4.5 Article

Stable isotope ratio analysis of bone collagen as indicator of different dietary habits and environmental conditions in northeastern Iberia during the 4th and 3rd millennium cal BC

期刊

ARCHAEOLOGICAL AND ANTHROPOLOGICAL SCIENCES
卷 11, 期 8, 页码 3931-3947

出版社

SPRINGER HEIDELBERG
DOI: 10.1007/s12520-018-0657-z

关键词

Sepulchral caves; Late Neolithic-Chalcolithic; Carbon and nitrogen isotopes; Cova de la Guineu; Cueva de Abauntz

资金

  1. Gobierno de Aragon
  2. Fondo Social Europeo [BOA20150701025]
  3. Fundacion Ibercaja-CAI
  4. DCSG's UCT
  5. BBVA research grants
  6. Transiciones climaticas y adaptaciones sociales en la prehistoria de la Cuenca del Ebro [HAR2014-59042-P]
  7. Basque Goverment
  8. [HAR2014-53536-P]
  9. [IT-662-13]

向作者/读者索取更多资源

The Late Neolithic and Chalcolithic periods are poorly understood in northeastern Iberia. Most of the information comes from the sepulchral structures rather than habitat settlements. The high number of individuals usually recovered from this types of collective burial spaces, together with the low number of direct radiocarbon dates available on them, forces us to be cautious and consider all the studied assemblages as belonging to the so-called Late Neolithic-Chalcolithic time period. To evaluate human dietary patterns of the Late Neolithic-Chalcolithic populations from the northeast of Iberia, stable carbon and nitrogen isotope analysis was carried out on 78 humans and 32 faunal bones from Cova de la Guineu (Font-rubi, Barcelona) and Cueva de Abauntz (Arraitz, Navarra), both of them sepulchral sites. Results show a common dietary pattern in both sites, indicating an homogeneous protein diet based on C-3 terrestrial resources and no isotopic evidence of the consumption of C-4 plants. Only one individual from Cueva de Abauntz, who directly dates to the first moments of the use of the cave as a burial place, suggests a different protein intake. The inter-population analysis shows a significant difference between both human and faunal delta C-13 values, suggesting an environmental influence on the isotope values depending on the geographic location. This effect should not be discarded and always assessed with baseline isotopic values in future studies at each area of Iberia and for different chronological moments.

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