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    Título
    New evidence for shellfishing seasonality and palaeoenvironmental contexts in Atlantic Europe during the Late Glacial through stable oxygen isotope (δ18O) analysis of Patella vulgata Linnaeus, 1758
    Autor(es)
    Marchán Fernandez, A.
    García Escarzaga, A.
    Martínez Varea, Carmen MaríaAutoridad USAL ORCID
    Aguirre Uribesalgo, Amaia
    Jordá Pardo, Jesús Francisco
    Martínez Villa, Alberto
    Fa, D. A.
    Álvarez-Fernández, Esteban
    Palabras clave
    Shellfish exploitation
    Upper Palaeolithic
    Cantabrian Spain
    Seasonality
    Palaeoclimate
    Stable oxygen isotopes
    Clasificación UNESCO
    5505.01 Arqueología
    5504.05 Prehistoria
    Fecha de publicación
    2025
    Citación
    MARCHÁN-FERNÁNDEZ, A. ; GARCÍA-ESCÁRZAGA, A.; MARTÍNEZ VAREA, C. M.; AGUIRRE-URIBESALGO, A.; JORDÁ PARDO, J. F.; MARTÍNEZ VILLA, A.; FA, D. A. & ÁLVAREZ-FERNÁNDEZ, E. (2025): New evidence for shellfishing seasonality and palaeoenvironmental contexts in Atlantic Europe during the Late Glacial through stable oxygen isotope (δ18O) analysis of Patella vulgata Linnaeus, 1758. Environmental Archaeology.
    Resumen
    [EN] In recent decades, the role of marine resources in prehistoric hunter-gatherer diets has been widely debated. While some scholars propose that shellfish served as an emergency food supply during resource scarcity, others highlight their broader nutritional benefits. This paper applies δ18O analyses to Patella vulgata Linnaeus, 1758 shells from Cuevona de Ardines and El Cierro caves (Asturias, Spain) to determine seasonal patterns in shellfish collection during the Early Magdalenian (ca. 19,600–18,900 cal BP) and Azilian (ca. 13,600– 12,700 cal BP) periods. These data provide insights into human subsistence strategies, enhancing our understanding of coastal resources in their diets and mobility patterns. Additionally, past sea surface temperatures (SST) were estimated using δ18O values derived from shells. The results were compared with anthracological remains from Cuevona de Ardines and El Cierro, as well as other available evidence (pollen surveys, marine cores, isotopic analyses, etc.), to achieve a more accurate palaeoenvironmental reconstruction. Findings indicate that, during the Early Magdalenian, shellfishing primarily occurred in autumn, followed by summer and spring. For this period, an annual mean SST of 12.6°C is proposed. During the Azilian period, harvesting also predominantly took place in autumn, albeit to a lesser extent throughout the rest of the year, with an annual mean SST close to 14°C. These results are compared and discussed in the context of other sites with similar chronologies.
    URI
    https://hdl.handle.net/10366/166985
    ISSN
    1461-4103
    DOI
    https://doi.org/10.1080/14614103.2025.2535759
    Aparece en las colecciones
    • PREHUSAL. Artículos [127]
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    2025. Marchan et al. Isotopos Cierro y Cuevona.pdfEmbargado hasta: 2050-12-31
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