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Land use and mobility during the Neolithic in Wales explored using isotope analysis of tooth enamel.
Neil, Samantha; Montgomery, Janet; Evans, Jane; Cook, Gordon T; Scarre, Chris.
Afiliación
  • Neil S; Department of Archaeology, Durham University, South Road, Durham, DH1 3LE, United Kingdom.
  • Montgomery J; Department of Archaeology, Durham University, South Road, Durham, DH1 3LE, United Kingdom.
  • Evans J; NERC Isotope Geosciences Laboratory, Keyworth, Nottingham, NG12 5GG, United Kingdom.
  • Cook GT; Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, G75 0QF, United Kingdom.
  • Scarre C; Department of Archaeology, Durham University, South Road, Durham, DH1 3LE, United Kingdom.
Am J Phys Anthropol ; 164(2): 371-393, 2017 10.
Article en En | MEDLINE | ID: mdl-28752654
OBJECTIVES: The nature of land use and mobility during the transition to agriculture has often been debated. Here, we use isotope analysis of tooth enamel from human populations buried in two different Neolithic burial monuments, Penywyrlod and Ty Isaf, in south-east Wales, to examine patterns of land use and to evaluate where individuals obtained their childhood diet. MATERIALS AND METHODS: We employ strontium (87 Sr/86 Sr) and oxygen (δ18 O) and carbon (δ13 C) isotope analysis of enamel from adjacent molars. We compare strontium isotope values measured in enamel to locally bioavailable 87 Sr/86 Sr values. We combine discussion of these results with evaluation of new radiocarbon dates obtained from both sites. RESULTS: The majority of enamel samples from Penywyrlod have strontium isotope ratios above 0.7140. In contrast, the majority of those from Ty Isaf have 87 Sr/86 Sr values below 0.7140. At Penywyrlod oxygen isotope ratios range between 25.9 and 28.2 ‰ (mean 26.7 ± 0.6 ‰, 1σ, n = 15) and enamel δ13 Ccarbonate values range between -18.0 and -15.0 ‰ (mean -16.0 ± 0.8 ‰, 1σ, n = 15). At Ty Isaf oxygen isotope ratios exhibited by Neolithic individuals range between 25.4 and 27.7 ‰ (mean 26.7 ± 0.6 ‰, 1σ, n = 15) and enamel δ13 Ccarbonate values range between -16.9 and -14.9 ‰ (mean -16.0 ± 0.6 ‰, 1σ, n = 15). DISCUSSION: The strontium isotope results suggest that the majority of individuals buried at Penywyrlod did not source their childhood diet locally. One individual in this group has strontium isotope ratios that exceed all current known biosphere values within England and Wales. This individual is radiocarbon dated to the first few centuries of the 4th millennium BC, consistent with the period in which agriculture was initiated in Wales: the results therefore provide evidence for migration during the transition to farming in Wales. In contrast, all individuals sampled from Ty Isaf post-date the period in which agriculture is considered to have been initiated and could have sourced their childhood diet from the local region in which they were buried.
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Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Esmalte Dental / Agricultura / Dieta / Migración Humana Límite: Adolescent / Adult / Child / Child, preschool / Humans País/Región como asunto: Europa Idioma: En Revista: Am J Phys Anthropol Año: 2017 Tipo del documento: Article País de afiliación: Reino Unido

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Esmalte Dental / Agricultura / Dieta / Migración Humana Límite: Adolescent / Adult / Child / Child, preschool / Humans País/Región como asunto: Europa Idioma: En Revista: Am J Phys Anthropol Año: 2017 Tipo del documento: Article País de afiliación: Reino Unido