Holocene high-resolution quantitative summer temperature reconstruction based on subfossil chironomids from the southeast margin of the Qinghai-Tibetan Plateau
We thank X.Y. Xiao, Y.L. Li, X Chen, E.F. Liu, J.J. Wang, and Y. Wang (Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences) for field assistance. This research was supported by the Program of Global Change and Mitigation (2016YFA0600502), the National Natural Science Foundation of China (No. 41572337). We thank Dr Dayou Zhai and the other anonymous reviewer for providing detailed comments on the manuscript.
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China; School of Earth and Environmental Sciences, The University of Queensland, St Lucia, Brisbane, Qld, Australia; College of Resources and Environmental Science, South-Central University for Nationalities, Wuhan, China; Research Centre of Hydrobiology, Jinan University, Guangzhou, China; Geography and Environment, University of Southampton, Southampton, United Kingdom
Recommended Citation:
Zhang E.,Chang J.,Cao Y.,et al. Holocene high-resolution quantitative summer temperature reconstruction based on subfossil chironomids from the southeast margin of the Qinghai-Tibetan Plateau[J]. Quaternary Science Reviews,2017-01-01,165