Palaeoatmospheric argon in Rhynie chert (original) (raw)
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- Published: 01 July 1977
Nature volume 268, pages 38–41 (1977)Cite this article
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Abstract
THE isotopic compositions and relative abundances of rare gases in the Earth's atmosphere impose rigid constraints on models of atmospheric evolution. Appreciable quantities of argon from the Devonian atmosphere have been extracted from silicified fossil plants and the isotopic composition of this argon implies that the Earth must have been strongly outgassed early in its history.
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Author notes
- PETER H. CADOGAN
Present address: , 100 Ryeworth Road, Charlton Kings, Cheltenham, UK
Authors and Affiliations
- Department of Physics, University of Sheffield, Sheffield, UK
PETER H. CADOGAN
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CADOGAN, P. Palaeoatmospheric argon in Rhynie chert.Nature 268, 38–41 (1977). https://doi.org/10.1038/268038a0
- Received: 17 February 1977
- Accepted: 16 May 1977
- Published: 01 July 1977
- Issue date: 07 July 1977
- DOI: https://doi.org/10.1038/268038a0