There are no good models for the chemical evolution of the Earth’s surface over the planet’s lifetime, because models typically overlook the progressive build-up of carbonate rocks in the crust. A new model that includes this accumulation enables the reconstruction of major oxygen and temperature trends throughout Earth’s history.
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References
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This is a summary of: Alcott, L. J. et al. Crustal carbonate build-up as a driver for Earth’s oxygenation. Nat. Geosci. https://doi.org/10.1038/41561-024-01417-1 (2024).
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Evolution of Earth’s oxygenation and temperature depends on surface carbonate accumulation. Nat. Geosci. (2024). https://doi.org/10.1038/s41561-024-01429-x
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DOI: https://doi.org/10.1038/s41561-024-01429-x
