{"id":82,"date":"2025-09-29T16:29:17","date_gmt":"2025-09-29T14:29:17","guid":{"rendered":"https:\/\/geops.geol.u-psud.fr\/pds\/?page_id=82"},"modified":"2025-09-29T16:39:29","modified_gmt":"2025-09-29T14:39:29","slug":"hydrosed","status":"publish","type":"page","link":"https:\/\/geops.geol.u-psud.fr\/pds\/hydrosed\/","title":{"rendered":"HYDROSED"},"content":{"rendered":"<p><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_2 1_2 fusion-flex-column\" style=\"--awb-padding-top:12%;--awb-padding-right:12%;--awb-padding-bottom:12%;--awb-padding-left:12%;--awb-bg-color:var(--awb-color1);--awb-bg-color-hover:var(--awb-color1);--awb-bg-size:cover;--awb-width-large:50%;--awb-margin-top-large:0px;--awb-spacing-right-large:3.84%;--awb-margin-bottom-large:0px;--awb-spacing-left-large:3.072%;--awb-width-medium:50%;--awb-order-medium:0;--awb-spacing-right-medium:3.84%;--awb-spacing-left-medium:3.072%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-title title fusion-title-1 fusion-sep-none fusion-title-text fusion-title-size-two\" style=\"--awb-margin-top-small:10px;--awb-margin-right-small:0px;--awb-margin-bottom-small:10px;--awb-margin-left-small:0px;\"><h2 class=\"fusion-title-heading title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:46;line-height:var(--awb-typography1-line-height);\"><strong>HYDROSED<\/strong><\/h2><\/div><div class=\"fusion-text fusion-text-1\"><p><strong>\u00ab Exploring paleo-hydrology and its impact on sedimentary dynamic processes in the South China Sea \u00bb \/ MD 215<\/strong><\/p>\n<\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_1_2 1_2 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:50%;--awb-margin-top-large:0px;--awb-spacing-right-large:3.84%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:3.84%;--awb-width-medium:50%;--awb-order-medium:0;--awb-spacing-right-medium:3.84%;--awb-spacing-left-medium:3.84%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\" data-scroll-devices=\"small-visibility,medium-visibility,large-visibility\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-image-element \" style=\"--awb-caption-title-font-family:var(--h2_typography-font-family);--awb-caption-title-font-weight:var(--h2_typography-font-weight);--awb-caption-title-font-style:var(--h2_typography-font-style);--awb-caption-title-size:var(--h2_typography-font-size);--awb-caption-title-transform:var(--h2_typography-text-transform);--awb-caption-title-line-height:var(--h2_typography-line-height);--awb-caption-title-letter-spacing:var(--h2_typography-letter-spacing);\"><span class=\" fusion-imageframe imageframe-none imageframe-1 hover-type-none\"><img decoding=\"async\" width=\"604\" height=\"403\" title=\"marion dufresne\" src=\"https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/marion-dufresne.jpg\" alt class=\"img-responsive wp-image-83\" srcset=\"https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/marion-dufresne-200x133.jpg 200w, https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/marion-dufresne-400x267.jpg 400w, https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/marion-dufresne-600x400.jpg 600w, https:\/\/geops.geol.u-psud.fr\/pds\/wp-content\/uploads\/sites\/3\/2025\/09\/marion-dufresne.jpg 604w\" sizes=\"(max-width: 640px) 100vw, 600px\" \/><\/span><\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-2 fusion-flex-container has-pattern-background has-mask-background nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-2 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:20px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-order-medium:0;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-order-small:0;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-text fusion-text-2\"><p><strong>Financement\u00a0: IFREMER<\/strong><\/p>\n<\/div><div class=\"fusion-text fusion-text-3\"><p><strong>Porteur du projet\u00a0:<\/strong> C. Colin (GEOPS)<\/p>\n<p><u>Chefs de mission <\/u>: C. COLIN (GEOPS, France), Z. LIU (Tongji University, China) et A. Tien-Shun LIN (National Central University, Taiwan),<\/p>\n<p><u>Equipe scientifique embarqu\u00e9<\/u>\u00a0: 35 chercheurs et \u00e9tudiants fran\u00e7ais (laboratoires GEOPS, LSCE, IFREMER, LOG), Chinois (Key State Laboratory of Marine Geology, Tongji University) et Taiwanaise (Department of Earth Sciences du National Central University, National Sun Yat-sen University, Institute of Oceanography du National Taiwan University).<\/p>\n<\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"align-self: center;margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:20px;width:100%;\"><div class=\"fusion-separator-border sep-single sep-solid\" style=\"--awb-height:20px;--awb-amount:20px;border-color:var(--awb-color3);border-top-width:2px;\"><\/div><\/div><div class=\"fusion-text fusion-text-4\"><p>La campagne oc\u00e9anographique MD215 HYDROSED \u00e0 bord du navire Marion Dufresne a permis de collecter de longues carottes de s\u00e9diments marins et des \u00e9chantillons d&#8217;eau de mer dans le nord de la mer de Chine du Sud. L\u2019objectif scientifique principal de cette mission est de restituer l\u2019hydrologie pass\u00e9e des masses d\u2019eaux interm\u00e9diaires et profondes ainsi que le climat de la r\u00e9gion sud-est asiatique et d\u2019en estimer l\u2019impact sur la dynamique du transport des s\u00e9diments au fond de l&#8217;oc\u00e9an et des transferts terre \u2013 mer. Les \u00e9chantillons pr\u00e9lev\u00e9s lors de la campagne oc\u00e9anographique HYDROSED vont permettre de :<\/p>\n<ul>\n<li>Mieux contraindre l&#8217;origine et les variations pass\u00e9es des masses d\u2019eaux interm\u00e9diaires et profondes du Nord de la mer de Chine du Sud et des relations existantes avec les changements glacio-eustatiques, l&#8217;\u00e9volution de la circulation thermohaline globale (Great Conveyor Belt) et les modifications climatiques r\u00e9gionales ;<\/li>\n<li>Reconstruire la variabilit\u00e9 pass\u00e9e du climat sud-est asiatique (la mousson Est asiatique et le syst\u00e8me ENSO) \u00e0 tr\u00e8s haute r\u00e9solution temporelle et en \u00e9tablir les potentiels impacts sur la s\u00e9dimentation profonde du Nord de la mer de Chine du Sud\u00a0;<\/li>\n<li>Reconstruire dans le pass\u00e9 la dynamique de transferts des s\u00e9diments depuis les continents (fleuves ta\u00efwanais) au nord de la mer de Chine du Sud avec une approche \u2018\u2019source to sink\u2019\u2019 et en \u00e9tablir les contr\u00f4les climatiques (pal\u00e9o-typhons, pal\u00e9o-moussons et changements du niveau marin) ;<\/li>\n<li>D\u00e9velopper et\/ou am\u00e9liorer des traceurs g\u00e9ochimiques utilis\u00e9s pour les reconstructions pal\u00e9o-oc\u00e9anographiques et am\u00e9liorer notre compr\u00e9hension de la distribution des isotopes du n\u00e9odyme (Nd) et des concentrations \u00e9l\u00e9mentaires en terres rares (REE) dans une mer marginale fortement influenc\u00e9e par d\u2019\u00e9normes d\u00e9charges d&#8217;eau douce et de s\u00e9diments par plusieurs fleuves asiatiques.<\/li>\n<\/ul>\n<\/div><div class=\"fusion-text fusion-text-5\"><p>Lien\u00a0: <a href=\"http:\/\/hydrosed.cearc.fr\/content\/la-campagne-oc%C3%A9anographique\">http:\/\/hydrosed.cearc.fr\/content\/la-campagne-oc\u00e9anographique<\/a><\/p>\n<\/div><\/div><\/div><\/div><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"100-width.php","meta":{"footnotes":""},"class_list":["post-82","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/82","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/comments?post=82"}],"version-history":[{"count":4,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/82\/revisions"}],"predecessor-version":[{"id":96,"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/pages\/82\/revisions\/96"}],"wp:attachment":[{"href":"https:\/\/geops.geol.u-psud.fr\/pds\/wp-json\/wp\/v2\/media?parent=82"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}