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| Photo Credit: Walter Frehner |
A new study reveals that methane can form in the upper layers of sandy seabeds — something that has taken scientists by surprise. Special microorganisms are at work, and the phenomenon may be happening along coastlines all over the world.
Methane is a powerful greenhouse gas, produced in many natural environments by microorganisms.
Until recently, scientists believed these microbes were intolerant of oxygen and could only survive in oxygen-free zones. But new research shows they can, in fact, persist in oxygenated environments — lying dormant until the oxygen disappears. That means an entirely new source of methane emissions has just been discovered.
“We do not yet know how much methane these microbes are producing. That is the next big question. But we suspect the contribution is significant and widespread in sandy coastal zones. This is not something confined to a few isolated spots on the globe,” says Ronnie N. Glud, professor at the Department of Biology and an expert in biogeochemistry.

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