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- W2983125989 abstract "Abstract Microbial aerobic oxidation is known to be a significant sink of marine methane (CH 4 ), contributing to the relatively minor atmospheric release of this greenhouse gas over vast stretches of the ocean. However, the chemical kinetics of aerobic CH 4 oxidation are not well established, making it difficult to predict and assess the extent that CH 4 is oxidized in seawater following seafloor release. Here we investigate the kinetics of aerobic CH 4 oxidation using mesocosm incubations of fresh seawater samples collected from seep fields in Hudson Canyon, U.S. Atlantic Margin and MC118, Gulf of Mexico to gain a fundamental chemical understanding of this CH 4 sink. The goals of this investigation were to determine the response or lag time following CH 4 release until more rapid oxidation begins, the reaction order, and the stoichiometry of reactants utilized (i.e., CH 4 , oxygen, nitrate, phosphate, trace metals) during CH 4 oxidation. The results for both Hudson Canyon and MC118 environments show that CH 4 oxidation rates sharply increased within less than one month following the CH 4 inoculation of seawater. However, the exact temporal characteristics of this more rapid CH 4 oxidation varied based on location, possibly dependent on the local circulation and biogeochemical conditions at the point of seawater collection. The data further suggest that methane oxidation behaves as a first‐order kinetic process and that the reaction rate constant remains constant once rapid CH 4 oxidation begins." @default.
- W2983125989 created "2019-11-22" @default.
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- W2983125989 date "2019-12-01" @default.
- W2983125989 modified "2023-10-15" @default.
- W2983125989 title "Investigations of Aerobic Methane Oxidation in Two Marine Seep Environments: Part 1—Chemical Kinetics" @default.
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- W2983125989 doi "https://doi.org/10.1029/2019jc015594" @default.
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