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Fossil Shark Coprolite – Turonian Stage – Cretaceous: Beachy Head, UK – Genuine Trace Fossil with Certificate

£12.60

Fossil Shark Coprolite – Turonian Stage – Cretaceous: Beachy Head, United Kingdom

Certified Authentic – Actual Fossil Shown – 100% Genuine Specimen

This listing features an authentic fossil shark coprolite from the Turonian stage of the Late Cretaceous period. The specimen was discovered at the iconic chalk cliffs of Beachy Head, East Sussex, UK – a renowned locality for mid-to-late Cretaceous marine fossils.

Coprolites (fossilised faeces) are invaluable trace fossils that provide unique insights into the diet, digestive anatomy, and ecological role of ancient animals. This particular specimen is likely from a Lamniform shark or related marine predator, which were prominent in the warm, epicontinental seas of the Cretaceous.

Scientific Classification and Geological Context:

  • Fossil Type: Coprolite (trace fossil – faeces)
  • Probable Source: Chondrichthyes – Shark (Lamniformes or similar)
  • Geological Period: Cretaceous
  • Geological Stage: Turonian (~93.9–89.8 million years ago)
  • Location: Beachy Head, East Sussex, United Kingdom
  • Depositional Environment:
  • This specimen was deposited in a tropical, shallow marine shelf environment characterised by carbonate (chalk) sedimentation. The region during the Turonian was a calm, warm sea rich in pelagic and nektonic fauna, forming a habitat for large marine predators.

Morphology & Features:

  • The coprolite shows a dense, solid texture and often exhibits a faint spiral or cylindrical form, suggestive of a spiral valve intestine—typical of sharks.
  • Mineralisation has preserved it in fine condition, with subtle surface detail and no restoration.
  • These fossils are not common in UK deposits and especially prized from well-known Cretaceous chalk sequences like Beachy Head.

Stratigraphic and Palaeontological Notes:

  • Formation: Upper Chalk Group
  • Zone & Biozone: While exact ammonite or microfossil biozonation is difficult for coprolites, this section corresponds broadly to the Inoceramus labiatus Zone of the Turonian stage.
  • Identification: Trace fossils like coprolites are not attributed to a precise species but classified by morphology.
  • Scientific Importance: Shark coprolites provide a rare glimpse into Cretaceous trophic dynamics and are often studied alongside fish teeth and vertebrate remains from the same strata.

Additional Details:

  • Scale Cube: 1cm cube visible in the photo for reference
  • Condition: Unrestored, stable and well-preserved
  • Authenticity: Comes with our Certificate of Authenticity
  • Photograph: The photo displays the actual fossil you will receive
  • Selection: This piece has been carefully chosen for its clarity and provenance

Summary:

This is a rare and scientifically valuable trace fossil—a genuine shark coprolite from the Turonian of Beachy Head. Ideal for collectors, educational settings, and anyone interested in Mesozoic marine life, this fossil offers a direct link to the behaviour and biology of ancient predatory sharks. Supplied with a Certificate of Authenticity, it’s a unique piece from one of Britain’s most celebrated fossil localities.

(Actual as seen)

Only 1 left in stock

SKU: SF0364 Category:

Description

Fossil Shark Coprolite – Turonian Stage – Cretaceous: Beachy Head, United Kingdom

Certified Authentic – Actual Fossil Shown – 100% Genuine Specimen

This listing features an authentic fossil shark coprolite from the Turonian stage of the Late Cretaceous period. The specimen was discovered at the iconic chalk cliffs of Beachy Head, East Sussex, UK – a renowned locality for mid-to-late Cretaceous marine fossils.

Coprolites (fossilised faeces) are invaluable trace fossils that provide unique insights into the diet, digestive anatomy, and ecological role of ancient animals. This particular specimen is likely from a Lamniform shark or related marine predator, which were prominent in the warm, epicontinental seas of the Cretaceous.

Scientific Classification and Geological Context:

  • Fossil Type: Coprolite (trace fossil – faeces)
  • Probable Source: Chondrichthyes – Shark (Lamniformes or similar)
  • Geological Period: Cretaceous
  • Geological Stage: Turonian (~93.9–89.8 million years ago)
  • Location: Beachy Head, East Sussex, United Kingdom
  • Depositional Environment:
  • This specimen was deposited in a tropical, shallow marine shelf environment characterised by carbonate (chalk) sedimentation. The region during the Turonian was a calm, warm sea rich in pelagic and nektonic fauna, forming a habitat for large marine predators.

Morphology & Features:

  • The coprolite shows a dense, solid texture and often exhibits a faint spiral or cylindrical form, suggestive of a spiral valve intestine—typical of sharks.
  • Mineralisation has preserved it in fine condition, with subtle surface detail and no restoration.
  • These fossils are not common in UK deposits and especially prized from well-known Cretaceous chalk sequences like Beachy Head.

Stratigraphic and Palaeontological Notes:

  • Formation: Upper Chalk Group
  • Zone & Biozone: While exact ammonite or microfossil biozonation is difficult for coprolites, this section corresponds broadly to the Inoceramus labiatus Zone of the Turonian stage.
  • Identification: Trace fossils like coprolites are not attributed to a precise species but classified by morphology.
  • Scientific Importance: Shark coprolites provide a rare glimpse into Cretaceous trophic dynamics and are often studied alongside fish teeth and vertebrate remains from the same strata.

Additional Details:

  • Scale Cube: 1cm cube visible in the photo for reference
  • Condition: Unrestored, stable and well-preserved
  • Authenticity: Comes with our Certificate of Authenticity
  • Photograph: The photo displays the actual fossil you will receive
  • Selection: This piece has been carefully chosen for its clarity and provenance

Summary:

This is a rare and scientifically valuable trace fossil—a genuine shark coprolite from the Turonian of Beachy Head. Ideal for collectors, educational settings, and anyone interested in Mesozoic marine life, this fossil offers a direct link to the behaviour and biology of ancient predatory sharks. Supplied with a Certificate of Authenticity, it’s a unique piece from one of Britain’s most celebrated fossil localities.

Additional information

Era

Cretaceous

Origin

United Kingdom

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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