The following species are known: •
A. aegypticus Capasso
et al, 2021 -
Maastrichtian of Egypt (
Dakhla Formation) •
A. aulercus (Sauvage, 1872) •
A. carteri Woodward, 1895 - Cenomanian of England (
Cambridge Greensand) •
A. cenomanicus (Sauvage, 1872) •
A. caddoi Suarez
et al., 2021 -
Albian of Arkansas, US (
Holly Creek Formation) •
A. confertus Woodward, 1895 - Cenomanian of England (Cambridge Greensand) •
A. couloni (Agassiz, 1843) - Late Cretaceous of Europe (
nomen dubium) •
A. cottreaui Priem, 1912 •
A. disparilis (Cornuel, 1877) - Early Cretaceous of France (
nomen dubium) •
A. distans (Coquand, 1860) - Late Cretaceous of France •
A. fraiponti Forir, 1889 - Maastrichtian of the Netherlands (
Maastricht Formation) •
A. hunteri •
A. latidens Gidley, 1913 -
Campanian to Maastrichtian of Maryland (
Monmouth Group), Mississippi, & New Jersey (
Navesink Formation), US •
A. mississippiensis Gidley, 1913 - Cretaceous of Mississippi, US •
A. muensteri (Agassiz, 1834) - Cenomanian of Germany (Hesseltal Formation) (syn:
Pycnodus depressus Agassiz, 1844,
P. complanatus Agassiz, 1844) •
A. woodwardi Sauvage, 1898
- Cretaceous of Portugal The majority of these species are only known from isolated dental elements. Only a few species (
A. angustus,
A. willetti,
A. subclavatus,
A. pauciseriale) are known from more than just teeth. Cooper & Martill (2020) determined that a diagnostic feature of
Anomoeodus is the presence of 4 tooth rows, excluding several former species. The former species
A. barberi has been reclassified into the genus
Agassizilia due to having more than 5 tooth rows, and the former species "
A"
nursalli Kriwet, 1999 is now considered an indeterminate pycnodontid due to having 6 tooth rows. Further taxonomic revisions are likely required for this genus. == Fossil record ==