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Sea change for the rise of oxygen

A model proposes that falling sea levels shifted the make-up of volcanic gases on the early Earth, triggering a chain of events that may have allowed photosynthesis in the ocean to oxygenate the atmosphere. See Letter p.229

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Figure 1: Sulphur isotopic data through Earth's history.

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Correspondence to Timothy W. Lyons or Christopher T. Reinhard.

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Lyons, T., Reinhard, C. Sea change for the rise of oxygen. Nature 478, 194–195 (2011). https://doi.org/10.1038/478194a

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