Evidence map›Paper›PMID 40560871›Full record

ArticlePloS one2025

Altiplano agricultural origins was a process of economic resilience, not hardship: Isotope chemistry, zooarchaeology, and archaeobotany in the Titicaca Basin, 5.5-3.0 ka.

Luis Flores-Blanco, Morgan Hall, Luisa Hinostroza, Jelmer Eerkens, Mark Aldenderfer, Randall Haas

Abstract readHistorical Article
In one paragraph

Article in PloS one, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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0citing papers in PubMed
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1 · What the graph read from it

What it found

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2 · The registry

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3 · Its place in the literature

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4 · The record

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5 · Who and what money

Authors and funding

6 authors.

Luis Flores-BlancoDepartment of Anthropology, University of California, Davis, California, United States of America.ORCID 0000-0003-2344-6542
Morgan HallDepartment of Anthropology, University of California, Davis, California, United States of America.
Luisa HinostrozaDepartment of Ethnobotany and Economic Botany of the Museum of Natural History, UNMSM, Lima, Peru.
Jelmer EerkensDepartment of Anthropology, University of California, Davis, California, United States of America.
Mark AldenderferDepartment of Anthropology and Heritage Studies, University of California, Merced, California, United States of America.
Randall HaasDepartment of Anthropology, University of Wyoming, Laramie, Wyoming, United States of America.ORCID 0000-0002-7742-2127

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Prevailing models of agricultural origins tend to envision that economic hardship drove the transition from foraging to farming economies. Growing human populations and the depletion of high-ranked animal resources forced humans into increasingly intensive and dependent relationships with plant foods. Current evidence from the Andean Altiplano (High Plateau, 3800 masl) identifies the Terminal Archaic Period (5.0-3.5 cal. ka) as the period of economic transition from Archaic foraging economies to Formative Period agro-pastoral economies. Consistent with models of agricultural origins, isotope chemistry (δ13Ccollagen, δ13Capatite, δ15Ncollagen) of human bone samples from 16 individuals from the Terminal Archaic sites of Kaillachuro and Jiskairumoko (5.3-3.0 cal. ka) indicates that C3 plants comprised approximately 84% of the dietary protein. Archaeobotanical data show that chenopods may have been the most important subsistence resource, and zooarchaeological remains indicate that protein was derived from camelid meat. Inconsistent with the working model of plant intensification, the Terminal Archaic diets reported here are statistically indistinguishable from previously published values of Early-Late Archaic (9.0-6.5 cal. ka) individuals in the same region, which also show approximately 84% of protein coming from plants. Rather than being a process of dramatic dietary change and economic hardship, the agricultural transition on the Altiplano appears to have been one of remarkable resilience in which plant:meat ratios remained relatively stable over six millennia, spanning the transition from Archaic foraging and hunting to Formative farming and herding economies. Plant and animal domestication on the Altiplano thus represents a process of economic sustainability rather than one of food insecurity and hardship, as many prevalent agricultural origins models would suggest.

Indexed as

AgricultureArchaeologyAnimalsBone and BonesCarbon IsotopesHistory, AncientHumansCarbon Isotopes

Identifiers

PMID40560871
PMCPMC12192108

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