Global cooling and enhanced Eocene Asian mid-latitude interior aridity

The role Tibetan Plateau uplift played in Asian inland aridification remains unclear due to a paucity of accurately dated records. Here, the authors present a continuous aeolian sequence for the period >51–39 Ma, analysis of which indicates that aridification was driven by global climatic forcing...

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Autores principales:	J. X. Li, L. P. Yue, A. P. Roberts, A. M. Hirt, F. Pan, Lin Guo, Y. Xu, R. G. Xi, Lei Guo, X. K. Qiang, C. C. Gai, Z. X. Jiang, Z. M. Sun, Q. S. Liu
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/6b768260639d40d3893e8dfacebf17b2
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spelling	oai:doaj.org-article:6b768260639d40d3893e8dfacebf17b22021-12-02T17:31:29ZGlobal cooling and enhanced Eocene Asian mid-latitude interior aridity10.1038/s41467-018-05415-x2041-1723https://doaj.org/article/6b768260639d40d3893e8dfacebf17b22018-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-05415-xhttps://doaj.org/toc/2041-1723The role Tibetan Plateau uplift played in Asian inland aridification remains unclear due to a paucity of accurately dated records. Here, the authors present a continuous aeolian sequence for the period >51–39 Ma, analysis of which indicates that aridification was driven by global climatic forcing rather than uplift.J. X. LiL. P. YueA. P. RobertsA. M. HirtF. PanLin GuoY. XuR. G. XiLei GuoX. K. QiangC. C. GaiZ. X. JiangZ. M. SunQ. S. LiuNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q J. X. Li L. P. Yue A. P. Roberts A. M. Hirt F. Pan Lin Guo Y. Xu R. G. Xi Lei Guo X. K. Qiang C. C. Gai Z. X. Jiang Z. M. Sun Q. S. Liu Global cooling and enhanced Eocene Asian mid-latitude interior aridity
description	The role Tibetan Plateau uplift played in Asian inland aridification remains unclear due to a paucity of accurately dated records. Here, the authors present a continuous aeolian sequence for the period >51–39 Ma, analysis of which indicates that aridification was driven by global climatic forcing rather than uplift.
format	article
author	J. X. Li L. P. Yue A. P. Roberts A. M. Hirt F. Pan Lin Guo Y. Xu R. G. Xi Lei Guo X. K. Qiang C. C. Gai Z. X. Jiang Z. M. Sun Q. S. Liu
author_facet	J. X. Li L. P. Yue A. P. Roberts A. M. Hirt F. Pan Lin Guo Y. Xu R. G. Xi Lei Guo X. K. Qiang C. C. Gai Z. X. Jiang Z. M. Sun Q. S. Liu
author_sort	J. X. Li
title	Global cooling and enhanced Eocene Asian mid-latitude interior aridity
title_short	Global cooling and enhanced Eocene Asian mid-latitude interior aridity
title_full	Global cooling and enhanced Eocene Asian mid-latitude interior aridity
title_fullStr	Global cooling and enhanced Eocene Asian mid-latitude interior aridity
title_full_unstemmed	Global cooling and enhanced Eocene Asian mid-latitude interior aridity
title_sort	global cooling and enhanced eocene asian mid-latitude interior aridity
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/6b768260639d40d3893e8dfacebf17b2
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Global cooling and enhanced Eocene Asian mid-latitude interior aridity

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