Provisioning Inka feasts at Tiwanaku, Bolivia: the geographic origins of camelids in the Pumapunku complex |
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Authors: | Kelly J. Knudson Kristin R. GardellaJason Yaeger |
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Affiliation: | a Center for Bioarchaeological Research, School of Human Evolution and Social Change, Arizona State University, PO Box 872402, Tempe, AZ 85287, USA b Department of Anthropology, University of Pennsylvania, Philadelphia, PA 19104, USA c Department of Anthropology, University of Texas at San Antonio, San Antonio, TX 78249, USA |
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Abstract: | While political integration can be achieved by many means, here we focus on the use of feasting and statecraft in the Inka Empire of the Andean Late Horizon (c. AD 1400-1532) in South America. In order to examine Inka political integration of the Lake Titicaca Basin of Bolivia, we examine paleomobility and paleodiet through radiogenic strontium and stable oxygen and carbon isotope data in archaeological camelid remains from the site of Tiwanaku. Mean radiogenic strontium isotope values from all archaeological camelid enamel and bone samples is 87Sr/86Sr = 0.70998 ± 0.00179 (1σ, n = 48), mean stable oxygen isotope values from a sub-set of archaeological camelid enamel and bone samples is δ18Ocarbonate (VPDB) = −10.0‰ ± 2.6‰ (1σ, n = 18) and mean stable carbon isotope values from a sub-set of archaeological camelid enamel and bone samples is δ13Ccarbonate (VPDB) = −9.0‰ ± 1.7‰ (1σ, n = 18). While many camelids consumed in these feasting events were likely local to the Lake Titicaca Basin, others came from a variety of different geologic zones, elucidating our understanding of Inka statecraft and the role of feasting in political integration in empires in the past. |
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Keywords: | Andes Inca Late Horizon Middle Horizon Radiogenic strontium isotopes Stable carbon isotopes Stable oxygen isotopes |
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