Abstract :
Reconstruction of palaeolandscapes for intervals with different climatic conditions helps the definition and study of regional trends in environmental evolution of the earthʹs surface territory as a response to global climatic change. Analyses of palaeogeographical, palaeobotanical, geomorphological and archaeological data from 162 sites over the Saharo-Arabian area let us reconstruct palaeolandscapes for the intervals 20-18 ka B.P., 9-8 ka B.P., and 6-5 ka B.P., and the present potential landscapes, and to compile maps at a 1/15,000,000 scale. Classification and detailed mapping of the present landscapes (at a 1/5,000,000 scale) was based on the analyses of, first, current factors of landscape differentiation, such as climate, relief, vegetation and soils, and, second, of the assessment of their spacio-temporal changes during the last 20,000 years. This allowed us to distinguish 172 evolutionary-chronological variations within 80 genus of landscapes in the Saharo-Arabian area.
Keywords :
Late Glacial Maximum , Holocene , globalclimatic change , palaeolandscape , Desert