Plinthicus, COPE, 1869

Adnet, Sylvain, Cappetta, Henri, Guinot, Guillaume & Sciara, Giuseppe Notarbartolo Di, 2012, Evolutionary history of the devilrays (Chondrichthyes: Myliobatiformes) from fossil and morphological inference, Zoological Journal of the Linnean Society 166 (1), pp. 132-159 : 141

publication ID

https://doi.org/ 10.1111/j.1096-3642.2012.00844.x

DOI

https://doi.org/10.5281/zenodo.5479982

persistent identifier

https://treatment.plazi.org/id/A260879A-FFCF-A21D-FC4C-886C32EC01B9

treatment provided by

Marcus

scientific name

Plinthicus
status

 

GENUS † PLINTHICUS COPE, 1869

Included species: † Plinthicus stenodon ( Cope, 1869) ; † Plinthicus kruibekensis Bor, 1990 .

Occurrences: Genus known from the Rupelian of the Boom Clay Formation, Belgium ( Bor, 1990) and Late Chattian of South Carolina, USA ( Cicimurri & Knight, 2009), until the middle Miocene of southern France ( Cappetta, 1970) and of Maryland and North Carolina, USA ( Cope, 1869; Müller, 1999; Purdy et al., 2001).

Remarks: The extinct genus † Plinthicus Cope, 1869 was tentatively placed in the mobulids ( Cappetta, 1987; Cappetta & Stringer, 2002) although these teeth recall those of some rhinopterids ( Purdy et al., 2001; Cicimurri & Knight, 2009). The largest species † P. stenodon ( Cope, 1869) appears to have had a rhinopterid-type dentition with multiple, weakly interlocked columns of teeth. Most striking in these teeth is the 45° angle of recline seen in lateral profile, the concave occlusal surface, and the labiolingually compressed root with regular and fine root lamellae. The species † P. kruibekensis Bor, 1990 is known from a unique tooth that strongly differs from the younger species by a flat occlusal surface (as in some Mobula ), a concave lingual face (as in † Mo. fragilis ), and anastomosing enameloid laminae on the labial and lingual faces of crown.

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