Abstract
NATURALLY occurring carbon shows considerable variability with respect to its stable isotope composition. The 13C/12C ratio in plant material (and in ancient residues) is generally roughly 2.5% lower than in the carbonate of marine limestones as a result of fractionation during photosynthesis. A summary of carbon isotope distribution and fractionation is given by Degens1.
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References
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CURTIS, C., PETROWSKI, C. & OERTEL, G. Stable Carbon Isotope Ratios within Carbonate Concretions: a Clue to Place and Time of Formation. Nature 235, 98–100 (1972). https://doi.org/10.1038/235098a0
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DOI: https://doi.org/10.1038/235098a0
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