Orbital climate variability on the northeastern Tibetan Plateau across the Eocene–Oligocene transition

Orbital climate variability on the northeastern Tibetan Plateau across the Eocene–Oligocene transition

Marine records indicate a greenhouse to icehouse climate transition at ~34 million years ago, but how the climate changed within continental interiors at this time is less well known. Here, the authors show an orbital climate response shift with aridification on the northeastern Tibetan Plateau duri...

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Bibliographic Details
Main Authors: Hong Ao, Guillaume Dupont-Nivet, Eelco J. Rohling, Peng Zhang, Jean-Baptiste Ladant, Andrew P. Roberts, Alexis Licht, Qingsong Liu, Zhonghui Liu, Mark J. Dekkers, Helen K. Coxall, Zhangdong Jin, Chunju Huang, Guoqiao Xiao, Christopher J. Poulsen, Natasha Barbolini, Niels Meijer, Qiang Sun, Xiaoke Qiang, Jiao Yao, Zhisheng An
Format: Article
Language:English
Published: Nature Publishing Group 2020-10-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-020-18824-8

Internet

https://doi.org/10.1038/s41467-020-18824-8

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