Abstract

Multi-tissue stable isotope models to reconstruct past diets (Froehle, Kellner, & Schoeninger, 2012; Kellner & Schoeninger, 2007) have lacked data from a heavily C4 -dependent population. Using new data from southern African agriculturalists, published models are evaluated for accuracy in dietary reconstruction and applicability to isotopically diverse diets. Additionally, isotopic variation between tooth enamel and bone apatite, which are often treated as isotopically equivalent, is investigated. δ13 Cbone apatite , δ13 Ctooth enamel , δ13 Ccollagen , and δ15 Ncollagen values for 51 adult southern African agriculturalists are presented. Bivariate (linear) and multivariate (cluster analysis, discriminant function analysis) models are recreated including these data, and the resulting dietary reconstructions evaluated against what we know of archaeological diets. Δ13 Ccollagen-enamel (5.67 ± 1.66‰) is significantly larger than Δ13 Ccollagen-bone apatite (4.77 ± 1.42‰) and are significantly different from each other (Mann Whitney U-Test, p = 0.0). δ13 Cbone apatite and δ13 Ctooth enamel were uncorrelated (R2 = 0.24). The agriculturalists consumed highly variable and heterogeneous diets, (mean δ13 Cbone apatite = -6.25 ± 2.49‰, δ13 Ctooth enamel = -2.88 ± 2.48‰, δ13 Ccollagen = -8.65 ± 2.16‰, δ15 Ncollagen = 10.05 ± 1.9‰). Multi- and bi-variate models under-estimate the probable contribution of C3 energy sources, and recreation of cluster analysis results in a significant reduction in the parsimony of the dietary clusters derived in Froehle et al., 2012. Bone apatite and tooth enamel are distinct biominerals, and their δ13 C values should not be treated as equivalent. Multiple tissue isotopes provide valuable insight into diet that cannot be achieved with single tissues, but current models are limited by the lack of isotopic diversity in the data on which they are based.

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