Variations in precipitation pathways of Mesoproterozoic shallow seawater carbonates from North China Platform:response in seawater redox fluctuations?
Wu Meng-Ting1,2, Fang Hao3, Sun Long-Fei3, Shi Xiao-Ying1,3, Tang Dong-Jie1,2
1 State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences (Beijing),Beijing 100083, China; 2 Institute of Earth Sciences,China University of Geosciences (Beijing),Beijing 100083, China; 3 School of Earth Sciences and Resources,China University of Geosciences (Beijing),Beijing 100083, China
Abstract：It has been considered that the precipitation pathways of marine carbonates are closely related to seawater redox conditions. Due to the presence of carbonate precipitation inhibitor(e.g.,Fe2+ and Mn2+)-rich shallow seawaters during Archean and Paleoproterozoic,nucleation of calcite mud in water column was inhibited but formation of seafloor aragonite precipitates was allowed. In contrast,the oxidative removal of carbonate precipitation inhibitors in Neoproterozoic shallow seawaters promoted the direct precipitation of carbonate mud from water column. However,it needs more detailed case studies to test the connection between seawater redox and pathways of carbonate precipitation,since the secular variation in the pathways of carbonate precipitation may controlled by other factors. This study focuses on the fabric and geochemistry of carbonates deposited during the Mesoproterozoic,a transitional period of carbonate precipitation. Abundant carbonate mud occurs in the Member Ⅲ of the Gaoyuzhuang Formation(~1.56 Ga),the Member Ⅳ of the Wumishan Formation(~1.48 Ga),and the Member Ⅱ of the Tieling Formation(~1.44 Ga)in North China. These water column precipitated carbonate mud has relatively high Ⅰ/(Ca+Mg)ratios(generally>0.5 μmol/mol)and negative Ce anomalies(down to 0.8),indicating moderately oxygenated conditions. In contrast,abundant seafloor precipitated aragonite fans occur in the lower Member Ⅳ of the Gaoyuzhuang Formation(~1.55 Ga)and the Member Ⅱ of the Wumishan Formation(~1.50 Ga). These seafloor precipitates have near zero Ⅰ/(Ca+Mg)ratios,suggesting suboxic to anoxic conditions. Therefore,this study,firstly using detailed cases,proves that the texture of Precambrian carbonates was largely controlled by the redox conditions of seawaters and could be used as a redox proxy to conduct long-term and multi-section study of marine redox conditions directly and efficiently based on outcrop observations in the field.
Wu Meng-Ting,Fang Hao,Sun Long-Fei et al. Variations in precipitation pathways of Mesoproterozoic shallow seawater carbonates from North China Platform:response in seawater redox fluctuations?[J]. JOPC, 2021, 23(4): 703-722.
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