环境化学
针铁矿
缺氧水域
甲烷
产甲烷
化学
碳酸盐
甲烷厌氧氧化
菱铁矿
铁酸盐
吸附
有机化学
作者
Edgardo I. Valenzuela,Karen A. Avendaño,Nagamani Balagurusamy,Sonia Arriaga,César Nieto-Delgado,Frédèric Thalasso,Francisco J. Cervantes
标识
DOI:10.1016/j.scitotenv.2018.09.388
摘要
Key pathways for the anaerobic oxidation of methane (AOM) have remained elusive, particularly in organic rich ecosystems. In this work, the occurrence of AOM driven by humus-catalyzed dissimilatory iron reduction was investigated in sediments from a coastal mangrove swamp. Anoxic sediment incubations supplied with both goethite (α-FeOOH) and leonardite (humic substances (HS)) displayed an average AOM rate of 10.7 ± 0.8 μmol CH4 cm−3 day−1, which was 7 and 3 times faster than that measured in incubations containing only goethite or HS, respectively. Additional incubations performed with 13C-methane displayed Pahokee Peat HS-mediated carbonate precipitation linked to 13CH4 oxidation and ferrihydrite reduction (~1.3 μmol carbonate cm−3 day−1). These results highlight the role of HS on mitigating greenhouse gases released from wetlands, not only by mediating the AOM process, but also by enhancing carbon sequestration as inert minerals (calcite, aragonite and siderite).
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