GINGLYMOSTOMATIDAE GEN. ET SP. INDET.

Cicimurri, David J. & Knight, James L., 2019, Late Eocene (Priabonian) elasmobranchs from the Dry Branch Formation (Barnwell Group) of Aiken County, South Carolina, USA, PaleoBios 36, pp. 1-31 : 6

publication ID

https://doi.org/ 10.5070/P9361043964

publication LSID

lsid:zoobank.org:pub:3F95876E-933FF-48AF-9CF0-A840A333220B

DOI

https://doi.org/10.5281/zenodo.13750210

persistent identifier

https://treatment.plazi.org/id/03E787A6-FE2E-FF8E-AAB5-F9A8FE7EFDD7

treatment provided by

Felipe

scientific name

GINGLYMOSTOMATIDAE GEN. ET SP. INDET.
status

 

GINGLYMOSTOMATIDAE GEN. ET SP. INDET. View in CoL

( FIG. 2H View Figure 2 )

Referred specimen —SC2013.38.7, incomplete anterior tooth.

Remarks —This specimen differs from Nebrius sp. cf. Neb. thielensi (see above) in having only a single pair of large lateral cusplets, and the labial crown foot is distinctively bifid but not drawn out into an elongate basal protuberance. SC2013.38.7 is similar to the anterior teeth of Cretaceous Plicatoscyllium Case and Cappetta, 1997 , but there is no indication of labial crown ornamentation. The single pair of lateral cusplets also distinguishes SC2013.38.7 from the various early Paleogene species of Ginglymostoma (Noubhani and Cappetta 1997) . In terms of gross morphology, SC2013.38.7 is similar to Protoginglymostoma ypresiensis ( Casier, 1946) from the early to middle Eocene of Belgium and Morocco ( Casier 1946, Herman 1977, Tabuce et al. 2005), but the poor condition of the only available tooth makes a more precise identification difficult.

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