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Pantosaurus striatus
Taxonomy
Parasaurus striatus was named by Marsh (1891). Its type specimen is YPM 543, a partial skeleton, and it is a 3D body fossil. Its type locality is Near Freezeout Mountain(s) [PROXY], which is in an Oxfordian marine horizon in the Sundance Formation of Wyoming. It is the type species of Parasaurus.
It was recombined as Pantosaurus striatus by Marsh (1895), Marsh (1897), Hay (1902), Williston (1903), Hay (1930), O'Keefe and Wahl (2003), Wilhelm and O'Keefe (2010).
It was recombined as Pantosaurus striatus by Marsh (1895), Marsh (1897), Hay (1902), Williston (1903), Hay (1930), O'Keefe and Wahl (2003), Wilhelm and O'Keefe (2010).
Synonyms
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Synonymy list
Year | Name and author |
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1895 | Pantosaurus striatus Marsh p. 338 |
1897 | Pantosaurus striatus Marsh p. 485 |
1902 | Pantosaurus striatus Hay p. 456 |
1903 | Pantosaurus striatus Williston p. 12 |
1912 | Muraenosaurus reedii Mehl p. 344 figs. 1, 3 |
1930 | Muraenosaurus reedii Hay p. 120 |
1930 | Pantosaurus striatus Hay p. 121 |
2003 | Pantosaurus striatus O'Keefe and Wahl pp. 37-38 |
2010 | Pantosaurus striatus Wilhelm and O'Keefe figs. 2-8 |
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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.
†Pantosaurus striatus Marsh 1891
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Invalid names: Muraenosaurus reedii Mehl 1912 [synonym]
Diagnosis
Reference | Diagnosis | |
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B. C. Wilhelm and F. R. O'Keefe 2010 | "A small cryptocleidoid plesiosaur possessing 35–40 cervical vertebrae. The cervical vertebrae are almost as long as they are wide, are waisted, and carry an elongate cervical rib articulation on a pedestal. Foramina subcentralia are small and placed closely together and the articular faces of the centra have well-ossified rims. Anterior neural spines are low, blade-like, and angled backward. Humerus with long, narrow shaft, radial articulation much longer than ulnar articulation; possessing an articulation for one supernumerary ossification in the epipodial row. Radius much longer and broader than ulna." |
Measurements
No measurements are available
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Source: o = order | |||||
Reference: Kiessling 2004 |
Age range: base of the Early/Lower Oxfordian to the top of the Oxfordian or 161.20000 to 157.30000 Ma
Collections (5 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Oxfordian | USA (Wyoming) | Pantosaurus striatus (96679 103921 119281) Pantosaurus striatus, Muraenosaurus reedii (type locality: 119282) | |
Early/Lower Oxfordian | USA (Wyoming) | Pantosaurus striatus (96690) |