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Stegopelta landerensis
Taxonomy
Stegopelta landerensis was named by Williston (1905). Its type specimen is FMNH UR88, a partial skeleton (?maxilla with three partial alveoli, ?indeterminate skull fragments, seven cervical vertebrae, two dorsal vertebrae, portions of the synsa- crum, proximal cauda), and it is a 3D body fossil. Its type locality is Conant Creek, Lander, which is in a Cenomanian estuary/bay shale/claystone in the Frontier Formation of Wyoming. It is the type species of Stegopelta. It was considered monophyletic by Vickaryous et al. (2004).
Synonymy list
Year | Name and author |
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1905 | Stegopelta landerensis Williston |
1915 | Stegopelta landerensis Hennig p. 13 |
1930 | Stegopelta landerensis Hay p. 232 |
1930 | Stegopelta landerensis Russell p. 138 |
1940 | Stegopelta landerensis Russell p. 23 |
1964 | Stegopelta landerensis Kuhn p. 52 |
1970 | Stegopelta landerensis Bodily p. 37 |
1996 | Stegopelta landerensis Coombs, Jr. and Deméré p. 319 |
1998 | Stegopelta landerensis Carpenter and Kirkland p. 263 |
2000 | Stegopelta landerensis Ford p. 171 |
2001 | Stegopelta landerensis Blows p. 378 |
2001 | Stegopelta landerensis Carpenter p. 457 |
2001 | Stegopelta landerensis Carpenter et al. p. 213 |
2001 | Stegopelta landerensis Ford and Kirkland p. 256 |
2004 | Stegopelta landerensis Vickaryous et al. p. 367 |
2009 | Stegopelta landerensis Osi and Makádi p. 236 fig. 7 |
2013 | Stegopelta landerensis Kirkland et al. p. 7 |
2014 | Stegopelta landerensis Blows p. 59 fig. 3 |
2016 | Stegopelta landerensis Arbour and Currie p. 395 |
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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.
†Stegopelta landerensis Williston 1905
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Diagnosis
Reference | Diagnosis | |
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V. M. Arbour and P. J. Currie 2016 | Differs from all other ankylosaurs in possessing the following combination of characters: pelvic shield composed of hexagonal co-ossified osteoderms; cervical half ring osteoderms not fused to an underlying band. Differs from Glyptodontopelta in the surface texture of the pelvic osteoderms, which lack the dendritic texture present in Glyptodontopelta. |
Measurements
No measurements are available
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Source: o = order | |||||
References: Marsh 1875, Kiessling 2004 |
Age range: Early/Lower Cenomanian or 100.50000 to 93.90000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Early/Lower Cenomanian | USA (Wyoming) | Stegopelta landerensis (type locality: 27889) |