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

  1. David Álvarez Alonso 1
  2. José Yravedra 2
  3. María de Andrés-Herrero 1
  4. Álvaro Arrizabalaga 3
  5. Jesús F. Jordá 4
  6. Julio Antonio Rojo Hernández 4
  1. 1 UNED. Asturias
  2. 2 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  3. 3 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info

    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

  4. 4 Universidad Nacional de Educación a Distancia
    info

    Universidad Nacional de Educación a Distancia

    Madrid, España

    ROR https://ror.org/02msb5n36

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Livre:
El Cuaternario Ibérico. Investigación en el s. XXI: VIII Reunión de Cuaternario Ibérico (Sevilla - La Rinconada 2013)
  1. Rafael Baena Escudero (coord.)
  2. José Juan Fernández Caro (coord.)
  3. Inmaculada Guerrero Amador (coord.)

Éditorial: Asociación Española para el Estudio del Cuaternario

ISBN: 978-84-695-8601-3

Année de publication: 2013

Pages: 83-86

Congreso: Reunión del Cuaternario Ibérico = Reuniâo do Quaternário Ibérico (8. 2013. La Rinconada (Sevilla))

Type: Communication dans un congrès

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Résumé

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.

La source de données: Dialnet