的存在和硫化物对镁水合物脱水的影响以及微生物白云石沉淀的环境因子。对微生物成因的原生白云石模式的深入认识,将为湖相白云石成因研究提供新的理论基础和研究思路。"/>
O42-,the impact of sulfide on dehydration of magnesium hydrate and the environmental factors on the precipitation of microbial dolomite. The deep understanding of microbiogenic of primary dolomite model will provide a new theoretical basis and a new insight for lacustrine dolomite."/>
Microbial mechanism of lacustrine primary dolomite
Microbial mechanism of lacustrine primary dolomite
Jiang Qicai1, Liu Bo1, Guo Rongtao1, Gao Xiaoqiao2, Li Yang2, Zhang Shanming1
1 School of Earth and Space Sciences/Oil & Gas Institute,Peking University,Beijing 100871.; 2 School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083;
Abstract Recently,with the in-depth research on the microbial dolomite mode,a new perspective on Dolomite Problem has been provided. Previous researches on the origin of microbial dolomite mainly focused on the microbial processes in unconsolidated sediments,which equals to organic penecontemporaneous dolomitization. It differs from bacteria￣induced organic primary dolomite in laboratory in mechanism. This study introduces the formation mechanism of microbial dolomite into lacustrine primary dolomite,concluding that it would also precipitate primary dolomite in the interface between lake water and sediment,organic primary dolomite. There is a distinction between lake water and sediment in microenvironment of interface,which can be generally divided into two subenvironments: Aerobic and anaerobic,living with different microflora. According to the subenvironments' characteristics of different lake types,different microorganism species and their various role in the formation of dolomite,three microbial dolomite modes can be distinguished,which are the aerobic oxidation mode,the sulphate reduction mode and the methanogenesis mode. Different modes of the microbial dolomite correspond to different lake environments: The aerobic oxidation mode mainly develops in aerobic,high Mg/Ca,salt water lake/saline. The sulphate reduction mode mostly develops in anaerobic,high Mg/Ca,salt water lake/saline. The methanogenesis mode primarily develops in anaerobic,low Mg/Ca,freshwater lake/salt water lake. Moreover,some still-controversial issues on the process of dolomite precipitation will be discussed,such as the changing of pH,the effect of SO42-,the impact of sulfide on dehydration of magnesium hydrate and the environmental factors on the precipitation of microbial dolomite. The deep understanding of microbiogenic of primary dolomite model will provide a new theoretical basis and a new insight for lacustrine dolomite.
Received: 17 November 2016
Published: 01 April 2017
About author: About the first author Jiang Qicai,born in 1992,is a Ph.D. candidate of Peking University. He is engaged in sedimentology. E-mail: jiangqc@pku.edu.cn.About the corresponding author Liu Bo,born in 1965,is a professor and Ph.D. supervisor in Peking University. He is engaged in sedimentology and structural geology. E-mail: bobliu@pku.edu.cn.
Cite this article:
Jiang Qicai,Liu Bo,Guo Rongtao et al. Microbial mechanism of lacustrine primary dolomite[J]. JOPC, 2017, 19(2): 257-269.
Jiang Qicai,Liu Bo,Guo Rongtao et al. Microbial mechanism of lacustrine primary dolomite[J]. JOPC, 2017, 19(2): 257-269.
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