Holocene climate changes and paleoecology on the Tibetan Plateau:recent advances  

作　　者：Juzhi HOU Xianyong CAO Duo WU Mingda WANG 

机构地区：[1]Group of Alpine Paleoecology and Human Adaptation,State Key Laboratory of Tibetan Earth System,Resources and Environment,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China [2]MOE Key Laboratory of Western China’s Environmental Systems,College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China [3]School of Geographical Sciences,Liaoning Normal University,Dalian 116029,China

出　　处：《Frontiers of Earth Science》2023年第4期899-904,共6页地球科学前沿（英文版）

摘　　要：1Introduction.The Tibetan Plateau(TP)is the largest and highest terrain on the Earth,comprising more than 80%of continents higher than 4000 m above sea level.The extremely high elevation resulted in cold and arid climate,sparse vegetation,limited available water resources,thin oxygen on TP,as well as desolated landscape,which makes it one of the most unfriendly habitable places on the Earth.However,ancient humans lived on TP as early as 200 thousand years ago(Chen et al.,2019;Zhang et al.,2020),and developed ancient civilizations,including the Tibetan Empire,Guge Kingdom in historical periods.

关 键 词：TIBETAN PLATEAU LANDSCAPE 

分 类 号：P467[天文地球—大气科学及气象学]