Ctenospondylus

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Ctenospondylus
Temporal range: Early Permian, Artinskian–Kungurian
Ctenospondylus2DB2.jpg
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Family: Sphenacodontidae
Subfamily: Sphenacodontinae
Genus: Ctenospondylus
Romer, 1936
Species
  • C. casei Romer, 1936
  • C. ninevehensis Berman, 1978

Ctenospondylus ("comb vertebra") is an extinct genus of sphenacodontid synapsid

Contents

Species were about three meters (ten feet) long. The genus is known only from the 'Seymouran' Land Vertebrate Faunachron, which is equivalent to the upper part of the Artinskian stage and the lowermost Kungurian stage of the Early Permian. [1] Its fossils were found in the U.S. states of Ohio and Texas. It was a carnivore and preyed upon animals close to its size. Ctenospondylus had a long tail, short back spines, and a very deep yet narrow skull with massive jaws that had sharp teeth. Because of its large size, it was probably the apex predator in its environment, and might have competed with other predators like Dimetrodon for food. A sphenacodontid, it was a close relative of Dimetrodon .

In 1936, Alfred Sherwood Romer named the type species Ctenospondylus casei. The generic name, from Greek κτείς, kteis, "comb", and σφόνδυλος, sphondylos, "vertebra", referred to the form of the back sail. The specific name honoured Ermine Cowles Case, who first reported the type specimen in 1910. [2] The fossil had been found in Archer County at the Slippery Creek site in the Belle Plains Formation, dating from the Artinskian. The holotype is AMNH 4047, already found in 1881 by William Fletcher Cummins, collecting for Edward Drinker Cope. It consists of a neck vertebra, two back vertebrae, two broken off spines and rib fragments. [3] In 1964, far more complete material from Utah and Arizona was referred to the species by Peter P. Vaughn. This included specimen NTM VP 1001: a partial skeleton with skull; NTM VP 10014: a number of back vertebrae; NTM VP 10015: additional back vertebrae; NTM VP 10016: two skull bones; and NTM VP 10017: a series of three back vertebrae. The specimens are part of the collection of the Navajo Tribal Museum . [4]

In 1978, David Berman named a second species: Ctenospondylus ninevehensis. The specific name refers to the Niniveh Limestone Member of the Greene Formation, dating from the Sakmarian where it was found at Clark Hill in Monroe County, Ohio. The holotype is specimen MCZ 3386, found by Donald Baird in June 1955. It consists of a partial skeleton with fragmentary skull, a spine from the axis, four back vertebrae, four tail vertebrae, neck ribs, dorsal ribs, a shoulder blade, two humeri, and the right pelvis. Specimen MCZ 4458, a right maxilla, was referred to the species. Berman considered C. ninevehensis more basal than Ctenospondylus casei and only referred the second species to the genus because of the similar spine length. [5] Later specimen MCZ 8635-42 was referred, a skull; MCZ 8665, a jugal bone and MCZ 3102, a skeleton with skull.

The spines of Ctenospondylus are longer than those of Sphenacodon but shorter than those of Dimetrodon. They also lack the dumbbell-shaped upper profile of the latter genus and are more transversely flattened. The skull of Ctenospondylus is, as far as can be judged from the limited material found, very similar to that of other sphenacodontids. [6]

See also

Related Research Articles

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<i>Sphenacodon</i> Extinct genus of synapsids

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<i>Secodontosaurus</i> Extinct genus of synapsids

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<i>Mycterosaurus</i> Extinct genus of tetrapods

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Casea is a genus of herbivorous caseid synapsids that lived during the late Lower Permian (Kungurian) in what is now Texas, United States. The genus is only represented by its type species, Casea broilii, named by Samuel Wendell Williston in 1910. The species is represented by a skull associated with a skeleton, a second skull, a partial skull with a better preserved dentition than that of the preceding skulls, and several incomplete postcranial skeletons. Three other Casea species were later erected, but these are considered today to be invalid or belonging to different genera. Casea was a small animal with a length of about 1.20 m and a weight of around 20 kg.

<i>Eothyris</i> Extinct genus of synapsids

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Cotylorhynchus is an extinct genus of herbivorous caseid synapsids that lived during the late Lower Permian (Kungurian) and possibly the early Middle Permian (Roadian) in what is now Texas and Oklahoma in the United States. The large number of specimens found make it the best-known caseid. Like all large herbivorous caseids, Cotylorhynchus had a short snout sloping forward and very large external nares. The head was very small compared to the size of the body. The latter was massive, barrel-shaped, and ended with a long tail. The limbs were short and robust. The hands and feet had short, broad fingers with powerful claws. The barrel-shaped body must have housed large intestines, suggesting that the animal had to feed on a large quantity of plants of low nutritional value. Caseids are generally considered to be terrestrial, though a semi-aquatic lifestyle has been proposed by some authors. The genus Cotylorhynchus is represented by three species, the largest of which could reach more than 6 m in length. However, a study published in 2022 suggests that the genus may be paraphyletic, with two of the three species possibly belonging to separate genera.

<i>Ctenorhachis</i> Extinct genus of synapsids

Ctenorhachis is an extinct genus of the family Sphenacodontidae. Ctenorhachis lived in the Early Permian epoch. Ctenorhachis was related to Dimetrodon, but did not belong to the same subfamily as Dimetrodon and Sphenacodon, being a more basal member of Sphenacodontidae. Two specimens are known that have been found from the Wichita Group outcropping in Baylor and Archer counties, north-central Texas. Only the vertebrae and pelvis are known. Articulated vertebrae from the holotype specimen possess blade like neural spines that are greatly enlarged, although not nearly to the extent that can be seen in more derived sphenacodontids such as Dimetrodon and Secodontosaurus, in which they form a large sail. The pelvis is nearly identical to that of Dimetrodon. As suggested in the original description of the genus, Ctenorhachis may represent a short-spined sexual dimorph, although the authors find this unlikely.

<i>Aerosaurus</i> Extinct genus of tetrapod

Aerosaurus is an extinct genus within Varanopidae, a family of non-mammalian synapsids. It lived between 252-299 million years ago during the Early Permian in North America. The name comes from Latin aes (aeris) “copper” and Greek sauros “lizard,” for El Cobre Canyon in northern New Mexico, where the type fossil was found and the site of former copper mines. Aerosaurus was a small to medium-bodied carnivorous synapsid characterized by its recurved teeth, triangular lateral temporal fenestra, and extended teeth row. Two species are recognized: A. greenleeorum (1937) and A. wellesi (1981).

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<i>Callibrachion</i>

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<i>Tarjadia</i> Extinct genus of reptiles

Tarjadia is an extinct genus of erpetosuchid pseudosuchian, distantly related to modern crocodilians. It is known from a single species, T. ruthae, first described in 1998 from the Middle Triassic Chañares Formation in Argentina. Partial remains have been found from deposits that are Anisian-Ladinian in age. Long known mostly from osteoderms, vertebrae, and fragments of the skull, specimens described in 2017 provided much more anatomical details and showed that it was a fairly large predator. Tarjadia predates known species of aetosaurs and phytosaurs, two Late Triassic groups of crurotarsans with heavy plating, making it one of the first heavily armored archosaurs. Prior to 2017, most studies placed it outside Archosauria as a member of Doswelliidae, a family of heavily armored and crocodile-like archosauriforms. The 2017 specimens instead show that it belonged to the Erpetosuchidae.

Ruthenosaurus is an extinct genus of caseid synapsids that lived in what is now southern France during the Early Permian about 285 million years ago. It is known from the holotype MNHN.F.MCL-1 an articulated partial postcranial skeleton. It was collected by D. Sigogneau-Russell and D. Russell in 1970 in the upper part of the M2 Member, Grès Rouge Group, in the Rodez Basin, near the village of Valady, in Occitanie Region. It was first named by Robert R. Reisz, Hillary C. Maddin, Jörg Fröbisch and Jocelyn Falconnet in 2011, and the type species is Ruthenosaurus russellorum.

<i>Euromycter</i> Extinct genus of synapsids

Euromycter is an extinct genus of caseid synapsids that lived in what is now southern France during the Early Permian about 285 million years ago. The holotype and only known specimen of Euromycter (MNHN.F.MCL-2) includes the complete skull with lower jaws and hyoid apparatus, six cervical vertebrae with proatlas, anterior part of interclavicle, partial right clavicle, right posterior coracoid, distal head of right humerus, left and right radius, left and right ulna, and complete left manus. It was collected by D. Sigogneau-Russell and D. Russell in 1970 at the top of the M1 Member, Grès Rouge Group, near the village of Valady, Rodez Basin. It was first assigned to the species "Casea" rutena by Sigogneau-Russell and Russell in 1974. More recently, it was reassigned to its own genus, Euromycter, by Robert R. Reisz, Hillary C. Maddin, Jörg Fröbisch and Jocelyn Falconnet in 2011. The preserved part of the skeleton suggests a size between 1,70 m (5,5 ft) and 1,80 m (5,9 ft) in length for this individual.

Tappenosaurus is an extinct genus of synapsids from the Middle Permian of Texas. American paleontologists Everett C. Olson and James Beerbower described the genus in 1953 based on three specimens that were uncovered from the San Angelo Formation. It was named for Neil Tappen, who found the type specimen in 1951 as a member of the field party.

References

  1. Lucas, S.G. (2006). "Global Permian tetrapod biostratigraphy and biochronology". In Lucas S.G.; Cassinis G.; Schneider J.W. (eds.). Non-Marine Permian Biostratigraphy and Biochronology. Special Publications. Vol. 265. London: Geological Society. pp. 65–93. ISBN   9781862392069 . Retrieved 10 December 2012.[ permanent dead link ]
  2. E.C. Case. 1910. "New or little known reptiles and amphibians of the Permian (?) of Texas". Bulletin of the American Museum of Natural History28: 163-181
  3. Romer, A.S. 1936. "Studies on American Permo-Carboniferous tetrapods". Problems of Paleontology, 1: 85–93
  4. Vaughn, P.P. 1964. "Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona". Journal of Paleontology38: 567–583
  5. Berman, D.S. 1978. "Ctenospondylus ninevehensis, a new species (Reptilia, Pelycosauria) from the Lower Permian Dunkard Group of Ohio". Annals of Carnegie Museum47: 493–514
  6. Eberth, D.A. 1985. "The skull of Sphenacodon ferocior, and comparisons with other sphenacodontines (Reptilia: Pelycosauria)". New Mexico Bureau of Mines and Mineral Resources Circular190: 5–39