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  • Lake Malawi levels have been as much as 5 m above modern peak values during the early? Holocene but, until more is known about changes in the overflow, the palaeoclimatic significance of these high levels must remain in doubt. In an attempt to view
  • Palynological work on Late Cainozoic deposits from the Transvaal and its potential for palaeoclimatic reconstructions are briefly assessed. Up to now only organic spring deposits of late Quaternary age from the province have provided detailed pollen