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Ursus deningeri Bear Tooth Fossil Pleistocene UK Westbury Somerset Genuine Cave Bear Fossil Specimen Collectible

£48.00

Authentic Ursus deningeri Bear Fossil Bone from the Pleistocene of Somerset

This genuine Ursus deningeri fossil bear bone originates from Westbury-sub-Mendip in Somerset, United Kingdom, a locality well known for its important Pleistocene cave deposits and Ice Age mammal fossils. Dating to the Pleistocene epoch, this specimen represents an early species of cave bear that inhabited Europe during the Middle Pleistocene.

The fossil shown in the photographs is the exact specimen you will receive, carefully selected for its preservation and authenticity. Each piece includes a Certificate of Authenticity lifetime guarantee generic card, confirming the fossil as a genuine prehistoric specimen.

Please refer to the photographs for full sizing and scale of the fossil bone.

The Species – Ursus deningeri

Ursus deningeri, commonly known as Deninger’s bear, was a large prehistoric bear species that lived throughout Europe during the Middle Pleistocene. It is widely considered to be an evolutionary predecessor of the later cave bear (Ursus spelaeus), which became widespread during the Late Pleistocene Ice Age.

Deninger’s bear belonged to the Order Carnivora, within the Family Ursidae, the same family that includes modern bears. Fossil remains of this species are important for understanding the evolutionary history of large European bears.

Key anatomical characteristics of Ursus deningeri included:

  • A large and robust skeletal structure
  • Powerful limb bones supporting significant body mass
  • Broad molars adapted primarily for plant-based diets
  • Cranial features that later evolved into the distinctive domed skull of cave bears

Adults were large animals, comparable in size to later cave bears, and were among the dominant mammals inhabiting European landscapes during the Middle Pleistocene.

The species was formally described by the German palaeontologist Wilhelm von Reichenau in 1904, based on fossil remains discovered in European cave deposits.

Geological Age – The Pleistocene Epoch

The Pleistocene epoch, spanning from approximately 2.58 million to 11,700 years ago, was a period characterised by repeated glacial cycles and major climatic fluctuations. Large mammals adapted to these environments formed the famous Pleistocene megafauna.

During this time, Britain and continental Europe supported diverse animal communities including:

  • Early cave bears such as Ursus deningeri
  • Woolly mammoths (Mammuthus primigenius)
  • Steppe bison (Bison priscus)
  • Giant deer (Megaloceros giganteus)
  • Early human populations and other large carnivores

Fossils from the Pleistocene provide key insights into the ecological conditions and evolutionary processes that shaped Ice Age environments.

Depositional Environment – Mendip Cave Systems

The Mendip Hills of Somerset are famous for their extensive limestone cave systems formed within Carboniferous Limestone. These caves developed through the dissolution of carbonate rock by groundwater, creating underground chambers and passages.

Such caves often served as natural shelters for animals and became important fossil preservation sites. Over thousands of years, bones accumulated within cave chambers through natural death, predator activity, and sediment deposition.

The site at Westbury-sub-Mendip has produced significant Pleistocene fossil material, including bones of bears and other large mammals. Cave environments provide favourable conditions for fossil preservation because skeletal remains can become rapidly buried and protected from surface weathering.

Morphology and Fossil Preservation

The fossil bone preserved in this specimen displays the characteristic mineralisation typical of Pleistocene mammal fossils recovered from cave deposits.

Common preservation features of Ice Age bear bones include:

  • Dense mineralised bone structure resulting from fossilisation
  • Natural surface textures reflecting original anatomical features
  • Colouration created by mineral absorption during burial
  • Structural robustness associated with large mammalian limb or skeletal elements

These characteristics provide valuable evidence for palaeontologists studying the anatomy and evolutionary relationships of prehistoric bears.

Collector and Display Information

  • Species: Ursus deningeri
  • Common Name: Deninger’s Bear
  • Fossil Type: Fossil bone fragment
  • Geological Age: Pleistocene Epoch
  • Animal Group: Mammal
  • Order: Carnivora
  • Family: Ursidae
  • Locality: Westbury-sub-Mendip, Somerset, United Kingdom
  • Preservation: Mineralised fossil bone from cave deposits
  • Authenticity: 100% genuine fossil specimen
  • Documentation: Includes Certificate of Authenticity lifetime guarantee generic card

This Pleistocene bear fossil from the Mendip Hills represents an important part of Britain’s Ice Age fossil record. Fossils of Ursus deningeri provide insight into the evolutionary history of European cave bears and the megafauna that once inhabited prehistoric Britain.

An excellent addition to any Ice Age fossil collection, British palaeontology display, natural history collection, or educational geological exhibit, this specimen offers a tangible connection to the wildlife that lived in Britain during the Pleistocene epoch.

(Actual as seen)

Only 1 left in stock

SKU: XF0098 Category:

Description

Ursus deningeri Bear Tooth – Genuine Pleistocene Fossil from Somerset, UK
This authentic fossil tooth of Ursus deningeri, an extinct Pleistocene bear species, originates from Westbury-sub-Mendip in Somerset, United Kingdom. This carefully selected specimen represents a genuine piece of Ice Age fauna, preserved over hundreds of thousands of years. The photo provided shows the exact fossil you will receive, ensuring complete confidence in authenticity and condition.

Species Identification & Taxonomy
Ursus deningeri is an extinct species of bear belonging to the family Ursidae and order Carnivora. It is widely considered an ancestral form of the later cave bear (Ursus spelaeus), which became prominent during the Late Pleistocene. This species lived during the Middle Pleistocene and played an important role in the evolutionary history of European bears. Fossil remains, particularly teeth, are commonly used for identification due to their durability and distinctive morphology.

Geological Age & Context
This specimen dates to the Pleistocene epoch, spanning approximately 2.6 million to 11,700 years ago. The deposits at Westbury-sub-Mendip are well known for yielding a diverse assemblage of Pleistocene vertebrate fossils. These fossils are typically preserved within fissure fills and cave deposits formed in Carboniferous limestone, where sediment and organic remains accumulated over time.

Locality – Westbury-sub-Mendip, Somerset
Westbury-sub-Mendip is one of the most significant Pleistocene fossil localities in the United Kingdom. The site has produced remains of large mammals including bears, hyenas, and other Ice Age fauna. The fossils are often found within ancient cave systems and fissures, where bones and teeth were transported or accumulated through natural processes such as water movement, predation, or denning behaviour.

Tooth Morphology & Preservation
This fossil tooth displays the robust structure typical of large bear dentition, with well-developed enamel and dentine layers. The crown may show wear patterns consistent with the diet and behaviour of the animal, while the root structure provides additional insight into its placement within the jaw. The preservation quality reflects mineralisation processes where original organic material has been replaced or reinforced by minerals, allowing the tooth to remain intact over geological timescales.

Depositional Environment & Fossilisation
The fossil formed within a karstic limestone environment, where fissures and caves acted as natural traps and repositories for organic remains. Over time, sediments filled these spaces, and mineral-rich groundwater facilitated fossilisation. These conditions are ideal for preserving durable elements such as teeth, which are often found in excellent condition compared to other skeletal remains.

Scientific & Educational Significance
Fossil teeth of Ursus deningeri are valuable for understanding the evolution, diet, and ecological role of Pleistocene bears. Their morphology provides insight into feeding habits and environmental adaptation. Specimens from well-documented localities such as Westbury-sub-Mendip are particularly significant for research and comparative studies.

Collecting, Display & Gifting
This fossil tooth is an exceptional addition to any fossil collection, offering both scientific importance and visual appeal. Its compact size makes it suitable for display in cabinets, specimen trays, or educational collections. It also makes a unique and meaningful gift for fossil collectors, natural history enthusiasts, or those with an interest in Ice Age fauna.

Authenticity & Guarantee
This fossil is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee generic card. Each piece is carefully selected to ensure authenticity, provenance, and quality.

Additional Information

  • Species: Ursus deningeri

  • Family: Ursidae

  • Order: Carnivora

  • Geological Period: Pleistocene

  • Locality: Westbury-sub-Mendip, Somerset, UK

  • Fossil Type: Tooth

  • Specimen: Exact piece shown in photo

  • Full sizing: Please refer to photo

This Ursus deningeri bear tooth fossil provides a direct connection to the Pleistocene epoch, offering a rare opportunity to own a genuine specimen from Britain’s prehistoric past.

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