The dinophysoid dinoflagellates (to which Ornithocercus belongs) achieve growth both by increase in size of individual wall elements and, during rapid lateral expansion associated with cell division, by the formation of a semimeridional band of material termed the megacytic zone (MZ). The MZ maintains mother cell wall integrity during complete cytokinesis of the cell body and enclosure with new wall elements. The lists, extensive wing-like extensions of the wall, can only be reformed after dissolution of the MZ. Beginning near the ventral region (which is the last region of the wall to be duplicated), the MZ dislocates and its material is apparently resorbed. The last region of attachment is invariably dorsal and in several, but not all species, the daughter cells may remain attached during early list formation by a special remnant of the MZ, termed here the dorsal megacytic bridge (DMB). After full separation of daughter cells remnants of the DMB persist for an unknown but presumably short period. The topography of this process, involving radical ontogenetic alterations in the appearance of the daughter cells and some wall surfaces, is illustrated here by the scanning electron microscope. In addition 2 aberrant types of division are shown, one of which results in a double individual, termed a geminoid. [ABSTRACT FROM AUTHOR]