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Shifting diet, shifting culture? A bioarchaeological approach to island dietary development on Iron‐Age Öland, Baltic Sea
Author(s) -
Wilhelmson Helene
Publication year - 2017
Publication title -
american journal of physical anthropology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.146
H-Index - 119
eISSN - 1096-8644
pISSN - 0002-9483
DOI - 10.1002/ajpa.23204
Subject(s) - subsistence agriculture , trophic level , chronology , typology , isotope analysis , domestication , geography , stable isotope ratio , iron age , land use , ecology , biology , archaeology , agriculture , physics , quantum mechanics
Objectives The diet and subsistence in Iron‐Age Öland is debated as earlier studies and different archaeological sources seemingly provide conflicting interpretations. The objectives of this study are therefore to: (i) add new insights on diet and (ii) investigate the chronological variation in detail. It is common in studies of diet to investigate differences between datasets defined by archaeological periods (determined by artefact typology), but it is rare to explore whether these dietary changes are, in fact, well correlated with these temporal categories or not. Materials and methods Stable isotope analysis of 108 individuals and 25 animals was used to interpret diet in comparison with data from earlier studies. Different values of TLE (Trophic Level Effect) for δ 15 N were compared for interpretations of diet. Of the 108 individuals, 42 were subjected to 14 C analysis in this study. Results The isotopes from Iron‐Age animals on Öland indicate that the local, contemporary ecology is specific. The human isotope values show chronological development both when pooled in chronological groups by typology and by more specific 14 C chronology. Discussion The new samples of animals as well as the use of 5‰ TLE for δ 15 N values results in the diet reinterpreted as mainly domesticate‐based, with at least two shifts in diet occurring in the Iron Age. The use of 14 C dates in connection with the stable isotope results indicates a dietary transition occurring between 200 BC and AD 200, a date range that spans two typologically determined time periods.