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- [1] Pollen record from red clay sequence in the central Loess Plateau between 8.10 and 2.60Ma[J]. MA Yuzhen1, WU Fuli1,3, FANG Xiaomin3,1, LI Jijun1, AN Zhisheng2 & WANG Wei1 1. Key Laboratory of Western China’s Environmental Systems (MOE) and College of Resources and Environment, Lanzhou University, Lanzhou 730000, China;2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710054, China;3. Institute of Tibetan Plateau Research,
- [4] Discovery of C4 species at high altitude in Qinghai-Tibetan Plateau[J]. WANG Luo, LU Houyuan, WU Naigin, CHU Duo, HAN Jiamao, WU Yuhu, WU Haibin & GU Zhaoyan Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Tibet Institute of Plateau Atmospheric and Environmental Sciences, Lhasa 850000, China Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining 810000, China Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, Ch
- [9] History and variability of Asian interior aridity recorded by eolian flux in the Chinese Loess Plateau during the past 7 Ma[J]. 孙有斌 ,安芷生.Science in China(Series D:Earth Sciences). 2002(05)
- [10] Carbon isotopic records in paleosols over the Pliocene in Northern China: Implication on vegetation development and Tibetan uplift[J]. JIANG Wenying, PENG Shuzhen, HAO Qingzhen & LIU Dongsheng (LIU Tungsheng)Institute of Geology and Geophysics, Chinese Academy of Sciences. Beijing 100029. China;Tai’an Teachers College, Tai’an 271000, China.Chinese Science Bulletin. 2002(08)