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Advances in the microbial mineralization of seafloor hydrothermal systems
Institution:1. Key Laboratory of Gas Hydrate (Ministry of Natural Resources), Qingdao Institute of Marine Geology, China Geological Survey, Ministry of Natural Resources, Qingdao 266071, China;2. Evaluation and Detection Technology Laboratory for Marine Mineral Resources, National Laboratory for Marine Science and Technology, Qingdao 266071, China;3. China University of Petroleum, Qingdao 266580, China;4. Linyi University, Linyi 276000, China;5. China University of Geosciences (Beijing), Beijing 100083, China;6. Geology Research Institute, Greatwall Drilling Company, Panjin 124010, China
Abstract:Research on the biomineralization in modern seafloor hydrothermal systems is conducive to unveiling the mysteries of the early Earth’s history, life evolution, subsurface biosphere and microbes in outer space. The hydrothermal biomineralization has become a focus of geo-biological research in the last decade, since the introduction of the microelectronic technology and molecular biology technology. Microorganisms play a critical role in the formations of oxide/hydroxides (e.g. Fe, Mn, S and Si oxide/hydroxides) and silicates on the seafloor hydrothermal systems globally. Furthermore, the biomineralization of modern chemolithoautotrophic microorganisms is regarded as a nexus between the geosphere and the biosphere, and as an essential complement of bioscience and geology. In this paper, we summarize the research progress of hydrothermal biomineralization, including the biogenic minerals, the microbial biodiversity, and also the interactions between minerals and microorganisms. In the foreseeable future, the research on hydrothermal biomineralization will inspire the development of geosciences and biosciences and thus enrich our knowledge of the Earth’s history, life evolution and even astrobiology.© 2019 China Geology Editorial Office.
Keywords:Seafloor hydrothermal systems  Biomineralization  Chemolithoautotrophic microorganisms  Life evolution
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