Relationship between the shell geochemistry of the modern aquatic gastropod Radix and water chemistry of lakes of the Tibetan Plateau

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• 作者：Feng Chen ; Jin-Liang Feng ; Hai-Ping Hu
• 关键词：Tibetan Plateau ; Gastropod Radix ; Hydrochemistry ; Shell geochemistry ; Oxygen and carbon isotopes ; Sr/Ca ratio
• 刊名：Hydrobiologia
• 出版年：2016
• 出版时间：May 2016
• 年：2016
• 卷：771
• 期：1
• 页码：239-254
• 全文大小：1,442 KB
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• 作者单位：Feng Chen (1) (2)
  Jin-Liang Feng (1)
  Hai-Ping Hu (1) (2)
  
  1. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Building 3, 16th Lincui Road, Chaoyang District, Beijing, 100101, China
  2. University of Chinese Academy of Sciences, Beijing, 100049, China
  
• 刊物类别：Biomedical and Life Sciences
• 刊物主题：Life Sciences
  Hydrobiology
  Ecology
  
• 出版者：Springer Netherlands
• ISSN：1573-5117

文摘

Fossil shells of the aquatic mollusk Radix are common in the exposed sediments of lake terraces on the Tibetan Plateau. However, the living environment of Radix, and the geochemical characteristics of its shells, is unclear. Here, we report the results of an investigation of the occurrence of modern Radix in lakes of the southeastern and central Tibetan Plateau, as well as measurements of various geochemical characteristics of the shells. The results indicate that the nutritional status of the lake waters is the main limiting factor for the survival of Radix in these lakes. The Sr/Ca ratio of the Radix shells is significantly positively correlated with both the Sr/Ca ratio and the conductivity of the lake water. Initially, Kd _Sr decreases rapidly with low values of Sr/Ca_water; however, in the case of Sr/Ca_water values above 0.0076, Kd _Sr exhibits only a small range of variation. The δ 13C_shell values are controlled by the δ 13C of lake water dissolved inorganic carbon (DIC). In addition, the contribution of DIC of organic origin to the Radix shells increases when the lake water is deficient in DIC of inorganic origin. The δ 18O values of the Radix shells provide useful information about the isotopic composition of the ambient waters.