Tropaeum
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Tropaeum
''Tropaeum'' is an extinct genus of ammonites found throughout the oceans of the world during the Early Cretaceous. As with many other members of the family Ancyloceratidae, there was a trend among species within this genus to uncoil somewhat, in a very similar manner to the genus ''Lytoceras''. The largest species, ''T. imperator'' of Australia, had a shell a little over one meter in diameter. The name "Tropaeum" was applied by paleontologist James De Carle Sowerby, in 1837. References External links * photograph of the holotype A holotype is a single physical example (or illustration) of an organism, known to have been used when the species (or lower-ranked taxon) was formally described. It is either the single such physical example (or illustration) or one of several ... of ''T. imperator' Ammonitida genera Early Cretaceous ammonites Ammonites of Australia Ancyloceratoidea {{Ammonite-stub ...
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Ancyloceratidae
Ancyloceratidae is a family of heteromorphic Ammonitida, ammonites that lived during the Early Cretaceous. Their shells begin as a loose spiral with whorls not touching which then turns into a straight shaft that ends in a J-shape hook or bend at end. Coarse ribbing and spines are common. Ancyloceratidae is the type family for the Ancyloceratoidea and of the suborder Ancyloceratina. They are found in Lower Cretaceous, Barremian to perhaps Lower Albian sediments. Genera include: *''Ammonitoceras'' Dumas, 1876 *''Ancyloceras'' D'Orbigny, 1842 - type genus *''Ancylotropaeum'' Casey, 1980 *''Antarcticoceras'' Thomson, 1974 M.R.A. Thomson, « Ammonite faunas of the Lower Cretaceous of south-eastern Alexander Island », ''British Antarctic Survey Scientific Reports'', 80 (1974), p.1-44. *''Audouliceras'' Thomel, 1965 *''Australiceras'' Whitehouse, 1926 *''Caspianites'' Casey, 1961 *''Epancyloceras'' Spath, 1930 *''Epitroapeum'' Kakabadze, 1977 *''Helicancyloceras'' Klinger & Kennedy, ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ...
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James De Carle Sowerby
James De Carle Sowerby (5 June 1787 – 26 August 1871) was a British mineralogist, botanist, and illustrator. He received an education in chemistry. Sowerby was born in London, the son of botanical artist James Sowerby (1757–1822), and his wife, Anne de Carle (1764–1815). He continued his father's work and published, together with his brother George Brettingham Sowerby I, the latter volumes of the ''Mineral Conchology of Great Britain'', begun by their father. Together with a cousin, he founded the Royal Botanic Society and Gardens, and was its secretary for 30 years. His son William Sowerby was also a botanist and illustrator, and succeeded him as Secretary of the Royal Botanic Society in 1869. In 1846, John William Salter (English naturalist, geologist, palaeontologist, and leading authority on trilobites) married Sally, daughter of Sowerby, and eventually fathered seven children with her. Sowerby died in Kilburn, London in 1871. See also * Sowerby family Referen ...
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