Wet tropical climate in SE Tibet during the Late Eocene

Abstract Cenozoic climate cooling at the advent of the Eocene-Oligocene transition (EOT), ~33.7 Ma ago, was stamped in the ocean by a series of climatic events albeit the impact of this global climatic transition on terrestrial environments is still fragmentary. Yet archival constraints on Late Eoce...

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Autores principales: Philippe Sorrel, Ines Eymard, Philippe-Herve Leloup, Gweltaz Maheo, Nicolas Olivier, Mary Sterb, Loraine Gourbet, Guocan Wang, Wu Jing, Haijian Lu, Haibing Li, Xu Yadong, Kexin Zhang, Kai Cao, Marie-Luce Chevalier, Anne Replumaz
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Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/03bb2b1eb9014d14926bb7923c217e09
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spelling oai:doaj.org-article:03bb2b1eb9014d14926bb7923c217e092021-12-02T15:05:51ZWet tropical climate in SE Tibet during the Late Eocene10.1038/s41598-017-07766-92045-2322https://doaj.org/article/03bb2b1eb9014d14926bb7923c217e092017-08-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-07766-9https://doaj.org/toc/2045-2322Abstract Cenozoic climate cooling at the advent of the Eocene-Oligocene transition (EOT), ~33.7 Ma ago, was stamped in the ocean by a series of climatic events albeit the impact of this global climatic transition on terrestrial environments is still fragmentary. Yet archival constraints on Late Eocene atmospheric circulation are scarce in (tropical) monsoonal Asia, and the paucity of terrestrial records hampers a meaningful comparison of the long-term climatic trends between oceanic and continental realms. Here we report new sedimentological data from the Jianchuan basin (SE Tibet) arguing for wetter climatic conditions in monsoonal Asia at ~35.5 Ma almost coevally to the aridification recognized northwards in the Xining basin. We show that the occurrence of flash-flood events in semi-arid to sub-humid palustrine-sublacustrine settings preceded the development of coal-bearing deposits in swampy-like environments, thus paving the way to a more humid climate in SE Tibet ahead from the EOT. We suggest that this moisture redistribution possibly reflects more northern and intensified ITCZ-induced tropical rainfall in monsoonal Asia around 35.5 Ma, in accordance with recent sea-surface temperature reconstructions from equatorial oceanic records. Our findings thus highlight an important period of climatic upheaval in terrestrial Asian environments ~2–4 millions years prior to the EOT.Philippe SorrelInes EymardPhilippe-Herve LeloupGweltaz MaheoNicolas OlivierMary SterbLoraine GourbetGuocan WangWu JingHaijian LuHaibing LiXu YadongKexin ZhangKai CaoMarie-Luce ChevalierAnne ReplumazNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-11 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Philippe Sorrel
Ines Eymard
Philippe-Herve Leloup
Gweltaz Maheo
Nicolas Olivier
Mary Sterb
Loraine Gourbet
Guocan Wang
Wu Jing
Haijian Lu
Haibing Li
Xu Yadong
Kexin Zhang
Kai Cao
Marie-Luce Chevalier
Anne Replumaz
Wet tropical climate in SE Tibet during the Late Eocene
description Abstract Cenozoic climate cooling at the advent of the Eocene-Oligocene transition (EOT), ~33.7 Ma ago, was stamped in the ocean by a series of climatic events albeit the impact of this global climatic transition on terrestrial environments is still fragmentary. Yet archival constraints on Late Eocene atmospheric circulation are scarce in (tropical) monsoonal Asia, and the paucity of terrestrial records hampers a meaningful comparison of the long-term climatic trends between oceanic and continental realms. Here we report new sedimentological data from the Jianchuan basin (SE Tibet) arguing for wetter climatic conditions in monsoonal Asia at ~35.5 Ma almost coevally to the aridification recognized northwards in the Xining basin. We show that the occurrence of flash-flood events in semi-arid to sub-humid palustrine-sublacustrine settings preceded the development of coal-bearing deposits in swampy-like environments, thus paving the way to a more humid climate in SE Tibet ahead from the EOT. We suggest that this moisture redistribution possibly reflects more northern and intensified ITCZ-induced tropical rainfall in monsoonal Asia around 35.5 Ma, in accordance with recent sea-surface temperature reconstructions from equatorial oceanic records. Our findings thus highlight an important period of climatic upheaval in terrestrial Asian environments ~2–4 millions years prior to the EOT.
format article
author Philippe Sorrel
Ines Eymard
Philippe-Herve Leloup
Gweltaz Maheo
Nicolas Olivier
Mary Sterb
Loraine Gourbet
Guocan Wang
Wu Jing
Haijian Lu
Haibing Li
Xu Yadong
Kexin Zhang
Kai Cao
Marie-Luce Chevalier
Anne Replumaz
author_facet Philippe Sorrel
Ines Eymard
Philippe-Herve Leloup
Gweltaz Maheo
Nicolas Olivier
Mary Sterb
Loraine Gourbet
Guocan Wang
Wu Jing
Haijian Lu
Haibing Li
Xu Yadong
Kexin Zhang
Kai Cao
Marie-Luce Chevalier
Anne Replumaz
author_sort Philippe Sorrel
title Wet tropical climate in SE Tibet during the Late Eocene
title_short Wet tropical climate in SE Tibet during the Late Eocene
title_full Wet tropical climate in SE Tibet during the Late Eocene
title_fullStr Wet tropical climate in SE Tibet during the Late Eocene
title_full_unstemmed Wet tropical climate in SE Tibet during the Late Eocene
title_sort wet tropical climate in se tibet during the late eocene
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/03bb2b1eb9014d14926bb7923c217e09
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