
Subduction's Hidden Role in Earth's Oxygen-Breathing Atmosphere
A new study ties Earth’s oxygen buildup to the subduction of carbon and sulfur: when subduction runs cooler, more C and S are carried into the mantle, later returning to the surface via volcanism and scavenging oxygen; warmer subduction releases more of these elements toward the surface, boosting atmospheric O2. The timing matches major oxygenation events (Great Oxygenation ~2.4–2.0 Ga and later boosts) and tracks with the cooling Earth and supercontinent cycles (Columbia, Gondwana, Pangaea). The findings suggest oxygen levels result from a complex interplay of biology, deep Earth chemistry, and plate tectonics.













