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Red Deer Antler Fossil Fragment Pleistocene Norfolk UK Genuine Ice Age Specimen with Certificate

£46.80

(Actual as seen)

Only 1 left in stock

SKU: P00705 Category:

Description

Genuine Pleistocene Red Deer Antler Fossil from Norfolk, United Kingdom

This genuine Red Deer Antler fossil fragment is a fascinating Ice Age mammal specimen originating from Pleistocene deposits in Norfolk, United Kingdom. Preserved for thousands of years within ancient sediments, this fossilised antler fragment represents part of a prehistoric Red Deer that once roamed the cold grasslands, river valleys and woodland environments of Ice Age Britain.

The specimen shown in the photographs is the exact fossil you will receive. Carefully selected for its natural preservation, texture and display appeal, this fossil antler fragment provides an authentic connection to Britain’s prehistoric past and the large mammals that inhabited the region during the Pleistocene Epoch.

This fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the specimen is 100% genuine.

Full sizing please see photo.

About Red Deer and Fossil Antlers

The Red Deer, belonging to the species Cervus elaphus, is one of the largest and most iconic deer species in Europe and has inhabited Britain for thousands of years. During the Pleistocene Epoch, populations of Red Deer lived alongside a diverse Ice Age fauna that included mammoths, woolly rhinoceroses, giant deer and steppe bison.

Male Red Deer develop large branching antlers composed of bone which are shed and regrown annually. Fossilised antler fragments are highly collectable because they preserve evidence of the animal’s growth structure, surface texture and natural biological development.

This specimen displays authentic fossilised antler material with visible natural texture and internal structure preserved through mineralisation over thousands of years. Antlers were used for display, territorial combat and mating competition, making them one of the most recognisable anatomical features of prehistoric deer species.

Pleistocene Britain and the Ice Age Environment

The Pleistocene Epoch spanned approximately 2.58 million to 11,700 years ago and was characterised by repeated glacial and interglacial periods. During colder phases, much of Britain experienced tundra and steppe-like conditions, while warmer intervals supported forests, wetlands and river systems rich in wildlife.

Norfolk is one of Britain’s most important regions for Pleistocene fossil discoveries due to its extensive river deposits, coastal exposures and glacial sediments. Fossils recovered from Norfolk provide valuable evidence for understanding Ice Age ecosystems, climate change and the evolution of large mammals in prehistoric Europe.

Many fossils from this region are recovered from ancient river gravels and coastal deposits where bones, antlers and teeth became buried within sediment and gradually fossilised through mineral replacement processes.

Natural Fossil Preservation

This fossil antler fragment retains its genuine natural character and has not been artificially replicated or reconstructed. The visible textures, coloration and mineralisation developed naturally during fossilisation and reflect the specimen’s long geological history.

The fossil has been carefully preserved to maintain the integrity of the original material while allowing the natural surface detail to remain clearly visible. Each specimen is entirely unique due to natural growth patterns and fossilisation processes.

Its earthy tones and organic structure make it an excellent addition to fossil collections, Ice Age displays, natural history collections or educational exhibits focused on prehistoric mammals and British palaeontology.

Geological and Historical Significance

Pleistocene mammal fossils from the United Kingdom are highly valued by collectors and researchers alike due to their importance in reconstructing ancient climates and ecosystems. Red Deer remains are especially significant because the species survived multiple climatic fluctuations and continues to exist today, providing a direct evolutionary connection between modern wildlife and Ice Age fauna.

This fossil fragment offers collectors the opportunity to own a genuine piece of prehistoric Britain preserved from a time when large mammals dominated the ancient landscapes of Europe.

The specimen is ideal for collectors of Ice Age fossils, British fossils, fossil mammals, cervid remains, antler fossils and authentic prehistoric natural history specimens.

Certificate of Authenticity

Included with the fossil is a Certificate of Authenticity lifetime guarantee generic card confirming that the specimen is genuine. The photographs provided show the exact fossil you will receive, ensuring complete confidence in the authenticity and individuality of the piece.

 

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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