28 July 2026|IfGeo-en
How oxygen found its way into the atmosphere: from rocks on land to the ocean floor
Archive of the iron/oxygen cycle: This black shale from the Late Devonian, a period within the Paleozoic, is a form of sedimentary rock that reflects paleo-environmental conditions.
More iron on the seafloor means less oxygen in the ocean and atmosphere – or at least, that has long been a common assumption in the...