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Cut and polished ammonite pairs, collected from Madagascar. Ammonites are one of the most distinctive and popular fossils in the world due to their distinctive spiral shell. These specimens are examples of their shells that have been cut and polished in order to show their inner workings. These specimens include both Desmoceras and Cleoniceras which both lived during the Lower Cretaceous period, approximately 110 – 102 million years ago. Each section measures approximately 3cm and come packaged as a pair in a polythene bag with information label.
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Cut and polished ammonite pairs, collected from Madagascar. Ammonites are one of the most distinctive and popular fossils in the world due to their distinctive spiral shell. These specimens are examples of their shells that have been cut and polished in order to show their inner workings. These specimens include both Desmoceras and Cleoniceras which both lived during the Lower Cretaceous period, approximately 110 – 102 million years ago. Each section measures approximately 3cm and come packaged as a pair in a polythene bag with information label.
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A fossil specimen of the fossil rugose coral phillipsastrea ananas found in Ramlia, Southern Morocco. The specimen is from the Devonian period and is approximately 350/360 m years old.
Species Name: Bos primigenius
Geological Age: 10,000. Pleistocene period
Location: North Sea Bed, Holland
Body Part: Ankle Bone
Good quality horn corals. Size approx 1.5″ to 2″ in length.
• Geological Age: Pennsylvanian stage, late Carboniferous period, 323 to 298 million years old
• Location: Indiana and Oklahoma, USA
• Family: Echinoderm
• Class: Blastoidea
• Species: Pentremites sp.
Pentremites sp. blastoid collected from Pennsylvanian sediments in Indiana or Oklahoma, USA. Pentremites belong to the class Blastoidea and they are a type of echinoderm. These specimens measure approximately 2 cm in diameter.
A genuine fossilised fragment of a dinosaur egg shell, discovered in Patagonia, Argentina. It has been dated to approximately 70-90 Million years ago, comes supplied in a perspex box with a detailed info label and 10x magnifying hand lens.
10 in stock
• Geological Age: Devonian period, Old red sandstone, Sandwick beds
• Location: Orkney Islands, Scotland
• Family: Osteolepidae
• Species: Osteolepis macrolepidotus
1 in stock
A colonial coral which lived in warm shallow waters and is common in the limestone rocks of the Silurian period. Heliolites is often associated with other corals that formed small reefs.
Out of stock
Species Name: Leptaena depressa
Family: Brachiopod
Age: Silurian, Wenlock Series
Location: Dudley, West Midlands, UK
Isastrea fossil coral of Jurassic age, collected from Steeple Ashton, Wiltshire, UK. Isastrea is an extinct species of Scleractinian coral which existed in the Jurassic and Cretaceous periods. These reef building corals had a symbiotic relationship with photosynthetic algae and so lived in in shallow, warm, clear marine waters. These specimens measure approximately 3″ in size and come in a white card tray with an information label.
7 in stock
A colonial coral which lived in warm shallow waters and is common in the limestone rocks of the Silurian period. Favosites is often associated with other corals that formed small reefs. Favosites specimens have a honeycomb appearance when viewed from above.
Leptopius duponti fossil weevil cacoons from the Holocene period found in Elliston, south Australia. Known informally as pixie clogs, the cacoons were spun by the weevils in their pupae stage in order to protect them during metamorphosis into adult beetles. An interesting piece for fossil collectors or educational use to exhibit an example of a ‘trace fossil’, the cacoons are approximately 50 mm in length and 30 mm in diameter and come supplied in a card tray with a label.
25 in stock
Flexycalymene trilobite fossils, (syn: diacalymene) are a well known extinct species which lived during the Ordovician period, 449 to 443 million years ago and were found in Erfoud, Morocco. These samples exhibit quite clear morphological features such as the pygidium, cephalon and thorax as well as the shape and segments as expected. They appear to have a rusty, limonotic colouration which is due to iron oxide staining in the beds the fossils were found in. Available in various sizes and come supplied in a tray with a label.
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