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Cimolodon peregrinus
Taxonomy
Cimolodon peregrinus was named by Donohue et al. (2013). Its type specimen is UW 15583, a mandible (right dentary fragment with p4), and it is a 3D body fossil. Its type locality is Dino Ray UW V-79033, which is in a Lancian terrestrial sandstone in the Lance Formation of Wyoming.
Synonymy list
Year | Name and author |
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2013 | Cimolodon peregrinus Donohue et al. p. 683 figs. 5E-F |
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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.
†Cimolodon peregrinus Donohue et al. 2013
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Diagnosis
Reference | Diagnosis | |
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S. L. Donohue et al. 2013 | Differing from Mesodma thompsoni in: larger p4 with greater number of serrations (16), arcuate mesial face (larger L2:L ratio). Differing from Cimolodon nitidus and Anconodon gidleyi in: large p4 (L = 7.00 mm) with greater number of serrations, gently sloping, rounded mesial face (smaller L2:L ratio), lower crown (smaller H:L ratio), and a smaller mesiobuccal lobe. Differing from C. similis and C. foxi in: larger p4 with greater number of serrations, lower crown (smaller H:L ratio). Differing from Meniscoessus robustus and M. seminoensis in: p4 with rounded, muted serrations, greater number of serrations, arcuate mesial face (larger L2:L ratio), lack of a notched first serration, and overall less robust crown. |
Measurements
No measurements are available
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Source: f = family, subo = suborder, c = class, subp = subphylum | |||||
References: Carroll 1988, Hendy et al. 2009, Hopson 1973, Gunnell et al. 1995, Krause 1982 |