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- W52557429 abstract "A key test for establishing the integrity of stable carbon isotope data from the mineral phase of fossil bones and teeth was the demonstration that only small differences existed between mean values for modern browsers and their fossil counterparts. The small difference increased with age; hence it was interpreted solely in terms of diagenesis. However, re-examination of the data suggests that the modern values used as references could themselves be anomalously depleted due to the effects on modern atmospheric CO2 of fossil fuel burning. Here carbon isotope results for animals of predictable diet at both ends of the carbon isotope “spectrum” are compared from sites with isotopically different depositional contexts and ages, in order to re-evaluate the effects of diagenesis. Where matrix carbonates are relatively enriched in 13C; the distinction between depleted browser values and enriched matrix material remains the most useful test, but where deposit carbonates are more depleted, the comparison between enriched grazers and depleted matrix values is more useful. The results for enamel and bone apatite of both browsers and grazers indicate that for about the first 100,000 years at least, isotopic differences observed between the modern and their fossil counterparts are attributable mainly to" @default.
- W52557429 created "2016-06-24" @default.
- W52557429 creator A5040652620 @default.
- W52557429 date "2006-01-17" @default.
- W52557429 modified "2023-10-17" @default.
- W52557429 title "Preservation of Biogenic Carbon Isotopic Signals in Plio-Pleistocene Bone and Tooth Mineral" @default.
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- W52557429 doi "https://doi.org/10.1007/0-306-47194-9_5" @default.
- W52557429 hasPublicationYear "2006" @default.
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