318/thumbnails/1.jpg","file_name":"Woodland_in_a_fluvio-lacustrine_environm20161104-26169-wew6g0.pdf","download_url":"https://www.academia.edu/attachments/50114318/download_file","bulk_download_file_name":"Woodland_in_a_fluvio_lacustrine_environm.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114318/Woodland_in_a_fluvio-lacustrine_environm20161104-26169-wew6g0-libre.pdf?1478319542=\u0026response-content-disposition=attachment%3B+filename%3DWoodland_in_a_fluvio_lacustrine_environm.pdf\u0026Expires=1740780277\u0026Signature=XPGrJjT7W~WV4qAppMfWAczqjKARyCG22NxU3RRPUkAHK-5zBYi4IOuS7hYE9iLr94gxW9hnHd9Sgj~aIIM6I5KI1T0d0bXsbaXNKwqQnYQLWddeUDU9GNFFFcXpZyH8GTOGlmthAVsVC5aBU-V3Rz9wbm6sRPXTeKSE~yt1w~bCFHf6fGZOQ66wjyldB9TxMAtQ~5HyB3aXDxRVMNUbOLEUhJDZhYRMMUyksNBs41JSQrAlz0WF~lC1kdKQArWyZNptHU0eYN5rrKKL1DVLa2RFTV4FqOuQWbmc-TMryTt7drPGGe7CU7OCygD0ODGRWuDLPfBUZJaAoplumkeLiQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856257"><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/3856257/The_age_of_the_dinosaur_bearing_Cretaceous_sediments_at_Dashuiguo_Inner_Mongolia_P_R_China_based_on_charophytes_ostracods_and_palynomorphs"><img alt="Research paper thumbnail of The age of the dinosaur-bearing Cretaceous sediments at Dashuiguo, Inner Mongolia, P.R. China based on charophytes, ostracods and palynomorphs" class="work-thumbnail" src="https://attachments.academia-assets.com/50114320/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/3856257/The_age_of_the_dinosaur_bearing_Cretaceous_sediments_at_Dashuiguo_Inner_Mongolia_P_R_China_based_on_charophytes_ostracods_and_palynomorphs">The age of the dinosaur-bearing Cretaceous sediments at Dashuiguo, Inner Mongolia, P.R. China based on charophytes, ostracods and palynomorphs</a></div><div class="wp-workCard_item"><span>Cretaceous Research</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Dashuiguo Formation has yielded numerous fossils of Probactrosaurus, a dinosaur with both igu...</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 Dashuiguo Formation has yielded numerous fossils of Probactrosaurus, a dinosaur with both iguanodontid and hadrosaurid characteristics. Based on the evolutionary position of Probactrosaurus, the dinosaur-bearing sediments have been considered to be Aptian–Albian, but new micropalaeontological data (charophytes, ostracods and palynomorphs) indicate that they may be as old as Barremian. The three charophyte species recovered are indicative of a Barremian–Aptian age. A rich fauna of non-marine Ostracoda (13 species in nine genera) includes two species described as new, Cypridea pseudomodica sp. nov. and C. dashuiguoensis sp. nov., while the remaining eleven species have been described previously from Lower Cretaceous sediments of the Gobi Basin and adjacent areas in China. Based on the ostracod assemblage, the Dashuiguo Formation can be correlated with the Dzun Bayn suite of the Gobi Basin and can therefore be regarded as Barremian–Albian in age. The palynomorph assemblage is very similar to that described from the nearby Tebch site with an estimated Barremian–Early Aptian age and is radiometrically calibrated on the basis of an overlying basalt layer.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8c88e1fd8d5960bf81f4aeae5e969187" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114320,"asset_id":3856257,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114320/download_file?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="3856257"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856257"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856257; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856257]").text(description); $(".js-view-count[data-work-id=3856257]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856257; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856257']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "8c88e1fd8d5960bf81f4aeae5e969187" } } $('.js-work-strip[data-work-id=3856257]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856257,"title":"The age of the dinosaur-bearing Cretaceous sediments at Dashuiguo, Inner Mongolia, P.R. China based on charophytes, ostracods and palynomorphs","internal_url":"https://www.academia.edu/3856257/The_age_of_the_dinosaur_bearing_Cretaceous_sediments_at_Dashuiguo_Inner_Mongolia_P_R_China_based_on_charophytes_ostracods_and_palynomorphs","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114320,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114320/thumbnails/1.jpg","file_name":"j.cretres.2004.02.00120161104-26173-1r97nb.pdf","download_url":"https://www.academia.edu/attachments/50114320/download_file","bulk_download_file_name":"The_age_of_the_dinosaur_bearing_Cretaceo.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114320/j.cretres.2004.02.00120161104-26173-1r97nb-libre.pdf?1478319540=\u0026response-content-disposition=attachment%3B+filename%3DThe_age_of_the_dinosaur_bearing_Cretaceo.pdf\u0026Expires=1740873910\u0026Signature=OA0vdl5EMNBZw8KGLorOg3gVTWEbq2KzUtwOgoT8YMQGeE2WjrX0aDQPcIvsq1MUcf12U1wwrXGU5LtSVvH4UGIOgSx8-Bu9~SsLwnVPZgip8~uBb~Zv9e1084BBIr~kLh5bOWkObD7rt0jm3oOb92dpcyFw7iygx7GmEnz6MX6ANV7wjnpzl0j1nDhCeM-pHKkJ-MAOW-VaTRLont2-ZkXvIyR-pEkh9v8opFj5weDCZuJGgeNpC~lkIK-X0~rNIBLcBYminb-hBVcJSyKFRMkoLD~AI1nbwI0JJwgN5boMHYrZv4PT-~h55FZq6fzTOPlEmeE0lqZZ88vbvIvvDQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856256"><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/3856256/Sedimentology_of_the_Upper_Cretaceous_mammal_and_dinosaur_bearing_sites_along_the_R%C3%A2ul_Mare_and_Barbat_rivers_Ha_t_eg_Basin_Romania"><img alt="Research paper thumbnail of Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Barbat rivers, Ha t ̧ eg Basin, Romania" class="work-thumbnail" src="https://attachments.academia-assets.com/50114316/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/3856256/Sedimentology_of_the_Upper_Cretaceous_mammal_and_dinosaur_bearing_sites_along_the_R%C3%A2ul_Mare_and_Barbat_rivers_Ha_t_eg_Basin_Romania">Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Barbat rivers, Ha t ̧ eg Basin, Romania</a></div><div class="wp-workCard_item"><span>Cretaceous Research</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Mammal and dinosaur localities in the Haeg Basin belonging to the Upper Cretaceous Sânpetru and D...</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">Mammal and dinosaur localities in the Haeg Basin belonging to the Upper Cretaceous Sânpetru and Densuş-Ciula formations have been known since the beginning of the last century. Recently, two new exposures with a comparable fauna have been discovered in the Râul Mare valley. The sediments at these new sites, Toteşti-baraj and Năla-Vad, have been compared with the sediments at the previously known Pui site. At all three sites the deposits reflect a fluvial environment with coarse-grained channel deposits channelized in fine-grained floodplain deposits with calcrete palaeosols. However, the nature of the calcrete palaeosols is different at the three sites. At Toteşti-baraj and Năla-Vad, hydromorphic calcic vertisols have been observed, and locally these grade into groundwater calcretes. At Pui, the calcretes are associated with redbed deposits. Considering the similar palaeogeographical situation and age of the deposits at the three sites, the difference in soil type should not be interpreted as a climatic difference but rather as a difference in the height of the palaeogroundwater table. The soils at Pui are indicative of a general semi-arid climate. Those at Toteşti-baraj and Năla-Vad do not directly reflect the climate, but rather the high seasonal groundwater table. Differences in palaeohydrology between the sites are reflected in the fossil content with humidity-loving species only occurring at the Râul Mare sites.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a6cd1f01ef4efb40f412b9f9d090427b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114316,"asset_id":3856256,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114316/download_file?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="3856256"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856256"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856256; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856256]").text(description); $(".js-view-count[data-work-id=3856256]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856256; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856256']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "a6cd1f01ef4efb40f412b9f9d090427b" } } $('.js-work-strip[data-work-id=3856256]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856256,"title":"Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Barbat rivers, Ha t ̧ eg Basin, Romania","internal_url":"https://www.academia.edu/3856256/Sedimentology_of_the_Upper_Cretaceous_mammal_and_dinosaur_bearing_sites_along_the_R%C3%A2ul_Mare_and_Barbat_rivers_Ha_t_eg_Basin_Romania","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114316,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114316/thumbnails/1.jpg","file_name":"Itterbeeck-KRes-2004.pdf","download_url":"https://www.academia.edu/attachments/50114316/download_file","bulk_download_file_name":"Sedimentology_of_the_Upper_Cretaceous_ma.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114316/Itterbeeck-KRes-2004-libre.pdf?1478319548=\u0026response-content-disposition=attachment%3B+filename%3DSedimentology_of_the_Upper_Cretaceous_ma.pdf\u0026Expires=1740873910\u0026Signature=ZmTol9gZRGXA6id~skik2T9blWcheIcK5NcRlcjQx2gYuxajP2r9AOnPmtnUXoiaFnXdLqPzSt3eiM4CxovTnktjn5PpfJVe5oJtfc5wm2-kqTQ8nzUV-4R-MSsZ89ouut5SBlWZPV73gbhGVYqUrefPv6esxKHLPwJz~c9Z1WhFiksErt2iLsKC73UmM8cZkoE5Y58aPFRQIGzCk07y47I4c3T1Umj97qYoM1PrYwMSsidbFp6Q1Jhm5PckVqio9g9oth7oikd7~YBjJ7j8OqrEywN8kl1l1m5WmXGEMEJOgi9b3S~ZBSIxTm~IXcaK2hf2fDt~oWFrdrSuxZXDSg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856255"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/3856255/Stratigraphy_sedimentology_and_palaeoecology_of_the_dinosaur_bearing_Kundur_section_Zeya_Bureya_Basin_Amur_Region_Far_Eastern_Russia"><img alt="Research paper thumbnail of Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/3856255/Stratigraphy_sedimentology_and_palaeoecology_of_the_dinosaur_bearing_Kundur_section_Zeya_Bureya_Basin_Amur_Region_Far_Eastern_Russia">Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia</a></div><div class="wp-workCard_item"><span>Geological Magazine</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">... In North America, the same floristic changes as those observed at the end of the Asian W. spi...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... In North America, the same floristic changes as those observed at the end of the Asian W. spinataA. subtilis palynozone coincide with the K/P boundary (Braman &amp;amp;amp;amp; Sweet, 1999; Nichols, 1990; Nichols, 2002; Nichols &amp;amp;amp;amp; Sweet, 1993; Sweet, Braman &amp;amp;amp;amp; Lerbekmo, 1999; Tschudy ...</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="3856255"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856255"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856255; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856255]").text(description); $(".js-view-count[data-work-id=3856255]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856255; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856255']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=3856255]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856255,"title":"Stratigraphy, sedimentology and palaeoecology of the dinosaur-bearing Kundur section (Zeya-Bureya Basin, Amur Region, Far Eastern Russia","internal_url":"https://www.academia.edu/3856255/Stratigraphy_sedimentology_and_palaeoecology_of_the_dinosaur_bearing_Kundur_section_Zeya_Bureya_Basin_Amur_Region_Far_Eastern_Russia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[]}, 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="3856254"><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/3856254/Stratigraphy_and_palaeoenvironment_of_the_dinosaur_bearing_Upper_Cretaceous_Iren_Dabasu_Formation_Inner_Mongolia_Peoples_Republic_of_China"><img alt="Research paper thumbnail of Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China" class="work-thumbnail" src="https://attachments.academia-assets.com/50114324/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/3856254/Stratigraphy_and_palaeoenvironment_of_the_dinosaur_bearing_Upper_Cretaceous_Iren_Dabasu_Formation_Inner_Mongolia_Peoples_Republic_of_China">Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China</a></div><div class="wp-workCard_item"><span>Cretaceous Research</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">New field observations and sedimentological analyses of the dinosaur-bearing Upper Cretaceous Ire...</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">New field observations and sedimentological analyses of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation in the Iren Nor region of Inner Mongolia (People's Republic of China) have led to a better understanding of its palaeoenvironment. The fluvial deposits represent a braided river that, due to the large amount of fines, does not fit the classical model for braided rivers. The study area is divided into two parts: in the northern part, sediments of the main channel belt of the ancient braided river system are exposed along a dry river valley on the northern edge of the Iren Nor salt lake, while in the southern part, comprising all other studied exposures, different facies of the ancient floodplain are represented, including minor channels, temporary ponds, and palaeosols. The difference between the northern and southern parts is also reflected in the fossil content; only the southern exposures have yielded dinosaur remains. The ancient braided river had a broad, vegetated floodplain populated by a diverse dinosaur fauna. Four species of charophytes are described and illustrated from the Iren Nor site, together with eight species of ostracods, one of which (Cypridea irennorensis sp. nov.) is new. Contrary to the vertebrate data, both groups of microfossils indicate a latest Cretaceous age (Campanian–Maastrichtian) for the Iren Dabasu Formation, and suggest a possible correlation with the Nemegt Formation, which would allow the age estimation to be refined to latest Campanian–Early Maastrichtian.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a3a3f3939fd02ef7355ad703dabf2765" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50114324,"asset_id":3856254,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50114324/download_file?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="3856254"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856254"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856254; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856254]").text(description); $(".js-view-count[data-work-id=3856254]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856254; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856254']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "a3a3f3939fd02ef7355ad703dabf2765" } } $('.js-work-strip[data-work-id=3856254]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856254,"title":"Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China","internal_url":"https://www.academia.edu/3856254/Stratigraphy_and_palaeoenvironment_of_the_dinosaur_bearing_Upper_Cretaceous_Iren_Dabasu_Formation_Inner_Mongolia_Peoples_Republic_of_China","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":50114324,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/50114324/thumbnails/1.jpg","file_name":"j.cretres.2005.03.00420161104-26167-sxh407.pdf","download_url":"https://www.academia.edu/attachments/50114324/download_file","bulk_download_file_name":"Stratigraphy_and_palaeoenvironment_of_th.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/50114324/j.cretres.2005.03.00420161104-26167-sxh407-libre.pdf?1478319540=\u0026response-content-disposition=attachment%3B+filename%3DStratigraphy_and_palaeoenvironment_of_th.pdf\u0026Expires=1740873910\u0026Signature=E7jGrjieeKZMF4ppnUzJE1RZ0FJLJippxU5zOBQp~ft-4n~P54oqWNjhBbMPh4-cqXvtfLR2dQ1pWAjmJNAxeSfZGLnUpXBzAlZWytA7-BLp0BPSdKM7TayPd5KhC6Meu~Q7iagFR-INOVARnpglpMl-xUXDnJppKqfjXTjJp4PbS4lxWdwZfvbMlmOhCDDfmd78307iEWEVdtriiiSllZeasWuX9hfSzJTU6jR5tHWxgC0Uur9-853a9ovF0SYWhz~WPMtgE80neHk1jYE7fDOmHKz-wTsqWNLiqtQxTfnfiuuy0WpiRicYJJfcVCQuZu7oElXEe3PaHvN6opi8MQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="3856253"><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/3856253/The_lambeosaurine_dinosaur_Amurosaurus_riabinini_from_the_Maastrichtian_of_Far_Eastern_Russia"><img alt="Research paper thumbnail of The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia" class="work-thumbnail" src="https://attachments.academia-assets.com/31498382/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/3856253/The_lambeosaurine_dinosaur_Amurosaurus_riabinini_from_the_Maastrichtian_of_Far_Eastern_Russia">The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Itterbeeck, J. 2004. The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Itterbeeck, J. 2004. The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia. Acta Palaeontologica Polonica 49 (4): 585-618.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6e0ad6f8775c90e2dfe38bfedffa2614" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":31498382,"asset_id":3856253,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/31498382/download_file?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="3856253"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3856253"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3856253; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3856253]").text(description); $(".js-view-count[data-work-id=3856253]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3856253; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3856253']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "6e0ad6f8775c90e2dfe38bfedffa2614" } } $('.js-work-strip[data-work-id=3856253]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":3856253,"title":"The lambeosaurine dinosaur Amurosaurus riabinini, from the Maastrichtian of Far Eastern Russia","internal_url":"https://www.academia.edu/3856253/The_lambeosaurine_dinosaur_Amurosaurus_riabinini_from_the_Maastrichtian_of_Far_Eastern_Russia","owner_id":4746200,"coauthors_can_edit":true,"owner":{"id":4746200,"first_name":"Jimmy","middle_initials":null,"last_name":"Van Itterbeeck","page_name":"JimmyVanItterbeeck","domain_name":"independent","created_at":"2013-07-04T12:06:58.541-07:00","display_name":"Jimmy Van Itterbeeck","url":"https://independent.academia.edu/JimmyVanItterbeeck"},"attachments":[{"id":31498382,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/31498382/thumbnails/1.jpg","file_name":"2004_godefroit_amurosaurus.pdf","download_url":"https://www.academia.edu/attachments/31498382/download_file","bulk_download_file_name":"The_lambeosaurine_dinosaur_Amurosaurus_r.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/31498382/2004_godefroit_amurosaurus-libre.pdf?1392348708=\u0026response-content-disposition=attachment%3B+filename%3DThe_lambeosaurine_dinosaur_Amurosaurus_r.pdf\u0026Expires=1740840026\u0026Signature=VIbuNl0LTRUDepXfur004y3Nr~bsrnk5b5UUBdnNww58Hzn3wrz-AuVJ8OY~uvCUEspXPmVHFutbTsfUr7LJezrVH0kV9Qew3TZlMKQE7q-7jVd1IqXaxF0QG9NYwRh8YJG9zL89w~6Dr4a8HKBJeTe6H3Y9qet3Zc6GjQQmXdonsfrzoFlCJLBBmlypsuL8pJa3RKmAEU7qi3lYUHcsJ3xsURORu6x~kKHpevAHjkw6dQNOZMWm42fsgC0aywzvRgedm8gjbd8oMmKNf13gAMosonCStaOg~9wi60VfnPUyVimSx7L9TS9hej7PLHj8aU9wf6IJuZ2LOcyIoNAaMQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/google_contacts-0dfb882d836b94dbcb4a2d123d6933fc9533eda5be911641f20b4eb428429600.js"], function() { // from javascript_helper.rb $('.js-google-connect-button').click(function(e) { e.preventDefault(); GoogleContacts.authorize_and_show_contacts(); Aedu.Dismissibles.recordClickthrough("WowProfileImportContactsPrompt"); }); $('.js-update-biography-button').click(function(e) { e.preventDefault(); Aedu.Dismissibles.recordClickthrough("UpdateUserBiographyPrompt"); $.ajax({ url: $r.api_v0_profiles_update_about_path({ subdomain_param: 'api', about: "", }), type: 'PUT', success: function(response) { location.reload(); } }); }); $('.js-work-creator-button').click(function (e) { e.preventDefault(); window.location = $r.upload_funnel_document_path({ source: encodeURIComponent(""), }); }); $('.js-video-upload-button').click(function (e) { e.preventDefault(); window.location = $r.upload_funnel_video_path({ source: encodeURIComponent(""), }); }); $('.js-do-this-later-button').click(function() { $(this).closest('.js-profile-nag-panel').remove(); Aedu.Dismissibles.recordDismissal("WowProfileImportContactsPrompt"); }); $('.js-update-biography-do-this-later-button').click(function(){ $(this).closest('.js-profile-nag-panel').remove(); Aedu.Dismissibles.recordDismissal("UpdateUserBiographyPrompt"); }); $('.wow-profile-mentions-upsell--close').click(function(){ $('.wow-profile-mentions-upsell--panel').hide(); Aedu.Dismissibles.recordDismissal("WowProfileMentionsUpsell"); }); $('.wow-profile-mentions-upsell--button').click(function(){ Aedu.Dismissibles.recordClickthrough("WowProfileMentionsUpsell"); }); new WowProfile.SocialRedesignUserWorks({ initialWorksOffset: 20, allWorksOffset: 20, maxSections: 1 }) }); </script> </div></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile_edit-5ea339ee107c863779f560dd7275595239fed73f1a13d279d2b599a28c0ecd33.js","https://a.academia-assets.com/assets/add_coauthor-22174b608f9cb871d03443cafa7feac496fb50d7df2d66a53f5ee3c04ba67f53.js","https://a.academia-assets.com/assets/tab-dcac0130902f0cc2d8cb403714dd47454f11fc6fb0e99ae6a0827b06613abc20.js","https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js"], function() { // from javascript_helper.rb window.ae = window.ae || {}; window.ae.WowProfile = window.ae.WowProfile || {}; if(Aedu.User.current && Aedu.User.current.id === $viewedUser.id) { window.ae.WowProfile.current_user_edit = {}; new WowProfileEdit.EditUploadView({ el: '.js-edit-upload-button-wrapper', model: window.$current_user, }); new AddCoauthor.AddCoauthorsController(); } var userInfoView = new WowProfile.SocialRedesignUserInfo({ recaptcha_key: "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB" }); WowProfile.router = new WowProfile.Router({ userInfoView: userInfoView }); Backbone.history.start({ pushState: true, root: "/" + $viewedUser.page_name }); new WowProfile.UserWorksNav() }); </script> </div> <div class="bootstrap login"><div class="modal fade login-modal" id="login-modal"><div class="login-modal-dialog modal-dialog"><div class="modal-content"><div class="modal-header"><button class="close close" data-dismiss="modal" type="button"><span aria-hidden="true">×</span><span class="sr-only">Close</span></button><h4 class="modal-title text-center"><strong>Log In</strong></h4></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><button class="btn btn-fb btn-lg btn-block btn-v-center-content" id="login-facebook-oauth-button"><svg style="float: left; width: 19px; line-height: 1em; margin-right: .3em;" aria-hidden="true" focusable="false" data-prefix="fab" data-icon="facebook-square" class="svg-inline--fa fa-facebook-square fa-w-14" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 448 512"><path fill="currentColor" d="M400 32H48A48 48 0 0 0 0 80v352a48 48 0 0 0 48 48h137.25V327.69h-63V256h63v-54.64c0-62.15 37-96.48 93.67-96.48 27.14 0 55.52 4.84 55.52 4.84v61h-31.27c-30.81 0-40.42 19.12-40.42 38.73V256h68.78l-11 71.69h-57.78V480H400a48 48 0 0 0 48-48V80a48 48 0 0 0-48-48z"></path></svg><small><strong>Log in</strong> with <strong>Facebook</strong></small></button><br /><button class="btn btn-google btn-lg btn-block btn-v-center-content" id="login-google-oauth-button"><svg style="float: left; width: 22px; line-height: 1em; margin-right: .3em;" aria-hidden="true" focusable="false" data-prefix="fab" data-icon="google-plus" class="svg-inline--fa fa-google-plus fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M256,8C119.1,8,8,119.1,8,256S119.1,504,256,504,504,392.9,504,256,392.9,8,256,8ZM185.3,380a124,124,0,0,1,0-248c31.3,0,60.1,11,83,32.3l-33.6,32.6c-13.2-12.9-31.3-19.1-49.4-19.1-42.9,0-77.2,35.5-77.2,78.1S142.3,334,185.3,334c32.6,0,64.9-19.1,70.1-53.3H185.3V238.1H302.2a109.2,109.2,0,0,1,1.9,20.7c0,70.8-47.5,121.2-118.8,121.2ZM415.5,273.8v35.5H380V273.8H344.5V238.3H380V202.8h35.5v35.5h35.2v35.5Z"></path></svg><small><strong>Log in</strong> with <strong>Google</strong></small></button><br /><style type="text/css">.sign-in-with-apple-button { width: 100%; height: 52px; border-radius: 3px; border: 1px solid black; cursor: pointer; } .sign-in-with-apple-button > div { margin: 0 auto; / This centers the Apple-rendered button horizontally }</style><script src="https://appleid.cdn-apple.com/appleauth/static/jsapi/appleid/1/en_US/appleid.auth.js" type="text/javascript"></script><div class="sign-in-with-apple-button" data-border="false" data-color="white" id="appleid-signin"><span   ="Sign Up with Apple" class="u-fs11"></span></div><script>AppleID.auth.init({ clientId: 'edu.academia.applesignon', scope: 'name email', redirectURI: 'https://www.academia.edu/sessions', state: "df2f72480f761b5f43bc9a89bcef9bb9615107dafc83b2efa69cd4649467fa76", });</script><script>// Hacky way of checking if on fast loswp if (window.loswp == null) { (function() { const Google = window?.Aedu?.Auth?.OauthButton?.Login?.Google; const Facebook = window?.Aedu?.Auth?.OauthButton?.Login?.Facebook; if (Google) { new Google({ el: '#login-google-oauth-button', rememberMeCheckboxId: 'remember_me', track: null }); } if (Facebook) { new Facebook({ el: '#login-facebook-oauth-button', rememberMeCheckboxId: 'remember_me', track: null }); } })(); }</script></div></div></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><div class="hr-heading login-hr-heading"><span class="hr-heading-text">or</span></div></div></div></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><form class="js-login-form" action="https://www.academia.edu/sessions" accept-charset="UTF-8" method="post"><input type="hidden" name="authenticity_token" value="G_O6QbEzNFQqksXeR2jszl9oRKFsSP5OXECEjzMgNM0vZ8jJ8s2zsJTO0wwpT2U25N6cFSeUAIXjm1w-WKo3UQ" autocomplete="off" /><div class="form-group"><label class="control-label" for="login-modal-email-input" style="font-size: 14px;">Email</label><input class="form-control" id="login-modal-email-input" name="login" type="email" /></div><div class="form-group"><label class="control-label" for="login-modal-password-input" style="font-size: 14px;">Password</label><input class="form-control" id="login-modal-password-input" name="password" type="password" /></div><input type="hidden" name="post_login_redirect_url" id="post_login_redirect_url" value="https://independent.academia.edu/JimmyVanItterbeeck" autocomplete="off" /><div class="checkbox"><label><input type="checkbox" name="remember_me" id="remember_me" value="1" checked="checked" /><small style="font-size: 12px; margin-top: 2px; display: inline-block;">Remember me on this computer</small></label></div><br><input type="submit" name="commit" value="Log In" class="btn btn-primary btn-block btn-lg js-login-submit" data-disable-with="Log In" /></br></form><script>typeof window?.Aedu?.recaptchaManagedForm === 'function' && window.Aedu.recaptchaManagedForm( document.querySelector('.js-login-form'), document.querySelector('.js-login-submit') );</script><small style="font-size: 12px;"><br />or <a data-target="#login-modal-reset-password-container" data-toggle="collapse" href="javascript:void(0)">reset password</a></small><div class="collapse" id="login-modal-reset-password-container"><br /><div class="well margin-0x"><form class="js-password-reset-form" action="https://www.academia.edu/reset_password" accept-charset="UTF-8" method="post"><input type="hidden" name="authenticity_token" value="3piXQ2tcbpWColx84Ikmxk_qjRn83Omo6nOfBxRoT3bqDOXLKKLpcTz-Sq6Orq8-9FxVrbcAF2NVqEe2f-JM6g" autocomplete="off" /><p>Enter the email address you signed up with and we'll email you a reset link.</p><div class="form-group"><input class="form-control" name="email" type="email" /></div><script src="https://recaptcha.net/recaptcha/api.js" async defer></script> <script> var invisibleRecaptchaSubmit = function () { var closestForm = function (ele) { var curEle = ele.parentNode; while (curEle.nodeName !== 'FORM' && curEle.nodeName !== 'BODY'){ curEle = curEle.parentNode; } return curEle.nodeName === 'FORM' ? curEle : null }; var eles = document.getElementsByClassName('g-recaptcha'); if (eles.length > 0) { var form = closestForm(eles[0]); if (form) { form.submit(); } } }; </script> <input type="submit" data-sitekey="6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj" data-callback="invisibleRecaptchaSubmit" class="g-recaptcha btn btn-primary btn-block" value="Email me a link" value=""/> </form></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/collapse-45805421cf446ca5adf7aaa1935b08a3a8d1d9a6cc5d91a62a2a3a00b20b3e6a.js"], function() { // from javascript_helper.rb $("#login-modal-reset-password-container").on("shown.bs.collapse", function() { $(this).find("input[type=email]").focus(); }); }); </script> </div></div></div><div class="modal-footer"><div class="text-center"><small style="font-size: 12px;">Need an account? <a rel="nofollow" href="https://www.academia.edu/signup">Click here to sign up</a></small></div></div></div></div></div></div><script>// If we are on subdomain or non-bootstrapped page, redirect to login page instead of showing modal (function(){ if (typeof $ === 'undefined') return; var host = window.location.hostname; if ((host === $domain || host === "www."+$domain) && (typeof $().modal === 'function')) { $("#nav_log_in").click(function(e) { // Don't follow the link and open the modal e.preventDefault(); $("#login-modal").on('shown.bs.modal', function() { $(this).find("#login-modal-email-input").focus() }).modal('show'); }); } })()</script> <div class="bootstrap" id="footer"><div class="footer-content clearfix text-center padding-top-7x" style="width:100%;"><ul class="footer-links-secondary footer-links-wide list-inline margin-bottom-1x"><li><a href="https://www.academia.edu/about">About</a></li><li><a href="https://www.academia.edu/press">Press</a></li><li><a href="https://www.academia.edu/documents">Papers</a></li><li><a href="https://www.academia.edu/topics">Topics</a></li><li><a href="https://www.academia.edu/journals">Academia.edu Journals</a></li><li><a rel="nofollow" href="https://www.academia.edu/hiring"><svg style="width: 13px; height: 13px;" aria-hidden="true" focusable="false" data-prefix="fas" data-icon="briefcase" class="svg-inline--fa fa-briefcase fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M320 336c0 8.84-7.16 16-16 16h-96c-8.84 0-16-7.16-16-16v-48H0v144c0 25.6 22.4 48 48 48h416c25.6 0 48-22.4 48-48V288H320v48zm144-208h-80V80c0-25.6-22.4-48-48-48H176c-25.6 0-48 22.4-48 48v48H48c-25.6 0-48 22.4-48 48v80h512v-80c0-25.6-22.4-48-48-48zm-144 0H192V96h128v32z"></path></svg> <strong>We're Hiring!</strong></a></li><li><a rel="nofollow" href="https://support.academia.edu/hc/en-us"><svg style="width: 12px; height: 12px;" aria-hidden="true" focusable="false" data-prefix="fas" data-icon="question-circle" class="svg-inline--fa fa-question-circle fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M504 256c0 136.997-111.043 248-248 248S8 392.997 8 256C8 119.083 119.043 8 256 8s248 111.083 248 248zM262.655 90c-54.497 0-89.255 22.957-116.549 63.758-3.536 5.286-2.353 12.415 2.715 16.258l34.699 26.31c5.205 3.947 12.621 3.008 16.665-2.122 17.864-22.658 30.113-35.797 57.303-35.797 20.429 0 45.698 13.148 45.698 32.958 0 14.976-12.363 22.667-32.534 33.976C247.128 238.528 216 254.941 216 296v4c0 6.627 5.373 12 12 12h56c6.627 0 12-5.373 12-12v-1.333c0-28.462 83.186-29.647 83.186-106.667 0-58.002-60.165-102-116.531-102zM256 338c-25.365 0-46 20.635-46 46 0 25.364 20.635 46 46 46s46-20.636 46-46c0-25.365-20.635-46-46-46z"></path></svg> <strong>Help Center</strong></a></li></ul><ul class="footer-links-tertiary list-inline margin-bottom-1x"><li class="small">Find new research papers in:</li><li class="small"><a href="https://www.academia.edu/Documents/in/Physics">Physics</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Chemistry">Chemistry</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Biology">Biology</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Health_Sciences">Health Sciences</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Ecology">Ecology</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Cognitive_Science">Cognitive Science</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Mathematics">Mathematics</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Computer_Science">Computer Science</a></li></ul></div></div><div class="DesignSystem" id="credit" style="width:100%;"><ul class="u-pl0x footer-links-legal list-inline"><li><a rel="nofollow" href="https://www.academia.edu/terms">Terms</a></li><li><a rel="nofollow" href="https://www.academia.edu/privacy">Privacy</a></li><li><a rel="nofollow" href="https://www.academia.edu/copyright">Copyright</a></li><li>Academia ©2025</li></ul></div><script> //<![CDATA[ window.detect_gmtoffset = true; window.Academia && window.Academia.set_gmtoffset && Academia.set_gmtoffset('/gmtoffset'); //]]> </script> <div id='overlay_background'></div> <div id='bootstrap-modal-container' class='bootstrap'></div> <div id='ds-modal-container' class='bootstrap DesignSystem'></div> <div id='full-screen-modal'></div> </div> </body> </html>