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Ophiomorpha Trace Fossil Burrows, Corallian Beds, Oxfordian, Jurassic - Cothill, Dry Sandford Pit, UK - Genuine with COA

Ophiomorpha Trace Fossil Burrows, Corallian Beds, Oxfordian, Jurassic – Cothill, Dry Sandford Pit, UK – Genuine with COA

£9.00

Ophiomorpha Trace Fossil Burrows – Corallian Beds, Oxfordian, Jurassic – Cothill, Dry Sandford Pit, UK

100% Genuine Fossil with Certificate of Authenticity

We are pleased to present this exceptional Ophiomorpha trace fossil burrow, discovered in the Corallian Beds of Cothill, Dry Sandford Pit, UK. This remarkable specimen dates from the Oxfordian Stage of the Jurassic Period, approximately 163 to 157 million years ago. The Ophiomorpha genus is known for its distinctive burrowing patterns, created by marine organisms, likely crustaceans, which left behind their branching burrow structures preserved in the rock.

Geological and Fossil Information:

  • Fossil Type: Ophiomorpha trace fossil burrows
  • Species: Ophiomorpha (trace fossil genus)
  • Morphology Features: The Ophiomorpha trace fossil burrows are characterized by branching, tunnel-like structures formed by burrowing organisms. These burrows are well-preserved, offering a detailed view of the irregular walls and branching tunnels, which are indicative of the organism’s burrowing behavior.
  • Geological Stage: Oxfordian, Jurassic (~163-157 million years ago)
  • Depositional Environment: The burrows were formed in shallow marine environments that were prevalent during the Oxfordian Stage. These marine organisms would have created their burrows in soft sediments that were later preserved in the Corallian Beds.
  • Biozone: The specimen comes from the Oxfordian biozone, which reflects marine life during the Late Jurassic period.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: This fossil has been professionally identified based on its morphological features and the geological context of its discovery in the Corallian Beds, Oxfordian, Dry Sandford Pit, and Cothill, UK.

Size and Visuals:

The fossil measures approximately as shown in the attached photo. A scale rule (1cm squares) is provided for accurate size reference. The photo shown is of the actual specimen you will receive, carefully chosen to highlight its exceptional preservation and distinctive features.

Authenticity and Certification:

All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity, ensuring the provenance and authenticity of the fossil. This Ophiomorpha trace fossil burrow from the Oxfordian is a rare and valuable specimen, making it an excellent addition to any fossil collection.

(Actual as seen)

Only 1 left in stock

SKU: UF4109 Category:

Description

Ophiomorpha Trace Fossil Burrows – Corallian Beds, Oxfordian, Jurassic – Cothill, Dry Sandford Pit, UK

100% Genuine Fossil with Certificate of Authenticity

We are pleased to present this exceptional Ophiomorpha trace fossil burrow, discovered in the Corallian Beds of Cothill, Dry Sandford Pit, UK. This remarkable specimen dates from the Oxfordian Stage of the Jurassic Period, approximately 163 to 157 million years ago. The Ophiomorpha genus is known for its distinctive burrowing patterns, created by marine organisms, likely crustaceans, which left behind their branching burrow structures preserved in the rock.

Geological and Fossil Information:

  • Fossil Type: Ophiomorpha trace fossil burrows
  • Species: Ophiomorpha (trace fossil genus)
  • Morphology Features: The Ophiomorpha trace fossil burrows are characterized by branching, tunnel-like structures formed by burrowing organisms. These burrows are well-preserved, offering a detailed view of the irregular walls and branching tunnels, which are indicative of the organism’s burrowing behavior.
  • Geological Stage: Oxfordian, Jurassic (~163-157 million years ago)
  • Depositional Environment: The burrows were formed in shallow marine environments that were prevalent during the Oxfordian Stage. These marine organisms would have created their burrows in soft sediments that were later preserved in the Corallian Beds.
  • Biozone: The specimen comes from the Oxfordian biozone, which reflects marine life during the Late Jurassic period.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: This fossil has been professionally identified based on its morphological features and the geological context of its discovery in the Corallian Beds, Oxfordian, Dry Sandford Pit, and Cothill, UK.

Size and Visuals:

The fossil measures approximately as shown in the attached photo. A scale rule (1cm squares) is provided for accurate size reference. The photo shown is of the actual specimen you will receive, carefully chosen to highlight its exceptional preservation and distinctive features.

Authenticity and Certification:

All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity, ensuring the provenance and authenticity of the fossil. This Ophiomorpha trace fossil burrow from the Oxfordian is a rare and valuable specimen, making it an excellent addition to any fossil collection.

Additional information

Era

Jurassic
Origin

United Kingdom

Jurassic Information

The Jurassic Period (201–145 million years ago) was the golden age of dinosaurs, with iconic species like Brachiosaurus, Stegosaurus, and Allosaurus dominating the land. It was a time of warm, humid climates, with high sea levels that created vast shallow seas, supporting abundant marine reptiles, ammonites, and early coral reefs. The first birds, such as Archaeopteryx, evolved from small theropod dinosaurs, while early mammals remained small and nocturnal. Lush forests of cycads, conifers, and ferns covered the land, providing food for giant herbivores. The breakup of the supercontinent Pangaea accelerated, shaping Earth's geography and setting the stage for the diverse ecosystems of the Cretaceous.

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