Encyclopedia of Geoarchaeology

2017 Edition
| Editors: Allan S. Gilbert

Stable Carbon Isotopes in Soils

Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-4409-0_13

Definition

Stable isotopes of carbon (13C and 12C) in soil organic matter and in pedogenic carbonate provide a means of paleoenvironmental reconstruction because the ratio of these two isotopes is influenced by biological, physical, and chemical reactions. The C3 and C4 plant communities that produced the organic carbon can be identified isotopically based on the degree of discrimination against atmospheric 13CO2 during photosynthesis (the degree to which a plant favors carbon dioxide containing the lighter 12CO2 isotope).

Introduction

The distribution of stable C isotopes in surface and buried soils is a powerful indicator of many kinds of pedologic and paleoenvironmental interpretations. Stable C isotope analysis of soil organic matter is commonly employed to quantify organic matter turnover rates (Balesdent and Mariotti, 1996; Bernoux et al., 1998) and to reconstruct past vegetation communities (Cerling, 1992; Cerling et al., 1993; Kelly et al., 1993; Wang et al., 1993; Nordt...

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Copyright information

© Springer Science+Business Media Dordrecht 2017

Authors and Affiliations

  1. 1.Department of GeologyBaylor UniversityWacoUSA
  2. 2.Anthropology and Departments GeosciencesUniversity of ArizonaTucsonUSA