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On the unusual holocene carbonate sediment in lake Nam Co, central Tibet

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Abstract

In lacustrine sediments, aragonite is a widespread mineral, whereas monohydrocalcite is a rare carbonate mineral. In the cold and high-attitude Xizang (Tibetan) Plateau, where aragonite has been commonly found in lacustrine sediments, there is no aragonite, but low-Mg calcite, monohydrocalcite and trace dolomite. The lake receives solutes primarily from surface runoffs and remains fairly constant water chemistry for a long time. The total CaCO3 percentage in sediments could be controlled by evaporation and inflow of detrital materials. The absence of aragonite is unusual when compared to other lacustrine sediments from the Tibetan Plateau. This could be due to low Ca/Mg ratio, low salinity, low Mg and Ca concentration. Monohydrocalcite might precipitate from the lake water mediated by biological activities. Low-Mg calcite originated from minor ostracoda shell and the precipitation of lake water with biological activities.

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Authors and Affiliations

  1. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing, 100085, China

    Minghui Li, Shichang Kang, Liping Zhu, Junbo Wang, Chaolu Yi, Xiaomin Fang & Manping Xie

  2. State Key Laboratory of Cryospheric Science, CAS, Lanzhou, 730000, China

    Shichang Kang

  3. Department of Environment and Geography and Department of Chemistry, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada

    Feiyue Wang

Authors
  1. Minghui Li
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  2. Shichang Kang
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  3. Liping Zhu
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  4. Feiyue Wang
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  7. Xiaomin Fang
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Correspondence to Shichang Kang.

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Li, M., Kang, S., Zhu, L. et al. On the unusual holocene carbonate sediment in lake Nam Co, central Tibet. J. Mt. Sci. 6, 346–353 (2009). https://doi.org/10.1007/s11629-009-1020-8

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  • DOI: https://doi.org/10.1007/s11629-009-1020-8

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