List Of Stratigraphic Units With Dinosaur Tracks
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List Of Stratigraphic Units With Dinosaur Tracks
Indeterminate or unspecified dinosaur tracks Ornithischians Indeterminate or unspecified ornithischian tracks Saurischians Theropods Sauropodomorphs See also List of dinosaur-bearing rock formations This list of dinosaur-bearing rock formations is a list of geologic formations in which dinosaur fossils have been documented. Containing body fossils * List of stratigraphic units with dinosaur body fossils ** List of stratigraphic units with ... Footnotes References * Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. . {{DEFAULTSORT:Stratigraphic Units With Dinosaur Tracks Tracks Dinosaur trace fossils * ...
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Arcabuco Formation
The Arcabuco Formation ( es, Formación Arcabuco, Jar, JKa) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of thick beds of light-coloured quartzitic sandstones and conglomerates with occasional shales and dates to the Late Jurassic and Early Cretaceous periods; Tithonian to Berriasian epochs. Dinosaur footprints have been found in the Arcabuco Formation near the Iguaque anticlinal outside Chíquiza, Boyacá. Etymology The formation was first defined by Scheibe in 1938 and named after Arcabuco, Boyacá. The type section of the Arcabuco Formation was redefined in 1985 by Galvis and Rubiano around Villa de Leyva.Galvis & Valencia, 2009, p.15 Description Lithologies The Arcabuco Formation is characterised by a sequence of light- to pink-coloured fine quartzitic sandstones and conglomerates with red shales up to in thickness intercalated.Galvis & Valencia, 2009, p.17Rodríguez & Solano, 2000, p.28 In ...
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Przysucha Formation
The Przysucha Formation is a geologic formation in Poland. Ichnofossils attributed to dinosaurs have been found in the formation. Fossil content The following fossils were reported from the formation:Przysucha Formation
at .org
;Ichnofossils * '' Anomoepus pienkovskii'' * ''

Lists Of Dinosaur-bearing Stratigraphic Units
This list of dinosaur-bearing rock formations is a list of geologic formations in which dinosaur fossils have been documented. Containing body fossils * List of stratigraphic units with dinosaur body fossils ** List of stratigraphic units with few dinosaur genera ** List of stratigraphic units with indeterminate dinosaur fossils Containing trace fossils * List of stratigraphic units with dinosaur trace fossils ** List of stratigraphic units with dinosaur tracks *** List of stratigraphic units with ornithischian tracks *** List of stratigraphic units with sauropodomorph tracks *** List of stratigraphic units with theropod tracks See also * Lists of fossiliferous stratigraphic units * List of fossil sites * Mesozoic The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceo ... {{DEFAULTSOR ...
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List Of Dinosaur-bearing Rock Formations
This list of dinosaur-bearing rock formations is a list of geologic formations in which dinosaur fossils have been documented. Containing body fossils * List of stratigraphic units with dinosaur body fossils ** List of stratigraphic units with few dinosaur genera ** List of stratigraphic units with indeterminate dinosaur fossils Containing trace fossils * List of stratigraphic units with dinosaur trace fossils ** List of stratigraphic units with dinosaur tracks *** List of stratigraphic units with ornithischian tracks *** List of stratigraphic units with sauropodomorph tracks *** List of stratigraphic units with theropod tracks See also * Lists of fossiliferous stratigraphic units * List of fossil sites * Mesozoic The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceo ... {{DEFAULTSOR ...
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Yuanpu Formation
The Nanxiong Formation (also known as Yuanpu Formation) is a Late Cretaceous geologic formation in Guangdong Province. Dinosaur remains are among the fossils that have been recovered from the formation. Description It consists of continental siliciclastic red beds, with fauna which similar to that of the Nemegt Formation. It has been dated about 66.7 ± 0.3 million years ago. It is the lowest unit of the Nanxiong Basin, a small graben created during Mesozoic rifting. Buck et al. state that it overlies Jurassic granite basement, and is conformably overlain by the Shanghu Formation. Alternative stratigraphic schemes for the Nanxiong basin have been proposed, one of which refers to the Nanxiong succession as the Nanxiong Group, and dividing it into the Yuanfu, Zhutian and Zhenshui formations, and overlying the Albian to Turonian Changba Formation. Paleobiota of the Nanxiong Formation Crocodilians Lizards Turtles Dinosaurs Hadrosaurs Oviraptorosaurs Sa ...
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Wangshi Group
The Wangshi Group () is a geological Group in Shandong, China whose strata date back to the Coniacian to Campanian stages of the Late Cretaceous.Wangshi Group
in the
Dinosaur remains are among the fossils that have been recovered from the group.Weishampel et al., 2004, pp.593-600


Vertebrate paleofauna


Dinosaurs


Other fauna


Fossil eggs

The following fossil eggs were recovered from the Jingangkou Format ...
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Wangi Formation
The Wangi Formation is a Mesozoic geologic formation in China. Indeterminate fossil dinosaur tracks have been reported from the formation.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. See also * List of dinosaur-bearing rock formations ** List of stratigraphic units with dinosaur tracks Indeterminate or unspecified dinosaur tracks Ornithischians Indeterminate or unspecified ornithischian tracks Saurischians Theropods Sauropodomorphs See also List of dinosaur-bearing rock formations This list of dinosaur-bearing rock f ... *** Indeterminate dinosaur tracks Footnotes References * Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. . Mesozoic Erathem of Asia {{China-geologic-formation-stub ...
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Quwu Formation
The Quwu Formation is a Mesozoic geologic formation in China. Indeterminate fossil dinosaur tracks have been reported from the formation. See also * List of dinosaur-bearing rock formations * List of stratigraphic units with dinosaur tracks Indeterminate or unspecified dinosaur tracks Ornithischians Indeterminate or unspecified ornithischian tracks Saurischians Theropods Sauropodomorphs See also List of dinosaur-bearing rock formations This list of dinosaur-bearing rock f ... * Indeterminate dinosaur tracks Footnotes Mesozoic Erathem of Asia {{China-geologic-formation-stub ...
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Jinjiang Formation
The Jinjiang Formation is a Mesozoic geologic formation in China. Indeterminate fossil dinosaur tracks have been reported from the formation.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. See also * List of dinosaur-bearing rock formations ** List of stratigraphic units with dinosaur tracks Indeterminate or unspecified dinosaur tracks Ornithischians Indeterminate or unspecified ornithischian tracks Saurischians Theropods Sauropodomorphs See also List of dinosaur-bearing rock formations This list of dinosaur-bearing rock f ... *** Indeterminate dinosaur tracks Footnotes References * Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. . Mesozoic Erathem of Asia {{China-geologic-formation-stub ...
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Industrial University Of Santander
The Industrial University of Santander ( es, Universidad Industrial de Santander), abbreviated in Spanish with the acronym UIS, is a public university, based in a coeducational, and research model. The university serves the Santander Department, being the main campus located in the city of Bucaramanga, Santander, Colombia. The university also has satellite campuses across the department in the cities of Barrancabermeja, Barbosa, Málaga, Piedecuesta, Socorro. UIS is the largest higher education institution and is regarded as one of the leading multidisciplinary research universities in Colombia by student population, research groups, academic output, technological development, and number of publications. UIS is one of the most selective Colombian universities and have been ranked as the top university in the North region of Colombia. The university was created by ordinance No. 83 of June 22, 1944, by the Departmental Assembly, and began its labors in March 1948. The universi ...
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El Jume Formation
The El Jume Formation is an Early Cretaceous geologic formation in Argentina. Indeterminate fossil dinosaur tracks have been reported from the formation.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. The formation, belonging to the El Gigante Group, overlies the Los Riscos Formation and is overlain by the El Toscal Formation. The sandstones and claystones of the formation were deposited in a fluvial environment.Gardini et al., 2009, p.554 Part of the formation was assigned to a new formation, Balde de Leyes Formation in 2015.Colombi et al., 2015, p.447 See also * List of dinosaur-bearing rock formations ** List of stratigraphic units with dinosaur tracks *** Indeterminate dinosaur tracks * Lagarcito Formation * La Cruz Formation * Quebrada del Barro Formation The Quebrada del Barro Formation is a geological formation of the Marayes-El Carrizal Basin in San Juan Province, Argentina. This formation is the most fossiliferous portion of the Triassic Maraye ...
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Djadochta Formation
The Djadochta Formation (sometimes transcribed and also known as Djadokhta, Djadokata, or Dzhadokhtskaya) is a highly fossiliferous geological formation situated in Central Asia, Gobi Desert, dating from the Late Cretaceous period, about 75 million to 71 million years ago. The type locality is the Bayn Dzak locality, famously known as the Flaming Cliffs. Dinosaur, mammal, and other reptile remains are among the fossils that have been recovered from the formation. Excavation history The Djadochta Formation was first documented and explored—though only a single locality—during paleontological expeditions of the American Museum of Natural History in 1922–1925, which were part of the Central Asiatic Expeditions. The expeditions were led by Roy Chapman Andrews, in company of Walter Willis Granger as chief paleontologist and field team. The team did extensive exploration at the Bayn Dzak (formerly Shabarakh Usu) region, which they nicknamed Flaming Cliffs given that at sunset th ...
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