Trigonotodus is an extinct genus of sharks, most likely belonging to the family Alopiidae. This genus includes three extinct species, which span from the early Eocene to the late Oligocene. It was originally placed in the family Otodontidae, but subsequently found to have affinities with Thresher sharks.[1] This genus is sometimes considered part of the genus Alopias.[1] It is currently only known from isolated teeth.
Species
Species within this genera include:
Species
Notes
Images
Ref.
Trigonotodusaktulgaicus
Known primarily from the early Eocene of Kazakhstan. It is extremely similar to T. tushbairicus, and if not synonymous is likely its ancestor. It is also sometimes spelled T. aktulagaicus. Some scientists regard it as a Nomen nudum, early eocene species being called Trigonotodus cf. T. tushbairicus.
Known primarily from the middle Eocene of Kazakhstan. It is similar to other early threshers such as A. hermani and A. latidens in terms of size and robustness but has lateral cusplets. It is the type species of Trigonotodus.
Known primarily from the late Oligocene of South Carolina (Ashley Marl and Chandler Bridge Formations). It is commonly known as the Cusped Giant Thresher. May have one or two lateral cusplets. It is much larger than the other two.
^ abZhelezko VI, Kozlov VA (1999). "Elasmobranhii i biostratigraphia paleogena Zauralia i Srednei Asii" [Elasmobranchii and Palaeogene biostratigraphy of Transural and Central Asia]. Materialy Po Stratigrafii I Paleontologii Urala [Materials on Stratigraphy and Paleontology of the Urals]. 3. Ekaterinburg: UrO RAN: 324.
^Kozlov VA (2001). "Novyj vid akuly roda Trigonotodus KOZLOV, 1999 iz oligotsenovykh otlozhenij severnoj ameriki" [A new shark species of the genus Trigonotodus Kozlov, 1999, from Oligocene sediments of Northern America]. Materialy Po Stratigrafii I Paleontologii Urala [Materials on Stratigraphy and Paleontology of the Urals]. 6: 89–91.
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