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ART🦖FOSSIL🦕MUSEUM🦣FOR SALE🦏ART🦖FOSSIL🦕MUSEUM🦣FOR SALE🦏

[Introduction] Real Fossil of Ophiopetra sp (Paleozoic Era, Devonian Period, Morocco)


販売中のクモヒトデ(モロッコ産)の実物化石(1/2)

This is a real fossil of Ophiopetra sp (from Morocco) currently available for sale. The fossil, dating back 300 to 400 million years, remarkably preserves the five slender, whip-like arms and the central disk.



販売中のクモヒトデ(モロッコ産)の実物化石(2/2)

Interestingly, Ophiopetra sp still exist today and are considered a type of living fossil.



オリジナル台座との組み合わせ

By combining it with the separately sold original stand featuring our logo, the fossil’s appeal as an art piece is enhanced, making it a perfect addition to your home or office, creating a unique and special atmosphere.




Ophiopetra sp
クモヒトデ(Ophiopetra sp)
Ophiopetra sp
  • Era: Paleozoic Era, Devonian Period (416 million to 360 million years ago)

  • Location: Morocco

  • Price: Available in-store(Note: The original stand is sold separately.)

  • Size: Approximately 15 cm wide (varies by specimen)




the Devonian Period of the Paleozoic Era

The Devonian Period (approximately 416 million to 360 million years ago) is known as the “Age of Fishes,” during which fish diversified and the first tetrapods ventured onto land. The Devonian continued the increase in biodiversity seen in the preceding Silurian Period, and further evolutionary advancements occurred. Large land plants, such as ferns and gymnosperms, thrived, leading to the formation of vast forests. This resulted in an increase in Earth’s oxygen levels, which promoted the growth of larger animals.


During this time, fish developed a wide variety of forms and ecological roles, leading to an increasingly complex marine ecosystem. Jawed fish became dominant, and early sharks and armored fish appeared. Additionally, the evolution of tetrapods progressed, with the first amphibians moving onto land. However, the end of the Devonian saw a major extinction event, which wiped out many marine species and some terrestrial plants. This extinction is thought to have been caused by climate change and ocean anoxia.




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