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• W4226514239 abstract "Methane (CH 4 ) is an important component of aquatic carbon cycling. Methane production by methanogenic archaea in sediments can account for up to 56% of the total carbon mineralization and additional oxic CH 4 production in surface water have recently been suggested. Microbial oxidation of CH 4 , consumes a large proportion of the produced CH 4 . The CH 4 oxidation can be comparable to total heterotrophic bacterial production, or in some lakes even to primary production, and results in substantial formation of microbial biomass. Thereby, CH 4 has the potential to be a significant food web carbon source. The CH 4 oxidation also consumes O 2 , which in insolated water bodies can result in O 2 depletion and suffocation of aquatic animals. Still, large amounts of aquatic CH 4 escape oxidation and are emitted to the atmosphere where CH 4 acts as the second most important greenhouse gas (after CO 2 ). Globally, inland waters are among the largest sources of atmospheric CH 4 . This chapter reviews the roles of CH 4 in internal carbon cycling in inland waters as well as the link between aquatic CH 4 dynamics and global greenhouse gas emissions." @default.
• W4226514239 created "2022-05-05" @default.
• W4226514239 creator A5078790493 @default.
• W4226514239 date "2022-01-01" @default.
• W4226514239 modified "2023-09-25" @default.
• W4226514239 title "Methane" @default.
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