Palaeoatmospheric argon in Rhynie chert (original) (raw)

Nature volume 268, pages 38–41 (1977)Cite this article

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

  1. PETER H. CADOGAN
    Present address: , 100 Ryeworth Road, Charlton Kings, Cheltenham, UK

Authors and Affiliations

  1. 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

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