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RARE Crioceratites nolani Heteromorph Ammonite Fossil | Cretaceous Hauterivian | Drome France | Authentic Specimen

Original price was: £540.00.Current price is: £432.00.

A RARE Crioceratites nolani fossil—an exceptional example of a heteromorph ammonite from the Upper Hauterivian Stage of the Lower Cretaceous, originating from the well-documented fossil-bearing strata of Drôme, France.

This genus, known for its open-coiled and ornamental shell structure, offers a remarkable insight into ammonite diversity and adaptation during the Early Cretaceous. The spiral architecture and preserved ornamentation of this specimen make it a highly desirable addition for collectors, educators, and palaeontology enthusiasts alike.

Specimen Information:

  • Species: Crioceratites nolani
  • Geological Formation: Drôme localities (likely part of the Vocontian Basin sequences)
  • Geological Age: Cretaceous – Upper Hauterivian Stage (~131 to 129 million years ago)
  • Stratigraphic Zone: Possibly associated with the Crioceratites nolani or Balearites balearis ammonite zones (regionally known biozones in Drôme)
  • Location: Drôme, southeastern France
  • Depositional Environment: Open marine, moderately deep shelf setting with rich nektonic fauna
  • Discovery & Preparation: Carefully chosen fossil, with actual specimen pictured
  • Scale: Each square or cube in scale = 1cm (see photos for precise sizing)
  • Authenticity: Supplied with a Certificate of Authenticity
  • Notable Features: Rare coiling structure, defined ribbing and potential tubercles

Scientific Classification:

  • Kingdom: Animalia
  • Phylum: Mollusca
  • Class: Cephalopoda
  • Order: Ammonitida
  • Superfamily: Ancyloceratoidea
  • Family: Crioceratitidae
  • Genus: Crioceratites
  • Species: C. nolani
  • Identified by: Described and named by A. Thomel (1964), as part of detailed studies on French Lower Cretaceous ammonite faunas

Morphology & Notable Features:

  • Heteromorph structure: Uncoiled, open-planispiral shell — unlike typical tightly coiled ammonites
  • Pronounced ornamentation: Strong ribbing with occasional nodes or tubercles
  • Functional adaptation: Likely had a unique mode of swimming or floating in the water column due to irregular shape
  • Visual impact: The aesthetic spiral geometry makes this a visually striking fossil for any display

Palaeoenvironmental Context:

This ammonite thrived in the Vocontian Basin, a Cretaceous marine basin in what is now southeastern France. The basin accumulated fine-grained sediments that provided excellent fossil preservation. This region is globally recognised for yielding key biostratigraphic ammonite assemblages used in dating the Early Cretaceous.

The Hauterivian Stage marks a time of diversification in ammonites following the Valanginian-Hauterivian boundary extinction event. Heteromorphs like Crioceratites emerged and rapidly diversified in marine environments with complex ecologies.

Why Add This Specimen to Your Collection?

  • Rare and visually unique heteromorph ammonite
  • Scientifically important: C. nolani is a recognised biostratigraphic marker in parts of Europe
  • From a classic Cretaceous fossil site in France
  • Perfect for advanced collectors, students, or academic display
  • Comes with Certificate of Authenticity
  • Photographed specimen is the exact one you’ll receive

Summary:

  • Genuine Crioceratites nolani fossil
  • From the Upper Hauterivian, Lower Cretaceous of Drôme, France
  • Rare heteromorph ammonite with open-coiled structure
  • Exceptional preservation and scientific significance
  • Professionally prepped and documented
  • Includes Certificate of Authenticity
  • Scale rule or cube = 1cm – see listing photo for full dimensions

 

(Actual as seen)

Includes a fully hand-signed Premium Certificate of Authenticity.

Only 1 left in stock

SKU: UF3888 Categories: ,

Description

A RARE Crioceratites nolani fossil—an exceptional example of a heteromorph ammonite from the Upper Hauterivian Stage of the Lower Cretaceous, originating from the well-documented fossil-bearing strata of Drôme, France.

This genus, known for its open-coiled and ornamental shell structure, offers a remarkable insight into ammonite diversity and adaptation during the Early Cretaceous. The spiral architecture and preserved ornamentation of this specimen make it a highly desirable addition for collectors, educators, and palaeontology enthusiasts alike.

Specimen Information:

  • Species: Crioceratites nolani
  • Geological Formation: Drôme localities (likely part of the Vocontian Basin sequences)
  • Geological Age: Cretaceous – Upper Hauterivian Stage (~131 to 129 million years ago)
  • Stratigraphic Zone: Possibly associated with the Crioceratites nolani or Balearites balearis ammonite zones (regionally known biozones in Drôme)
  • Location: Drôme, southeastern France
  • Depositional Environment: Open marine, moderately deep shelf setting with rich nektonic fauna
  • Discovery & Preparation: Carefully chosen fossil, with actual specimen pictured
  • Scale: Each square or cube in scale = 1cm (see photos for precise sizing)
  • Authenticity: Supplied with a Certificate of Authenticity
  • Notable Features: Rare coiling structure, defined ribbing and potential tubercles

Scientific Classification:

  • Kingdom: Animalia
  • Phylum: Mollusca
  • Class: Cephalopoda
  • Order: Ammonitida
  • Superfamily: Ancyloceratoidea
  • Family: Crioceratitidae
  • Genus: Crioceratites
  • Species: C. nolani
  • Identified by: Described and named by A. Thomel (1964), as part of detailed studies on French Lower Cretaceous ammonite faunas

Morphology & Notable Features:

  • Heteromorph structure: Uncoiled, open-planispiral shell — unlike typical tightly coiled ammonites
  • Pronounced ornamentation: Strong ribbing with occasional nodes or tubercles
  • Functional adaptation: Likely had a unique mode of swimming or floating in the water column due to irregular shape
  • Visual impact: The aesthetic spiral geometry makes this a visually striking fossil for any display

Palaeoenvironmental Context:

This ammonite thrived in the Vocontian Basin, a Cretaceous marine basin in what is now southeastern France. The basin accumulated fine-grained sediments that provided excellent fossil preservation. This region is globally recognised for yielding key biostratigraphic ammonite assemblages used in dating the Early Cretaceous.

The Hauterivian Stage marks a time of diversification in ammonites following the Valanginian-Hauterivian boundary extinction event. Heteromorphs like Crioceratites emerged and rapidly diversified in marine environments with complex ecologies.

Why Add This Specimen to Your Collection?

  • Rare and visually unique heteromorph ammonite
  • Scientifically important: C. nolani is a recognised biostratigraphic marker in parts of Europe
  • From a classic Cretaceous fossil site in France
  • Perfect for advanced collectors, students, or academic display
  • Comes with Certificate of Authenticity
  • Photographed specimen is the exact one you’ll receive

Summary:

  • Genuine Crioceratites nolani fossil
  • From the Upper Hauterivian, Lower Cretaceous of Drôme, France
  • Rare heteromorph ammonite with open-coiled structure
  • Exceptional preservation and scientific significance
  • Professionally prepped and documented
  • Includes Certificate of Authenticity
  • Scale rule or cube = 1cm – see listing photo for full dimensions

 

Additional information

Era

Cretaceous

Origin

France

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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