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El pleistoceno medio y superior en la secuencia ceneral de las terrazas del Guadalquivir (sgtg): nuevas dataciones por luminiscencia de la t12 y t13 en la Rinconada (SW de España)

Abstract

This work includes the luminescence dating (quartz-OSL, pIRIR on K-feldespar and TL) of the T12 and T13 terraces of the Guadalquivir River near La Rinconada (Seville). Lithic Achelense industry is located from the basal USLC-1 unit of T12, together with remains of macromammal fauna. The results obtained of the analysis of the T12 terrace in “Sando-La Cabaña” show that the age or the unit lower in the terrace is older than 240 ka, probably, corresponding to MIS12-MIS11 or MIS10-MIS9.The upper part of the alluvial formation of the T13 presents an absolute age (quartz-OSL) of ca.75 ka (MIS5a)

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