Nerja Cave (Málaga, southern Spain) was carried out in order to determine the conditions of
deposition in isotopic equilibrium and non-equilibrium. We obtained a record of climate
change from 190 000 to 160 000 years ago. A series of carbon (δ13C) and oxygen (δ18O)
isotopes analyses have been carried out in parallel to the stalactite growth axis. Sampling
was done in each growth layer. A curve of the secular δ18O aragonite variations for the …