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作 者:ZHANG Wanyi Steffen MISCHKE ZHANG Chengjun ZHANG Huirong WANG Peng
机构地区:[1]School of Resources and Environmental Sciences,Lanzhou University [2]Institute of Earth and Environmental Science,University of Potsdam [3]Faculty of Earth Sciences,University of Iceland [4]School of Earth Sciences & Key Laboratory of Mineral Resources in Western China(Gansu Province),Lanzhou University
出 处:《Acta Geologica Sinica(English Edition)》2015年第3期1041-1042,共2页地质学报(英文版)
基 金:supported by NSFC(grant no.41173015);the China Scholarship Council(CSC);National Education Ministry Doctoral Foundation(grant no. 20100211110020).
摘 要:The central and northwestern Tibetan Plateau region,also called"Qiangtang Plateau"(30°27'25"-35°39'13"N,83o41'14"-95°10'46"E),is the highest and largest arcticalpine area of the Earth covering approximately 600,000km^2 with altitude ranging from 4600 to 5100 m a.s.l.(Song et al.,2012,Fig.1).The central and northwestern Tibetan Plateau region,also called"Qiangtang Plateau"(30°27'25"-35°39'13"N,83o41'14"-95°10'46"E),is the highest and largest arcticalpine area of the Earth covering approximately 600,000km^2 with altitude ranging from 4600 to 5100 m a.s.l.(Song et al.,2012,Fig.1).
关 键 词:Sub-Recent Sexual Populations of Limnocythere inopinata Recorded for the First Time from>3500 m Altitude on the Tibetan Plateau
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