Temporal range: Upper Carboniferous – Upper Permian
|Dimetrodon grandis skeleton at the |
National Museum of Natural History
These tetrapods appeared during the Pennsylvanian and went extinct at the end of the Permian period. They were the dominant land animals for some 40 million years, and were almost wiped out by the P/Tr extinction event. A few survived until the lower Triassic to form the therapsids, a group which led to the mammals. Because the term does not include their descendants, it is not used much now.
Characteristics[change | change source]
At least two pelycosaur clades independently evolved a tall sail, consisting of elongated vertebral spines: the edaphosaurids and the sphenacodontids. In life, this would have been covered by skin, and possibly functioned as a thermoregulatory device and/or a mating display.
Unlike lepidosaurian reptiles, pelycosaurs lacked epidermal scales. Fossil evidence from some ophiacodonts shows that parts of the skin was naked, but that the belly was covered in dermal scutes. These scutes looked like the scutes present in reptile groups, but they are of a different type of structure.
In 1940 the group was reviewed in detail and every species known at the time described (and many illustrated) in an important monograph.
Taxonomy[change | change source]
- Order †Pelycosauria*
- Order †Therapsida*
References[change | change source]
|Wikispecies has information on: Pelycosauria.|
- Botha-Brink J. and Modesto S.P. 2007. A mixed-age classed ‘pelycosaur’ aggregation from South Africa: earliest evidence of parental care in amniotes? Proceedings of the Royal Society B, 274(1627): 2829–2834. 
- Carroll R.L. 1969. Problems of the origin of reptiles. Biological Reviews, 44: 393-432.
- Romer A.S. & Price L.I 1940. Review of the Pelycosauria. Geol. Soc. Amer. Spec. Papers 28: 1-538.