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

作     者：Juzhi HOU Xianyong CAO Duo WU Mingda WANG Juzhi HOU;Xianyong CAO;Duo WU;Mingda WANG

作者机构：Group of Alpine Paleoecology and Human AdaptationState Key Laboratory of Tibetan Earth SystemResources and EnvironmentInstitute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China MOE Key Laboratory of Western China’s Environmental SystemsCollege of Earth and Environmental SciencesLanzhou UniversityLanzhou 730000China School of Geographical SciencesLiaoning Normal UniversityDalian 116029China 

出 版 物：《Frontiers of Earth Science》 (地球科学前沿（英文版）)

年 卷 期：2023年第17卷第4期

页      面：899-904页

核心收录：

学科分类：07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

主　　题：Tibetan Plateau landscape 

摘      要：*** Tibetan Plateau(TP)is the largest and highest terrain on the Earth,comprising more than 80%of continents higher than 4000 m above sea *** 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 ***,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.