Dentalium martini Whitfield, 1882, is a calcareous worm tube, not a mollusk
, and is placed in synonymy of Coleolus crenatocinctum Hall, 1879. The grow
th of D. martini mimics logarithmic curvature in the holotype, but in other
specimens shape varies from irregularly curved to straight. A prime reason
for reassignment is variation of the wall thickness around the circumferen
ce in D. martini, which in late Paleozoic and Recent scaphopods of the same
size is of uniform thickness.