Home > News > Tibet > Human & Nature >

Researchers reveal climate change on ancient Qinghai-Tibet Plateau
update:July 08,2020
BEIJING, July 8,2020 -- Chinese researchers have found that the southeastern region of the Qinghai-Tibet Plateau went through great climatic and vegetation changes from desert to forest due to a topography shift 44 million years ago.
The research article, by the Institute of Tibetan Plateau Research under the Chinese Academy of Sciences, was recently published in the journal Earth and Planetary Science Letters.
According to the article, the altitude of the area rose rapidly from 700 to 3,800 meters above sea level due to the northward subduction of the Indian subcontinent, leading to a series of climatic and vegetation changes.
In the expeditions to a basin in the southeast of the plateau, the researchers discovered two different sedimentary strata.
The lower stratum was mainly made of sand and fluvial deposits formed in a dry climate, while the upper one was mainly lacustrine deposits formed in a humid environment, said the article.
According to Ding Lin, corresponding author of the article, the area was once a hot, dry and low-altitude desert with subtropical vegetation.
As the Indian subcontinent subducted northward, the terrain lifted, and the monsoons were able to bring rain to the area, making its climate moister and cooler.
Mountain forests sprung up due to the climate change and the environmental conditions in the area were close to what they are now, Ding said. 
  • View of Yamzbog Yumco Lake in Shannan, SW China’s Tibet
  • Scenery along Yarlung Zangbo River in Shannan, Tibet
  • People visit Longwangtan Park near Potala Palace in Lhasa

E-mail:editor@tibetol.cn |About Us|Contact Us |Site Maps|
Address:3/F, C Tower, RECREO International Centre, 8 Wangjing East Road, Chaoyang District, Beijing 100102, PRC
Copyright by China Intercontinental Communication Co., Ltd All Rights Reserved.