Macluritina Cox and Knight 1960 The Euomphalina comprise a major suborder of mainly Paleozoic archaeogastropods,[1] shells of which are hyperstophic to depressed orthstrophic, commonly with an angulation at the outer upper whorl surface thought to be coincident with the exhalent channel; shell wall thick, outer layer calcitic, inner layers aragonitic but not nacreous; operculum calcareous and heavy.

More recent classifications have expanded the Euomphalina to include the superfamilies: The Ophiletoidea were separated from the family Helicotomidae of the Euomphaloidea (Euomphalatacea in the original form).

The Oriostomatoidea and Platyceratoidea (in—acea form) are included in the suborder Trochina in the Treatise while (ibid) the Craspidostomatoidea, Palaeotrochoidea, and Pseudophoroidea (also as—acea taxa) are regarded simply as Archaeogastropoda of uncertain affinities.

The taxonomy of Bouchet and Rocroi, 2005 includes the superfamilies Euomphaloidea and Maclurioidea within mollusca with anisotrophically coiled shells of uncertain position (Gastropoda?)

The taxonomy of Ponder and Lindberg, 1997 on the other hand is more expansive and includes the Euomphalina as the order Euomphalida within the Eogastropoda, but adding only the Platyceratoidea to the Euomphaloidea and Macluritoidea.