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Microbial methane oxidation is an important process because it drastically limits the release of this dangerous...

Microbial methane oxidation is an important process because it drastically limits the release of this dangerous greenhouse gas. A group of microbiologists used enrichment cultures of archaea from sediments to obtain two isolates. One oxidized CH4 to CO2 using NO3 as an electron acceptor to generate N2. The other isolate reduced Fe(III) to Fe(II) during methane oxidation. If you mixed the two isolates with equal amounts of nitrate and Fe(III), which methane-oxidizing archaeon do you think would grow fastest? Why?

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Answer: Fe reducing microbes will grow faster and oxidized the methane very quickly as compared to NO3- reducing species. Because, reduction potential of Fe(+3) to Fe(+2) is +0.74 V but reduction potential of conversation of NO3- to N2 is 1.38 V. Reduction of Fe(+3) is easy and achieve with low potential difference. On the other hand, only single methane will oxidized with reduction of single NO3- molecules. But in other case, for oxidation of 1 methane molecules, 4 molecules of Fe(+3) will reduced. Hence, Fe reducing strain will grow fast in consortium.

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