Fossil Shell Morphology-or- The Terminology used in the Description of Externally Shelled Cephalopods (Nautiloids and Ammonoids)By Kevin Bylund Note: Kevin welcomes discussion on this article in the Fossils and History forum. The structure secreted by the mantle of cephalopods for protection or neutral buoyancy is called the Shell or Conch. The complete shell is basically a hollow cone with two major parts, the Body Chamber, or Living Chamber, and the Phragmocone. The opening on the large end is called the Aperture, and the Apex is at the tip of the small end. The shell or Test that forms the cone is called the Shell Wall.
Figure 1. Two lateral views of the
shell of Nautilus, external on the left and internal
on the right. Orientation
Figure 2. Drawings of an imaginary
coiled
cephalopod shell.
Figure 3.
Drawing of an orthoconic cephalopod shell and internal mold. Body Chamber
At maturity several kinds of modifications can occur on
the aperture. Lateral Lappets
are projections from the lateral part of the
peristome. A Ventral Lappet
or Rostrum
projects from the venter. A Constriction
is a necking down; a Contraction is a closing off. Sometimes the whole body chamber is Expanded.
Figure 5.
Parts of a Septal Suture line. The
septum is attached to the shell wall along a Suture,
seen as a series of simple to complex lines on internal
molds. Parts of the suture line directed
adorally are termed Saddles, and
those directed adapically are termed Lobes.
Figure 6.
Types of suture lines. Sutural
formulas are sometimes used to describe suture patterns (mostly
Paleozoic
ammonoids, and only briefly described here).
The primary lobes are given a letter designation, E
for the External (ventral) Lobe, L for the Lateral
Lobe and I
for the Internal (Dorsal) Lobe.
Adventitious Lobes, lobes forming later, between E and
L, are lettered A and numbered
consecutively in
accordance with their ontogenetic appearance.
New lobes appearing between L and
I are Umbilical Lobes, lettered U, and
numbered the same way. Siphuncle In
fossil cephalopod shells, anything that was in contact with the
siphuncular
chord is considered part of the Siphuncle. The non-living part of the siphuncle that
covers the living siphuncular chord is termed the Ectosiphuncle
it is composed of the septal neck and the connecting
ring. The area, and any structures,
inside the ectosiphuncle are termed the Endosiphuncle. The
Septal Neck is where the siphuncle
passes through the septum. Septal necks
directed adorally are termed Prochoanitic,
those directed adapically are termed Retrochoanitic. Several other terms are used for
retrochoanitic necks. Acoanitic
necks are barely developed or
extremely short. Loxochoanitic
necks point inward at moderate lengths.
Figure 7.
Types of Septal Necks. Connecting Rings are tubular structures connecting the
septa or
septal necks. Some rings are thin and
simple, others are thick and composed of two or three layers of
deposits. Connecting rings can be
straight, concave,
convex or bulbous.
Figure 8.
Several types of connecting rings (in red). Deposits Some
Cephalopods, mostly Nautiloids, deposited calcareous structures inside
the
shell, probably for buoyancy and attitude control. Cameral
Deposits were deposited inside the chambers, Mural
Deposits are on the shell wall, Episeptal Deposits on
the adapertural side of the septum and Hyposeptal Deposits
on the adapical
side of the septum. Endosiphuncular
deposits include
cone shaped Endocones,
longitudinal Lamellae, transverse partions called Diaphrams, Rods are round structures
laying on the ventral wall of the siphuncle, Annulosiphonate
deposits are donut shaped deposits inside the siphuncle, and Parietal are deposits
looking like and attached to the inside of the septal neck.
Figure
9.
Cameral deposits (in blue).
Figure 10. Endosiphuncular deposits (in blue). Shell Shape Nautiloid
shells can be Planispirally Coiled
(coiled in one plane) or straight, curved, open spiral etc., ammonoids
not
Planispirally coiled or have an open spiral are termed Heteromorphs. Curved or coiled shells are Exogastric
if the ventral side, or Venter, is convex and on the
outer
side, and Endogastric if the dorsal
side, or Dorsum, is convex and on
the outer side.
Figure
11.
Cartoon showing Exogastric and Endogastic coiling. The
cross sectional shape, or Whorl Section,
can be Round, Oval, Square,
Rectangular, Triangular,
Lanceolate (shaped
like a lance point), Fastigate (tapering
towards the venter), Tabulate (with
a flattened venter) or some variation of each.
Compressed shells are shorter
laterally, and Depressed shells are
shorter ventro-dorsally.
Figure
12.
Common whorl section shapes.
A Whorl is one
complete volution of a coiled shell. The
space enclosed on both sides by the last whorl is termed the Umbilicus. Shells with a
wide umbilicus are termed Evolute and shells with a
narrow
umbilicus are termed Involute. The
umbilical
Seam is where the shell wall attaches to the preceding whorl. The Umbilical
Wall is between the umbilical shoulder and the umbilical seam. The Umbilical
Shoulder is where the shell wall bends toward the preceding whorl. The Ventrolateral
Shoulder is where the shell bends toward the venter, and the Side or Flank, is between the
ventrolateral shoulder and the umbilical
shoulder.
Figure
13. Cross
section of a coiled shell showing parts and
common dimensions. Dimensions
most commonly used for the description of coiled shells are the
diameter, D, whorl width, W, whorl
height, H, the
umbilical diameter, U, the umbilical
ratio, U/D. Lately it has
become appropriate to have an
arrow pointing at the last septum, if visible.
Figure
15.
Planispiral shell shapes.
All
cephalopod shells are ornamented with at least Growth Lines,
each one representing a former position of the peristome.
Constrictions are internal shell thickenings and usually
only show
on the internal mold as sinuous transverse grooves.
Lirae are
small, usually longitudinal, raised portions of the shell separated by striae, small grooves. If
they are strong enough they will show on
internal molds.
Figure
17.
Ornamentation other than ribs.
Arkell, W. J., 1957, Introduction to Mesozoic Ammonoidea, in:
Treatise on
Invertebrate Paleontology, Part L, Mollusca 4, Cephalopoda-Ammonoidea,
Edited
by R. C. Moore, Geological Society of America and University of Kansas
Press, p.
L80-L100
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