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Secular variation in carbon isotope ratios from Upper Proterozoic successions of Svalbard and East Greenland

Nature volume 321, pages 832–838 (1986)Cite this article

Abstract

Analyses of stratigraphically continuous suites of samples from Upper Proterozoic sedimentary successions of East Greenland, Spitsbergen and Nordaustlandet (Svalbard) provide an approximation to the secular variation in carbon isotope ratios during a geologically and biologically important period of change from around 900 million years ago to the beginning of the Cambrian period. Late Riphean carbonates and organic material show a stratigraphically useful pattern of enrichment in 13C relative to Phanerozoic or earlier Proterozoic samples. Isotopic compositions of isolated samples from other localities are consistent with a worldwide extended interval of enhanced organic burial and consequent net survival of oxidized material, probably O2, just before the initial radiation of metazoans.

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Author information

Authors and Affiliations

  1. Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, 02138, USA

    A. H. Knoll

  2. Biogeochemical Laboratories, Department of Chemistry and Geology, Indiana University, Bloomington, Indiana, 47405-5101, USA

    J. M. Hayes & A. J. Kaufman

  3. Department of Geology, University of Iowa, Iowa City, Iowa, 52242, USA

    K. Swett

  4. Baas Becking Geobiological Laboratory, PO Box 378, Canberra, ACT, 2601, Australia

    I. B. Lambert

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  1. A. H. Knoll
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  4. K. Swett
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  5. I. B. Lambert
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Knoll, A., Hayes, J., Kaufman, A. et al. Secular variation in carbon isotope ratios from Upper Proterozoic successions of Svalbard and East Greenland. Nature 321, 832–838 (1986). https://doi.org/10.1038/321832a0

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