Vast stores of methane gas lie buried beneath the seafloor, yet little escapes from the sediments into the ocean and the atmosphere above. Geochemists have long suspected that methane-munching microbes gobble the gas before it can seep upward out of the ooze. But scientists had been at a loss to explain how a microorganism could consume methane where oxygen is in short supply, as it is in the sediments.
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