Archaeotriakis ornatus
Case, 1987
Classification: Elasmobranchii Carcharhiniformes Triakidae
Reference of the original description
A new selachian fauna from the Late Campanian of Wyoming (Teapot Sandstone Member, Mesaverde Formation, Big Horn Basin). Palaeontographica, Abt. A, 197(1–3), 1–37
A new selachian fauna from the Late Campanian of Wyoming (Teapot Sandstone Member, Mesaverde Formation, Big Horn Basin). Palaeontographica, Abt. A, 197(1–3), 1–37
Types
Archaeotriakis ornatus
Archaeotriakis ornatus
Description:
Citation: Archaeotriakis ornatus Case, 1987: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
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References
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Combining palaeontological and neontological data shows a delayed diversification burst of carcharhiniform sharks likely mediated by environmental change. Scientific Reports, 12, Article 21906
DOI: 10.1038/s41598-022-26010-7
A late Campanian Euselachian Assemblage from the Bearpaw Formation of Alberta, Canada: Some Notable Range Extensions. Canadian Journal of Earth Sciences, 54(9), 973–980
DOI: 10.1139/cjes-2016-0233
A new selachian fauna from the Late Campanian of Wyoming (Teapot Sandstone Member, Mesaverde Formation, Big Horn Basin). Palaeontographica, Abt. A, 197(1–3), 1–37
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Combining palaeontological and neontological data shows a delayed diversification burst of carcharhiniform sharks likely mediated by environmental change. Scientific Reports, 12, Article 21906
DOI: 10.1038/s41598-022-26010-7
A late Campanian Euselachian Assemblage from the Bearpaw Formation of Alberta, Canada: Some Notable Range Extensions. Canadian Journal of Earth Sciences, 54(9), 973–980
DOI: 10.1139/cjes-2016-0233
A new selachian fauna from the Late Campanian of Wyoming (Teapot Sandstone Member, Mesaverde Formation, Big Horn Basin). Palaeontographica, Abt. A, 197(1–3), 1–37