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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British Triassic Stromatolite Fossil Cotham Marble Rhaetic Blue Anchor 14 in UK: Large Rhaetic North Somerset Display Specimen

Original price was: £264.00.Current price is: £240.00.

(Actual as seen)

Includes a fully hand-signed Premium Certificate of Authenticity.

Only 1 left in stock

SKU: P00764 Category:

Description

Genuine British Late Triassic Stromatolite Fossil

This impressive 14 inch British stromatolite fossil is a carefully chosen genuine specimen from the Cotham Marble of Blue Anchor, near Bristol, North Somerset. Dating from the Rhaetic of the Late Triassic, this fossil represents a remarkable piece of British geological history from a time close to the Triassic-Jurassic boundary, when changing seas, lagoons and coastal environments shaped the landscape that would eventually become south-west England.

The photograph shows the actual fossil specimen you will receive. Full sizing and visual details can be seen in the photo, making this a highly displayable and collectible example for fossil collectors, geology enthusiasts, educational collections and natural history displays.

Geology and Formation

Cotham Marble is a distinctive ornamental limestone associated with the uppermost Triassic Rhaetic deposits of south-west Britain. Despite its traditional name, it is not a true metamorphic marble, but a fine-grained limestone known for its attractive patterned structure. The material is especially associated with stromatolitic and microbial textures, creating natural markings that can resemble branching, landscape-like or mossy forms when cut or polished.

This specimen comes from Blue Anchor, North Somerset, an important area for British Triassic and Rhaetic geology. The Late Triassic rocks of this region record shallow marine and marginal marine conditions, with periods of restricted water circulation, changing salinity and carbonate deposition. Stromatolitic limestone such as Cotham Marble formed in environments where microbial communities helped trap, bind and precipitate sediment, gradually building layered carbonate structures over time.

Fossil Type and Stromatolite Structure

Stromatolites are among the most ancient and important fossil structures known in the geological record. Rather than being the preserved remains of a single animal or plant, they are sedimentary structures created by microbial mats, especially cyanobacteria and other microorganisms. These microbial communities grew across sediment surfaces, trapping fine particles and encouraging carbonate minerals to form. Over repeated cycles, this process produced layered, domed, wrinkled or branching structures.

In Cotham Marble, the stromatolitic textures are valued for their distinctive natural patterns. These features make each piece unique, with the internal structure reflecting the growth of microbial mats in a Late Triassic carbonate setting. The fossil is therefore both a decorative natural history specimen and an important example of microbial fossil activity.

Age, Location and Scientific Interest

This fossil is from the Rhaetic stage of the Late Triassic, making it approximately 201 to 208 million years old. The Rhaetic was the final stage of the Triassic Period, immediately preceding the Jurassic. Fossils and rocks from this interval are particularly interesting because they record environmental changes that occurred shortly before one of the major extinction events in Earth history.

The Blue Anchor and wider North Somerset coast are well known for Triassic and early Mesozoic geology. Specimens from this region are prized by collectors because they combine strong British provenance with attractive fossil and sedimentary features. Cotham Marble from this area is especially recognised for its stromatolitic textures and historic use as a decorative stone.

Display and Collectability

At 14 inches, this is a substantial fossil display specimen with strong visual impact. Its British origin, Late Triassic age and Cotham Marble association make it suitable for collectors of UK fossils, stromatolites, sedimentary structures, natural history specimens and geological display pieces. The natural patterning makes it especially appealing as both a fossil and a decorative geological specimen.

This fossil would make an excellent addition to a fossil cabinet, teaching collection, geology display, natural history collection or interior display for anyone interested in ancient life, microbial fossils and British geology.

Authenticity and Certificate

This fossil is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee generic card. The certificate provides reassurance that the fossil supplied is an authentic natural specimen. The photo shows the actual fossil you will receive, so you can buy with confidence knowing the colour, form and appearance shown are representative of the exact piece being offered.

Additional information

Era

Triassic

Origin

United Kingdom

Triassic Information

The Triassic Period (252–201 million years ago) marked the beginning of the Mesozoic Era, following the Permian-Triassic mass extinction, the most severe extinction event in Earth's history. The climate was hot and dry, with vast deserts and little polar ice. Life slowly recovered, leading to the rise of the first dinosaurs, pterosaurs (flying reptiles), and early mammals. Reptiles, including large archosaurs (ancestors of crocodiles and dinosaurs), dominated both land and sea. In the oceans, ichthyosaurs and plesiosaurs thrived alongside ammonites and early coral reefs. The first true conifers and ginkgo trees spread across the land. The period ended with another mass extinction, paving the way for the Jurassic and the golden age of dinosaurs.

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