Tropidostoma dubium (SAM-PK-K11238) in (A) dorsal, (D) ventral, (G) right lateral, and (J) anterior views. Bulbasaurus phylloxyron (CGP/1/938) in (B) dorsal, (E) ventral, (H) right lateral, and (K) anterior views. Specimen has suffered some lateral compression. Scale bars equal 5 cm.
The first Tropidostomafossil material was found during a field expedition in the Upper Permian-aged Teekloof Formation of the Beaufort Group. This material was later described by Seeley (1889) in a study in which he described two fossils which had been named Dicynodon microtrema and Tropidostoma dunni. In 1915, several years after Seeley's death, the paleontologist, Robert Broom, reexamined the same material and discovered that the fossil material in question was of the same species. This new single species was renamed Tropidostoma microtrema.[3] Some years later, the name T. microtrema was changed to Tropidostoma dubium, and Tropidostoma dunni is now considered to be the type species.[4][5][6][7]
Description
Two subspecies exist among the specimens referred to as Tropidostoma dubium and Tropidostoma dunni . T. dubium is observed to have two cranial morphs, one being robust form with a tall snout and large tusks and the other more gracile with a low snout and small or no tusks. The robust and gracile forms are considered to either represent sexual dimorphism or individual variation.[8]
Classification
Tropidostoma is currently classified as an oudenodontid within the larger dicynodontcladeBidentalia. This clade is characterized collectively by their reduced dentition with only their maxillarytusks being intact. However, many species in this clade sporadically lack tusks completely and their fossils only hold evidence that they retained their keratinous beaks.[9] Many Tropidostoma fossils previously collected have been misidentified as other species, such as of Oudenodon bainii due to their remarkable similarity.[7] In addition, the type fossil of the recently discovered Bulbasaurus phylloxyron was misidentified as a Tropidostomafossil for several years.[10][11]
^Smith, R.M.H.; Keyser, A.W. "Biostratigraphy of the Tropidostoma Assemblage Zone". In Rubidge, B.S. (ed.). Biostratigraphy of the Beaufort Group (Karoo Supergroup). South African Committee for Stratigraphy Biostratigraphic Series. Vol. 1. Pretoria: Council for Geoscience. pp. 18–22.
^Keyser, A.W.; Smith, R.M.H. (1978). "Vertebrate biozonation of the Beaufort Group with special reference to the western Karoo Basin". Annals of the Geological Survey of South Africa. 12: 1–36.
^Keyser, A.W. (1981). "The stratigraphic distribution of the Dicynodontia of Africa reviewed in a Gondwana context". In Creswell, M.M.; Vella, P. (eds.). Gondwana five. Rotterdam: A.A. Balkema. pp. 61–63.