Photoferrotrophic Bacteria Initiated Plate Tectonics in the Neoarchean
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Researchers suggest that about 2 1/2 billion years ago, bacteria caused iron to precipitate out of the oceans, depositing 1 km of heavy rock layers every million years. It eventually punched through Earth’s crust and initiated the plate tectonic cycle. Since then, plate tectonics has helped to stabilize Earth’s climate.