Palaeolakes of the south central Sahara — problems of palaeoclimatological interpretation

Abstract

The results of palaeoecological studies of Holocene swamp and lake deposits of a number of endorheic depressions of the Kawar, Djado and Great Erg of Bilma region of eastern Niger are presented, comprising analysis of their stratigraphy, sedimentology, diatom flora and macrofossils.

The investigations demonstrate that various palaeolakes have reacted differently in space and time and by type of lake to climatic conditions. Some of the lakes reacted rapidly to changes in the precipitation regime, as evidenced by changing size, level, water balance and water chemistry, while perennial freshwater lakes nearby show changes relatively independent of short-term climatic fluctuations. These facts suggest a more complex influence of local and regional geomorphological, hydrological and hydrogeological factors on the Holocene lake evolution than a mere climatic dependence. Beyond doubt humidity considerably increased during early and mid-Holocene periods, but the stratigraphical and ecological status obtained for individual endorheic depressions seems to be mainly a reflection of differences among groundwater catchments, aquifers of different size, local topographical conditions and changes in geomorphology (e.g. dune activity) — superimposed on the major climatic tendencies — and thus of a considerable diversity of palaeoenvironmental conditions occurring within the region at any given time of the Holocene.