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

Abstract The first major build-up of Antarctic glaciation occurred in two consecutive stages across the Eocene–Oligocene transition (EOT): the EOT-1 cooling event at ~34.1–33.9 Ma and the Oi-1 glaciation event at ~33.8–33.6 Ma. Detailed orbital-scale terrestrial environmental responses to these even...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Ao, Hong, Dupont-Nivet, Guillaume, Rohling, Eelco J., Zhang, Peng, Ladant, Jean-Baptiste, Roberts, Andrew P., Licht, Alexis, Liu, Qingsong, Liu, Zhonghui, Dekkers, Mark J., Coxall, Helen K., Jin, Zhangdong, Huang, Chunju, Xiao, Guoqiao, Poulsen, Christopher J., Barbolini, Natasha, Meijer, Niels, Sun, Qiang, Qiang, Xiaoke, Yao, Jiao, An, Zhisheng
Other Authors: National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2020
Subjects:
General Physics and Astronomy
General Biochemistry, Genetics and Molecular Biology
General Chemistry
Antarctic
Antarc*
Online Access:http://dx.doi.org/10.1038/s41467-020-18824-8
https://www.nature.com/articles/s41467-020-18824-8.pdf
https://www.nature.com/articles/s41467-020-18824-8
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Summary:Abstract The first major build-up of Antarctic glaciation occurred in two consecutive stages across the Eocene–Oligocene transition (EOT): the EOT-1 cooling event at ~34.1–33.9 Ma and the Oi-1 glaciation event at ~33.8–33.6 Ma. Detailed orbital-scale terrestrial environmental responses to these events remain poorly known. Here we present magnetic and geochemical climate records from the northeastern Tibetan Plateau margin that are dated precisely from ~35.5 to 31 Ma by combined magneto- and astro-chronology. These records suggest a hydroclimate transition at ~33.7 Ma from eccentricity dominated cycles to oscillations paced by a combination of eccentricity, obliquity, and precession, and confirm that major Asian aridification and cooling occurred at Oi-1. We conclude that this terrestrial orbital response transition coincided with a similar transition in the marine benthic δ 18 O record for global ice volume and deep-sea temperature variations. The dramatic reorganization of the Asian climate system coincident with Oi-1 was, thus, a response to coeval atmospheric CO 2 decline and continental-scale Antarctic glaciation.

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