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Rare paracrioceras occulatum fossil ammonite fragment – barremian, cretaceous, bouches-du-rhône, france – genuine specimen with coa

£18.00

This is a rare Paracrioceras occulatum fossil ammonite fragment, dating to the Barremian stage of the Early Cretaceous (~129-125 million years ago), discovered in Bouches-du-Rhône, France. Paracrioceras is a heteromorph ammonite, meaning it had an irregular, uncoiled shell, differing from the typical tightly coiled ammonites. These ammonites likely had unique buoyancy and swimming adaptations, allowing them to drift in the Cretaceous seas.

Fossils from the Barremian stage are highly sought after, as this was a period of significant ammonite diversification. The presence of Paracrioceras occulatum provides valuable insight into the evolution of heteromorph ammonites during the Early Cretaceous.

Though this is a fragment, it still preserves intricate details of the ammonite’s structure, including well-defined growth lines and ribbing, making it a great specimen for collectors and researchers.

Geological Information:

  • Formation: Cretaceous Marine Deposits
  • Stage: Barremian, Early Cretaceous (~129-125 million years old)
  • Location: Bouches-du-Rhône, France
  • Depositional Environment: Marine seafloor with fine-grained sedimentation

Fossil Characteristics:

  • Heteromorph ammonite with preserved ribbing and growth lines
  • Distinct features despite being a fragment
  • Rare Early Cretaceous ammonite from France
  • Valuable for collectors, researchers, and fossil enthusiasts

Key Features:

  • Authentic Paracrioceras occulatum fossil ammonite fragment
  • Rare specimen from the Barremian stage
  • From the Alice Purnell Collection
  • 100% genuine specimen with Certificate of Authenticity

Scale Rule / Cube = 1cm – Please refer to the photos for accurate sizing.

All fossils are securely packaged for worldwide shipping.

(Actual as seen)

Out of stock

SKU: AF0562 Category:

Description

This is a rare Paracrioceras occulatum fossil ammonite fragment, dating to the Barremian stage of the Early Cretaceous (~129-125 million years ago), discovered in Bouches-du-Rhône, France. Paracrioceras is a heteromorph ammonite, meaning it had an irregular, uncoiled shell, differing from the typical tightly coiled ammonites. These ammonites likely had unique buoyancy and swimming adaptations, allowing them to drift in the Cretaceous seas.

Fossils from the Barremian stage are highly sought after, as this was a period of significant ammonite diversification. The presence of Paracrioceras occulatum provides valuable insight into the evolution of heteromorph ammonites during the Early Cretaceous.

Though this is a fragment, it still preserves intricate details of the ammonite’s structure, including well-defined growth lines and ribbing, making it a great specimen for collectors and researchers.

Geological Information:

  • Formation: Cretaceous Marine Deposits
  • Stage: Barremian, Early Cretaceous (~129-125 million years old)
  • Location: Bouches-du-Rhône, France
  • Depositional Environment: Marine seafloor with fine-grained sedimentation

Fossil Characteristics:

  • Heteromorph ammonite with preserved ribbing and growth lines
  • Distinct features despite being a fragment
  • Rare Early Cretaceous ammonite from France
  • Valuable for collectors, researchers, and fossil enthusiasts

Key Features:

  • Authentic Paracrioceras occulatum fossil ammonite fragment
  • Rare specimen from the Barremian stage
  • From the Alice Purnell Collection
  • 100% genuine specimen with Certificate of Authenticity

Scale Rule / Cube = 1cm – Please refer to the photos for accurate sizing.

All fossils are securely packaged for worldwide shipping.

Additional information

Weight 0.1 g
Dimensions 10 × 10 × 10 cm
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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