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Updated: Apr 11, 2026

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Decoding Redox Evolution Before Oxygenic Photosynthesis Based on the Sulfur-Mass Independent Fractionation (S-MIF)
Yuichiro Ueno1, Sebastian Danielache, Naohiro Yoshida
1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 152-8551, Japan, ueno.y.ac@m.titech.ac.jp.
Abstract:
The isotopic anomaly of stable sulfur isotope could be a useful new tracer for decoding atmospheric chemistry of early Earth from ancient rock samples. Here, we summarize current status of the experimental works and discuss what the isotopic anomaly tells about early Earth's atmosphere.
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