Fossils for Sale - High-quality BRITISH and WORLDWIDE Fossils. An impressive selection of fossils, including Ammonites, Trilobites, Belemnites, Fossil Fish, Fossil Shark Teeth, Fossilised Insects in Amber, Dinosaurs, and Reptiles. UK Fossils was formed in 1988 and collects and preps our own fossils in the heart of the Jurassic Coast, collecting fossils from Lyme Regis, Charmouth and Somerset. Our passion for fossils is reflected in our carefully curated collection, which includes some of the rarest and most unique specimens available.

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Stratiolamia beltinge (herne bay) fossil shark tooth, eocene, kent, uk certificated
Stratiolamia beltinge (herne bay) fossil shark tooth, eocene, kent, uk certificated - Image 2

Stratiolamia beltinge (herne bay) fossil shark tooth, eocene, kent, uk certificated

Original price was: £12.00.Current price is: £8.40.

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity

Species: Stratiolamia

Specimen: Tooth

Age: Eocene

Location: Beltinge (Herne Bay), Kent, UK

 

Scale cube=1cm: Full sizing please see photo

 

Over 50 million years ago England was under water! These genuine Sand Shark teeth were found at Herne Bay in Kent, from sharks that once controlled the oceans. When a sharks teeth become worn the predator will ‘shed’ these teeth, and these will be replaced with new sharper, stronger teeth. However, unlike humans, Sharks are known for re-shedding hundreds of teeth on a regular basis, which makes them a fruitful find with fossil hunters.

 

ACTUAL AS SEEN: The image shows the EXACT specimen you will receive. The specimen has been carefully hand selected and photographed. Measurements are as accurate as possible, though be aware measuring precise dimensions can be difficult from irregular shaped items. Whilst we portray colours as close to life-like as we can, colours will vary if taken in sunlight, indoors, from monitor to monitor and device to device. Once this specimen is sold, we will update this listing with new similar selected item, with a new photo and dimensions.

(Actual as seen)

Only 1 left in stock

SKU: FP9046 Category:

Description

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity

Species: Stratiolamia

Specimen: Tooth

Age: Eocene

Location: Beltinge (Herne Bay), Kent, UK

 

Scale cube=1cm: Full sizing please see photo

 

Over 50 million years ago England was under water! These genuine Sand Shark teeth were found at Herne Bay in Kent, from sharks that once controlled the oceans. When a sharks teeth become worn the predator will ‘shed’ these teeth, and these will be replaced with new sharper, stronger teeth. However, unlike humans, Sharks are known for re-shedding hundreds of teeth on a regular basis, which makes them a fruitful find with fossil hunters.

 

ACTUAL AS SEEN: The image shows the EXACT specimen you will receive. The specimen has been carefully hand selected and photographed. Measurements are as accurate as possible, though be aware measuring precise dimensions can be difficult from irregular shaped items. Whilst we portray colours as close to life-like as we can, colours will vary if taken in sunlight, indoors, from monitor to monitor and device to device. Once this specimen is sold, we will update this listing with new similar selected item, with a new photo and dimensions.

Additional information

Era

Eocene
Origin

United Kingdom

Eocene Information

The Eocene Period (56–33.9 million years ago) was a time of warm global temperatures and the rapid evolution of mammals following the extinction of the dinosaurs. The climate was hot and humid, with lush rainforests covering much of the planet, even near the poles. Mammals diversified into new ecological roles, with early primates, whales (like Basilosaurus), large herbivores, and carnivores emerging. Birds and reptiles also thrived, and the first grasses began spreading, setting the stage for later grassland ecosystems. By the late Eocene, the Earth’s climate cooled significantly, leading to the formation of the first Antarctic ice sheets and the eventual transition to the drier, cooler Oligocene Period.

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