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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZORZI, Coralie
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDESPRAT, Stephanie
IDREF: 088638960
dc.contributor.authorCLÉMENT, Charlotte
dc.contributor.authorTHIRUMALAI, Kaustubh
dc.contributor.authorOLIVIERA, Dulce
dc.contributor.authorANUPAMA, Krishnamurthy
dc.contributor.authorPRASAD, Srinivasan
dc.contributor.authorMARTINEZ, Philippe
IDREF: 154067628
dc.date.accessioned2023-05-17T07:28:36Z
dc.date.available2023-05-17T07:28:36Z
dc.date.issued2022-08-09
dc.identifier.issn1944-8007en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/182175
dc.description.abstractEnDuring the last glacial period, the tropical hydrological cycle exhibited large variability across orbital and millennial timescales. However, the response of the Indian summer monsoon (ISM), its related impact on terrestrial ecosystems, and associated forcing mechanisms remain controversial. Here we present a marine record of pollen-inferred vegetation changes suggesting that eastern India shifted from woody-savanna mosaics during Marine Isotopic Stage 3 to grasslands during the Last Glacial Maximum resulting from large-scale drying. Our data shows that ISM maximum is in phase with obliquity and precession maxima suggesting a dominant role of the Indian Ocean interhemispheric temperature gradient on glacial ISM variability. Persistent and abrupt dryland expansions of varying magnitude suggest rapid-scale onset of aridity during Heinrich Stadial events and during the Toba eruption. We propose that the amplitude of ISM drought events are initiated by high latitude and volcanic forcings, although modulated by precession.
dc.language.isoENen_US
dc.rightsAttribution-NoDerivs 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nd/3.0/us/*
dc.title.enWhen Eastern India Oscillated Between Desert Versus Savannah-Dominated Vegetation
dc.typeArticle de revueen_US
dc.identifier.doi10.1029/2022GL099417en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalGeophysical Research Lettersen_US
bordeaux.volume49en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue16en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.exportfalse
dc.rights.ccCC BY-NCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geophysical%20Research%20Letters&rft.date=2022-08-09&rft.volume=49&rft.issue=16&rft.eissn=1944-8007&rft.issn=1944-8007&rft.au=ZORZI,%20Coralie&DESPRAT,%20Stephanie&CL%C3%89MENT,%20Charlotte&THIRUMALAI,%20Kaustubh&OLIVIERA,%20Dulce&rft.genre=article


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