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Rare: jaekelotodus robustus british eocene shark tooth, woolwich beds, paleocene-eocene, beltinge, kent, uk

£36.00

This listing features a genuine Jaekelotodus robustus shark tooth fossil from the Woolwich Beds, dating back to the Paleocene-Eocene transition (~56 million years ago). This well-preserved specimen was discovered in Beltinge, Kent, UK, a renowned fossil site along the British coastline known for producing exceptional early Paleogene shark fossils.

What is Jaekelotodus robustus?

Jaekelotodus robustus was an extinct species of lamniform shark, belonging to the same order as modern mako sharks and great whites. It was a fast and powerful predator that thrived in the warm seas of the early Cenozoic, preying on fish and smaller marine creatures.

These sharks are known for their large, robust teeth, characterized by:

🔹 A broad triangular cusp—ideal for slicing through prey

🔹 Well-developed lateral cusplets—helping to grasp and secure struggling fish

🔹 Fine enamel detail and sharp cutting edges—enhancing feeding efficiency

This particular specimen exhibits outstanding preservation, retaining its natural shape, fine enamel detail, and well-defined lateral cusplets.

Fossil Details:

✅ Species: Jaekelotodus robustus

✅ Fossil Type: Shark Tooth

✅ Geological Formation: Woolwich Beds

✅ Geological Age: Paleocene-Eocene (~56 million years old)

✅ Location: Beltinge, Kent, UK

✅ Collection: Alice Purnell Collection – One of the world’s largest ammonite collections

Geological Significance:

The Woolwich Beds are a well-known fossil-bearing deposit from the Paleocene-Eocene boundary, a time of significant climate shifts and marine evolution. These deposits formed in shallow coastal and estuarine environments, preserving a rich diversity of marine life, including sharks, rays, mollusks, and other invertebrates. Fossils from this formation provide valuable insights into the early adaptation and diversification of sharks following the mass extinction event that ended the Cretaceous period.

Why This Fossil is Special:

🔹 Rare British Shark Tooth – Jaekelotodus robustus teeth are much less common than those of other Eocene sharks.

🔹 Exceptional Preservation – Crisp enamel, sharp cusp, and intact lateral cusplets.

🔹 Museum-Grade Specimen – Sourced from the renowned Alice Purnell Collection.

🔹 Guaranteed Authenticity – 100% genuine fossil, accompanied by a Certificate of Authenticity.

📏 Scale Rule / Cube = 1cm – Please see photos for full sizing details.

📸 What You See Is What You Get – The specimen in the photos is the exact fossil you will receive.

This rare British Eocene shark tooth is a must-have for fossil collectors, educators, and paleontology enthusiasts, offering a fascinating glimpse into prehistoric marine ecosystems.

💎 Don’t miss this opportunity to own a unique and scientifically significant fossil!

(Actual as seen)

Out of stock

SKU: VF0097 Category:

Description

This listing features a genuine Jaekelotodus robustus shark tooth fossil from the Woolwich Beds, dating back to the Paleocene-Eocene transition (~56 million years ago). This well-preserved specimen was discovered in Beltinge, Kent, UK, a renowned fossil site along the British coastline known for producing exceptional early Paleogene shark fossils.

What is Jaekelotodus robustus?

Jaekelotodus robustus was an extinct species of lamniform shark, belonging to the same order as modern mako sharks and great whites. It was a fast and powerful predator that thrived in the warm seas of the early Cenozoic, preying on fish and smaller marine creatures.

These sharks are known for their large, robust teeth, characterized by:

🔹 A broad triangular cusp—ideal for slicing through prey

🔹 Well-developed lateral cusplets—helping to grasp and secure struggling fish

🔹 Fine enamel detail and sharp cutting edges—enhancing feeding efficiency

This particular specimen exhibits outstanding preservation, retaining its natural shape, fine enamel detail, and well-defined lateral cusplets.

Fossil Details:

✅ Species: Jaekelotodus robustus

✅ Fossil Type: Shark Tooth

✅ Geological Formation: Woolwich Beds

✅ Geological Age: Paleocene-Eocene (~56 million years old)

✅ Location: Beltinge, Kent, UK

✅ Collection: Alice Purnell Collection – One of the world’s largest ammonite collections

Geological Significance:

The Woolwich Beds are a well-known fossil-bearing deposit from the Paleocene-Eocene boundary, a time of significant climate shifts and marine evolution. These deposits formed in shallow coastal and estuarine environments, preserving a rich diversity of marine life, including sharks, rays, mollusks, and other invertebrates. Fossils from this formation provide valuable insights into the early adaptation and diversification of sharks following the mass extinction event that ended the Cretaceous period.

Why This Fossil is Special:

🔹 Rare British Shark Tooth – Jaekelotodus robustus teeth are much less common than those of other Eocene sharks.

🔹 Exceptional Preservation – Crisp enamel, sharp cusp, and intact lateral cusplets.

🔹 Museum-Grade Specimen – Sourced from the renowned Alice Purnell Collection.

🔹 Guaranteed Authenticity – 100% genuine fossil, accompanied by a Certificate of Authenticity.

📏 Scale Rule / Cube = 1cm – Please see photos for full sizing details.

📸 What You See Is What You Get – The specimen in the photos is the exact fossil you will receive.

This rare British Eocene shark tooth is a must-have for fossil collectors, educators, and paleontology enthusiasts, offering a fascinating glimpse into prehistoric marine ecosystems.

💎 Don’t miss this opportunity to own a unique and scientifically significant fossil!

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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