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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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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DOI: https://doi.org/10.1038/305019a0
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