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Iguanodontid Dinosaur Tooth Fossil Cretaceous Sussex UK Ashdown Formation Genuine Ornithopod Dinosaur Tooth Pett Level Hastings with COA

£240.00

Iguanodontid Ornithopod Dinosaur Tooth Fossil – Ashdown Formation, Sussex

Presented here is a genuine Ornithopod dinosaur tooth fossil attributed to an Iguanodontid, discovered within the Ashdown Formation at Pett Level near Hastings, East Sussex, England. This specimen originates from the Lower Cretaceous Wealden Group, dating to the Early Cretaceous when dinosaurs roamed extensive river plains across what is now southern Britain.

The Ashdown Formation represents one of the most important terrestrial fossil-bearing sequences in the United Kingdom, preserving remains of dinosaurs that lived approximately 140–130 million years ago. This fossil tooth provides a direct link to those Early Cretaceous ecosystems.

The specimen has been carefully selected as an attractive collector’s piece, and the listing photographs show the exact fossil you will receive. The fossil includes a Certificate of Authenticity lifetime guarantee generic card, confirming its genuine status.

Full sizing and scale can be seen in the listing photographs.

Ornithopod Dinosaurs and the Iguanodontids

This fossil tooth belonged to an ornithopod dinosaur, most likely a member of the Iguanodontidae, a group of herbivorous dinosaurs that flourished during the Early Cretaceous.

Ornithopods were part of the order Ornithischia, the bird-hipped dinosaurs. Within this group, iguanodontids represent some of the most successful and widespread plant-eating dinosaurs of the Early Cretaceous.

One of the most famous dinosaurs associated with these fossils is Iguanodon, first scientifically described in the early 19th century by English geologist Gideon Mantell, based on fossil discoveries from Sussex.

Typical characteristics of iguanodontid dinosaurs include:

• Large herbivorous body form

• Powerful hind limbs allowing bipedal locomotion

• Ability to move both on two and four legs

• Beaked jaws used for cropping vegetation

• Complex dental batteries for grinding plant material

These dinosaurs were major herbivores within Early Cretaceous ecosystems, feeding on ferns, cycads, conifers, and early flowering plants.

Tooth Morphology and Feeding Adaptation

Ornithopod dinosaur teeth were highly specialised for plant processing. Rather than simple conical teeth, iguanodontid teeth evolved into broad leaf-shaped grinding structures capable of breaking down tough vegetation.

Typical features of iguanodontid teeth include:

• Flattened crown with a leaf-like shape

• Prominent central ridge running vertically along the crown

• Fine serrations or denticles along the edges

• Enamel distribution adapted for grinding plant matter

These teeth were arranged in dental batteries, allowing worn teeth to be replaced continuously throughout the dinosaur’s life. The arrangement produced an efficient grinding surface capable of processing fibrous plant material.

The fossil tooth offered here preserves the distinctive morphology associated with herbivorous ornithopod dinosaurs.

Ashdown Formation and the Wealden Group

This fossil originates from the Ashdown Formation, part of the Wealden Group, a major Early Cretaceous sedimentary sequence exposed across Sussex and Kent.

The Ashdown Formation dates to the Valanginian Stage of the Lower Cretaceous, roughly 140–133 million years ago.

Unlike many fossil deposits formed in marine environments, the Wealden sediments represent terrestrial and freshwater environments, including:

• River channels

• Floodplains

• Freshwater lakes

• Coastal lagoons and wetlands

These environments preserved a diverse ecosystem that included dinosaurs, crocodilians, turtles, fish, and early mammals.

The sediments consist primarily of sandstones, siltstones, and mudstones deposited by river systems flowing across large floodplain landscapes.

Pett Level – A Classic Wealden Fossil Locality

The fossil was discovered at Pett Level near Hastings, one of the best known exposure sites of Wealden strata along the Sussex coast. Coastal erosion regularly reveals fossil-bearing layers containing remains of dinosaurs and other Early Cretaceous animals.

Fossils from this region have contributed significantly to the understanding of Britain’s dinosaur fauna and were central to some of the earliest dinosaur discoveries in scientific history.

The combination of river deposits, floodplain sediments, and coastal exposure makes Pett Level an important location for studying Early Cretaceous ecosystems.

Fossil Preservation

Dinosaur teeth fossilise readily because they are composed of highly mineralised enamel and dentine, which resist decay. Teeth were frequently shed during the dinosaur’s lifetime and became buried within sediment on floodplains or river channels.

Over millions of years, mineralisation preserved the tooth structure within the surrounding rock. Many specimens retain clear details of the enamel ridges and serrations that characterise ornithopod teeth.

Such fossils provide valuable evidence for the diet, anatomy, and evolutionary history of Early Cretaceous dinosaurs.

Authenticity and Collector Information

• Genuine fossil specimen – not a cast or replica

• Fossil Type: Ornithopod Dinosaur Tooth (Iguanodontid)

• Order: Ornithischia

• Clade: Ornithopoda

• Geological Formation: Ashdown Formation, Wealden Group

• Age: Lower Cretaceous, Valanginian Stage (~140–133 million years old)

• Locality: Pett Level, Hastings, East Sussex, England

• Includes Certificate of Authenticity lifetime guarantee generic card

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

This genuine Iguanodontid dinosaur tooth fossil from the Ashdown Formation of Sussex represents an excellent addition to any dinosaur fossil collection, Cretaceous fossil display, or natural history cabinet, preserving a remarkable piece of Early Cretaceous dinosaur life from southern England.

 

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Description

Iguanodontid Ornithopod Dinosaur Tooth Fossil – Ashdown Formation, Sussex

Presented here is a genuine Ornithopod dinosaur tooth fossil attributed to an Iguanodontid, discovered within the Ashdown Formation at Pett Level near Hastings, East Sussex, England. This specimen originates from the Lower Cretaceous Wealden Group, dating to the Early Cretaceous when dinosaurs roamed extensive river plains across what is now southern Britain.

The Ashdown Formation represents one of the most important terrestrial fossil-bearing sequences in the United Kingdom, preserving remains of dinosaurs that lived approximately 140–130 million years ago. This fossil tooth provides a direct link to those Early Cretaceous ecosystems.

The specimen has been carefully selected as an attractive collector’s piece, and the listing photographs show the exact fossil you will receive. The fossil includes a Certificate of Authenticity lifetime guarantee generic card, confirming its genuine status.

Full sizing and scale can be seen in the listing photographs.

Ornithopod Dinosaurs and the Iguanodontids

This fossil tooth belonged to an ornithopod dinosaur, most likely a member of the Iguanodontidae, a group of herbivorous dinosaurs that flourished during the Early Cretaceous.

Ornithopods were part of the order Ornithischia, the bird-hipped dinosaurs. Within this group, iguanodontids represent some of the most successful and widespread plant-eating dinosaurs of the Early Cretaceous.

One of the most famous dinosaurs associated with these fossils is Iguanodon, first scientifically described in the early 19th century by English geologist Gideon Mantell, based on fossil discoveries from Sussex.

Typical characteristics of iguanodontid dinosaurs include:

• Large herbivorous body form

• Powerful hind limbs allowing bipedal locomotion

• Ability to move both on two and four legs

• Beaked jaws used for cropping vegetation

• Complex dental batteries for grinding plant material

These dinosaurs were major herbivores within Early Cretaceous ecosystems, feeding on ferns, cycads, conifers, and early flowering plants.

Tooth Morphology and Feeding Adaptation

Ornithopod dinosaur teeth were highly specialised for plant processing. Rather than simple conical teeth, iguanodontid teeth evolved into broad leaf-shaped grinding structures capable of breaking down tough vegetation.

Typical features of iguanodontid teeth include:

• Flattened crown with a leaf-like shape

• Prominent central ridge running vertically along the crown

• Fine serrations or denticles along the edges

• Enamel distribution adapted for grinding plant matter

These teeth were arranged in dental batteries, allowing worn teeth to be replaced continuously throughout the dinosaur’s life. The arrangement produced an efficient grinding surface capable of processing fibrous plant material.

The fossil tooth offered here preserves the distinctive morphology associated with herbivorous ornithopod dinosaurs.

Ashdown Formation and the Wealden Group

This fossil originates from the Ashdown Formation, part of the Wealden Group, a major Early Cretaceous sedimentary sequence exposed across Sussex and Kent.

The Ashdown Formation dates to the Valanginian Stage of the Lower Cretaceous, roughly 140–133 million years ago.

Unlike many fossil deposits formed in marine environments, the Wealden sediments represent terrestrial and freshwater environments, including:

• River channels

• Floodplains

• Freshwater lakes

• Coastal lagoons and wetlands

These environments preserved a diverse ecosystem that included dinosaurs, crocodilians, turtles, fish, and early mammals.

The sediments consist primarily of sandstones, siltstones, and mudstones deposited by river systems flowing across large floodplain landscapes.

Pett Level – A Classic Wealden Fossil Locality

The fossil was discovered at Pett Level near Hastings, one of the best known exposure sites of Wealden strata along the Sussex coast. Coastal erosion regularly reveals fossil-bearing layers containing remains of dinosaurs and other Early Cretaceous animals.

Fossils from this region have contributed significantly to the understanding of Britain’s dinosaur fauna and were central to some of the earliest dinosaur discoveries in scientific history.

The combination of river deposits, floodplain sediments, and coastal exposure makes Pett Level an important location for studying Early Cretaceous ecosystems.

Fossil Preservation

Dinosaur teeth fossilise readily because they are composed of highly mineralised enamel and dentine, which resist decay. Teeth were frequently shed during the dinosaur’s lifetime and became buried within sediment on floodplains or river channels.

Over millions of years, mineralisation preserved the tooth structure within the surrounding rock. Many specimens retain clear details of the enamel ridges and serrations that characterise ornithopod teeth.

Such fossils provide valuable evidence for the diet, anatomy, and evolutionary history of Early Cretaceous dinosaurs.

Authenticity and Collector Information

• Genuine fossil specimen – not a cast or replica

• Fossil Type: Ornithopod Dinosaur Tooth (Iguanodontid)

• Order: Ornithischia

• Clade: Ornithopoda

• Geological Formation: Ashdown Formation, Wealden Group

• Age: Lower Cretaceous, Valanginian Stage (~140–133 million years old)

• Locality: Pett Level, Hastings, East Sussex, England

• Includes Certificate of Authenticity lifetime guarantee generic card

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

This genuine Iguanodontid dinosaur tooth fossil from the Ashdown Formation of Sussex represents an excellent addition to any dinosaur fossil collection, Cretaceous fossil display, or natural history cabinet, preserving a remarkable piece of Early Cretaceous dinosaur life from southern England.

 

Additional information

Era

Cretaceous

Origin

United Kingdom

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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