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Rare Fossil Crabs Brachyura Eocene Cairo Egypt Marine Crab Fossil Prehistoric Crustacean

£120.00

Rare Fossil Crab Specimen from the Eocene of Egypt

This rare fossil crab belonging to the infraorder Brachyura originates from Eocene marine deposits near Cairo, Egypt. Dating to the Eocene epoch of the Paleogene Period, approximately 56–33.9 million years ago, this specimen represents part of the diverse crustacean fauna that inhabited the warm tropical seas covering northern Africa during the early Cenozoic.

The fossil is a carefully selected specimen preserved within its natural matrix, displaying the characteristic structure of ancient brachyuran crabs. The photographs show the exact fossil you will receive, allowing collectors to examine the preserved features and natural condition of the specimen. Please refer to the photographs for the full sizing and proportions. The fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the authenticity of the specimen.

About Brachyura – True Crabs in the Fossil Record

True crabs belong to the infraorder Brachyura within the order Decapoda, a diverse group of crustaceans that includes modern crabs, lobsters, shrimps, and prawns. Brachyuran crabs are distinguished by their broad, flattened carapace, reduced abdomen folded beneath the body, and strong chelae or claws adapted for feeding and defence.

Crabs first appeared in the fossil record during the Jurassic and became highly diverse by the Cretaceous and Paleogene periods. By the time of the Eocene epoch, brachyuran crabs had already radiated into numerous ecological niches, occupying shallow marine seabeds, reef environments, estuaries, and coastal habitats.

Although the exact species of this specimen cannot be determined with certainty, fossil crabs from Eocene deposits commonly represent members of several crab families adapted to warm shallow marine conditions.

Morphology and Anatomical Characteristics

Brachyuran crabs possess a distinctive body plan dominated by a wide protective carapace covering the cephalothorax. The carapace protects vital organs and provides attachment points for the limbs and muscles used in movement and feeding.

The abdomen is strongly reduced and tucked beneath the body, a defining feature that differentiates true crabs from other decapod crustaceans. Five pairs of legs extend from the underside of the body, with the front pair forming powerful claws used for manipulating food, capturing prey, and defence against predators.

In fossil specimens, the carapace outline and surface ornamentation are often the most clearly preserved features. Even partial preservation can display the distinctive shape and segmentation that allow identification as brachyuran crabs.

Geological Setting – Eocene Marine Deposits of Northern Egypt

During the Eocene epoch, much of northern Egypt was covered by a warm shallow sea connected to the early Mediterranean and Tethyan ocean systems. Marine sediments deposited during this time preserved a wide range of marine organisms including crustaceans, molluscs, echinoids, and fish.

The fossil-bearing sediments around the Cairo region consist primarily of marine limestones and marls that accumulated in calm offshore environments. Fine sediment settling on the seabed helped bury and preserve the remains of marine animals.

These deposits are well known for producing a variety of marine fossils and provide valuable insight into the biodiversity of Eocene marine ecosystems in North Africa.

Eocene Marine Ecosystems of the Tethyan Realm

The Eocene seas were characterised by warm climates and high biological diversity. The region that is now northern Egypt formed part of the extensive Tethyan marine realm, which supported abundant marine life.

Crabs were important members of these ecosystems, living along the seabed where they acted as both predators and scavengers. They likely fed on small molluscs, worms, organic debris, and other marine organisms.

These crustaceans played an important role in maintaining the balance of marine ecosystems, recycling organic matter and contributing to complex food webs that included fish, sharks, marine reptiles, and numerous invertebrates.

Authenticity and Collectability

• Genuine fossil crabs belonging to the infraorder Brachyura

• Eocene epoch, approximately 56–33.9 million years old

• Collected from the Cairo region, Egypt

• Rare prehistoric marine crustacean fossil

• The exact fossil shown in the photographs is the specimen you will receive

• Includes a Certificate of Authenticity lifetime guarantee generic card

Fossil crabs from Eocene deposits are highly valued by collectors due to their distinctive morphology and connection to ancient marine ecosystems. This rare specimen from Egypt represents a fascinating piece of Paleogene marine life and makes an excellent addition to any fossil collection, geological display, or natural history collection.

 

(Actual as seen)

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Description

Rare Fossil Crab Specimen from the Eocene of Egypt

This rare fossil crab belonging to the infraorder Brachyura originates from Eocene marine deposits near Cairo, Egypt. Dating to the Eocene epoch of the Paleogene Period, approximately 56–33.9 million years ago, this specimen represents part of the diverse crustacean fauna that inhabited the warm tropical seas covering northern Africa during the early Cenozoic.

The fossil is a carefully selected specimen preserved within its natural matrix, displaying the characteristic structure of ancient brachyuran crabs. The photographs show the exact fossil you will receive, allowing collectors to examine the preserved features and natural condition of the specimen. Please refer to the photographs for the full sizing and proportions. The fossil includes a Certificate of Authenticity lifetime guarantee generic card confirming the authenticity of the specimen.

About Brachyura – True Crabs in the Fossil Record

True crabs belong to the infraorder Brachyura within the order Decapoda, a diverse group of crustaceans that includes modern crabs, lobsters, shrimps, and prawns. Brachyuran crabs are distinguished by their broad, flattened carapace, reduced abdomen folded beneath the body, and strong chelae or claws adapted for feeding and defence.

Crabs first appeared in the fossil record during the Jurassic and became highly diverse by the Cretaceous and Paleogene periods. By the time of the Eocene epoch, brachyuran crabs had already radiated into numerous ecological niches, occupying shallow marine seabeds, reef environments, estuaries, and coastal habitats.

Although the exact species of this specimen cannot be determined with certainty, fossil crabs from Eocene deposits commonly represent members of several crab families adapted to warm shallow marine conditions.

Morphology and Anatomical Characteristics

Brachyuran crabs possess a distinctive body plan dominated by a wide protective carapace covering the cephalothorax. The carapace protects vital organs and provides attachment points for the limbs and muscles used in movement and feeding.

The abdomen is strongly reduced and tucked beneath the body, a defining feature that differentiates true crabs from other decapod crustaceans. Five pairs of legs extend from the underside of the body, with the front pair forming powerful claws used for manipulating food, capturing prey, and defence against predators.

In fossil specimens, the carapace outline and surface ornamentation are often the most clearly preserved features. Even partial preservation can display the distinctive shape and segmentation that allow identification as brachyuran crabs.

Geological Setting – Eocene Marine Deposits of Northern Egypt

During the Eocene epoch, much of northern Egypt was covered by a warm shallow sea connected to the early Mediterranean and Tethyan ocean systems. Marine sediments deposited during this time preserved a wide range of marine organisms including crustaceans, molluscs, echinoids, and fish.

The fossil-bearing sediments around the Cairo region consist primarily of marine limestones and marls that accumulated in calm offshore environments. Fine sediment settling on the seabed helped bury and preserve the remains of marine animals.

These deposits are well known for producing a variety of marine fossils and provide valuable insight into the biodiversity of Eocene marine ecosystems in North Africa.

Eocene Marine Ecosystems of the Tethyan Realm

The Eocene seas were characterised by warm climates and high biological diversity. The region that is now northern Egypt formed part of the extensive Tethyan marine realm, which supported abundant marine life.

Crabs were important members of these ecosystems, living along the seabed where they acted as both predators and scavengers. They likely fed on small molluscs, worms, organic debris, and other marine organisms.

These crustaceans played an important role in maintaining the balance of marine ecosystems, recycling organic matter and contributing to complex food webs that included fish, sharks, marine reptiles, and numerous invertebrates.

Authenticity and Collectability

• Genuine fossil crabs belonging to the infraorder Brachyura

• Eocene epoch, approximately 56–33.9 million years old

• Collected from the Cairo region, Egypt

• Rare prehistoric marine crustacean fossil

• The exact fossil shown in the photographs is the specimen you will receive

• Includes a Certificate of Authenticity lifetime guarantee generic card

Fossil crabs from Eocene deposits are highly valued by collectors due to their distinctive morphology and connection to ancient marine ecosystems. This rare specimen from Egypt represents a fascinating piece of Paleogene marine life and makes an excellent addition to any fossil collection, geological display, or natural history collection.

 

Additional information

Era

Eocene

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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