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Updated: Jul 6, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
Published on: July 24, 2016
Comment on "Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state"
Kosei E Yamaguchi1, Hiroshi Ohmoto
1Institute for Research on Earth Evolution (IFREE), Japan, Agency for Marine-Earth Science and Technology (JAMSTEC),2-15 Natsushima, Yokosuka 237-0061, Japan. kosei@jamstec.go.jp
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.
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