Ruta, Marcello and Bolt, John R. (2006) A reassessment of the temnospondyl amphibian Perryella olsoni from the Lower Permian of Oklahoma. Transactions of the Royal Society of Edinburgh: Earth Sciences, 97 (2). pp. 113-165. ISSN 1755-6910

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Abstract

Additional mechanical preparation of the type material of the temnospondyl amphibian Perryella olsoni (Lower Permian, Wellington Formation, Oklahoma) highlights new cranial and postcranial features and provides additional data on previously known structures. Important new information is available for the quadrate, palatal bones and their associated dentition, parasphenoid, and appendicular skeleton. The revised diagnosis and redescription of Perryella provide the basis for a re-evaluation of its systematic affinities. A cladistic analysis of (mostly) Carboniferous and Permian temnospondyls, together with several Devonian and Carboniferous stem tetrapod outgroups, supports a single origin for temnospondyls. The sequence of branching events within temnospondyls consists of: (1) a paraphyletic Edopoidea; (2) a clade of Zatracheidae, Eryopidae, and basal Archegosauriformes; (3) a monophyletic Dvinosauria; and (4) a monophyletic Dissorophoidea. Perryella is nested within Dvinosauria in an intermediate position between Trimerorhachidae and Dvinosauroidea.

Item Type:	Article
Additional Information:	Additional mechanical preparation of the type material of the temnospondyl amphibian Perryella olsoni (Lower Permian, Wellington Formation, Oklahoma) highlights new cranial and postcranial features and provides additional data on previously known structures. Important new information is available for the quadrate, palatal bones and their associated dentition, parasphenoid, and appendicular skeleton. The revised diagnosis and redescription of Perryella provide the basis for a re-evaluation of its systematic affinities. A cladistic analysis of (mostly) Carboniferous and Permian temnospondyls, together with several Devonian and Carboniferous stem tetrapod outgroups, supports a single origin for temnospondyls. The sequence of branching events within temnospondyls consists of: (1) a paraphyletic Edopoidea; (2) a clade of Zatracheidae, Eryopidae, and basal Archegosauriformes; (3) a monophyletic Dvinosauria; and (4) a monophyletic Dissorophoidea. Perryella is nested within Dvinosauria in an intermediate position between Trimerorhachidae and Dvinosauroidea.
Keywords:	Carboniferous, characters, Dissorophoidea, Dvinosauroidea, phylogeny, Temnospondyli, Triassic, Trimerorhachidae
Subjects:	C Biological Sciences > C300 Zoology C Biological Sciences > C182 Evolution F Physical Sciences > F641 Palaeontology C Biological Sciences > C181 Biodiversity
Divisions:	College of Sciences > Faculty of Science > School of Life Sciences
Depositing User:	Marcello Ruta
Date Deposited:	28 Oct 2012 21:46
Last Modified:	13 Mar 2013 09:18
URI:	http://eprints.lincoln.ac.uk/id/eprint/6721

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