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dc.contributor.authorMarchán Fernandez, A.
dc.contributor.authorGarcía Escarzaga, A.
dc.contributor.authorMartínez Varea, Carmen María 
dc.contributor.authorAguirre Uribesalgo, Amaia
dc.contributor.authorJordá Pardo, Jesús Francisco
dc.contributor.authorMartínez Villa, Alberto
dc.contributor.authorFa, D. A.
dc.contributor.authorÁlvarez-Fernández, Esteban
dc.date.accessioned2025-09-09T11:52:30Z
dc.date.available2025-09-09T11:52:30Z
dc.date.issued2025
dc.identifier.citationMARCHÁN-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.es_ES
dc.identifier.issn1461-4103
dc.identifier.urihttp://hdl.handle.net/10366/166985
dc.description.abstract[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.es_ES
dc.language.isoenges_ES
dc.subjectShellfish exploitationes_ES
dc.subjectUpper Palaeolithices_ES
dc.subjectCantabrian Spaines_ES
dc.subjectSeasonalityes_ES
dc.subjectPalaeoclimatees_ES
dc.subjectStable oxygen isotopeses_ES
dc.titleNew evidence for shellfishing seasonality and palaeoenvironmental contexts in Atlantic Europe during the Late Glacial through stable oxygen isotope (δ18O) analysis of Patella vulgata Linnaeus, 1758es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.subject.unesco5505.01 Arqueologíaes_ES
dc.subject.unesco5504.05 Prehistoriaes_ES
dc.identifier.doihttps://doi.org/10.1080/14614103.2025.2535759
dc.relation.projectIDPID2020-114462GB-I00/AEI/ 10.13039/501100011033es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/embargoedAccesses_ES
dc.journal.titleEnvironmental Archaeologyes_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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