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Anancus
''Anancus'' is an extinct genus of elephantoid proboscideans ("gomphothere" ''sensu lato'') native to Afro-Eurasia, that lived from the Tortonian stage of the late Miocene until the genus' extinction during the early Pleistocene, roughly from 8.5–2 million years ago. Taxonomy The type genus of the family, ''Anancus'', was named by Auguste Aymard in 1855. It was traditionally allocated to Gomphotheriidae, but was later assigned to the family Elephantidae by McKenna and Bell (1997), Lambert and Shoshani (1998), Kalb and Froelich (1995), and Shoshani and Tassy (2005). Hautier et al. (2009) assigned the genus to the subfamily Anancinae within Gomphotheriidae. Recently ''Anancus'' along with other tetralophodont gomphotheres have been removed from Gomphotheridae, and are now regarded as members of Elephantoidea instead. Description ''Anancus'' stood around tall, with a weight up to 5 tons, and closely resembled a modern elephant. Aside from its somewhat shorter legs, ''Anancus' ...
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Anancus NT Small
''Anancus'' is an extinct genus of elephantoid proboscideans ("gomphothere" ''sensu lato'') native to Afro-Eurasia, that lived from the Tortonian stage of the late Miocene until the genus' extinction during the early Pleistocene, roughly from 8.5–2 million years ago. Taxonomy The type genus of the family, ''Anancus'', was named by Auguste Aymard in 1855. It was traditionally allocated to Gomphotheriidae, but was later assigned to the family Elephantidae by McKenna and Bell (1997), Lambert and Shoshani (1998), Kalb and Froelich (1995), and Shoshani and Tassy (2005). Hautier et al. (2009) assigned the genus to the subfamily Anancinae within Gomphotheriidae. Recently ''Anancus'' along with other tetralophodont gomphotheres have been removed from Gomphotheridae, and are now regarded as members of Elephantoidea instead. Description ''Anancus'' stood around tall, with a weight up to 5 tons, and closely resembled a modern elephant. Aside from its somewhat shorter legs, ''Anancus' ...
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Anancus
''Anancus'' is an extinct genus of elephantoid proboscideans ("gomphothere" ''sensu lato'') native to Afro-Eurasia, that lived from the Tortonian stage of the late Miocene until the genus' extinction during the early Pleistocene, roughly from 8.5–2 million years ago. Taxonomy The type genus of the family, ''Anancus'', was named by Auguste Aymard in 1855. It was traditionally allocated to Gomphotheriidae, but was later assigned to the family Elephantidae by McKenna and Bell (1997), Lambert and Shoshani (1998), Kalb and Froelich (1995), and Shoshani and Tassy (2005). Hautier et al. (2009) assigned the genus to the subfamily Anancinae within Gomphotheriidae. Recently ''Anancus'' along with other tetralophodont gomphotheres have been removed from Gomphotheridae, and are now regarded as members of Elephantoidea instead. Description ''Anancus'' stood around tall, with a weight up to 5 tons, and closely resembled a modern elephant. Aside from its somewhat shorter legs, ''Anancus' ...
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Pliocene Proboscideans
The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58See the 2014 version of the ICS geologic time scale
million years ago. It is the second and most recent epoch of the Period in the . The Pliocene follows the Epoch and is followed by the

Gomphothere
Gomphotheres are any members of the diverse, extinct taxonomic family Gomphotheriidae. Gomphotheres were elephant-like proboscideans, but do not belong to the family Elephantidae. They were widespread across Afro-Eurasia and North America during the Miocene and Pliocene epochs and dispersed into South America during the Pleistocene following the Great American Interchange. Gomphotheriidae in its broadest sense is probably paraphyletic with respect to Elephantidae, which contains modern elephants. While most famous forms such as ''Gomphotherium'' had long lower jaws with tusks, which is the ancestral condition for the group, after these forms became extinct, the surviving gomphotheres had short jaws with either vestigial or no lower tusks (brevirostrine), looking very similar to modern elephants, an example of parallel evolution. By the end of the Early Pleistocene, gomphotheres became extinct in Afro-Eurasia, with the last two genera, ''Cuvieronius'' persisting in southern North ...
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Pliocene
The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58See the 2014 version of the ICS geologic time scale
million years ago. It is the second and most recent epoch of the Neogene Period in the . The Pliocene follows the Epoch and is followed by the Epoch. Prior to the 2009 ...
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Gomphotheriidae
Gomphotheres are any members of the diverse, extinct taxonomic family Gomphotheriidae. Gomphotheres were elephant-like proboscideans, but do not belong to the family Elephantidae. They were widespread across Afro-Eurasia and North America during the Miocene and Pliocene epochs and dispersed into South America during the Pleistocene following the Great American Interchange. Gomphotheriidae in its broadest sense is probably paraphyletic with respect to Elephantidae, which contains modern elephants. While most famous forms such as ''Gomphotherium'' had long lower jaws with tusks, which is the ancestral condition for the group, after these forms became extinct, the surviving gomphotheres had short jaws with either vestigial or no lower tusks (brevirostrine), looking very similar to modern elephants, an example of parallel evolution. By the end of the Early Pleistocene, gomphotheres became extinct in Afro-Eurasia, with the last two genera, ''Cuvieronius'' persisting in southern North ...
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Elephantoidea
Elephantoidea is a taxonomic group that contains the elephants as well as their closest extinct relatives. The following cladogram shows the relationships among elephantoids, based on hyoid The hyoid bone (lingual bone or tongue-bone) () is a horseshoe-shaped bone situated in the anterior midline of the neck between the chin and the thyroid cartilage. At rest, it lies between the base of the mandible and the third cervical vertebra. ... characteristics: References Taxa named by John Edward Gray {{afrotheria-stub ...
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Elephantoid
Elephantoidea is a taxonomic group that contains the elephants as well as their closest extinct relatives. The following cladogram shows the relationships among elephantoids, based on hyoid The hyoid bone (lingual bone or tongue-bone) () is a horseshoe-shaped bone situated in the anterior midline of the neck between the chin and the thyroid cartilage. At rest, it lies between the base of the mandible and the third cervical vertebra. ... characteristics: References Taxa named by John Edward Gray {{afrotheria-stub ...
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Proboscidea
The Proboscidea (; , ) are a taxonomic order of afrotherian mammals containing one living family (Elephantidae) and several extinct families. First described by J. Illiger in 1811, it encompasses the elephants and their close relatives. From the mid-Miocene onwards, most proboscideans were very large. The largest land mammal of all time may have been a proboscidean; ''Palaeoloxodon namadicus'' was up to at the shoulder and may have weighed up to , almost double the weight of some sauropods like ''Diplodocus carnegii''. The largest extant proboscidean is the African bush elephant, with a record of size of at the shoulder and . In addition to their enormous size, later proboscideans are distinguished by tusks and long, muscular trunks, which were less developed or absent in early proboscideans. Three species of elephant are currently recognised: the African bush elephant, the African forest elephant, and the Asian elephant. Elephantidae is the only surviving family of the or ...
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Auguste Aymard
Auguste Aymard (5 December 1808 – 26 June 1889) was a French prehistorian and palaeontologist who lived and died in Puy-en-Velay (Haute-Loire). He described the fossil '' Entelodon magnus'' and the fossil genera ''Anancus'' and ''Amphechinus''. Auguste Aymard was the archivist for the Departement Haute-Loire and Conservateur of Musée du Puy-en-Velay. He made archaeological discoveries in Puy-en-Velay, Polignac, Haute-Loire and Espaly-Saint-Marcel Espaly-Saint-Marcel () is a commune in the Haute-Loire department in south-central France. Population See also * Communes of the Haute-Loire department The following is a list of the 257 communes of the Haute-Loire department of France. .... Works * Aymard, A., 1848, Essai monographique sur un nouveau genre de Mammifère fossile trouvé dans la Haute-Loire, et nommé Entélodon, ''Annales de la Société d’Agriculture Sciences, Arts et Commerce du Puy'', Vol.12, 1848, pp. 227–268 * Aymard, A. 1854, Acquisitions ...
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Tapir
Tapirs ( ) are large, herbivorous mammals belonging to the family Tapiridae. They are similar in shape to a pig, with a short, prehensile nose trunk. Tapirs inhabit jungle and forest regions of South and Central America, with one species inhabiting Southeast Asia. They are one of three extant branches of Perissodactyla (odd-toed ungulates), alongside equines and rhinoceros. Only a single genus, ''Tapirus'' is currently extant. Tapirs migrated into South America during the Pleistocene epoch from North America after the formation of the Isthmus of Panama as part of the Great American Interchange. Tapirs were once widespread in North America until the arrival of humans at the end of the Late Pleistocene, around 12,000 years ago. Species There are four widely recognized extant species of tapir, all in the genus ''Tapirus'' of the family Tapiridae. They are the South American tapir, the Malayan tapir, Baird's tapir, and the mountain tapir. In 2013, a group of researchers said they ...
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Miocene Proboscideans
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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