Bioavailable strontium, human paleogeography, and migrations in the Southern Andes: A machine learning and GIS approach
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Barberena, Ramiro
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Bioavailable strontium, human paleogeography, and migrations in the Southern Andes: A machine learning and GIS approach
Author
- Barberena, Ramiro;
- Cardillo, Marcelo;
- Lucero, Gustavo;
- Le Roux, Petrus J.;
- Tessone, Augusto;
- Llano, Carina;
- Gasco, Alejandra;
- Marsh, Erik J.;
- Nuevo Delaunay, Amalia;
- Novellino, Paula;
- Frigolé, Cecilia;
- Winocur, Diego;
- Benítez, Anahí;
- Cornejo, Luis;
- Falabella Gellona, Fernanda;
- Sanhueza Riquelme, Maria Lorena;
- Santana Sagredo, Francisca;
- Troncoso Melendez, Andres Rolando;
- Cortegoso, Valeria;
- Durán, Víctor A.;
- Méndez, César;
Abstract
The Andes are a unique geological and biogeographic feature of South America. From
the perspective of human geography, this mountain range provides ready access to
highly diverse altitudinally arranged ecosystems. The combination of a geologically and
ecologically diverse landscape provides an exceptional context to explore the potential
of strontium isotopes to track the movements of people and the conveyance of material
culture. Here we develop an isotopic landscape of bioavailable strontium (87Sr/86Sr)
that is applied to reconstruct human paleogeography across time in the southern Andes
of Argentina and Chile (31 –34 S). These results come from a macro-regional sampling
of rodents (N = 65) and plants (N = 26) from modern and archeological contexts.
This “Southern Andean Strontium Transect” extends over 350 km across the Andes,
encompassing the main geological provinces between the Pacific coast (Chile) and the
eastern lowlands (Argentina). We follow a recently developed approach to isoscape
construction based on Random Forest regression and GIS analysis. Our results suggest
that bioavailable strontium is tightly linked with bedrock geology and offers a highly
resolved proxy to track human paleogeography involving the levels of territories or
daily mobility and anomalous events that disrupt home ranges, such as migration. The southern Andes provide an ideal geological setting to develop this approach, since the
geological variation in rock age and composition produces distinctive isotopic signatures
for each main biogeographical region. Finally, we apply this framework to a set of results
from human remains from the Uspallata Valley in Mendoza (Argentina), to assess the
incidence of migration in the key period of the consolidation of agropastoral economies
between AD 800 and 1400. The application of the isoscape to the values from human
remains confirms the persistence of human groups with relatively restricted territories
encompassing Uspallata and the adjacent Precordillera between AD 800 and 1500. We
also identify a pulse of human migration between AD 1280 and 1420, shortly preceding
the Inka conquest. Looking forward, we expect to converge with ongoing efforts in
South America to build a continental research framework to track the movement of
people, animals, and artifacts across space and time.
Patrocinador
National Geographic Society HJ-136R-17
ANID-FONDECYT 1170408
Programa Regional ANID (Chile) 20F0002
Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) 0301
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Artículo de publícación WoS Artículo de publicación SCOPUS
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Frontiers in Ecology and Evolution March 2021 | Volume 9 | Article 584325
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