Central Asian modulation of Northern Hemisphere moisture transfer over the Late Cenozoic

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MetadadosDescriçãoIdioma
Autor(es): dc.contributorMax Planck Inst Chem-
Autor(es): dc.contributorUniversidade Estadual Paulista (UNESP)-
Autor(es): dc.contributorUniv Paris-
Autor(es): dc.contributorAix Marseille Univ-
Autor(es): dc.contributorInst Geol Sci K Satpaeva-
Autor(es): dc.contributorGoethe Univ Frankfurt-
Autor(es): dc.creatorPrud'homme, Charlotte-
Autor(es): dc.creatorScardia, Giancarlo [UNESP]-
Autor(es): dc.creatorVonhof, Hubert-
Autor(es): dc.creatorGuinoiseau, Damien-
Autor(es): dc.creatorNigmatova, Saida-
Autor(es): dc.creatorFiebig, Jens-
Autor(es): dc.creatorGerdes, Axel-
Autor(es): dc.creatorJanssen, Renee-
Autor(es): dc.creatorFitzsimmons, Kathryn E.-
Data de aceite: dc.date.accessioned2022-08-04T21:57:40Z-
Data de disponibilização: dc.date.available2022-08-04T21:57:40Z-
Data de envio: dc.date.issued2022-04-28-
Data de envio: dc.date.issued2022-04-28-
Data de envio: dc.date.issued2021-06-03-
Fonte completa do material: dc.identifierhttp://dx.doi.org/10.1038/s43247-021-00173-z-
Fonte completa do material: dc.identifierhttp://hdl.handle.net/11449/218266-
Fonte: dc.identifier.urihttp://educapes.capes.gov.br/handle/11449/218266-
Descrição: dc.descriptionEarth's climatic evolution over the last 5 million years is primarily understood from the perspective of marine mechanisms, however, the role of terrestrial feedbacks remains largely unexplored. Here we reconstruct the last 5 million years of soil moisture variability in Central Asia using paleomagnetism data and isotope geochemistry of an 80 m-thick sedimentary succession at Charyn Canyon, Kazakhstan. We identify a long-term trend of increasing aridification throughout the period, along with shorter-term variability related to the interaction between mid-latitude westerlies and the Siberian high-pressure system. This record highlights the long-term contribution of mid-latitude Eurasian terrestrial systems to the modulation of moisture transfer into the Northern Hemisphere oceans and back onto land via westerly air flow. The response of Earth-surface dynamics to Plio-Pleistocene climatic change in Central Asia likely generated terrestrial feedbacks affecting ocean and atmospheric circulation. This missing terrestrial link elucidates the significance of land-water feedbacks for long-term global climate. Late Cenozoic variation in Central Asian hydroclimate resulted from the interaction between mid-latitude westerlies and the Siberian high-pressure system and may have driven terrestrial feedbacks, according to analyses of sediments from Charyn Canyon, Kazakhstan.-
Descrição: dc.descriptionMax Planck Research Group-
Descrição: dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)-
Descrição: dc.descriptionWilhelm and Else Heraeus Foundation-
Descrição: dc.descriptionDeutsche Forschungsgemeinschaft-
Descrição: dc.descriptionMax Planck Inst Chem, Res Grp Terr Palaeoclimates, Mainz, Germany-
Descrição: dc.descriptionUniv Estadual Paulista, Inst Geociencias & Ciencias Exatas, Rio Claro, Brazil-
Descrição: dc.descriptionMax Planck Inst Chem, Climate Geochem, Mainz, Germany-
Descrição: dc.descriptionUniv Paris, Inst Phys Globe Paris, Paris, France-
Descrição: dc.descriptionAix Marseille Univ, CNRS, IRD, INRAE,Coll France,CEREGE, Aix En Provence, France-
Descrição: dc.descriptionInst Geol Sci K Satpaeva, Alma Ata, Kazakhstan-
Descrição: dc.descriptionGoethe Univ Frankfurt, Inst Geosci, Frankfurt, Germany-
Descrição: dc.descriptionGoethe Univ Frankfurt, Frankfurt Element & Isotope Res Ctr, Frankfurt, Germany-
Descrição: dc.descriptionUniv Estadual Paulista, Inst Geociencias & Ciencias Exatas, Rio Claro, Brazil-
Descrição: dc.descriptionCNPq: 424365/2016-2-
Descrição: dc.descriptionDeutsche Forschungsgemeinschaft: INST 161/921-1 FUGG-
Formato: dc.format8-
Idioma: dc.languageen-
Publicador: dc.publisherSpringer-
Relação: dc.relationCommunications Earth & Environment-
???dc.source???: dc.sourceWeb of Science-
Título: dc.titleCentral Asian modulation of Northern Hemisphere moisture transfer over the Late Cenozoic-
Tipo de arquivo: dc.typelivro digital-
Aparece nas coleções:Repositório Institucional - Unesp

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