“…55–50 million years ago) due to the Indo‐Asian Collision (Royden, Burchfiel, & van der Hilst, 2008). The subsequent mountain uplift and climatic changes have significantly influenced the historical biogeography of TP's lineages (Ding, Ree, Spicer, & Xing, 2020; Favre et al, 2015), and ultimately altered the biota on the TP over time (He, Lin, Li, Yu, & Jiang, 2020). These contexts indicate that the TP is one of the most challenging and evolutionarily unique regions on Earth (Deng, Wu, Zhou, & Su, 2019), and serves as a good model for testing the eco‐evolutionary processes that generate and maintain the diversity patterns (Favre et al, 2015; Yu et al, 2019; Ding et al, 2020).…”