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Paleomobility in the Tiwanaku Diaspora

Biogeochemical analyses at R io M uerto, M oquegua, P eru

Bibliographic Data

ID8316352
AuthorsK J Knudson (0000-0002-2885-6228, Arizona State University, corresponding author), P S Goldstein (0000-0002-4431-6731, University of California San Diego, corresponding author), Allisen C Dahlstedt (0000-0003-0567-0049, Arizona State University), Allisen Dahlstedt (Center for Bioarchaeological Research, School of Human Evolution and Social Change, Arizona State University Tempe AZ 85287), A D Somerville (0000-0003-4839-2739, University of California San Diego), Andrew Somerville (Department of Anthropology University of California at San Diego La Jolla CA 92093), Margaret J Schoeninger (Department of Anthropology University of California at San Diego La Jolla CA 92093)
Year2014
Volume155
Issue3
Pages405-421
Publication date2014-11-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueAmerican Journal of Physical Anthropology (JOURNAL)
Journal identifiersISSN: 0002-9483 • E-ISSN: 1096-8644
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ajpa.22584
PMID25066931
OpenAlexW1854309918
LanguageEN
Citations received47
References cited89

Paleomobility has been a key element in the study of the expansion of ancient states and empires, including the Tiwanaku polity of the South Central Andes (AD 500–1000). We present radiogenic strontium and oxygen isotope data from human burials from three cemeteries in the Tiwanaku‐affiliated Middle Horizon archaeological site complex of Rio Muerto in the Moquegua Valley of southern Peru. At Rio Muerto, archaeological human enamel and bone values range from 87 Sr/ 86 Sr = 0.70657–0.72018, with a mean of 87 Sr/ 86 Sr = 0.70804 ± 0.00207 (1σ, n = 55). For the subset of samples analyzed for oxygen isotope values ( n = 48), the data ranges from δ 18 O carbonate(VSMOW) = +18.1 to +27.0‰. When contextualized with other lines of archaeological evidence, we interpret these data as evidence for an archaeological population in which the majority of individuals had “local” origins, and were likely second‐generation, or more, immigrants from the Tiwanaku heartland in the altiplano . Based on detailed life history data, we argue a smaller number of individuals came at different ages from various regions within the Tiwanaku polity. We consider whether these individuals with isotopic values consistent with “nonlocal” geographic origins could represent first‐generation migrants, marriage exchange partners, or occupationally mobile herders, traders or other travelers. By combining isotopic life history studies with mortuary treatment data, we use a person‐centered migration history approach to state integration and expansion. Isotopic analyses of paleomobility at the Rio Muerto site complex contribute to the role of diversity in ancient states by demonstrating the range of geographic origins rather than simply colonists from the Lake Titicaca Basin. Am J Phys Anthropol 155:405–421, 2014. © 2014 Wiley Periodicals, Inc

Archaeology · Geography · Polity · Population · Sociology · Archaeology and ancient environmental studies · Demography · Forensic Anthropology and Bioarchaeology Studies · Pacific and Southeast Asian Studies

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Unique citing works47
Citations per year3,92
Citation span2014 - 2026 (13)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 46

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