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Gastropod Fossil Shell Block Isle of Wight Eocene Totland Bay Genuine Specimen Authentic

£24.00

Specimen Overview

This genuine gastropod fossil shell block is a beautifully preserved piece from the renowned fossil locality of Totland Bay on the Isle of Wight. Featuring multiple fossilised shells embedded within natural limestone matrix, this specimen offers both strong visual appeal and valuable geological context. Carefully selected for quality and composition, the exact fossil block shown in the photographs is the one you will receive.

Discovered by our dedicated team members, Alister and Alison, and professionally cleaned, prepped, and treated by Alison, this specimen has been expertly handled to highlight its natural features while preserving its authenticity. It includes a Certificate of Authenticity with a lifetime guarantee, confirming its genuine origin.

Geological Origin – Headon Hill Formation, Isle of Wight

This fossil block originates from the Hatherwood Limestone Member of the Headon Hill Formation, exposed at Totland Bay on the Isle of Wight, UK. These deposits date to the Eocene epoch, approximately 56 to 34 million years ago, a time when southern England experienced a warm, subtropical climate.

The Headon Hill Formation is characterised by alternating limestones, marls, and clays that represent a sequence of freshwater, lagoonal, and brackish environments. The Hatherwood Limestone Member in particular formed under calm, shallow water conditions, allowing fine carbonate sediments to accumulate and preserve delicate fossil shells in remarkable detail.

Fossil Identification – Gastropod Assemblage

This specimen represents a natural assemblage of fossil gastropods, likely including freshwater and lagoonal species such as Viviparus and planorbid-type gastropods. These organisms belong to the class Gastropoda, one of the most diverse groups of molluscs, known for their coiled shells and wide ecological distribution.

Gastropods in this formation display a range of morphological features, including:

  • Spiral coiling, either high-spired or planispiral
  • Defined whorls with visible sutures
  • Smooth to subtly ornamented shell surfaces
  • Rounded apertures indicative of soft-bodied extension

The presence of multiple shells within a single block reflects natural accumulation within the ancient environment.

Morphology and Preservation

This fossil block preserves numerous gastropod shells within their original limestone matrix, offering a snapshot of Eocene life. The shells exhibit varying shapes and sizes, from compact coiled forms to more elongated spirals, creating a visually interesting and scientifically valuable specimen.

The preservation quality highlights the fine details of shell morphology, including whorl structure and surface texture. The limestone matrix provides both structural support and aesthetic contrast, enhancing the visibility of the fossils while maintaining their natural context.

Mineralisation over millions of years has resulted in subtle colour variations, adding to the authenticity and character of the piece.

Paleoenvironment and Depositional Setting

During the Eocene, the Isle of Wight region was dominated by freshwater lakes, lagoons, and coastal plains. The Hatherwood Limestone Member represents a calm depositional environment where gastropods thrived in shallow waters.

These snails played an important ecological role as grazers, feeding on algae and organic material. The accumulation of shells within the sediment suggests a stable and productive ecosystem, periodically buried by fine carbonate deposits that preserved them in situ.

This fossil block captures a moment in that ancient environment, providing insight into the biodiversity and conditions of Eocene freshwater systems.

Authenticity and Preparation

This fossil is a genuine natural specimen, not a cast or reproduction. It has been carefully prepared by Alison to reveal the fossil shells while preserving the integrity of the matrix. The included Certificate of Authenticity with lifetime guarantee ensures confidence in its provenance.

All photographs show the exact specimen, allowing you to fully assess its quality, composition, and detail before purchase.

Collectability and Display Appeal

Gastropod fossil blocks from the Headon Hill Formation are highly sought after for their combination of scientific interest and natural beauty. The presence of multiple shells within a single matrix piece enhances both its rarity and display value.

This specimen is ideal for collectors of British fossils, educational use, or as a distinctive display piece. Its natural composition and well-preserved fossils make it a compelling addition to any collection, offering a tangible connection to life in the Eocene period.

(Actual as seen)

Only 1 left in stock

SKU: CF3541 Category:

Description

Specimen Overview

This genuine gastropod fossil shell block is a beautifully preserved piece from the renowned fossil locality of Totland Bay on the Isle of Wight. Featuring multiple fossilised shells embedded within natural limestone matrix, this specimen offers both strong visual appeal and valuable geological context. Carefully selected for quality and composition, the exact fossil block shown in the photographs is the one you will receive.

Discovered by our dedicated team members, Alister and Alison, and professionally cleaned, prepped, and treated by Alison, this specimen has been expertly handled to highlight its natural features while preserving its authenticity. It includes a Certificate of Authenticity with a lifetime guarantee, confirming its genuine origin.

Geological Origin – Headon Hill Formation, Isle of Wight

This fossil block originates from the Hatherwood Limestone Member of the Headon Hill Formation, exposed at Totland Bay on the Isle of Wight, UK. These deposits date to the Eocene epoch, approximately 56 to 34 million years ago, a time when southern England experienced a warm, subtropical climate.

The Headon Hill Formation is characterised by alternating limestones, marls, and clays that represent a sequence of freshwater, lagoonal, and brackish environments. The Hatherwood Limestone Member in particular formed under calm, shallow water conditions, allowing fine carbonate sediments to accumulate and preserve delicate fossil shells in remarkable detail.

Fossil Identification – Gastropod Assemblage

This specimen represents a natural assemblage of fossil gastropods, likely including freshwater and lagoonal species such as Viviparus and planorbid-type gastropods. These organisms belong to the class Gastropoda, one of the most diverse groups of molluscs, known for their coiled shells and wide ecological distribution.

Gastropods in this formation display a range of morphological features, including:

  • Spiral coiling, either high-spired or planispiral
  • Defined whorls with visible sutures
  • Smooth to subtly ornamented shell surfaces
  • Rounded apertures indicative of soft-bodied extension

The presence of multiple shells within a single block reflects natural accumulation within the ancient environment.

Morphology and Preservation

This fossil block preserves numerous gastropod shells within their original limestone matrix, offering a snapshot of Eocene life. The shells exhibit varying shapes and sizes, from compact coiled forms to more elongated spirals, creating a visually interesting and scientifically valuable specimen.

The preservation quality highlights the fine details of shell morphology, including whorl structure and surface texture. The limestone matrix provides both structural support and aesthetic contrast, enhancing the visibility of the fossils while maintaining their natural context.

Mineralisation over millions of years has resulted in subtle colour variations, adding to the authenticity and character of the piece.

Paleoenvironment and Depositional Setting

During the Eocene, the Isle of Wight region was dominated by freshwater lakes, lagoons, and coastal plains. The Hatherwood Limestone Member represents a calm depositional environment where gastropods thrived in shallow waters.

These snails played an important ecological role as grazers, feeding on algae and organic material. The accumulation of shells within the sediment suggests a stable and productive ecosystem, periodically buried by fine carbonate deposits that preserved them in situ.

This fossil block captures a moment in that ancient environment, providing insight into the biodiversity and conditions of Eocene freshwater systems.

Authenticity and Preparation

This fossil is a genuine natural specimen, not a cast or reproduction. It has been carefully prepared by Alison to reveal the fossil shells while preserving the integrity of the matrix. The included Certificate of Authenticity with lifetime guarantee ensures confidence in its provenance.

All photographs show the exact specimen, allowing you to fully assess its quality, composition, and detail before purchase.

Collectability and Display Appeal

Gastropod fossil blocks from the Headon Hill Formation are highly sought after for their combination of scientific interest and natural beauty. The presence of multiple shells within a single matrix piece enhances both its rarity and display value.

This specimen is ideal for collectors of British fossils, educational use, or as a distinctive display piece. Its natural composition and well-preserved fossils make it a compelling addition to any collection, offering a tangible connection to life in the Eocene period.

Additional information

Era

Eocene

Origin

United Kingdom

Eocene Information

The Eocene Period (56–33.9 million years ago) was a time of warm global temperatures and the rapid evolution of mammals following the extinction of the dinosaurs. The climate was hot and humid, with lush rainforests covering much of the planet, even near the poles. Mammals diversified into new ecological roles, with early primates, whales (like Basilosaurus), large herbivores, and carnivores emerging. Birds and reptiles also thrived, and the first grasses began spreading, setting the stage for later grassland ecosystems. By the late Eocene, the Earth’s climate cooled significantly, leading to the formation of the first Antarctic ice sheets and the eventual transition to the drier, cooler Oligocene Period.

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