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  • Remnants of Coleoptera of late glacial age have been investigated at 8 sites in Belarus. The sites are situated at varying distances from the maximum extent of the last glaciation. The palaeo-temperatures of the month of july during the lifespan
  • of varying size, often with numerous secondary forms. Active ice zones represent probable ice streams within the ice sheet, reflected by outwash plains and previous subglacial channels. Different sediments in each zone suggest a coincidence of dead-ice