Estudio geoarqueológico de la secuencia estratigráfica del yacimiento Los Graneros: Achelense pleno en el Valle del Guadalquivir

J.A. Caro ^[1] ; F. Díaz del Olmo ^[2] ; M. Cañete ^[1] ; C. Borja ^[2] ; J.M. Recio ^[1]
1. [1] Universidad de Córdoba
  
  Universidad de Córdoba
  
  Cordoba, España
2. [2] Universidad de Sevilla
  
  Universidad de Sevilla
  
  Sevilla, España
Localización: XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes, 2019, ISBN 978-84-17713-16-4, págs. 125-128
Idioma: español
Enlaces
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Resumen
- A geoarchaeological study of the fluvial deposits from the Los Graneros archaeological site is carried out, located in the High Terraces of the Guadalquivir Complex (T9), at + 73-75 m. We have analyzed a sequence with 5 different sediment phases: alluvialconglomeratic, fluvial-lacustrine, alluvial-rill, alluvial with lateral incision, alluvial stream and colluvium-alluvial. Some chronologies with OSL and U / Th techniques that define a temporal range between 350 k and 30 k and BP have been obtained. Finally, in relation to the lithic set and the chronologies obtained, Los Graneros deposit can be identified as a full Acheulean model, except for some of the cooler industries of the last period (Phase V), and the surface series, closest to the middle Paleolithic technocomplexes