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Proterozoic seawater sulfate scarcity and the evolution of ocean–atmosphere chemistry

Abstract.

"Oceanic sulfate concentrations are widely thought to have reached millimolar levels during the Proterozoic Eon, 2.5 to 0.54 billion years ago. Yet the magnitude of the increase in seawater sulfate concentrations over the course of the Eon remains largely unquantified. A rise in seawater sulfate concentrations has been inferred from the increased range of marine sulfide δ34S values following the Great Oxidation Event and was induced by two processes: enhanced oxidative weathering of sulfides on land, and the onset of marine sulfur redox cycling. [...]"

Source: Nature Geoscience
Authors: Mojtaba Fakhraee et al.
DOI: 10.1038/s41561-019-0351-5

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