Sinomastodon
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Sinomastodon
''Sinomastodon'' ("Chinese mastodont") is an extinct gomphothere genus (of order Proboscidea), from the Late Miocene to the Early Pleistocene deposits of Asia ( China, Japan, Thailand, Myanmar, Kashmir, and Indonesia). It is not to be confused with the genus ''Sinomammut'' from a different proboscidean family, whose members are commonly called "mastodons". The animal was very similar to modern elephants with sizes ranging from 3.6 to 5.3 m. Several species are known from China, the best-known being ''S. hanjiangensis'' from the Late Miocene and Early Pliocene of the Shanxi province. It is known from an incomplete skeleton of an adult (measuring 5.3 m) including maxilla, mandibles, teeth, tusks and other materials has been discovered. The Japanese species ''S. sendaicus'' described in 1924 from dentary materials from Pliocene deposits has been ascribed to the genus, as well as the species ''S. bumiajuensis'' (formerly ''Tetralophodon'') from the late Pliocene of Java. One in ...
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Sinomammut
''Sinomammut'' (meaning "Chinese mastodon") is a proboscidean found in the Miocene of China. Only one species, ''S. tobieni'', is known, named in 2016. Discovery and naming It was known from GIOTC 0984-9-178, a single, fragmentary, mandible found in the 1990s, however, most of the specimen has been lost, leaving only the right ramus and an in-situ photograph of the mandible. The surviving ramus was collected in 1999 in the Neogene-aged Xihe Linxian Basin in Miocene-aged deposits by Zhao Desi. The left branch of the jaw was lost during the salvage and is only documented by a photo of the fossil ''in situ''. In 2007, Xie GuangPu, also involved in the initial description, published the find under the scientific name ''Sinomastodon intermedium''.GP, Xie. (2007). Identification on elephantoid teeth and fossil elephantoids in Gansu (in Chinese). In: EJ (Ed), ''The Collection of Disquisitions for West China's Museum Forum Contents. Lanzhou: Sanqin Press'' p. 152-181. In 2014, GIOTC ...
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Notiomastodon
''Notiomastodon'' is an extinct proboscidean genus of gomphotheres (a distant relative to modern elephants) endemic to South America from the Pleistocene to the beginning of the Holocene. ''Notiomastodon'' specimens reached a size similar to that of the modern Asian elephant. Like other brevirostrine gomphotheres such as ''Cuvieronius'' and '' Stegomastodon'', ''Notiomastodon'' was characterized by its short snout and tall, highly arched skull. The short jaw was due to the loss of the lower tusks found in more primitive gomphotheres. ''Notiomastodon'' was a generalist feeder capable of consuming various types of plants, which varied according to local environments. In the course of the last glacial period, there was an adaptation towards the consumption of grasses. The genus was originally named in 1929, and has been controversial in the course of taxonomic history as it has frequently been confused with or synonymized with forms called ''Haplomastodon'' and ''Stegomastodon''. Ex ...
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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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Gomphotheres
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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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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Eubelodon
''Eubelodon'' is an extinct genus of gomphothere (a family in the order Proboscidea, which also includes modern elephants) which lived in North America during the Miocene Epoch. It contains a single species: ''Eubelodon morrilli''. Like other gomphotheres, it had a superficially elephant-like appearance with a trunk and tusks. Fossil distribution Fossils are restricted to what is now the Great Plains of the United States. Remains were found in the Poison Ivy Quarry, Antelope, Brown County, Nebraska, and Tripp County, South Dakota. Taxonomy ''Eubelodon'' was named by Erwin Hinckly Barbour in 1914. It was synonymized subjectively with ''Trilophodon'' by Osborn in 1918 and again by Tobien in 1973 with ''Gomphotherium''. It was assigned to 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 a ...
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Stegomastodon
''Stegomastodon'' ('roof breast tooth') is an extinct genus of gomphotheres, a family of proboscideans. It ranged throughout North America from the early Blancan ~4 Ma, to the early Irvingtonian (~1.2 Ma). The South American species have been synonymized with '' Notiomastodon platensis''. Species The following definite species have been described:''Stegomastodon''
at Fossilworks.org
* ''S. aftoniae'' * ''S. mirificus'' * ''S. nebrascensis'' * ''S. primitivus'' ''S. waringi'' is considered synonymous with ''S. platensis''. A dispute now exists over whether ''S. platensis'' should remain within the North and Central American genus ''Stegomastodon'' or should be moved over to the exclusively South American gen ...
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Stegodon
''Stegodon'' ("roofed tooth" from the Ancient Greek words , , 'to cover', + , , 'tooth' because of the distinctive ridges on the animal's molars) is an extinct genus of proboscidean, related to elephants. It was originally assigned to the family Elephantidae along with modern elephants but is now placed in the extinct family Stegodontidae. Like elephants, ''Stegodon'' had teeth with plate-like lophs that are different from those of more primitive proboscideans like gomphotheres and mastodons. The oldest fossils of the genus are found in Late Miocene strata in Asia, likely originating from the more archaic ''Stegolophodon,'' shortly afterwards migrating into Africa. While the genus became extinct in Africa during the Pliocene, ''Stegodon'' remained widespread in Asia until the end of the Pleistocene. Morphology Size Some species of ''Stegodon'' were amongst the largest proboscideans. ''S. zdanskyi'' is known from an old male (50-plus years old) from the Yellow River that is tall ...
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Cuvieronius
''Cuvieronius'' is an extinct New World genus of gomphothere, named after the French naturalist Georges Cuvier. Alive, specimens typically stood about tall at the shoulder, weighed about and would have superficially resembled a modern elephant with spiral-shaped tusks. Taxonomy The species now known as ''Cuvieronius hyodon'' was among the first fossil animals from the New World to be studied. The first remains of this species were recovered from Ecuador by Alexander von Humboldt, at a location the local population referred to as the "Field of Giants".Mayor, A. (2005). Fossil legends of the first Americans. Princeton University Press. Humboldt recognized that, rather than being bones of giant humans as had been thought by the local population and previous Spanish colonists, they were similar to the giant elephants (''Mastodon'') being described from Ohio. Humboldt sent teeth that he had collected from Mexico, Ecuador, and Chile to French anatomist Georges Cuvier, who classifie ...
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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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Rhynchotherium
''Rhynchotherium'' is an extinct genus of proboscidea endemic to North America and Central America during the Miocene through Pliocene from 13.650 to 3.6 Ma, living for approximately . This gomphothere had two tusks and may have evolved from ''Gomphotherium''. Taxonomy ''Rhynchotherium'' was first described in 1868 on the basis of a lower jaw from the Miocene of Tlaxcala, Mexico. Later, the type species epithet ''R. tlascalae'' was erected for the jaw by Henry Fairfield Osborn in 1918. In 1921, a gomphothere skull from the Mt. Eden area of southern California was described as a subspecies of ''Trilophodon shepardi'' (a now-defunct combination for ''Mastodon shepardi''), ''T. s. edensis'', but was subsequently reassigned to ''Rhynchotherium''. Other species subsequently assigned to ''Rhynchotherium'' included ''R. falconeri'', ''R. paredensis'', ''R. browni'', and ''R. simpsoni''. It was the closest relative to ''Cuvieronius'', and may be ancestral to it. Lucas and Morgan (20 ...
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Cenozoic Mammals Of Asia
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that larg ...
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