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Pelodosotis elongatum

Ostodolepidae

Taxonomy
Pelodosotis elongatum was named by Carroll and Gaskill (1978). Its type specimen is UMMP 11156, a skeleton, and it is a 3D body fossil. Its type locality is Coffee Creek, 34 (Arroyo Formation), which is in a Kungurian terrestrial claystone/sandstone in the Arroyo Formation of Texas.

Synonymy list
YearName and author
1978Pelodosotis elongatum Carroll and Gaskill p. 78 figs. 48-51, 58
1998Pelodosotis elongatum Carroll et al. p. 51

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RankNameAuthor
kingdomAnimalia()
—Bilateria
—EubilateriaAx 1987
—Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
—Osteichthyes()
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
RankNameAuthor
—Tetrapoda
—Reptiliomorpha
—Anthracosauria
subclassAmphibiosauriaKuhn 1967
—Cotylosauria()
—Amniota
—RecumbirostraAnderson 2007
familyOstodolepidaeRomer 1945
genusPelodosotis
specieselongatum

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

†Pelodosotis elongatum Carroll and Gaskill 1978
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialuc
Locomotion: actively mobilec
Created: 2017-04-17 15:15:35
Modified: 2017-04-17 15:15:35
Source: c = class, subp = subphylum, uc = unranked clade
References: Hendy et al. 2009, Carroll 1988

Age range: Kungurian or 279.30000 to 272.30000 Ma

Collections: one only


Time interval Ma Country or state Original ID and collection number
Kungurian279.3 - 272.3USA (Texas) Pelodosotis elongatum (type locality: 28256)