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. 2022 Jul 1;13:3787. doi: 10.1038/s41467-022-31512-z

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© The Author(s) 2022

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. 3 — a The red line represents a log plot of lineage accumulation of spiny plants in eudicots in Eurasia during the Cenozoic. The blue curve represents a log plot of lineage accumulation of mammalian herbivore species in central Asia during the Cenozoic. Being log plots, the linear rise is indicative of exponential diversification. Source data are provided as Source Data files. b South (left) to north (right) transects of mean elevation changes across Himalaya-Tibet at different phases in its geological evolution (modified from Su, et al.⁵¹).