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A global transition to ferruginous conditions in the early Neoproterozoic oceans

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Figure

Fig. S1: Sample locations modified after Dong et al. (2008) and Tang et al. (2013). The upper part locates the study sites within the Rodinia supercontinent at ~900 Ma
Fig. S2: Sulphur isotope quality checks for the Liulaobei Fm. and the conformable Jiuliqiao and
Fig. S3: Sensitivity tests for deposition rates and δfigure). Plausible sulphate concentrations (i.e

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