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. 2012 Mar 5;109(14):5180-5184. doi: 10.1073/pnas.1111784109

Fig. 3.

Fig. 3.

Plot of the isotopic composition of the pyrite sulfur (δ34S) in the fossiliferous portion of the Chengjiang from a new drill core extracted near Haikou town, Kunming, Yunnan Province, China. Event-deposited beds (blue diamonds) are characterized by heavy values [average +9.6 ± 2.0‰ (SEM)] that display less fractionation from Cambrian seawater (ca. +30‰; ref. 31) than background sediments [orange circles; average -6.0‰ ± 0.6‰ (SEM)].