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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSANCHEZ GONI, Maria Fernanda
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEXTIER, Thomas
dc.contributor.authorPOLANCO-MARTÍNEZ, Josué M.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZORZI, Coralie
dc.contributor.authorRODRIGUES, Teresa
dc.contributor.authorBAHR, André
dc.date.accessioned2024-05-22T13:01:45Z
dc.date.available2024-05-22T13:01:45Z
dc.date.issued2023-05-10
dc.identifier.issn2041-1723en_US
dc.identifier.urioai:crossref.org:10.1038/s41467-023-38337-4
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199983
dc.description.abstractEnAbstractThe end of the Middle Pleistocene Transition (MPT, ~ 800-670 thousand years before present, ka) was characterised by the emergence of large glacial ice-sheets associated with anomalously warm North Atlantic sea surface temperatures enhancing moisture production. Still, the direction and intensity of moisture transport across Eurasia towards potential ice-sheets is poorly constrained. To reconstruct late MPT moisture production and dispersal, we combine records of upper ocean temperature and pollen-based Mediterranean forest cover, a tracer of westerlies and precipitation, from a subtropical drill-core collected off South-West Iberia, with records of East Asia summer monsoon (EASM) strength and West Pacific surface temperatures, and model simulations. Here we show that south-western European winter precipitation and EASM strength reached high levels during the Marine Isotope Stage 18 glacial. This anomalous situation was caused by nearly-continuous moisture supply from both oceans and its transport to higher latitudes through the westerlies, likely fuelling the accelerated expansion of northern hemisphere ice-sheets during the late MPT.
dc.language.isoENen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.sourcecrossref
dc.title.enMoist and warm conditions in Eurasia during the last glacial of the Middle Pleistocene Transition
dc.typeArticle de revueen_US
dc.identifier.doi10.1038/s41467-023-38337-4en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalNature Communicationsen_US
bordeaux.volume14en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcedissemin
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Nature%20Communications&rft.date=2023-05-10&rft.volume=14&rft.issue=1&rft.eissn=2041-1723&rft.issn=2041-1723&rft.au=SANCHEZ%20GONI,%20Maria%20Fernanda&EXTIER,%20Thomas&POLANCO-MART%C3%8DNEZ,%20Josu%C3%A9%20M.&ZORZI,%20Coralie&RODRIGUES,%20Teresa&rft.genre=article


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