Characterisation of methane production pathways in sediment of overwashed mangrove forests “2279

HIGHLIGHTS

SUMMARY

    Methanogenesis, or the production of methane in wetlands, is critical to the global carbon cycle. Warming temperatures cause more methanogens or methaneproducing microorganisms to proliferate, resulting in faster methanogenesis, with an optimum temperature range from 35 ◦ C to 42 ◦ C. Elevated CO2 concentrations in the atmosphere generally increase plant productivity, producing photosynthate and increasing root exudation, which increases the supply of organic substrates for consumption by methanogens. Numerous in situ studies have also shown that methylotrophic methanogens always coexist with the other methanogens and SRBs. Ramamurthy et_al initially described this phenomenon while looking into . . .

     

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