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Beudanticeras subparandieri Fossil Ammonite | Lower Albian Cretaceous | Gault Clay Folkestone UK | Certified Authentic Specimen

£24.00

Presented here is a Beudanticeras subparandieri Fossil Ammonite, a beautifully preserved and scientifically significant example from the Lower Albian Stage of the Early Cretaceous, collected from the Gault Clay Formation in Folkestone, Kent, United Kingdom.

This fossil represents Beudanticeras subparandieri, a genus known for its compressed and involute shell with fine, flexuous ribbing and a smooth venter, typical of the Beudanticeratinae subfamily. The piece is a carefully selected specimen that showcases the distinctive characteristics of this rare ammonite.

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity.

The photograph shows the actual specimen you will receive, placed beside a 1cm scale cube for accurate sizing. Please refer to the image for full dimensions.

 

Geological and Taxonomic Information:

  • Species: Beudanticeras subparandieri
  • Fossil Type: Ammonite (extinct marine cephalopod)
  • Age: Early Cretaceous, Lower Albian Stage (~113 to 110 million years ago)
  • Locality: Folkestone, Kent, United Kingdom
  • Formation: Gault Clay Formation
  • Depositional Environment: Marine shelf setting, relatively deep, soft muds deposited under low-energy conditions
  • Biozone: Typically found within the Leymeriella tardefurcata or Douvilleiceras mammillatum ammonite zones
  • Geological Stage: Lower Albian

 

Taxonomic Classification:

  • Order: Ammonitida
  • Superfamily: Desmoceratoidea
  • Family: Desmoceratidae
  • Subfamily: Beudanticeratinae
  • Genus: Beudanticeras
  • Species: Beudanticeras subparandieri
  • Described By: Pervinquière, early 20th century

 

Morphology & Notable Features:

  • Compressed, involute shell with low umbilicus
  • Fine, weakly sinuous ribbing across the flanks
  • Smooth and rounded venter lacking prominent keels
  • Sutural pattern relatively simple for an ammonite of its age
  • Generally lacks tubercles or strong ornamentation
  • Often found preserved in dark claystone or iron-rich concretions

 

Scientific & Collector Significance:

Beudanticeras subparandieri is an excellent representative of the transitional faunas between more strongly ornamented mid-Cretaceous forms and smoother-shelled Late Cretaceous ammonites. Its presence within the Gault Clay provides valuable insights into the biostratigraphy and paleoenvironment of Lower Albian marine settings in southern England.

This particular specimen from Folkestone is especially prized due to the exceptional preservation conditions of the Gault Clay, making it a desirable addition for both amateur fossil enthusiasts and serious collectors.

 

Specimen Details:

  • Approximate Size: See photo with 1cm scale cube
  • Condition: Matrix-free or lightly matrix-backed, ideal for display
  • Locality: Folkestone, United Kingdom
  • Includes: Certificate of Authenticity

 

Ideal For:

  • Cretaceous ammonite enthusiasts
  • Educational and museum-quality collections
  • Geological teaching sets
  • Unique gifts for fossil lovers and natural history fans

 

(Actual as seen)

Only 1 left in stock

SKU: UF4391 Category:

Description

Presented here is a Beudanticeras subparandieri Fossil Ammonite, a beautifully preserved and scientifically significant example from the Lower Albian Stage of the Early Cretaceous, collected from the Gault Clay Formation in Folkestone, Kent, United Kingdom.

This fossil represents Beudanticeras subparandieri, a genus known for its compressed and involute shell with fine, flexuous ribbing and a smooth venter, typical of the Beudanticeratinae subfamily. The piece is a carefully selected specimen that showcases the distinctive characteristics of this rare ammonite.

All of our Fossils are 100% Genuine Specimens & come with a Certificate of Authenticity.

The photograph shows the actual specimen you will receive, placed beside a 1cm scale cube for accurate sizing. Please refer to the image for full dimensions.

 

Geological and Taxonomic Information:

  • Species: Beudanticeras subparandieri
  • Fossil Type: Ammonite (extinct marine cephalopod)
  • Age: Early Cretaceous, Lower Albian Stage (~113 to 110 million years ago)
  • Locality: Folkestone, Kent, United Kingdom
  • Formation: Gault Clay Formation
  • Depositional Environment: Marine shelf setting, relatively deep, soft muds deposited under low-energy conditions
  • Biozone: Typically found within the Leymeriella tardefurcata or Douvilleiceras mammillatum ammonite zones
  • Geological Stage: Lower Albian

 

Taxonomic Classification:

  • Order: Ammonitida
  • Superfamily: Desmoceratoidea
  • Family: Desmoceratidae
  • Subfamily: Beudanticeratinae
  • Genus: Beudanticeras
  • Species: Beudanticeras subparandieri
  • Described By: Pervinquière, early 20th century

 

Morphology & Notable Features:

  • Compressed, involute shell with low umbilicus
  • Fine, weakly sinuous ribbing across the flanks
  • Smooth and rounded venter lacking prominent keels
  • Sutural pattern relatively simple for an ammonite of its age
  • Generally lacks tubercles or strong ornamentation
  • Often found preserved in dark claystone or iron-rich concretions

 

Scientific & Collector Significance:

Beudanticeras subparandieri is an excellent representative of the transitional faunas between more strongly ornamented mid-Cretaceous forms and smoother-shelled Late Cretaceous ammonites. Its presence within the Gault Clay provides valuable insights into the biostratigraphy and paleoenvironment of Lower Albian marine settings in southern England.

This particular specimen from Folkestone is especially prized due to the exceptional preservation conditions of the Gault Clay, making it a desirable addition for both amateur fossil enthusiasts and serious collectors.

 

Specimen Details:

  • Approximate Size: See photo with 1cm scale cube
  • Condition: Matrix-free or lightly matrix-backed, ideal for display
  • Locality: Folkestone, United Kingdom
  • Includes: Certificate of Authenticity

 

Ideal For:

  • Cretaceous ammonite enthusiasts
  • Educational and museum-quality collections
  • Geological teaching sets
  • Unique gifts for fossil lovers and natural history fans

 

Additional information

Era

Cretaceous

Origin

United Kingdom

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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