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Ophiomorpha nodosa Trace Fossil Burrows, Reading Formation, Eocene - Knowl Hill Quarry, UK - Genuine with Certificate of Authenticity

Ophiomorpha nodosa Trace Fossil Burrows, Reading Formation, Eocene – Knowl Hill Quarry, UK – Genuine with Certificate of Authenticity

£9.00

Ophiomorpha nodosa Trace Fossil Burrows – Reading Formation, Eocene – Knowl Hill Quarry, UK

100% Genuine Fossil with Certificate of Authenticity

We are excited to offer this exceptional Ophiomorpha nodosa trace fossil burrow, dating from the Eocene Period (~55-34 million years ago). This specimen was discovered in the Reading Formation at Knowl Hill Quarry, UK, a region well-known for its rich Eocene fossil deposits. Ophiomorpha nodosa is a genus of trace fossil created by burrowing organisms, most likely marine crustaceans, which left behind distinctive burrow structures.

Geological and Fossil Information:

  • Fossil Type: Ophiomorpha nodosa trace fossil burrows
  • Species: Ophiomorpha nodosa
  • Morphology Features: The Ophiomorpha nodosa trace fossil burrows are characterized by their distinctive, branching tunnel-like structures. The burrows typically show irregular walls and are often associated with nodular structures, which are produced by the burrowing activity of organisms, likely crustaceans.
  • Geological Stage: Eocene (~55-34 million years ago)
  • Depositional Environment: These burrows were formed in shallow marine environments, where burrowing crustaceans would have inhabited the seabed, creating their tunnels in soft sediments.
  • Biozone: The specimen comes from the Reading Formation biozone, which is part of the Eocene and represents shallow marine deposition from that period.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: This fossil has been formally identified by paleontologists based on its morphological features and the geological context of its discovery in the Reading Formation at Knowl Hill Quarry, UK.

Size and Visuals:

The fossil measures approximately as shown in the accompanying photo. A scale rule (1cm squares) is included for accurate size reference. The photo shows the actual specimen you will receive, carefully chosen to highlight its exceptional preservation and geological significance.

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 nodosa trace fossil burrow is a fascinating and rare find from the Eocene period, making it an excellent addition to any fossil collection.

(Actual as seen)

Only 1 left in stock

SKU: UF4099 Category:

Description

Ophiomorpha nodosa Trace Fossil Burrows – Reading Formation, Eocene – Knowl Hill Quarry, UK

100% Genuine Fossil with Certificate of Authenticity

We are excited to offer this exceptional Ophiomorpha nodosa trace fossil burrow, dating from the Eocene Period (~55-34 million years ago). This specimen was discovered in the Reading Formation at Knowl Hill Quarry, UK, a region well-known for its rich Eocene fossil deposits. Ophiomorpha nodosa is a genus of trace fossil created by burrowing organisms, most likely marine crustaceans, which left behind distinctive burrow structures.

Geological and Fossil Information:

  • Fossil Type: Ophiomorpha nodosa trace fossil burrows
  • Species: Ophiomorpha nodosa
  • Morphology Features: The Ophiomorpha nodosa trace fossil burrows are characterized by their distinctive, branching tunnel-like structures. The burrows typically show irregular walls and are often associated with nodular structures, which are produced by the burrowing activity of organisms, likely crustaceans.
  • Geological Stage: Eocene (~55-34 million years ago)
  • Depositional Environment: These burrows were formed in shallow marine environments, where burrowing crustaceans would have inhabited the seabed, creating their tunnels in soft sediments.
  • Biozone: The specimen comes from the Reading Formation biozone, which is part of the Eocene and represents shallow marine deposition from that period.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: This fossil has been formally identified by paleontologists based on its morphological features and the geological context of its discovery in the Reading Formation at Knowl Hill Quarry, UK.

Size and Visuals:

The fossil measures approximately as shown in the accompanying photo. A scale rule (1cm squares) is included for accurate size reference. The photo shows the actual specimen you will receive, carefully chosen to highlight its exceptional preservation and geological significance.

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 nodosa trace fossil burrow is a fascinating and rare find from the Eocene period, making it an excellent addition to any fossil collection.

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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