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An oscillating trend in Phanerozoic non-skeletal carbonate mineralogy

Nature volume 305, pages 19–22 (1983)Cite this article

Abstract

Textural and compositional data on ancient ooids and cements suggest the existence of an oscillating Phanerozoic temporal trend in non-skeletal carbonate mineralogy. The trend shows good correlation with eustatic–climatic oscillations proposed by others. The most likely mechanism appears to be plate-tectonically influenced oscillations in PCO2, the vapour pressure of CO2, rather than change in oceanic Mg/Ca ratio.

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Authors and Affiliations

  1. Department of Geology, University of Illinois, Urbana, Illinois, 61801, USA

    Philip A. Sandberg

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  1. Philip A. Sandberg
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Sandberg, P. An oscillating trend in Phanerozoic non-skeletal carbonate mineralogy. Nature 305, 19–22 (1983). https://doi.org/10.1038/305019a0

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