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British Chalk Fossil Echinoid – Echinocorys scutata | Santonian Upper Chalk Foreness Point Margate Kent UK | Genuine Specimen with COA

Original price was: £48.00.Current price is: £43.20.

Offered here is a classic example of Echinocorys scutata, an extinct fossil echinoid (sea urchin) from the Upper Chalk Formation, deposited during the Santonian stage of the Late Cretaceous period, and collected from the well-known coastal site of Foreness Point, Margate, Kent, UK. This iconic species is one of the most recognisable and important fossils from the British chalk.

Fossil Type: Echinoid (Sea Urchin)

Species: Echinocorys scutata

Geological Period: Late Cretaceous (~86.3 to 83.6 million years ago)

Geological Stage: Santonian

Formation: Upper Chalk (Chalk Group)

Location: Foreness Point, Margate, Kent, United Kingdom

Scale Rule: Squares/Cube = 1cm (See photo for full sizing details)

Specimen: The fossil in the photo is the exact one you will receive

Authenticity: All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity

Geological and Paleontological Context

Echinocorys scutata is a widespread and well-documented species of irregular echinoid, commonly found throughout the Upper Cretaceous chalk of Europe. It lived as a deposit feeder, burrowing within soft seafloor sediments beneath the ancient Cretaceous seas.

  • Phylum: Echinodermata
  • Class: Echinoidea
  • Order: Holasteroida
  • Family: Holasteridae
  • Genus: Echinocorys
  • Species: scutata
  • Depositional Environment: Quiet, shallow marine shelf with fine carbonate sedimentation from coccoliths; conditions ideal for fossilisation of echinoids and other marine invertebrates
  • Morphological Features: Oval to subglobular test (shell), well-developed ambulacral petals on the aboral surface, with a central periproct and flattened oral surface; radial symmetry with slight elongation along the oral-aboral axis
  • Biozone: Frequently found in mid-to-late Santonian stratigraphic levels; associated with key foraminiferal and inoceramid zones
  • Notable: Echinocorys scutata is an important biostratigraphic indicator for Upper Cretaceous chalk sequences and is widely used in geological studies of the British chalk

Why This Fossil is Special

This specimen is a true classic of British fossil collecting. Well-preserved, naturally shaped, and collected from a site of national geological importance, this Echinocorys scutata fossil makes an excellent teaching tool or collector’s piece. Its simple symmetry and subtle surface features also make it a beautiful display fossil.

Why Buy From Us?

  • 100% genuine fossil with Certificate of Authenticity
  • You receive the exact item pictured
  • Carefully sourced from reputable British chalk fossil sites
  • Perfect for collectors, educators, or display in natural history settings

Add a timeless fossil to your collection with this Echinocorys scutata chalk echinoid from the Santonian stage of the Upper Cretaceous, Foreness Point, Kent—an elegant remnant of ancient marine life from over 85 million years ago.

(Actual as seen)

Only 1 left in stock

SKU: UF3410 Category:

Description

Offered here is a classic example of Echinocorys scutata, an extinct fossil echinoid (sea urchin) from the Upper Chalk Formation, deposited during the Santonian stage of the Late Cretaceous period, and collected from the well-known coastal site of Foreness Point, Margate, Kent, UK. This iconic species is one of the most recognisable and important fossils from the British chalk.

Fossil Type: Echinoid (Sea Urchin)

Species: Echinocorys scutata

Geological Period: Late Cretaceous (~86.3 to 83.6 million years ago)

Geological Stage: Santonian

Formation: Upper Chalk (Chalk Group)

Location: Foreness Point, Margate, Kent, United Kingdom

Scale Rule: Squares/Cube = 1cm (See photo for full sizing details)

Specimen: The fossil in the photo is the exact one you will receive

Authenticity: All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity

Geological and Paleontological Context

Echinocorys scutata is a widespread and well-documented species of irregular echinoid, commonly found throughout the Upper Cretaceous chalk of Europe. It lived as a deposit feeder, burrowing within soft seafloor sediments beneath the ancient Cretaceous seas.

  • Phylum: Echinodermata
  • Class: Echinoidea
  • Order: Holasteroida
  • Family: Holasteridae
  • Genus: Echinocorys
  • Species: scutata
  • Depositional Environment: Quiet, shallow marine shelf with fine carbonate sedimentation from coccoliths; conditions ideal for fossilisation of echinoids and other marine invertebrates
  • Morphological Features: Oval to subglobular test (shell), well-developed ambulacral petals on the aboral surface, with a central periproct and flattened oral surface; radial symmetry with slight elongation along the oral-aboral axis
  • Biozone: Frequently found in mid-to-late Santonian stratigraphic levels; associated with key foraminiferal and inoceramid zones
  • Notable: Echinocorys scutata is an important biostratigraphic indicator for Upper Cretaceous chalk sequences and is widely used in geological studies of the British chalk

Why This Fossil is Special

This specimen is a true classic of British fossil collecting. Well-preserved, naturally shaped, and collected from a site of national geological importance, this Echinocorys scutata fossil makes an excellent teaching tool or collector’s piece. Its simple symmetry and subtle surface features also make it a beautiful display fossil.

Why Buy From Us?

  • 100% genuine fossil with Certificate of Authenticity
  • You receive the exact item pictured
  • Carefully sourced from reputable British chalk fossil sites
  • Perfect for collectors, educators, or display in natural history settings

Add a timeless fossil to your collection with this Echinocorys scutata chalk echinoid from the Santonian stage of the Upper Cretaceous, Foreness Point, Kent—an elegant remnant of ancient marine life from over 85 million years ago.

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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