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Contents

   



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1 Taxonomy  





2 Gallery  





3 References  





4 External links  














Seymouriamorpha






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From Wikipedia, the free encyclopedia
 


Seymouriamorpha

Temporal range: Late Carboniferous[1] - Late Permian

Fossil of Seymouria in the National Museum of Natural History
Scientific classification Edit this classification
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 stem-amniotes (reptiliomorphs), and most paleontologists 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[edit]

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

Seymouriamorpha

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

Gallery[edit]

References[edit]

  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.
  • ^ Laurin, Michel (2010). How Vertebrates Left the Water. Berkeley: University of California Press. ISBN 978-0-520-26647-6.
  • ^ Bulanov VV (2003). "Evolution and systematics of seymouriamorph parareptiles". Paleontological Journal. 37 (Supplement 1): 1–105.
  • ^ Olson, E. C. (1951). "Fauna of upper Vale and Choza: 1-5" (PDF). Fieldiana Geology. 10 (11): 89–128. doi:10.5962/bhl.title.3264.
  • ^ 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. PMC 1691537. PMID 14667343.
  • ^ 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.
  • ^ Klembara, Jozef (2011). "The cranial anatomy, ontogeny, and relationships of Karpinskiosaurus secundus (Amalitzky) (Seymouriamorpha, Karpinskiosauridae) from the Upper Permian of European Russia" (PDF). Zoological Journal of the Linnean Society. 161 (1): 184–212. doi:10.1111/j.1096-3642.2009.00629.x.
  • External links[edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Seymouriamorpha&oldid=1215522417"

    Categories: 
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    Pennsylvanian first appearances
    Lopingian extinctions
    Prehistoric tetrapod orders
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    This page was last edited on 25 March 2024, at 17:04 (UTC).

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