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Fossil ammonite viewed under UV light, Desmoceras spp. upper early cretaceous, Albian stage, Mahajanga province, Madagascar
Ammonite fossil on beach, Charmouth, Jurassic Coast World Heritage Site, Dorset, England, November 2004
Fossil leaves of seed ferns, a kind of extinct plant, Joggins Fossil Cliffs UNESCO World Heritage Site, Bay of Fundy, Nova Scotia, Canada. May 2017
Limestone microfossils in a 0. 03mm-thick slice of fossil-rich limestone viewed at high magnificationLimestone microfossils in a 0.03mm-thick slice of fossil-rich limestone viewed at high magnification, image area is 3mm across in real life
Lithograph with later hand colouring combining two of Benjamin Waterhouse Hawkins six wall posters Waterhouse Hawkins Diagrams of the Extinct Animals produced for the Department of Science
Part of a submerged Holocene forest, revealed after a winter storm from beneath the sand at Hells Mouth (Porth Neigwl), Abersoch Wales, UK March 2014
Fossil ammonite, Cleoniceras spp. from upper early cretaceous period, Albian stage, Mahajanga province, Madagascar
Fossil ammonite viewed under UV light, Cleoniceras spp. from upper early cretaceous period, Albian stage, Mahajanga province, Madagascar
Fossil Ammonite, cross-section, Cleoniceras sp. from Upper Early Cretaceous period, Albian stage, Mahajanga province, Madagascar
Tetrapod tracks preserved in rock at the Joggins Fossil Cliffs UNESCO World Heritage Site, Bay of Fundy, Nova Scotia, Canada. May 2017
Tree-like lycopodiophyte (Sigillaria) preserved in situ at Joggins Fossil Cliffs UNESCO World Heritage Site along the shore, Bay of Fundy, Nova Scotia, Canada. May 2017
Fossil dinosaur {Struthiomimus altus} Royal Tyrrell Museum, Drumheller, Alberta, Canada
Theropod dinosaur tracks preserved in Lower Jurassic (200 million years old) rock. Near Tuba City, Arizona, USA
Fossilized remains of Lepidendron, the tallest of the coal age trees, at the Joggins Fossil Cliffs UNESCO World Heritage Site, Bay of Fundy, Nova Scotia, Canada. May 2017
Sectioned fossil ammonite where the shell material has been replaced by pyrites, and the empty cavities of the shell have filled during fossilisation with crystalised yellow/green calcite preserving