{"id":7217,"date":"2019-03-02T06:05:09","date_gmt":"2019-03-02T05:05:09","guid":{"rendered":"https:\/\/www.mio.osupytheas.fr\/fr\/archive_page\/vahine-devenir-de-la-fixation-dazote-dans-locean\/"},"modified":"2024-09-19T15:07:28","modified_gmt":"2024-09-19T13:07:28","slug":"vahine-devenir-de-la-fixation-dazote-dans-locean","status":"publish","type":"archive_page","link":"https:\/\/www.mio.osupytheas.fr\/en\/vahine-the-future-of-nitrogen-fixation-in-locean\/","title":{"rendered":"VAHINE &#8211; Devenir de la fixation d&rsquo;azote dans l&rsquo;Oc\u00e9an"},"content":{"rendered":"<div id=\"basic-page-content\" class=\"page-content\">\r\n<div class=\"content\">\r\n<div class=\"container-fluid\">\r\n<div class=\"row\">\r\n<div class=\"container clearfix\">\r\n<div class=\"row\">\r\n<div class=\"col-xs-12\"><\/div>\r\n<\/div>\r\n<\/div>\r\n<div class=\"paragraphs\">\r\n<div class=\"paragraphs-items paragraphs-items-field-paragraphs paragraphs-items-field-paragraphs-full paragraphs-items-full\">\r\n<div class=\"field field-name-field-paragraphs field-type-paragraphs field-label-hidden\">\r\n<div class=\"field-items\">\r\n<div class=\"field-item even\"><section class=\"paragraph-section paragraph-texte-simple paragraph-gris\">\r\n<div class=\"container\">\r\n<div class=\"paragraph-content\">\r\n<p class=\"rtejustify\"><strong>Coordination<\/strong> :\u00a0 <a href=\"mailto:sophie.bonnet@mio.osupytheas.fr\" target=\"_blank\" rel=\"noopener\">Sophie Bonnet<\/a> (Senior scientist IRD)<\/p>\r\n<p class=\"rtejustify\">L&rsquo;objectif du projet VAHINE est d&rsquo;\u00e9tudier le devenir de l&rsquo;azote fix\u00e9 dans le r\u00e9seau trophique planctonique oc\u00e9anique et son impact potentiel sur l\u2019export de carbone. La campagne VAHINE s&rsquo;est d\u00e9roul\u00e9e dans le sud-ouest du Pacifique (Nouvelle-Cal\u00e9donie) en 2013, \u00e0 laquelle ont particip\u00e9 45 scientifiques de France, d&rsquo;Isra\u00ebl, d&rsquo;Allemagne et des \u00c9tats-Unis.<\/p>\r\n<p class=\"rtejustify\">VAHINE is funded by the ANR (ANR Jeune chercheur S. Bonnet), the CNRS INSU-LEFE, the GOPS and the IRD.<\/p>\r\n\r\n<table style=\"width: 800px;\" border=\"0\" cellspacing=\"1\" cellpadding=\"1\" align=\"center\">\r\n<tbody>\r\n<tr>\r\n<td class=\"rtecenter\">\r\n<div class=\"video-background\"><iframe src=\"https:\/\/www.youtube.com\/embed\/r9Abtt8p2Hs\" width=\"560\" height=\"315\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"> <\/iframe><\/div><\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<\/div>\r\n<\/div>\r\n<\/section><\/div>\r\n<div class=\"field-item odd\"><section class=\"paragraph-section paragraph-texte-simple paragraph-bleu\">\r\n<div class=\"container\">\r\n<div class=\"paragraph-content\">\r\n<h4 class=\"rtejustify\"><span style=\"color: #e6e6fa;\">The scientific results of VAHINE are published in 16 articles grouped together in a <a href=\"https:\/\/www.biogeosciences.net\/special_issue193.html\" target=\"_blank\" rel=\"noopener\">Special issue of the international journal Biogeosciences<\/a><\/span><\/h4>\r\n<table border=\"0\" width=\"1000\" cellspacing=\"1\" cellpadding=\"1\" align=\"center\">\r\n<tbody>\r\n<tr>\r\n<td class=\"rtecenter\"><img fetchpriority=\"high\" decoding=\"async\" style=\"width: 519px; height: 733px;\" src=\"\/wp-content\/uploads\/ancien-site\/images\/vahineissue.jpg\" alt=\"\" width=\"519\" height=\"733\" \/><\/td>\r\n<\/tr>\r\n<tr>\r\n<td class=\"rtejustify\">\r\n<h4 class=\"rtejustify\"><span style=\"color: #e6e6fa;\">Biogeochemical and biological response to a diazotroph bloom in a low-nutrient, low-chlorophyll ecosystem: results from the VAHINE mesocosms experiment<\/span><\/h4>\r\n<p class=\"rtejustify\"><strong>Editor(s)<\/strong> : S. Bonnet, D. G. Capone, F. Lacan, and E. Mara\u00f1\u00f3n<\/p>\r\n<p class=\"rtejustify\"><em>Biogeosciences<\/em><\/p>\r\n<p class=\"rtejustify\"><strong>Abstract<\/strong> The goal of this special issue is to present the knowledge regarding the fate of N2 fixation in the oligotrophic ocean based on the large data set acquired during the VAHINE experiment. VAHINE was a multidisciplinary project involving close collaborations between biogeochemists, molecular ecologist, chemists, marine opticians and modellers. In marine ecosystems, biological N2 fixation provides the predominant external source of nitrogen (N; 140 \u00b1 50 Tg N yr-1), contributing more than atmospheric and riverine inputs to the N supply. Yet the fate and magnitude of the newly fixed N, or diazotroph-derived N (hereafter named DDN) in marine ecosystems is poorly understood. Whether the DDN is preferentially and directly exported out of the photic zone, recycled by the microbial loop and\/or transferred into larger organisms remains unclear. During VAHINE, triplicate large volume (\u223c 50 m3) mesocosms were deployed in the tropical south-west Pacific coastal ocean (New Caledonia). A total of 47 stocks, fluxes, enzymatic activities and diversity parameters were measured daily inside and outside the mesocosms by the 40 scientists involved in the project. The special issue details the major experimental and modelling results obtained during the project regarding the evolution of the main standing stocks, fluxes, plankton diversity and activity over the 23-day experiment, the contribution of N2 fixation to export fluxes, the DDN released to dissolved pool and its transfer to the planktonic food web (bacteria, phytoplankton, zooplankton). Finally, a synthesis study attempts to summarize the knowledge and the unresolved questions regarding the fate of DDN in the ocean to synthetize and link the major experimental and modelling results obtained during the project. It reconciles the diverse and complementary methodological approaches used in this study to answer the scientific questions of the VAHINE project.<\/p>\r\n<\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<\/div>\r\n<\/div>\r\n<\/section><\/div>\r\n<div class=\"field-item even\"><section class=\"paragraph-section paragraph-texte-simple paragraph-blanc\">\r\n<div class=\"container\">\r\n<div class=\"paragraph-content\">\r\n<table style=\"width: 1000px;\" border=\"0\" cellspacing=\"1\" cellpadding=\"1\" align=\"center\">\r\n<tbody>\r\n<tr>\r\n<td>\r\n<p class=\"rtecenter\"><img decoding=\"async\" style=\"width: 1231px; height: 807px;\" src=\"\/wp-content\/uploads\/ancien-site\/images\/vahine.png\" alt=\"\" width=\"1231\" height=\"807\" \/><\/p>\r\n<\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<\/div>\r\n<\/div>\r\n<\/section><\/div>\r\n<div class=\"field-item odd\"><section class=\"paragraph-section paragraph-texte-simple paragraph-gris\">\r\n<div class=\"container\">\r\n<div class=\"paragraph-content\">\r\n<p class=\"rtecenter\"><a class=\"colorbox-load\" href=\"\/wp-content\/uploads\/ancien-site\/images\/vahine.jpg\"><img decoding=\"async\" style=\"width: 1100px; height: 619px;\" src=\"\/wp-content\/uploads\/ancien-site\/resize\/images\/vahine-1100x619.jpg\" alt=\"\" width=\"1100\" height=\"619\" \/><\/a><\/p>\r\n\r\n<\/div>\r\n<\/div>\r\n<\/section><\/div>\r\n<\/div>\r\n<\/div>\r\n<\/div>\r\n<\/div>\r\n<\/div>\r\n<\/div>\r\n<\/div>\r\n<\/div>","protected":false},"featured_media":4489,"parent":0,"template":"","class_list":["post-7217","archive_page","type-archive_page","status-publish","has-post-thumbnail","hentry"],"acf":{"id_old":"1904","category_old":"Mers et oc\u00e9ans Changement global"},"_links":{"self":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/archive_page\/7217","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/archive_page"}],"about":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/types\/archive_page"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/media\/4489"}],"wp:attachment":[{"href":"https:\/\/www.mio.osupytheas.fr\/en\/wp-json\/wp\/v2\/media?parent=7217"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}