La secuencia aluvial del bajo Guadalquivir (sw España) durante el Pleistoceno Superior-Holoceno
- F. Borja 1
- C. Borja 2
- F. Díaz del Olmo 2
- J.M. Recio 3
- J.A. Caro 3
- J.A. Valiente
- P. Fraile 2
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1
Universidad de Huelva
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2
Universidad de Sevilla
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3
Universidad de Córdoba
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Editorial: Universidad del País Vasco = Euskal Herriko Unibertsitatea
ISBN: 978-84-17713-16-4
Año de publicación: 2019
Páginas: 144-147
Congreso: Reunión Nacional de Cuaternario (15. 2019. Bilbao)
Tipo: Aportación congreso
Resumen
Pleistocene to Holocene evolution of the lower Guadalquivir floodplain (SW Spain) is analyzed from a geoarchaeological approach. We especially study sedimentological data from the valley of the ancient Tagarete River, a small left tributary of the Guadalquivir which is now nolonger there. Our study suggests a transition from the Pleistocene to the Holocene with a triple sedimentary system. The sequence begins with a thick detritic series of upper Pleistocene alluvial gravels, including well-rounded stone tools of the Middle Paleolithic (1). The transit of this alluvial system to the Holocene facies occurs through a strong stratigraphic unconformity that gives way, first, to an organic sediment formation environment (lagoon) correlative with the end of the sea level rise in the mid-Holocene (2), and, subsequently (late Holocene), to a predominance of flooding deposits and emerging facies at the top of the sequenc