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Decade-Long Geology Project Rewrites Origins of Earth's Methane

Explore abiotic methane formation and its implications for energy, nature, and even extraterrestrial life.

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Methane bubbles up from below a lake. (Credit: Strelyuk/Shutterstock) Turkey’s Mount Chimaera is on fire, and has been for millennia. Dozens of campfire-sized flames burst straight of the mountain’s rocky, sea-facing slope. These eternal flames are fueled by methane, the odorless, colorless substance that provides much of our natural gas for fuel, as well as a potent greenhouse gas. Most methane (a single carbon atom surrounded by four hydrogens) forms from the decay of ancient plants, animals and other life. But the Earth itself can create methane, too. When water reacts with a mineral called olivine in certain types of rocks, it releases hydrogen gas. This hydrogen reacts with a carbon source like carbon dioxide to form methane. Scientists call this kind of methane “abiotic” because it can happen without any lifeforms present. And scientists are finding more and more of it, researchers announced Monday. What's more, they've also discovered ...

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