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. 2017 Mar 13;114(13):E2571–E2579. doi: 10.1073/pnas.1618798114

Fig. S1.

Fig. S1.

Geological map of the Transvaal Supergroup preserved on the Kaapvaal Craton with a geographical insert, modified from refs. 53 and 68. The position of cores where Δ36S/Δ33S–δ13C covariation has been previously reported (core GKF01, ref. 9; core BH1-Sacha, ref. 8) is indicated by labeled stars. Additionally the extra Agouron core (GKP01) that we discuss below in terms of chronological constraints is also given. The shallow-water Ghaap plateau facies are separated from their deep-water equivalents by the fault at Griquatown (GFZ; refs. 37 and 53), hence the different stratigraphic nomenclature between Zerkle et al. (9) and Izon et al. (8).