Shansitherium
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Shansitherium
''Shansitherium'' ("beast of Shanxi")Killgus, H., 1922. Die unterpliocaenen chinesischen Säugetierreste der Tafelschen Sammlung zu Tübingen (Doctoral dissertation) is an extinct genus of superficially moose-like or antelope-like giraffids from the late Miocene epoch of Shanxi Province, China. They are closely related to the genus ''Samotherium ''Samotherium'' ("beast of Samos") is an extinct genus of Giraffidae from the Miocene and Pliocene of Eurasia and Africa. ''Samotherium'' had two ossicones on its head, and long legs. The ossicones usually pointed upward, and were curved backwar ...''. Species The genus consists of the following species: * '' Shansitherium fuguensis'' * '' Shansitherium tafeli'' * '' Shansitherium quadricornis''Bohlin, K., 1926. Über den veränderlichen Stern BC (7.1926) Ophiuchi. Astronomische Nachrichten, 229, p.65. References External links * Prehistoric giraffes Miocene mammals of Asia Miocene even-toed ungulates Miocene genus ...
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Shansitherium Quadricornis
''Shansitherium'' ("beast of Shanxi")Killgus, H., 1922. Die unterpliocaenen chinesischen Säugetierreste der Tafelschen Sammlung zu Tübingen (Doctoral dissertation) is an extinct genus of superficially moose-like or antelope-like Giraffidae, giraffids from the late Miocene Epoch (reference date), epoch of Shanxi Province, China. They are closely related to the genus ''Samotherium''. Species The genus consists of the following species: * ''Shansitherium fuguensis'' * ''Shansitherium tafeli'' * ''Shansitherium quadricornis''Bohlin, K., 1926. Über den veränderlichen Stern BC (7.1926) Ophiuchi. Astronomische Nachrichten, 229, p.65. References External links

* Prehistoric giraffes Miocene mammals of Asia Miocene even-toed ungulates Miocene genus extinctions Prehistoric even-toed ungulate genera {{Paleo-eventoedungulate-stub ...
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Shansitherium Tafeli
''Shansitherium'' ("beast of Shanxi")Killgus, H., 1922. Die unterpliocaenen chinesischen Säugetierreste der Tafelschen Sammlung zu Tübingen (Doctoral dissertation) is an extinct genus of superficially moose-like or antelope-like giraffids from the late Miocene epoch of Shanxi Province, China. They are closely related to the genus ''Samotherium''. Species The genus consists of the following species: * '' Shansitherium fuguensis'' * '' Shansitherium tafeli'' * ''Shansitherium quadricornis ''Shansitherium'' ("beast of Shanxi")Killgus, H., 1922. Die unterpliocaenen chinesischen Säugetierreste der Tafelschen Sammlung zu Tübingen (Doctoral dissertation) is an extinct genus of superficially moose-like or antelope-like Giraffidae, g ...''Bohlin, K., 1926. Über den veränderlichen Stern BC (7.1926) Ophiuchi. Astronomische Nachrichten, 229, p.65. References External links * Prehistoric giraffes Miocene mammals of Asia Miocene even-toed ungulates Miocene genus exti ...
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Shansitherium Fuguensis
''Shansitherium'' ("beast of Shanxi")Killgus, H., 1922. Die unterpliocaenen chinesischen Säugetierreste der Tafelschen Sammlung zu Tübingen (Doctoral dissertation) is an extinct genus of superficially moose-like or antelope-like giraffids from the late Miocene epoch of Shanxi Province, China. They are closely related to the genus ''Samotherium''. Species The genus consists of the following species: * '' Shansitherium fuguensis'' * ''Shansitherium tafeli'' * ''Shansitherium quadricornis ''Shansitherium'' ("beast of Shanxi")Killgus, H., 1922. Die unterpliocaenen chinesischen Säugetierreste der Tafelschen Sammlung zu Tübingen (Doctoral dissertation) is an extinct genus of superficially moose-like or antelope-like Giraffidae, g ...''Bohlin, K., 1926. Über den veränderlichen Stern BC (7.1926) Ophiuchi. Astronomische Nachrichten, 229, p.65. References External links * Prehistoric giraffes Miocene mammals of Asia Miocene even-toed ungulates Miocene genus extin ...
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Giraffidae
The Giraffidae are a family of ruminant artiodactyl mammals that share a common ancestor with deer and bovids. This family, once a diverse group spread throughout Eurasia and Africa, presently comprises only two extant genera, the giraffe (one or more species of ''Giraffa'', depending on taxonomic interpretation) and the okapi (the only known species of ''Okapia''). Both are confined to sub-Saharan Africa: the giraffe to the open savannas, and the okapi to the dense rainforest of the Congo. The two genera look very different on first sight, but share a number of common features, including a long, dark-coloured tongue, lobed canine teeth, and horns covered in skin, called ossicones. Taxonomy Evolutionary background The giraffids are ruminants of the clade Pecora. Other extant pecorans are the families Antilocapridae (pronghorns), Cervidae (deer), Moschidae (musk deer), and Bovidae (cattle, goats and sheep, wildebeests and allies, and antelopes). The exact interrelationships a ...
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Samotherium
''Samotherium'' ("beast of Samos") is an extinct genus of Giraffidae from the Miocene and Pliocene of Eurasia and Africa. ''Samotherium'' had two ossicones on its head, and long legs. The ossicones usually pointed upward, and were curved backwards, with males having larger, more curved ossicones, though in the Chinese species, ''S. sinense'', the straight ossicones point laterally, not upwards. The genus is closely related to ''Shansitherium''. Fossil evidence suggests that ''Samotherium'' had a rounded muzzle, which would suggest a grazing lifestyle and a habitat composed of grassland. One common predator of this animal was the Amphimachairodus According to biologist Richard Ellis the skull of a ''Samotherium'' is portrayed on an ancient Greek vase as a monster that Heracles is fighting. Description A 2015 study found that ''Samotherium'' had a neck intermediate in length between the giraffe and the okapi The okapi (; ''Okapia johnstoni''), also known as the forest ...
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Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ...
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Miocene Even-toed Ungulates
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ...
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Miocene Mammals Of Asia
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ...
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Prehistoric Giraffes
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. ...
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China
China, officially the People's Republic of China (PRC), is a country in East Asia. It is the world's most populous country, with a population exceeding 1.4 billion, slightly ahead of India. China spans the equivalent of five time zones and borders fourteen countries by land, the most of any country in the world, tied with Russia. Covering an area of approximately , it is the world's third largest country by total land area. The country consists of 22 provinces, five autonomous regions, four municipalities, and two Special Administrative Regions (Hong Kong and Macau). The national capital is Beijing, and the most populous city and financial center is Shanghai. Modern Chinese trace their origins to a cradle of civilization in the fertile basin of the Yellow River in the North China Plain. The semi-legendary Xia dynasty in the 21st century BCE and the well-attested Shang and Zhou dynasties developed a bureaucratic political system to serve hereditary monarchies, or dyna ...
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Beijing Museum Of Natural History
The Beijing Museum of Natural History (BMNH; ) is located at 126 Tian Qiao Nan Street, Dongcheng District, Beijing, 100050, and is the most popular natural history museum in China.Home and Abroad
It was founded in 1951 as the National Central Museum of Natural History, and its name was changed to the ''Beijing Museum of Natural History'' in 1962. The BMNH is the first large scale natural history museum created in China.BMNH website
The BMNH has total floor space of 24,000 square meters, of which 8,000 square meters are available for display and owns more than 200,000 specimens. The major display area is the Tian Jiabing Building. The collections include



Epoch (reference Date)
In chronology and periodization, an epoch or reference epoch is an instant in time chosen as the origin of a particular calendar era. The "epoch" serves as a reference point from which time is measured. The moment of epoch is usually decided by congruity, or by following conventions understood from the epoch in question. The epoch moment or date is usually defined from a specific, clear event of change, an ''epoch event''. In a more gradual change, a deciding moment is chosen when the ''epoch criterion'' was reached. Calendar eras Pre-modern eras * The Yoruba calendar (''Kọ́jọ́dá'') uses 8042 BC as the epoch, regarded as the year of the creation of Ile-Ife by the god Obatala, also regarded as the creation of the earth. * ''Anno Mundi'' (years since the creation of the world) is used in the Byzantine calendar (5509 BC). * ''Anno Mundi'' (years since the creation of the world) as used in the Hebrew calendar (3761 BC). * Olympiads, the ancient Greek era of four-year ...
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