Rhinoptera, Cuvier, 1829
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-FF88-4E13-1EB7-F9C7FA17FCAF |
treatment provided by |
Felipe |
scientific name |
Rhinoptera |
status |
|
Rhinoptera View in CoL cf. R. studeri (Agassiz, 1843)
Fig. 6G View Fig .
Referred specimens.—BCGM 9122 and 9123, SC 2009.18.24.
Comments.—These teeth differ from those of Myliobatinae gen. indet. in having labial and lingual crown ornamentation consisting of fine vertical wrinkles (as opposed to having a granular texture), and the lingual basal ridge is thick and rounded (as opposed to rather narrow and sharp). In these respects, the Chandler Bridge teeth are quite similar to Rhinoptera studeri from the European Miocene ( Leriche 1927; Cappetta 1970, 1987), but a specific assignment cannot be made with confidence because our sample size is small and the material incomplete. A specimen from the Belgrade Formation of North Carolina was identified as Rhinoptera aff. R. bonasus Mitchill, 1815 by Müller (1999: pl. 15: 7), but it does not appear to be different than a tooth of R. studeri illustrated by Leriche (1927: pl. 6: 3). Other teeth from the Belgrade Formation were identified as Rhinoptera aff. R. brasiliensis Müller, 1835 by Müller (1999: pl. 15: 4, 5), but the inter− and intraspecific variation in extant Rhinoptera (i.e., Cappetta 1987) suggests that only a single species was present during deposition of the Belgrade Formation. The North Carolina and Chandler Bridge specimens appear to be conspecific, but a larger sample is needed to make a more accurate determination. Rhinoptera may have been more widespread during the Oligocene than previously indicated, as Rupelian specimens identified as Myliobatis by Genault (1993: figs. 65, 66), Baut and Génault (1999: pl. 7: 3), and Reinecke et al. (2001: pl. 55: A, B) possess the same attributes as Chandler Bridge teeth we refer to Rhinoptera .
Stratigraphic and geographic range.—?Oligocene (Chattian), USA (North and South Carolina); Miocene, Europe.
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