Abstract
Devonian miospores of the Tunisian borehole MG-1 from the northern part of the Hammadah Basin have been analyzed and compared with the available faunal data. The age of the various formations drilled by this borehole has been revised and this has led to the conclusion that the Emsian and the Eifelian are represented by a thicker sedimentation than the other stages. The published faunas from this borehole are not in contradiction with the palynological results which confirm the opinion of the present authors that the Devonian stratigraphy in this area is more complex than was previously believed.
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