Paleoclimate changes of the last 1000 yr on the eastern Qinghai-Tibetan Plateau recorded by elemental, isotopic, and molecular organic matter proxies in sediment from glacial Lake Ximencuo
School of Remote Sensing, Nanjing University of Information Science and Technology, Nanjing 210044, China; Duke University, Division of Earth and Ocean Sciences, Durham, NC 27708-0227, United States; Department of Earth and Environmental Sciences, The University of Michigan, Ann Arbor, MI, 48109-1005, United States; Key Laboratory of Plateau Lake Ecology and Global Change, Yunnan Normal University, Kunming Chenggong 650500, China; Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou 730000, China; Department of Marine Sciences, The University of Georgia, Athens, GA 30602, United States
Recommended Citation:
Pu Y.,Nace T.,Meyers P.A.,et al. Paleoclimate changes of the last 1000 yr on the eastern Qinghai-Tibetan Plateau recorded by elemental, isotopic, and molecular organic matter proxies in sediment from glacial Lake Ximencuo[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2013-01-01,379-380