Fossil tooth - Lot of 3 Cretaceous Fossil Teeth – Spinosaurus, Globidens & Mosasaur – Morocco (No reserve price)

00
days
12
hours
14
minutes
39
seconds
Current bid
€ 2
No reserve price
Sullivan Halipré
Expert
Estimate  € 150 - € 200
DE
€2

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Description from the seller

Interesting collection of three fossil teeth from the Late Cretaceous of Morocco, representing different predatory reptiles that inhabited the region approximately 100–66 million years ago.
The lot includes:
Spinosaurus sp. tooth – A characteristic elongated and conical tooth with visible longitudinal striations. Spinosaurus was a large theropod dinosaur adapted to a semi-aquatic lifestyle and is one of the most iconic predators of the Cretaceous.
Globidens sp. tooth with root – A robust, rounded tooth characteristic of this specialized mosasaur. Its globular teeth were adapted for crushing hard-shelled prey such as molluscs and other marine organisms.
Mosasaur tooth with root – A large, curved tooth belonging to a mosasaur, one of the dominant marine reptiles of the Late Cretaceous seas.
The specimens show natural wear, cracks and mineralization consistent with their fossil nature. Some stabilization or restoration may be present, as commonly occurs in Moroccan fossil specimens of this type.

Interesting collection of three fossil teeth from the Late Cretaceous of Morocco, representing different predatory reptiles that inhabited the region approximately 100–66 million years ago.
The lot includes:
Spinosaurus sp. tooth – A characteristic elongated and conical tooth with visible longitudinal striations. Spinosaurus was a large theropod dinosaur adapted to a semi-aquatic lifestyle and is one of the most iconic predators of the Cretaceous.
Globidens sp. tooth with root – A robust, rounded tooth characteristic of this specialized mosasaur. Its globular teeth were adapted for crushing hard-shelled prey such as molluscs and other marine organisms.
Mosasaur tooth with root – A large, curved tooth belonging to a mosasaur, one of the dominant marine reptiles of the Late Cretaceous seas.
The specimens show natural wear, cracks and mineralization consistent with their fossil nature. Some stabilization or restoration may be present, as commonly occurs in Moroccan fossil specimens of this type.

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