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Liostrea delta are an extinct species of bivalve belonging to the oyster family which lived during the Jurassic period between 199 to 145 million years ago. These fossil specimens were found in the Kimmeridge clay beds in Weymouth in Dorset, they measure 13 x 10 cm in size on average and as expected, have a fairly flat profile. As suggested from the species name, they lived in brackish delta environments and look very similar to modern days fauna. They are excellent fossils specimens which have been clenaed of matrix so that growth lines can easily be seen, supplied in a a card tray with an information label.
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• Geological Age: Jurassic period, Lower Lias, 200 to 174 million years ago.
• Location: Hook Cliff, Gloucestershire, Yorkshire, UK.
• Family: Bivalve
• Species: Gryphaea arcuata
Gryphea Arcuata are a common bivalve fossil and as such, these specimens are often used for educational purposes. These study grade samples come from Hook Cliff in Yorkshire and are roughly 4 to 5 cm in length, found in Jurassic strata, they are 200 to 174 million years old and are of a lower quality than our A Grade material, thus making them more cost effective for schools and educational bodies to purchase, showing such morphological features as growth lines and hinges, the specimens are between 4 to 5 cm in length and come supplied in a card tray with a label.
A sample of three Gryphaea Arcuata that were found joined together. An ideal specimen for teaching use.
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Fossil name: Exogyra Conica
Fossil type: Bivalve
Geological Age: Cretacious period, upper greensand
Fossil Location: Niton, Isle of White
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Large Bivalves specimens of Cardita Planicostata on a fine grained shelly conglomeritic matrix. Approximate diameter, 7 cm.
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• Geological Age: Jurassic period, Lower Lias, 200 to 174 million years ago.
• Location: Hook Cliff, Gloucestershire, Yorkshire, UK.
• Family: Bivalve
• Species: Gryphaea arcuata
Gryphea Arcuata are a common bivalve fossil and as such, these specimens are often used for educational purposes. These samples come from Hook Cliff in Yorkshire and are roughly 6 cm in length, found in Jurassic strata, they are 200 to 174 million years old and are of high quality, showing such morphological features as growth lines, hinges and more. A dull grey colour, they are suitable for collectors as well of fine quality specimens.
• Geological Age: Pleistocene period, 2,588,000 to 11,700 years ago.
• Location: Red Crag, Walton on Naze, UK.
• Family: Bivalve
• Species: Glycymeris glycymeris
Glycymeris Glycymeris fossil bivalve specimens, these shells, although tarnished yellow still show growth lines, hinges and more, they were excavated from the Red Crag formation in Walton on Naze, UK and are excellent Pleistocene fossil samples for those with an interest in more recent fauna. Shells are approximately 4 to 5 cm in size and come supplied in a card tray with a label.
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• Geological Age: Jurassic period, Lower Lias, Ibex zone, 200 to 145 million years ago.
• Location: Blockley Quarry, Near, Moreton, Gloucestershire, UK
• Family: Bivalve
• Species: Mactromya Cardioides
Mactroymya bivalve fossil specimens dated from the Lower Lias of the Jurassic period over 200 million years old, these B grade samples from Blockley quarry in Gloucestershire are lower quality, still showing morphologicla features, but will exhibit broken parts and discolouration, available in two sizes, supplied in a tray with a label.
Fossil name: Panopea Gurgitis
Fossil type: Bivalve
Geological Age: Cretacious period, Lower greensand
Fossil Location: Atherfield, Isle of White
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Specimen: Modiolus Hillianus
Geological Age: Jurassic, Ibex Zone, Lower Lias
Location: Blockley, Gloucestershire, UK.
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