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Hamulina alpina fossil heteromorph ammonite – barremian, cretaceous – alp de provence, france

Original price was: £84.00.Current price is: £67.20.

HAMULINA ALPINA Fossil Heteromorph Ammonite – Barremian, Cretaceous – Alp de Provence, France

About the Fossil:

This exceptionally preserved Hamulina alpina heteromorph ammonite fossil originates from the Barremian stage of the Early Cretaceous period (~129-125 million years ago) and was discovered in Alp de Provence, France. Hamulina is a genus of heteromorph ammonites, recognized for their uncoiled, elongated shells with a unique curved morphology, differing from the more common tightly coiled ammonites.

During the Early Cretaceous, heteromorph ammonites like Hamulina alpina thrived in shallow marine environments, floating in ancient seas. Their distinctive shell shape suggests adaptations for neutral buoyancy and specialized swimming behavior, likely drifting along ocean currents to feed on plankton. The Barremian deposits of Alp de Provence are well known for their diverse marine fossils, including ammonites, bivalves, and gastropods, providing valuable insights into prehistoric marine ecosystems.

Geology & Formation:

  • Geological Age: Barremian, Early Cretaceous (~129-125 million years ago)
  • Formation: Marine sedimentary deposits
  • Location: Alp de Provence, France
  • Preservation: Exceptional fossilization with well-defined shell whorls, surface ornamentation, and characteristic heteromorph structure

Why This Fossil?

100% Genuine Specimen – Comes with a Certificate of Authenticity

Rare Heteromorph Ammonite – Unusual shell shape makes it highly desirable

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: AF1080 Category:

Description

HAMULINA ALPINA Fossil Heteromorph Ammonite – Barremian, Cretaceous – Alp de Provence, France

About the Fossil:

This exceptionally preserved Hamulina alpina heteromorph ammonite fossil originates from the Barremian stage of the Early Cretaceous period (~129-125 million years ago) and was discovered in Alp de Provence, France. Hamulina is a genus of heteromorph ammonites, recognized for their uncoiled, elongated shells with a unique curved morphology, differing from the more common tightly coiled ammonites.

During the Early Cretaceous, heteromorph ammonites like Hamulina alpina thrived in shallow marine environments, floating in ancient seas. Their distinctive shell shape suggests adaptations for neutral buoyancy and specialized swimming behavior, likely drifting along ocean currents to feed on plankton. The Barremian deposits of Alp de Provence are well known for their diverse marine fossils, including ammonites, bivalves, and gastropods, providing valuable insights into prehistoric marine ecosystems.

Geology & Formation:

  • Geological Age: Barremian, Early Cretaceous (~129-125 million years ago)
  • Formation: Marine sedimentary deposits
  • Location: Alp de Provence, France
  • Preservation: Exceptional fossilization with well-defined shell whorls, surface ornamentation, and characteristic heteromorph structure

Why This Fossil?

100% Genuine Specimen – Comes with a Certificate of Authenticity

Rare Heteromorph Ammonite – Unusual shell shape makes it highly desirable

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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