Biology:Araeoscelidia
| Araeoscelidans | |
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| Life restoration (top) and skull reconstruction (bottom) of Petrolacosaurus kansensis | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Clade: | Diapsida |
| Order: | †Araeoscelidia Williston, 1913 |
| Genera | |
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Araeoscelidia or Araeoscelida is a clade of extinct diapsid reptiles superficially resembling lizards, extending from the Late Carboniferous to the Early Permian. The group contains the genera Araeoscelis, Petrolacosaurus, the possibly aquatic Spinoaequalis, and less well-known genera such as Kadaliosaurus and Zarcasaurus. This clade is usually considered to be the sister group to all (currently known) later diapsids.
Description
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]
References
- ↑ Vaughn 1955
- ↑ Reisz, Berman & Scott 1984
- ↑ Peabody 1952
- ↑ Reisz 1981
- ↑ deBraga & Reisz 1995
- ↑ deBraga & Rieppel 1997
- ↑ Brinkman, Berman & Eberth 1984
- ↑ Gervais 1859
- ↑ Thévenin 1910
- ↑ Falconnet & Steyer 2007
- ↑ Credner 1889
- ↑ Olson 1970
- ↑ Evans 1988
- ↑ May & Hall 2002
- ↑ Swanson & Carlson 2002
- ↑ Simões, T. R.; Kammerer, C. F.; Caldwell, M. W.; Pierce, S. E. (2022). "Successive climate crises in the deep past drove the early evolution and radiation of reptiles". Science Advances 8 (33): eabq1898. doi:10.1126/sciadv.abq1898. PMID 35984885.
- ↑ Henrici, Amy C.; Berman, David S; Sumida, Stuart S.; Huttenlocker, Adam K. (2023-11-15). "Halgaitosaurus gregarius, a New Upper Carboniferous Araeoscelidian (Reptilia: Diapsida) from the Halgaito Formation, Bears Ears National Monument, Utah, USA". Annals of Carnegie Museum 88 (3). doi:10.2992/007.088.0301. ISSN 0097-4463. https://bioone.org/journals/annals-of-carnegie-museum/volume-88/issue-3/007.088.0301/Halgaitosaurus-gregarius-a-New-Upper-Carboniferous-Araeoscelidian-Reptilia--Diapsida/10.2992/007.088.0301.full.
- ↑ Reisz, Modesto & Scott 2011
Further reading
- Carroll, Robert L. (1988). Vertebrate Paleontology and Evolution. New York: W.H. Freeman and Co. ISBN 0-7167-1822-7. https://archive.org/details/vertebratepaleon0000carr.
- Benton, Michael J. (2000). Vertebrate Paleontology (2nd ed.). Oxford: Blackwell Science. ISBN 0-632-05614-2.
- deBraga, M.; Reisz, R. R. (1995). "A new diapsid reptile from the uppermost Carboniferous (Stephanian) of Kansas". Palaeontology 38: 199–212.
- deBraga, M.; Rieppel, O. (1997). "Reptile phylogeny and the interrelationships of turtles". Zoological Journal of the Linnean Society 120 (3): 281–354. doi:10.1111/j.1096-3642.1997.tb01280.x.
- Brinkman, D. B.; Berman, D. S.; Eberth, D. Z. (1984). "A new araeoscelid reptile, Zarcasaurus tandyderus, from the Culter Formation, (Lower Permian) of north-central New Mexico". New Mexico Geology 6 (2): 34–39. https://geoinfo.nmt.edu/publications/periodicals/nmg/6/n2/nmg_v6_n2_p34.pdf.
- 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.. The phylogeny and classification of the tetrapods. 1: Amphibians, Reptiles, Birds. Systematics Association Special Volume 35 A. Oxford: Clarendon Press. pp. 221–260. ISBN 0-19-857705-2.
- 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.
- Reisz, R. R. (1981). "A diapsid reptile from the Pennsylvanian of Kansas". Special Publication of the Museum of Natural History, University of Kansas 7: 1–74. https://www.biodiversitylibrary.org/bibliography/8440.
- 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.
- Reisz, Robert R.; Modesto, Sean P.; Scott, Diane M. (2011). "A new Early Permian reptile and its significance in early diapsid evolution". Proceedings of the Royal Society B 278 (1725): 3731–3737. doi:10.1098/rspb.2011.0439. PMID 21525061.
- Swanson, B. A.; Carlson, K. J. (2002). "Walk, Wade, or Swim? Vertebrate Traces on an Early Permian Lakeshore". PALAIOS 17 (2): 123–133. doi:10.1669/0883-1351(2002)017<0123:WWOSVT>2.0.CO;2. Bibcode: 2002Palai..17..123S. http://doc.rero.ch/record/14748/files/PAL_E1875.pdf.
- Thévenin, A. (1910). "Les plus anciens quadrupèdes de France". Annales de Paléontologie 5: 1–65.
- Vaughn, P. P. (1955). "The Permian reptile Araeoscelis restudied". Bulletin of the Harvard Museum of Comparative Zoology 113: 305–467.
Wikidata ☰ Q136663 entry
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