Revised description:Single spherical, reticulate lattice bearing four tetrahedrally arranged, multicostate spines.
Remarks:Ormiston and Lane (1976) were incorrect in suggesting that the genus possesses an internal spicule; Deflandre stressed that he could find no traces of spicule in his type material from the Cabrières assemblage.
Stratigraphic range:[No information given]
Subsequent descriptions:?

Literature cited:- Holdsworth, B. K., D. Jones, and Allison (1978). Upper Devonian radiolarians separated from chert of the Ford Lake Shale, Alaska. Journal of Research, United States Geological Survey 6(6): 775-788.
- Ormiston, A. R. and H. R. Lane (1976). A unique radiolarian fauna from the Sycamore Limestone (Mississippian) and its biostratigraphic significance. Paläontographica, 154: 158-180.