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Stable Carbon and Oxygen Isotopes in Soils

  • Nordt L
Springer US, (2001), 419-448
DOI: 10.1007/978-1-4615-1183-0_15
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Abstract

The most common use of stable carbon (C) and oxygen (O) isotopes in archaeology is to infer paleodiet, artifact provenance, and paleoenvironment (Herz, 1990; Herz and Garrison, 1998).

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Nordt, L. C. (2001). Stable Carbon and Oxygen Isotopes in Soils. In Earth Sciences and Archaeology (pp. 419–448). Springer US. https://doi.org/10.1007/978-1-4615-1183-0_15

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