Fossils for Sale - High-quality BRITISH and WORLDWIDE Fossils. An impressive selection of fossils, including Ammonites, Trilobites, Belemnites, Fossil Fish, Fossil Shark Teeth, Fossilised Insects in Amber, Dinosaurs, and Reptiles. UK Fossils was formed in 1988 and collects and preps our own fossils in the heart of the Jurassic Coast, collecting fossils from Lyme Regis, Charmouth and Somerset. Our passion for fossils is reflected in our carefully curated collection, which includes some of the rarest and most unique specimens available.

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Ogyginus corndensis Trilobite Impression – Llanvirn, Ordovician – Gilwern Quarry, Wales – Genuine UK Fossil

£8.40

Authentic Ogyginus corndensis Trilobite Impression – Ordovician, Llanvirn Series – Upper Gilwern Quarry, Wales, UK

This listing features a well-preserved impression fossil of the trilobite species Ogyginus corndensis from the Upper Gilwern Quarry in Wales. Dating to the Llanvirn Series of the Middle Ordovician Period (approx. 460–465 million years ago), this is a striking and scientifically important example of early marine arthropod life in what was then a shallow epicontinental sea environment.

Scientific & Geological Information:

  • Species: Ogyginus corndensis
  • Family: Asaphidae
  • Superfamily: Asaphoidea
  • Order: Asaphida
  • Geological Period: Middle Ordovician
  • Series: Llanvirn Series
  • Location: Upper Gilwern Quarry, Wales, UK
  • Depositional Environment: Shallow marine shelf with low oxygen conditions, promoting fine preservation of benthic organisms
  • Fossil Zone: Typically associated with the Didymograptus murchisoni Biozone, a key graptolite zone used for correlation
  • Notable Identification: Ogyginus corndensis has been formally described in historical British palaeontology literature and is considered an index fossil for its strata.

Morphology Features:

  • Broad, smooth cephalon (head) with indistinct glabella
  • Thorax with ~8–9 wide pleurae (segments)
  • Pygidium (tail) is relatively large and semi-circular
  • This specimen is a fossil impression, meaning it shows the outline and surface texture of the trilobite as a negative mould rather than the full-bodied fossil.

Specimen Details:

  • Discovered by: Alister and Alison of our UKGE team
  • Date of Discovery: 27 March 2024
  • Cleaned & Prepped by: Alison
  • Photographs: What you see is exactly what you will receive – carefully selected for quality and visual clarity
  • Size Reference: Includes 1cm scale cube in photographs – please refer to images for accurate sizing
  • Certification: Comes with a Certificate of Authenticity – all our fossils are 100% genuine specimens, responsibly sourced and expertly prepared.

Why This Fossil?

Ogyginus corndensis is a hallmark trilobite of British Ordovician strata, prized for its completeness, clarity, and paleontological importance. This specimen offers a beautiful glimpse into prehistoric marine ecosystems and is ideal for collectors, educational use, and display.

Add a true piece of Earth’s deep history to your collection today.

(Actual as seen)

Out of stock

SKU: CS8033 Category:

Description

Authentic Ogyginus corndensis Trilobite Impression – Ordovician, Llanvirn Series – Upper Gilwern Quarry, Wales, UK

This listing features a well-preserved impression fossil of the trilobite species Ogyginus corndensis from the Upper Gilwern Quarry in Wales. Dating to the Llanvirn Series of the Middle Ordovician Period (approx. 460–465 million years ago), this is a striking and scientifically important example of early marine arthropod life in what was then a shallow epicontinental sea environment.

Scientific & Geological Information:

  • Species: Ogyginus corndensis
  • Family: Asaphidae
  • Superfamily: Asaphoidea
  • Order: Asaphida
  • Geological Period: Middle Ordovician
  • Series: Llanvirn Series
  • Location: Upper Gilwern Quarry, Wales, UK
  • Depositional Environment: Shallow marine shelf with low oxygen conditions, promoting fine preservation of benthic organisms
  • Fossil Zone: Typically associated with the Didymograptus murchisoni Biozone, a key graptolite zone used for correlation
  • Notable Identification: Ogyginus corndensis has been formally described in historical British palaeontology literature and is considered an index fossil for its strata.

Morphology Features:

  • Broad, smooth cephalon (head) with indistinct glabella
  • Thorax with ~8–9 wide pleurae (segments)
  • Pygidium (tail) is relatively large and semi-circular
  • This specimen is a fossil impression, meaning it shows the outline and surface texture of the trilobite as a negative mould rather than the full-bodied fossil.

Specimen Details:

  • Discovered by: Alister and Alison of our UKGE team
  • Date of Discovery: 27 March 2024
  • Cleaned & Prepped by: Alison
  • Photographs: What you see is exactly what you will receive – carefully selected for quality and visual clarity
  • Size Reference: Includes 1cm scale cube in photographs – please refer to images for accurate sizing
  • Certification: Comes with a Certificate of Authenticity – all our fossils are 100% genuine specimens, responsibly sourced and expertly prepared.

Why This Fossil?

Ogyginus corndensis is a hallmark trilobite of British Ordovician strata, prized for its completeness, clarity, and paleontological importance. This specimen offers a beautiful glimpse into prehistoric marine ecosystems and is ideal for collectors, educational use, and display.

Add a true piece of Earth’s deep history to your collection today.

Additional information

Era

Ordovician

Origin

United Kingdom

Ordovician Information

The Ordovician Period (485–443 million years ago) was a time of marine expansion and biodiversity growth, following the Cambrian Explosion. Warm, shallow seas covered much of the continents, supporting trilobites, brachiopods, corals, and the first true reefs. Jawless fish (early vertebrates) diversified, and the first sea scorpions (eurypterids) became dominant predators. On land, the first primitive plants (moss-like bryophytes) began colonizing damp environments. The climate was initially warm, but by the late Ordovician, a major ice age caused a drastic drop in sea levels, triggering the Ordovician-Silurian mass extinction, which wiped out nearly 85% of marine species. Despite this, the period laid the foundation for the rise of more complex ecosystems in the Silurian.

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