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Molecular preservation and bulk isotopic signals of ancient rice from the Neolithic Tianluoshan site, lower Yangtze River valley, China 期刊论文
Organic Geochemistry, 2013, 卷号: 63, 页码: 85-93
作者:  Gupta,NS(Gupta,Neal S.);  Leng,Q(Leng,Qin);  Yang,H(Yang,Hong);  Cody,GD(Cody,George D.);  Fogel,ML(Fogel,Marilyn L.);  Liu,WG(Liu,Weiguo);  Sun,GP(Sun,Guoping)
Adobe PDF(2243Kb)  |  收藏  |  浏览/下载：217/0  |  提交时间：2018/12/07
Proxy value of n-alkan-2-ones in the Hongyuan peat sequence to reconstruct Holocene climate changes on the eastern margin of the Tibetan Plateau 期刊论文
CHEMICAL GEOLOGY, 2011, 卷号: 288, 期号: 3-4, 页码: 97-104
作者:  Zheng, YH (Zheng, Yanhong)[1,2];  Zhou, WJ (Zhou, Weijian)[2];  Meyers, PA (Meyers, Philip A.)[3]
Adobe PDF(2167Kb)  |  收藏  |  浏览/下载：187/0  |  提交时间：2019/01/07
The Tibetan Plateau  Peat  n-Alkan-2-ones  Paleoclimatic changes  
The n-alkanol paleoclimate records in two peat deposits: a comparative study of the northeastern margin of the Tibetan Plateau and Northeast China 期刊论文
ENVIRONMENTAL EARTH SCIENCES, 2011, 卷号: 63, 期号: 1, 页码: 135-143
作者:  Zheng, YH (Zheng, Yanhong)[1,2];  Zhou, WJ (Zhou, Weijian)[2];  Liu, Z (Liu, Zhao)[2];  Liu, XM (Liu, Xiaomin)[1]
Adobe PDF(749Kb)  |  收藏  |  浏览/下载：226/0  |  提交时间：2019/01/07
n-Alkanols  Paleoclimate  Comparative study  The Tibetan Plateau  Northeast China  Solar radiation  
n-Alkan-2-one distributions in a northeastern China peat core spanning the last 16 kyr 期刊论文
ORGANIC GEOCHEMISTRY, 2011, 卷号: 42, 期号: 1, 页码: 25-30
作者:  Zheng,YH (Zheng, Yanhong)[1,2];  Zhou,WJ (Zhou, Weijian)[2,3];  Liu,XM (Liu, Xiaomin)[2];  Zhang,CLL (Zhang, Chuanlun L.)[4]
Adobe PDF(485Kb)  |  收藏  |  浏览/下载：260/0  |  提交时间：2019/01/07
Postglacial climate-change record in biomarker lipid compositions of the Hani peat sequence, Northeastern China 期刊论文
EARTH AND PLANETARY SCIENCE LETTERS, 2010, 卷号: 294, 期号: 1-2, 页码: 37-46
作者:  W.J. Zhou;  Y.H. Zheng;  P.A. Meyers;  A.J.T. Jull;  S.C. Xie
Adobe PDF(1066Kb)  |  收藏  |  浏览/下载：827/76  |  提交时间：2011/05/09
Peat  N-alkanes  N-alkanols  N-alkanoic Acids  Pre-boreal  Holocene Climate Optimum