This research was financially supported by the NSFC (Nos. 41172165, 41302138, and 41440020), “the Fundamental Research Funds for the Central Universities” (Nos. XDJK2013A012 and XDJK2014C010), “Karst Dynamics Laboratory, MLR and GZAR” (No. KDL201301) and the open project of “State Key Laboratory of Loess and Quaternary Geology” (No. SKLLQG1310) to T.-Y. Li and J.-Y. Li. This study was also supported by a Taiwan MOST grant (103-2119-M-002-022 to C.-C.S.).
Chongqing Key Laboratory of Karst Environment, School of Geographical Sciences, Southwest University, Chongqing, China; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China; Field Scientific Observation & Research Base of Karst Eco-environments at Nanchuan in Chongqing, Ministry of Land and Resources of China, Chongqing, China; Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, China; Department of Earth Sciences, University of Minnesota, Minneapolis, MN, United States; Department of Geosciences, National Taiwan University, Taipei, Taiwan; Institut für Geologie, Universität Innsbruck, Innsbruck, Austria
Recommended Citation:
Zhang T.-T.,Li T.-Y.,Cheng H.,et al. Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 79 ka BP[J]. Quaternary Science Reviews,2017-01-01,160