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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.
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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.
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• Geological Age: Silurian period, 443 to 416 millions years old
• Location: Djebel Issoumour, Alnif, Morocco
• Family: Echinoderm
• Species: Crinoid
Moroccan fossil crinoid stem specimens supplied in packets of 5 pieces, dated to over 400 million years old, they lived during the Silurian period and show excellent clear morphological details such as stem segments. Ideal for educational use and young collectors.
Specimens of Thecosmilia annularis from the Jurassic period, Corallian beds. The specimens were found at Steeple Ashton, Wiltshire, U.K. Specimens are available in a range of sizes and are supplied with a card tray and a information label.
A chain coral which lived in warm shallow waters and is common in the limestone rocks of the Silurian period. Halysites is often associated with other corals that formed small reefs. Specimens come in various sizes in a white card tray with an information label.
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
Perisphinctes are an extinct species of ammonite which lived during the lower Jurassic period, 163 to 145 million years ago. The animal could grown from anywhere between 10 mm to over a meter in diameter, making them among the largest of the ammonites. Their shells exhibit excellent morphological features such as clear, distinct ribbing and occasionally, well defined ammonitic suture lines, among the near perfect coil shape, it could be said that perisphinctes are the text book ammonite. These specimens are 1.5″ – 2″ in size and come supplied in a white card tray with information label.
45 in stock
Specimen: Horn Coral
Geological Age: Silurian, Wenlock Series
Location: Shropshire, UK
• 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.
Fossil specimens of the solitary coral Calceola. The coral is from the Devonian period (lower – middle) and was found in the Western Sahara. The specimens are supplied in a small card tray with an information label. Specimens come in multiple sizes, in a white card tray with an information label.
Ogyginus comdensis was a species of asaphid trilobites from the Ordovician period, and found in abundance in Wales. They were characterised by their squat, rounded bodies. These specimens are preserved within a mud stone matrix, some of which has been polished, but all of which has been cut to display the fossils in their entirety. A perfect specimen for analysis of different orders of trilobite if purchased along side a more common variation, these fossils could also be used as a display piece. All fossils are provided with a white card tray and information label.
Available in the folowing sizes:
These sizes refer to the length of the trilobite, not the matrix they are contained in. Matrix size varies between specimens.
Specimens of Dinosaur Bone, collected from Abingdon, Oxfordshire in the UK. These samples are from an unidentified species, however they date to approximately 157 – 152 Ma. This puts these samples in the Kimmeridgian stage of the Jurassic period, which is the apex of the dinosaur’s rule on Earth. The specimens display a rusty brown colouration and showcase their porous bone structure. The pieces are from undetermined body parts and could be remnants from various parts of the animal. These samples are available in various sizes and come supplied in a white card tray with an information label.
Fossil twigs, collected from Madagascar. These twigs are Triassic in age and come supplied in packs of 5 pieces. Packaged in a polythene bag with an information label.
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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