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Discohoplites subfalcatus Fossil Ammonite Upper Albian Cretaceous Morocco | Genuine Specimen with Certificate

£14.40

Offered here is a well-preserved Discohoplites subfalcatus ammonite fossil, originating from the Upper Albian Stage of the Cretaceous Period, found in the rich fossil beds of Morocco, North Africa. This rare and attractive ammonite specimen dates to approximately 105–100 million years ago, when much of what is now northern Africa was submerged beneath a warm, shallow epicontinental sea.

The specimen shown in the listing is the exact fossil you will receive, carefully chosen for its scientific interest and display quality. All ammonites are supplied with a Certificate of Authenticity.

Geological & Palaeontological Details:

  • Species: Discohoplites subfalcatus
  • Fossil Type: Ammonite
  • Family: Hoplitidae
  • Superfamily: Hoplitoidea
  • Order: Ammonitida
  • Geological Period: Cretaceous
  • Stage: Upper Albian (approx. 105–100 million years ago)
  • Location: Morocco
  • Biozone: Often found within the Upper Albian ammonite assemblage zones of the Tafilalt region, although exact zone attribution may vary by locality
  • Depositional Environment: Shallow marine shelf rich in calcareous and siliceous sediments, supporting a high diversity of invertebrates such as ammonites, bivalves, and crustaceans. Conditions favoured the preservation of calcitic shells and internal moulds.

Morphology & Features:

  • Discohoplites subfalcatus is recognised by its flattened, discoidal shell, with strong falcoid (sickle-shaped) ribbing and an involute coiling pattern
  • Whorls exhibit pronounced ornamentation with ribs that bend forward toward the venter (outer edge)
  • May feature subtle tubercles and a slightly keeled venter, typical of advanced hoplitid ammonites
  • The combination of compressed form and delicate ribbing creates a visually striking fossil, both scientifically important and aesthetically appealing

Notability: Discohoplites subfalcatus is a classic Upper Albian ammonite genus originally described by Spath (1923). It is part of a key lineage used in the biostratigraphic correlation of Albian marine sequences across Europe and North Africa. Fossils from Moroccan beds are well-preserved and often studied for their evolutionary significance in Late Albian cephalopod assemblages.

Additional Details:

  • All our fossils are 100% genuine specimens
  • Supplied with a Certificate of Authenticity
  • The photo shows the exact fossil for sale
  • Scale cube = 1cm – refer to photos for full sizing

Whether for scientific study, display, or collecting, this rare ammonite from Morocco offers a captivating glimpse into the ancient marine ecosystems of the Late Albian seas. A standout piece for any fossil collection.

(Actual as seen)

Out of stock

SKU: SF0202 Category:

Description

Offered here is a well-preserved Discohoplites subfalcatus ammonite fossil, originating from the Upper Albian Stage of the Cretaceous Period, found in the rich fossil beds of Morocco, North Africa. This rare and attractive ammonite specimen dates to approximately 105–100 million years ago, when much of what is now northern Africa was submerged beneath a warm, shallow epicontinental sea.

The specimen shown in the listing is the exact fossil you will receive, carefully chosen for its scientific interest and display quality. All ammonites are supplied with a Certificate of Authenticity.

Geological & Palaeontological Details:

  • Species: Discohoplites subfalcatus
  • Fossil Type: Ammonite
  • Family: Hoplitidae
  • Superfamily: Hoplitoidea
  • Order: Ammonitida
  • Geological Period: Cretaceous
  • Stage: Upper Albian (approx. 105–100 million years ago)
  • Location: Morocco
  • Biozone: Often found within the Upper Albian ammonite assemblage zones of the Tafilalt region, although exact zone attribution may vary by locality
  • Depositional Environment: Shallow marine shelf rich in calcareous and siliceous sediments, supporting a high diversity of invertebrates such as ammonites, bivalves, and crustaceans. Conditions favoured the preservation of calcitic shells and internal moulds.

Morphology & Features:

  • Discohoplites subfalcatus is recognised by its flattened, discoidal shell, with strong falcoid (sickle-shaped) ribbing and an involute coiling pattern
  • Whorls exhibit pronounced ornamentation with ribs that bend forward toward the venter (outer edge)
  • May feature subtle tubercles and a slightly keeled venter, typical of advanced hoplitid ammonites
  • The combination of compressed form and delicate ribbing creates a visually striking fossil, both scientifically important and aesthetically appealing

Notability: Discohoplites subfalcatus is a classic Upper Albian ammonite genus originally described by Spath (1923). It is part of a key lineage used in the biostratigraphic correlation of Albian marine sequences across Europe and North Africa. Fossils from Moroccan beds are well-preserved and often studied for their evolutionary significance in Late Albian cephalopod assemblages.

Additional Details:

  • All our fossils are 100% genuine specimens
  • Supplied with a Certificate of Authenticity
  • The photo shows the exact fossil for sale
  • Scale cube = 1cm – refer to photos for full sizing

Whether for scientific study, display, or collecting, this rare ammonite from Morocco offers a captivating glimpse into the ancient marine ecosystems of the Late Albian seas. A standout piece for any fossil collection.

Additional information

Era

Cretaceous

Origin

Morocco

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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