18 research outputs found

    Mobility in the Atacama Desert, northern Chile, in the Late Intermediate Period (AD 900–1450): A re-evaluation using stable isotope analysis

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    Research on the Late Intermediate Period (AD 900–1450) in northern Chile has been strongly influenced by two mobility models: John Murra's classic vertical ecological archipelago model, with highland colonies in the lowlands; and the gyratory mobility model, with pastoralists and their llama caravans controlling trade. The widespread application of these two models, however, suffers from a lack of supporting archaeological evidence. Stable isotope analysis provides a more direct approach for studying both diet and mobility patterns, complementing material culture studies. The aim of this paper is to evaluate the presence of colonies and/or specialised highland caravans in the lowlands of northern Chile through the application of ή13C, ή15N and ή18O to human tooth enamel, bone collagen and bone apatite. The results show strong local traditions in terms of diet and mobility associated with the Loa-San Pedro, Antofagasta and Pica-Tarapacá cultural groups. Our results suggest a non-local origin for some individuals in Pica-Tarapacá and Loa-San Pedro, but provide little evidence to support either the presence of ‘colonies’ or of specialised ‘caravans’. Mobility patterns were, instead, diverse and flexible, including female and male individuals that moved at different moments of their lives

    A chronology for the earliest human burials at Cuchipuy, central Chile

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    Cuchipuy is an archaeological site within the ancient Laguna de Tagua Tagua area (O’Higgins Region, central Chile; known for containing the remains of extinct fauna), with evidence for cultural activity spanning most of the Holocene, including over 50 human burials. The bulk of chronometric work at Cuchipuy was carried out in the 1980s, where a discrepancy within the radiocarbon dating results raised questions on the antiquity of the oldest funerary deposits (Stratum 4). Given the importance of both the site and area in prehistoric studies, this analysis aimed to reassess the chronology of Stratum 4 through the production of new radiocarbon dates on human remains and the application of Bayesian modelling. When combined with previously published ages, results place the commencement of Stratum 4 at 7320–7160 cal BP, within the early-mid Holocene. This is later than previous conclusions based on the discrepant dataset, refuting a temporal connection to Paleoindian deposits within the region. In addition, stable light isotope results suggest that human diet during the period was diverse, relying on both terrestrial and freshwater aquatic resources. This pattern changes with later populations, however, where the isotopic signal reflects the consumption of mainly terrestrial resources

    Paired radiocarbon dating on human samples and camelid fibers and textiles from northern Chile: the case of Pica 8

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    Pica 8 is a Late Intermediate Period (AD 900-1450) cemetery located in the Atacama Desert. Burials at the site present unexpectedly high variability in ÎŽ13C (-8‰ to -16‰) and ÎŽ15N (10‰ to 24‰) values in their skeletal tissues implying highly diverse diets. There are two possible explanations for this variability: the first is diachronic change in diet and the second synchronic socio-cultural distinctions. To distinguish between them a radiocarbon dating program (n = 23) was initiated. The presumed importance of marine foods adds the complication of a marine reservoir effect. To address this problem, paired radiocarbon dates were obtained on human bone and camelid textiles from nine graves. The results fall into two groups, one showing an average offset of 117 ± 9 14C yr, and the other no statistically significant offsets. We conclude that the contribution of marine foods to bone collagen at Pica 8 was less than previously supposed. Other factors must be invoked to account for the unusually high human ÎŽ15N values at the site. Manuring crops with sea-bird guano emerges as a probable explanation. No relationship with chronology is seen implying the presence of considerable diversity in diets and hence lifeways within the Pica 8 community

    ‘White gold’ guano fertilizer drove agricultural intensification in the Atacama Desert from AD 1000

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    The archaeological record shows that large pre-Inca agricultural systems supported settlements for centuries around the ravines and oases of northern Chile’s hyperarid Atacama Desert. This raises questions about how such productivity was achieved and sustained, and its social implications. Using isotopic data of well-preserved ancient plant remains from Atacama sites, we show a dramatic increase in crop nitrogen isotope values (ή15N) from around AD 1000. Maize was most affected, with ή15N values as high as +30‰, and human bone collagen following a similar trend; moreover, their carbon isotope values (ή13C) indicate a considerable increase in the consumption of maize at the same time. We attribute the shift to extremely high ή15N values—the highest in the world for archaeological plants—to the use of seabird guano to fertilize crops. Guano—‘white gold’ as it came to be called—thus sustained agricultural intensification, supporting a substantial population in an otherwise extreme environment

    Two ancient human genomes reveal Polynesian ancestry among the indigenous Botocudos of Brazil.

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    Understanding the peopling of the Americas remains an important and challenging question. Here, we present (14)C dates, and morphological, isotopic and genomic sequence data from two human skulls from the state of Minas Gerais, Brazil, part of one of the indigenous groups known as 'Botocudos'. We find that their genomic ancestry is Polynesian, with no detectable Native American component. Radiocarbon analysis of the skulls shows that the individuals had died prior to the beginning of the 19th century. Our findings could either represent genomic evidence of Polynesians reaching South America during their Pacific expansion, or European-mediated transport.GeoGenetics members were supported by the Lundbeck Foundation, the Danish National Research Foundation (DNRF94) and the European Union (FP7/2007-2013/317184 and 319209). A.S.M. was supported by a fellowship from the Swiss National Science Foundation (PBSKP3_143529); M.D. by the US National Science Foundation (grant DBI-1103639); P.L.J. by the National Institutes of Health (grant K99 GM104158); V.F.G. by a Strategic Training for Advanced Genetic Epidemiology (STAGE) fellowship, University of Toronto.This is the final version. It was first published by Elsevier at http://www.sciencedirect.com/science/article/pii/S096098221401274
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