Environmental variation in central Tibetan Plateau in the last 200 years
文献类型:期刊论文
作者 | Wu, YH; Wang, SM; Xia, WL; Zhu, YX; Yin, Y |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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出版日期 | 2001 |
卷号 | 44期号:supp页码:332-337 |
关键词 | Cuoe Lake central Tibetan Plateau carbonate content isotope |
英文摘要 | Through the analyses on sediment lithology, Pb-210 and Cs-137 dating, carbonate content, Sr/Ca and Mg/Ca of Ostrocod, and carbon and oxygen stable isotope of carbonate of gravity core from Cuoe Lake in the Naqu area, Tibetan Plateau, the paleolimnology was studied to investigate the environmental variation in the central Tibetan Plateau in the last 200 years. It is inferred that the environmental variation has undergone two stages. The climate was arid in the early 100 years, while it became warmer and more humid in the later 100 years, with a period of 20 years for humidity change. |
公开日期 | 2012-03-02 |
源URL | [http://159.226.73.51/handle/332005/2341] ![]() |
专题 | 南京地理与湖泊研究所_湖泊室 |
推荐引用方式 GB/T 7714 | Wu, YH,Wang, SM,Xia, WL,et al. Environmental variation in central Tibetan Plateau in the last 200 years[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2001,44(supp):332-337. |
APA | Wu, YH,Wang, SM,Xia, WL,Zhu, YX,&Yin, Y.(2001).Environmental variation in central Tibetan Plateau in the last 200 years.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,44(supp),332-337. |
MLA | Wu, YH,et al."Environmental variation in central Tibetan Plateau in the last 200 years".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 44.supp(2001):332-337. |
入库方式: OAI收割
来源:南京地理与湖泊研究所
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