Shut down of the South American summer monsoon during the penultimate glacial
dc.rights.license | open | en_US |
hal.structure.identifier | Institut des Sciences de l'Evolution de Montpellier [UMR ISEM] | |
dc.contributor.author | RODRÍGUEZ-ZORRO, Paula | |
hal.structure.identifier | Institut des Sciences de l'Evolution de Montpellier [UMR ISEM] | |
hal.structure.identifier | Institut de Recherche pour le Développement [IRD] | |
dc.contributor.author | LEDRU, Marie-Pierre | |
hal.structure.identifier | Collège de France - Chaire Evolution du climat et de l'océan | |
dc.contributor.author | BARD, Edouard | |
hal.structure.identifier | Institut des Sciences de l'Evolution de Montpellier [UMR ISEM] | |
dc.contributor.author | AQUINO-ALFONSO, Olga | |
hal.structure.identifier | Universidade Estadual de Campinas = University of Campinas [UNICAMP] | |
dc.contributor.author | CAMEJO, Adriana | |
hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
dc.contributor.author | DANIAU, Anne-Laure
IDREF: 12852538X | |
hal.structure.identifier | Institut des Sciences de l'Evolution de Montpellier [UMR ISEM] | |
dc.contributor.author | FAVIER, Charly | |
hal.structure.identifier | Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE] | |
dc.contributor.author | GARCIA, Marta | |
hal.structure.identifier | Universidade de São Paulo = University of São Paulo [USP] | |
dc.contributor.author | MINELI, Thays | |
hal.structure.identifier | Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE] | |
dc.contributor.author | ROSTEK, Frauke | |
hal.structure.identifier | Universidade Estadual de Campinas = University of Campinas [UNICAMP] | |
dc.contributor.author | RICARDI-BRANCO, Fresia | |
hal.structure.identifier | Universidade de São Paulo = University of São Paulo [USP] | |
dc.contributor.author | SAWAKUCHI, André Oliveira | |
hal.structure.identifier | Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE] | |
dc.contributor.author | SIMON, Quentin | |
hal.structure.identifier | Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE] | |
dc.contributor.author | TACHIKAWA, K. | |
hal.structure.identifier | Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE] | |
dc.contributor.author | THOUVENY, Nicolas | |
dc.date.accessioned | 2024-04-02T13:10:13Z | |
dc.date.available | 2024-04-02T13:10:13Z | |
dc.date.issued | 2020-04-15 | |
dc.identifier.issn | 2045-2322 | en_US |
dc.identifier.uri | https://oskar-bordeaux.fr/handle/20.500.12278/189128 | |
dc.description.abstractEn | We analysed changes in mean annual air temperature (MAAt), vegetation and biomass burning on a long and continuous lake-peat sediment record from the colônia basin, southeastern Brazil, examining the responses of a wet tropical rainforest over the last 180 ka. Stronger southern atmospheric circulation up to the latitude of colônia was found for the penultimate glacial with lower temperatures than during the last glacial, while strengthening of the South American summer monsoon (SASM) circulation started during the last interglacial and progressively enhanced a longer wet summer season from 95 ka until the present. Past MAAT variations and fire history were possibly modulated by eccentricity, although with signatures which differ in average and in amplitude between the last 180 ka. Vegetation responses were driven by the interplay between the SASM and southern circulation linked to Antarctic ice volume, inferred by the presence of a cool mixed evergreen forest from 180 to 45 ka progressively replaced by a rainforest. We report cooler temperatures during the marine isotope stage 3 (MIS 3: 57-29 ka) than during the Last Glacial Maximum (LGM: 23–19 ka). Our findings show that tropical forest dynamics display different patterns than mid-latitude during the last 180 ka. | |
dc.language.iso | EN | en_US |
dc.title.en | Shut down of the South American summer monsoon during the penultimate glacial | |
dc.type | Article de revue | en_US |
dc.identifier.doi | 10.1038/s41598-020-62888-x | en_US |
dc.subject.hal | Planète et Univers [physics]/Sciences de la Terre/Climatologie | en_US |
dc.subject.hal | Sciences de l'environnement/Milieux et Changements globaux | en_US |
bordeaux.journal | Scientific Reports | en_US |
bordeaux.page | 6275 | en_US |
bordeaux.volume | 10 | en_US |
bordeaux.hal.laboratories | EPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805 | 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 | hal | |
hal.identifier | hal-02543791 | |
hal.version | 1 | |
hal.popular | non | en_US |
hal.audience | Internationale | en_US |
hal.export | false | |
workflow.import.source | hal | |
dc.rights.cc | CC BY | en_US |
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