Goniatite Ammonites
Phylum Mollusca;
Class: Cephalopoda; Subclass: Ammonoidea; Order: Goniatida
Geologic
Age: Devonian (400 million years old)
Fossil Site: Atlas Mountains in Morocco
Goniatites are Ammonoids with a distinctive goniotitic
zig-zag pattern in the sutures that mark the spiraling growth
of the shell. The extinct ammonite that decended from Nautiloids
is an example of the remarkable symmetry often found in nature.
Mineral exchange over the eons can create an amazing array of
contrasting colors and the beautiful natural display you see
here. Ammonites were Cephalopods sharing a common ancestor with
the squid and octopus. The ammonites that appeared in the Devonian
became very diverse and widespread in the Paleozoic and Mesazoic
before going extinct along with the dinosaurs at the end of the
Cretaceous period. The goniatites lived early in the Devonian
period, some 400 million years ago, and became extinct during
the Permian period.
The pictures tell the story of this large, beautifully polished
display fossil exhibiting a mixture of earth-tones. The thin
walls between the internal chambers of the shell are called the
septa, and as the goniatite grew it would move its body forward
in the shell secreting septa behind it, thereby adding new chambers
to the shell. The sutures (or suture lines) are visible as a
series of narrow, wavy lines on the surface of the shell. The
sutures appear where each septa contacts the wall of the outer
shell.
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