{"id":36352,"date":"2023-07-21T10:28:37","date_gmt":"2023-07-21T08:28:37","guid":{"rendered":"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/?page_id=36352"},"modified":"2023-09-22T12:20:44","modified_gmt":"2023-09-22T10:20:44","slug":"archives-sedimentaires-et-paleoenvironnements","status":"publish","type":"page","link":"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/en\/archives-sedimentaires-et-paleoenvironnements\/","title":{"rendered":"Sedimentary archives and paleoenvironments"},"content":{"rendered":"<div id=\"pl-36352\"  class=\"panel-layout\" ><div id=\"pg-36352-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-0-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><div id=\"pg-36352-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-1-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h1 class=\"col-xs bottom-xs flexbox image-group-bottom-3-img space-bottom-xs center-xs\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-4511\" style=\"color: #1269b0; font-size: 30px;\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1-300x34.png\" alt=\"\" width=\"150\" height=\"17\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1-300x34.png 300w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1.png 331w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/><br \/>\n<span style=\"color: #1269b0; font-size: 2.2rem; background-color: #e6e9ed;\">Archives s\u00e9dimentaires<\/span><br \/>\n<img loading=\"lazy\" decoding=\"async\" class=\"wp-image-4511\" style=\"color: #1269b0; font-size: 30px;\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1-300x34.png\" alt=\"\" width=\"150\" height=\"17\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1-300x34.png 300w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1.png 331w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/><\/h1>\n<h1 class=\"col-xs bottom-xs flexbox image-group-bottom-3-img space-bottom-xs center-xs\"><span style=\"color: #1269b0; font-size: 2.2rem; background-color: #e6e9ed;\">et pal\u00e9oenvironnements<\/span><\/h1>\n<h1 class=\"col-xs bottom-xs flexbox image-group-bottom-3-img space-bottom-xs center-xs\"><\/h1>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-36352-2\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-2-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><div id=\"pgc-36352-2-1\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-2-1-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-4e6925654b7a-36352\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img \n\tsrc=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2023\/07\/picto_paleo-removebg-preview.png\" width=\"150\" height=\"150\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2023\/07\/picto_paleo-removebg-preview.png 150w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2023\/07\/picto_paleo-removebg-preview-12x12.png 12w\" sizes=\"(max-width: 150px) 100vw, 150px\" alt=\"\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><div id=\"pgc-36352-2-2\"  class=\"panel-grid-cell panel-grid-cell-mobile-last\" ><div id=\"panel-36352-2-2-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"2\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 20px; color: #1269b0; text-align: justify;\"><em>L'\u00e9tude des pal\u00e9oenvironnements et des archives s\u00e9dimentaires permet de pr\u00e9dire les changements climatiques futurs, d'\u00e9valuer les risques environnementaux et de prendre des d\u00e9cisions \u00e9clair\u00e9es pour la gestion des zones c\u00f4ti\u00e8res et la protection de l'environnement marin.<\/em><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-36352-2-3\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><div id=\"pg-36352-3\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-3-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><div id=\"pg-36352-4\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-4-0\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-4-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"3\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h1 class=\"col-xs bottom-xs flexbox image-group-bottom-3-img space-bottom-xs center-xs\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-4511\" style=\"color: #1269b0; font-size: 40px;\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1-300x34.png\" alt=\"\" width=\"220\" height=\"25\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1-300x34.png 300w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/trait-1.png 331w\" sizes=\"auto, (max-width: 220px) 100vw, 220px\" \/><\/h1>\n<h1 class=\"col-xs bottom-xs flexbox image-group-bottom-3-img space-bottom-xs center-xs\"><\/h1>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-36352-5\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-5-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><div id=\"pg-36352-6\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-6-0\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-6-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"4\" ><div class=\"panel-widget-style panel-widget-style-for-36352-6-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">L'\u00e9tude des conditions climatiques pass\u00e9es et des changements climatiques survenus jusqu'\u00e0 aujourd'hui rev\u00eat une importance cruciale pour la <strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">pr\u00e9diction des \u00e9ventuels changements climatiques<\/span><\/strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\"> et des \u00e9v\u00e9nements extr\u00eames qui pourraient menacer les zones c\u00f4ti\u00e8res. En analysant les archives s\u00e9dimentaires et les pal\u00e9oenvironnements, nous sommes en mesure d'explorer les variations climatiques ant\u00e9rieures.<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"panel-36352-6-0-1\" class=\"so-panel widget widget_sow-editor\" data-index=\"5\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"text-align: justify;\"><span style=\"color: #1269b0;\"><span style=\"font-size: 18px;\"><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">La reconstitution des pal\u00e9oclimats et des pal\u00e9oenvironnements n\u00e9cessite une analyse et l<strong>'i<\/strong><\/span><strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">dentification de divers indicateurs<\/span><\/strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">. Parmi ceux-ci, nous examinons les <strong>pollens<\/strong>, qui nous renseignent sur la v\u00e9g\u00e9tation pass\u00e9e et les conditions climatiques associ\u00e9es. Mais \u00e9galement les <\/span><strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">foraminif\u00e8res<\/span><\/strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">, de minuscules organismes marins pr\u00e9sents dans les s\u00e9diments, qui fournissent des informations sur les caract\u00e9ristiques des oc\u00e9ans pass\u00e9s. Finalement nous nous int\u00e9ressons aux <\/span><strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">dinophytes<\/span><\/strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\">, des algues unicellulaires, dont la pr\u00e9sence dans les s\u00e9diments refl\u00e8te l'\u00e9tat des \u00e9cosyst\u00e8mes marins d'autrefois.<\/span><\/span><\/span><\/p>\n<\/div>\n<\/div><\/div><div id=\"panel-36352-6-0-2\" class=\"so-panel widget widget_sow-editor panel-last-child\" data-index=\"6\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">Mis \u00e0 part la richesse que la connaissance intrins\u00e8que nous apporte, ces informations extraites des archives s\u00e9dimentaires nous permettent de mieux <strong>comprendre les changements climatiques<\/strong> pass\u00e9s, d<strong>'\u00e9valuer les risques environnementaux<\/strong> actuels et de <strong>projeter les tendances climatiques<\/strong> \u00e0 venir. Gr\u00e2ce \u00e0 ces approches nous sommes en mesure de prendre des d\u00e9cisions plus \u00e9clair\u00e9es en mati\u00e8re de gestion des zones c\u00f4ti\u00e8res et de protection de l'environnement marin.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-36352-7\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-7-0\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-7-0-0\" class=\"so-panel widget widget_sow-button panel-first-child panel-last-child\" data-index=\"7\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-button so-widget-sow-button-wire-f9a073c29d3c-36352\"\n\t\t\t\n\t\t><div class=\"ow-button-base ow-button-align-center\"\n>\n\t\t\t<a\n\t\t\t\t\thref=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/projets-de-recherche\/\"\n\t\t\t\t\tclass=\"sowb-button ow-icon-placement-left ow-button-hover\" \t>\n\t\t<span>\n\t\t\t\n\t\t\tD\u00e9couvrir les projets\t\t<\/span>\n\t\t\t<\/a>\n\t<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-36352-8\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-8-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><div id=\"pg-36352-9\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-9-0\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-9-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"8\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<div class='white' style='border-radius:0px; 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margin:0px 0%; background-image:url(&quot;https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/12\/Photo-1.png&quot;); background-position:center center; background-size:contain; background-repeat:no-repeat; '>\n<style>.SliderButton4{background:rgba(0, 0, 0, 0) !important;color:rgba(0, 0, 0, 0) !important}.SliderButton4:hover{background:rgba(0, 0, 0, 0)!important;color:rgba(0, 0, 0, 0)!important}<\/style>\n<div class='textContainer'><\/div>\n<div><a href=' '  type='button'   target='_self' class='btn SliderButton4'><\/a><\/div>\n<\/div>\n<\/div>\n<\/div>\n<p><script type='text\/javascript'>\n\tjQuery(document).ready(function() {\n\t\tjQuery('#Slider_38158').owlCarousel({\n\t\t\titems : 1,\n\t\t\tsmartSpeed : 200,\n\t\t\tautoplay : true,\n\t\t\tautoplayTimeout : 10000,\n\t\t\tautoplayHoverPause : true,\n\t\t\tsmartSpeed : 200,\n\t\t\tfluidSpeed : 200,\n\t\t\tautoplaySpeed : 200,\n\t\t\tnavSpeed : 200,\n\t\t\tdotsSpeed : 200,\n\t\t\tdotsEach : 1,\n\t\t\tloop : true,\n\t\t\tnav : true,\n\t\t\tnavText : ['Previous','Next'],\n\t\t\tdots : true,\n\t\t\tresponsiveRefreshRate : 200,\n\t\t\tslideBy : 1,\n\t\t\tmergeFit : true,\n\t\t\tautoHeight : false,\n\t\t\tmouseDrag : true,\n\t\t\ttouchDrag : true\n\t\t});\n\t\tjQuery('#Slider_38158').css('visibility', 'visible');\n\t\tsa_resize_Slider_38158();\n\t\twindow.addEventListener('resize', sa_resize_Slider_38158);\n\t\tfunction sa_resize_Slider_38158() {\n\t\t\tvar min_height = '500';\n\t\t\tvar win_width = jQuery(window).width();\n\t\t\tvar slider_width = jQuery('#Slider_38158').width();\n\t\t\tif (win_width < 480) {\n\t\t\t\tvar slide_width = slider_width \/ 480;\n\t\t\t} else if (win_width < 768) {\n\t\t\t\tvar slide_width = slider_width \/ 768;\n\t\t\t} else if (win_width < 980) {\n\t\t\t\tvar slide_width = slider_width \/ 980;\n\t\t\t} else if (win_width < 1200) {\n\t\t\t\tvar slide_width = slider_width \/ 1200;\n\t\t\t} else if (win_width < 1500) {\n\t\t\t\tvar slide_width = slider_width \/ 1500;\n\t\t\t} else {\n\t\t\t\tvar slide_width = slider_width \/ 1800;\n\t\t\t}\n\t\t\tslide_width = Math.round(slide_width);\n\t\t\tvar slide_height = '500';\n\t\t\tif (min_height == 'aspect43') {\n\t\t\t\tslide_height = (slide_width \/ 4) * 3;\t\t\t\tslide_height = Math.round(slide_height)+'px';\n\t\t\t} else if (min_height == 'aspect169') {\n\t\t\t\tslide_height = (slide_width \/ 16) * 9;\t\t\t\tslide_height = Math.round(slide_height)+'px';\n\t\t\t} else {\n\t\t\t\tslide_height = slide_height;\t\t\t\tslide_height = Math.round(slide_height)+'px';\n\t\t\t}\n\t\t\tjQuery('#Slider_38158 .owl-item .sa_hover_container').css('min-height', slide_height);\n\t\t}\n\t\tvar owl_goto = jQuery('#Slider_38158');\n\t\tjQuery('.Slider_38158_goto1').click(function(event){\n\t\t\towl_goto.trigger('to.owl.carousel', 0);\n\t\t});\n\t\tjQuery('.Slider_38158_goto2').click(function(event){\n\t\t\towl_goto.trigger('to.owl.carousel', 1);\n\t\t});\n\t\tjQuery('.Slider_38158_goto3').click(function(event){\n\t\t\towl_goto.trigger('to.owl.carousel', 2);\n\t\t});\n\t\tjQuery('.Slider_38158_goto4').click(function(event){\n\t\t\towl_goto.trigger('to.owl.carousel', 3);\n\t\t});\n\t\tvar resize_38158 = jQuery('.owl-carousel');\n\t\tresize_38158.on('initialized.owl.carousel', function(e) {\n\t\t\tif (typeof(Event) === 'function') {\n\t\t\t\twindow.dispatchEvent(new Event('resize'));\n\t\t\t} else {\n\t\t\t\tvar evt = window.document.createEvent('UIEvents');\n\t\t\t\tevt.initUIEvent('resize', true, false, window, 0);\n\t\t\t\twindow.dispatchEvent(evt);\n\t\t\t}\n\t\t});\n\t});\n<\/script>\n<\/p>\n<p>&nbsp;<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-36352-10\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-10-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><div id=\"pg-36352-11\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-11-0\"  class=\"panel-grid-cell\" ><div id=\"panel-36352-11-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"9\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<h3><strong><span style=\"color: #1269b0;\">Publications associ\u00e9es<\/span><\/strong><span class=\"WdYUQQ text-decoration-none text-strikethrough-none\" style=\"font-size: 16px; color: #1269b0; text-align: justify;\"><br \/>\n<\/span><\/h3>\n<\/div>\n<\/div><\/div><div id=\"panel-36352-11-0-1\" class=\"so-panel widget widget_sow-editor\" data-index=\"10\" ><div class=\"panel-widget-style panel-widget-style-for-36352-11-0-1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">1. Gorczynska, Aneta &amp; St\u00e9phan, Pierre &amp; Yvan, Pailler &amp; Nicolas, Cl\u00e9ment &amp; Penaud, Aur\u00e9lie &amp;\u00a0<strong>David, Oph\u00e9lie<\/strong>\u00a0&amp; Vidal, Muriel &amp; Le Gall, Bernard. <strong>(2023)<\/strong>. Holocene evolution of coastal dunes in western France: Regional reconstruction from archaeological and historical data. Aeolian Research.\u00a0<a href=\"https:\/\/dx.doi.org\/10.1016\/j.aeolia.2022.100851\">Lire l'article<\/a><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"panel-36352-11-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"11\" ><div class=\"panel-widget-style panel-widget-style-for-36352-11-0-2\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">2.\u00a0<strong>Novico<\/strong>\u00a0<strong>F<\/strong>.,\u00a0<strong>Menier D<\/strong>.,\u00a0<strong>Mathew M<\/strong>., Ramkumar M., Santosh M., Endyana C., Tri Dewi K., Kurniawan I.,\u00a0<strong>Lambert C<\/strong>.,\u00a0<strong>Goubert E<\/strong>., Hendarmawan, <strong>(2022)<\/strong>. Impact of Late Quaternary climatic fluctuations on coastal systems: Evidence from high-resolution geophysical, sedimentological and geochronological data from the Java Island.\u00a0<em>Marine and Petroleum Geology,\u00a0<\/em>105399. DOI : 10.1016\/j.marpetgeo.2021. <a href=\"https:\/\/www.researchgate.net\/publication\/356098732_Impact_of_Late_Quaternary_climatic_fluctuations_on_coastal_systems_Evidence_from_high-resolution_geophysical_sedimentological_and_geochronological_data_from_the_Java_Island\" target=\"_blank\" rel=\"noopener\">Lire l'article<\/a><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"panel-36352-11-0-3\" class=\"so-panel widget widget_sow-editor\" data-index=\"12\" ><div class=\"panel-widget-style panel-widget-style-for-36352-11-0-3\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">3.\u00a0<strong>Lambert C<\/strong>., Penaud A., Poirier C.,\u00a0<strong>Goubert E<\/strong>.,<strong> (2022)<\/strong>. Distribution of modern dinocysts in surface sediments of southern Brittany (NW France) in relation to environmental parameters: Implications for paleoreconstructions.\u00a0<em>Review of Palaeobotany and Palynology, 297,\u00a0<\/em>104578. DOI : 10.1016\/j.revpalbo.2021.104578. <a href=\"https:\/\/doi.org\/10.1016\/j.revpalbo.2021.104578\" target=\"_blank\" rel=\"noopener\">Lire l'article<\/a><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"panel-36352-11-0-4\" class=\"so-panel widget widget_sow-editor\" data-index=\"13\" ><div class=\"panel-widget-style panel-widget-style-for-36352-11-0-4\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">4. Ramkumar, Muthuvairavasamy &amp; K., Kumaraswamy &amp; K., Balasubramani &amp; Nagarajan, Ramasamy &amp; Santosh, M. &amp; Rahaman, s. Abdul &amp; Kumar, Arun &amp; K J, Juni &amp; Fathima, Al &amp; Siddiqui, Numair &amp;\u00a0<strong>Mathew, Manoj &amp; Menier, David<\/strong>\u00a0&amp; Sautter, et al... <strong>(2021)<\/strong>. Neolithic cultural sites and extreme climate related channel avulsion: Evidence from the Vaigai River Basin, southern India. Journal of Archaeological Science: Reports.\u00a0<a href=\"https:\/\/doi.org\/10.1016\/j.jasrep.2021.103204\">Lire l'article<\/a><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"panel-36352-11-0-5\" class=\"so-panel widget widget_sow-editor\" data-index=\"14\" ><div class=\"panel-widget-style panel-widget-style-for-36352-11-0-5\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p style=\"font-size: 18px; color: #1269b0; text-align: justify;\">5. <strong>Lambert C.,\u00a0<\/strong>Penaud A., Vidal M., Klouch K., Gregoire G., Ehrhold A., Eynaud F., Schmidt S., Ragueneau O., Siano R., <strong>(2018)<\/strong>. Human-induced river runoff overlapping natural climate variability over the last 150 years : palynological evidences (Bay of Brest, NW France).(<em>Global and Planetary Change<\/em>). 160, 109-122. DOI : 10.1016\/j.gloplacha.2017.11.004 <a href=\"https:\/\/doi.org\/10.1016\/j.gloplacha.2017.11.004\" target=\"_blank\" rel=\"noopener\">Lire l'article<\/a><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"panel-36352-11-0-6\" class=\"so-panel widget widget_sow-button panel-last-child\" data-index=\"15\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-button so-widget-sow-button-wire-f9a073c29d3c-36352\"\n\t\t\t\n\t\t><div class=\"ow-button-base ow-button-align-center\"\n>\n\t\t\t<a\n\t\t\t\t\thref=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/publications-scientifiques\/\"\n\t\t\t\t\tclass=\"sowb-button ow-icon-placement-left ow-button-hover\" \t>\n\t\t<span>\n\t\t\t\n\t\t\tD\u00e9couvrir les publications\t\t<\/span>\n\t\t\t<\/a>\n\t<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-36352-12\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-36352-12-0\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Sedimentary archives and paleoenvironments<\/p>","protected":false},"author":9,"featured_media":36377,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-36352","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - 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