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Rare: Barrandia Fossil Trilobite – Lower Ordovician, Hope Shales, Shelve Formation – Minsterley, Shropshire, UK – COA

£60.00

This listing features a rare and well-preserved Barrandia trilobite fossil from the Lower Ordovician period (~466 million years ago). This specimen was discovered in the Hope Shales, Hope Member, Shelve Formation, a geologically significant deposit from Whitsburn Dingle, Minsterley, Shropshire, UK.

About Barrandia Trilobites:

Barrandia trilobites belong to the Pliomeridae family, a group of well-armoured, ancient marine arthropods. These trilobites are distinguished by their semi-elongated, convex exoskeleton, well-defined glabella, and thoracic segments. They were seafloor dwellers, likely scavengers or detritivores that lived in shallow marine environments.

Geological Information:

  • Species: Barrandia sp.
  • Fossil Type: Trilobite
  • Formation: Hope Shales, Hope Member, Shelve Formation
  • Stage: Abereiddian Stage
  • Series: Lower Llanvirn Series
  • Age: Lower Ordovician (~466 million years ago)
  • Location: Whitsburn Dingle, Minsterley, Shropshire, UK
  • Depositional Environment: Silty marine sediments of an ancient shallow sea

Fossil Features:

✔ Distinct segmentation with well-preserved exoskeleton

✔ Rare and highly sought-after British trilobite species

✔ From a well-known UK fossil locality

✔ Detailed preservation of glabella, thorax, and pygidium

✔ A great addition to any trilobite collection

Additional Information:

All fossils are 100% genuine specimens and come with a Certificate of AuthenticityScale Rule / Cube = 1cm – Please refer to the photos for accurate sizing.

This Barrandia trilobite fossil is a stunning piece of British palaeontology, perfect for museum collections, fossil enthusiasts, and educational study. A rare opportunity to own a Lower Ordovician trilobite from the famous Shelve Formation in Shropshire!

(Actual as seen)

Out of stock

SKU: AF0567 Category:

Description

This listing features a rare and well-preserved Barrandia trilobite fossil from the Lower Ordovician period (~466 million years ago). This specimen was discovered in the Hope Shales, Hope Member, Shelve Formation, a geologically significant deposit from Whitsburn Dingle, Minsterley, Shropshire, UK.

About Barrandia Trilobites:

Barrandia trilobites belong to the Pliomeridae family, a group of well-armoured, ancient marine arthropods. These trilobites are distinguished by their semi-elongated, convex exoskeleton, well-defined glabella, and thoracic segments. They were seafloor dwellers, likely scavengers or detritivores that lived in shallow marine environments.

Geological Information:

  • Species: Barrandia sp.
  • Fossil Type: Trilobite
  • Formation: Hope Shales, Hope Member, Shelve Formation
  • Stage: Abereiddian Stage
  • Series: Lower Llanvirn Series
  • Age: Lower Ordovician (~466 million years ago)
  • Location: Whitsburn Dingle, Minsterley, Shropshire, UK
  • Depositional Environment: Silty marine sediments of an ancient shallow sea

Fossil Features:

✔ Distinct segmentation with well-preserved exoskeleton

✔ Rare and highly sought-after British trilobite species

✔ From a well-known UK fossil locality

✔ Detailed preservation of glabella, thorax, and pygidium

✔ A great addition to any trilobite collection

Additional Information:

All fossils are 100% genuine specimens and come with a Certificate of AuthenticityScale Rule / Cube = 1cm – Please refer to the photos for accurate sizing.

This Barrandia trilobite fossil is a stunning piece of British palaeontology, perfect for museum collections, fossil enthusiasts, and educational study. A rare opportunity to own a Lower Ordovician trilobite from the famous Shelve Formation in Shropshire!

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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