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Kryptobaatar Dashzevegi
''Kryptobaatar''and also known as ''Gobibaatar'' or ''Tugrigbaatar'' is an extinct mammalian genus dating from the Upper Cretaceous Period and identified in Central Asia. This animal was a member of the extinct order of Multituberculata within the suborder Cimolodonta, and was a member of the family Djadochtatheriidae. It lived contemporaneously with some of the dinosaurs. Its skull had a length of perhaps 3 cm. The generic name ''Kryptobaatar'' is derived from Greek : ''kruptós'', "hidden," (alludes to the ventral position of infraorbital foramen) and Mongolian : ''baatar'', "hero" (alludes to the name of the capital of Mongolia, Ulan Baatar). The specific name ''dashzevegi'' is named in honour of Mongolian palaeontologist Demberelyin Dashzeveg. The derivation of its synonym ''Gobibaatar parvus'' is Gobi (occurring in the Gobi Desert, Mongolia) and baatar ("a hero", the same as ''Kryptobaatar''). Another synonym ''Tugrigbaatar saichanensis'' is a generic name derived ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campanian
The Campanian is the fifth of six ages of the Late Cretaceous Epoch on the geologic timescale of the International Commission on Stratigraphy (ICS). In chronostratigraphy, it is the fifth of six stages in the Upper Cretaceous Series. Campanian spans the time from 83.6 (± 0.2) to 72.1 (± 0.2) million years ago. It is preceded by the Santonian and it is followed by the Maastrichtian. The Campanian was an age when a worldwide sea level rise covered many coastal areas. The morphology of some of these areas has been preserved: it is an unconformity beneath a cover of marine sedimentary rocks. Etymology The Campanian was introduced in scientific literature by Henri Coquand in 1857. It is named after the French village of Champagne in the department of Charente-Maritime. The original type locality was a series of outcrop near the village of Aubeterre-sur-Dronne in the same region. Definition The base of the Campanian Stage is defined as a place in the stratigraphic column wher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ulan Baatar
Ulan may refer to: Places * Ulan, New South Wales, a town in Australia *Ulan County, in Qinghai Province, China *Ulan District, eastern Kazakhstan *Ulan, Iran, a village in Zanjan Province People *Ulan, politician from Inner Mongolia, China Military * Uhlan, Tatar-modelled light cavalry that formed part of the Polish, Russian, Prussian, and Austrian armies until the 20th century *ASCOD Ulan, a modern Austrian infantry fighting vehicle Music * "Ulan" (Rivermaya song), on the group's 1994 self-titled album * "Ulan", a song by Filipino rock group Cueshé on their 2005 album ''Half Empty, Half Full'' Other uses * Ulan (cycling team), a 2008 Kazakh road-racing team * ''Ulan'' (film), a 2019 Filipino film * Oil of Ulan, the Australasian localisation used until the 1990s for the skin-cream product Olay * Union List of Artist Names (ULAN), a controlled vocabulary maintained by the Getty Vocabulary Program * Ulan, the player character of the 2021 video game '' Astria Ascending'' See ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Australia and Anta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mongolia
Mongolia; Mongolian script: , , ; lit. "Mongol Nation" or "State of Mongolia" () is a landlocked country in East Asia, bordered by Russia to the north and China to the south. It covers an area of , with a population of just 3.3 million, making it the world's most sparsely populated sovereign nation. Mongolia is the world's largest landlocked country that does not border a closed sea, and much of its area is covered by grassy steppe, with mountains to the north and west and the Gobi Desert to the south. Ulaanbaatar, the capital and largest city, is home to roughly half of the country's population. The territory of modern-day Mongolia has been ruled by various nomadic empires, including the Xiongnu, the Xianbei, the Rouran, the First Turkic Khaganate, and others. In 1206, Genghis Khan founded the Mongol Empire, which became the largest contiguous land empire in history. His grandson Kublai Khan conquered China proper and established the Yuan dynasty. After the co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baruungoyot Formation
The Barun Goyot Formation (also known as Baruungoyot Formation or West Goyot Formation) is a Formation (stratigraphy), geological formation dating to the Late Cretaceous Period (geology), Period. It is located within and is widely represented in the Gobi Desert Basin, in the Ömnögovi Province of Mongolia. Description It was previously known as the Lower Nemegt Beds occurring beneath the Nemegt Formation and above the Djadokhta Formation. It has been suggested that the Djadokhta and Barun Goyot Formations are lower and upper parts, respectively, of the same lithological unit and the boundary between the two does not exist. The stratotype of the Barun Goyot Formation is the Khulsan locality, east of Nemegt. At Nemegt, only the uppermost barungoyotian beds are visible. The ''Red Beds of Khermeen Tsav'' are also considered part of the Barun Goyot Formation. It is approximately in thickness,Gradzinski, R.; & Jerzykiewicz, T. (1974). Sedimentation of the Barun Goyot formation. Palae ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flaming Cliffs
The Flaming Cliffs site (also known as Bayanzag ( zh, 巴彥扎格), Bain-Dzak or Bayn Dzak) ( mn, Баянзаг ''rich in saxaul''), with the alternative Mongolian name of mn, Улаан Эрэг (''red cliffs''), is a region of the Gobi Desert in the Ömnögovi Province of Mongolia, in which important fossil finds have been made. It was given this name by American paleontologist Roy Chapman Andrews, who visited in the 1920s. The area is most famous for yielding the first discovery of dinosaur eggs. Other finds in the area include specimens of ''Velociraptor'' and eutherian mammals. It exposes rocks of the Djadochta Formation. It is illegal to remove fossils from the area without appropriate permits. The nickname refers to the red or orange color of the sandstone cliffs (especially at a sunset),. Dinosaur bones/fossils The following are dinosaur fossils that have been found in the Flaming Cliffs. Theropods: *Maniraptorans: ''Archaeornithoides'', ''Velociraptor'', ''Saurornith ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Djadokhta 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kryptobaatar Skull
''Kryptobaatar''and also known as ''Gobibaatar'' or ''Tugrigbaatar'' is an extinct mammalian genus dating from the Upper Cretaceous Period and identified in Central Asia. This animal was a member of the extinct order of Multituberculata within the suborder Cimolodonta, and was a member of the family Djadochtatheriidae. It lived contemporaneously with some of the dinosaurs. Its skull had a length of perhaps 3 cm. The generic name ''Kryptobaatar'' is derived from Greek : ''kruptós'', "hidden," (alludes to the ventral position of infraorbital foramen) and Mongolian : ''baatar'', "hero" (alludes to the name of the capital of Mongolia, Ulan Baatar). The specific name ''dashzevegi'' is named in honour of Mongolian palaeontologist Demberelyin Dashzeveg. The derivation of its synonym ''Gobibaatar parvus'' is Gobi (occurring in the Gobi Desert, Mongolia) and baatar ("a hero", the same as ''Kryptobaatar''). Another synonym ''Tugrigbaatar saichanensis'' is a generic name derived from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gurvan Saikhan Mountains
The Gurvan Saikhan ( mn, Гурван Сайхан, ''lit.'' ''"three beauties"''), is a mountain range in the Ömnögovi Province of southern Mongolia. It is named for three subranges: Baruun Saikhany Nuruu (the ''Western Beauty''), Dund Saikhany Nuruu (the ''Middle Beauty'') and Zuun Saikhany Nuruu (the ''Eastern Beauty''). The highest peak is found in Dund Saikhany Nuruu, and is above sea level. A notable gorge, Yolyn Am, is found in Zuun Saikhany Nuruu. Though the range is surrounded by the Gobi desert, Yolyn Am contains a semi-permanent ice field. The range forms the eastern part of the Gobi Gurvansaikhan National Park Gobi Gurvansaikhan National Park (, ''Gobi three beauties nature complex'') is a national park in southern Mongolia. The park was established in 1993, and expanded to its current size in 2000. The park, at nearly 27,000 square kilometers, is the .... External linksTourist map of Gobi Gurvansaikhan National Park Altai Mountains Mountain ranges of Mongol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
