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Fossil Crab in Display Box Gault Clay Folkestone Kent Cretaceous Genuine UK Crab Fossil Collector Specimen Natural History Gift

£84.00

Genuine Fossil Crab from the Gault Clay Formation – Folkestone, Kent

This authentic fossil crab preserved in a presentation display box originates from the famous Gault Clay Formation of Folkestone, Kent, UK, one of Britain’s most historically significant Cretaceous fossil localities. Dating to the Lower Cretaceous Period during the Albian Stage, approximately 113–100 million years ago, this specimen represents marine life that once thrived in the warm Cretaceous seas covering southern England.

The fossil shown in the photographs is the exact specimen you will receive, carefully selected for collectors and natural history enthusiasts. The fossil is housed in a protective display box, making it ideal for presentation, study, or display in a fossil collection.

The specimen includes a Certificate of Authenticity lifetime guarantee generic card, confirming that it is a genuine fossil specimen. Full sizing and proportions can be clearly seen in the listing photographs.

Geological Context – The Gault Clay Formation

The Gault Clay Formation is one of the most renowned fossil-bearing deposits in the United Kingdom. Exposed prominently along the coast at Folkestone in Kent, this geological unit represents sediments deposited during the Albian Stage of the Lower Cretaceous.

During this period, southern Britain lay beneath a relatively deep marine shelf sea that connected to the wider proto-Atlantic and Tethyan ocean systems. Fine clay sediments accumulated slowly on the sea floor in calm offshore conditions, creating ideal circumstances for the preservation of delicate marine organisms.

These clay-rich deposits are famous for preserving a diverse marine fauna including:

  • Ammonites
  • Bivalves
  • Gastropods
  • Fish remains
  • Marine reptiles
  • Crustaceans such as crabs

The exceptional fossil preservation found within the Gault Clay is the result of rapid burial in fine marine muds, which protected organisms from scavengers and allowed detailed anatomical features to fossilise.

Fossil Crab Classification and Evolutionary Significance

Crabs belong to the crustacean order Decapoda, a highly successful group of marine arthropods that includes lobsters, shrimp, and crabs. By the Cretaceous Period, true crabs had diversified significantly and occupied many ecological niches within marine environments.

Scientific Classification

  • Kingdom: Animalia
  • Phylum: Arthropoda
  • Subphylum: Crustacea
  • Class: Malacostraca
  • Order: Decapoda
  • Infraorder: Brachyura

Members of the Brachyura, or true crabs, are characterised by a broad carapace and reduced abdomen tucked beneath the body. Fossil crabs from the Gault Clay represent early representatives of this successful lineage during a time of major crustacean diversification in the Cretaceous oceans.

Morphology and Anatomical Features

Fossil crabs preserved in the Gault Clay often retain impressive detail due to the fine sediment in which they were buried. Typical anatomical features visible in such fossils include:

  • A broad carapace (protective shell) covering the main body
  • Segmented walking legs used for locomotion across the sea floor
  • Prominent chelae (claws) adapted for feeding and defence
  • Symmetrical body structure typical of brachyuran crabs
  • Subtle surface textures and ornamentation preserved within the carapace

These crabs were benthic organisms, living along the sea floor where they fed on small invertebrates, organic debris, and other food sources found within the sediment.

The compact body plan of true crabs allowed them to move efficiently through complex marine environments, including reefs, soft sediments, and rocky seabeds.

Depositional Environment and Marine Ecosystem

The environment represented by the Gault Clay sea was a relatively deep offshore marine basin characterised by quiet water conditions and slow sediment accumulation.

This marine ecosystem supported a rich diversity of life. Fossils recovered from these deposits reveal a thriving Cretaceous sea containing:

  • Ammonites drifting in open water
  • Bivalves and gastropods living within the sediment
  • Crustaceans moving across the sea floor
  • Predatory fish and marine reptiles

Crabs played an important ecological role within these environments as scavengers and opportunistic predators, helping recycle organic material within the marine ecosystem.

Fossil Preservation and Display

Over millions of years the crab’s original organic material was gradually replaced by minerals through the fossilisation process. The surrounding clay hardened into rock while preserving the shape and structure of the crustacean’s exoskeleton.

This natural mineralisation has allowed the specimen to survive for more than 100 million years, preserving a remarkable record of ancient marine life.

The fossil is supplied in a protective display box, allowing it to be safely exhibited while maintaining its integrity.

Certificate of Authenticity

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

Each fossil is carefully selected to ensure authenticity and quality, providing collectors with a true piece of prehistoric natural history.

A Classic British Marine Fossil

Fossils from the Gault Clay of Folkestone are highly regarded by collectors due to their historical significance and rich fossil diversity. This fossil crab specimen offers a tangible connection to the ancient Cretaceous seas that once covered southern Britain.

Whether displayed in a fossil cabinet, educational collection, or natural history display, this specimen represents a fascinating example of Cretaceous marine arthropods preserved within one of the UK’s most famous fossil formations.

 

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Description

Genuine Fossil Crab from the Gault Clay Formation – Folkestone, Kent

This authentic fossil crab preserved in a presentation display box originates from the famous Gault Clay Formation of Folkestone, Kent, UK, one of Britain’s most historically significant Cretaceous fossil localities. Dating to the Lower Cretaceous Period during the Albian Stage, approximately 113–100 million years ago, this specimen represents marine life that once thrived in the warm Cretaceous seas covering southern England.

The fossil shown in the photographs is the exact specimen you will receive, carefully selected for collectors and natural history enthusiasts. The fossil is housed in a protective display box, making it ideal for presentation, study, or display in a fossil collection.

The specimen includes a Certificate of Authenticity lifetime guarantee generic card, confirming that it is a genuine fossil specimen. Full sizing and proportions can be clearly seen in the listing photographs.

Geological Context – The Gault Clay Formation

The Gault Clay Formation is one of the most renowned fossil-bearing deposits in the United Kingdom. Exposed prominently along the coast at Folkestone in Kent, this geological unit represents sediments deposited during the Albian Stage of the Lower Cretaceous.

During this period, southern Britain lay beneath a relatively deep marine shelf sea that connected to the wider proto-Atlantic and Tethyan ocean systems. Fine clay sediments accumulated slowly on the sea floor in calm offshore conditions, creating ideal circumstances for the preservation of delicate marine organisms.

These clay-rich deposits are famous for preserving a diverse marine fauna including:

  • Ammonites
  • Bivalves
  • Gastropods
  • Fish remains
  • Marine reptiles
  • Crustaceans such as crabs

The exceptional fossil preservation found within the Gault Clay is the result of rapid burial in fine marine muds, which protected organisms from scavengers and allowed detailed anatomical features to fossilise.

Fossil Crab Classification and Evolutionary Significance

Crabs belong to the crustacean order Decapoda, a highly successful group of marine arthropods that includes lobsters, shrimp, and crabs. By the Cretaceous Period, true crabs had diversified significantly and occupied many ecological niches within marine environments.

Scientific Classification

  • Kingdom: Animalia
  • Phylum: Arthropoda
  • Subphylum: Crustacea
  • Class: Malacostraca
  • Order: Decapoda
  • Infraorder: Brachyura

Members of the Brachyura, or true crabs, are characterised by a broad carapace and reduced abdomen tucked beneath the body. Fossil crabs from the Gault Clay represent early representatives of this successful lineage during a time of major crustacean diversification in the Cretaceous oceans.

Morphology and Anatomical Features

Fossil crabs preserved in the Gault Clay often retain impressive detail due to the fine sediment in which they were buried. Typical anatomical features visible in such fossils include:

  • A broad carapace (protective shell) covering the main body
  • Segmented walking legs used for locomotion across the sea floor
  • Prominent chelae (claws) adapted for feeding and defence
  • Symmetrical body structure typical of brachyuran crabs
  • Subtle surface textures and ornamentation preserved within the carapace

These crabs were benthic organisms, living along the sea floor where they fed on small invertebrates, organic debris, and other food sources found within the sediment.

The compact body plan of true crabs allowed them to move efficiently through complex marine environments, including reefs, soft sediments, and rocky seabeds.

Depositional Environment and Marine Ecosystem

The environment represented by the Gault Clay sea was a relatively deep offshore marine basin characterised by quiet water conditions and slow sediment accumulation.

This marine ecosystem supported a rich diversity of life. Fossils recovered from these deposits reveal a thriving Cretaceous sea containing:

  • Ammonites drifting in open water
  • Bivalves and gastropods living within the sediment
  • Crustaceans moving across the sea floor
  • Predatory fish and marine reptiles

Crabs played an important ecological role within these environments as scavengers and opportunistic predators, helping recycle organic material within the marine ecosystem.

Fossil Preservation and Display

Over millions of years the crab’s original organic material was gradually replaced by minerals through the fossilisation process. The surrounding clay hardened into rock while preserving the shape and structure of the crustacean’s exoskeleton.

This natural mineralisation has allowed the specimen to survive for more than 100 million years, preserving a remarkable record of ancient marine life.

The fossil is supplied in a protective display box, allowing it to be safely exhibited while maintaining its integrity.

Certificate of Authenticity

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

Each fossil is carefully selected to ensure authenticity and quality, providing collectors with a true piece of prehistoric natural history.

A Classic British Marine Fossil

Fossils from the Gault Clay of Folkestone are highly regarded by collectors due to their historical significance and rich fossil diversity. This fossil crab specimen offers a tangible connection to the ancient Cretaceous seas that once covered southern Britain.

Whether displayed in a fossil cabinet, educational collection, or natural history display, this specimen represents a fascinating example of Cretaceous marine arthropods preserved within one of the UK’s most famous fossil formations.

 

Additional information

Era

Cretaceous

Origin

United Kingdom

Cretaceous Information

The Cretaceous Period (145–66 million years ago) was the final era of the Mesozoic, marked by the dominance of dinosaurs and the rise of flowering plants. It had a warm, greenhouse climate, with high sea levels that created vast shallow inland seas. Marine life flourished, including mosasaurs, ammonites, and rudist reefs, while the land was ruled by iconic dinosaurs like Tyrannosaurus rex, Triceratops, and Spinosaurus. Mammals and birds diversified, and insects thrived. The period ended with the mass extinction event, likely caused by an asteroid impact, wiping out the dinosaurs and paving the way for the rise of mammals in the Cenozoic.

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