Anaerobic oxidation of methane by Mn oxides in sulfate-poor environments
文献类型:期刊论文
作者 | Cai, Chunfang1,2; Li, Kaikai3; Liu, Dawei2; John, Cedric M.4; Wang, Daowei3; Fu, Bin5; Fakhraee, Mojtaba6; He, Hong7; Feng, Lianjun1; Jiang, Lei1 |
刊名 | GEOLOGY |
出版日期 | 2021-07-01 |
卷号 | 49期号:7页码:761-766 |
ISSN号 | 0091-7613 |
DOI | 10.1130/G48553.1 |
英文摘要 | Strongly C-13-depleted authigenic carbonates (e.g., delta C-13(VPDB) <-30 parts per thousand; VPDB-Vienna Peedee belemnite) in nature are generally believed to form by sulfate-dependent anaerobic oxidation of methane (AOM). However, we demonstrate using geochemical data and thermodynamic calculation that such calcites are most likely derived from biogenic oxidation of methane in sulfate-poor, nonmarine environments during early diagenesis, as observed in the Triassic sandy conglomerates from the Junggar Basin, northwestern China. This process operated through preferential oxidation of C-13-depleted methane by Mn oxides in closed conditions, producing calcites with higher Mn contents and delta C-13 values in association with more C-13-enriched residual methane as a result of kinetic isotope fractionation. Thus, the Mn-rich and C-13-depleted carbonates are proposed as tracers of Mn-dependent AOM, which should have served as an important sink of greenhouse methane in low-sulfate early Earth's oceans. |
WOS关键词 | JUNGGAR BASIN ; DIAGENETIC ORIGIN ; SICHUAN BASIN ; CHINA ; ISOTOPE ; MANGANESE ; BACTERIAL ; CARBON ; IRON ; GEOCHEMISTRY |
资助项目 | National Natural Science Foundation of China[41730424] ; National Natural Science Foundation of China[4181101560] |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | GEOLOGICAL SOC AMER, INC |
WOS记录号 | WOS:000675396700008 |
资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/101951] |
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.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 3.China Univ Geosci Beijing, Sch Energy Resources, Beijing 100083, Peoples R China 4.Imperial Coll London, Dept Earth Sci & Engn, London SW7 2BU, England 5.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 2601, Australia 6.Yale Univ, Dept Geol & Geophys, New Haven, CT 06520 USA 7.SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China |
推荐引用方式 GB/T 7714 | Cai, Chunfang,Li, Kaikai,Liu, Dawei,et al. Anaerobic oxidation of methane by Mn oxides in sulfate-poor environments[J]. GEOLOGY,2021,49(7):761-766. |
APA | Cai, Chunfang.,Li, Kaikai.,Liu, Dawei.,John, Cedric M..,Wang, Daowei.,...&Jiang, Lei.(2021).Anaerobic oxidation of methane by Mn oxides in sulfate-poor environments.GEOLOGY,49(7),761-766. |
MLA | Cai, Chunfang,et al."Anaerobic oxidation of methane by Mn oxides in sulfate-poor environments".GEOLOGY 49.7(2021):761-766. |
入库方式: OAI收割
来源:地质与地球物理研究所
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