A 16-ka oxygen-isotope record from Genggahai Lake on the northeastern Qinghai-Tibetan Plateau: Hydroclimatic evolution and changes in atmospheric circulation
We thank Prof. X.P. Yang, Dr. K. Apolinarska and two anonymous reviewers for their constructive comments and suggestions to improve the early version of this paper. We also thank Dr. A.C.G. Henderson and Dr. J. Bloemendal for their valuable comments and language improvements, Prof. H.Z. Pan for identifying mollusc shells, and Ms. P.Y. Zhang for her assistance in isotopic analyses. This research was supported by the National Natural Science Foundation of China (grants 41271219, 41671190) and the National Research Foundation for the Doctoral Program of Higher Education of China (grant 20130211110035).
MOE Key Laboratory of Western China's Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, China; Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, China; Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
Recommended Citation:
Qiang M.,Song L.,Jin Y.,et al. A 16-ka oxygen-isotope record from Genggahai Lake on the northeastern Qinghai-Tibetan Plateau: Hydroclimatic evolution and changes in atmospheric circulation[J]. Quaternary Science Reviews,2017-01-01,162