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Rare Harpes Trilobite Fossil Ordovician Fezouata Formation Morocco – Exceptional Paleozoic Arthropod Specimen with Hand Signed Certificate

£300.00

Rare Harpes Trilobite Fossil from the Fezouata Formation of Morocco

This genuine Harpes trilobite fossil originates from the renowned Fezouata Formation of Morocco, a world-famous Lower Ordovician fossil deposit dating to approximately 485–470 million years ago. Specimens from this locality represent some of the most scientifically important early Paleozoic fossils known, preserving marine life from a time when complex ecosystems were rapidly diversifying following the Cambrian Explosion.

The Fezouata Formation is globally recognised for its exceptional fossil preservation and is considered one of the most important Ordovician fossil Lagerstätten. Trilobites discovered here often display remarkable morphological detail, offering valuable insight into early arthropod evolution.

The fossil displayed in the photographs is the exact specimen you will receive, carefully selected for its preservation and authenticity. This specimen includes a fully hand-signed Premium Certificate of Authenticity, confirming the fossil is genuine.

Please refer to the photographs for full specimen sizing and scale.

About Harpes Trilobites – Distinctive Ordovician Arthropods

Trilobites were among the most successful marine arthropods of the Paleozoic Era, inhabiting Earth’s oceans for nearly 270 million years. The genus Harpes is particularly distinctive due to its unusual body morphology and expanded cephalic shield.

Taxonomic classification:

  • Kingdom: Animalia
  • Phylum: Arthropoda
  • Class: Trilobita
  • Order: Harpetida
  • Family: Harpetidae
  • Genus: Harpes

Members of the Harpetidae family are known for their broad, semicircular head shields, which often extend outward into wide margins or fringes. These morphological adaptations are thought to have played a role in sediment feeding or filtering small organic particles from the seafloor.

Unlike many trilobites that possessed pronounced eyes and spiny ornamentation, Harpes trilobites typically display smoother exoskeletons and wide cephalic borders, giving them a unique and easily recognisable appearance among trilobite groups.

These trilobites were benthic organisms that lived on or slightly within the sediment of ancient seafloors.

Geological Context – The Fezouata Formation Lagerstätte

The Fezouata Formation of southeastern Morocco is one of the most extraordinary Ordovician fossil sites known. Deposited during the Tremadocian to Floian stages of the Early Ordovician, these sediments formed in a marine basin along the northern margin of the ancient Gondwana supercontinent.

The formation consists primarily of fine-grained shales and siltstones, deposited in relatively calm marine conditions. These sediments allowed for the exceptional preservation of both mineralised and soft-bodied organisms.

Fossils recovered from the Fezouata Formation include:

  • Trilobites such as Harpes and other early arthropods
  • Echinoderms including primitive starfish and crinoids
  • Brachiopods
  • Molluscs and cephalopods
  • Early marine worms and soft-bodied organisms

The Fezouata biota provides a unique snapshot of early Ordovician ecosystems and demonstrates that many animal groups first seen in the Cambrian continued to thrive into later geological periods.

Morphology and Adaptations of Harpes Trilobites

One of the defining characteristics of the genus Harpes is its broad cephalic shield, which often forms a wide, flattened border around the head. This structure likely helped stabilise the animal on soft seafloor sediments.

Key morphological features of Harpes trilobites include:

  • Large semicircular cephalon with expanded marginal rim
  • A relatively smooth exoskeleton lacking prominent spines
  • A narrow axial lobe running down the centre of the body
  • Segmented thorax allowing flexibility
  • Rounded pygidium forming the tail shield

The broad cephalic margin may have functioned as a sediment plough or filter surface, helping the trilobite feed on organic material present within fine seafloor muds.

Like other trilobites, the body was protected by a calcite exoskeleton, which fossilises particularly well and is often preserved in exceptional detail within the Fezouata shales.

A Genuine Ordovician Trilobite with Premium Certificate

This specimen represents a genuine fossil from one of the most important Ordovician fossil sites in the world. Trilobites from the Fezouata Formation are highly sought after due to both their scientific importance and distinctive morphology.

Key features of this fossil include:

  • Genuine Harpes trilobite fossil
  • Geological formation: Fezouata Formation
  • Age: Lower Ordovician Period, Tremadocian–Floian stages
  • Locality: Morocco
  • Rare Paleozoic marine arthropod fossil
  • Distinctive Harpetidae trilobite morphology
  • The exact specimen shown in the photographs
  • Includes a fully hand-signed Premium Certificate of Authenticity

Trilobites such as Harpes lived in ancient seas nearly 480 million years ago, long before the emergence of dinosaurs or even land animals. Fossils from the Fezouata Formation provide an extraordinary window into early marine life during one of the most important evolutionary periods in Earth’s history, making this specimen a fascinating and authentic addition to any fossil collection.

 

(Actual as seen)

Includes a fully hand-signed Premium Certificate of Authenticity.

Only 1 left in stock

SKU: P00395 Category:

Description

Rare Harpes Trilobite Fossil from the Fezouata Formation of Morocco

This genuine Harpes trilobite fossil originates from the renowned Fezouata Formation of Morocco, a world-famous Lower Ordovician fossil deposit dating to approximately 485–470 million years ago. Specimens from this locality represent some of the most scientifically important early Paleozoic fossils known, preserving marine life from a time when complex ecosystems were rapidly diversifying following the Cambrian Explosion.

The Fezouata Formation is globally recognised for its exceptional fossil preservation and is considered one of the most important Ordovician fossil Lagerstätten. Trilobites discovered here often display remarkable morphological detail, offering valuable insight into early arthropod evolution.

The fossil displayed in the photographs is the exact specimen you will receive, carefully selected for its preservation and authenticity. This specimen includes a fully hand-signed Premium Certificate of Authenticity, confirming the fossil is genuine.

Please refer to the photographs for full specimen sizing and scale.

About Harpes Trilobites – Distinctive Ordovician Arthropods

Trilobites were among the most successful marine arthropods of the Paleozoic Era, inhabiting Earth’s oceans for nearly 270 million years. The genus Harpes is particularly distinctive due to its unusual body morphology and expanded cephalic shield.

Taxonomic classification:

  • Kingdom: Animalia
  • Phylum: Arthropoda
  • Class: Trilobita
  • Order: Harpetida
  • Family: Harpetidae
  • Genus: Harpes

Members of the Harpetidae family are known for their broad, semicircular head shields, which often extend outward into wide margins or fringes. These morphological adaptations are thought to have played a role in sediment feeding or filtering small organic particles from the seafloor.

Unlike many trilobites that possessed pronounced eyes and spiny ornamentation, Harpes trilobites typically display smoother exoskeletons and wide cephalic borders, giving them a unique and easily recognisable appearance among trilobite groups.

These trilobites were benthic organisms that lived on or slightly within the sediment of ancient seafloors.

Geological Context – The Fezouata Formation Lagerstätte

The Fezouata Formation of southeastern Morocco is one of the most extraordinary Ordovician fossil sites known. Deposited during the Tremadocian to Floian stages of the Early Ordovician, these sediments formed in a marine basin along the northern margin of the ancient Gondwana supercontinent.

The formation consists primarily of fine-grained shales and siltstones, deposited in relatively calm marine conditions. These sediments allowed for the exceptional preservation of both mineralised and soft-bodied organisms.

Fossils recovered from the Fezouata Formation include:

  • Trilobites such as Harpes and other early arthropods
  • Echinoderms including primitive starfish and crinoids
  • Brachiopods
  • Molluscs and cephalopods
  • Early marine worms and soft-bodied organisms

The Fezouata biota provides a unique snapshot of early Ordovician ecosystems and demonstrates that many animal groups first seen in the Cambrian continued to thrive into later geological periods.

Morphology and Adaptations of Harpes Trilobites

One of the defining characteristics of the genus Harpes is its broad cephalic shield, which often forms a wide, flattened border around the head. This structure likely helped stabilise the animal on soft seafloor sediments.

Key morphological features of Harpes trilobites include:

  • Large semicircular cephalon with expanded marginal rim
  • A relatively smooth exoskeleton lacking prominent spines
  • A narrow axial lobe running down the centre of the body
  • Segmented thorax allowing flexibility
  • Rounded pygidium forming the tail shield

The broad cephalic margin may have functioned as a sediment plough or filter surface, helping the trilobite feed on organic material present within fine seafloor muds.

Like other trilobites, the body was protected by a calcite exoskeleton, which fossilises particularly well and is often preserved in exceptional detail within the Fezouata shales.

A Genuine Ordovician Trilobite with Premium Certificate

This specimen represents a genuine fossil from one of the most important Ordovician fossil sites in the world. Trilobites from the Fezouata Formation are highly sought after due to both their scientific importance and distinctive morphology.

Key features of this fossil include:

  • Genuine Harpes trilobite fossil
  • Geological formation: Fezouata Formation
  • Age: Lower Ordovician Period, Tremadocian–Floian stages
  • Locality: Morocco
  • Rare Paleozoic marine arthropod fossil
  • Distinctive Harpetidae trilobite morphology
  • The exact specimen shown in the photographs
  • Includes a fully hand-signed Premium Certificate of Authenticity

Trilobites such as Harpes lived in ancient seas nearly 480 million years ago, long before the emergence of dinosaurs or even land animals. Fossils from the Fezouata Formation provide an extraordinary window into early marine life during one of the most important evolutionary periods in Earth’s history, making this specimen a fascinating and authentic addition to any fossil collection.

 

Additional information

Era

Ordovician

Origin

Morocco

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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