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Beetle in amber
Weevil in amberA weevil beetle preserved in Dominican amber. This specimen originates from the Lower Miocene period
Zygolophodon atticus, mastodonFront view of a skull of an extinct elephant from the Miocene of Pikermi, Greece. This fossil gave rise to the myth of the one-eyed giant, Cyclops
Megazostrodon skullSpecimen from the Late Triassic to Early Jurassic of Lesotho, Africa. Megazostrodon was thought to be a small, mouse-sized, nocturnal mammal and fed on insects
Dalmanites myops, trilobiteA Silurian fossil trilobite from the Wenlock Limestone, Dudley, Worcestershire. This specimen measures 40mm head to tail
Palaeoniscus freislebeni, fossil fishPalaeoniscus freislebeni a fossil fish from the Permian rocks near Midderidge, Durham
Fungus gnat in amberFungus gnat, about 2mm in length, in Eocene Baltic amber about 40 million years old
Isochirotherium footprintA cast of fossil footprints, measuring 38 cms long, from both hind feet of Isochirotherium herculis, an extinct reptile, discovered in Tarporley, Cheshire
Rhynchosaurus footprintsFossil footprints made by Rhynchosaurus on a slab of Triassic, Keuper Sandstone from a quarry in Rathbone Street, Liverpool. Dimensions of slab are 5 inches x 6 inches
Bronze Age necklace made of PorosphaeraThe fossil sponge Porosphaera can be found within Britains Cretaceous chalk. This necklace of 79 Porosphaera specimens was found around the neck of a skeleton dating back 4
Troodon toothA fossil tooth specimen that once belonged to the dinosaur, Troodon. It was a carnivorous dinosaur that lived around 65 million years ago
Lithostrotion, coralShown here is a Carboniferous coral. Corals comprise a soft bodied animal called a polyp. Each polyp inhabits a calcareous skeleton called a corallum
Lonsdaleia, coralShown here is the Carboniferous coral, Lonsdaleia. Corals comprise a soft bodied animal called a polyp. Each polyp inhabits a calcareous skeleton called a corallum
Jurassic BritainAn artists impression of Jurassic (206 to 144 million years ago) Britain from space, with forested swamps and warm seas
SlateCambrian slate from North Wales. Slate is metamorphosed shale
CheirotheriumArid desert of Triassic Britain with imagined reconstructions of Cheirotherium ( hand-beast ), a labyrinthodont reptile, whose prints are common in Triassic rocks but no remains have been found
Didymograptus, graptoliteDidymograptus, Ordovician tuning-fork planktonic graptolites. Graptolites are an extinct group of marine, colonial animals
Hyolithes, primitive molluscShown here is Hyolithes, a Cambrian primitive mollusc. Hyolithes had an oval or cone-shaped, elongated shell and often occured in clusters along bedding planes of Cambrian shale
Dictyonema, graptoliteShown here is Dictyonema, a Cambrian dendroid graptolite. Graptolites are the fossil remains of small colonial animals. Graptolite colonies were connected together by living tissue
Quartzite
Protobarinophyton obrutscheviiThe fossilised leafless stems of Protobarinophyton obrutschevii topped by a cone-like array of sopre sacs. Approximately 3 mm wide
Rhynia major, fossilised plantA complete soft tissue preservation at the cellular level in Rhynia major. Transverse section through stem, approximately 2mm in diameter. From Rhynie Chert, Scotland, Early Devonian
Bothrodendron minutifoliu, fossil clubmossShown here is a fossilised leafy twig of a clubmoss originating from Carboniferous rocks near Barnsley, England
Ammonite selectionThree ammonites as follows: (Left to right) Oistoceras wrighti; Asteroceras obtusum (zonal index species); Tragophylloceras loscombi all specimens originate from the Jurassic rocks near Lyme Regis
Athleta luctator, fossil sea snailA fossil sea snail (Athleta luctator) dating from the late Eocene rocks around Barton, England
Sigillaria rugosa, fossil club mossThis section of a club moss trunk displays leaf scars where leaves grew straight out from. Club mosses could grow up to heights of 30 metres
Fossil branches of CalamitesThe fossil branches of Calamites sp. bearing leaves and cones; Palaeostachya and Asterophyllites. Specimen discovered in Wales, dating back to the Late Carboniferous period
Coal, from the late carboniferousCoal is formed from fossil plants. The regular pattern on the surface of this 14 cm long piece is the impression of the bark of a fossil tree; Lepidodendron
Lepidotes, fossil fish
Pentacrinites, crinoidPentacrinites is a fossil crinoid from the Jurassic. Crinoids are ancient, marine organisms. The majority have long stalks anchored to the bottom
Sigillaria rugosa, fossil plantShown here is a section of the stem of a 300 million year old Carboniferous plant, probably abundant in the Carboniferous swamplands. The stem or trunk is the most common part to be fossilised
Cupressinoxylon, fossil woodComposite photomicrograph showing transverse (left), tangential (centre) and radial (right) sections through fossil wood; Cupressinoxylon from the London Clay at Ashford, Kent, England
Asteroceras obtusum, ammoniteShown here is a Jurassic ammonite. Ammonites are an extinct group of fossil cephalopods related to todays Nautilus
Trigona, bivalvesShown here are a pair of Jurassic bivalves. Bivalves are shelled creatures and first appeared in the Middle Cambrian and are still common in todays seas and oceans
Coal forest
Ordovician seascapeAn artists impression of the Eden Valley, Cumbria in the Ordovician period (490 to 443 million years ago), with volcanoes in the sea
Dapedium orbicularis, fossil fishA well preseved example of an enamel-scaled fish from the Lower Lias, Lyme Regis, Dorset, England
Pleistocene landscapeAn artists impression of the Eden Valley, Cumbria during the Pleistocene epoch which occurred between 1.8 million years ago to 10, 000 years ago
Asteroceras marstonensis and Promicroceras, ammonites