Cueva Huenul 1 Archaeological Site, Northwestern Patagonia, Argentina

Initial Colonization and Mid-Holocene Demographic Retraction

Bibliographic Data

ID4951708
AuthorsRamiro Barberena
Year2015
Volume26
Issue3
Pages304-318
Publication date2015-09-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueLatin American Antiquity (JOURNAL)
Journal identifiersISSN: 1045-6635 • E-ISSN: 2325-5080
DOI10.7183/1045-6635.26.3.304
LanguageEN
Citations received21
References cited32

In this paper 1 present an intensively dated chrono-stratigraphic sequence for the Cueva Huenul 1 archaeological site, Neuquen Province, Argentina. Located in the inland deserts of northwestern Patagonia, Cueva Huenul 1 offers a remarkable temporal record of events for a largely unstudied desert region. I connect this local record with available data on a macroregional scale to reassess (1) the timing of the first human colonization of the area and its implications for explaining the extinction of megafauna (ca. 14,000-10,000 cal B.P.) and (2) the decrease in human occupation recorded in several South American deserts during parts of the mid-Holocene (ca. 8000-6000 cal B .P.). The data presented here show a gap of about 1,500 calendar years between the extinction of megafauna and the appearance of humans. A review of evidence from the northern Patagonia and southern Cuyo regions is consistent with this record, favoring ecological causes for regional extinction ofmegafaunal taxa. Integration of this record with those indicating the earliest human presence in South America (e.g., Monte Verde, Chile) is consistent with a process of human radiation to the inland Patagonian deserts from nodes of initial occupation. The chrono-stratigraphic sequence from Cueva Huenul 1 also contributes to an assessment of a trough in human occupation along the South American Arid Diagonal around 8000-6000 cal B.P. Evidence for a decrease in occupational intensity during this period is found in the highland and lowland deserts in Mendoza and San Juan, the Puna region in northwestern Argentina, the Atacama Desert in Chile, and possibly the Pampean region. Previous researchers have suggested that persistent arid conditions would have produced increasing landscape fragmentation, particularly affecting desert areas. A more specific understanding of the demographic processes underlying this archaeological signal is needed. In this paper I suggest that this trough reflects not only spatial and social rearrangements, but also a macro-regional demographic retraction. This could have caused a population bottleneck with lasting biological and cultural implications

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