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Inferring critical transitions in paleoecological time series with irregular sampling and variable time-averaging [期刊论文]
Quaternary Science Reviews, 2019-01-01, 207
Stegner M.A.;  Ratajczak Z.;  Carpenter S.R.;  Williams J.W.
View/Download：28/0
 
Quaternary paleoenvironmental evolution of the Tengger Desert and its implications for the provenance of the loess of the Chinese Loess Plateau [期刊论文]
Quaternary Science Reviews, 2018-01-01, 197
Fan Y.;  Mou X.;  Wang Y.;  Liu C.;  Zhao H.;  Wang F.;  Li Z.;  Mao X.;  Liu W.;  Ma J.;  Liu C.;  Zhang F.;  Zhang F.
View/Download：19/0
 
Early to Middle Holocene sea level fluctuation, coastal progradation and the Neolithic occupation in the Yaojiang Valley of southern Hangzhou Bay, Eastern China [期刊论文]
Quaternary Science Reviews, 2018-01-01, 189
Liu Y.;  Sun Q.;  Fan D.;  Dai B.;  Ma F.;  Xu L.;  Chen J.;  Chen Z.
View/Download：47/0
 
Paleomagnetic chronology and paleoenvironmental records from drill cores from the Hetao Basin and their implications for the formation of the Hobq Desert and the Yellow River [期刊论文]
Quaternary Science Reviews, 2017-01-01, 156
Li B.;  Sun D.;  Xu W.;  Wang F.;  Liang B.;  Ma Z.;  Wang X.;  Li Z.;  Chen F.
View/Download：22/0
 
Magnetostratigraphic age and monsoonal evolution recorded by the thickest Quaternary loess deposit of the Lanzhou region, western Chinese Loess Plateau [期刊论文]
Quaternary Science Reviews, 2016-01-01, 139
Zhang J.;  Li J.;  Guo B.;  Ma Z.;  Li X.;  Ye X.;  Yu H.;  Liu J.;  Yang C.;  Zhang S.;  Song C.;  Hui Z.;  Peng T.
View/Download：20/0
 
Monsoon influence on planktic δ18O records from the South China Sea [期刊论文]
Quaternary Science Reviews, 2016-01-01, 142
Wang P.;  Li Q.;  Tian J.;  He J.;  Jian Z.;  Ma W.;  Dang H.
View/Download：15/0
 
Initiation and variation of the dune fields in semi-arid China - with aspecial reference to the Hunshandake Sandy Land, Inner Mongolia [期刊论文]
Quaternary Science Reviews, 2013-01-01, 78
Yang X.;  Wang X.;  Liu Z.;  Li H.;  Ren X.;  Zhang D.;  Ma Z.;  Rioual P.;  Jin X.;  Scuderi L.
View/Download：31/0
 

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