La secuencia cronoestratigráfica del Paleolítico Superior de la cueva de Coímbre(Asturias, España)
- David Álvarez Alonso 1
- José Yravedra 2
- María de Andrés-Herrero 1
- Álvaro Arrizabalaga 3
- Jesús F. Jordá 4
- Julio Antonio Rojo Hernández 4
- 1 UNED. Asturias
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2
Universidad Complutense de Madrid
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3
Universidad del País Vasco/Euskal Herriko Unibertsitatea
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Universidad del País Vasco/Euskal Herriko Unibertsitatea
Lejona, España
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4
Universidad Nacional de Educación a Distancia
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- Rafael Baena Escudero (coord.)
- José Juan Fernández Caro (coord.)
- Inmaculada Guerrero Amador (coord.)
Editorial: Asociación Española para el Estudio del Cuaternario
ISBN: 978-84-695-8601-3
Ano de publicación: 2013
Páxinas: 83-86
Congreso: Reunión del Cuaternario Ibérico = Reuniâo do Quaternário Ibérico (8. 2013. La Rinconada (Sevilla))
Tipo: Achega congreso
Resumo
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.