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Aetobatus irregularis fossil ray plate | lower eocene | bracklesham bay sussex uk | authentic fossil with coa | alice purnell collection
Aetobatus irregularis fossil ray plate | lower eocene | bracklesham bay sussex uk | authentic fossil with coa | alice purnell collection - Image 2

Aetobatus irregularis fossil ray plate | lower eocene | bracklesham bay sussex uk | authentic fossil with coa | alice purnell collection

Original price was: £9.00.Current price is: £7.20.

Aetobatus irregularis Fossil Ray Plate | Lower Eocene | Bracklesham Bay, Sussex, UK

Explore the ancient marine world with this Aetobatus irregularis Fossil Ray Plate, dating back to the Lower Eocene Epoch, approximately 56 to 47.8 million years ago. This remarkable specimen was unearthed from the renowned Bracklesham Bay in Sussex, UK, an area celebrated for its rich fossil beds. Part of the esteemed Alice Purnell Collection, this fossil offers a unique window into the evolutionary history of cartilaginous fish.

Geology & Fossil Information:

  • Species: Aetobatus irregularis (Eagle Ray)
  • Fossil Type: Ray Plate
  • Geological Period: Lower Eocene (Ypresian Stage, ~56 – 47.8 million years ago)
  • Location Found: Bracklesham Bay, Sussex, United Kingdom

Aetobatus irregularis, a member of the eagle ray family, was known for its flat, disc-shaped body and distinct dental plates designed for crushing hard-shelled prey like mollusks and crustaceans. This fossilized ray plate captures the intricate details of its feeding apparatus, making it a valuable addition to any fossil collection.

Key Features:

  • 100% Genuine Fossil Specimen
  • Includes a Certificate of Authenticity
  • From the renowned Alice Purnell Collection
  • Actual specimen shown – Scale rule squares/cube = 1cm (full sizing available in the photo)

This fossil is an exceptional find for collectors, educators, and paleontology enthusiasts. The accompanying photo highlights the exact specimen you will receive, ensuring complete transparency and authenticity.

Add this stunning Eocene fossil to your collection today and own a piece of prehistoric marine history!

(Actual as seen)

Only 1 left in stock

SKU: AF0909 Category:

Description

Aetobatus irregularis Fossil Ray Plate | Lower Eocene | Bracklesham Bay, Sussex, UK

Explore the ancient marine world with this Aetobatus irregularis Fossil Ray Plate, dating back to the Lower Eocene Epoch, approximately 56 to 47.8 million years ago. This remarkable specimen was unearthed from the renowned Bracklesham Bay in Sussex, UK, an area celebrated for its rich fossil beds. Part of the esteemed Alice Purnell Collection, this fossil offers a unique window into the evolutionary history of cartilaginous fish.

Geology & Fossil Information:

  • Species: Aetobatus irregularis (Eagle Ray)
  • Fossil Type: Ray Plate
  • Geological Period: Lower Eocene (Ypresian Stage, ~56 – 47.8 million years ago)
  • Location Found: Bracklesham Bay, Sussex, United Kingdom

Aetobatus irregularis, a member of the eagle ray family, was known for its flat, disc-shaped body and distinct dental plates designed for crushing hard-shelled prey like mollusks and crustaceans. This fossilized ray plate captures the intricate details of its feeding apparatus, making it a valuable addition to any fossil collection.

Key Features:

  • 100% Genuine Fossil Specimen
  • Includes a Certificate of Authenticity
  • From the renowned Alice Purnell Collection
  • Actual specimen shown – Scale rule squares/cube = 1cm (full sizing available in the photo)

This fossil is an exceptional find for collectors, educators, and paleontology enthusiasts. The accompanying photo highlights the exact specimen you will receive, ensuring complete transparency and authenticity.

Add this stunning Eocene fossil to your collection today and own a piece of prehistoric marine history!

Additional information

Era

Eocene
Origin

United Kingdom

Eocene Information

The Eocene Period (56–33.9 million years ago) was a time of warm global temperatures and the rapid evolution of mammals following the extinction of the dinosaurs. The climate was hot and humid, with lush rainforests covering much of the planet, even near the poles. Mammals diversified into new ecological roles, with early primates, whales (like Basilosaurus), large herbivores, and carnivores emerging. Birds and reptiles also thrived, and the first grasses began spreading, setting the stage for later grassland ecosystems. By the late Eocene, the Earth’s climate cooled significantly, leading to the formation of the first Antarctic ice sheets and the eventual transition to the drier, cooler Oligocene Period.

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