Polished Ammonite Split Pair - 4.22" Cleoniceras
Polished Ammonite Split Pair - 4.22" Cleoniceras
Ammonites are an extinct group of cephalopods that entered the fossil record 400 million years ago. This specimen is a 4.22" polished Cleoniceras fossil from Madagascar. The fossil has been split into a paired set to showcase the beautiful internal chambers of the shell.
These internal chambers are called septa and the ammonite could fill them with air in order to float through the ocean like a balloon. After millions of years, they are now mineralized with beautiful spiral patterns. A pair of stands and informational card is included the fossil.
📸 A Split Ammonite Shell in hand
Ammonites are an extinct group of cephalopods that entered the fossil record 400 million years ago. They survived several mass extinction events, including the Permian–Triassic "Great Dying" which wiped out 96% of all marine species. They finally succumbed during the Cretaceous-Paleogene extinction event 66 million years ago, which also wiped out the dinosaurs.
This specimen is a pair of fossilized Cleoniceras ammonite shells from Madagascar and is estimated to be over 100 million years old. The shell has been split and polished to display the beautiful internal chambers of fossil. Each of these segments, called septa, are have been filled with stunning minerals over the course of millions of years. These septa were an evolutionary adaptation that allowed the ammonite to float through the water even with a heavy shell.
📸 A sample pair of split ammonites
These Split Ammonites are pairs and comes with two stands for display. A small informational card that serves as certificate of authenticity is also included.
These ammonites are quite large and the perfect size to hold in your hand. Their polishing makes them smooth to the touch and you can see the incredible interior of the fossils as well. They will delight any visitor and are perfect for display in every setting.
Check out all our ammonites at the collection below!
📸 An artist's depiction of an ammonite swimming through the prehistoric sea
MORE ABOUT AMMONITES
ESTIMATED AGE : c. 110,000,000 years old
📸 A sample split Shell Ammonite
A Perfect Spiral
Ammonites are an extinct group of cephalopods which entered the fossil record 400 million years ago. They survived several mass extinction events, including the Permian–Triassic "Great Dying" which wiped out 96% of all marine species. They finally succumbed during the Cretaceous-Paleogene extinction event 66 million years ago, which also wiped out the dinosaurs.
The size of ammonite shells range from sub-centimeter dwarf species to giants nearly three meters in diameter. Most iconic shells exhibit a nearly perfect logarithmic spiral.
This ammonite is from the genus Cleoniceras, a subset of the ammonite class that lived during the Cretaceous period. Given its abundance in the fossil record, Cleoniceras (along with other ammonites) are often used to estimate the age of the geological layer in which the fossils are found. Cleoniceras have been found across the world, from the European mainland to along the Caspian Sea. The fossils in our collection come from Madagascar and lived in the seaway growing between the island and the paleocontinent Gondwana.
📸 A close look at the suture patterns in Cleoniceras
The Strength of Sutures
The shells of Cleoniceras are separated into chambers called septa, which show highly complex sutured patterning. These beautiful patterns evolved over time to solve a difficult problem: shell strength. In order to survive at deeper pressures, ammonites needed tougher shells, but increasing the size and thickness of the shell could slow them down.
Sutured shells could spread the water pressure across the surface, increasing the strength of each chamber without making it much heavier. This made the shells safer at high depths while staying efficient to grow and kept the animal swimming quickly.
📸 A variety of different ammonoid shells
How these creatures lived is of intense interest to science, as ammonites likely played a vital role in the food chain in the ancient seas. Evidence exists to suggest that ammonites were a prime food source for Mosasaurs and fishes, while other studies suggest the bite marks on their remains were created after death by limpets or even by other cephalopods.
Many thousands of distinct species make up the long-lived ammonoid subclass. Though most ammonite shells are the classic spiral, there are also straight and gastropod-like shells and even some shells that are partially uncoiled. The surface of the shells also vary quite widely, from smooth to wildly thorny.
Ammonites were an incredibly diverse and plentiful group of animals that survived for hundreds of millions of years and lived all across the planet. Their rapid diversification and tough, rocky shells means there are many different and easily identifiable species in the fossil record. Because of this, scientists can use them to easily identify the age of other fossils and geologic deposits found in the same layer of the ammonites. They're a welcome sight to the eyes of any inquisitive geologist!
Aside from their complex shells, there is little direct evidence regarding the appearance of ammonites due to the absence of soft tissue fossils. However, many scientists believe ammonites had bodies similar to that of the present-day Nautilus.
📸 A logarithmic spiral in a natural ammonite fossil
Ammonite shells grew in a natural spiral and made a consistent, mathematically significant pattern. This special shape is known as a logarithmic spiral.
The main property of a logarithmic spiral is that the shape of the spiral is unaltered as it increases in size. Each turn is a pure geometrical progression of the last with a common ratio. This form is found in many natural phenomena, from the shape of galaxies to patterns on sunflower heads.
Front of the Specimen Card
Back of the Specimen Card
Staaf, Danna. Monarchs of the Sea: The Extraordinary 500-Million-Year History of Cephalopods. The Experiment, 2020.
Tsujita, Cameron J., and Gerd EG Westermann. "Were limpets or mosasaurs responsible for the perforations in the ammonite Placenticeras?." Palaeogeography, Palaeoclimatology, Palaeoecology 169.3 (2001): 245-270.
Moulton, D. E., A. Goriely, and R. Chirat. "The morpho-mechanical basis of ammonite form." Journal of theoretical biology 364 (2015): 220-230.
Lemanis, Robert, et al. "A new approach using high-resolution computed tomography to test the buoyant properties of chambered cephalopod shells." Paleobiology 41.02 (2015): 313-329.