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Ursus spelaeus Cave Bear Fossil Bone Pleistocene France Ice Age Bear Fossil

£42.00

Authentic Ursus spelaeus Cave Bear Fossil Bone from the Pleistocene of France

This genuine Ursus spelaeus cave bear fossil bone originates from Gondemans-les-Moulins in the Doubs region of France, a locality known for important Ice Age fossil discoveries. Dating to the Pleistocene epoch, this specimen represents the remains of one of the most iconic large mammals of the European Ice Age.

The fossil displayed in the photographs is the exact specimen you will receive, carefully selected for its preservation and authenticity. Each fossil includes a Certificate of Authenticity lifetime guarantee generic card, confirming that the specimen is a genuine fossil from the Pleistocene period.

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

The Ice Age Species – Ursus spelaeus

Ursus spelaeus, commonly known as the cave bear, was a large species of bear that inhabited Europe throughout much of the Pleistocene epoch, becoming extinct approximately 24,000 years ago near the end of the last Ice Age.

Cave bears belonged to the Order Carnivora, Family Ursidae, and were closely related to modern brown bears (Ursus arctos). However, cave bears were typically larger and more heavily built, with a distinctive domed skull and robust skeletal structure.

Key anatomical features of Ursus spelaeus included:

  • A large, heavy skeletal frame adapted for cold Ice Age climates
  • Massive limb bones designed to support considerable body weight
  • Broad teeth adapted primarily for herbivorous feeding, although they were capable of opportunistic omnivory
  • Thick fur and fat reserves allowing survival in glacial environments

Adult cave bears could reach lengths of over 3 metres when standing upright and were among the largest terrestrial carnivores of the Pleistocene European landscape.

Geological Age – The Pleistocene Epoch

The Pleistocene epoch, which lasted from approximately 2.58 million to 11,700 years ago, is commonly referred to as the Ice Age due to repeated cycles of glacial expansion and retreat. During this time, Europe hosted a diverse assemblage of large mammals known as Pleistocene megafauna.

These ecosystems included species such as:

  • Woolly mammoths (Mammuthus primigenius)
  • Woolly rhinoceroses (Coelodonta antiquitatis)
  • Cave lions (Panthera spelaea)
  • Giant deer (Megaloceros giganteus)
  • Cave bears (Ursus spelaeus)

The fossils preserved from this period provide valuable insight into the ecosystems that existed during the final stages of the Ice Age.

Depositional Environment and Cave Preservation

Cave bear fossils are commonly discovered in limestone cave systems, where the animals frequently sheltered during winter months for hibernation. Many caves across Europe contain extensive deposits of cave bear bones due to generations of bears using the same sites.

The Doubs region of eastern France contains numerous limestone formations and karst landscapes, which naturally form cave environments through the dissolution of carbonate rock by groundwater. These caves provide ideal conditions for fossil preservation, as bones can accumulate and remain protected from surface weathering.

Within these sheltered environments, skeletal remains can become gradually buried by sediment or mineral deposits, allowing bones to fossilise over thousands of years.

Morphology and Fossil Preservation

The fossil bone in this specimen represents part of the skeletal structure of a cave bear and displays the natural texture and mineralisation typical of Pleistocene fossils.

Fossil bones from cave bear deposits often retain:

  • Dense mineralised bone structure
  • Surface textures showing the original anatomical form
  • Natural colouration created during fossilisation
  • Structural characteristics of large Ice Age mammals

These features provide tangible evidence of the anatomy and life history of one of the most remarkable mammals of the Pleistocene.

Collector Information

  • Species: Ursus spelaeus
  • Common Name: Cave Bear
  • Fossil Type: Fossil bone fragment
  • Geological Age: Pleistocene Epoch
  • Animal Group: Mammal
  • Order: Carnivora
  • Family: Ursidae
  • Locality: Gondemans-les-Moulins, Doubs, France
  • Preservation: Mineralised fossil bone
  • Authenticity: 100% genuine fossil specimen
  • Documentation: Includes Certificate of Authenticity lifetime guarantee generic card

This Ice Age cave bear fossil bone represents a fascinating connection to the megafauna that once inhabited Europe during the Pleistocene. Fossils of Ursus spelaeus are among the most recognisable remains of prehistoric mammals and are highly valued by collectors of Ice Age fossils.

An excellent addition to any fossil collection, Ice Age megafauna display, natural history collection, or educational geological exhibit, this specimen provides a direct link to the remarkable animals that lived during the final phases of the last glacial period.

(Actual as seen)

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Description

Authentic Ursus spelaeus Cave Bear Fossil Bone from the Pleistocene of France

This genuine Ursus spelaeus cave bear fossil bone originates from Gondemans-les-Moulins in the Doubs region of France, a locality known for important Ice Age fossil discoveries. Dating to the Pleistocene epoch, this specimen represents the remains of one of the most iconic large mammals of the European Ice Age.

The fossil displayed in the photographs is the exact specimen you will receive, carefully selected for its preservation and authenticity. Each fossil includes a Certificate of Authenticity lifetime guarantee generic card, confirming that the specimen is a genuine fossil from the Pleistocene period.

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

The Ice Age Species – Ursus spelaeus

Ursus spelaeus, commonly known as the cave bear, was a large species of bear that inhabited Europe throughout much of the Pleistocene epoch, becoming extinct approximately 24,000 years ago near the end of the last Ice Age.

Cave bears belonged to the Order Carnivora, Family Ursidae, and were closely related to modern brown bears (Ursus arctos). However, cave bears were typically larger and more heavily built, with a distinctive domed skull and robust skeletal structure.

Key anatomical features of Ursus spelaeus included:

  • A large, heavy skeletal frame adapted for cold Ice Age climates
  • Massive limb bones designed to support considerable body weight
  • Broad teeth adapted primarily for herbivorous feeding, although they were capable of opportunistic omnivory
  • Thick fur and fat reserves allowing survival in glacial environments

Adult cave bears could reach lengths of over 3 metres when standing upright and were among the largest terrestrial carnivores of the Pleistocene European landscape.

Geological Age – The Pleistocene Epoch

The Pleistocene epoch, which lasted from approximately 2.58 million to 11,700 years ago, is commonly referred to as the Ice Age due to repeated cycles of glacial expansion and retreat. During this time, Europe hosted a diverse assemblage of large mammals known as Pleistocene megafauna.

These ecosystems included species such as:

  • Woolly mammoths (Mammuthus primigenius)
  • Woolly rhinoceroses (Coelodonta antiquitatis)
  • Cave lions (Panthera spelaea)
  • Giant deer (Megaloceros giganteus)
  • Cave bears (Ursus spelaeus)

The fossils preserved from this period provide valuable insight into the ecosystems that existed during the final stages of the Ice Age.

Depositional Environment and Cave Preservation

Cave bear fossils are commonly discovered in limestone cave systems, where the animals frequently sheltered during winter months for hibernation. Many caves across Europe contain extensive deposits of cave bear bones due to generations of bears using the same sites.

The Doubs region of eastern France contains numerous limestone formations and karst landscapes, which naturally form cave environments through the dissolution of carbonate rock by groundwater. These caves provide ideal conditions for fossil preservation, as bones can accumulate and remain protected from surface weathering.

Within these sheltered environments, skeletal remains can become gradually buried by sediment or mineral deposits, allowing bones to fossilise over thousands of years.

Morphology and Fossil Preservation

The fossil bone in this specimen represents part of the skeletal structure of a cave bear and displays the natural texture and mineralisation typical of Pleistocene fossils.

Fossil bones from cave bear deposits often retain:

  • Dense mineralised bone structure
  • Surface textures showing the original anatomical form
  • Natural colouration created during fossilisation
  • Structural characteristics of large Ice Age mammals

These features provide tangible evidence of the anatomy and life history of one of the most remarkable mammals of the Pleistocene.

Collector Information

  • Species: Ursus spelaeus
  • Common Name: Cave Bear
  • Fossil Type: Fossil bone fragment
  • Geological Age: Pleistocene Epoch
  • Animal Group: Mammal
  • Order: Carnivora
  • Family: Ursidae
  • Locality: Gondemans-les-Moulins, Doubs, France
  • Preservation: Mineralised fossil bone
  • Authenticity: 100% genuine fossil specimen
  • Documentation: Includes Certificate of Authenticity lifetime guarantee generic card

This Ice Age cave bear fossil bone represents a fascinating connection to the megafauna that once inhabited Europe during the Pleistocene. Fossils of Ursus spelaeus are among the most recognisable remains of prehistoric mammals and are highly valued by collectors of Ice Age fossils.

An excellent addition to any fossil collection, Ice Age megafauna display, natural history collection, or educational geological exhibit, this specimen provides a direct link to the remarkable animals that lived during the final phases of the last glacial period.

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