Biology:Seymouriamorpha

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Short description: Extinct order of amphibians

Seymouriamorpha
Temporal range: Late Carboniferous[1] - Late Permian
Seymouria1.jpg
Fossil of Seymouria in the National Museum of Natural History
Scientific classification e
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Reptiliomorpha
Order: Seymouriamorpha
Watson, 1917
Subgroups

See text.

Seymouriamorpha were a small but widespread group of limbed vertebrates (tetrapods). They have long been considered reptiliomorphs, and most paleontologists may still accept this point of view, but some analyses suggest that seymouriamorphs are stem-tetrapods (not more closely related to Amniota than to Lissamphibia).[2] Many seymouriamorphs were terrestrial or semi-aquatic. However, aquatic larvae bearing external gills and grooves from the lateral line system have been found, making them unquestionably amphibians. Though as they matured, they became more terrestrial and reptile-like. They ranged from 30 cm (1 ft) long lizard-sized creatures to the 1.5 m (5 ft) long Enosuchus. If seymouriamorphs are reptiliomorphs, they were the distant relatives of amniotes. Seymouriamorphs form into three main groups, Kotlassiidae, Discosauriscidae, and Seymouriidae, a group that includes the best known genus, Seymouria. The last seymouriamorph became extinct by the end of the Permian.[3]

Taxonomy

Cladogram based on Ruta, Jeffery, & Coates (2003):[5]

Seymouriamorpha

Kotlassia

Utegenia

Seymouria baylorensis

Seymouria sanjuanensis

Ariekanerpeton

Discosauriscus austriacus

Discosauriscus pulcherrimus

Cladogram based on Klembara (2009) & Klembara (2010):[6][7]

Seymouriamorpha

Utegenia

Seymouria

Karpinskiosaurus

Discosauriscidae

Makowskia

Spinarerpeton

Ariekanerpeton

Discosauriscus

Gallery

References

  1. Klembara, J.; Werneburg, R.; Mikudíková, M.; Šurka, J.; Štamberg, S. (2023). "The oldest records of the stem amniote Discosauriscus (Seymouriamorpha, Discosauriscidae) from the European Carboniferous-Permian boundary". Bulletin of Geosciences 98 (3): 233–246. doi:10.3140/bull.geosci.1882. 
  2. Laurin, Michel (2010). How Vertebrates Left the Water. Berkeley: University of California Press. ISBN 978-0-520-26647-6. 
  3. Bulanov, V. V. (2003). "Evolution and systematics of seymouriamorph parareptiles". Paleontological Journal 37 (Supplement 1): 1–105. 
  4. Olson, E. C. (1951). "Fauna of upper Vale and Choza: 1-5". Fieldiana Geology 10 (11): 89–128. doi:10.5962/bhl.title.3264. https://www.archive.org/download/faunaofuppervale1011olso/faunaofuppervale1011olso.pdf. 
  5. Ruta, M.; Jeffery, J. E.; Coates, M. I. (2003). "A supertree of early tetrapods". Proceedings of the Royal Society B 270 (1532): 2507–16. doi:10.1098/rspb.2003.2524. PMID 14667343. 
  6. Klembara, Jozef (2009). "The skeletal anatomy and relationships of a new discosauriscid seymouriamorph from the lower Permian of Moravia (Czech Republic)". Annals of Carnegie Museum 77 (4): 451–483. doi:10.2992/0097-4463-77.4.451. 
  7. Klembara, Jozef (2011). "The cranial anatomy, ontogeny, and relationships of Karpinskiosaurus secundus (Amalitzky) (Seymouriamorpha, Karpinskiosauridae) from the Upper Permian of European Russia". Zoological Journal of the Linnean Society 161 (1): 184–212. doi:10.1111/j.1096-3642.2009.00629.x. 

External links

Wikidata ☰ Q134777 entry