青藏高原高寒区生物地理学研究进展

宋艾,杨久成,丁文娜,刘佳

The advances in biogeography research on Tibetan Plateau alpine bioregion

Ai SONG,Jiucheng YANG,Wenna DING,Jia LIU

图5 青藏高寒区生物分化时间、新生代全球气候变化和高原隆升关系（新生代气候变化根据文献［102］、［103］修改） 注：青藏高原隆升示意图从左到右依次为古近纪早期高原南部安第斯型山脉，古近纪中晚期高原中部东西向峡谷模型，新近纪早期高原中部和南部隆升，新近纪晚期高原北部生长［81-82，84-85，87，94，96-97］

Fig.5 The relationship between the divergence times of species of the Tibetan Plateau and its surrounding areas， Cenozoic climate change and Tibetan Plateau tectonic history （The Cenozoic climate change is Revised from References ［102］， ［103］） Note：The tectonic history of the Tibetan Plateau shows the Andean-type mountains in the southern plateau in the early Paleogene， the east-west canyon model in the middle plateau until the late Paleogene， the uplift of the central and southern plateau in the early Neogene， and the growth of the northern plateau during the late Neogene［81-82，84-85，87，94，96-97］