13C bioapatite-diet spacing, and not that of Δ
13C collagen-diet .
KEYWORDS: BIOMINERAL, ISOTOPE ANALYSIS, PALAEODIET, ISOTOPE ECOLOGY
INTRODUCTIONThe relationship between the carbon and nitrogen isotope composition of an individual's diet and their body tissues is now frequently employed as a method of dietary analysis in several different research fields, including ecology, archaeology and physiology (Gannes et al. 1998; Lee-Thorp 2008;Boecklen et al. 2011). The underlying basis of such work is that there is an isotopic 'fine structure' within the biosphere due to fractionation during natural processes, which results in isotopic differences between food types. An individual's diet can thus be inferred from the isotopic signature, which is transferred to and retained in the body during the absorption and incorporation of food.The interpretation of diet is predicated on understanding and therefore accounting for any isotopic fractionation resulting from the incorporation of diet into body tissues. Over the decades, there have been a number of empirical studies aimed at elucidating isotopic fractionation during the body's metabolism, yet some observed patterns remain puzzling. One such is the offset between the carbon isotopic values of the biomineral and protein components of bone. This study *Received 21 January 2016; accepted 24 March 2016 †Corresponding author: email tco21@cam.ac.uk Archaeometry 59, 2 (2017Archaeometry 59, 2 ( ) 302-315 doi: 10.1111 This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Krueger and Sullivan (1984) found a Δ 13 C ap-coll spacing of +7‰ for modern herbivores (n = 20), and +3-4‰ for modern carnivores (n = 40). Their analyses of over 200 archaeological humans showed that the majority had Δ 13 C ap-coll spacings of +3 to +7‰, as would be predicted for omnivores. In modern southern African wild fauna, Lee-Thorp et al. (1989) found that the Δ 13 C ap-coll was +6.8 ± 1.4‰ for herbivores (n = 67) and +4.3 ± 1.0‰ for carnivores (n = 49), with both groups having similar bioapatite δ C ap-coll between herbivores (+7.6 ± 0.5‰, n = 46) and carnivores (+4.8 ± 0.4‰, n = 27). Similar Δ 13 C ap-coll values have been found in a range of other ungulate herbivores (Schoeninger and DeNiro 1982;Nelson et al. 1986;Kellner and Schoeninger 2007). In predominately herbivorous primates, Crowley et al. (2010) observed a mean Δ
13C ap-coll of +5.6‰, with some variability (range of +3.6 to +8.6‰). Ambrose (1993) analysed East African historical human bone, and showed that the Δ
13C ap-coll of pastoralists (Kalenjin, Turkana, Pokot and Dasenech) was +3.8 ± 1.2‰ (n = 8), whereas the Δ 13 C ap-coll of Kikuyu farmers was +5.5 ± 0.5‰ (n = 16), supporting the theory that those humans with a diet high in animal protein have a smaller spacing between their collagen and bioapatite δ 13 C than predominantly plant-eating farmers. Although based on a limited number of...