What was Earth's atmosphere like at different times in the past? Studies of sulphate-rich rocks, which are found to contain an unusual oxygen-isotope signature derived from chemical interactions in the atmosphere, may provide a new tool to tackle the question.
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References
Bao, H. et al. Nature 406, 176–178 (2000).
Urey, H. C. J. Chem. Soc. 562–581 ( 1947).
Thiemens, M. H. & Heidenreich, J. E. Science 219, 1073–1075 ( 1983).
Mauersberger, K. Geophys. Res. Lett. 8, 935–937 (1981).
Thiemens, M. H. Science 283, 341–345 ( 1999).
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Clayton, R. Rock signature from the sky. Nature 406, 136–137 (2000). https://doi.org/10.1038/35018193
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DOI: https://doi.org/10.1038/35018193