Henry Scott of Indiana University in South Bend and colleagues at the Carnegie Institution in Washington, Harvard University and the Lawrence Livermore National Lab subjected materials commonly found in the Earth’s crust to temperatures of up to 1500°C and pressures as high as 11 gigapascals (Proc. Natl. Acad. Sci. to be published). These conditions are similar to those found in the Earth’s upper mantle…

However, Scott is more cautious about his team’s results. “Although I believe the Earth’s mantle could contain a significant quantity of even heavier hydrocarbons, I cannot constrain how much of this reaches the Earth’s surface, or the extent to which it may augment resources that we exploit commercially,” he told PhysicsWeb. “I do not want to suggest in any way that these hydrocarbons are likely to represent an untapped energy reserve.”

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