Anomotodon cravenensis
Case, 1980
Classification: Elasmobranchii Lamniformes Mitsukurinidae
Reference of the original description
A selachian fauna from the Trent Formation, Lower Miocene (Aquitanian) of Eastern North Carolina. Palaeontographica, Abt. A, 171(1–3), 75–103
A selachian fauna from the Trent Formation, Lower Miocene (Aquitanian) of Eastern North Carolina. Palaeontographica, Abt. A, 171(1–3), 75–103
Synonyms / new combinations and misspellings
Anomotodon cf. cravenensis
Anomotodon cf. cravenensis
Types
Anomotodon cravenensis
Holotype: AMNH.: 9627; Paratype: AMNH.: 9620; AMNH.: 9621; AMNH.: 9622; AMNH.: 9624; AMNH.: 9625; AMNH.: 9626;
Anomotodon cravenensis
Holotype: AMNH.: 9627; Paratype: AMNH.: 9620; AMNH.: 9621; AMNH.: 9622; AMNH.: 9624; AMNH.: 9625; AMNH.: 9626;
Description:
Citation: Anomotodon cravenensis Case, 1980: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
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Description
Original diagnose after Case (1980) p. 83 [390]: Teeth medium to large in dimension, ranging in size from 1 to 3 cm, and averaging about 2 cm, blades flattened and slightly sigmoidal, with no lateral denticles.
Original diagnose after Case (1980) p. 83 [390]: Teeth medium to large in dimension, ranging in size from 1 to 3 cm, and averaging about 2 cm, blades flattened and slightly sigmoidal, with no lateral denticles.
References
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
Palaeobiogeographic relationships and palaeoenvironmental implications of an earliest Oligocene Tethyan ichthyofauna from Egypt. Canadian Journal of Earth Sciences, 51(10), 909–918
DOI: 10.1139/cjes-2014-0097
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department
Die Neoselachier der Paleokaribik (Pisces: Elasmobranchii). Courier Forschungsinstitut Senckenberg, 119, 1–102
A selachian fauna from the Trent Formation, Lower Miocene (Aquitanian) of Eastern North Carolina. Palaeontographica, Abt. A, 171(1–3), 75–103
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
Palaeobiogeographic relationships and palaeoenvironmental implications of an earliest Oligocene Tethyan ichthyofauna from Egypt. Canadian Journal of Earth Sciences, 51(10), 909–918
DOI: 10.1139/cjes-2014-0097
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department
Die Neoselachier der Paleokaribik (Pisces: Elasmobranchii). Courier Forschungsinstitut Senckenberg, 119, 1–102
A selachian fauna from the Trent Formation, Lower Miocene (Aquitanian) of Eastern North Carolina. Palaeontographica, Abt. A, 171(1–3), 75–103
