原文服务方: 地球化学学报(英文)       
摘要:
The Earth surface contains various oxic and anoxic environments. The later include natural wetlands, river and lake sediments, paddy field soils and landfills. In the last few decades, the biogeochemical cycle of carbon in anoxic environments, which leads to the production and emission of methane, a potent greenhouse gas in the atmosphere, has drawn great attentions from both scientific and public sectors. New organisms and mechanisms involved in methanogenesis and carbon cycling have been uncovered. Interspecies electron transfer is considered as a crucial step in methanogenesis in anoxic environments. Electron-carrying mediators, like H2 and formate, are known to play the key role in electron transfer. Recently, it has been found that in addition to the conventional electron transfer via chemical mediators, direct interspecies electron transfer (DIET) can occur. In this Review, we describe the ecology and biogeochemistry of methanogenesis and highlight the effect of microbe-mineral interaction on microbial syntrophy. Recent advances in the study of DIET may pave the way towards a mechanistic understanding of methanogenesis and the influence of microbe-mineral interaction on this process.
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篇名 Biogeochemistry of methanogenesis with a specific emphasis on the mineral-facilitating effects
来源期刊 学科 地球科学
关键词 Syntrophy Methanogenesis Direct interspecies electron transfer Magnetite Wetland Paddy fields
年,卷(期) 2022,(3) 所属期刊栏目
研究方向 页码范围 379-384
页数 5页 分类号
字数 语种 英文
DOI 10.1007/s11631-017-0168-0
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研究主题发展历程
节点文献
Syntrophy
Methanogenesis
Direct interspecies electron transfer
Magnetite
Wetland
Paddy fields
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研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
出版文献量(篇)
230
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0
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0
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