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. 2020 Jul 31;3:415. doi: 10.1038/s42003-020-01154-2

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© The Author(s) 2020

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 1 — Palaeotopography was derived from a palaeo-digital elevation model (palaeoDEM, 1° × 1° resolution) developed by Scotese & Wright⁵². Changes in the atmosphere–ocean climate system were compiled from the data of Sun & Wang⁵⁰. Present-day zoogeographical regions were adapted from Kreft & Jetz⁶ and Holt et al.⁵. CA Central Asia, MP Mongolian Plateau, NA North Asia, NC North China, SA South Asia, SC South China, SEA Southeast Asia, TP Tibetan Plateau, WA West Asia.