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Fossil Pectin Shell – Eocene Epoch, Clallam Bay Washington USA, Genuine Bivalve Specimen
Fossil Pectin Shell – Eocene Epoch, Clallam Bay Washington USA, Genuine Bivalve Specimen - Image 2

Fossil Pectin Shell – Eocene Epoch, Clallam Bay Washington USA, Genuine Bivalve Specimen

£12.60

A well-preserved Fossil Pectin Shell (scallop) from the Eocene Epoch, approximately 40–50 million years old. This specimen was collected from the Clallam Formation near Clallam Bay, Washington State, USA, a site known for producing beautifully preserved marine invertebrate fossils from the early Paleogene period.

Pectin shells belong to the family Pectinidae, a group of marine bivalves distinguished by their fan-shaped, radially ribbed shells. This fossil showcases the elegant symmetry and surface ribbing typical of this family, preserved in fine-grained sediment.

Fossil Type: Bivalve (Scallop) Shell

Geological Age: Eocene – Ypresian to Lutetian Stages

Formation: Clallam Formation

Depositional Environment: The Clallam Formation was deposited in a shallow marine environment along a continental shelf. Calm conditions and fine silts contributed to the exceptional preservation of molluscs, echinoderms, and other invertebrates in the fossil record.

Morphological Features:

  • Distinct fan-shaped shell outline
  • Radiating ribs across the surface
  • Some specimens retain hinge or growth lines

Notable:

  • Classic marine invertebrate from the Eocene of the Pacific Northwest
  • Ideal for educational displays, fossil collectors, or palaeontology enthusiasts
  • The photograph shows the exact item offered for sale

Authenticity: All of our fossils are 100% genuine natural specimens and come with a Certificate of Authenticity. Please refer to the scale image for exact size – each square or cube equals 1cm.

 

This Eocene Pectin shell from Clallam Bay offers a glimpse into the marine ecosystems of ancient Washington. A beautiful and scientifically valuable specimen for any fossil enthusiast.

(Actual as seen)

Out of stock

SKU: UF3260 Category:

Description

A well-preserved Fossil Pectin Shell (scallop) from the Eocene Epoch, approximately 40–50 million years old. This specimen was collected from the Clallam Formation near Clallam Bay, Washington State, USA, a site known for producing beautifully preserved marine invertebrate fossils from the early Paleogene period.

Pectin shells belong to the family Pectinidae, a group of marine bivalves distinguished by their fan-shaped, radially ribbed shells. This fossil showcases the elegant symmetry and surface ribbing typical of this family, preserved in fine-grained sediment.

Fossil Type: Bivalve (Scallop) Shell

Geological Age: Eocene – Ypresian to Lutetian Stages

Formation: Clallam Formation

Depositional Environment: The Clallam Formation was deposited in a shallow marine environment along a continental shelf. Calm conditions and fine silts contributed to the exceptional preservation of molluscs, echinoderms, and other invertebrates in the fossil record.

Morphological Features:

  • Distinct fan-shaped shell outline
  • Radiating ribs across the surface
  • Some specimens retain hinge or growth lines

Notable:

  • Classic marine invertebrate from the Eocene of the Pacific Northwest
  • Ideal for educational displays, fossil collectors, or palaeontology enthusiasts
  • The photograph shows the exact item offered for sale

Authenticity: All of our fossils are 100% genuine natural specimens and come with a Certificate of Authenticity. Please refer to the scale image for exact size – each square or cube equals 1cm.

 

This Eocene Pectin shell from Clallam Bay offers a glimpse into the marine ecosystems of ancient Washington. A beautiful and scientifically valuable specimen for any fossil enthusiast.

Additional information

Era

Eocene
Origin

USA

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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