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Mammuthus Primigenius (Wooly Mammoth) tusk section. Siberia.(#L2)

Mammuthus Primigenius (Wooly Mammoth) tusk section. Siberia.(#L2)

Regular price £82.00 GBP
Regular price £86.00 GBP Sale price £82.00 GBP
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Own a piece of prehistory with this larger fragment of of Mammuthus Primigenius (Woolly Mammoth) tusk bark, sourced from the permafrost of Siberia. This fossilized tusk fragment is dated to approximately 30,000 years old (Devensian stage) and comes from a region where tusk material is extremely rare and highly sought after--The permafrost season in Siberia is brief, and material can only be collected for a few weeks each year. Combined with current regional high tensions, the availability of authentic Siberian tusk is increasingly limited, making this piece highly collectible.

For this reason, Siberian material is considered much more valuable compared to North Sea specimens.

YOU WILL RECIEVE THE ACTUAL FOSSIL IN THE IMAGE.

This section of tusk bark has a lovely patina, with natural unpolished character and clear growth lines and textured layering of the tusks natural formation. Its colorations and texture changes are thanks to the Siberian permafrost sealing it from the outside world for the last approximately 30,000 years. Every change of color and texture resembles a moment in time that took place during this period.

Provenance & Origin:

Location: Tamiyr, Siberia, Russia

Age: ~30,000 years (Pleistocene)

Material: Fossilized tusk bark (outer layer of tusk)

100% AUTHENTIC GUARANTEED.

Dimensions- large tusk bark section, approximately 125 x 53mm

 Supplied with a museum-style label detailing species, origin, and age, ready to display.

  • Sourced responsibly from Siberian permafrost deposits

  • Ideal for collectors, educational displays, or a unique gift

Add a piece of the Ice Age to your collection today!

Please note: Every effort is made to photograph specimens in natural light for accurate representation. However, variations in screen settings may cause slight differences in colour appearance.

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