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作 者:Fahu CHEN Huan XIA Zhenxiu JIA Dongju ZHANG
机构地区:[1]Group of Alpine Paleoecology and Human Adaptation(ALPHA),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China [2]State Key Laboratory of Tibetan Plateau Earth System,Resources and Environment(TPESRE),Beijing 100101,China [3]MOE Key Laboratory of Western China’s Environmental System,Lanzhou University,Lanzhou 730000,China
出 处:《Science China Earth Sciences》2022年第4期769-772,共4页中国科学(地球科学英文版)
基 金:supported by the National Natural Science Foundation of China(Grant No.41988101)。
摘 要:As a result of rapid uplift since the late Cenozoic, the Tibetan Plateau eventually developed an enormous area(3.08 million km^(2)) and became the highest elevation plateau on Earth. The cold and hypoxic environments of the Tibetan Plateau,combined with the strong solar radiation receipt and lack of biological resources, present a major challenge to the occupation and expansion of humans.
关 键 词:Tibetan Plateau INTERIOR
分 类 号:Q981[天文地球—古生物学与地层学]
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