In ammonoids, a soft body organ (possibly a supracephalic mantle fold), ext
ending from the conch aperture secreted aragonitic wrinkles, forming a laye
r on the surface of the preceding whorl. The dorsal shell wall consists of
the outer and inner components which were deposited sequentially, beginning
at the aperture of the Living chamber inwards. The dorsal wall attains its
full thickness near the last septum. The outer component is visible in the
apertural region and is smooth or wrinkled; it is called the wrinkled laye
r in the latter case. The wrinkles may be continuous, interrupted, or form
isolated patches arranged in rows. The wrinkles are usually triangular in c
ross section. A further stage of dorsal wall development involves filling i
n the space between the apices of triangles, and then adding one or more in
ner prismatic layers from the inside of the living chamber. This pattern oc
curs at least in the postembryonic stage of all genera studied, belonging t
o five suborders of Ammonoidea ranging from Late Carboniferous to Late Cret
aceous. In many genera, the outer component of the dorsal shell wall exhibi
ts remarkable ontogenetic change in its ultrastructure and micro-ornament.
It may be compared with the black film of Recent Nautilus shells with respe
ct to place of formation. The outer component of the ammonoid dorsal shell
wall is regarded as a product of organic secretion and carbonate precipitat
ion in the area of the supracephalic mantle fold.