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Polished Ammonite Fossil Madagascar Cretaceous Marine Cephalopod Cut and Polished Display Fossil

£36.00

Genuine Polished Ammonite Fossil from the Cretaceous of Madagascar

This genuine polished ammonite fossil originates from Cretaceous marine deposits of Madagascar, one of the world’s most famous locations for beautifully preserved ammonites. Dating to the Cretaceous Period, approximately 145–66 million years ago, this specimen represents a marine cephalopod that lived in the ancient oceans during the age of dinosaurs.

The fossil has been carefully cut and polished to reveal the intricate internal chamber structure of the ammonite shell, creating an attractive natural display piece. The polished surface highlights the mineralised chambers and natural patterns formed during fossilisation, making this specimen both scientifically interesting and visually striking.

The photographs show the exact specimen you will receive. Please refer to the photos for the full sizing and proportions of the fossil. This genuine fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the authenticity of the specimen.

About Ammonites – Iconic Marine Cephalopods of the Mesozoic

Ammonites belong to the extinct order Ammonitida, a group of marine cephalopods related to modern squid, octopus, and cuttlefish. These animals flourished throughout the Mesozoic Era and were among the most abundant marine organisms in Jurassic and Cretaceous oceans.

Ammonites possessed coiled external shells divided into chambers that helped regulate buoyancy. The living animal occupied the outermost chamber, while the inner chambers were filled with gas and fluid that allowed the animal to control its position in the water column.

These animals were active swimmers and predators, feeding on small fish, crustaceans, plankton, and other marine organisms. Their shells are among the most distinctive fossils found in marine sedimentary rocks and are widely used by palaeontologists as index fossils for dating geological strata.

Internal Shell Structure Revealed by Polishing

The ammonite shell is composed of a series of chambers separated by curved internal walls known as septa. As the ammonite grew, it built new chambers and moved forward in the shell, sealing off the older chambers behind it.

These chambers were connected by a narrow tube called the siphuncle, which allowed the animal to regulate gas and liquid within the shell. This system provided a highly effective method of buoyancy control, allowing ammonites to move vertically through the water column.

Cutting and polishing the fossil reveals the chamber structure and mineralisation that occurred during fossilisation. The chambers are often filled with calcite or other minerals, creating attractive internal patterns and colours that make polished ammonites highly desirable display specimens.

Geological Setting – Cretaceous Marine Deposits of Madagascar

Madagascar is internationally known for producing some of the finest ammonite fossils in the world. The island contains extensive marine sedimentary deposits dating to the Jurassic and Cretaceous periods when the region was covered by warm tropical seas connected to the ancient Tethyan Ocean.

These marine environments supported a rich diversity of marine life including ammonites, marine reptiles, fish, and various invertebrates. Over millions of years, the shells of ammonites were buried in marine sediment and mineralised, preserving their intricate structures.

Many ammonites from Madagascar are later cut and polished to reveal their internal chambers, creating spectacular specimens that combine natural fossil preservation with beautiful mineral displays.

Cretaceous Marine Ecosystem

During the Cretaceous Period, the oceans were home to a wide variety of marine organisms. Ammonites were a key component of these ecosystems, serving both as predators and as prey for larger animals such as marine reptiles and large fish.

The warm tropical seas surrounding Madagascar supported abundant marine life, allowing ammonites to flourish and diversify into many different forms. Their rapid evolution and wide distribution make ammonites some of the most important fossils for understanding the geological history of the Mesozoic oceans.

Authenticity and Collectability

• Genuine polished ammonite fossil

• Cretaceous Period, approximately 145–66 million years old

• Collected from Madagascar

• Cut and polished to reveal internal chamber structure

• The exact fossil shown in the photographs is the specimen you will receive

• Includes a Certificate of Authenticity lifetime guarantee generic card

Polished ammonites from Madagascar are highly sought after by collectors due to their beautiful internal structures and excellent preservation. This Cretaceous ammonite specimen makes an outstanding display piece and a fascinating addition to any fossil collection, geological display, or natural history collection.

(Actual as seen)

Only 1 left in stock

SKU: P00620 Category:

Description

Genuine Polished Ammonite Fossil from the Cretaceous of Madagascar

This genuine polished ammonite fossil originates from Cretaceous marine deposits of Madagascar, one of the world’s most famous locations for beautifully preserved ammonites. Dating to the Cretaceous Period, approximately 145–66 million years ago, this specimen represents a marine cephalopod that lived in the ancient oceans during the age of dinosaurs.

The fossil has been carefully cut and polished to reveal the intricate internal chamber structure of the ammonite shell, creating an attractive natural display piece. The polished surface highlights the mineralised chambers and natural patterns formed during fossilisation, making this specimen both scientifically interesting and visually striking.

The photographs show the exact specimen you will receive. Please refer to the photos for the full sizing and proportions of the fossil. This genuine fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the authenticity of the specimen.

About Ammonites – Iconic Marine Cephalopods of the Mesozoic

Ammonites belong to the extinct order Ammonitida, a group of marine cephalopods related to modern squid, octopus, and cuttlefish. These animals flourished throughout the Mesozoic Era and were among the most abundant marine organisms in Jurassic and Cretaceous oceans.

Ammonites possessed coiled external shells divided into chambers that helped regulate buoyancy. The living animal occupied the outermost chamber, while the inner chambers were filled with gas and fluid that allowed the animal to control its position in the water column.

These animals were active swimmers and predators, feeding on small fish, crustaceans, plankton, and other marine organisms. Their shells are among the most distinctive fossils found in marine sedimentary rocks and are widely used by palaeontologists as index fossils for dating geological strata.

Internal Shell Structure Revealed by Polishing

The ammonite shell is composed of a series of chambers separated by curved internal walls known as septa. As the ammonite grew, it built new chambers and moved forward in the shell, sealing off the older chambers behind it.

These chambers were connected by a narrow tube called the siphuncle, which allowed the animal to regulate gas and liquid within the shell. This system provided a highly effective method of buoyancy control, allowing ammonites to move vertically through the water column.

Cutting and polishing the fossil reveals the chamber structure and mineralisation that occurred during fossilisation. The chambers are often filled with calcite or other minerals, creating attractive internal patterns and colours that make polished ammonites highly desirable display specimens.

Geological Setting – Cretaceous Marine Deposits of Madagascar

Madagascar is internationally known for producing some of the finest ammonite fossils in the world. The island contains extensive marine sedimentary deposits dating to the Jurassic and Cretaceous periods when the region was covered by warm tropical seas connected to the ancient Tethyan Ocean.

These marine environments supported a rich diversity of marine life including ammonites, marine reptiles, fish, and various invertebrates. Over millions of years, the shells of ammonites were buried in marine sediment and mineralised, preserving their intricate structures.

Many ammonites from Madagascar are later cut and polished to reveal their internal chambers, creating spectacular specimens that combine natural fossil preservation with beautiful mineral displays.

Cretaceous Marine Ecosystem

During the Cretaceous Period, the oceans were home to a wide variety of marine organisms. Ammonites were a key component of these ecosystems, serving both as predators and as prey for larger animals such as marine reptiles and large fish.

The warm tropical seas surrounding Madagascar supported abundant marine life, allowing ammonites to flourish and diversify into many different forms. Their rapid evolution and wide distribution make ammonites some of the most important fossils for understanding the geological history of the Mesozoic oceans.

Authenticity and Collectability

• Genuine polished ammonite fossil

• Cretaceous Period, approximately 145–66 million years old

• Collected from Madagascar

• Cut and polished to reveal internal chamber structure

• The exact fossil shown in the photographs is the specimen you will receive

• Includes a Certificate of Authenticity lifetime guarantee generic card

Polished ammonites from Madagascar are highly sought after by collectors due to their beautiful internal structures and excellent preservation. This Cretaceous ammonite specimen makes an outstanding display piece and a fascinating addition to any fossil collection, geological display, or natural history collection.

Additional information

Era

Cretaceous

Origin

Madagascar

Cretaceous Information

The Cretaceous Period (145–66 million years ago) was the final era of the Mesozoic, marked by the dominance of dinosaurs and the rise of flowering plants. It had a warm, greenhouse climate, with high sea levels that created vast shallow inland seas. Marine life flourished, including mosasaurs, ammonites, and rudist reefs, while the land was ruled by iconic dinosaurs like Tyrannosaurus rex, Triceratops, and Spinosaurus. Mammals and birds diversified, and insects thrived. The period ended with the mass extinction event, likely caused by an asteroid impact, wiping out the dinosaurs and paving the way for the rise of mammals in the Cenozoic.

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