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Crioceras majoriensis fossil heteromorph ammonite – lower barremian, cretaceous – alps, france

Original price was: £180.00.Current price is: £144.00.

CRIOCERAS MAJORIENSIS Fossil Heteromorph Ammonite – Lower Barremian, Cretaceous – Alps, France

About the Fossil:

This well-preserved Crioceras majoriensis heteromorph ammonite fossil originates from the Lower Barremian stage of the Early Cretaceous period (~129-125 million years ago) and was discovered in the Alps, France. Crioceras is a genus of heteromorph ammonites, characterized by their loosely coiled, uncoiled, or irregular shell morphologies, distinguishing them from the more common spiral ammonites.

During the Early Cretaceous, ammonites like Crioceras majoriensis thrived in shallow marine environments, where they played an essential role in marine food chains. Their distinctive ribbed and ornamented shells indicate they had adaptations for buoyancy and movement, allowing them to navigate ancient seas differently from standard ammonites. The Lower Barremian deposits of the French Alps are world-famous for their diverse ammonite faunas, making this specimen a valuable addition to any collection.

Geology & Formation:

  • Geological Age: Lower Barremian, Early Cretaceous (~129-125 million years ago)
  • Formation: Marine sedimentary deposits
  • Location: Alps, France
  • Preservation: Excellent fossilization with clearly defined shell ribs, whorls, and morphological features

Why This Fossil?

100% Genuine Specimen – Comes with a Certificate of Authenticity

Rare Heteromorph Ammonite – Unique uncoiled shell structure makes it highly collectible

Highly Collectible – From the renowned Alice Purnell Collection

Perfect for Display or Study – Ideal for fossil collectors, students, and paleontology enthusiasts

Scale Rule/Cube = 1cm – See photos for full sizing

The fossil in the photo is the exact specimen you will receive!

📦 Secure Packaging & Fast Shipping – Your fossil will be carefully packed for a safe journey!

(Actual as seen)

Only 1 left in stock

SKU: AF1079 Category:

Description

CRIOCERAS MAJORIENSIS Fossil Heteromorph Ammonite – Lower Barremian, Cretaceous – Alps, France

About the Fossil:

This well-preserved Crioceras majoriensis heteromorph ammonite fossil originates from the Lower Barremian stage of the Early Cretaceous period (~129-125 million years ago) and was discovered in the Alps, France. Crioceras is a genus of heteromorph ammonites, characterized by their loosely coiled, uncoiled, or irregular shell morphologies, distinguishing them from the more common spiral ammonites.

During the Early Cretaceous, ammonites like Crioceras majoriensis thrived in shallow marine environments, where they played an essential role in marine food chains. Their distinctive ribbed and ornamented shells indicate they had adaptations for buoyancy and movement, allowing them to navigate ancient seas differently from standard ammonites. The Lower Barremian deposits of the French Alps are world-famous for their diverse ammonite faunas, making this specimen a valuable addition to any collection.

Geology & Formation:

  • Geological Age: Lower Barremian, Early Cretaceous (~129-125 million years ago)
  • Formation: Marine sedimentary deposits
  • Location: Alps, France
  • Preservation: Excellent fossilization with clearly defined shell ribs, whorls, and morphological features

Why This Fossil?

100% Genuine Specimen – Comes with a Certificate of Authenticity

Rare Heteromorph Ammonite – Unique uncoiled shell structure makes it highly collectible

Highly Collectible – From the renowned Alice Purnell Collection

Perfect for Display or Study – Ideal for fossil collectors, students, and paleontology enthusiasts

Scale Rule/Cube = 1cm – See photos for full sizing

The fossil in the photo is the exact specimen you will receive!

📦 Secure Packaging & Fast Shipping – Your fossil will be carefully packed for a safe journey!

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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