Afficher la notice abrégée

dc.rights.licenseopenen_US
dc.contributor.authorWAELBROECK, Claire
dc.contributor.authorTJIPUTRA, Jerry
dc.contributor.authorGUO, Chuncheng
dc.contributor.authorNISANCIOGLU, Kerim H.
dc.contributor.authorJANSEN, Eystein
dc.contributor.authorVAZQUEZ RIVEIROS, Natalia
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorTOUCANNE, Samuel
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorROSSIGNOL, Linda
dc.contributor.authorDEWILDE, Fabien
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARCHES, Elodie
dc.contributor.authorLEBREIRO, Susana
dc.contributor.authorNAVE, Silvia
dc.date.accessioned2023-09-27T09:01:17Z
dc.date.available2023-09-27T09:01:17Z
dc.date.issued2022-11-15
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/183809
dc.description.abstractEn<p><strong class="journal-contentHeaderColor">Abstract.</strong> We combine consistently dated benthic carbon isotopic records distributed over the entire Atlantic Ocean with numerical simulations performed by a glacial configuration of the Norwegian Earth System Model with active ocean biogeochemistry, in order to interpret the observed <em>Cibicides</em> &delta;<sup>13</sup>C changes at the stadial-interstadial transition corresponding to the end of Heinrich Stadial 4 (HS4) in terms of ocean circulation and remineralization changes. We show that the marked increase in <em>Cibicides</em> &delta;<sup>13</sup>C observed at the end of HS4 between ~2000 and 4200 m in the Atlantic can be explained by changes in nutrient concentrations as simulated by the model in response to the halting of freshwater input in the high latitude glacial North Atlantic. Our model results show that this <em>Cibicides</em> &delta;<sup>13</sup>C signal is associated with changes in the ratio of southern-sourced (SSW) versus northern-sourced (NSW) water masses at the core sites, whereby SSW is replaced by NSW as a consequence of the resumption of deep water formation in the northern North Atlantic and Nordic Seas after the freshwater input is halted. Our results further suggest that the contribution of ocean circulation changes to this signal increases from ~40 % at 2000 m to ~80 % at 4000 m. Below ~4200 m, the model shows little ocean circulation change but an increase in remineralization across the transition marking the end of HS4. The simulated lower remineralization during stadials than interstadials is particularly pronounced in deep subantarctic sites, in agreement with the decrease in the export production of carbon to the deep Southern Ocean during stadials found in previous studies.</p>
dc.language.isoENen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.title.enAtlantic circulation changes across a stadial-interstadial transition
dc.typeArticle de revueen_US
dc.identifier.doi10.5194/cp-2022-83en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalClimate of the Past Discussionsen_US
bordeaux.page1-21en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&amp;rft_val_fmt=info:ofi/fmt:kev:mtx:journal&amp;rft.jtitle=Climate%20of%20the%20Past%20Discussions&amp;rft.date=2022-11-15&amp;rft.spage=1-21&amp;rft.epage=1-21&amp;rft.au=WAELBROECK,%20Claire&amp;TJIPUTRA,%20Jerry&amp;GUO,%20Chuncheng&amp;NISANCIOGLU,%20Kerim%20H.&amp;JANSEN,%20Eystein&amp;rft.genre=article


Fichier(s) constituant ce document

Thumbnail
Thumbnail

Ce document figure dans la(les) collection(s) suivante(s)

Afficher la notice abrégée