Sphyrna Rafinesque, 1810

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 : 635

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-FF8E-4E15-1EB7-FDE3FE5BFAD3

treatment provided by

Felipe

scientific name

Sphyrna Rafinesque, 1810
status

 

Genus Sphyrna Rafinesque, 1810 View in CoL

Type species: Squalus zygaena Linneaus, 1758 , Recent, “Europe, America”.

Sphyrna cf. S. media Springer, 1940

Fig. 5K View Fig .

Referred specimens.— BCGM 9075–9077, SC 2009.18.11.

Comments.—Our sample compares favorably to material identified as Sphyrna cf. S. media by Purdy et al. (2001). We concur with Purdy et al. (2001) that S. arambourgi Cappetta, 1970 (pl. 19: 3–16) is indistinguishable from teeth they identify as Sphyrna cf. S. media . Based on overall size, cusp morphology, and elongated, low distal heel, we believe that specimens identified as Scoliodon terraenovae (Richardson, 1836) by Case (1980: pl. 7: 1, 2) are assignable to Sphyrna cf. S. media . The morphology and size of the tooth identified as Rhizoprionodon by Génault (1993: figs. 61, 62) also appears to be closer to S. media . Maximum tooth width of Sphyrna cf. S. media in our sample is approximately 10 mm, and they differ from those of S. zygaena (Linnaeus, 1758) in being smaller in size, having a much more gracile cusp, and mesial cutting edges are straight to concave.

Stratigraphic and geographic range.—Oligocene, USA (North and South Carolina), France (?); Miocene, USA (North Carolina), France.

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