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Riparovenator milnerae
Taxonomy
Riparovenator milnerae was named by Barker et al. (2021). Its type specimen is IWCMS 2014.95.6, IWCMS 2014.96.1, 2; 2020.448.1, 2, IWCMS 2014.96.3, a partial skeleton, and it is a 3D body fossil. Its type locality is east of Chilton Chine, which is in a Barremian fluvial sandstone in the Wessex Formation of the United Kingdom. It is the type species of Riparovenator.
Synonymy list
Year | Name and author |
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2021 | Riparovenator milnerae Barker et al. p. 4 |
2023 | Riparovenator milnerae Barker et al. p. 2 |
2023 | Riparovenator milnerae Santos-Cubedo et al. p. 1 |
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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.
†Riparovenator milnerae Barker et al. 2021
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Diagnosis
Reference | Diagnosis | |
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C. T. Barker et al. 2021 | Baryonychine distinguished by the presence of the following unique traits: notched dorsal orbital
margin between prefrontal and postorbital process of the frontal; deeply inset facial nerve (CN VII) foramen that is largely obscured from lateral view; deep subcondylar recess (depth over 1/3 of its mediolateral width; depth less than 1/5 in other baryonychines); reduced exposure of ventral surface of the basipterygoid processes in lateral view. This taxon can be further separated from other baryonychines by the following combination of traits: curved dorsal margin of the frontal process of the nasal in lateral view (margin effectively straight in Baryonyx); straight dorsal margin of the dorsum sellae (V-shaped in Baryonyx and Ceratosuchops); exoccipital components of the occipital condyle closely spaced (as in Ceratosuchops and cf. Suchomimus but not Baryonyx); mediolaterally thick crests bordering the subcondylar recess (as in Baryonyx but not Ceratosuchops or cf. Suchomimus); lateral margins of the basipterygoid processes concave in ventral view. |
Measurements
No measurements are available
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Source: o = order | |||||
Reference: Marsh 1875 |