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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Pecopteris Fossil Fern Frond Carboniferous Somerset UK Specimen with Certificate

£62.40

(Actual as seen)

Only 1 left in stock

SKU: SF2131 Category:

Description

Genuine Pecopteris Fossil Fern Frond from the Upper Carboniferous of Somerset

This genuine Pecopteris sp. fossil fern frond is a beautifully preserved prehistoric plant specimen originating from Upper Carboniferous deposits in Somerset, United Kingdom. Dating to approximately 323 to 299 million years ago, this fossil preserves part of an ancient fern-like plant that once grew within the vast tropical coal swamp forests covering prehistoric Britain during the late Paleozoic Era.

The specimen shown in the photographs is the exact fossil you will receive. Carefully selected for its preservation, natural detail and display appeal, this authentic fossil plant captures the delicate frond structure and fine leaf impressions characteristic of Pecopteris.

This fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the specimen is 100% genuine.

Full sizing please see photo.

About Pecopteris

Pecopteris is a well-known genus of extinct fern-like foliage commonly associated with seed ferns and true ferns that flourished throughout the Carboniferous Period. These plants formed a major component of the dense swamp forests that dominated equatorial regions during the late Paleozoic.

The name Pecopteris refers to the distinctive feather-like arrangement of the leaflets along the frond. Fossils of Pecopteris often preserve highly detailed pinnules and vein structures, creating elegant natural impressions within fine sedimentary rock.

These prehistoric plants thrived in warm humid conditions alongside giant lycopods, horsetails and early seed plants. Their delicate fronds formed part of the lush understory vegetation that covered Carboniferous wetlands and floodplains.

Pecopteris fossils are especially valued due to their intricate preservation and visual appeal. This specimen preserves the classic morphology associated with Carboniferous fern fronds, including the branching frond structure and naturally arranged leaflets characteristic of the genus.

Upper Carboniferous Coal Swamp Environment

During the Upper Carboniferous period, much of what is now the United Kingdom lay close to the equator and experienced a warm tropical climate with extensive humid wetlands and swamp forests. These environments supported some of the earliest large terrestrial ecosystems in Earth’s history.

The Carboniferous forests were dominated by giant lycopod trees, seed ferns, horsetails and fern-like plants such as Pecopteris. Thick vegetation accumulated within waterlogged low-oxygen swamps where plant debris was buried beneath sediment and eventually transformed into coal deposits over millions of years.

The Carboniferous rocks of Somerset preserve important evidence of these ancient ecosystems and contain a wide variety of fossil plants, helping scientists reconstruct prehistoric climates and terrestrial biodiversity.

Fine muds and silts settling within swamp and floodplain environments allowed delicate fern fronds to become fossilised in remarkable detail.

Natural Fossil Preservation

This fossil retains authentic natural preservation and has not been artificially replicated or reconstructed. The visible frond impressions, vein structures and plant textures formed naturally during fossilisation over hundreds of millions of years.

The specimen displays genuine botanical detail associated with Pecopteris foliage, including preserved leaflet arrangement and natural plant symmetry. Variations in colour and texture are entirely natural and reflect the mineral conditions present during burial and lithification.

Carboniferous plant fossils are highly collectable because they provide direct evidence of prehistoric forests that existed long before the rise of flowering plants and modern ecosystems.

Scientific and Collectable Importance

Pecopteris fossils are important to palaeobotany because they help scientists understand the composition and ecology of Carboniferous swamp forests. These plants played a major role in the formation of the coal deposits that later fuelled Britain’s Industrial Revolution.

Fossil fern fronds are particularly desirable among collectors because they preserve delicate organic structures rarely seen in other fossil groups. Their elegant appearance and exceptional age make them highly attractive display specimens as well as scientifically valuable fossils.

This specimen is ideal for collectors of fossil plants, Carboniferous fossils, fern fossils, British fossils, palaeobotanical specimens and authentic prehistoric natural history artefacts.

Certificate of Authenticity

Included with the fossil is a Certificate of Authenticity lifetime guarantee generic card confirming that the specimen is genuine. The photographs provided show the exact fossil you will receive, allowing collectors and buyers to purchase with complete confidence.

 

Additional information

Era

Carboniferous

Origin

United Kingdom

Carboniferous Information

The Carboniferous Period (359–299 million years ago) was a time of vast forests, giant insects, and the first reptiles. Named for its extensive coal deposits, this period saw lush swamps filled with towering lycophyte trees, ferns, and horsetails, which would later become today’s coal reserves. The climate was warm and humid, with high oxygen levels fueling the growth of giant arthropods like the dragonfly-like Meganeura and the massive millipede Arthropleura. Amphibians thrived in swampy environments, while the first reptiles evolved, laying eggs on land. In the oceans, sharks and early bony fish dominated, and corals flourished in warm, shallow seas. The period ended with a cooling climate and glaciation, leading to the drying of swamps and the decline of many species.

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