Rhizoprionodon sp.

Cicimurri, David J. & Knight, James L., 2009, Late Oligocene sharks and rays from the Chandler Bridge Formation, Dorchester County, South Carolina, USA, Acta Palaeontologica Polonica 54 (4), pp. 627-647 : 634

publication ID

https://doi.org/ 10.4202/app.2008.0077

publication LSID

lsid:zoobank.org:pub:3D85D369-7A74-44B6-9766-7C4B8B26705B

persistent identifier

https://treatment.plazi.org/id/03A6C023-FF81-4E1A-1E7D-FDC9FD56FB8E

treatment provided by

Felipe

scientific name

Rhizoprionodon sp.
status

 

Rhizoprionodon sp.

Fig. 5H View Fig .

Referred specimens.—BCGM 9069 and 9070, SC 2009.18.9.

Comments.—These teeth are small (6 mm in total width) and imperfectly preserved, making it difficult to distinguish them from similarly toothed sharks like Sphyrna and even Physogaleus . Teeth of all of these taxa can have highly concave mesial cutting edges, as is the case with our specimens. Our specimens lack cusplets as seen on the distal blade of Physogaleus . Teeth of Sphyrna media Springer, 1940 can have concave mesial edges and convex distal heel, but we identify our specimens as Rhizoprionodon because the mesial edge is very concave, with the cusp being narrower and cusp apex more vertically oriented. Our teeth are similar to Oligocene specimens from North Carolina identified as R. fischeuri ( Müller 1999: pl. 8: 2–4), but a larger sample is needed to accurately determine the identity of these Chandler Bridge teeth.

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