In the latest classification of the family Conidae by Puillandre N., Duda T.F., Meyer C., Olivera B.M. & Bouchet P. (2015), Lithoconus has become a subgenus of Conus as Conus (Lithoconus) Mörch, 1852 (type species:Conus millepunctatus Lamarck, 1822) represented as Conus Linnaeus, 1758
The basic shell shape is conical to elongated conical, has a deep anal notch on the shoulder, a smooth periostracum and a small operculum. The shoulder of the shell is usually nodulose and the protoconch is usually multispiral. Markings often include the presence of tents except for black or white color variants, with the absence of spiral lines of minute tents and textile bars.
Radular tooth (not known for fossil species)
The radula has an elongated anterior section with serrations and a large exposed terminating cusp, a non-obvious waist, blade is either small or absent and has a short barb, and lacks a basal spur.
Geographical distribution
These species are found in the Indo-Pacific region.
The shell is large, thick and obconic in shape, and the shoulders are subangular. The protoconch is multispiral, and the whorl tops are usually concave in cross section and have just one or two cords. The shell is ornamented with nodules which are obsolete but present. The anal notch is shallow to moderately deep, depending upon the species. The color pattern includes spiral rows of brown, red or black markings, and the anterior end is usually colored black, red, blue or lavender. The periostracum is smooth and very thick, and the operculum is large.
Radular tooth (not known for fossil species)
The anterior section of the radular tooth may be shorter or significantly longer than the length of posterior section, and the blade is long and covers most of the anterior section. A basal spur is present, and the barb is short. The radular tooth has several rows of coarse denticles.
Geographical distribution
The species in this genus occur in the occur in the Indo-Pacific region.