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Parareptilia

Parareptilia ("near-reptiles") is an extinct subclass of basal sauropsids ("reptiles"). Traditionally considered the sister taxon to Eureptilia, its validity as a monophyletic clade has been disputed by modern cladistic analyses.

Description
Skull '', a probable acleistorhinid from the Early Permian. Unlike most parareptiles, this species lacks tabular bones and has a heterodont dentition with large caniform teeth. Parareptilian skulls were diverse, from mesosaurs with elongated snouts filled with hundreds of thin teeth, to the snub-nosed, knob-encrusted skulls of pareiasaurs. "Parareptile" teeth were quite variable in shape and function between different species. However, they were relatively homogenous on the same skull. While most synapsids and many early eureptiles had a caniform region of enlarged fang-like teeth in the front half of the skull, very few "parareptiles" possessed caniform teeth. Many amniotes have a row of small pits running along bones at the edge of the mouth, but "parareptiles" have only a few pits, with one especially large pit near the front of the maxilla. When seen from above, the rear edge of the skull is straight or has a broad median embayment. Apart from the long, slender jaws of mesosaurs, most "parareptile" jaws were short and thick. The jaw joint is formed by the articular (in the lower jaw) and the quadrate (in the upper jaw). In many "parareptiles", the jaw joint is shifted forwards on the skull past the rear part of the braincase. Postcranial skeleton '', a procolophonid from the Middle Triassic of England There was some variation in the body shape of "parareptiles", with early members of the group having an overall lizard-like appearance, with thin limbs and long tails. The most successful and diverse groups of "parareptiles", the pareiasaurs and procolophonids, had massively-built bodies with reduced tails and stout limbs with short digits. This general body shape is shared with other "cotylosaurs" such as captorhinids, diadectomorphs, and seymouriamorphs. ==History of classification==
History of classification
The name Parareptilia was coined by Olson in 1947 to refer to an extinct group of Paleozoic reptiles, as opposed to the rest of the reptiles or Eureptilia ("true reptiles"). Olsen's term was generally ignored, and various taxa later known as "parareptiles" were generally not placed into exclusive groups with each other. Many were classified as "cotylosaurs" (a wastebasket taxon of stout-bodied "primitive" reptiles or reptile-like tetrapods) or "anapsids" (reptiles without temporal fenestrae, such as modern turtles). Parareptilia's usage was revived by cladistic studies, to refer to those traditional "anapsids" that were thought to be unrelated to turtles. Gauthier et al. (1988) provided the first phylogenetic definitions for the names of many amniote taxa and argued that captorhinids and turtles were sister groups, constituting the clade Anapsida (in a much more limited context than typically applied). A name had to be found for a clade of various early-diversing Permian and Triassic reptiles no longer included in the anapsids. Olsen's term "parareptiles" was chosen to refer to this clade, although its instability within their analysis meant that Gauthier et al. (1988) were not confident enough to erect Parareptilia as a formal taxon. Their cladogram is as follows: }} Laurin & Reisz (1995) found a slightly different topology, in which Reptilia is divided into Parareptilia and Eureptilia. They argued that Testudines (turtles) were members of Parareptilia; in fact, they explicitly defined Parareptilia as "Testudines and all amniotes more closely related to them than to diapsids". Captorhinidae was transferred to Eureptilia, while Parareptilia included turtles alongside many of the taxa named as such by Gauthier et al. (1988). There was one major exception: mesosaurs were placed outside both groups, as the sister taxon to the crown group Reptilia. Mesosaurs were still considered sauropsids, as they were closer to reptiles than to synapsids. The traditional group "Anapsida" was rejected as a paraphyletic assemblage. The cladogram of Laurin & Reisz (1995) is provided below: }} In contrast, several studies in the mid-to-late 1990s by Olivier Rieppel and Michael deBraga argued that turtles were actually lepidosauromorph diapsids related to the sauropterygians. The diapsid affinities of turtles have been supported by molecular phylogenies. The first genome-wide phylogenetic analysis was completed by Wang et al. (2013). Using the draft genomes of Chelonia mydas and Pelodiscus sinensis, the team used the largest turtle data set to date in their analysis and concluded that turtles are likely a sister group of crocodilians and birds (Archosauria). This placement within the diapsids suggests that the turtle lineage lost diapsid skull characteristics, since turtles possess an anapsid skull. This would make Parareptilia a totally extinct group with skull features that resemble those of turtles through convergent evolution. With turtles positioned outside of "parareptiles", Tsuji and Müller (2009) redefined Parareptilia as "the most inclusive clade containing Milleretta rubidgei and Procolophon trigoniceps, but not Captorhinus aguti." }} A 2020 study by David P. Ford and Roger B. J. Benson found that Parareptilia was nested within Diapsida as the sister group to Neodiapsida, with the clade containing Neodiapsida and Parareptilia dubbed Neoreptilia, which suggests that "parareptiles" were ancestrally diapsid. This excluded mesosaurs, which were again found to be basal among the sauropsids. More recent studies support this hypothesis, instead finding anatomical evidence placing millerettid "parareptiles" as sister to Neodiapsida, forming the clade Parapleurota. Cladogram after Jenkins et al. (2025), with traditional "parareptiles" highlighted in orange: }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} == Evolutionary history ==
Evolutionary history
The oldest known "parareptiles" are the bolosaur Erpetonyx and the acleistorhinid Carbonodraco from the Late Carboniferous (Moscovian-Gzhelian) of North America, which represents the only known Carboniferous "parareptiles", indicating that the initial diversification of the group took place in the Late Carboniferous. Numerous "parareptile" lineages appeared during the early Permian and the group reached a cosmopolitan distribution. "Parareptile" diversity declined towards the end of the Permian and procolophonoids, which first appeared during the Late Permian, were the only group of "parareptiles" to survive the Permian–Triassic extinction event. Procolophonid diversity sharply declined beginning in the Middle Triassic, with the group becoming extinct by the end of the Triassic. == References ==
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