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. 2012 Sep 4;109(38):15146-15151. doi: 10.1073/pnas.1207491109

Fig. 3.

Fig. 3.

Sulfur isotopic compositions of kerogen and sulfide minerals present within SPF stromatolites. Histograms represent δ34S values measured with two ion probes from acid extracts, in situ from six different regions of the stromatolite (Fig. 2), and in situ from pyrite crystals (Fig. S4).