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A-Grade British Chalk Fossil Echinoid – Echinocorys scutata striatum | Santonian Upper Chalk Broadstairs Kent UK | Genuine Specimen with COA

£36.00

This listing features an exceptional A-grade British Chalk fossil echinoid – Echinocorys scutata striatum, collected from the Upper Chalk Formation of the Santonian stage in the Late Cretaceous, at Broadstairs, Kent, UK. This rare and well-preserved subspecies is notable for its subtle yet diagnostic striations that distinguish it from other Echinocorys forms.

Fossil Type: Echinoid (Sea Urchin)

Species/Subspecies: Echinocorys scutata striatum

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

Geological Stage: Santonian

Formation: Upper Chalk (Chalk Group)

Location: Broadstairs, Kent, United Kingdom

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

Specimen: You will receive the exact item shown in the photos

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

Geological and Paleontological Context

Echinocorys scutata striatum is a subtly ornamented form of the well-known Echinocorys genus, characterised by faint surface striations visible under favourable lighting. This subspecies is found in Santonian chalk beds and reflects evolutionary adaptation to infaunal living in soft sedimentary marine environments.

  • Phylum: Echinodermata
  • Class: Echinoidea
  • Order: Holasteroida
  • Family: Holasteridae
  • Genus: Echinocorys
  • Subspecies: scutata striatum
  • Depositional Environment: Quiet, shallow marine carbonate platform dominated by coccolith deposition; excellent preservation conditions for echinoids
  • Morphological Features: Subglobular to slightly domed test with fine striations on the surface, well-formed ambulacral petals, and centrally located periproct and peristome; striations may assist in subspecies-level identification
  • Biozone: Occurs within established Santonian biostratigraphic intervals; often found alongside inoceramid bivalves and foraminifera used in chalk zonation
  • Notable: This subspecies is of particular interest for evolutionary and stratigraphic research in Late Cretaceous marine invertebrates

Why This Fossil Is Special

This specimen of Echinocorys scutata striatum is a rare and desirable example from the Kent coast. Its distinct surface ornamentation and strong preservation make it a fine representative of Santonian echinoids, suitable for collectors, researchers, and educational use.

Why Buy From Us?

  • 100% genuine fossil with Certificate of Authenticity
  • You will receive the exact specimen shown in the listing photos
  • Ethically collected from reputable geological sites in the UK
  • Ideal for collectors, educators, museums, or natural history enthusiasts

Bring home a rare and elegant piece of Britain’s fossil heritage with this Echinocorys scutata striatum fossil echinoid from the Upper Chalk of Broadstairs, Kent—a scientifically significant sea urchin from over 85 million years ago.

(Actual as seen)

Out of stock

SKU: UF3416 Category:

Description

This listing features an exceptional A-grade British Chalk fossil echinoid – Echinocorys scutata striatum, collected from the Upper Chalk Formation of the Santonian stage in the Late Cretaceous, at Broadstairs, Kent, UK. This rare and well-preserved subspecies is notable for its subtle yet diagnostic striations that distinguish it from other Echinocorys forms.

Fossil Type: Echinoid (Sea Urchin)

Species/Subspecies: Echinocorys scutata striatum

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

Geological Stage: Santonian

Formation: Upper Chalk (Chalk Group)

Location: Broadstairs, Kent, United Kingdom

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

Specimen: You will receive the exact item shown in the photos

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

Geological and Paleontological Context

Echinocorys scutata striatum is a subtly ornamented form of the well-known Echinocorys genus, characterised by faint surface striations visible under favourable lighting. This subspecies is found in Santonian chalk beds and reflects evolutionary adaptation to infaunal living in soft sedimentary marine environments.

  • Phylum: Echinodermata
  • Class: Echinoidea
  • Order: Holasteroida
  • Family: Holasteridae
  • Genus: Echinocorys
  • Subspecies: scutata striatum
  • Depositional Environment: Quiet, shallow marine carbonate platform dominated by coccolith deposition; excellent preservation conditions for echinoids
  • Morphological Features: Subglobular to slightly domed test with fine striations on the surface, well-formed ambulacral petals, and centrally located periproct and peristome; striations may assist in subspecies-level identification
  • Biozone: Occurs within established Santonian biostratigraphic intervals; often found alongside inoceramid bivalves and foraminifera used in chalk zonation
  • Notable: This subspecies is of particular interest for evolutionary and stratigraphic research in Late Cretaceous marine invertebrates

Why This Fossil Is Special

This specimen of Echinocorys scutata striatum is a rare and desirable example from the Kent coast. Its distinct surface ornamentation and strong preservation make it a fine representative of Santonian echinoids, suitable for collectors, researchers, and educational use.

Why Buy From Us?

  • 100% genuine fossil with Certificate of Authenticity
  • You will receive the exact specimen shown in the listing photos
  • Ethically collected from reputable geological sites in the UK
  • Ideal for collectors, educators, museums, or natural history enthusiasts

Bring home a rare and elegant piece of Britain’s fossil heritage with this Echinocorys scutata striatum fossil echinoid from the Upper Chalk of Broadstairs, Kent—a scientifically significant sea urchin 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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