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- W2047394759 abstract "The carbon and oxygen isotopic composition of CO2 evolved from the apatite fraction of bones from freshly killed deer, and the carbon isotopic composition of bone collagen is controlled by environmental factors. Deer from high latitudes have δ 13CCO2 values of about −15‰ relative to PDB and δ 18OCO2 values of about −3‰. A fairly constant difference (Δ) of about 8‰ exists between δ 13C collagen and δ 13CCO2, and the bones all contain about 3.4 wt.% CO2. Deer from more arid areas are systematically enriched in both 13C and 18O, but Δ values and the amount of CO2 in the bones are unaffected. Most Pleistocene deer bones we have analyzed have isotopic compositions inconsistent with recent kills despite the fact that the weight % CO2 in the bone (after leaching with acetic acid to remove calcite) and X-ray diffraction data are unchanged. In most cases the CO2 derived from apatite is unsuitable for paleoecologic or 14C age determinations, and in several cases the δ 13C of collagen appears to have been altered as well." @default.
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- W2047394759 date "1980-01-01" @default.
- W2047394759 modified "2023-10-16" @default.
- W2047394759 title "Isotopic ecology of deer bones" @default.
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- W2047394759 doi "https://doi.org/10.1016/0031-0182(80)90037-1" @default.
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