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Trace Fossil Crab Faecal Pellets, Eocene – Hampshire, UK – Genuine with Certificate of Authenticity

£12.60

Trace Fossil Crab Faecal Pellets – Eocene – Hampshire, UK

100% Genuine Fossil with Certificate of Authenticity

We are delighted to offer this unique trace fossil of crab faecal pellets, found in Hampshire, UK. This fascinating specimen dates from the Eocene Epoch, approximately 56-34 million years ago, and is a rare find. These crab faecal pellets were created by ancient crustaceans and represent a unique trace fossil, offering insight into the digestive processes and behaviors of these ancient creatures. The Eocene was a time of significant marine and terrestrial life, and this fossil is an intriguing example of how organisms interacted with their environment.

Geological and Fossil Information:

  • Fossil Type: Trace Fossil Crab Faecal Pellets
  • Species: Not applicable (trace fossil genus)
  • Morphology Features: These faecal pellets are small, rounded structures that were deposited by crabs. The preserved pellets show the unique composition of the crab excrement, offering insights into the organism’s diet and environmental interactions. The pellets are fossilized within the surrounding sediments, providing valuable information on the feeding habits of ancient crustaceans.
  • Geological Stage: Eocene (~56-34 million years ago)
  • Depositional Environment: The faecal pellets were deposited in a marine environment during the Eocene. This period is known for its rich marine life, and the presence of crab excrement suggests a thriving ecosystem of crustaceans and other marine organisms.
  • Biozone: The specimen is from the Eocene biozone, a time of diverse marine life and significant evolutionary developments in marine crustaceans.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: This fossil has been formally identified based on its morphological characteristics and the geological context of its discovery in Hampshire, UK.

Size and Visuals:

The fossil measures approximately as shown in the attached 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 fascinating details of the crab faecal pellets.

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 trace fossil of crab faecal pellets from the Eocene offers a rare and unique view into the feeding behavior of ancient crustaceans, making it a valuable addition to any fossil collection.

(Actual as seen)

Only 1 left in stock

SKU: UF4114 Category:

Description

Trace Fossil Crab Faecal Pellets – Eocene – Hampshire, UK

100% Genuine Fossil with Certificate of Authenticity

We are delighted to offer this unique trace fossil of crab faecal pellets, found in Hampshire, UK. This fascinating specimen dates from the Eocene Epoch, approximately 56-34 million years ago, and is a rare find. These crab faecal pellets were created by ancient crustaceans and represent a unique trace fossil, offering insight into the digestive processes and behaviors of these ancient creatures. The Eocene was a time of significant marine and terrestrial life, and this fossil is an intriguing example of how organisms interacted with their environment.

Geological and Fossil Information:

  • Fossil Type: Trace Fossil Crab Faecal Pellets
  • Species: Not applicable (trace fossil genus)
  • Morphology Features: These faecal pellets are small, rounded structures that were deposited by crabs. The preserved pellets show the unique composition of the crab excrement, offering insights into the organism’s diet and environmental interactions. The pellets are fossilized within the surrounding sediments, providing valuable information on the feeding habits of ancient crustaceans.
  • Geological Stage: Eocene (~56-34 million years ago)
  • Depositional Environment: The faecal pellets were deposited in a marine environment during the Eocene. This period is known for its rich marine life, and the presence of crab excrement suggests a thriving ecosystem of crustaceans and other marine organisms.
  • Biozone: The specimen is from the Eocene biozone, a time of diverse marine life and significant evolutionary developments in marine crustaceans.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: This fossil has been formally identified based on its morphological characteristics and the geological context of its discovery in Hampshire, UK.

Size and Visuals:

The fossil measures approximately as shown in the attached 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 fascinating details of the crab faecal pellets.

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 trace fossil of crab faecal pellets from the Eocene offers a rare and unique view into the feeding behavior of ancient crustaceans, making it a valuable 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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