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Pliocene Fossil Pecten Scallop Shell Lillo Formation Antwerp Belgium Genuine Marine Fossil Specimen

£60.00

Genuine Pliocene Fossil Pecten Scallop Shell from Antwerp, Belgium

This authentic Pliocene fossil Pecten scallop shell originates from the well-known Lillo Formation in Antwerp, Belgium, a classic European fossil locality famous for its abundant marine fossils. The specimen represents a fossilised shell of a scallop belonging to the genus Pecten, a group of marine bivalve molluscs that inhabited shallow seas during the Neogene Period.

The fossil has been carefully selected for its preservation and natural shell structure, offering a clear representation of the distinctive fan-shaped morphology typical of scallop fossils. The listing photographs show the exact fossil specimen you will receive, allowing collectors to examine the fossil’s preservation, rib structure, and natural character before purchase. Full sizing can be viewed clearly in the listing images.

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

Fossil Identification and Taxonomic Classification

The fossil belongs to the genus Pecten, a group of marine bivalves within the scallop family that have existed for tens of millions of years and continue to be represented by modern scallop species.

Scientific classification includes:

  • Kingdom: Animalia
  • Phylum: Mollusca
  • Class: Bivalvia
  • Order: Pectinida
  • Superfamily: Pectinoidea
  • Family: Pectinidae
  • Genus: Pecten

Members of the Pectinidae family are easily recognised by their distinctive shell shape and radiating rib patterns. Fossil scallops are commonly preserved due to the relatively robust structure of their calcium carbonate shells.

Pecten species were active marine bivalves capable of swimming by rapidly opening and closing their shells, propelling themselves through the water using jet propulsion.

Geological Age and Stratigraphy

This fossil specimen dates to the Pliocene Epoch, a geological period within the Neogene Period, spanning approximately 5.33 to 2.58 million years ago. During this time, much of northwestern Europe was covered by shallow marine environments connected to the early North Sea basin.

The fossil specifically originates from the Lillo Formation, a well-documented sedimentary formation exposed in the Antwerp region. The formation is composed primarily of marine sands and shell-rich sediments, deposited in coastal marine environments.

The Lillo Formation contains a diverse assemblage of marine fossils, including:

  • Bivalves and scallops
  • Gastropods
  • Bryozoans
  • Marine vertebrate remains
  • Other molluscan fauna

These sediments provide important evidence of marine biodiversity during the later stages of the Neogene.

Shell Morphology and Fossil Characteristics

Pecten scallop shells possess a distinctive fan-shaped form with strong radial ribs extending outward from the hinge line. These ribs strengthen the shell while providing a characteristic appearance that makes scallops among the most recognisable fossil bivalves.

Typical morphological features include:

  • Broad fan-shaped shell outline
  • Prominent radial ribbing across the shell surface
  • Hinge line with symmetrical ear-like extensions known as auricles
  • Growth lines indicating stages of shell development

The shell structure consists primarily of calcium carbonate, originally secreted by the mollusc during life. Over millions of years, burial in sediment allowed the shell to fossilise while preserving much of its original shape and surface ornamentation.

Depositional Environment of the Lillo Formation

During the Pliocene Epoch, the Antwerp region formed part of a shallow marine shelf environment associated with the early North Sea basin. Rivers transported sediments into coastal waters, where shell beds accumulated on the seabed.

These environments typically consisted of:

  • Sandy marine seabeds
  • Coastal marine channels
  • Shallow offshore environments
  • Shell-rich sediment layers

The abundance of scallop shells in these deposits indicates that scallops were common inhabitants of the Pliocene seafloor, living in sandy substrates where they could filter-feed on plankton and organic particles suspended in the water.

Fossilisation Process

The preservation of scallop shells occurs when the shell becomes buried within sediment shortly after the organism dies. Layers of sand and sediment protect the shell from rapid erosion while groundwater carrying dissolved minerals gradually stabilises and preserves the fossil.

In many cases, fossil scallop shells from the Lillo Formation retain fine details such as ribbing, hinge structures, and growth lines, offering valuable information about the biology of the original organism.

Collecting and Scientific Interest

Pliocene scallop fossils from Antwerp are popular among fossil collectors due to their distinctive shell morphology and their association with a historically significant fossil locality. The Lillo Formation has long been studied by palaeontologists because of its rich marine fossil assemblage.

Collectors value Pecten fossils for several reasons:

  • Recognisable fan-shaped shell structure
  • Clear ribbed shell ornamentation
  • Well-documented geological locality
  • Connection to marine ecosystems of the Pliocene Epoch

Such fossils are commonly displayed in fossil collections, geological teaching sets, and natural history displays.

Authentic Fossil Specimen

This specimen is a genuine fossil Pecten scallop shell from the Lillo Formation in Antwerp, Belgium. It has been selected for its preservation and natural appearance.

Key features include:

  • Authentic Pliocene fossil scallop shell
  • Genus: Pecten
  • Family: Pectinidae
  • Formation: Lillo Formation
  • Age: Pliocene Epoch, Neogene Period
  • Locality: Antwerp, Belgium
  • Marine bivalve fossil specimen
  • Exact fossil shown in listing photographs
  • Full sizing visible in listing images
  • Includes Certificate of Authenticity lifetime guarantee generic card

This fossil provides a fascinating glimpse into ancient marine environments of the North Sea basin during the Pliocene, making it an excellent addition to fossil collections, educational displays, or natural history cabinets.

(Actual as seen)

Only 1 left in stock

SKU: P00226 Category:

Description

Genuine Pliocene Fossil Pecten Scallop Shell from Antwerp, Belgium

This authentic Pliocene fossil Pecten scallop shell originates from the well-known Lillo Formation in Antwerp, Belgium, a classic European fossil locality famous for its abundant marine fossils. The specimen represents a fossilised shell of a scallop belonging to the genus Pecten, a group of marine bivalve molluscs that inhabited shallow seas during the Neogene Period.

The fossil has been carefully selected for its preservation and natural shell structure, offering a clear representation of the distinctive fan-shaped morphology typical of scallop fossils. The listing photographs show the exact fossil specimen you will receive, allowing collectors to examine the fossil’s preservation, rib structure, and natural character before purchase. Full sizing can be viewed clearly in the listing images.

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

Fossil Identification and Taxonomic Classification

The fossil belongs to the genus Pecten, a group of marine bivalves within the scallop family that have existed for tens of millions of years and continue to be represented by modern scallop species.

Scientific classification includes:

  • Kingdom: Animalia
  • Phylum: Mollusca
  • Class: Bivalvia
  • Order: Pectinida
  • Superfamily: Pectinoidea
  • Family: Pectinidae
  • Genus: Pecten

Members of the Pectinidae family are easily recognised by their distinctive shell shape and radiating rib patterns. Fossil scallops are commonly preserved due to the relatively robust structure of their calcium carbonate shells.

Pecten species were active marine bivalves capable of swimming by rapidly opening and closing their shells, propelling themselves through the water using jet propulsion.

Geological Age and Stratigraphy

This fossil specimen dates to the Pliocene Epoch, a geological period within the Neogene Period, spanning approximately 5.33 to 2.58 million years ago. During this time, much of northwestern Europe was covered by shallow marine environments connected to the early North Sea basin.

The fossil specifically originates from the Lillo Formation, a well-documented sedimentary formation exposed in the Antwerp region. The formation is composed primarily of marine sands and shell-rich sediments, deposited in coastal marine environments.

The Lillo Formation contains a diverse assemblage of marine fossils, including:

  • Bivalves and scallops
  • Gastropods
  • Bryozoans
  • Marine vertebrate remains
  • Other molluscan fauna

These sediments provide important evidence of marine biodiversity during the later stages of the Neogene.

Shell Morphology and Fossil Characteristics

Pecten scallop shells possess a distinctive fan-shaped form with strong radial ribs extending outward from the hinge line. These ribs strengthen the shell while providing a characteristic appearance that makes scallops among the most recognisable fossil bivalves.

Typical morphological features include:

  • Broad fan-shaped shell outline
  • Prominent radial ribbing across the shell surface
  • Hinge line with symmetrical ear-like extensions known as auricles
  • Growth lines indicating stages of shell development

The shell structure consists primarily of calcium carbonate, originally secreted by the mollusc during life. Over millions of years, burial in sediment allowed the shell to fossilise while preserving much of its original shape and surface ornamentation.

Depositional Environment of the Lillo Formation

During the Pliocene Epoch, the Antwerp region formed part of a shallow marine shelf environment associated with the early North Sea basin. Rivers transported sediments into coastal waters, where shell beds accumulated on the seabed.

These environments typically consisted of:

  • Sandy marine seabeds
  • Coastal marine channels
  • Shallow offshore environments
  • Shell-rich sediment layers

The abundance of scallop shells in these deposits indicates that scallops were common inhabitants of the Pliocene seafloor, living in sandy substrates where they could filter-feed on plankton and organic particles suspended in the water.

Fossilisation Process

The preservation of scallop shells occurs when the shell becomes buried within sediment shortly after the organism dies. Layers of sand and sediment protect the shell from rapid erosion while groundwater carrying dissolved minerals gradually stabilises and preserves the fossil.

In many cases, fossil scallop shells from the Lillo Formation retain fine details such as ribbing, hinge structures, and growth lines, offering valuable information about the biology of the original organism.

Collecting and Scientific Interest

Pliocene scallop fossils from Antwerp are popular among fossil collectors due to their distinctive shell morphology and their association with a historically significant fossil locality. The Lillo Formation has long been studied by palaeontologists because of its rich marine fossil assemblage.

Collectors value Pecten fossils for several reasons:

  • Recognisable fan-shaped shell structure
  • Clear ribbed shell ornamentation
  • Well-documented geological locality
  • Connection to marine ecosystems of the Pliocene Epoch

Such fossils are commonly displayed in fossil collections, geological teaching sets, and natural history displays.

Authentic Fossil Specimen

This specimen is a genuine fossil Pecten scallop shell from the Lillo Formation in Antwerp, Belgium. It has been selected for its preservation and natural appearance.

Key features include:

  • Authentic Pliocene fossil scallop shell
  • Genus: Pecten
  • Family: Pectinidae
  • Formation: Lillo Formation
  • Age: Pliocene Epoch, Neogene Period
  • Locality: Antwerp, Belgium
  • Marine bivalve fossil specimen
  • Exact fossil shown in listing photographs
  • Full sizing visible in listing images
  • Includes Certificate of Authenticity lifetime guarantee generic card

This fossil provides a fascinating glimpse into ancient marine environments of the North Sea basin during the Pliocene, making it an excellent addition to fossil collections, educational displays, or natural history cabinets.

Additional information

Era

Pliocene

Pliocene Information

The Pliocene Epoch (5.3–2.58 million years ago) was a time of cooling climates, marking the transition to the Ice Ages of the Pleistocene. Grasslands and savannas expanded as forests shrank, driving the evolution of large grazing mammals like early horses, antelope, and elephants. The first modern mammals and birds became widespread, and early hominins, including Australopithecus, began walking upright in Africa. In the oceans, whales and seals thrived, while the Isthmus of Panama formed, connecting North and South America and altering ocean currents, which contributed to further global cooling. The Pliocene set the stage for both the Ice Ages and the eventual rise of modern humans.

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