Description:
This is a lovely presentation of display characteristics. The center
portion exhibits the rich red and green ammolite “fire”
on both sides. Other colors like the subtle pink and muted greens
fan outward. Suture patterns are revealed closer to the keel.
Sphenodiscus
is an extinct genus of acanthoceratacean ammonite. The genus has
been found from many continents and is thought to have had a large
global distribution during the Maastrichtian stage of the Late Cretaceous.
It was one of the last ammonoids to have evolved before the entire
subclass went extinct at the end of the period during the Cretaceous–Tertiary
extinction event. The shell of Sphenodiscus was streamlined and
lateromedially compressed with overlapping whorls and a small umbilicus.
The ventral edge of the shell tends to be sharply angled. The outer
surface is generally smooth in fossil specimens, although certain
species at different stages of ontogenic development may possess
many small tubercles along their surfaces[
The
iridescent color display of these ammonites is what makes them so
stunning and collectable. The ammonite shell is comprised primarily
of aragonite with a number of associated trace elements. This gem
quality material is called ammolite. The percentage of ammolite
in a specimen can make it very valuable. The ammolite is also graded
according to color, iridescence, chromatic shift and other factors.
This specimen has a thin layer of exposed ammolite on one side.
The predominant colors are red and green, with brilliant iridescence.
The
Cretaceous Pierre Shale formation where this ammonite originates
outcrops in the United States and Canada. It’s famous ammonite
fossils; include Baculites, Placenticeras, Scaphites, Hoploscaphites,
and Jeletzkytes, as well as many uncoiled forms. Many of these also
have much or all of the original shell, as well as the complete
body chamber, still intact. Many Pierre Shale ammonites are found
within concretions from which they must be removed, at least in
part.
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