Squatina sp.
publication ID |
https://doi.org/ 10.4202/app.2012.0123 |
persistent identifier |
https://treatment.plazi.org/id/C45E8796-6974-1978-FC91-3DA3FD0DB0A1 |
treatment provided by |
Felipe |
scientific name |
Squatina sp. |
status |
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Fig. 3I–J View Fig .
Material.—Four teeth collected from the Ce of Stevns Kridtbrud (MGUH 29836, MGUH 29837, GMV2012-64 [batch number]) and a few specimens in private collections from the Br2 of Faxe.
Description.—Monocuspid teeth with a long narrow elongat- ed main cusp with continuous cutting edges. The shoulders are almost horizontal and long and low. The labial face of the crown is convex and smooth, with a well-demarcated apron that projects below the basal face of the root. The lingual face of the crown is strongly convex and smooth. The labial face of the root is low and wide and the basal face of the root is flat. The lingual face of the root has a protuberance with a foramen and several foramina below the crown-root junction on the shoulders.Teeth reaching 2.7 mm in height and 3 mm in width.
Remarks.—The separation of individual species of Squatina is extremely difficult ( Dalinkevičius 1935; Cappetta 1987; Rees 2005). Squatina cranei ( Woodward 1888) and S. decipiens ( Dalinkevičius 1935) from the Late Cretaceous and earliest Paleocene were demonstrated to be synonyms ( Guinot et al. 2012), the former being based on the teeth of juveniles and the latter, adults. This species demonstrates a higher degree of heterodonty than seen in Recent Squatina and was therefore placed in a separate subgenus, Cretascyllium Guinot et al. 2012 . It is probable that these specimens belong to S. cranei , however, while evidence of the heterodonty is absent from these specimens, they are better left in open nomenclature.
Stratigraphic and geographic range.— Squatina ranges from the late Jurassic to Recent, Worldwide. It is most likely that it will be subdivided into separate genera or subgenera.
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