Does the Paleoproterozoic Animikie Basin record the sulfidic ocean transition?: COMMENT
Author(s) -
Philip Fralick,
Simon W. Poulton,
Donald E. Canfield
Publication year - 2011
Publication title -
geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.609
H-Index - 215
eISSN - 1943-2682
pISSN - 0091-7613
DOI - 10.1130/g31747c.1
Subject(s) - geology , structural basin , oceanic basin , oceanography , paleontology , geochemistry , earth science
[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],
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