Palynological and paleobotanical data from more than 60 cores and sections of the Qinghai-Xizang Plateau show that the Late Cenozoic vegetation changed markedly due to the strong uplift of the Himalayas and the global climatic changes.
英
美
- 從青藏高原目前已知的60余個(gè)剖面和鉆孔揭示的大量古植物資料來(lái)看,由于喜馬拉雅山的強烈隆升、地質(zhì)事件及全球氣候變化,青藏高原晚新生代植被發(fā)生顯著(zhù)的變化。