Abrupt cooling and surface uplift at ~3.6 Ma in the Northeastern Tibetan Plateau and changes in dust source region to the Chinese Loess Plateau
Fabiana Richter1, Carmala N Garzione1, Zhisheng An2, Weiguo Liu3, Xiaoke Qiang4, Hong Chang4, Aradhna K Tripati5 and Xiangzhong Li6, (1)University of Rochester, Department of Earth and Environmental Sciences, Rochester, NY, United States, (2)State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China, (3)Chinese Academy of Sciences, State Key Laboratory of Loess and Quaternary Geology, Xi'an, China, (4)IEE Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China, (5)University of California Los Angeles, Department of Earth, Planetary, and Space Sciences, Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, Institute of Geophysics and Planetary Physics, Los Angeles, CA, United States, (6)Yunnan University, Research Center for Earth System Science, Kunming, China