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DOIhttps://doi.org/10.1594/PANGAEA.855634
Pore water and sediment geochemistry of the Bothian Sea
Egger; Matthias; Rasigraf; Olivia; Sapart; Célia-Julia; Jilbert; Tom; Jetten; Mike S M; Röckmann; Thomas; van der Veen; Carina; Bânda; Narcisa; Kartal; Boran; Ettwig; Katharina; Slomp; Caroline P
发布日期2015-12-07
数据集类型dataset
英文简介Methane is a powerful greenhouse gas and its biological conversion in marine sediments, largely controlled by anaerobic oxidation of methane (AOM), is a crucial part of the global carbon cycle. However, little is known about the role of iron oxides as an oxidant for AOM. Here we provide the first field evidence for iron-dependent AOM in brackish coastal surface sediments and show that methane produced in Bothnian Sea sediments is oxidized in distinct zones of iron- and sulfate-dependent AOM. At our study site, anthropogenic eutrophication over recent decades has led to an upward migration of the sulfate/methane transition zone in the sediment. Abundant iron oxides and high dissolved ferrous iron indicate iron reduction in the methanogenic sediments below the newly established sulfate/methane transition. Laboratory incubation studies of these sediments strongly suggest that the in situ microbial community is capable of linking methane oxidation to iron oxide reduction. Eutrophication of coastal environments may therefore create geochemical conditions favorable for iron-mediated AOM and thus increase the relevance of iron-dependent methane oxidation in the future. Besides its role in mitigating methane emissions, iron-dependent AOM strongly impacts sedimentary iron cycling and related biogeochemical processes through the reduction of large quantities of iron oxides.
空间范围Latitude: 62.586200 * Longitude: 19.968800
语种英语
国家国际
学科大类气候变化
学科子类气候变化
文献类型数据集
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/215426
推荐引用方式
GB/T 7714
Egger,Matthias,Rasigraf,et al. Pore water and sediment geochemistry of the Bothian Sea.2015-12-07.https://doi.org/10.1594/PANGAEA.855634.
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