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Oryctodromeus cubicularis
Taxonomy
Oryctodromeus cubicularis was named by Varricchio et al. (2007). Its type specimen is MOR 1636a, a partial skeleton, and it is a 3D body fossil. Its type locality is Lima Peaks (MOR), which is in an Albian floodplain mudstone/sandstone in the Blackleaf Formation of Montana.
Synonymy list
| Year | Name and author |
|---|---|
| 2007 | Oryctodromeus cubicularis Varricchio et al. p. 1361 figs. 2-4 |
| 2010 | Oryctodromeus cubicularis Krumenacker p. 59 |
| 2012 | Oryctodromeus cubicularis Ullmann et al. p. 311 |
| 2013 | Oryctodromeus cubicularis Brown et al. p. 504 |
| 2017 | Oryctodromeus cubicularis Krumenacker et al. p. 170 |
| 2018 | Oryctodromeus cubicularis Bell et al. p. 27 |
| 2018 | Oryctodromeus cubicularis Herne et al. p. 45 |
| 2019 | Oryctodromeus cubicularis Andrzejewski et al. p. 23 |
| 2019 | Oryctodromeus cubicularis Cruzado-Caballero et al. p. 216 |
| 2019 | Oryctodromeus cubicularis Párraga and Prieto-Márquez p. 251 |
| 2020 | Oryctodromeus cubicularis Yang et al. p. 4 |
| 2021 | Oryctodromeus cubicularis Duncan et al. p. 2 |
| 2022 | Oryctodromeus cubicularis Krumenacker et al. p. 1339 |
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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.
†Oryctodromeus cubicularis Varricchio et al. 2007
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| L. J. Krumenacker 2010 | Autapomorphic features of Oryctodromeus cubicularis: long paraoccipital processes indicating a skull with relatively broad proportions; basioccipital with a steeply sided ventral 'box' just rostral to the occipital condyle, seven sacral vertebrae, including two sacralized posterior dorsals and their ribs; large scapula with a sharply angled and narrow acromion process bearing a thin-edged laterally projecting scapular spine and a distinct posterior bend to the scapular blade; ilium with very short pre-acetabular and long post-acetabular portions; brevis shelf slopes mediolaterally and is visible laterally throughout its length; and long prepubic process with a transversely broad proximal portion possessing an elongate ventral fossa (Varricchio et al., 2007). |