Abstract

Palynological assemblages of the lower Karoo Morupule Main Seam of Botswana are similar to those of the Striatopodocarpites fusus Biozone of the Collie Basin, Western Australia and the 3a Microfloral Biozone of the northern Karoo Basin, South Africa. This indicates an Aktastinian (Early Permian) age for the strata of Morupule.

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