Fossils for Sale - High-quality BRITISH and WORLDWIDE Fossils. An impressive selection of fossils, including Ammonites, Trilobites, Belemnites, Fossil Fish, Fossil Shark Teeth, Fossilised Insects in Amber, Dinosaurs, and Reptiles. UK Fossils was formed in 1988 and collects and preps our own fossils in the heart of the Jurassic Coast, collecting fossils from Lyme Regis, Charmouth and Somerset. Our passion for fossils is reflected in our carefully curated collection, which includes some of the rarest and most unique specimens available.

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Fossil Shark Tooth Odontaspis cuspidata teretidens | Abbey Wood, London | Eocene Blackheath Beds | Genuine UK Fossil

£9.60

This listing is for a 100% genuine Fossil Shark Tooth from the extinct species Odontaspis cuspidata teretidens, collected from the renowned Blackheath Beds in Abbey Wood, London, UK. This specimen dates to the Eocene Epoch, approximately 56 to 47.8 million years ago, and represents an exceptional opportunity to own a piece of Britain’s rich paleontological heritage.

Geological Details:

  • Formation: Blackheath Beds
  • Stratigraphy: Part of the Lambeth Group, London Basin
  • Geological Period: Eocene (Ypresian Stage)
  • Depositional Environment: Nearshore marine environment; shallow warm seas with high-energy conditions suitable for elasmobranch preservation
  • Biozone: Likely within NP10-NP12 nannoplankton zones (based on regional stratigraphy)

Paleontological Significance: Odontaspis cuspidata teretidens is a species within the Order Lamniformes, Family Odontaspididae, a group commonly referred to as sand sharks or mackerel sharks. These were predatory fish with slender, curved teeth adapted for gripping slippery prey such as fish and squid. The morphology of this tooth, with its narrow crown and smooth edges, is indicative of its subspecies teretidens.

  • Order: Lamniformes
  • Superfamily: Lamnoidea
  • Family: Odontaspididae
  • Genus: Odontaspis
  • Species: cuspidata
  • Subspecies: teretidens

Morphological Features:

  • Narrow, elongated central cusp
  • Slender root structure
  • Smooth enamel surface
  • No prominent lateral cusplets (a key trait in identifying subspecies teretidens)

Notable Characteristics:

  • From a classic British Eocene fossil locality
  • Rare and scientifically significant elasmobranch specimen
  • Ideal for collectors, educators, and display

Authenticity & Provenance:

  • This is a carefully chosen piece from a well-known locality, presented with a clear photo of the exact specimen you will receive.
  • Comes with a Certificate of Authenticity.
  • Scale cube in the photo equals 1cm for precise sizing reference.

Additional Notes: This specimen is not only a beautiful example of early shark evolution but also a testament to the quality of preservation found in British Eocene marine deposits. Whether you’re an experienced fossil collector, a teacher, or an enthusiast of ancient marine life, this fossil tooth is a fantastic addition to any collection.

 

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity.

(Actual as seen)

Only 1 left in stock

SKU: SF0372 Category:

Description

This listing is for a 100% genuine Fossil Shark Tooth from the extinct species Odontaspis cuspidata teretidens, collected from the renowned Blackheath Beds in Abbey Wood, London, UK. This specimen dates to the Eocene Epoch, approximately 56 to 47.8 million years ago, and represents an exceptional opportunity to own a piece of Britain’s rich paleontological heritage.

Geological Details:

  • Formation: Blackheath Beds
  • Stratigraphy: Part of the Lambeth Group, London Basin
  • Geological Period: Eocene (Ypresian Stage)
  • Depositional Environment: Nearshore marine environment; shallow warm seas with high-energy conditions suitable for elasmobranch preservation
  • Biozone: Likely within NP10-NP12 nannoplankton zones (based on regional stratigraphy)

Paleontological Significance: Odontaspis cuspidata teretidens is a species within the Order Lamniformes, Family Odontaspididae, a group commonly referred to as sand sharks or mackerel sharks. These were predatory fish with slender, curved teeth adapted for gripping slippery prey such as fish and squid. The morphology of this tooth, with its narrow crown and smooth edges, is indicative of its subspecies teretidens.

  • Order: Lamniformes
  • Superfamily: Lamnoidea
  • Family: Odontaspididae
  • Genus: Odontaspis
  • Species: cuspidata
  • Subspecies: teretidens

Morphological Features:

  • Narrow, elongated central cusp
  • Slender root structure
  • Smooth enamel surface
  • No prominent lateral cusplets (a key trait in identifying subspecies teretidens)

Notable Characteristics:

  • From a classic British Eocene fossil locality
  • Rare and scientifically significant elasmobranch specimen
  • Ideal for collectors, educators, and display

Authenticity & Provenance:

  • This is a carefully chosen piece from a well-known locality, presented with a clear photo of the exact specimen you will receive.
  • Comes with a Certificate of Authenticity.
  • Scale cube in the photo equals 1cm for precise sizing reference.

Additional Notes: This specimen is not only a beautiful example of early shark evolution but also a testament to the quality of preservation found in British Eocene marine deposits. Whether you’re an experienced fossil collector, a teacher, or an enthusiast of ancient marine life, this fossil tooth is a fantastic addition to any collection.

 

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity.

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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