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Brittlestar Fossil Multislab Ophuroides sp Ordovician Morocco Draa Valley Specimen Genuine with Certificate

Original price was: £264.00.Current price is: £184.80.

(Actual as seen)

Includes a fully hand-signed Premium Certificate of Authenticity.

Only 1 left in stock

SKU: FSR158 Category:

Description

Product Overview
This Brittlestar Fossil Multislab featuring Ophuroides sp. is an exceptional and visually striking specimen from the renowned fossil beds of the Draa Valley in Morocco. Preserved within a natural rock matrix, this multi-specimen slab displays multiple brittle stars in a single piece, offering an impressive snapshot of ancient marine life from the Ordovician period. Each fossil has been carefully selected for quality and detail, with the listing images representing an example of the exact type of specimen you will receive.

This fossil is supplied with a Certificate of Authenticity lifetime guarantee card, confirming its genuine origin and natural formation. Please refer to the listing photographs for full sizing and scale.


Fossil Identification & Classification

  • Species: Ophuroides sp.
  • Class: Ophiuroidea (Brittle Stars)
  • Phylum: Echinodermata
  • Geological Age: Ordovician Period (approximately 485–444 million years ago)
  • Locality: Kataoua Formation, Mecissi area, Draa Valley, Morocco

Brittle stars are echinoderms closely related to modern starfish but distinguished by their long, slender, flexible arms radiating from a distinct central disc. The genus Ophuroides represents early brittle star forms that inhabited ancient seabeds during the Paleozoic era.


Geological Context & Formation
This fossil originates from the famous Kataoua Formation within the Draa Valley, a region globally recognised for its exceptionally preserved Ordovician marine fossils. During this period, the area was covered by a shallow epicontinental sea, rich in biodiversity. Fine-grained sedimentary conditions allowed delicate organisms like brittle stars to be rapidly buried and preserved in remarkable detail.

The depositional environment consisted of calm marine settings where periodic sediment influx created ideal fossilisation conditions. The presence of multiple individuals on a single slab suggests a possible mass burial event, such as a storm-induced sediment flow, which rapidly covered and preserved the organisms in situ.


Morphology & Preservation Features
Each brittle star fossil within the slab displays characteristic radial symmetry, with a central disc and five elongated arms extending outward. In well-preserved examples, fine structural details such as arm segmentation and skeletal plating may be visible, highlighting the intricate calcitic ossicles that make up the echinoderm skeleton.

The multislab format enhances both scientific and visual interest, as it captures multiple organisms preserved together, often in natural orientations. This provides insight into the behaviour and distribution of these ancient marine animals.

The fossils are naturally embedded within a sedimentary matrix, typically a fine shale or mudstone, which contrasts with the fossilised remains and enhances visibility.


Collecting & Display Appeal
This Brittlestar multislab is a highly desirable piece for fossil collectors, educators, and enthusiasts of Paleozoic life. Its combination of multiple specimens, clear morphology, and classic Moroccan locality makes it an excellent addition to any collection.

The slab format allows for easy display on a shelf, cabinet, or desk, making it both an educational specimen and a natural conversation piece. It is also an ideal gift for those interested in geology, palaeontology, or natural history.


Authenticity & Assurance

  • Genuine Ophuroides sp. Brittlestar fossil
  • Sourced from the Draa Valley, Morocco
  • Supplied with Certificate of Authenticity lifetime guarantee card
  • Carefully selected specimen matching the quality shown in listing images
  • A natural fossil formed over hundreds of millions of years

Care & Handling
As a natural fossil preserved in sedimentary rock, this specimen should be handled with care. Avoid dropping or applying pressure to delicate areas. It is best kept in a dry environment and can be gently dusted with a soft brush to maintain its appearance.

Additional information

Origin

Morocco

Era

Ordovician

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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