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RARE Wrens Nest Dudley Cornulitid Tubeworm – Cornulites serpularius, Silurian Much Wenlock Limestone Formation, Wren’s Nest, Dudley, UK

£24.00

RARE Wrens Nest Dudley Cornulitid Tubeworm – Cornulites serpularius

Formation: Much Wenlock Limestone Formation

Geological Period: Silurian (approximately 444 to 419 million years ago)

Location: Wren’s Nest, Dudley, West Midlands, UK

Certificate of Authenticity Included

Scale Rule Squares / Cube = 1cm

Full sizing details in the photo

This RARE Cornulites serpularius tubeworm fossil was sourced from the Much Wenlock Limestone Formation at Wren’s Nest in Dudley, West Midlands, UK. This site is a well-known source of Silurian fossils, particularly from the Silurian period. The Cornulites serpularius is a well-preserved cornulitid tubeworm species that once lived in ancient seas, making it a fascinating addition to any fossil collection.

Species and Morphology Information:

  • Species: Cornulites serpularius (A cornulitid tubeworm)
  • Geological Age: Silurian period, approximately 444 to 419 million years ago
  • Depositional Environment: The Much Wenlock Limestone Formation represents an ancient marine environment from the Silurian period. The Cornulites serpularius tubeworm lived in shallow seas, and its tube-like structure contributed to the reef-building organisms of the time.
  • Morphology Features: This tubeworm fossil exhibits a well-preserved calcareous tube characteristic of the Cornulites species. The tubes are often spiraled, which is a defining feature of this cornulitid tubeworm, and it offers an excellent representation of the Silurian marine life. The fossil is distinct in its texture and formation, making it an exceptional specimen for collectors.
  • Notable Features: This fossil is an important find due to its rarity, as Cornulites serpularius is not frequently found in such high quality from the Much Wenlock Limestone Formation. The tubeworm fossil adds an important piece to the understanding of ancient marine ecosystems during the Silurian period.
  • Family: Cornulitidae
  • Superfamily: Cornulitoidea
  • Order: Cornulitida
  • Biozone: This fossil is from the Silurian biozone, a region noted for its diversity of marine life, including corals, brachiopods, and trilobites.
  • Depositional Environment: The Much Wenlock Limestone Formation was formed during a period of warm shallow seas, providing the ideal conditions for marine organisms like cornulitid tubeworms to thrive. The tube-like structure of these organisms can still be clearly seen in the fossil, which offers a glimpse into the marine ecosystems of the time.

Size and Visuals:

The tubeworm fossil measures approximately X inches/cm (as shown in the photos). The scale rule cube in the image represents 1cm, allowing you to assess the size and proportions of the fossil.

Authenticity and Certification:

This Cornulites serpularius tubeworm fossil is 100% genuine and comes with a Certificate of Authenticity. The certificate confirms that the specimen was sourced from the Much Wenlock Limestone Formation at Wren’s Nest, Dudley, West Midlands, UK, and dates back to the Silurian period.

Why Buy This Fossil:

  • Authentic and Genuine: Comes with a Certificate of Authenticity confirming its UK origin and Silurian age.
  • Perfect for Collectors: A rare fossil from a renowned Silurian formation, ideal for anyone interested in Silurian marine life and ancient reef systems.
  • Educational Value: Offers an excellent opportunity to study cornulitid tubeworms and marine ecosystems from the Silurian period.
  • Unique Display Piece: The tubular structure and spiral formation of this fossil make it a striking and fascinating addition to any fossil collection or natural history display.

Note: The photo shown is of the actual specimen you will receive. The scale cube in the image represents 1cm, and full-size details are provided through the photos.

(Actual as seen)

Out of stock

SKU: SF0834 Category:

Description

RARE Wrens Nest Dudley Cornulitid Tubeworm – Cornulites serpularius

Formation: Much Wenlock Limestone Formation

Geological Period: Silurian (approximately 444 to 419 million years ago)

Location: Wren’s Nest, Dudley, West Midlands, UK

Certificate of Authenticity Included

Scale Rule Squares / Cube = 1cm

Full sizing details in the photo

This RARE Cornulites serpularius tubeworm fossil was sourced from the Much Wenlock Limestone Formation at Wren’s Nest in Dudley, West Midlands, UK. This site is a well-known source of Silurian fossils, particularly from the Silurian period. The Cornulites serpularius is a well-preserved cornulitid tubeworm species that once lived in ancient seas, making it a fascinating addition to any fossil collection.

Species and Morphology Information:

  • Species: Cornulites serpularius (A cornulitid tubeworm)
  • Geological Age: Silurian period, approximately 444 to 419 million years ago
  • Depositional Environment: The Much Wenlock Limestone Formation represents an ancient marine environment from the Silurian period. The Cornulites serpularius tubeworm lived in shallow seas, and its tube-like structure contributed to the reef-building organisms of the time.
  • Morphology Features: This tubeworm fossil exhibits a well-preserved calcareous tube characteristic of the Cornulites species. The tubes are often spiraled, which is a defining feature of this cornulitid tubeworm, and it offers an excellent representation of the Silurian marine life. The fossil is distinct in its texture and formation, making it an exceptional specimen for collectors.
  • Notable Features: This fossil is an important find due to its rarity, as Cornulites serpularius is not frequently found in such high quality from the Much Wenlock Limestone Formation. The tubeworm fossil adds an important piece to the understanding of ancient marine ecosystems during the Silurian period.
  • Family: Cornulitidae
  • Superfamily: Cornulitoidea
  • Order: Cornulitida
  • Biozone: This fossil is from the Silurian biozone, a region noted for its diversity of marine life, including corals, brachiopods, and trilobites.
  • Depositional Environment: The Much Wenlock Limestone Formation was formed during a period of warm shallow seas, providing the ideal conditions for marine organisms like cornulitid tubeworms to thrive. The tube-like structure of these organisms can still be clearly seen in the fossil, which offers a glimpse into the marine ecosystems of the time.

Size and Visuals:

The tubeworm fossil measures approximately X inches/cm (as shown in the photos). The scale rule cube in the image represents 1cm, allowing you to assess the size and proportions of the fossil.

Authenticity and Certification:

This Cornulites serpularius tubeworm fossil is 100% genuine and comes with a Certificate of Authenticity. The certificate confirms that the specimen was sourced from the Much Wenlock Limestone Formation at Wren’s Nest, Dudley, West Midlands, UK, and dates back to the Silurian period.

Why Buy This Fossil:

  • Authentic and Genuine: Comes with a Certificate of Authenticity confirming its UK origin and Silurian age.
  • Perfect for Collectors: A rare fossil from a renowned Silurian formation, ideal for anyone interested in Silurian marine life and ancient reef systems.
  • Educational Value: Offers an excellent opportunity to study cornulitid tubeworms and marine ecosystems from the Silurian period.
  • Unique Display Piece: The tubular structure and spiral formation of this fossil make it a striking and fascinating addition to any fossil collection or natural history display.

Note: The photo shown is of the actual specimen you will receive. The scale cube in the image represents 1cm, and full-size details are provided through the photos.

Additional information

Era

Silurian

Origin

United Kingdom

Silurian Information

The Silurian Period (443–419 million years ago) was a time of climate stabilization following the end-Ordovician mass extinction. The climate became warmer, and sea levels rose, leading to the expansion of shallow marine ecosystems. Coral reefs flourished, and new marine predators like Eurypterids (sea scorpions) and early jawed fish emerged. One of the most significant events was the colonization of land—early vascular plants such as Cooksonia appeared, along with the first arthropods to venture onto land. These evolutionary advances set the stage for the more complex terrestrial ecosystems that developed in the Devonian.

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