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La secuencia cronoestratigráfica del Paleolítico Superior de la cueva de Coímbre (Asturias, España)

    1. [1] Universidad Complutense de Madrid

      Universidad Complutense de Madrid

      Madrid, España

    2. [2] Universidad Nacional de Educación a Distancia

      Universidad Nacional de Educación a Distancia

      Madrid, España

    3. [3] UNED. Asturias
    4. [4] UPV/EHU
  • Localización: El Cuaternario Ibérico: investigación en el s. XXI: VIII Reunión de Cuaternario Ibérico (Sevilla - La Rinconada 2013) / Rafael Baena Escudero (ed. lit.), José Juan Fernández Caro (ed. lit.), Inmaculada Guerrero Amador (ed. lit.), 2013, ISBN 978-84-695-8601-3, págs. 83-86
  • Idioma: español
  • Títulos paralelos:
    • Upper Paleolithic chronoestratigraphical sequence of Coímbre cave (Asturias, Spain)
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  • Resumen
    • This paper shows the first results of the archaeological excavation of Coímbre B, a site which until this moment has provided evidences of a rich Upper Magdalenian habitat, as well as Lower Magdalenian and Gravettian occupation remains. Stratigraphical sequence identified in B zone of Coímbre cave, significantly influenced by the movement of a seasonal and frequent wáter current, but in a more marginal form by the end of Upper Paleolithic each time, conditioned an sporadic human presence in B zone, combined with the occupation of another areas of the cave, thus becoming in a preferential habitat area in the moment in which water flow ceases definitely. This levels succession shows, in a graphic way, how had influenced different climatic oscillations in karstic activity and in the human occupation model developed in Coímbre cave.


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