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.





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