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British Trilobite Ogyginus Partial Fossil with Stand – Llanvirn Series, Ordovician, Upper Gilwern Quarry, Wales, UK

Original price was: £9.00.Current price is: £6.30.

Step back in time with this exceptional partial fossil of a British Trilobite (Ogyginus), originating from the historic Upper Gilwern Quarry in Wales, UK. This specimen hails from the Llanvirn Series of the Ordovician period, offering a unique window into ancient marine life.

Key Features:

  • Authentic Ordovician Fossil: This partial Ogyginus trilobite fossil is a genuine relic from the Ordovician era, meticulously verified and comes complete with a Certificate of Authenticity.
  • Expertly Curated: Discovered by our dedicated team member Alison on 25th March 2024, this fossil has been expertly cleaned, prepared, and treated to highlight its intricate details and preserve its integrity.
  • Display Ready: Presented on a bespoke stand, this fossil is not only an intriguing piece of prehistoric life but also a striking display piece that will captivate attention in any setting.
  • Educational Value: Ideal for educators, collectors, or enthusiasts, this fossil offers significant educational value, providing insights into the paleobiology of trilobites and their ecological role in Ordovician marine environments.
  • Gift of Heritage: With its roots in the Welsh landscape, this trilobite fossil is a piece of the geological heritage of the UK, making it a meaningful gift for anyone fascinated by natural history or geology.

In the Box:

  • 1 x Partial Ogyginus Trilobite Fossil on Stand
  • 1 x Certificate of Authenticity
  • Detailed imagery of your specific fossil

Embrace the opportunity to own a fragment of Earth’s ancient seas with this beautifully preserved partial Ogyginus trilobite fossil. Whether for study, collection, or display, this piece brings with it the intrigue and beauty of the natural world, frozen in time for millions of years.

(Actual as seen)

Only 1 left in stock

SKU: CF1445 Category:

Description

Authentic British Trilobite (Ogyginus) Partial Fossil from Wales

This exceptional British Trilobite (Ogyginus) Partial Fossil with Stand was discovered in the Upper Gilwern Quarry, Wales, UK, and dates to the Llanvirn Series of the Middle Ordovician, approximately 465 million years ago. It represents a remarkable specimen of one of Britain’s most iconic Ordovician trilobites, preserved in fine detail and displayed on a professional stand for easy viewing and protection.

The fossil was discovered by our own field team members, Alister and Alison, on 2 April 2024, and has been carefully cleaned, prepped, and treated by Alison to bring out the intricate anatomical features of the trilobite while maintaining its natural integrity. The photo shows the exact specimen you will receive, and a 1 cm scale cube is included for accurate sizing. Every specimen comes with a Certificate of Authenticity, confirming its genuine origin and preparation.


Geological Setting and Historical Context

This specimen originates from the Llanvirn Series, a subdivision of the Middle Ordovician, representing an age of immense biological diversification within marine ecosystems. The Ordovician seas covering what is now Wales were part of the ancient Avalonia microcontinent, located near the equator and bathed in warm, nutrient-rich waters that supported an explosion of early marine life.

The Upper Gilwern Quarry exposures belong to the Bala Group, composed mainly of dark mudstones and fine-grained siltstones. These sediments were deposited in an offshore marine environment, likely below the wave base, where fine mud slowly accumulated on the seafloor. Periodic underwater sediment flows would have rapidly buried marine organisms, such as trilobites, in low-oxygen conditions ideal for fossilisation.

Fossils from this site are scientifically significant, providing insight into the biostratigraphy and palaeoecology of the Ordovician seas of Avalonia. The assemblage, including Ogyginus, is key to defining faunal zones used by geologists for correlating strata across Europe and beyond.


Taxonomy and Classification

  • Phylum: Arthropoda

  • Class: Trilobita

  • Order: Asaphida

  • Superfamily: Asaphoidea

  • Family: Asaphidae

  • Genus: Ogyginus (Murchison, 1839)

  • Geological Stage: Llanvirn Series, Middle Ordovician (~465 million years ago)

  • Locality: Upper Gilwern Quarry, Wales, UK

The genus Ogyginus was formally described by Sir Roderick Impey Murchison in 1839, one of the founding figures of modern geology and author of The Silurian System. Ogyginus is among the most recognisable and widely studied British trilobites, frequently used as an index fossil for Ordovician strata due to its distinct morphology and broad stratigraphic distribution.


Morphological Description

This partial specimen preserves the cephalon (head shield) and part of the thorax, allowing for clear identification. Ogyginus trilobites are characterised by their broad, rounded cephalon with a smooth surface and gently convex glabella. Unlike many trilobites, Ogyginus lacked compound eyes—a trait suggesting it lived in low-light or deeper marine environments. Its thoracic segments were smooth and flattened, allowing it to move efficiently across soft sea-floor muds.

The fossil shows excellent preservation of the exoskeletal surface, with fine details visible under light, including faint segmentation and subtle curvature of the shell. The natural mineralisation of the fossil matrix has created a visually appealing contrast, highlighting the form of the trilobite against its sedimentary background. The specimen is displayed on a custom stand, making it ideal for collectors, educators, or anyone interested in British palaeontology.


Depositional Environment and Palaeoecology

The Ordovician seas of Avalonia were rich ecosystems filled with trilobites, brachiopods, graptolites, and cephalopods. Ogyginus was a benthic detritivore, living on or just below the sediment surface, feeding on organic material deposited on the seafloor. Its broad, smooth exoskeleton would have allowed it to move easily through soft mud, while its lack of eyes implies a reliance on touch and chemical cues rather than sight.

The depositional environment of the Upper Gilwern mudstones was quiet and anoxic, preventing decay and scavenging after burial. This created ideal conditions for the preservation of delicate arthropod fossils, allowing scientists today to study the fine morphological details of these early marine creatures. The mudstones also record subtle sedimentary layering, reflecting variations in Ordovician sea conditions and offering clues to ancient climate and sea-level changes.


Collector and Display Value

This Ogyginus trilobite fossil from Wales is both scientifically valuable and visually captivating. Professionally prepared and mounted, it embodies the quality and historical importance of British Ordovician fossil sites. Its provenance from the Upper Gilwern Quarry, combined with its fine preservation and professional preparation, makes it a museum-quality display piece and a fascinating addition to any fossil collection.

Owning this specimen connects you to an ancient world 465 million years old—a time when trilobites like Ogyginus thrived on the seabed of what would one day become the Welsh hills.

All of our Fossils are 100% Genuine Specimens and come with a Certificate of Authenticity.
Scale cube = 1 cm – for full sizing, please refer to the photos.

Additional information

Weight 0.1 g
Dimensions 10 × 10 × 10 cm
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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