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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)
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
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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