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Crocodile Tibia Fossil Cretaceous Morocco Kem Kem Beds Genuine Specimen

Original price was: £240.00.Current price is: £168.00.

Long Description: Discover a genuine piece of ancient history with this Crocodile Tibia Fossil from the Kem Kem Beds, located in the Tegana Formation, Kem Kem Basin, Morocco. This fossil dates back to the Aptian stage of the Cretaceous period, approximately 100-125 million years ago.

This unique specimen showcases the remarkable preservation and evolution of ancient crocodilian species that roamed the region millions of years ago. The fossil in the photo is the exact piece you will receive, ensuring authenticity and attention to detail. To assist with accurate sizing, please refer to the accompanying photo with a 1cm scale cube for reference.

  • Location: Kem Kem Basin, Tegana Formation, Morocco
  • Geological Age: Cretaceous (Aptian stage)
  • Fossil Type: Crocodile Tibia

Each fossil comes with a Certificate of Authenticity, assuring you that it is a 100% genuine specimen. This fossil makes an excellent addition to any collection, a fantastic educational tool, or a unique gift for fossil enthusiasts and history lovers alike.

Don’t miss the opportunity to own a real piece of prehistoric life!

(Actual as seen)

Only 1 left in stock

Description

Crocodile Tibia Fossil from the Kem Kem Beds, Morocco
This genuine crocodile tibia fossil originates from the renowned Kem Kem Beds of the Tegana Formation in the Kem Kem Basin, Morocco. Dating to the Upper Cretaceous period, specifically the Cenomanian stage approximately 100–94 million years ago, this specimen represents a powerful semi-aquatic predator that thrived alongside dinosaurs in ancient river systems. The fossil shown in the photograph is the exact specimen you will receive, carefully selected for its quality, preservation, and structural detail.

Geological Context – Tegana Formation, Kem Kem Basin
The Kem Kem Beds are one of the most important fossil-producing regions in the world, representing a vast fluvial and deltaic system that existed during the Late Cretaceous. The Tegana Formation is composed primarily of sandstones and siltstones deposited by ancient river channels, floodplains, and estuarine environments connected to the Tethys Ocean. This dynamic landscape supported a diverse ecosystem of large theropod dinosaurs, herbivores, fish, pterosaurs, and crocodilian species.

The sedimentary conditions in this region allowed for rapid burial of remains, particularly within river channel deposits, leading to the preservation of robust skeletal elements such as limb bones.

Fossil Type and Biological Classification
This specimen represents a tibia, or lower leg bone, from a crocodilian reptile belonging to the order Crocodyliformes. During the Cretaceous, crocodilians were highly diverse and occupied a range of ecological niches, from fully aquatic to semi-terrestrial forms. These ancient crocodiles were well adapted to life in river systems, where they functioned as ambush predators.

Fossilised limb bones such as this tibia provide important insight into locomotion, body structure, and the evolutionary adaptations of these reptiles within prehistoric ecosystems.

Morphological Features and Structural Characteristics
The tibia is a long, robust bone that formed a key part of the hind limb, connecting the knee joint to the ankle. This specimen displays the elongated shape typical of crocodilian limb bones, with subtle expansion at the ends where it would have articulated with adjacent bones. The surface may show natural texture and mineralisation, preserving details of the original bone structure.

The strength and density of the tibia reflect its functional role in supporting the animal’s body weight and enabling movement both in water and on land. Its preserved form provides valuable information about the biomechanics and lifestyle of Cretaceous crocodilians.

Depositional Environment and Preservation
The fossilisation process occurred within sediment-rich river systems where remains were rapidly buried by sand and silt. This rapid burial protected the bone from scavenging and environmental degradation. Over millions of years, mineralisation replaced the original organic material, preserving the bone in stone while retaining its overall structure.

The Kem Kem Beds are particularly noted for producing well-preserved vertebrate fossils, with bones often retaining strong structural integrity and clear anatomical features.

Authenticity and Certificate of Guarantee
This fossil is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee card. Each piece is carefully handled and prepared to preserve its natural condition, ensuring you receive an authentic and high-quality fossil suitable for any collection.

Ideal for Collectors, Display, and Educational Use
A crocodile tibia fossil from the Kem Kem Beds is a unique and scientifically significant addition to any fossil collection. Its connection to ancient river ecosystems and prehistoric reptiles makes it both visually interesting and educational. Whether displayed in a cabinet, study, or educational setting, it offers a tangible link to Cretaceous life.

Size and Exact Specimen Assurance
Please refer to the photograph for full sizing and scale. The fossil shown is the exact specimen you will receive, ensuring complete confidence and providing a distinctive addition to your collection.

Additional information

Era

Cretaceous

Origin

Morocco

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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