摘要
A long-standing question regarding the Holocene evolution of the East Asian Summer Monsoon(EASM)is whether it peaked during the early Holocene(EH)as inferred from rainfall-related proxy records[1,2],or during the mid-Holocene as inferred from ecoenvironmental records from northern China[3,4].Cheng et al.
作者
Wenchao Zhang
Haibin Wu
Qin Li
Zhengyu Liu
Jun Cheng
张文超;吴海斌;李琴;刘征宇;程军(Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Center for Excellence in Life and Paleoenvironment,Chinese Academy of Sciences,Beijing 100044,China;College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China;School of Geography,Liaoning Normal University,Dalian 116029,China;Atmospheric Science Program,Department of Geography,The Ohio State University,Columbus OH 43210,USA;Center for Ocean-Atmosphere Interaction Research,Nanjing University of Information Science and Technology,Nanjing 210044,China)
基金
supported by the National Key Research and Development Program of China(2020YFA0607700)
the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB26000000)
the National Natural Science Foundation of China(41807424,41888101,41572165,and 41690114)。
