Nowadays, Compsodon has become a topic of great relevance in our society. With the advancement of technology and globalization, Compsodon has acquired a meaning and importance that transcends borders and cultures. Since its inception, Compsodon has been the object of study and analysis, its implications are broad and deep, impacting aspects as diverse as the economy, politics, culture and society in general. In this article, we will explore the different aspects of Compsodon, its evolution over time, and its impact on the world today.
Compsodon Temporal range: Cistecephalus Assemblage Zone,
| |
---|---|
Scientific classification ![]() | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Synapsida |
Clade: | Therapsida |
Suborder: | †Anomodontia |
Clade: | †Dicynodontia |
Superfamily: | †Emydopoidea |
Genus: | †Compsodon van Hoepen, 1934 |
Type species | |
Compsodon helmoedi van Hoepen, 1934
|
Compsodon is an extinct genus of dicynodont belonging to the superfamily Emydopoidea. Fossils have been found in the Balfour Formation of South Africa and the Madumabisa Mudstone of Zambia.
Compsodon helmoedi was originally described by Egbert Cornelis Nicolaas van Hoepen in 1934 on the basis of a single specimen from late Permian deposits in the Karoo Basin of South Africa.[1] Two additional specimens from South African museum collections and three new specimens from the Luangwa Basin of Zambia have elucidated new aspects of the morphology of this species and indicate that it occurred in the upper Cistecephalus and lower Daptocephalus assemblage zones. Compsodon can be diagnosed by features of its palate, but also the presence of maxillary postcanines and parietals fused and narrowly exposed between broad postorbitals on the dorsal surface of the skull.[2]