中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Methanogen-mediated dolomite precipitation in an early Permian lake in northwestern China

文献类型:期刊论文

作者Sun, Funing3,4; Hu, Wenxuan2,4; Wang, Xiaolin2,4; Hu, Zhongya4; Wu, Haiguang1; Guo, Yangrui5; Wei, Gangjian5
刊名GEOLOGICAL SOCIETY OF AMERICA BULLETIN
出版日期2024-07-01
卷号136期号:7-8页码:2637-2645
ISSN号0016-7606
DOI10.1130/B37156.1
英文摘要Microbes are known to mediate dolomite precipitation in laboratory experiments; however, the linkage of specific microbes to ancient dolomites remains poorly constrained due to scarce diagnostic biogeochemical signatures and mineralized microbial relics in the rock record. Here, we report the occurrence of methanogen-mediated dolomite in the Lower Permian lacustrine Lucaogou Formation in northwestern China. The clumped isotope (Delta(47 )) temperature provides direct evidence of a low-temperature origin (typically <40 degrees C). The extremely positive delta Mg-26 ( DSM3) (up to +0.44%0) and delta C-13 ( VPDB) (up to +19%0) values in the dolomite indicate authigenic precipitation in methanogenic lake sediments. Micron-sized spheroidal bodies and filamentous and sheetlike structures are interpreted as mineralized coccoid methanogenic archaea and extracellular polymeric substances (EPSs), respectively. Dolomite nanoglobules (primarily 40-100 nm in diameter) are interpreted as mineralized viruses attached to the archaea and EPSs and between the cells. A combination of geochemical and microscale evidence confirms the microbial origin of the dolomite induced by methanogens and their associated bacteriophages. Furthermore, dolomite nanoglobules initially nucleated on the surfaces of methanogen cells, EPSs, and viruses and then merged into larger aggregates. The formation of microbial dolomite is characterized by a metabolic incubation, heterogeneous nucleation, and aggregative growth pathway. These findings provide valuable clues to decipher the biosignatures of these particular ancient dolomites.
WOS研究方向Geology
语种英语
WOS记录号WOS:001271970100001
源URL[http://ir.gig.ac.cn/handle/344008/72339]  
专题同位素地球化学国家重点实验室
通讯作者Hu, Wenxuan
作者单位1.Northeast Petr Univ, Sch Earth Sci, Daqing 163318, Peoples R China
2.Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Nanjing 210023, Peoples R China
3.China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
4.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Peoples R China
5.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
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GB/T 7714
Sun, Funing,Hu, Wenxuan,Wang, Xiaolin,et al. Methanogen-mediated dolomite precipitation in an early Permian lake in northwestern China[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2024,136(7-8):2637-2645.
APA Sun, Funing.,Hu, Wenxuan.,Wang, Xiaolin.,Hu, Zhongya.,Wu, Haiguang.,...&Wei, Gangjian.(2024).Methanogen-mediated dolomite precipitation in an early Permian lake in northwestern China.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,136(7-8),2637-2645.
MLA Sun, Funing,et al."Methanogen-mediated dolomite precipitation in an early Permian lake in northwestern China".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 136.7-8(2024):2637-2645.

入库方式: OAI收割

来源:广州地球化学研究所

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