Something at the Bottom of the Pacific Is Making Oxygen in the Dark
Four kilometers below the surface, far past the reach of sunlight, the seafloor of the Clarion-Clipperton Zone appears to be producing oxygen. The leading explanation is that the metallic lumps littering the mud act like tiny natural batteries, splitting seawater into hydrogen and oxygen. If it holds up, it dents a textbook assumption that all of Earth's free oxygen comes from photosynthesis.