Abstract
A chronology is given for the alluvial fan deposits in the Tabernas Basin (Internal Zone, Betic Cordillera). Palaeontological and sedimentological data are used to establish a palaeoclimatic model for the Quaternary in southeastern Spain.
Highlights
Stratigraphy oC the siteThe Tabernas Basin is situated in the Internal Zone of the Betic Cordillera
The more modern stage, in which the alluvial fans of System 11 were formed, corresponds to the Mediterranean Riss-Würm according to the fauna from the Serra-1lacustrine site
The younger faunal set observed is that of the Cueva del Agua, with species such as Clethrionomys glareolus, L
Summary
Stratigraphy oC the siteThe Tabernas Basin is situated in the Internal Zone of the Betic Cordillera. The stratigraphic sequence of the section of the Serra-1 site beings with a layer of conglomerates ~fig. The morphology of the crown of MIl is a basic triplet, common to all the Arvicolidae and made up of three closed triangles (TI, T2 and T3) and the anteroconid complex formed by a single space delimiting vertices 3e, 4e, 4i and Si. The values of the Enamel Units (EU) (defined in Ruiz Bustos, 1988) in specimen S-l give the Enamel Units Graph (EUG) in fig.
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