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[Pufahl et al. (2010)][1] question the interpretation of data in [Poulton et al. (2004)][2], showing a transition from ferruginous to euxinic conditions on the continental shelf of a major ocean basin at ca. 1840 Ma. In contrast with [Poulton et al. (2004)][2] and also [Johnston et al. (2006)][3],

Does the Paleoproterozoic Animikie Basin record the sulfidic ocean transition?: COMMENT