Description
Genuine Lepidodendron Fossil Lycopod Wood and Stigmaria Root from North Yorkshire
This genuine Lepidodendron sp. Fossil Lycopod Wood and Stigmaria Root specimen is a remarkable piece of prehistoric plant history originating from the Upper Carboniferous deposits of Pateley Bridge, North Yorkshire, United Kingdom. Preserved for over 300 million years, this fossil captures part of an ancient coal swamp ecosystem that once covered large areas of prehistoric Britain during the Carboniferous Period.
The specimen shown in the photographs is the exact fossil you will receive. Carefully selected for its quality, preservation and natural detail, this authentic fossil preserves both sections of Lepidodendron lycopod wood and associated Stigmaria rooting structures, making it an especially interesting and scientifically significant example of Paleozoic plant life.
This fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the specimen is 100% genuine.
Full sizing please see photo.
About Lepidodendron
Lepidodendron was a giant extinct lycopod tree belonging to the class Lycopodiopsida, an ancient lineage of vascular plants related to modern club mosses. During the Carboniferous Period, these enormous plants formed dense swamp forests that dominated tropical lowland environments across much of the planet.
Unlike modern lycopods, which are generally small ground plants, Lepidodendron species could grow to heights exceeding 30 metres. Their trunks were covered in characteristic diamond-shaped leaf scars produced as leaves were shed during growth. These distinctive bark patterns are among the most recognisable features of Carboniferous plant fossils.
Lepidodendron reproduced using spores rather than seeds and played a major role in the development of the extensive coal-forming forests that define Carboniferous geology worldwide.
Stigmaria Root Structures
The specimen also preserves Stigmaria root material, the specialised rooting system associated with Lepidodendron and related giant lycopods. Stigmaria structures spread horizontally through soft swamp sediment and produced thousands of fine rootlets used to stabilise these towering plants within waterlogged environments.
Fossilised Stigmaria roots are easily recognised by their circular rootlet scars and textured surface patterns. Their preservation alongside Lepidodendron wood provides valuable insight into the full anatomy and growth habits of these extraordinary prehistoric plants.
Specimens preserving both stem and root structures are highly desirable among collectors and palaeobotanical enthusiasts because they illustrate multiple parts of the original organism within a single fossil piece.
Carboniferous Coal Swamp Environment
During the Upper Carboniferous period, approximately 323 to 299 million years ago, Britain lay near the equator and experienced warm humid tropical conditions. Vast swamp forests developed across extensive floodplains, creating one of the most productive ecosystems in Earth’s history.
These wetlands supported giant lycopods, horsetails, seed ferns and early insects in oxygen-rich environments. Over millions of years, dead plant material accumulated within oxygen-poor swamps and became buried beneath sediment, eventually forming the coal seams associated with Britain’s industrial history.
The Carboniferous deposits of North Yorkshire preserve important evidence of these ancient ecosystems and provide exceptional fossil plant material that helps scientists reconstruct prehistoric climates and vegetation patterns.
Natural Fossil Preservation
This specimen retains authentic natural preservation and has not been artificially replicated or reconstructed. The visible bark textures, root scars and mineralisation formed naturally during fossilisation over hundreds of millions of years.
The fossil displays genuine geological character with preserved structural details that reflect the original biological form of the plant. Variations in colour and texture are entirely natural and result from mineral replacement processes occurring during burial and lithification.
Carboniferous fossil plants are highly collectable because they represent some of the earliest large forest ecosystems on Earth and played a major role in shaping the planet’s atmosphere and coal deposits.
Scientific and Collectable Importance
Lepidodendron fossils are among the most iconic plant fossils from the Paleozoic Era and remain highly important to palaeobotanical research. Their remains provide evidence for the evolution of vascular plants, prehistoric climate conditions and the formation of coal-producing ecosystems.
Specimens containing both Lepidodendron and Stigmaria material are especially significant because they preserve multiple anatomical components of these giant prehistoric plants within a single display piece.
This fossil is ideal for collectors of Carboniferous fossils, fossil plants, British fossils, palaeobotanical specimens, coal swamp fossils 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.
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