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dc.rights.licenseopenen_US
hal.structure.identifierLaboratoire des Sciences de l'Environnement Marin (LEMAR) [LEMAR]
dc.contributor.authorCIVEL-MAZENS, Matthieu
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCROSTA, Xavier
hal.structure.identifierGNS Science [Lower Hutt]
dc.contributor.authorCORTESE, Giuseppe
hal.structure.identifierÉcole Pratique des Hautes Études [EPHE]
dc.contributor.authorLOWE, Vikki
hal.structure.identifierGeological Survey of Japan [GSJ]
dc.contributor.authorITAKI, Takuya
hal.structure.identifierKochi University
dc.contributor.authorIKEHARA, Minoru
hal.structure.identifierSimon Fraser University = Université Simon Fraser [SFU.ca]
dc.contributor.authorKOHFELD, Karen
dc.date.accessioned2025-03-26T14:14:26Z
dc.date.available2025-03-26T14:14:26Z
dc.date.issued2024-07-09
dc.identifier.issn0012-821Xen_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/205698
dc.description.abstractEnIn the Indian sector of the Southern Ocean, the main Antarctic Circumpolar Current (ACC) transport is associatedwith the subantarctic jet and deviates around several subantarctic islands and volcanic plateaus. This formsregional eddies that are hotspots for productivity, nutrient and CO2 cycling. Though ACC jet migrations related topast climate variations have been reported in previous studies, little is known about their effect on verticalmixing where fronts interact with bathymetry. Here, we investigate past frontal shifts and their impacts on watercolumn structure in the Del Ca˜no Rise, Crozet Archipelago, and Conrad Rise regions over the last 160,000 yearsby reconstructing surface and subsurface temperatures from siliceous microfossils assemblages in four sedimentcores. Our results suggest that the ACC core was displaced equatorward during the last glacial period (70–18kyrs), away from bathymetric features of the Indian sector of the Southern Ocean. This equatorward shiftprobably reduced front/bathymetry interactions and, with it, mixing of the upper layer of the ocean in the lee ofsubantarctic islands and plateaus. We propose that this process participated in the regional isolation of AntarcticSurface Water from deeper water masses. During Marine Isotope Stage (MIS) 5e (132–118 kyrs), an interglacialepisode with a warmer-than-modern climate, the reverse situation is reconstructed, whereby the tightening ofthe ACC fronts against volcanic plateaus probably resulted in enhanced vertical mixing.
dc.description.sponsorshipCarottage Paleoclimatique: Haute résolution et Innovations - ANR-11-EQPX-0009en_US
dc.description.sponsorshipCarottage Paleoclimatique: Haute résolution et Innovations - ANR-11-EQPX-0009en_US
dc.language.isoENen_US
dc.subject.enSouthern ocean
dc.subject.enACC fronts
dc.subject.enMicropaleontology
dc.subject.enTemperature
dc.title.enSubantarctic jet migrations regulate vertical mixing in the Southern Indian
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.epsl.2024.118877en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalEarth and Planetary Science Lettersen_US
bordeaux.page118877en_US
bordeaux.volume642en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04644496
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Earth%20and%20Planetary%20Science%20Letters&rft.date=2024-07-09&rft.volume=642&rft.spage=118877&rft.epage=118877&rft.eissn=0012-821X&rft.issn=0012-821X&rft.au=CIVEL-MAZENS,%20Matthieu&CROSTA,%20Xavier&CORTESE,%20Giuseppe&LOWE,%20Vikki&ITAKI,%20Takuya&rft.genre=article


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