Dark oxygen
Four kilometers down in the Pacific, on a plain that never sees light, the seafloor is scattered with lumps of metal the size of potatoes. Manganese, mostly, with iron and nickel and cobalt, grown over millions of years a few millimeters at a time around a fleck of shell or shark tooth. Polymetallic nodules. They’re what the deep-sea mining industry wants. A couple of years ago a team sealed chambers over patches of this seafloor and watched the oxygen inside go up. Not down, the way it should in a closed box full of things that breathe — up, to three times the background level in two days. The proposed explanation is that the nodules act like little batteries. Measured across two of them sitting near each other: about 0.95 volts. It takes around 1.4 to split seawater into hydrogen and oxygen, and clustered nodules might get there. Oxygen, the thing we file under sunlight and photosynthesis and the surface, being made in total darkness by rocks. The first author says he spent years assuming his instruments were broken before he let himself believe it. ...