Moist and warm conditions in Eurasia during the last glacial of the Middle Pleistocene Transition
| dc.rights.license | open | en_US |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | SANCHEZ GONI, Maria Fernanda | |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | EXTIER, Thomas | |
| dc.contributor.author | POLANCO-MARTÍNEZ, Josué M. | |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | ZORZI, Coralie | |
| dc.contributor.author | RODRIGUES, Teresa | |
| dc.contributor.author | BAHR, André | |
| dc.date.accessioned | 2024-05-22T13:01:45Z | |
| dc.date.available | 2024-05-22T13:01:45Z | |
| dc.date.issued | 2023-05-10 | |
| dc.identifier.issn | 2041-1723 | en_US |
| dc.identifier.uri | oai:crossref.org:10.1038/s41467-023-38337-4 | |
| dc.identifier.uri | https://oskar-bordeaux.fr/handle/20.500.12278/199983 | |
| dc.description.abstractEn | AbstractThe 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.iso | EN | en_US |
| dc.rights | Attribution 3.0 United States | * |
| dc.rights.uri | http://creativecommons.org/licenses/by/3.0/us/ | * |
| dc.source | crossref | |
| dc.title.en | Moist and warm conditions in Eurasia during the last glacial of the Middle Pleistocene Transition | |
| dc.type | Article de revue | en_US |
| dc.identifier.doi | 10.1038/s41467-023-38337-4 | en_US |
| dc.subject.hal | Sciences de l'environnement | en_US |
| bordeaux.journal | Nature Communications | en_US |
| bordeaux.volume | 14 | en_US |
| bordeaux.hal.laboratories | EPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805 | en_US |
| bordeaux.issue | 1 | en_US |
| bordeaux.institution | Université de Bordeaux | en_US |
| bordeaux.institution | CNRS | en_US |
| bordeaux.team | PALEO | en_US |
| bordeaux.peerReviewed | oui | en_US |
| bordeaux.inpress | non | en_US |
| bordeaux.import.source | dissemin | |
| hal.popular | non | en_US |
| hal.audience | Internationale | en_US |
| hal.export | false | |
| workflow.import.source | dissemin | |
| dc.rights.cc | CC BY | en_US |
| bordeaux.COinS | ctx_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 |
