Araeoscelidians were small animals (less than one meter in length) looking somewhat like lizards, though they are only distantly related to true lizards. They differ from other, earlier sauropsids by their slender limbs, their elongated tail, and of course by the presence of two temporal openings, the feature defining the diapsid condition. In Araeoscelis, only the upper temporal opening remains, thus resulting in a derived euryapsid condition.
Genera
Araeoscelidia includes well-known genera such as Araeoscelis Williston 1910,[1][2]Petrolacosaurus Lane 1945[3][4] and Spinoaequalis,[5][6] known from virtually complete skeletons. Zarcasaurus,[7]Aphelosaurus[8][9][10] and Kadaliosaurus[11] belong to this clade but are known only from post-cranial remains and a mandible fragment for Zarcasaurus.
The genus Dictybolos has been included in Araeoscelidia by Olson (1970)[12] but this inclusion has been criticized e.g., by Evans (1988),[13] especially since Olson also included distantly related groups such as protorosaurs and mesosaurs.
New specimens have been discovered in the United States state of Oklahoma,[14][15] but lack a scientific description as of 2023.
Phylogeny
The majority of phylogenetic studies recover araeoscelidians as the most basal group of diapsids; however, Simões et al. (2022) recover them as stem-amniotes instead, as the sister group to the clade including Captorhinidae and Protorothyris archeri.[16]
Stratigraphic and geographic distribution
Araeoscelidia are known from the Late Carboniferous in the United States (Petrolacosaurus, Spinoaequalis) to the Early Permian in France (Aphelosaurus), Germany (Kadaliosaurus) and the United States (Dictybolos, Zarcasaurus, Araeoscelis, Halgaitosaurus[17]). Apart from araeoscelidans, only one other diapsid is known before the Late Permian: Orovenator from the Early Permian of Oklahoma.[18]
Credner, H. (1889). "Die Stegocephalen und Saurier aus dem Rothliegenden des Plauen'schen Grundes bei Dresden. 8 – Kadaliosaurus priscus Cred". Zeitschrift der Deutschen Geologischen Gesellschaft. 41: 319–342.
Evans, S. E. (1988). "The early history and relationships of the Diapsida". In Benton, M. J. (ed.). The phylogeny and classification of the tetrapods. Vol. 1: Amphibians, Reptiles, Birds. Systematics Association Special Volume 35 A. Oxford: Clarendon Press. pp. 221–260. ISBN0-19-857705-2.
Falconnet, J. & Steyer, J.-S. (2007). "Revision, osteology and locomotion of Aphelosaurus, an enigmatic reptile from the Lower Permian of France". Journal of Morphology (abstract of the 8th International Congress of Vertebrate Morphology, Paris, July 2007): 38.
Gervais, P. (1859). Zoologie et paléontologie française (2nd ed.). Paris: Bertrand.
Laurin, M. (1991). "The osteology of a Lower Permian eosuchian from Texas and a review of a diapsid phylogeny". Zoological Journal of the Linnean Society. 101: 59–95. doi:10.1111/j.1096-3642.1991.tb00886.x.
May, W. J. & Hall, J. D. (2002). "Geology and vertebrate fauna of a new site in the Wellington Formation (Lower Permian) of Northern Oklahoma". Oklahoma Geology Notes. 62 (2): 63–66.
Olson, E. C. (1970). "New and little known genera and species of vertebrates from the Lower Permian of Oklahoma". Fieldiana: Geology. 18: 359–434.
Peabody, F. E. (1952). "Petrolacosaurus kansensis Lane, a Pennsylvanian reptile from Kansas". University of Kansas Paleontological Contributions. 10: 1–41. hdl:1808/3785.
Reisz, R. R.; Berman, D. S. & Scott, D. (1984). "The anatomy and relationships of the Lower Permian reptile Araeoscelis". Journal of Vertebrate Paleontology. 4 (1): 57–67. doi:10.1080/02724634.1984.10011986.
