Description
Genuine Lepidodendron Fossil Lycopod Wood and Stigmaria Root from North Yorkshire
This genuine Lepidodendron sp. Fossil Lycopod Wood and Stigmaria Root specimen is an exceptional 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 represents part of the ancient swamp forests that once covered vast regions 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 fossil preserves both Lepidodendron lycopod wood and associated Stigmaria root structures, offering a remarkable glimpse into one of the earliest forest ecosystems on Earth.
This fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the specimen is 100% genuine.
Full sizing please see photo.
About Lepidodendron and Stigmaria
Lepidodendron was a giant extinct lycopod tree belonging to the class Lycopodiopsida, an ancient group of vascular plants related to modern club mosses. Unlike the small ground-covering lycopods alive today, Lepidodendron species could grow to towering heights exceeding 30 metres and formed dense forests throughout the Carboniferous coal swamps.
These prehistoric trees possessed tall trunks covered in distinctive diamond-shaped leaf scar patterns created as leaves were shed during growth. Their bark-like outer structure and rapid growth allowed them to dominate wet tropical environments during the Carboniferous.
Stigmaria refers to the specialised rooting structures associated with Lepidodendron and related lycopod trees. These root systems spread horizontally through swamp sediments and produced numerous rootlets used to stabilise the giant plants within soft waterlogged ground.
Fossilised Stigmaria roots are highly recognisable due to their circular rootlet scars and textured surface patterns. Specimens preserving both Lepidodendron wood and Stigmaria structures are particularly desirable because they illustrate both the aerial and underground anatomy of these extraordinary prehistoric plants.
Carboniferous Coal Forest Ecosystems
During the Upper Carboniferous period, approximately 323 to 299 million years ago, much of Britain was located near the equator and experienced warm humid tropical conditions. Extensive swamp forests developed across low-lying regions, supporting giant lycopods, horsetails, seed ferns and early insects.
The dense vegetation of these ancient forests accumulated within oxygen-poor wetlands where dead plant material became buried beneath sediment and gradually transformed into coal deposits over millions of years. Fossils from these environments provide important evidence for the origin of coal-forming ecosystems and the evolution of terrestrial plant life.
The Carboniferous deposits of northern England are internationally significant for preserving fossil plants in remarkable detail. Pateley Bridge and surrounding Yorkshire localities have yielded numerous well-preserved examples of fossilised lycopods and associated root systems.
Natural Fossil Preservation
This specimen preserves authentic fossilised plant material with naturally formed textures and structural detail. The visible bark patterns, root scars and mineralisation developed naturally during fossilisation and provide evidence of the original biological structure of the plant.
The fossil has not been artificially replicated or reconstructed. Natural colour variation and surface texture reflect the geological processes that preserved the specimen over hundreds of millions of years.
Fossilised plant remains from the Carboniferous period are highly valued by collectors because they represent some of the earliest large forest ecosystems in Earth’s history. Specimens containing both stem and root material are especially desirable due to their scientific and educational significance.
Geological and Scientific Importance
Lepidodendron fossils are among the most iconic plant fossils from the Paleozoic Era and played a major role in forming the coal deposits that powered the Industrial Revolution. Their remains provide critical evidence for understanding the evolution of terrestrial ecosystems, atmospheric oxygen levels and prehistoric climates.
The Stigmaria root structures associated with these plants also offer important insights into how early giant plants adapted to unstable swamp environments. Together, these fossils represent an extraordinary record of life long before the appearance of dinosaurs or flowering plants.
This specimen is ideal for collectors of Carboniferous fossils, fossil plants, British fossils, paleo-botanical specimens, coal forest 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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