In marine ecology, dietary interpretations of faunal assemblages often rely on nitrogen isotopes as the main or only applicable trophic level tracer. We investigate the geographic variability and trophic level… Click to show full abstract
In marine ecology, dietary interpretations of faunal assemblages often rely on nitrogen isotopes as the main or only applicable trophic level tracer. We investigate the geographic variability and trophic level isotopic discrimination factors of bone zinc 66 Zn/ 64 Zn ratios (δ 66 Zn value) and compared it to collagen nitrogen and carbon stable isotope (δ 15 N and δ 13 C) values. Focusing on ringed seals ( Pusa hispida ) and polar bears ( Ursus maritimus ) from multiple Arctic archaeological sites, we investigate trophic interactions between predator and prey over a broad geographic area. All proxies show variability among sites, influenced by the regional food web baselines. However, δ 66 Zn shows a significantly higher homogeneity among different sites. We observe a clear trophic spacing for δ 15 N and δ 66 Zn values in all locations, yet δ 66 Zn analysis allows a more direct dietary comparability between spatially and temporally distinct locations than what is possible by δ 15 N and δ 13 C analysis alone. When combining all three proxies, a more detailed and refined dietary analysis is possible. McCormack et al. present the first comparison of archaeological δ66Zn from bone material compared with traditional δ15 N and δ13 C values derived from collagen samples over a large geographic area. This study shows that the inclusion of δ66Zn analysis can provide otherwise inaccessible supplementary dietary information and more robust trophic level estimations.
               
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