Species of Enchodus are generally classified into two different clades, the North American and the Mediterranean. It has been proposed that this distinction is the result of several isolated events between the two populations over the Late Cretaceous.[5]
Enchodus species were small to medium in size, large species (E. zinensis) reached 172.2 centimetres (67.8 in).[11] One of the genus' most notable attributes are the large "fangs" at the front of the upper and lower jaws and on the palatine bones, leading to its misleading nickname among fossil hunters and paleoichthyologists, "the saber-toothed herring". These fangs, along with a long sleek body and large eyes, suggest Enchodus was a predatoryspecies.[1]
E. petrosus, with standard length around 76.7 centimetres (30.2 in)[11] and sometimes over 1 metre (3 ft 3 in),[12] remains of which are common from the Niobrara Chalk, the Mooreville Chalk Formation, the Pierre Shale, and other geological formations deposited within the Western Interior Seaway and the Mississippi Embayment. Large individuals of this species had fangs measuring over 6 centimetres (2.4 in) in length, giving its skull an appearance somewhat reminiscent of modern deep-sea fishes, such as anglerfish and viperfish. Other species were considerably smaller, some like E. parvus were only some centimeters (a few inches) long.[13]
Despite being a formidable predator, remains of Enchodus are commonly found among the stomach contents of larger predators, including sharks, other bony fish, mosasaurs, plesiosaurs and seabirds such as Baptornis advenus.[citation needed]
^Fielitz, Christopher; González-Rodríguez, Katia A. (2010). "A New Species of Enchodus (aulopiformes: Enchodontidae) from the Cretaceous (albian to Cenomanian) of Zimapán, Hidalgo, México". Journal of Vertebrate Paleontology. 30 (5): 1343–1351. Bibcode:2010JVPal..30.1343F. doi:10.1080/02724634.2010.501438. JSTOR40864352. S2CID84281080.
^ abRana, R. S.; Kumar, K.; Singh, H.; Rose, K. D. (2005). "Lower vertebrates from the Late Palaeocene–Earliest Eocene Akli Formation, Giral Lignite Mine, Barmer District, western India". Current Science. 89 (9): 1606–1613. JSTOR24110948.
^ abDavis, Matthew P.; Fielitz, Christopher (December 2010). "Estimating divergence times of lizardfishes and their allies (Euteleostei: Aulopiformes) and the timing of deep-sea adaptations". Molecular Phylogenetics and Evolution. 57 (3): 1194–1208. Bibcode:2010MolPE..57.1194D. doi:10.1016/j.ympev.2010.09.003. PMID20854916.
^ abDíaz-Cruz, Jesús Alberto; Alvarado-Ortega, Jesús; Ramírez-Sánchez, Marcia M.; Bernard, Emma Louise; Allington-Jones, Lu; Graham, Mark (November 2021). "Phylogenetic morphometrics, geometric morphometrics and the Mexican fossils to understand evolutionary trends of enchodontid fishes". Journal of South American Earth Sciences. 111: 103492. Bibcode:2021JSAES.11103492D. doi:10.1016/j.jsames.2021.103492.
^Chida, Mori; Brinkman, Donald B.; Murray, Alison M. (October 2023). "A large, new dercetid fish (Teleostei: Aulopiformes) from the Campanian Bearpaw Formation of Alberta, Canada". Cretaceous Research. 150: 105579. Bibcode:2023CrRes.15005579C. doi:10.1016/j.cretres.2023.105579. S2CID258803963.
^Everhart, M.J. (2017). Oceans of Kansas, Second Edition: A Natural History of the Western Interior Sea (Life of the Past). Indiana University Press. p. 117. ISBN978-0253026323.
Russell, Dale A. (1988). A Check List of North American Marine Cretaceous Vertebrates Including Fresh Water Fishes. Tyrrell Museum of Palaeontology. ISBN978-1-55006-106-2.
Davis, Matthew P.; Fielitz, Christopher (December 2010). "Estimating divergence times of lizardfishes and their allies (Euteleostei: Aulopiformes) and the timing of deep-sea adaptations". Molecular Phylogenetics and Evolution. 57 (3): 1194–1208. Bibcode:2010MolPE..57.1194D. doi:10.1016/j.ympev.2010.09.003. PMID20854916.