Otodus (Carcharocles) cf. sokolowi (Jaekel, 1895)
publication ID |
https://doi.org/ 10.5252/geodiversitas2021v43a5 |
publication LSID |
urn:lsid:zoobank.org:pub:697FC553-E37B-4EF9-97A4-950E4DEE246C |
DOI |
https://doi.org/10.5281/zenodo.4606609 |
persistent identifier |
https://treatment.plazi.org/id/03923C45-FF87-FF8E-30A4-FAACFBB6145E |
treatment provided by |
Felipe |
scientific name |
Otodus (Carcharocles) cf. sokolowi (Jaekel, 1895) |
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Otodus (Carcharocles) cf. sokolowi (Jaekel, 1895)
EXAMINED MATERIAL. — Around twenty broken isolated teeth, figured material includes FSAC Bouj-320, 321 and 322 .
DESCRIPTION
Teeth can reach up to 10 cm in height, displaying a large triangular cusp with well-marked and regular serrations on the cutting edges and a pair of lateral cusplets ( Fig. 2A View FIG ). Cusplets are not very high when conserved and often divergent in lateral teeth ( Fig. 2A View FIG ) to less developed in anterior teeth ( Fig. 2B View FIG ).
REMARKS
Teeth of Otodus (Carcharocles) cf. sokolowi are relatively common around the archaeocete carcasses ( Fig. 2 View FIG A-C). Case & Cappetta (1990) have discussed about the taxonomic distinctness of Otodus (Carcharocles) sokolowi compared to the other Eocene species of subgenus, and in particularly with the smaller and coeval species Otodus (Carcharocles) auriculatus (Blainville, 1818) . Otodus (Carcharocles) sokolowi appears widely distributed and relatively common in the tropical marine realm since the GEA-C (uppermost Bartonian-lowermost Priabonian) and throughout the Priabonian successions (GE D-G, BQ, QS) according to Underwood et al. (2011), southwestern Morocco included ( Adnet et al. 2010). However this species seems relatively discrete in older deposits, as in the MI ( Underwood et al. 2011). Its occurrence in Bartonian of Gueran, Morocco, testify of its spatial expansion along the Tethysian coasts during the Bartonian.
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Elasmobranchii |
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