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Micraster coranguinum Fossil Echinoid in Flint – Cretaceous Sea Urchin – Small Dole, Sussex, UK – Genuine with Certificate

£18.00

This listing features a beautifully preserved Micraster coranguinum fossil echinoid, found encased in flint from the Gravel Beds of Small Dole, Sussex, United Kingdom. The specimen is displayed with a 1cm scale cube for accurate size reference. Please see the photo for the exact specimen you will receive.

Micraster coranguinum is a classic and well-known species of fossil echinoid (sea urchin) from the Late Cretaceous period. It is distinguished by its distinct heart-shaped profile and fine ambulacral grooves. This particular specimen is preserved within flint, a hard, silica-rich sediment formed in marine chalk deposits.

Geological & Palaeontological Information:

  • Species: Micraster coranguinum
  • Type: Fossil Echinoid (Sea Urchin)
  • Geological Age: Late Cretaceous (Santonian–Campanian)
  • Location: Small Dole, Sussex, UK
  • Formation: Gravel Beds (derived from Chalk Formation)
  • Preservation: In flint nodule
  • Family: Spatangidae
  • Order: Spatangoida
  • Class: Echinoidea
  • Morphology Features: Heart-shaped test, sunken petaloid ambulacra, symmetrical form, flattened base
  • Depositional Environment: Shallow marine chalk sea; flint formed by post-depositional silica replacement of carbonate sediments
  • Notable: Iconic British fossil used as a biostratigraphic marker in the Upper Chalk
  • Biozone: Micraster coranguinum Zone (Late Cretaceous)
  • Formally Described By: Jean-Baptiste de Lamarck (1816)

Why Buy From Us?

  • All fossils are 100% genuine specimens
  • Accompanied by a Certificate of Authenticity
  • What you see is what you get – you receive the exact fossil shown
  • Expertly sourced and professionally handled

This Micraster echinoid offers a beautiful and historically significant piece from Britain’s fossil-rich chalk deposits. It’s ideal for collectors, educators, or as a natural history display piece.

(Actual as seen)

Out of stock

SKU: SF0421 Category:

Description

This listing features a beautifully preserved Micraster coranguinum fossil echinoid, found encased in flint from the Gravel Beds of Small Dole, Sussex, United Kingdom. The specimen is displayed with a 1cm scale cube for accurate size reference. Please see the photo for the exact specimen you will receive.

Micraster coranguinum is a classic and well-known species of fossil echinoid (sea urchin) from the Late Cretaceous period. It is distinguished by its distinct heart-shaped profile and fine ambulacral grooves. This particular specimen is preserved within flint, a hard, silica-rich sediment formed in marine chalk deposits.

Geological & Palaeontological Information:

  • Species: Micraster coranguinum
  • Type: Fossil Echinoid (Sea Urchin)
  • Geological Age: Late Cretaceous (Santonian–Campanian)
  • Location: Small Dole, Sussex, UK
  • Formation: Gravel Beds (derived from Chalk Formation)
  • Preservation: In flint nodule
  • Family: Spatangidae
  • Order: Spatangoida
  • Class: Echinoidea
  • Morphology Features: Heart-shaped test, sunken petaloid ambulacra, symmetrical form, flattened base
  • Depositional Environment: Shallow marine chalk sea; flint formed by post-depositional silica replacement of carbonate sediments
  • Notable: Iconic British fossil used as a biostratigraphic marker in the Upper Chalk
  • Biozone: Micraster coranguinum Zone (Late Cretaceous)
  • Formally Described By: Jean-Baptiste de Lamarck (1816)

Why Buy From Us?

  • All fossils are 100% genuine specimens
  • Accompanied by a Certificate of Authenticity
  • What you see is what you get – you receive the exact fossil shown
  • Expertly sourced and professionally handled

This Micraster echinoid offers a beautiful and historically significant piece from Britain’s fossil-rich chalk deposits. It’s ideal for collectors, educators, or as a natural history display piece.

Additional information

Era

Cretaceous

Origin

United Kingdom

Cretaceous Information

The Cretaceous Period (145–66 million years ago) was the final era of the Mesozoic, marked by the dominance of dinosaurs and the rise of flowering plants. It had a warm, greenhouse climate, with high sea levels that created vast shallow inland seas. Marine life flourished, including mosasaurs, ammonites, and rudist reefs, while the land was ruled by iconic dinosaurs like Tyrannosaurus rex, Triceratops, and Spinosaurus. Mammals and birds diversified, and insects thrived. The period ended with the mass extinction event, likely caused by an asteroid impact, wiping out the dinosaurs and paving the way for the rise of mammals in the Cenozoic.

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