Fig. 3: Output of our S-cycling box-model. | Nature Communications

Fig. 3: Output of our S-cycling box-model.

From: Sulfate triple-oxygen-isotope evidence confirming oceanic oxygenation 570 million years ago

Fig. 3

Driven forces: changes in a coefficient kmsr of MSR (microbial sulfate reduction) flux in the water-column, b fraction of H2S-reoxidized during the MSR, c proportion of aerobic oxidation during H2S reoxidation, and d added sulfate flux from oxidation of the pre-existing sulfur pool. Model results: e seawater sulfate δ34S, f seawater sulfate δ18O, g seawater sulfate ∆′17O, and h seawater sulfate concentration. The initial steady states with sulfate concentration of 0.5 mM (SS4-2, see Supplementary Table 3) and 1.1 mM (SS8-2) were adopted as suggested72,73.

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