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Cornwallius sookensis
Taxonomy
Desmostylus sookensis was named by Cornwall (1922). Its type specimen is BCPM 486, a tooth, and it is a 3D body fossil. Its type locality is Kirby Creek, east, which is in a Chattian marine sandstone in the Sooke Formation of Canada.
It was recombined as Cornwallius sookensis by Hay (1923), Hay (1930), VanderHoof (1937), VanderHoof (1942), Reinhart (1959), Shikama (1966), Domning (1996), Domning (2008), Beatty (2009), Matsui and Tsuihiji (2019), Beatty (2023).
It was recombined as Cornwallius sookensis by Hay (1923), Hay (1930), VanderHoof (1937), VanderHoof (1942), Reinhart (1959), Shikama (1966), Domning (1996), Domning (2008), Beatty (2009), Matsui and Tsuihiji (2019), Beatty (2023).
Synonymy list
Year | Name and author |
---|---|
1922 | Desmostylus sookensis Cornwall p. 122 |
1923 | Desmostylus sookensis Clark and Arnold p. 177 |
1923 | Cornwallius sookensis Hay p. 106 |
1930 | Cornwallius sookensis Hay p. 654 |
1937 | Cornwallius sookensis VanderHoof p. 191 |
1942 | Cornwallius sookensis VanderHoof p. 301 |
1959 | Cornwallius sookensis Reinhart p. 66 |
1966 | Cornwallius sookensis Shikama p. 156 |
1996 | Cornwallius sookensis Domning p. 394 |
2008 | Cornwallius sookensis Domning p. 642 |
2009 | Cornwallius sookensis Beatty p. 896 |
2019 | Cornwallius sookensis Matsui and Tsuihiji |
2023 | Cornwallius sookensis Beatty |
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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.
†Cornwallius sookensis Cornwall 1922
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Diagnosis
Reference | Diagnosis | |
---|---|---|
B. L. Beatty 2009 | Apomorphies of taxon: dental formula is 2.1.2?.3/1.1.1?.3;.
Differs from Behemotops in: molars with longitudinal rows of columnar cusps that are closely appressed to each other; molars lacking labial or lingual cingula; molars, specifically M3 and m3, have styles/stylids in between the main cusps/cuspids, not large enough to qualify as extra cusps themselves, and these styles/ stylids vary in size between left and right teeth; postorbital process of the jugal; coronoid process of mandible is more strongly posterior inclined. Differs from Paleoparadoxia in: molars lacking labial or lingual cingula; molars with thicker enamel; postorbital process of the jugal; juvenile mandibles have a posterior thickening of the symphysis; coronoid process of mandible is more strongly posterior inclined. Differs from Desmostylus in:molars brachydont; postorbital process does not contact the zygomatic process of the squamosal since the zygomatic process of the squamosal is not dorsoventrally expanded. |