Centetodon pulcher Marsh, 1872b

Murphey, Paul C. & Kelly, Thomas S., 2017, Mammals from the earliest Uintan (middle Eocene) Turtle Bluff Member, Bridger Formation, southwestern Wyoming, USA, Part 2: Apatotheria, Lipotyphla, Carnivoramorpha, Condylartha, Dinocerata, Perissodactyla and Artiodactyla, Palaeontologia Electronica (Cambridge, England: 2003) 20 (2), pp. 1-51 : 14

publication ID

https://doi.org/ 10.26879/720

publication LSID

lsid:zoobank.org:pub:341D2FE3-977D-4C82-A337-C681FC00C53A

persistent identifier

https://treatment.plazi.org/id/BB4187B4-FF97-FF8A-FED9-76E2FB41FBC4

treatment provided by

Felipe

scientific name

Centetodon pulcher Marsh, 1872b
status

 

Centetodon pulcher Marsh, 1872b

Figure 6.5-10 View FIGURE 6 View FIGURE 7 View FIGURE 8 View FIGURE 9 View FIGURE 10 , Table 2

Referred specimens. From DMNH Locality 4672: Rm2, DMNH 75327. From UCM Locality 92189: Lp4, UCM 68534; partial dentary with Lp4-m1,

UCM 95767; partial dentary with Lp1 and p4-m3, UCM 68963; Rp4, UCM 67889; Rm1 or 2, UCM 95768; Rm3s, UCM 69968, 95682.

Description. The p4-m3 of Centetodon pulcher have been well described in the literature ( McKenna, 1960b; McKenna et al., 1962; West, 1973a; Lillegraven et al., 1981) and the new specimens from the TBM do not provide any additional information, so detailed descriptions of them are not necessary. However, to the best of our knowledge, the p1 of C. pulcher has not been previously described. The p1 is moderately worn. It has two roots that are about equal in size and inclined anteriorly. The crown is anteroposteriorly elongated, transversely compressed, and procumbent with the apex of the primary cusp positioned anteriorly. A short ridge is present that extends anteriorly from the primary cusp to terminate as what appears to be an incipient cuspid, but this may just be an artifact of wear. A long, wedge-shaped, slightly convex ridge extends posteriorly from the apex of the primary cusp to terminate at a small posterior accessory cuspid. A labial cingulid is lacking.

Remarks. The eight Centetodon specimens from the TBM are significantly larger than those referred above to C. bemicophagus ( Table 2). In size and occlusal morphology, they are indistinguishable from those of C. pulcher ( Lillegraven et al., 1981) and are referred to the species.

DMNH

Delaware Museum of Natural History

UCM

University of Colorado Museum of Natural History

Kingdom

Animalia

Phylum

Chordata

Class

Mammalia

Family

Geolabididae

Genus

Centetodon

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