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    Volume 50 Issue 3
    Mar.  2025
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    Article Navigation >  Earth Science  > 2025  >  50(3): 887-907
    Yuan Yuan, Liu Yongqin, 2025. Research Progress on Microbes Involved in Lacustrine Iron/Sulfur Cycling. Earth Science, 50(3): 887-907. doi: 10.3799/dqkx.2024.055
    Citation: Yuan Yuan, Liu Yongqin, 2025. Research Progress on Microbes Involved in Lacustrine Iron/Sulfur Cycling. Earth Science, 50(3): 887-907. doi: 10.3799/dqkx.2024.055
    shu

    Research Progress on Microbes Involved in Lacustrine Iron/Sulfur Cycling

    doi: 10.3799/dqkx.2024.055
    • 1.

      Center for Pan-Third Pole Environment, Lanzhou University, Lanzhou 730000, China

    • 2.

      State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China

    • 3.

      University of Chinese Academy of Sciences, Beijing 100101, China

    • Received Date: 2024-03-22
    • Publish Date: 2025-03-25
      Abstract
    • Lake, as an important part of inland water bodies, is a key site of action for the cycling of material elements by linking the atmosphere, rocks and hydrosphere. Iron, the fourth most abundant element in the Earth's crust, is prevalent in various mineral phases, and sulfur exists in various inorganic/organic compounds in a variety of valence states. The mutual transformation and interaction between iron and sulfur in different valence states in lakes constitute the process of iron and sulfur cycling in lakes, in which microorganisms play a dominant role and become an indispensable part of the cycle. This review summarizes the types of microorganisms, metabolic pathways and environmental influences involved in the iron and sulfur cycles in lakes, focusing on the current status of microbial research related to the iron and sulfur cycles in lakes on the Qinghai-Xizang Plateau, and presenting the future direction of microbial-driven iron and sulfur cycling research in lakes on the Qinghai-Xizang Plateau.

       

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