The analysis of the literature about the Guadix-Baza Basin, shows some doubts and disputations concerning the connection between the basin and the open sea trough the Almanzora Corridor. This connection is considered to have finished at the end of Late Tòrtonian. However, recently the hypothesis of a Early Pliocene transgression in the central and eastern aereas of the basin is suggestted. In this paper bibliographic data are reviewed and the stratigraphic study of the materials involved provides arguments against the hypothesis of the Early Pliocene transgression
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