Comment on "Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state"
- PMID: 16410508
- DOI: 10.1126/science.311.5758.177
Comment on "Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state"
Abstract
Rouxel et al. (Reports, 18 February 2005, p. 1088) argued that changes in the iron isotopic composition of sedimentary sulfides reflect changes in the oxidation state of the atmosphere-ocean system between 2.3 and 1.8 million years ago. We show that misinterpretations of the origins of these minerals undermine their conclusions.
Comment on
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Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state.Science. 2005 Feb 18;307(5712):1088-91. doi: 10.1126/science.1105692. Science. 2005. PMID: 15718467
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