“…The extensive uplift of the Himalayas and subsequent uplift of the Southeastern Tibet and Yunnan Plateau (Figure S2) during the early Miocene to Pliocene (Cao et al, ; Favre et al, ; Harrison, Copeland, Kidd, & Yin, ; Ruddiman, ; Shi et al, ) would have completely divided the Bellamya lineage in the Pearl River basin from that in India and Thailand. Many studies have associated the divergence of organisms, such as in lizards, birds, frogs and fish, with the Miocene uplift of the QTP and simultaneous climate changes (Che et al, ; Guo & Wang, ; Johansson et al, ; Wang, Gan, Li, Chen, & He, ). Furthermore, the divergence between the India lineage and Thailand lineage approximately 13.03 mya (15.02 ~ 11.55 mya), coinciding with the Himalayan and Indo‐Burma Mountains (Figure S2), rapidly uplifted during the early to middle Miocene (Alam, Alam, Curray, Chowdhury, & Gani, ; Khin, Sakai, & Zaw, ; Wang et al, ).…”