Fossils for Sale - High-quality BRITISH and WORLDWIDE Fossils. An impressive selection of fossils, including Ammonites, Trilobites, Belemnites, Fossil Fish, Fossil Shark Teeth, Fossilised Insects in Amber, Dinosaurs, and Reptiles. UK Fossils was formed in 1988 and collects and preps our own fossils in the heart of the Jurassic Coast, collecting fossils from Lyme Regis, Charmouth and Somerset. Our passion for fossils is reflected in our carefully curated collection, which includes some of the rarest and most unique specimens available.

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Procerozigzag crassizigzag Ammonite Fossil | Lower Callovian, Jurassic | Ashton Keynes UK | Alice Purnell Collection

£60.00

Fossil Type & Species:

This listing features a genuine ammonite fossil of Procerozigzag crassizigzag, a rare and highly detailed species from the Lower Callovian Stage of the Jurassic Period. Collected from the historically significant locality of Ashton Keynes, Wiltshire, United Kingdom, this fossil is part of the esteemed Alice Purnell Collection, ensuring both authenticity and excellent preservation.

Geological Formation & Insight:

Procerozigzag belongs to the zigzag-patterned ammonite groups of the Jurassic, known for their distinctive, often coarse ribbing and strongly involute shell forms. The species crassizigzag is particularly notable for its thickened ribbing and precise stratigraphic placement within the Lower Callovian.

These ammonites were nektonic marine cephalopods, active swimmers in shallow Jurassic seas that covered much of Europe during the Middle Jurassic (~166–163 million years ago). The fossil-bearing strata in Ashton Keynes are part of the Oxford Clay Formation, one of Britain’s most productive marine fossil units.

The fine clays and silts of the Oxford Clay formed in low-energy, offshore marine environments, which helped preserve delicate features of ammonite shells — such as suture lines and ribbing — in remarkable detail.

Item Specifics:

  • Fossil Type: Ammonite
  • Species: Procerozigzag crassizigzag
  • Geological Age: Lower Callovian, Middle Jurassic (~166–163 million years ago)
  • Formation: Oxford Clay Formation
  • Locality: Ashton Keynes, Wiltshire, United Kingdom
  • Provenance: From the Alice Purnell Collection
  • Preservation: Excellent – clear ribbing and shell coiling detail
  • Colour: Typically grey-brown fossil in contrasting natural matrix
  • Size: See photo – scale rule/cube = 1cm
  • Condition: 100% natural, unrestored
  • Specimen: You will receive the exact item shown in the photograph

Authenticity Guarantee:

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity. This ammonite fossil comes from the respected Alice Purnell Collection, offering traceable provenance and professional curation.

Shipping & Packaging:

Your fossil will be securely packaged and shipped with full tracking. A rare and scientifically valuable addition for collectors, educators, or as a timeless natural history gift.

Thank you for visiting our shop — explore more rare and authentic fossils, minerals, and crystals in our full collection!

(Actual as seen)

Out of stock

SKU: AF2063 Category:

Description

Fossil Type & Species:

This listing features a genuine ammonite fossil of Procerozigzag crassizigzag, a rare and highly detailed species from the Lower Callovian Stage of the Jurassic Period. Collected from the historically significant locality of Ashton Keynes, Wiltshire, United Kingdom, this fossil is part of the esteemed Alice Purnell Collection, ensuring both authenticity and excellent preservation.

Geological Formation & Insight:

Procerozigzag belongs to the zigzag-patterned ammonite groups of the Jurassic, known for their distinctive, often coarse ribbing and strongly involute shell forms. The species crassizigzag is particularly notable for its thickened ribbing and precise stratigraphic placement within the Lower Callovian.

These ammonites were nektonic marine cephalopods, active swimmers in shallow Jurassic seas that covered much of Europe during the Middle Jurassic (~166–163 million years ago). The fossil-bearing strata in Ashton Keynes are part of the Oxford Clay Formation, one of Britain’s most productive marine fossil units.

The fine clays and silts of the Oxford Clay formed in low-energy, offshore marine environments, which helped preserve delicate features of ammonite shells — such as suture lines and ribbing — in remarkable detail.

Item Specifics:

  • Fossil Type: Ammonite
  • Species: Procerozigzag crassizigzag
  • Geological Age: Lower Callovian, Middle Jurassic (~166–163 million years ago)
  • Formation: Oxford Clay Formation
  • Locality: Ashton Keynes, Wiltshire, United Kingdom
  • Provenance: From the Alice Purnell Collection
  • Preservation: Excellent – clear ribbing and shell coiling detail
  • Colour: Typically grey-brown fossil in contrasting natural matrix
  • Size: See photo – scale rule/cube = 1cm
  • Condition: 100% natural, unrestored
  • Specimen: You will receive the exact item shown in the photograph

Authenticity Guarantee:

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity. This ammonite fossil comes from the respected Alice Purnell Collection, offering traceable provenance and professional curation.

Shipping & Packaging:

Your fossil will be securely packaged and shipped with full tracking. A rare and scientifically valuable addition for collectors, educators, or as a timeless natural history gift.

Thank you for visiting our shop — explore more rare and authentic fossils, minerals, and crystals in our full collection!

Additional information

Era

Jurassic

Origin

United Kingdom

Jurassic Information

The Jurassic Period (201–145 million years ago) was the golden age of dinosaurs, with iconic species like Brachiosaurus, Stegosaurus, and Allosaurus dominating the land. It was a time of warm, humid climates, with high sea levels that created vast shallow seas, supporting abundant marine reptiles, ammonites, and early coral reefs. The first birds, such as Archaeopteryx, evolved from small theropod dinosaurs, while early mammals remained small and nocturnal. Lush forests of cycads, conifers, and ferns covered the land, providing food for giant herbivores. The breakup of the supercontinent Pangaea accelerated, shaping Earth's geography and setting the stage for the diverse ecosystems of the Cretaceous.

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