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Coelodus
''Coelodus'' is an extinct genus of fish in the family Pycnodontidae from the Late Jurassic to early Paleocene (Danian). Fossils of the genus have been found in:''Coelodus'' at .org ;Jurassic * Gardies, France ;Cretaceous * , Argentina * , Bolivia * [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yacoraite Formation
The Yacoraite Formation is a largely Mesozoic geologic formation. The deposits of this formation mainly date from the Maastrichtian of the Upper Cretaceous, but the Cretaceous–Paleogene boundary (K–T boundary) runs right through this formation near its top, and the uppermost parts are consequently from the Danian (Lower Paleocene). It was probably deposited around the intertidal zone, as the sedimentary rocks of this formation alternate according to sea level changes between deposits of muddy beaches and of shallow ocean.Marquillas ''et al.'' (2003) Fossil content Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel ''et al.'' (2004: pp.517-607) Well-preserved dinosaur footprints assigned to '' Hadrosaurichnus australis'' have been found in this formation, as were fossil eggs, stromatolites and the Mesozoic palynomorph '' Aquilapollenites''. Other fossils recovered from the formation are: * '' Pucapristis branisi''Leonardi, 199 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
El Molino Formation
The El Molino Formation is a Maastrichtian geologic formation pertaining to the Puca Group of central Bolivia. The formation comprises fine-grained sandstones and sandy limestones with stromatolites deposited in a shallow marine to lacustrine environment. The formation has provided fossils of '' Dolichochampsa minima'',Buffetaut, 1987 and ichnofossils of Ankylosauria indet., Ornithopoda indet., Theropoda indet. and Titanosauridae indet.Lockley et al., 2002, p.389 The tracksite of Cal Orcko is the best known example of the ichnofossil locations of the formation. The ichnofossil of '' Ligabueichnum bolivianum'' may be attributed to an ankylosaur.Leonardi, 1994, p.39 The fossil fish species ''Dasyatis molinoensis'' is named after the formation. Fossil content Other fossils retrieved from the formation are: [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pycnodontiformes Genera
Pycnodontiformes is an extinct order of primarily marine bony fish. The group first appeared during the Late Triassic and disappeared during the Eocene. The group has been found in rock formations in Africa, Asia, Europe, North and South America. They were small to middle-sized fish, generally with laterally-compressed deep bodies, some with almost circular outlines, adapted for manuverability in reef-like environments. The group was morphologically diverse containing forms such the very short but deep Gebrayelichthyidae and the horned ''Ichthyoceros,'' both from the early Late Cretaceous of Lebanon. Most, but not all members of the groups had jaws with round and flattened teeth, well adapted to crush food items (durophagy), such as echinoderms, crustaceans and molluscs. Some pyncodontiformes developed piranha like teeth used for eating flesh. Most species inhabited shallow marine reef environments, while a handful of species lived in freshwater or brackish conditions. While rare ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pycnodontiformes
Pycnodontiformes is an extinct order of primarily marine bony fish. The group first appeared during the Late Triassic and disappeared during the Eocene. The group has been found in rock formations in Africa, Asia, Europe, North and South America. They were small to middle-sized fish, generally with laterally-compressed deep bodies, some with almost circular outlines, adapted for manuverability in reef-like environments. The group was morphologically diverse containing forms such the very short but deep Gebrayelichthyidae and the horned ''Ichthyoceros,'' both from the early Late Cretaceous of Lebanon. Most, but not all members of the groups had jaws with round and flattened teeth, well adapted to crush food items (durophagy), such as echinoderms, crustaceans and molluscs. Some pyncodontiformes developed piranha like teeth used for eating flesh. Most species inhabited shallow marine reef environments, while a handful of species lived in freshwater or brackish conditions. While rare ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pycnodontidae
Pycnodontidae is an extinct family of ray-finned fishes, ranging from the Triassic period until the Eocene. Genera * '' Acrotemnus'' Agassiz, 1843 * '' Anomoeodus'' Forir, 1887 * ''Athrodon'' Sauvage, 1880 * '' Callodus'' Thurmond, 1974 * ''Coccodus'' * '' Coelodus'' Haeckel * ''Gyrodus'' Agassiz, 1843 * '' Iemanja'' Wenz, 1989 * '' Macromesodon'' Blake, 1905 * '' Microdus'' * '' Micropycnodon'' Hibbard and Graffham, 1945 * '' Neoproscinetes'' De Figueiredo and Silva Santos, 1990 * '' Nonaphalagodus'' Thurmond, 1974 * '' Omphalodus'' von Meyer, 1847 * '' Paleobalistum'' * ''Paramicrodon'' Thurmond, 1974 * '' Polypsephis'' Hay, 1899 * ''Proscinetes'' Gistl, 1848 * '' Pycnodus'' Agassiz, 1835 * '' Pycnomicrodon'' Hibbard and Graffham, 1941 * '' Scalacurvichthys'' Cawley and Kriwet, 2017 * '' Sphaerodus'' Agassiz, 1843 * ''Stemmatodus ''Stemmatodus'' is an extinct genus of prehistoric ray-finned fish that lived in Europe during the Early Cretaceous approximately 129 to 125 milli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunbridge Wells Sand Formation
The Tunbridge Wells Sand Formation is a geological unit which forms part of the Wealden Group and the uppermost and youngest part of the unofficial Hastings Beds. These geological units make up the core of the geology of the Weald in the English counties of West Sussex, East Sussex and Kent. The other component formations of the Hastings Beds are the underlying Wadhurst Clay Formation and the Ashdown Formation. The Hastings Beds in turn form part of the Wealden Group which underlies much of southeast England. The sediments of the Weald, including the Tunbridge Wells Sand Formation, were deposited during the Early Cretaceous Period, which lasted for approximately 40 million years from 140 to 100 million years ago. The Tunbridge Wells Sands are of Late Valanginian age.Hopson, P.M., Wilkinson, I.P. and Woods, M.A. (2010) ''A stratigraphical framework for the Lower Cretaceous of England''. Research Report RR/08/03. British Geological Survey, Keyworth. The Formation takes its name f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Huérguina Formation
The La Huérguina Formation (also known as the Calizas de La Huérguina Formation, La Huérguina Limestone Formation or as the Una Formation) is a geological formation in Spain whose strata date back to the Barremian stage of the Early Cretaceous.Martínez et al., 2017 Las Hoyas is a Konservat-Lagerstätte within the formation, located near the city of Cuenca, Spain. The site is mostly known for its exquisitely preserved dinosaurs, especially enantiornithines.Weishampel et al., 2004, pp.556-563 The lithology of the formation mostly consists of lacustarine limestone deposited in a freshwater wetland environment. Las Hoyas Taphonomy As a Konservat-Lagerstätten, the preservation is exceptional. This may be a result of three factors: Microbial mats, Obruption and Stagnation. Microbial mats may be responsible for the preservation of soft tissue in many fossils from Las Hoyas, like ''Pelecanimimus''' crest. The iron carbonate depositions, a result from bacterial metabolism whic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cabana Formation
Cabana, cabanas or cabañas may refer to: *Cabana (structure), either a small hut built with a thatched roof, or a recreational structure with at least one wall open at a beachside or poolside club Places * Cabana, Peru, capital of the Cabana District in Ancash, Peru * Cabanas, Galicia, a municipality in A Coruña, Galicia, Spain * Cabanas, Girona, a municipality in Alt Empordà, Girona, Catalonia, Spain * Cabañas, Cuba, a town in Artemisa Province of Cuba * Cabañas, Copán, a municipality in Honduras * Cabañas, La Paz, a municipality in Honduras * Cabañas, Zacapa, Guatemala * Cabana de Bergantiños, Galicia, Spain * Cabana District (Ancash), Pallasca Province, Ancash Region, Peru * Cabanas de Tavira, a town in Algarve, Portugal * Cabanas de Torres, a freguesia in Alenquer, Portugal * Cabanas de Viriato, a town in Portugal * Cabañas Department, El Salvador * Cabanas Island, Portugal; see List of islands of Portugal * Las Cabañas de Castilla, Spain * Cabana (ancient la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pierre Shale
The Pierre Shale is a geologic formation or series in the Upper Cretaceous which occurs east of the Rocky Mountains in the Great Plains, from Pembina Valley in Canada to New Mexico. The Pierre Shale was described by Meek and Hayden in 1862 in the Proceedings of the Academy of Sciences (Philadelphia). They described it as a dark-gray shale, fossiliferous, with veins and seams of gypsum, and concretions of iron oxide. The Pierre Shale is about 700 feet (210m) thick at the type locality. It overlies the Niobrara division and underlies the Fox Hills beds. It was named for an occurrence near Fort Pierre on the Missouri River in South Dakota. The Pierre Shale is of marine origin and was deposited in the Western Interior Seaway. It is correlative with other marine shales that occur farther west, such as the Bearpaw Shale, Mancos Shale and the Lewis Shale. It correlates with the Lea Park Formation in central Alberta. The Pierre is overlain by marginal marine deposits of the Fox H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Twin Mountains Formation
The Twin Mountains Formation, also known as the Twin Mak Formation, is a sedimentary rock formation, within the Trinity Group, found in Texas of the United States of America. It is a terrestrial formation of Aptian age (Lower Cretaceous), and is notable for its dinosaur fossils. Dinosaurs from this formation include the large theropod ''Acrocanthosaurus'', the sauropod ''Sauroposeidon'', as well as the ornithopods ''Tenontosaurus'' and ''Convolosaurus''. It is the lowermost unit of the lower Cretaceous, lying unconformably on Carboniferous strata. It is overlain by the Glen Rose Formation. It is the lateral equivalent of the lower part of the Antlers Formation. Paleobiota * '' Acrocanthosaurus atokensis''Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 553-556. . * Dromaeosauridae indet. * The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tucumcari Formation
The Tucumcari Formation is a geologic formation in New Mexico. It preserves fossils dating back to the Albian Age of the early Cretaceous period. Description The formation consists of highly fossiliferous gray shale and buff calcareous sandstone with some limestone nodules. It overlies the Morrison Formation and is overlain by the Mesa Rica Sandstone. The formation is interpreted as marine shales deposited during the Kiowa-Skull Creek transgression. It is likely the lateral equivalent of the Glencairn Formation. Fossils More than 65 marine invertebrate species have been found in the Tucumcari Shale. The macrofossils are mostly bivalves, with some gastropods and ammonoids. Microfossils include ostracods, foraminiferans, and palynomorphs. Species found in the formation include the solitary corals ''Desmophyllum'' and '' Platycyathus'', the bivalves '' Scabrotrigonia'', '' Pteria'', ''Texigryphaea'', ''Botula'', and ''Lopha'', and gastropod '' Turritella''. The shells show bor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zinder
Zinder (locally, ''Damagaram''), formerly also spelled Sinder, is the third largest city in Niger, with a population of 170,574 (2001 census);Population figures from citypopulation.de citin (2001) Institut National de la Statistique du Niger by the 2012 census its population reached 235,605. It is situated east of the capital and north of the Nigerian city of . History Early history ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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