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Pelycosaurs
Fossil range: Late Carboniferous - Late Permian
Dimetrodon
Dimetrodon grandis skeleton at the National Museum of Natural History
Scientific classification

Superclass:

Tetrapoda

Class:

Synapsida

Order:

Pelycosauria * Cope, 1878

Suborders:

The pelycosaurs were primitive Late Paleozoic synapsid amniotes. Some species were quite large and could grow up to 3 meters or more, although most species were much smaller.

Evolutionary historyEdit

See Also: Evolution of mammals

The pelycosaurs appeared during the Late Carboniferous and reached their acme in the early part of the Permian Period, remaining the dominant land animals for some 40 million years. A few continued into the late Permian. They were succeeded by their descendants, the therapsids, which had a short but successful reign before the Permian–Triassic extinction event, giving a chance for the archosaur reptiles to take over in the Triassic.

CharacteristicsEdit

Ophiacomorphs2

Cotylorhynchus (background), Ophiacodon and Varanops

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 or for mating display. Pelycosaur fossils have been found mainly in Europe and North America, although some small, late-surviving forms are known from Russia and South Africa.

Unlike most reptiles, pelycosaurs lacked epidermal scales. Fossil evidence from some ophiacodonts shows that the skin was naked, and that the belly was covered in dermal "scales", the same type of scales possessed by early tetrapods, unrelated to reptile scales, which evolved independently and are a different type of structure.[1]

Skulls comp1

Comparison of "pelycosaurian" skulls: 1 - sphenacodont, 2 - ophiacodont, 3 - caseid. Quadratojugale is green, squamosale is red, jugale is blue.

In 1940 the group was reviewed in detail and every species known at the time described (and many illustrated) in an important monograph by Alfred Sherwood Romer and Llewellyn Price.

Pelycosauria is a paraphyletic taxon because it excludes the therapsids. For that reason the term is not used in some modern books. Eupelycosauria is used to designate the clade that includes most Pelycosaurs along with the Therapsida and the Mammals. In contrast to "Pelycosaurs", this is monophyletic group. Caseasauria refers to a pelycosaur side-branch or clade that did not leave any descendants.

The pelycosaurs appear to have been a group of synapsids that had direct ancestral links with the mammalia, having differentiated teeth and a developing hard palate.

Well-known pelycosaurs include the genera Dimetrodon, Sphenacodon, Edaphosaurus, and Ophiacodon.

SystematicsEdit

Eothyris BW

Eothyris

Cotylorhynchus BW

Cotylorhynchus - a Caseid

Varanops BW

Varanops

Ophiacodon BW

Ophiacodon

Edaphosaurus BW

Edaphosaurus

Haptodus BW

Haptodus

Dimetrodon BW

Dimetrodon

In traditional classification, the order Pelycosauria is paraphyletic--that is, it is a grouping of animals that does not contain all descendants of a common ancestor, as is often required by a different system of naming organisms, phylogenetic nomenclature. In the later, Pelycosauria is treated as a clade rather than a taxon with the rank "order", and includes the clade Therapsida, which in turn contains the clade Mammalia. In traditional taxonomy, Therapsida is separated from Pelycosauria in its own biological order, and mammals are separated from both as their own class.

TaxonomyEdit

PhylogenyEdit

In phylogenetic nomenclature, the "Pelycosauria" is not used, since it does not constitute a clade (a group of organisms descended from one common ancestor and including all the descendants of that ancestor) because the group excludes the therapsids. Instead, it represents a paraphyletic "grade" of basal synapsids leading up to the clade Therapsida.

See alsoEdit

ReferencesEdit

  1. ^ Carroll, R.L. (1969). "Problems of the origin of reptiles." Biological Reviews, 44: 393-432.

External linksEdit

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