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What does the occurrence of Sporormiella (Preussia) spores mean in Australian fossil sequences? 期刊论文
JOURNAL OF QUATERNARY SCIENCE, 2018, 卷号: 33, 期号: 4, 页码: 380-392
作者:  Dodson, John;  Field, Judith H.
Adobe PDF(6717Kb)  |  收藏  |  浏览/下载：293/1  |  提交时间：2018/09/21
Cuddie Springs  Megafauna Extinctions  Megaherbivores  Palaeoenvironment  Sporormiella  
Cosmogenic Be-10 surface exposure dating and glacier reconstruction for the Last Glacial Maximum in the Quemuqu Valley, western Nyainqentanglha Mountains, south Tibet 期刊论文
JOURNAL OF QUATERNARY SCIENCE, 2017, 卷号: 32, 期号: 5, 页码: 639-652
作者:  Dong, Guocheng;  Xu, Xiangke;  Zhou, Weijian;  Fu, Yunchong;  Zhang, Li;  Li, Ming
Adobe PDF(10039Kb)  |  收藏  |  浏览/下载：307/0  |  提交时间：2018/10/16
Be-10 Surface Exposure Dating  Equilibrium Line Altitude  Glacier Reconstruction  Last Glacial Maximum  Nyainqentanglha  
Speleothem-derived Asian summer monsoon variationsin Central China, 54–46 ka 期刊论文
JOURNAL OF QUATERNARY SCIENCE, 2011, 卷号: 26, 期号: 8, 页码: 781-790
作者:  Zhou,HY(Zhou,Houyun)[1,2,6]ou,;  Zhao,JX(Zhao,Jianxin)[3,4];  Wang,Q(Wang,Qing)[5];  Feng,YX(Feng,Yuexing)[3];  Tang,J(Tang,Jing)[1]
Adobe PDF(289Kb)  |  收藏  |  浏览/下载：244/0  |  提交时间：2019/01/07
stalagmite  d18O  U–Th ages  climate change  Central China  Late Pleistocene  
Luminescence dating of sand–loess sequences and response of Mu Us and Otindag sand fields (northChina) to climatic changes 期刊论文
JOURNAL OF QUATERNARY SCIENCE, 2009, 卷号: 24, 期号: 4, 页码: 336-344
作者:  Y.L. Zhou;  H.Y. Lu;  J.F. Zhang;  J.A. Mason;  L.P. Zhou
Adobe PDF(375Kb)  |  收藏  |  浏览/下载：297/45  |  提交时间：2011/06/07
Optical Dating  Sand–loess System  Dry Climate Events  Late Quaternary  North China  
East Asia winter monsoon variations on a millennial time-scale before the last glacial-interglacial cycle 期刊论文
JOURNAL OF QUATERNARY SCIENCE, 1999, 卷号: 14, 期号: 2, 页码: 101-110
作者:  Lu, HY;  Van Huissteden, KO;  An, ZS;  Nugteren, G;  Vandenberghe, J
收藏  |  浏览/下载：137/0  |  提交时间：2020/05/28
East Asia winter monsoon  millennial time-scale variability  Middle and Early Pleistocene