收稿日期: 2018-10-30
修回日期: 2018-12-11
网络出版日期: 2019-03-26
基金资助
国家自然科学基金面上项目“南海北部湾沉积物有机质成岩矿化过程及其对孔隙水溶解无机碳（DIC)的贡献”（编号：41676061）；上海市自然科学基金项目“长江口及其邻近海域不同盐度环境下沉积物硫酸盐还原及铁硫矿物的形成”（编号：16ZR1438200）资助.
Sedimentary Organic Carbon Mineralization and Its Contribution to the Marine Carbon Cycle in the Marginal Seas
Received date: 2018-10-30
Revised date: 2018-12-11
Online published: 2019-03-26
Supported by
Project supported by the National Natural Science Foundation of China “Organic matter diagenetic mineralization process and its contribution to pore water Dissolved Inorganic Carbon (DIC) in the sediments of Beibu Gulf, South China Sea”(No.41676061);The Shanghai Natural Science Foundation Project “Sulphate reduction and formation of iron and sulfur minerals under different salinity environments in the sediments of the Changjiang Estuary and its adjacent seas”(No. 16ZR1438200);Project supported by the National Natural Science Foundation of China “Organic matter diagenetic mineralization process and its contribution to pore water Dissolved Inorganic Carbon (DIC) in the sediments of Beibu Gulf, South China Sea” （No.41676061）; The Shanghai Natural Science Foundation Project “Sulphate reduction and formation of iron and sulfur minerals under different salinity environments in the sediments of the Changjiang Estuary and its adjacent seas” (No. 16ZR1438200).
张咏华 , 吴自军 . 陆架边缘海沉积物有机碳矿化及其对海洋碳循环的影响[J]. 地球科学进展, 2019 , 34(2) : 202 -209 . DOI: 10.11867/j.issn.1001-8166.2019.02.0202
Continental margin sediments are important ocean carbon repository, and the internal carbon cycle is mainly driven by the mineralization processes of sedimentary organic matter. Most organic carbon is transformed to Dissolved Inorganic Carbon (DIC) by mineralization processes after being delivered to continental margin sediments, and DIC from pore water diffuses into the upper water column and participates in the ocean carbon cycle. At the same time, some DIC combines ions such as Ca2+ and Mg2+ and precipitates as authigenic carbonate minerals so that carbon is stored in the deposits. Based on the biogeochemical study of the mechanism and efficiency of organic matter burial, we discussed the interaction among sulfate reduction, methanogenesis and anaerobic oxidation of methane, and the effect of organic mineralization on the formation of authigenic carbonate. By reviewing the above-mentioned aspects, we can obtain a better understanding of the role of continental margin sediments in the global carbon cycling budgets as well as its climate and environmental effects.
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