Carcharias, Rafinesque, 1810
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.4606613 |
persistent identifier |
https://treatment.plazi.org/id/03923C45-FF87-FF80-33B7-FA0CFC9717BE |
treatment provided by |
Felipe |
scientific name |
Carcharias |
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‘ Carcharias View in CoL View at ENA ’ koerti ( Stromer, 1910)
MATERIAL. — 30 broken isolated teeth, figured material included FSAC Bouj-325 and 326.
DESCRIPTION
Occurrence of the middle Eocene ‘ Carcharias ’ koerti is confirmed in Gueran ( Fig. 2F, G View FIG ). Interestingly, the majority of recovered teeth (e.g., Fig. 2G View FIG ) are relatively small compared to the usual Lutetian representatives.
REMARKS
The generic affinity of this large pelagic shark to ‘‘ Carcharias ” or “ Brachycarcharias ” still remains unclear (e.g., Strougo et al. 2007; Underwood et al. 2011), it is preferentially known in the Lutetian deposits and is widely distributed around the North and Western African coasts ( Stromer 1910; White 1955; Dartevelle & Casier 1959; Cappetta & Traverse 1988; Cappetta et al. 2000; Noubhani & Cappetta 1997; Strougo et al. 2007). Rarely recovered in MI (Uppermost LutetianLowermost Bartonian), GA (Lutetian-Bartonian) and lacking in GE A-C (uppermost Bartonian) and the remainder of the succession of Wadi al Hitan, Egypt (see Underwood et al. 2011), its occurrence in Boujdour area seems to indicate that the age of the deposits is likely older than latest Bartonian.
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