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dc.contributor.authorFontela, Marcoses_ES
dc.contributor.authorGarcía-Ibáñez, Maribel I.es_ES
dc.contributor.authorHansell, Dennis A.es_ES
dc.contributor.authorMercier, Herlées_ES
dc.contributor.authorPérez, Fiz F.es_ES
dc.date.accessioned2016-06-06T09:14:45Z-
dc.date.available2016-06-06T09:14:45Z-
dc.date.issued2016-
dc.identifier.citationScientific Reports 6: 26931 (2016)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/133014-
dc.description9 páginas, 4 figuras, 1 tabla.-- This work is licensed under a Creative Commons Attribution 4.0 International Licensees_ES
dc.description.abstractThe quantitative role of the Atlantic Meridional Overturning Circulation (AMOC) in dissolved organic carbon (DOC) export is evaluated by combining DOC measurements with observed water mass transports. In the eastern subpolar North Atlantic, both upper and lower limbs of the AMOC transport high-DOC waters. Deep water formation that connects the two limbs of the AMOC results in a high downward export of non-refractory DOC (197 Tg-C·yr−1). Subsequent remineralization in the lower limb of the AMOC, between subpolar and subtropical latitudes, consumes 72% of the DOC exported by the whole Atlantic Ocean. The contribution of DOC to the carbon sequestration in the North Atlantic Ocean (62 Tg-C·yr−1) is considerable and represents almost a third of the atmospheric CO2 uptake in the regiones_ES
dc.description.sponsorshipFor this work M. Fontela was funded by the Spanish Ministry of Economy and Competitiveness (BES-2014-070449) through the BOCATS project (CTM2013-41048-P) supported by the Spanish Government and co-funded by the Fondo Europeo de Desarrollo Regional 2007–2012 (FEDER); and this article is going to be part of her PhD that is attached to the framework of the doctoral program “Marine Science, Technology and Management” (DO*MAR) of the University of Vigo. M.I. García-Ibáñez and F.F. Pérez were supported by the BOCATS project (CTM2013-41048-P) co-funded by the Spanish Government and the Fondo Europeo de Desarrollo Regional (FEDER). D.A. Hansell was supported by US National Science Foundation award OCE-1436748. H. Mercier was supported by the CNRS and the ATLANTOS project (GA 633211)es_ES
dc.language.isoenges_ES
dc.publisherNature Publishing Groupes_ES
dc.relationinfo:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2013-41048-Pes_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/633211-
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.titleDissolved Organic Carbon in the North Atlantic Meridional Overturning Circulationes_ES
dc.typeartículoes_ES
dc.identifier.doi10.1038/srep26931-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1038/srep26931es_ES
dc.identifier.e-issn2045-2322-
dc.rights.licensehttp://creativecommons.org/licenses/by/4.0/es_ES
dc.contributor.funderMinisterio de Economía y Competitividad (España)es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
dc.identifier.pmid27240625-
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.openairetypeartículo-
item.languageiso639-1en-
item.grantfulltextopen-
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