El Achelense del bajo Guadalquivier: comentario a su proceso secuencial

J.A. Caro Gómez ^[1]
1. [1] Universidad de Córdoba
  
  Universidad de Córdoba
  
  Cordoba, España
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. 309-313
Idioma: español
Títulos paralelos:
- The Acheulian in the lower Guadalquivir: remarks on its sequential process
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Resumen
- This paper focuses on the essential features of the technolithic process which shaped the Acheulian Sequence in the Lower Guadalquivir: 1) the basic complex (T6 to T9), is characterised by the appearance of the earliest macrolithic material. 2) This situation culminates, in the assemblages found in T10, in the development of a regional Full Acheulian, characterised by a marked growth in bifacial indices, which at times predominate. 3) From T11 onwards, despite the continuing presence of clearly-Acheulian material, the assemblages are typically post-Acheulian. 4) This altered substrate finally becomes Middle Palaeolithic by the low terrace T13, suggesting that they should be regarded as a Middle Palaeolithic specific to peninsular fluvial areas (or Middle Palaeolithic Quarry).