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Rare Fossil Crab Late Cretaceous New Jersey USA Genuine Authentic Specimen with Certificate of Authenticity

£96.00

Exceptional Rare Fossil Crab from the Late Cretaceous of New Jersey, USA

This beautiful and rare Fossil Crab originates from the Late Cretaceous deposits of New Jersey, USA, dating to approximately 70–66 million years ago. It represents an ancient marine arthropod preserved from a time when North America was divided by the Western Interior Seaway, a vast inland ocean that supported diverse marine life. This specimen is a genuine example of a Cretaceous crustacean fossil, showcasing the extraordinary preservation that makes these finds both scientifically significant and visually striking.

Each fossil is 100% genuine, carefully prepared, and comes with a Certificate of Authenticity. The exact specimen shown in the photographs is the one you will receive, ensuring full transparency and authenticity. The scale cube (1 cm) visible in the image provides precise sizing reference; full dimensions are included in the listing photos.

Geological Context and Formation

This fossil originates from the Navesink and Hornerstown Formations of New Jersey, which span the Maastrichtian Stage of the Late Cretaceous Period, approximately 70 to 66 million years ago. These formations are composed primarily of greensand glauconitic marls and silty sands, deposited in shallow marine environments along the ancient Atlantic Coastal Plain. During this period, the coastline of eastern North America was submerged under a warm, tropical sea filled with ammonites, molluscs, crustaceans, and early marine vertebrates.

The depositional environment was nearshore and subtidal, with soft, fine-grained sediment ideal for the preservation of delicate marine organisms like crabs. The anaerobic conditions within these marine sediments prevented decay and allowed mineralisation to occur. Over millions of years, the crab’s exoskeleton was replaced by minerals such as calcite and iron-rich silicates, preserving even intricate details of the carapace and limbs.

The Cretaceous sediments of New Jersey are globally famous for yielding fossils of marine invertebrates and vertebrates alike — including fossil crabs, ammonites, belemnites, mosasaurs, and ancient fish — all recording the rich biodiversity of this prehistoric shoreline.

Scientific Classification

  • Kingdom: Animalia
  • Phylum: Arthropoda
  • Subphylum: Crustacea
  • Class: Malacostraca
  • Order: Decapoda
  • Infraorder: Brachyura
  • Family: Cenomanocarcinidae (possible)
  • Genus: Cenomanocarcinus (tentative attribution based on morphology and locality)
  • Age: Late Cretaceous (Maastrichtian Stage, ~70–66 million years ago)
  • Formation: Navesink / Hornerstown Formation
  • Locality: New Jersey, United States of America

Crabs from these formations are often attributed to Cenomanocarcinus or related genera, members of the Cenomanocarcinidae, an extinct family of early true crabs. These fossils demonstrate the early evolution of the Brachyura, or “short-tailed” crabs, which diversified rapidly during the Cretaceous and went on to become one of the most successful groups of crustaceans.

Morphology and Preservation

This specimen preserves a beautifully detailed carapace (crab shell) along with portions of the claws (chelae) and possible leg impressions, offering an excellent example of the characteristic features of Late Cretaceous marine crabs. The surface detail reveals the segmented exoskeleton, orbital notches, and subtle ornamentation that defined the crab’s body structure.

The fossil exhibits natural mineralisation, with hues of light brown, tan, and grey contrasting against the fine-grained matrix. This coloration results from iron oxide and silica replacement during diagenesis, a process that gradually transformed the original chitinous shell into stone.

The crab’s overall flattened profile suggests post-mortem compression typical of marine sediment fossilisation. Yet despite this, the specimen retains strong relief and definition, with the delicate curvature of the carapace and margins still visible. Such well-preserved crab fossils are relatively rare compared to molluscs or fish, as crustacean exoskeletons are more fragile and often disarticulate before burial.

Palaeoenvironment and Significance

During the Late Cretaceous, the region now known as New Jersey lay beneath a warm, shallow sea, located near the equator. This was a period of high sea levels, with extensive marine ecosystems thriving across the continental shelves. The crab represented by this fossil likely lived on or near the seabed, scavenging or hunting smaller invertebrates among soft sediments and shell debris.

The marine ecosystem of the Cretaceous Atlantic Coastal Plain included ammonites, echinoids, fish, and marine reptiles like mosasaurs, alongside an abundance of benthic life such as crabs and lobsters. Crabs were an important part of this food web, occupying ecological niches as scavengers and opportunistic predators.

The discovery of fossil crabs from this formation provides valuable insight into Cretaceous crustacean diversity and evolution, helping palaeontologists trace the development of modern crab lineages. These fossils are particularly significant because they represent early adaptations toward the robust, rounded body shapes typical of modern brachyuran crabs, which allowed them to burrow and manoeuvre effectively within sandy and silty environments.

Scientific and Collectible Importance

Fossil crabs from the Cretaceous of New Jersey are considered rare and scientifically important, both for their preservation and their contribution to the understanding of decapod evolution. Specimens of this quality are seldom found intact, as crab shells typically disintegrate quickly after death. This makes this fossil not only a striking collector’s piece but also a scientifically valuable example of early crab morphology.

Collectors, educators, and enthusiasts alike appreciate these fossils for their combination of beauty and historical importance — a direct link to a time when giant reptiles ruled the seas and the earliest true crabs scuttled along the seabed.

This specimen is ideal for display, research, or as a centrepiece in any serious fossil collection, showcasing the delicate balance of life that existed at the end of the Age of Dinosaurs.

Authenticity and Provenance

All of our fossils are 100% genuine specimens, responsibly sourced and professionally curated. Each piece is supplied with a Certificate of Authenticity, verifying its geological origin and species identification. The fossil shown in the photographs is the exact specimen you will receive — no stock images are ever used.

This Rare Fossil Crab from the Late Cretaceous of New Jersey, USA, is a scientifically valuable and visually captivating piece of Earth’s history. Representing one of the earliest true crabs to appear in the fossil record, it stands as a tangible connection to the ancient oceans of the Cretaceous and the remarkable evolution of marine life that shaped our modern world.

(Actual as seen)

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Description

Exceptional Rare Fossil Crab from the Late Cretaceous of New Jersey, USA

This beautiful and rare Fossil Crab originates from the Late Cretaceous deposits of New Jersey, USA, dating to approximately 70–66 million years ago. It represents an ancient marine arthropod preserved from a time when North America was divided by the Western Interior Seaway, a vast inland ocean that supported diverse marine life. This specimen is a genuine example of a Cretaceous crustacean fossil, showcasing the extraordinary preservation that makes these finds both scientifically significant and visually striking.

Each fossil is 100% genuine, carefully prepared, and comes with a Certificate of Authenticity. The exact specimen shown in the photographs is the one you will receive, ensuring full transparency and authenticity. The scale cube (1 cm) visible in the image provides precise sizing reference; full dimensions are included in the listing photos.

Geological Context and Formation

This fossil originates from the Navesink and Hornerstown Formations of New Jersey, which span the Maastrichtian Stage of the Late Cretaceous Period, approximately 70 to 66 million years ago. These formations are composed primarily of greensand glauconitic marls and silty sands, deposited in shallow marine environments along the ancient Atlantic Coastal Plain. During this period, the coastline of eastern North America was submerged under a warm, tropical sea filled with ammonites, molluscs, crustaceans, and early marine vertebrates.

The depositional environment was nearshore and subtidal, with soft, fine-grained sediment ideal for the preservation of delicate marine organisms like crabs. The anaerobic conditions within these marine sediments prevented decay and allowed mineralisation to occur. Over millions of years, the crab’s exoskeleton was replaced by minerals such as calcite and iron-rich silicates, preserving even intricate details of the carapace and limbs.

The Cretaceous sediments of New Jersey are globally famous for yielding fossils of marine invertebrates and vertebrates alike — including fossil crabs, ammonites, belemnites, mosasaurs, and ancient fish — all recording the rich biodiversity of this prehistoric shoreline.

Scientific Classification

  • Kingdom: Animalia
  • Phylum: Arthropoda
  • Subphylum: Crustacea
  • Class: Malacostraca
  • Order: Decapoda
  • Infraorder: Brachyura
  • Family: Cenomanocarcinidae (possible)
  • Genus: Cenomanocarcinus (tentative attribution based on morphology and locality)
  • Age: Late Cretaceous (Maastrichtian Stage, ~70–66 million years ago)
  • Formation: Navesink / Hornerstown Formation
  • Locality: New Jersey, United States of America

Crabs from these formations are often attributed to Cenomanocarcinus or related genera, members of the Cenomanocarcinidae, an extinct family of early true crabs. These fossils demonstrate the early evolution of the Brachyura, or “short-tailed” crabs, which diversified rapidly during the Cretaceous and went on to become one of the most successful groups of crustaceans.

Morphology and Preservation

This specimen preserves a beautifully detailed carapace (crab shell) along with portions of the claws (chelae) and possible leg impressions, offering an excellent example of the characteristic features of Late Cretaceous marine crabs. The surface detail reveals the segmented exoskeleton, orbital notches, and subtle ornamentation that defined the crab’s body structure.

The fossil exhibits natural mineralisation, with hues of light brown, tan, and grey contrasting against the fine-grained matrix. This coloration results from iron oxide and silica replacement during diagenesis, a process that gradually transformed the original chitinous shell into stone.

The crab’s overall flattened profile suggests post-mortem compression typical of marine sediment fossilisation. Yet despite this, the specimen retains strong relief and definition, with the delicate curvature of the carapace and margins still visible. Such well-preserved crab fossils are relatively rare compared to molluscs or fish, as crustacean exoskeletons are more fragile and often disarticulate before burial.

Palaeoenvironment and Significance

During the Late Cretaceous, the region now known as New Jersey lay beneath a warm, shallow sea, located near the equator. This was a period of high sea levels, with extensive marine ecosystems thriving across the continental shelves. The crab represented by this fossil likely lived on or near the seabed, scavenging or hunting smaller invertebrates among soft sediments and shell debris.

The marine ecosystem of the Cretaceous Atlantic Coastal Plain included ammonites, echinoids, fish, and marine reptiles like mosasaurs, alongside an abundance of benthic life such as crabs and lobsters. Crabs were an important part of this food web, occupying ecological niches as scavengers and opportunistic predators.

The discovery of fossil crabs from this formation provides valuable insight into Cretaceous crustacean diversity and evolution, helping palaeontologists trace the development of modern crab lineages. These fossils are particularly significant because they represent early adaptations toward the robust, rounded body shapes typical of modern brachyuran crabs, which allowed them to burrow and manoeuvre effectively within sandy and silty environments.

Scientific and Collectible Importance

Fossil crabs from the Cretaceous of New Jersey are considered rare and scientifically important, both for their preservation and their contribution to the understanding of decapod evolution. Specimens of this quality are seldom found intact, as crab shells typically disintegrate quickly after death. This makes this fossil not only a striking collector’s piece but also a scientifically valuable example of early crab morphology.

Collectors, educators, and enthusiasts alike appreciate these fossils for their combination of beauty and historical importance — a direct link to a time when giant reptiles ruled the seas and the earliest true crabs scuttled along the seabed.

This specimen is ideal for display, research, or as a centrepiece in any serious fossil collection, showcasing the delicate balance of life that existed at the end of the Age of Dinosaurs.

Authenticity and Provenance

All of our fossils are 100% genuine specimens, responsibly sourced and professionally curated. Each piece is supplied with a Certificate of Authenticity, verifying its geological origin and species identification. The fossil shown in the photographs is the exact specimen you will receive — no stock images are ever used.

This Rare Fossil Crab from the Late Cretaceous of New Jersey, USA, is a scientifically valuable and visually captivating piece of Earth’s history. Representing one of the earliest true crabs to appear in the fossil record, it stands as a tangible connection to the ancient oceans of the Cretaceous and the remarkable evolution of marine life that shaped our modern world.

Additional information

Era

Cretaceous

Origin

USA

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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