Palaeoclimate records which came from different profiles are usually reconstructed on the basis of different geochronology methods. From this reason it is hard to place these profiles on one time scale. Even more problems occur when the correlation of records is based on the non-isotopic time scales (depth, biostratigraphy, etc.). As a solution we propose nonparametric methods and computer software based on genetic algorithms as a tool for correlation palaeoclimatic records regardless of the time scale. Described algorithms we show using stable isotope records from several stalagmites from Demianova Caves System (Low Tatra Mts., Slovakia) dated by radiocarbon and U-series methods.