Early rudists, which had coiled shells, did not produce reefs as we define them. Intermediate forms (i.e. recumbents and clingers with spirogyrate forms) were, at their densest, probably "reef-like". That is, assemblages of these rudists (called bouquets, clusters and thickets) could have provided superstratal relief and limited baffling. More advanced rudists, with close-packing potential, a stable, elevated cylindrical shape and a non-spiraled cap valve do meet reef-building criteria (Kauffman & Johnson, 1988). These true rudistid reefs were paucispecific, composed of dead and living rudists, created superstratal relief that baffled current flow, were cemented to the substrate, grew rapidly and possibly harbored photosynthetic algae. Evidence of epibionts on these reef-building rudists shows that binding algae, sponges and bryozoans also lived in these reefs (Kauffman & Sohl, 1974).