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RARE Conulus subrotundus Fossil Sea Urchin in Flint – Cretaceous Chalk – Glyde Quarry, Sussex, England | COA

Original price was: £36.00.Current price is: £32.40.

This listing features a RARE Fossil Chalk Echinoid – Conulus subrotundus preserved in flint, collected from the famous Cretaceous chalk deposits of Glyde Quarry, Sussex, England. A highly sought-after fossil, this specimen showcases the exceptional preservation and geological story of the English chalk seas.

This is a 100% genuine fossil, professionally curated and backed by a Certificate of Authenticity. The actual fossil shown is the one you will receive. Please refer to the photo with the 1cm scale cube for full sizing.

 

Fossil Overview:

  • Species: Conulus subrotundus (Lamarck, 1816)
  • Common Name: Chalk Sea Urchin / Fossil Echinoid
  • Geological Period: Late Cretaceous
  • Stage: Likely Middle to Upper Cenomanian (~100–94 million years ago)
  • Formation: Upper Chalk (likely part of the Seaford or New Pit Chalk Formation)
  • Location: Glyde Quarry, Sussex, England, UK
  • Preservation Type: Silicified fossil in flint nodule

 

Geological & Depositional Environment:

Glyde Quarry is part of the famous South Downs chalk landscape, formed in the Late Cretaceous within a warm, shallow epicontinental sea that once covered much of Europe. The chalk is composed mainly of microscopic calcareous algae (coccoliths), forming a fine, pure limestone ideal for fossil preservation.

Over millions of years, silica-rich fluids percolated through these chalk beds, replacing calcium carbonate in fossils like echinoids and forming flint nodules. As a result, this specimen is beautifully preserved in durable flint, often revealing sharper external features than those in chalk matrix.

 

Taxonomy & Classification:

  • Phylum: Echinodermata
  • Class: Echinoidea
  • Order: Echinoneoida
  • Superfamily: Conulidea
  • Family: Conulidae
  • Genus: Conulus
  • Species: Conulus subrotundus (formally described by Jean-Baptiste Lamarck in 1816)

 

Morphological Features:

Conulus subrotundus is identified by:

  • A symmetrical, sub-rounded, slightly heart-shaped test
  • Smooth surface with minimal ornamentation
  • Broad, domed upper side and a gently concave base
  • Shallow, faintly petaloid ambulacra
  • Anteriorly positioned mouth (peristome) and posterior anal opening (periproct)

Its body shape suggests a semi-infaunal lifestyle, partially buried in soft seabed sediments while feeding on organic particles.

 

Notable Features:

  • Rare flint preservation from a key locality in the English chalk
  • Fossil originally described by renowned naturalist Jean-Baptiste Lamarck in 1816
  • Excellent condition and clarity due to silicification
  • Ideal for collectors, educational display, or scientific reference

 

Why Buy From Us?

  • All fossils are 100% genuine, ethically sourced
  • Includes a Certificate of Authenticity
  • The exact fossil shown is what you’ll receive
  • Secure packaging and fast, tracked dispatch

This Conulus subrotundus fossil in flint from Glyde Quarry is a beautiful and scientifically important piece from the Cretaceous chalk seas of Sussex. A rare opportunity to own a genuine sea urchin fossil with exceptional preservation and provenance.

(Actual as seen)

Only 1 left in stock

SKU: UF4639 Category:

Description

This listing features a RARE Fossil Chalk Echinoid – Conulus subrotundus preserved in flint, collected from the famous Cretaceous chalk deposits of Glyde Quarry, Sussex, England. A highly sought-after fossil, this specimen showcases the exceptional preservation and geological story of the English chalk seas.

This is a 100% genuine fossil, professionally curated and backed by a Certificate of Authenticity. The actual fossil shown is the one you will receive. Please refer to the photo with the 1cm scale cube for full sizing.

 

Fossil Overview:

  • Species: Conulus subrotundus (Lamarck, 1816)
  • Common Name: Chalk Sea Urchin / Fossil Echinoid
  • Geological Period: Late Cretaceous
  • Stage: Likely Middle to Upper Cenomanian (~100–94 million years ago)
  • Formation: Upper Chalk (likely part of the Seaford or New Pit Chalk Formation)
  • Location: Glyde Quarry, Sussex, England, UK
  • Preservation Type: Silicified fossil in flint nodule

 

Geological & Depositional Environment:

Glyde Quarry is part of the famous South Downs chalk landscape, formed in the Late Cretaceous within a warm, shallow epicontinental sea that once covered much of Europe. The chalk is composed mainly of microscopic calcareous algae (coccoliths), forming a fine, pure limestone ideal for fossil preservation.

Over millions of years, silica-rich fluids percolated through these chalk beds, replacing calcium carbonate in fossils like echinoids and forming flint nodules. As a result, this specimen is beautifully preserved in durable flint, often revealing sharper external features than those in chalk matrix.

 

Taxonomy & Classification:

  • Phylum: Echinodermata
  • Class: Echinoidea
  • Order: Echinoneoida
  • Superfamily: Conulidea
  • Family: Conulidae
  • Genus: Conulus
  • Species: Conulus subrotundus (formally described by Jean-Baptiste Lamarck in 1816)

 

Morphological Features:

Conulus subrotundus is identified by:

  • A symmetrical, sub-rounded, slightly heart-shaped test
  • Smooth surface with minimal ornamentation
  • Broad, domed upper side and a gently concave base
  • Shallow, faintly petaloid ambulacra
  • Anteriorly positioned mouth (peristome) and posterior anal opening (periproct)

Its body shape suggests a semi-infaunal lifestyle, partially buried in soft seabed sediments while feeding on organic particles.

 

Notable Features:

  • Rare flint preservation from a key locality in the English chalk
  • Fossil originally described by renowned naturalist Jean-Baptiste Lamarck in 1816
  • Excellent condition and clarity due to silicification
  • Ideal for collectors, educational display, or scientific reference

 

Why Buy From Us?

  • All fossils are 100% genuine, ethically sourced
  • Includes a Certificate of Authenticity
  • The exact fossil shown is what you’ll receive
  • Secure packaging and fast, tracked dispatch

This Conulus subrotundus fossil in flint from Glyde Quarry is a beautiful and scientifically important piece from the Cretaceous chalk seas of Sussex. A rare opportunity to own a genuine sea urchin fossil with exceptional preservation and provenance.

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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