Fossil gastropods from the MGS3 stratigraphic segment in the Salawusu River Valley and their climatic and environmental implications

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• 作者：BaoSheng Li (1) (2)
  DeNiu Chen (3)
  David Dian Zhang (4)
  XiaoHao Wen (1)
  ShiFan Qiu (1)
  XianJiao Ou (1)
  ShuHuan Du (1)
  DongFeng Niu (1)
  Yi Yang (1)
  JianPing Ye (1)
  YunHai Guo (1)
  
• 关键词：Salawusu River Valley ; Milanggouwan Section ; MGS3 stratigraphic segment ; fossil gastropods ; climatic environment
• 刊名：Science China Earth Sciences
• 出版年：2008
• 出版时间：March 2008
• 年：2008
• 卷：51
• 期：3
• 页码：339-348
• 全文大小：1686KB
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• 作者单位：BaoSheng Li (1) (2)
  DeNiu Chen (3)
  David Dian Zhang (4)
  XiaoHao Wen (1)
  ShiFan Qiu (1)
  XianJiao Ou (1)
  ShuHuan Du (1)
  DongFeng Niu (1)
  Yi Yang (1)
  JianPing Ye (1)
  YunHai Guo (1)
  
  1. School of Geography, South China Normal University, Guangzhou, 510631, China
  2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi鈥檃n, 710075, China
  3. Institute of Zoology, Chinese Academy of Sciences, Beijing, 100080, China
  4. Department of Geography and Geology, the University of Hong Kong, Hong Kong, China
  
• ISSN：1869-1897

文摘

Contemporaneous with MIS3, the MGS3 segment of the Milanggouwan stratigraphic section in the Salawusu River Valley, Mu Us Desert, China contains fossil gastropods (terrestrial and freshwater snails) in strata 33LS, 35LS, 37FL and 39LS. Examination of these fossils revealed 11 species belonging to 8 families and 10 genera. They can be classified as: (1) assemblage of Gyraulus and Galba mainly consisting of Gyraulus convexiusculus, Gyraulus sibiricus, Galba pervia and Galba superegra Gredler, etc. (2) assemblage of Vallonia mainly consisting of terrestrial snails, such as Vallonia patens, Pupilla muscorum and Discus paupe, etc. Based on the dating results, and the living habits, living conditions, and geographic distribution of their extant species, we suggest that: the ages of 33LS, 35LS, 37FL, and 39LS are 26000, 29000, 33000 and 38000 a, respectively, corresponding well to the interstadial period in GRIP 4, 5, 6 and 10 in terms of chronology and climatic characters; 33LS, 35LS and 39LS represent very warm-humid periods, while 37FL represents a less warm-humid period; the four periods of climatic fluctuations recorded in MGS3 were related to the strong impact of the summer monsoon in East Asia in Mu Us Desert of China during the interstadial of MIS3 on a global climatic background.