During the Late Upper Pleistocene and the Lower and Middle Holocene an important sedimentary
record was deposited in the ancien entry of Nerja Cave (Málaga, Spain). The 41 calibrated valid 14C dates
obtained from this record show a chronological spread between 30 and 3,6 ky. cal. BP for the archaeological
record of Nerja Cave. This large stratigraphic record constitutes one of the most important archaeological
and palaeobiological sequences of the western Mediterranean, which contains remains of the Gravettian,
Solutrian, Magdalenian, Epipaleolithic, Neolithic and Cooper Age. In this paper we establish a narrower
correlation between the main palaeoclimatological events detected in Alborán Sea and the sedimentary
and occupational episodes of the cave