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Chondrites on Thalassinoides Trace Fossil Burrows, Upper Chalk, Cretaceous – Sulham Old Chalk Pit, Sulham Wood, UK – Genuine with COA

£14.40

Chondrites on Thalassinoides Trace Fossil Burrows – Upper Chalk, Cretaceous – Sulham Old Chalk Pit, Sulham Wood, UK

100% Genuine Fossil with Certificate of Authenticity

We are excited to offer this exceptional Chondrites on Thalassinoides trace fossil burrow specimen, discovered in the Sulham Old Chalk Pit in Sulham Wood, UK. This fascinating specimen was formed during the Upper Chalk stage of the Cretaceous Period, approximately 70-100 million years ago. It represents a unique combination of two different types of trace fossils: Chondrites, which are associated with burrowing activity, and Thalassinoides, another burrowing organism. Together, these trace fossils offer an insight into ancient marine environments and the behavior of their inhabitants.

Geological and Fossil Information:

  • Fossil Type: Chondrites on Thalassinoides trace fossil burrows
  • Species: Chondrites (trace fossil genus), Thalassinoides (trace fossil genus)
  • Morphology Features: The Chondrites trace fossils are linear burrows that exhibit a unique branching structure. The Thalassinoides burrows are larger, branching tunnels, which were likely created by ancient burrowing organisms like crustaceans. The combination of these two species is rare and offers a valuable glimpse into the complex sedimentary processes of the Cretaceous period.
  • Geological Stage: Upper Chalk, Cretaceous (~70-100 million years ago)
  • Depositional Environment: This specimen was formed in a marine environment, typical of the Upper Chalk seas during the Cretaceous period. The presence of both Chondrites and Thalassinoides suggests a dynamic and active marine ecosystem with significant burrowing activity.
  • Biozone: The specimen is part of the Upper Chalk biozone, which is known for its deep marine conditions and the abundance of burrowing organisms.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: The fossil has been professionally identified by paleontologists based on its distinct morphology and the geological context of its discovery in the Sulham Old Chalk Pit, Sulham Wood, 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 shown is of the actual specimen you will receive, carefully chosen to highlight its remarkable 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 Chondrites on Thalassinoides trace fossil burrow specimen is a rare find from the Upper Chalk, providing a fascinating example of Cretaceous marine life and burrowing activity.

(Actual as seen)

Out of stock

SKU: UF4096 Category:

Description

Chondrites on Thalassinoides Trace Fossil Burrows – Upper Chalk, Cretaceous – Sulham Old Chalk Pit, Sulham Wood, UK

100% Genuine Fossil with Certificate of Authenticity

We are excited to offer this exceptional Chondrites on Thalassinoides trace fossil burrow specimen, discovered in the Sulham Old Chalk Pit in Sulham Wood, UK. This fascinating specimen was formed during the Upper Chalk stage of the Cretaceous Period, approximately 70-100 million years ago. It represents a unique combination of two different types of trace fossils: Chondrites, which are associated with burrowing activity, and Thalassinoides, another burrowing organism. Together, these trace fossils offer an insight into ancient marine environments and the behavior of their inhabitants.

Geological and Fossil Information:

  • Fossil Type: Chondrites on Thalassinoides trace fossil burrows
  • Species: Chondrites (trace fossil genus), Thalassinoides (trace fossil genus)
  • Morphology Features: The Chondrites trace fossils are linear burrows that exhibit a unique branching structure. The Thalassinoides burrows are larger, branching tunnels, which were likely created by ancient burrowing organisms like crustaceans. The combination of these two species is rare and offers a valuable glimpse into the complex sedimentary processes of the Cretaceous period.
  • Geological Stage: Upper Chalk, Cretaceous (~70-100 million years ago)
  • Depositional Environment: This specimen was formed in a marine environment, typical of the Upper Chalk seas during the Cretaceous period. The presence of both Chondrites and Thalassinoides suggests a dynamic and active marine ecosystem with significant burrowing activity.
  • Biozone: The specimen is part of the Upper Chalk biozone, which is known for its deep marine conditions and the abundance of burrowing organisms.
  • Family: Not applicable (trace fossils)
  • Super Family: Not applicable (trace fossils)
  • Order: Trace Fossils (Ichnology)
  • Formally Identified By: The fossil has been professionally identified by paleontologists based on its distinct morphology and the geological context of its discovery in the Sulham Old Chalk Pit, Sulham Wood, 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 shown is of the actual specimen you will receive, carefully chosen to highlight its remarkable 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 Chondrites on Thalassinoides trace fossil burrow specimen is a rare find from the Upper Chalk, providing a fascinating example of Cretaceous marine life and burrowing activity.

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