Photosynthesis is the main source of oxygen in Earth's atmosphere. But it may have been geological activity that first allowed an oxygen-rich atmosphere to develop.
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References
Kump, L. R., Kasting, J. F. & Barley, M. E. Geochem. Geophys. Geosyst. (2001). http://146.201.254.53/publicationsfinal/researchletters/2000GC000114/fs2000GC000114.html
Langan, R. T. & Sleep, N. H. J. Geophys. Res. 87, 9225–9235 (1982).
Garrels, R. M. & Perry, E. A. Jr in The Sea Vol. 5 (ed. Goldberg, E. D.) 303–336 (Wiley, New York, 1974).
Godderis, Y. & Veizer, J. Am. J. Sci. 300, 434–461 (2000).
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Sleep, N. Oxygenating the atmosphere. Nature 410, 317–318 (2001). https://doi.org/10.1038/35066664
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DOI: https://doi.org/10.1038/35066664