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Thalassinoides Trace Fossil Burrows, Forest Marble, Great Oolite, Jurassic – Herbury Head, UK – Genuine with Certificate of Authenticity

£9.00

Thalassinoides Trace Fossil Burrows – Forest Marble, Great Oolite, Jurassic – Herbury Head, UK

100% Genuine Fossil with Certificate of Authenticity

We are pleased to present this remarkable Thalassinoides trace fossil burrow, discovered in the Forest Marble of the Great Oolite at Herbury Head, UK. This fossil dates from the Jurassic Period, providing an exceptional glimpse into ancient marine life. The Thalassinoides genus is known for its distinct burrowing activity, which is preserved in the form of branching tunnel-like structures that represent the behavior of ancient organisms, most likely marine crustaceans.

Geological and Fossil Information:

  • Fossil Type: Thalassinoides trace fossil burrows
  • Species: Thalassinoides (trace fossil genus)
  • Morphology Features: The Thalassinoides burrows exhibit distinctive, branching structures that are characteristic of the burrowing behavior of ancient marine organisms. The tunnel-like features are intricately preserved, showing the complex patterns formed as these creatures created their burrows.
  • Geological Stage: Jurassic (~200-145 million years ago)
  • Depositional Environment: The fossil was formed in a shallow marine environment, typical of the Great Oolite deposits. This suggests a dynamic marine ecosystem where burrowing organisms such as crustaceans thrived, leaving behind these intricate trace fossils.
  • Biozone: The specimen is part of the Forest Marble biozone, which is known for its marine deposits from the Middle 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 characteristics and the geological context of its discovery in the Forest Marble, Great Oolite, Herbury Head, UK.

Size and Visuals:

The fossil measures approximately as shown in the accompanying photo. Please refer to the scale rule (1cm squares) for accurate size reference. The photo shown is of the actual specimen you will receive, carefully chosen to highlight its exceptional preservation and the fascinating complexity of its trace features.

Authenticity and Certification:

All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity, guaranteeing the provenance and authenticity of the fossil. This Thalassinoides trace fossil burrow from the Great Oolite is an exceptional specimen and would make a valuable addition to any fossil collection or scientific study.

(Actual as seen)

Only 1 left in stock

SKU: UF4102 Category:

Description

Thalassinoides Trace Fossil Burrows – Forest Marble, Great Oolite, Jurassic – Herbury Head, UK

100% Genuine Fossil with Certificate of Authenticity

We are pleased to present this remarkable Thalassinoides trace fossil burrow, discovered in the Forest Marble of the Great Oolite at Herbury Head, UK. This fossil dates from the Jurassic Period, providing an exceptional glimpse into ancient marine life. The Thalassinoides genus is known for its distinct burrowing activity, which is preserved in the form of branching tunnel-like structures that represent the behavior of ancient organisms, most likely marine crustaceans.

Geological and Fossil Information:

  • Fossil Type: Thalassinoides trace fossil burrows
  • Species: Thalassinoides (trace fossil genus)
  • Morphology Features: The Thalassinoides burrows exhibit distinctive, branching structures that are characteristic of the burrowing behavior of ancient marine organisms. The tunnel-like features are intricately preserved, showing the complex patterns formed as these creatures created their burrows.
  • Geological Stage: Jurassic (~200-145 million years ago)
  • Depositional Environment: The fossil was formed in a shallow marine environment, typical of the Great Oolite deposits. This suggests a dynamic marine ecosystem where burrowing organisms such as crustaceans thrived, leaving behind these intricate trace fossils.
  • Biozone: The specimen is part of the Forest Marble biozone, which is known for its marine deposits from the Middle 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 characteristics and the geological context of its discovery in the Forest Marble, Great Oolite, Herbury Head, UK.

Size and Visuals:

The fossil measures approximately as shown in the accompanying photo. Please refer to the scale rule (1cm squares) for accurate size reference. The photo shown is of the actual specimen you will receive, carefully chosen to highlight its exceptional preservation and the fascinating complexity of its trace features.

Authenticity and Certification:

All of our fossils are 100% genuine specimens and come with a Certificate of Authenticity, guaranteeing the provenance and authenticity of the fossil. This Thalassinoides trace fossil burrow from the Great Oolite is an exceptional specimen and would make a valuable addition to any fossil collection or scientific study.

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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