Abstract:Hydrogen sulfide (H2S) is produced in a wide range of anoxic environments where sulfate (SO42−) reduction is coupled to decomposition of organic matter. In the same environments, methane (CH4) is the end product of an anaerobic food chain and both H2S and CH4 diffuse upwards into oxic zones where aerobic microorganisms can utilize these gases. Methane-oxidizing bacteria are known to oxidize a major part of the produced CH4 in these ecosystems, mitigating the emissions of this potent greenhouse gas to the atmos… Show more
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