Turrilepadids are not uncommon in late Paleozoic shales being often as
sociated with ostracodes, foraminifers, and minute molluscs, In North
America they range from the late Missippian (Chesterian) to early Perm
ian (Leonardian). Sclerites of the inner scleritome row are more commo
n than outer sclerites. Some clusters have been found. Sclerite consis
ts of two layers with the thicker, lower layer penetrated by a transve
rse tubular structures oriented perpendicular to the sclerite surface,
which may represent canals related to the papillae on the inner surfa
ce of the sclerite. Turrilepas lepros sp. n., T. trigoniodes sp. n., T
. asketos sp. n., Clarkeolepis alloeospinosa sp. n., and Ambonlepidos
petalos gen. et sp. n. are proposed.