R. Damiani et al., First trematosaurid temnospondyl from the Lystrosaurus Assemblage Zone of South Africa and its biostratigraphic implications, GEOL MAG, 137(6), 2000, pp. 659-665
A large temnospondyl mandible from the Lystrosaurus Assemblage Zone (Early
Triassic) of South Africa is referred to the higher-level taxon Trematosaur
idae. The mandible is remarkably similar to that described for Trematosauru
s from the Middle Buntsandstein of Germany, a genus closely related to the
South African Trematosuchus, for which the mandible is unknown. However, th
e mandible cannot be referred unequivocally to either of these taxa. Tremat
osuchus is considered to be restricted to the lowermost subzone of the over
lying Cynognathus Assemblage Zone, which, based principally on the temnospo
ndyl and therapsid fauna, is considered to be of Upper Olenekian age. The m
andible described here extends back the range of the Trematosauridae to the
underlying Lystrosaurus Assemblage Zone and argues against the long-held n
otion of a sharp palaeontological break between the faunas of the Lystrosau
rus and Cynognathus Assemblage zones. It also supports the hypothesis that
the Lystrosaurus Assemblage Zone extended up to the Upper Olenekian.