Eocene climate and hydrology of eastern Asia controlled by orbital forcing and Tibetan Plateau uplift
Author:
Funder
National Natural Science Foundation of China
Southwest Petroleum University
Peking University
King Saud University
Publisher
Elsevier BV
Reference78 articles.
1. Step-wise change of Asian interior climate preceding the Eocene–Oligocene Transition (EOT);Abels;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2011
2. Orbital climate variability on the northeastern Tibetan Plateau across the Eocene-Oligocene transition;Ao;Nat. Commun.,2020
3. The middle to late Eocene greenhouse climate modelled using the CESM 1.0. 5;Baatsen;Clim. Past,2020
4. Berger, A., Loutre, M.F., 1994. Astronomical forcing through geologic time. In: de Boer, P.L., Smith, D.G. (Eds.), Orbital Forcing and Cyclic Sequences: IAS Special Publication, 19, pp. 15–24. https://doi.org/10.1002/9781444304039.ch2.
5. Age and driving mechanisms of the Eocene–Oligocene transition from astronomical tuning of a lacustrine record (Rennes Basin, France);Boulila;Clim. Past,2021
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