Flemingites is an extinct genus of evolute ammonoid from the Smithian (Lower Triassic) with spiral ridges on the shell.

Whorls are robust, slightly embracing, usually a little higher than wide and increasing very slowly.

Fine spiral ridges typically cover the shell, found even in casts.

The suture is distinctly ceratitic with rounded entire saddles and deep serrated lobes.

Later it was reassigned to the Flemingitidae and Noritaceae as shown in part L of the American Treatise[2] Other classifications put Flemingites in the Meekocerataceae,[3] or as recently renamed, Meekoceratoidea.