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When did the Anthropocene begin? A mid-twentieth centuryboundary level is stratigraphically optimal 期刊论文
Quaternary International, 2015, 卷号: 383, 期号: 2015, 页码: 196-203
作者:  Zalasiewicz,J(Zalasiewicz,Jan)[1];  Waters,CN(Waters,Colin N)[2];  Williams,M(Williams,Mark)[1];  Barnosky,AD(Barnosky,Anthony D)[3];  Cearreta,A(Cearreta,Alejandro)[4];  Crutzen,P(Crutzen,Paul)[5];  Ellis,E(Ellis,Erle)[6];  Ellis,MA(Ellis,Michael A)[2];  Fairchild,IJ(Fairchild,Ian J)[7];  Grinevald,J(Grinevald,Jacques)[8];  Haff,PK(Haff,Peter K)[9];  Hajdas,I(Hajdas,Irka)[10];  Leinfelder,R(Leinfelder,Reinhold)[11];  McNeill,J(McNeill,John)[12];  Odada,EO(Odada,Eric O)[13];  Poirier,C(Poirier,C)[14];  Richter,D(Richter,Daniel)[15];  Steffen,W(Steffen,Will)[16];  Summerhayes,C(Summerhayes,Colin)[17];  Syvitski,JPM(Syvitski,James P.M)[18];  Vidas,D(Vidas,Davor)[19];  Wagreich,M(Wagreich,Michael)[20];  Wing,SL(Wing,Scott L)[21];  Wolfe,AP(Wolfe,Alexander P)[22];  An,ZS(An,Zhisheng)[23];  Oreskes,N(Oreskes, Naomi)[24]
收藏  |  浏览/下载：327/0  |  提交时间：2018/11/21
Anthropocene  Stratigraphy  GSSP  GSSA  
When did the Anthropocene begin? A mid-twentieth centuryboundary level is stratigraphically optimal 期刊论文
Quaternary International, 2015, 卷号: 383, 期号: 2015, 页码: 196-203
作者:  Zalasiewicz,J(Zalasiewicz,Jan)[1];  Waters,CN(Waters,Colin N)[2];  Williams,M(Williams,Mark)[1];  Barnosky,AD(Barnosky,Anthony D)[3];  Cearreta,A(Cearreta,Alejandro)[4];  Crutzen,P(Crutzen,Paul)[5];  Ellis,E(Ellis,Erle)[6];  Ellis,MA(Ellis,Michael A)[2];  Fairchild,IJ(Fairchild,Ian J)[7];  Grinevald,J(Grinevald,Jacques)[8];  Haff,PK(Haff,Peter K)[9];  Hajdas,I(Hajdas,Irka)[10];  Leinfelder,R(Leinfelder,Reinhold)[11];  McNeill,J(McNeill,John)[12];  Odada,EO(Odada,Eric O)[13];  Poirier,C(Poirier,C)[14];  Richter,D(Richter,Daniel)[15];  Steffen,W(Steffen,Will)[16];  Summerhayes,C(Summerhayes,Colin)[17];  Syvitski,JPM(Syvitski,James P.M)[18];  Vidas,D(Vidas,Davor)[19];  Wagreich,M(Wagreich,Michael)[20];  Wing,SL(Wing,Scott L)[21];  Wolfe,AP(Wolfe,Alexander P)[22];  An,ZS(An,Zhisheng)[23];  Oreskes,N(Oreskes, Naomi)[24]
Adobe PDF(498Kb)  |  收藏  |  浏览/下载：331/0  |  提交时间：2018/11/14
Anthropocene  Stratigraphy  Gssp  Gssa  
Soil N retention and nitrateleaching in three types of dunesin the Mu Us desert of China 期刊论文
Scientific Reports, 2015, 卷号: 5, 页码: 14222
作者:  Jin,Z(Jin,Zhao)[1];  Zhu,YJ(Zhu,Yajuan)[2];  Li,XR(Li,Xiangru)[1];  Dong,YS(Dong,Yueshe)[3];  An,ZS(An,Zhisheng)[1]
Adobe PDF(881Kb)  |  收藏  |  浏览/下载：204/0  |  提交时间：2018/11/13
Soil N retention and nitrateleaching in three types of dunesin the Mu Us desert of China 期刊论文
Scientific Reports, 2015, 卷号: 5, 页码: 14222
作者:  Jin,Z(Jin,Zhao)[1];  Zhu,YJ(Zhu,Yajuan)[2];  Li,XR(Li,Xiangru)[1];  Dong,YS(Dong,Yueshe)[3];  An,ZS(An,Zhisheng)[1]
收藏  |  浏览/下载：133/0  |  提交时间：2018/11/21
A Chinese cave links climatechange, social impacts, and humanadaptation over the last 500 years 期刊论文
Scientific Reports, 2015, 卷号: 5, 期号: 2015, 页码: 12284
作者:  Tan,LC(Tan,Liangcheng)[1,2];  Can,YJ(Cai,Yanjun)[1,3];  An,ZS(An,Zhisheng)[1,3];  Cheng,H(Cheng,Hai)[3,4];  Shen,CC(Shen,Chuan-Chou)[5];  Breitenbach,S F.M.(Breitenbach,Sebastian F.M.)[6];  Gao,YL(Gao,Yongli)[7];  Edwards, R.L(Edwards, R.Lawrence)[4];  Zhang,HW(Zhang,Haiwei)[3];  Du,YJ(Du,Yajun)[1]
Adobe PDF(2502Kb)  |  收藏  |  浏览/下载：240/0  |  提交时间：2018/11/09
黄土区小流域土壤容重和饱和导水率的时空动态特征 期刊论文
农业工程学报, 2015, 卷号: 31, 期号: 13, 页码: 128-134
作者:  傅子洹;  王云强;  安芷生
Adobe PDF(1803Kb)  |  收藏  |  浏览/下载：236/0  |  提交时间：2019/01/08
土壤  水分  流域  饱和导水率  容重  时空动态  黄土高原  
Miocene climate change on the Chinese Loess Plateau: Possiblelinks to the growth of the northern Tibetan Plateau and globalcooling 期刊论文
Geochemistry, Geophysics, Geosystems, 2015, 页码: 2097-2108
作者:  Sun,YB(Sun,Youbin)[1,2];  Ma,L(Ma,Long)[1,3];  Bloemendal,J(Bloemendal,Jan)[4];  Clemens,S(Clemens,Steven)[5];  Qiang,XK(Qiang,Xiaoke)[1];  An,ZS(An,Zhisheng)[1]
Adobe PDF(5052Kb)  |  收藏  |  浏览/下载：235/0  |  提交时间：2018/11/13
Miocene climate change on the Chinese Loess Plateau: Possiblelinks to the growth of the northern Tibetan Plateau and globalcooling 期刊论文
Geochemistry, Geophysics, Geosystems, 2015, 页码: 2097-2108
作者:  Sun,YB(Sun,Youbin)[1,2];  Ma,L(Ma,Long)[1,3];  Bloemendal,J(Bloemendal,Jan)[4];  Clemens,S(Clemens,Steven)[5];  Qiang,XK(Qiang,Xiaoke)[1];  An,ZS(An,Zhisheng)[1]
收藏  |  浏览/下载：186/0  |  提交时间：2018/11/21
Mass accumulation rate changes in Chinese loess during MIS 2, andasynchrony with records from Greenland ice cores and North PacificOcean sediments during the Last Glacial Maximum 期刊论文
Aeolian Research, 2015, 卷号: 19, 期号: 2015, 页码: 251-258
作者:  Kang,SG(Kang,Shugang)[1];  Roberts,HM(Roberts,Helen M)[2];  Wang,XL(Wang,Xulong)[1];  An,ZS(An,Zhisheng)[1];  Wang,M(Wang,Min)[3]
Adobe PDF(1113Kb)  |  收藏  |  浏览/下载：252/0  |  提交时间：2018/11/13
Chinese Loess  Quartz Osl  Dust Accumulation  Last Glacial Maximum  Westerly Jet  East Asian Winter Monsoon  
Carbon isotope composition of long chain leaf wax n-alkanes in lakesediments: A dual indicator of paleoenvironment in the Qinghai-TibetPlateau 期刊论文
Organic Geochemistry, 2015, 卷号: 83-84, 页码: 190-201
作者:  Liu,WG(Liu,Weiguo)[1,2];  Yang,H(Yang,Hong)[3];  Wang,HY(Wang,Huanye)[1,4];  An,ZS(An,Zhisheng)[1];  Wang,Z(Wang,Zheng)[1];  Leng,Q(Leng,Qin)[3]
Adobe PDF(1829Kb)  |  收藏  |  浏览/下载：224/0  |  提交时间：2018/11/09
Long-chain N-alkanes  D13c Values  Aquatic Plants  Terrestrial Plants  Lake Qinghai