Distinguishing microbial from thermochemical sulfate reduction from the upper Ediacaran in South China
文献类型:期刊论文
作者 | Hu, Yongjie1,2; Cai, Chunfang2,3,4,5; Liu, Dawei6; Peng, Yanyan2,3,5; Wei, Tianyuan2,3,5; Jiang, Ziwen2,3,5; Ma, Rongtu1; Jiang, Lei2,5 |
刊名 | CHEMICAL GEOLOGY
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出版日期 | 2021-11-20 |
卷号 | 583页码:17 |
关键词 | Microbial sulfate reduction Thermochemical sulfate reduction Cryptic sulfur cycle Sulfur disproportionation |
ISSN号 | 0009-2541 |
DOI | 10.1016/j.chemgeo.2021.120482 |
英文摘要 | It is hard to distinguish pyrites generated by microbial sulfate reduction (MSR) from thermochemical sulfate reduction (TSR). The upper Ediacaran Dengying Formation (ca 551-541 Ma) of Sichuan basin is chosen to study for this purpose by means of petrological, bulk and micrometer-scale analyses on barite, pyrite, calcite, and dolomite for carbon and sulfur isotope and rare earth elements and yttrium (REY) compositions. We find that MSR-derived pyrites precipitated from near-surface to shallow burial settings are characterized by seawater-like REY patterns and superchondritic Y/Ho ratios (74.3 +/- 9.5), and have delta S-34(pyrite) values in a wide range from -36.8 parts per thousand to 34.8 parts per thousand, positively correlated with arsenic contents, likely through cryptic sulfur cycles driven by arsenic. In contrast, TSR-derived pyrites generated during deep burial settings have REY characterized by non-seawater-like patterns and chondritic Y/Ho ratios (33.6 +/- 5.1), and show small sulfur isotopic fractionations (similar to 10.5 parts per thousand). TSR-pyrites yield both U-shaped and bell-shaped delta S-34 transects compared with U-shaped distributions of MSR-pyrites. The calcites associated with the TSR-pyrites show LREE enrichment, elevated Y/Ho ratios (85.8 +/- 14.2) and negative delta C-13 values, likely resulting from decomposition of organic matter. This study highlights a combination method from REY patterns, delta C-13 and delta S-34 values from analyses on micro-sized pyrite and the associated calcites can be used to effectively distinguish MSR from TSR. |
WOS关键词 | RARE-EARTH-ELEMENTS ; SULFUR ISOTOPE FRACTIONATION ; NEOPROTEROZOIC DOUSHANTUO FORMATION ; BOHAI BAY BASIN ; SICHUAN BASIN ; GEOCHEMICAL CHARACTERISTICS ; TRACE-ELEMENT ; CARBONATE RESERVOIRS ; HYDROTHERMAL FLUIDS ; DOLOMITE RESERVOIRS |
资助项目 | Natural Science Foundation of China[41730424] ; Natural Science Foundation of China[4181101560] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
WOS记录号 | WOS:000702309700024 |
出版者 | ELSEVIER |
资助机构 | Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/102971] ![]() |
专题 | 地质与地球物理研究所_中国科学院新生代地质与环境重点实验室 |
通讯作者 | Cai, Chunfang |
作者单位 | 1.Sinopec Int Petr Explorat & Prod Corp, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 4.Yangtze Univ, Key Lab Explorat Technol Oil & Gas Resources, Minist Educ, Wuhan 430100, Peoples R China 5.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China 6.SINOPEC, Petr Explorat & Prod Res Inst, Beijing 102206, Peoples R China |
推荐引用方式 GB/T 7714 | Hu, Yongjie,Cai, Chunfang,Liu, Dawei,et al. Distinguishing microbial from thermochemical sulfate reduction from the upper Ediacaran in South China[J]. CHEMICAL GEOLOGY,2021,583:17. |
APA | Hu, Yongjie.,Cai, Chunfang.,Liu, Dawei.,Peng, Yanyan.,Wei, Tianyuan.,...&Jiang, Lei.(2021).Distinguishing microbial from thermochemical sulfate reduction from the upper Ediacaran in South China.CHEMICAL GEOLOGY,583,17. |
MLA | Hu, Yongjie,et al."Distinguishing microbial from thermochemical sulfate reduction from the upper Ediacaran in South China".CHEMICAL GEOLOGY 583(2021):17. |
入库方式: OAI收割
来源:地质与地球物理研究所
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