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Coelodonta antiquitatis Woolly Rhino Jaw with Tooth Fossil | Pleistocene Devensian | Sutton Courtenay Oxfordshire UK | Genuine Specimen

£288.00

A rare and authentic Woolly Rhinoceros (Coelodonta antiquitatis) fossil jaw section with an in-situ tooth, discovered in Sutton Courtenay (Sutton Hardcourt), Oxfordshire, England. This specimen dates to the Pleistocene Epoch, more specifically the Devensian Stage (~115,000 to 11,700 years ago), when glacial cycles dominated Northern Europe and megafauna roamed the Ice Age landscapes.

Geological & Stratigraphic Context:

  • Location: Sutton Courtenay, Oxfordshire, UK
  • Geological Epoch: Pleistocene
  • Stage: Devensian (Late Pleistocene)
  • Depositional Environment: Cold-climate river terrace gravels and glacial outwash plains typical of British Ice Age fossil sites. These deposits often contain bones and teeth of large mammals adapted to tundra and steppe-like environments.

Fossil Type & Classification:

  • Type: Fossilised Jaw Section with Tooth in situ
  • Species: Coelodonta antiquitatis (Blumenbach, 1799)
  • Common Name: Woolly Rhinoceros
  • Order: Perissodactyla
  • Family: Rhinocerotidae
  • Superfamily: Rhinocerotoidea

Morphological Features:

  • Robust jaw fragment with partial or complete molar preserved in situ
  • Hypsodont (high-crowned) tooth showing complex enamel folding and wear from grinding tough vegetation
  • Compact bone structure indicative of large Ice Age herbivores

Notable Details:

  • The Woolly Rhinoceros was a key member of the Pleistocene megafauna, ranging from Western Europe to Siberia, adapted to cold steppes and mammoth tundra
  • Fossils from Sutton Courtenay are notable for their excellent preservation and significance within the British Quaternary fossil record
  • This specimen is carefully chosen for its anatomical clarity and completeness, ideal for display or research

Biozone:

  • Typically falls within the Late Devensian faunal assemblage, often associated with other cold-adapted mammals like Mammuthus primigenius and Bison priscus

Specimen & Scale Information:

  • Scale Rule Squares/Cube = 1cm — Please consult the photograph for precise dimensions
  • The item in the photo is the exact fossil you will receive, selected for preservation and clarity

 

Certification & Authenticity: All of our fossils are 100% genuine specimens, and this item comes with a Certificate of Authenticity. This Woolly Rhino jaw with tooth has been ethically sourced and professionally assessed for authenticity.

 

Own a tangible piece of Ice Age history with this remarkable Woolly Rhinoceros fossil jaw and tooth from Pleistocene Oxfordshire—a standout addition to any fossil or prehistoric mammal collection.

(Actual as seen)

Only 1 left in stock

SKU: XV5001 Category:

Description

A rare and authentic Woolly Rhinoceros (Coelodonta antiquitatis) fossil jaw section with an in-situ tooth, discovered in Sutton Courtenay (Sutton Hardcourt), Oxfordshire, England. This specimen dates to the Pleistocene Epoch, more specifically the Devensian Stage (~115,000 to 11,700 years ago), when glacial cycles dominated Northern Europe and megafauna roamed the Ice Age landscapes.

Geological & Stratigraphic Context:

  • Location: Sutton Courtenay, Oxfordshire, UK
  • Geological Epoch: Pleistocene
  • Stage: Devensian (Late Pleistocene)
  • Depositional Environment: Cold-climate river terrace gravels and glacial outwash plains typical of British Ice Age fossil sites. These deposits often contain bones and teeth of large mammals adapted to tundra and steppe-like environments.

Fossil Type & Classification:

  • Type: Fossilised Jaw Section with Tooth in situ
  • Species: Coelodonta antiquitatis (Blumenbach, 1799)
  • Common Name: Woolly Rhinoceros
  • Order: Perissodactyla
  • Family: Rhinocerotidae
  • Superfamily: Rhinocerotoidea

Morphological Features:

  • Robust jaw fragment with partial or complete molar preserved in situ
  • Hypsodont (high-crowned) tooth showing complex enamel folding and wear from grinding tough vegetation
  • Compact bone structure indicative of large Ice Age herbivores

Notable Details:

  • The Woolly Rhinoceros was a key member of the Pleistocene megafauna, ranging from Western Europe to Siberia, adapted to cold steppes and mammoth tundra
  • Fossils from Sutton Courtenay are notable for their excellent preservation and significance within the British Quaternary fossil record
  • This specimen is carefully chosen for its anatomical clarity and completeness, ideal for display or research

Biozone:

  • Typically falls within the Late Devensian faunal assemblage, often associated with other cold-adapted mammals like Mammuthus primigenius and Bison priscus

Specimen & Scale Information:

  • Scale Rule Squares/Cube = 1cm — Please consult the photograph for precise dimensions
  • The item in the photo is the exact fossil you will receive, selected for preservation and clarity

 

Certification & Authenticity: All of our fossils are 100% genuine specimens, and this item comes with a Certificate of Authenticity. This Woolly Rhino jaw with tooth has been ethically sourced and professionally assessed for authenticity.

 

Own a tangible piece of Ice Age history with this remarkable Woolly Rhinoceros fossil jaw and tooth from Pleistocene Oxfordshire—a standout addition to any fossil or prehistoric mammal collection.

Additional information

Era

Pleistocene

Origin

United Kingdom

Pleistocene Information

The Pleistocene Epoch (2.58 million – 11,700 years ago) was a time of repeated ice ages, shaping Earth's landscapes and ecosystems. Massive glaciers advanced and retreated, covering large parts of North America, Europe, and Asia. This period saw the rise of megafauna, including woolly mammoths, saber-toothed cats, giant ground sloths, and cave bears. Early humans (Homo erectus, Neanderthals, and Homo sapiens) spread across the world, developing tools, art, and early societies. Many species adapted to harsh, cold climates, but as the Ice Age ended, global warming and human hunting contributed to the extinction of many large mammals. The Pleistocene transitions into the Holocene, the current epoch, marking the beginning of human civilization.

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