First Modern Human peopling recorded in the Iberian hinterland occurred during Heinrich Stadial 2 in a harsh environment: a sequence of human environment interactions at the Peña Capón rock shelter
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2021
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Alcaraz- Castaño, M., Alcolea-González, J.J., Andrés-Herrero, M. de, Castillo-Jiménez, S., Cuenca-Bescós, G., Cuartero, F., Kehl, M., López-Sáez, J.A., Luque, L., Pérez-Díaz, S., Piqué, R., Ruiz-Alonso, M., Weniger, G-Ch., Yravedra, J. (2021): “First Modern Human peopling recorded in the Iberian hinterland occurred during Heinrich Stadial 2 in a harsh environment: a sequence of human environment interactions at the Peña Capón rock shelter”, Scientific Reports 11(1), DOI: 10.1038/s41598-021-94408-w
Abstract
As the south-westernmost region of Europe, the Iberian Peninsula stands as a key area for understanding the process of modern human dispersal into Eurasia. However, the precise timing, ecological setting and cultural context of this process remains controversial concerning its spatiotemporal distribution within the different regions of the peninsula. While traditional models assumed that the whole Iberian hinterland was avoided by modern humans due to ecological factors until the retreat of the Last Glacial Maximum, recent research has demonstrated that hunter-gatherers entered the Iberian interior at least during Solutrean times. We provide a multi-proxy geoarchaeological, chronometric and paleoecological study on human–environment interactions based on the key site of Peña Capón (Guadalajara, Spain). Results show (1) that this site hosts the oldest modern human presence recorded to date in central Iberia, associated to pre-Solutrean cultural traditions around 26,000 years ago, and (2) that this presence occurred during Heinrich Stadial 2 within harsh environmental conditions. These findings demonstrate that this area of the Iberian hinterland was recurrently occupied regardless of climate and environmental variability, thus challenging the widely accepted hypothesis that ecological risk hampered the human settlement of the Iberian interior highlands since the first arrival of modern humans to Southwest Europe.
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This research was carried out in the context of the ERC MULTIPALEOIBERIA project, funded by the European Research Council (ERC-2018-STG-805478), and the PALEOINTERIOR project, funded by the Spanish Ministry of Science and Innovation (HAR2017-82483-C3-3-P). The sedimentological, micromorphological and part of the radiocarbon analyses were funded by subproject C1 of the CRC 806 “Our way to Europe” (DFG, German Research Foundation) and the Marie Curie Intra European Fellowship project ‘Hiatus LPleis Iberia’ (FP7-2013-IEF-628179). We gratefully acknowledge contributions made by the wide excavation and laboratory team. Fieldworks at Peña Capón were authorized by the Dirección General de Cultura de la Junta de Comunidades de Castilla–La Mancha (Spain) (Exp. 14.0955-P4 and Exp.: 19.248) with permission from the Confederación Hidrográfica del Tajo.












