Articles | Volume 12, issue 2
Clim. Past, 12, 255–272, 2016
https://doi.org/10.5194/cp-12-255-2016
Clim. Past, 12, 255–272, 2016
https://doi.org/10.5194/cp-12-255-2016

Research article 11 Feb 2016

Research article | 11 Feb 2016

Terrestrial responses of low-latitude Asia to the Eocene–Oligocene climate transition revealed by integrated chronostratigraphy

Y. X. Li et al.

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Cited articles

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Short summary
An integrated litho-, bio-, cyclo-, and magnetostratigraphy constrains the onset of a depositional environmental change from a lacustrine to a deltaic environment in the Maoming Basin, China, at 33.88 Ma. This coincides with the global cooling during the Eocene-Oligocene transition (EOT) at ~ 33.7–33.9 Ma. This change represents terrestrial responses of low-latitude Asia to the EOT. The greatly refined chronology permits detailed examination of the late Paleogene climate change in southeast Asia.