Methane, a chemical compound with the molecular formula CH4, is not only a powerful greenhouse gas, but also an important energy source. It heats our homes, and even seafloor microbes make a living of it. The microbes use a process called anaerobic oxidation of methane (AOM), which happens commonly in the seafloor in so-called sulfate-methane transition zones—layers in the seafloor where sulfate from the seawater meets methane from the deeper sediment. Here, specialized microorganisms, the ANaerobically MEthane-oxidizing (ANME) archaea, consume the methane. They live in close association with bacteria, which use electrons released during methane oxidation for sulfate reduction. For this purpose, these organisms form characteristic consortia.
Click here for original story, Strange isotopes: Scientists explain a methane isotope paradox of the seafloor
Source: Phys.org