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Mounted Jurassic Ammonite

Late Jurassic, Oxfordian Stage (approx. 161-154 million years ago), Madagascar

Session begins in

July 14, 02:00 PM GMT

Estimate

4,000 - 6,000 USD

Bid

4,200 USD

Lot Details

Description

Mounted Jurassic Ammonite

Kranaosphinctes rabei

Late Jurassic, Oxfordian Stage (approx. 161-154 million years ago)

Madagascar


20 x 17¼ x 8½ inches (50.8 x 43.8 x 21.6 cm), 26 inches (66 cm) on stand. 117 pounds (53.1 kg).


This ammonite species, Kranaosphinctes rabei, displays prominent folds together with tight whorl development on its shell. It is complete, nicely cleaned and in its natural state. This species of ammonite is highly regarded by both collectors and designers due to its sculptural qualities and aesthetic appeal.

Alongside trilobites and dinosaurs, ammonites are among the most iconic fossils. Ammonites swam the seas freely during the Jurassic and Cretaceous Periods, evolving rapidly and leaving abundant examples in the fossil record. Ammonites were cephalopods, a taxonomic class that includes today's nautilus, octopus, and squid. They used a long, tubular organ known as a siphuncle to fill or empty their chambers with water and thus move up or down in the water column. Apart from the siphuncle, the animal lived solely in the outermost chamber.


The outermost layer of ammonite shells was made up of aragonite, a type of calcium carbonate, which provided strong protection and allowed ammonites to fossilize much more readily than animals that either had a soft shell or lacked a shell. In the case of the Kranaosphinctes offered here, its aragonite shell has developed a beautifully nacreous and pearlescent outer layer.


Kranaosphinctes lived during the Late Jurassic Period, approximately 161 to 154 million years ago. Because ammonites rapidly evolved into new species and their shells were prone to fossilization, they have been crucial for scientists interested in dating the Earth's layers: finding the same species of ammonite in layers of soil thousands of miles apart implies that those layers are from the same time period in Earth's history.