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Caseasauria is one of the two main of early , the other being the . Caseasaurs are currently known only from the Late Carboniferous and the , and include two superficially different families, the small insectivorous or carnivorous , and the large, . These two groups share a number of specialised features associated with the morphology of the snout and external .

The ancestor of caseasaurs can be traced back to an insect eating or an omnivorous -like from the Pennsylvanian time of the , possibly resembling , the earliest known synapsid. The caseasaurs were abundant during the later part of the , but by the caseasaur diversity declined because the group was outcompeted by the more successful . The last caseasaurs became extinct at the end of the Guadalupian (Middle Permian).


Description
Among the most conspicuous characteristics uniting caseasaurs are an enlarged nostril and a snout tip that overhangs the tooth row.

Early caseasaurs, including all eothyridids, were relatively small animals. However, most caseids reached larger sizes, and some caseids, such as Cotylorhynchus and , were among the largest terrestrial animals of the early Permian. These large herbivorous taxa reached a length of and a mass of .


Evolution
Caseasaurs first appear in the fossil record in the late , alongside many other early amniote groups. The earliest known synapsid, from the age, may be an eothyridid caseasaur. The earliest definitive caseasaur is .

Caseids thrived during the age, and numerous large herbivorous caseids are known from the Kungurian of the .

Caseasaurs are one of the two pelycosaur clades known to have survived into the epoch, along with varanopids. Two caseasaur taxa are known from the Guadalupian of Russia, representing the geologically youngest known caseasaurs: the small, possibly omnivorous or insectivorous , and the large, herbivorous .


Classification
Caseasauria is generally regarded as the most basal clade of synapsids, with all other synapsids being grouped in the clade . However, not all studies have supported this position. In 2012, Roger Benson argued that most of the characters supporting a basal position for caseasaurs pertained to the skull, and presented a phylogenetic analysis incorporating more postcranial data that resolved a clade comprising ophiacodontids and varanopids as the basalmost synapsid clade. However, new postcranial data from eothyridids and basal caseids established that caseasaurs were more basal than ophiacodontids and varanopids after all, with the characters supporting a more derived position for caseasaurs being the result of convergent evolution between caseids and more derived synapsids. The , conventionally regarded as anamniote tetrapods, may prove to be synapsids even more basal than Caseasauria.

Most caseasaurs are divided into two families, and . The affinities of the earliest definitive caseasaur, Eocasea, are uncertain, with some phylogenetic analyses finding it to be a caseid and others finding it to be a basal caseasaur belonging to neither family.

Three genera are typically regarded as belonging to the family Eothyrididae: Eothyris, Oedaleops, and Vaughnictis. However, some phylogenetic analyses have failed to resolve the eothyridids as a clade, instead finding them to be paraphyletic with respect to Caseidae. Asaphestera has been provisionally regarded as an eothyridid as well, without being included in a phylogenetic analysis.

The remaining caseasaurs belong to the family Caseidae.


List of species
+
E. martini2014incertae sedis May be a caseid
A. platyris1934 Synapsida incertae sedis; may be an eothyridid
E. parkeyi1937
O. campi1965
V. smithae1965 Originally assigned to the genus
C. gaudryi1893
D. macrourus1904
O. dolesorum2005
P. aenigmatum1954
M. bromackerensis2020
R. russellorum2011
C. broilii1910
C. halselli1954
C. nicholsi1954
E. rutenus1974 Originally described as Casea rutena
E. tecton1956 The geologically youngest known caseasaur
C. agilis1962
C. sanangelensis1953
A. simplex2019
A. ronchii2014
C. romeri1937
C. hancocki1953
C. bransoni1962
A. dolani1953
A. greeni1962
A. romeri1962
T. texensis1910


Paleoecology
The paleoecology of caseids is debated. They are typically interpreted as terrestrial animals of dry, upland habitats. However, Caseids exhibit a similar bone microstructure to cetaceans and pinnipeds, which has led to the hypothesis that they led an aquatic lifestyle. This hypothesis has been challenged on the grounds that their bone microstructure specifically resembles fully pelagic animals, and is unlike the bone microstructure of semiaquatic animals, but that the body plan of caseids is inconsistent with a pelagic lifestyle. Moreover, caseid fossils are predominantly associated with arid upland deposits.


See also
  • Evolution of mammals
  • Vertebrate paleontology
  • Permian tetrapods


Bibliography


External links

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