Cuvieronius is an extinct New World genus of gomphotheres and is 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". 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 being described from Ohio. Humboldt sent teeth that he had collected from Mexico, Ecuador, and Chile to French anatomist Georges Cuvier, who classified the teeth into two species, which he referred to as the "mastodonte des cordilières" and the "mastodonte humboldtien", in an 1806 paper. It was not until 1824 that Cuvier formally named the species. He referred both to the genus Mastodon, calling them M. andium and M. humboldtii. Unknown to Cuvier, Fischer had, in 1814, already named the two species based on Cuvier's original description, in the new genus Mastotherium as M. hyodon and M. humboldtii. The idea of two distinct species continued to be accepted into the 20th century, usually using Cuvier's names, though Fischer's names were older. In 1923, Henry Fairfield Osborn recognized that these species were distinct from Mastodon, and assigned each to its own new genus, as Cuvieronius humboldtii and Cordillerion andium. However, by the 1930s, general agreement had shifted to regard both forms as representing a single, geographically widespread species, with Cuvieronius humboldtii considered to be the correct name. During the 1950s, the nomenclature of this species became increasingly tangled, as various scientists regarded the type species of the genus Cuvieronius to be Fischer's first published name Mastotherium hyodon, rather than the originally designated Mastodon humboldtii. This situation went unaddressed until 2009, when Spencer Lucas petitioned the International Commission on Zoological Nomenclature to officially change the type species of Cuvieronius to M. hyodon as had been followed for over 50 years by that time, rather than abandoning the well-known Cuvieronius as a synonym. In 2011, Opinion 2276 of the ICZN ruled to conserve the names.
Evolution
Cuvieronius initially evolved in North America during the Late Pliocene. It is considered closely related to, if not derived from, Rhynchotherium, a North Americangomphothere genus known from the Late Miocene and Pliocene. Cuvieronius was expirated from most of North America during Irvingtonian after the arrival of mammoths in North America around 1.3 Ma, presumably due to competitive exclusion by mammoths and mastodons, but persisted in southern North America until the very end of the Pleistocene. During the Great American Interchange, Cuvieronius and a relative, Notiomastodon, dispersed into South America. Cuvieronius apparently reached South America considerably later than Notiomastodon, with the oldest possible date being 0.76 ±0.03 Mya and the oldest confirmed date being 304 ±54 ka, and had a much more restricted range, confined mostly to the Andes. Cuvieronius remains have been identified as far south as Chile, with remains initially suggested to represent Cuvieronius at the Quereo I site dating to the Late Pleistocene 11,600—11,400 BP. However, more recent studies suggest that they were extirpated from South America by the end of the Late Pleistocene, before the arrival of people.
Distribution and habitat
The oldest fossil remains to date are of Cuvieronius species found in Lincoln County, Nevada, which date to an accurate 4.6 million years ago. It was also found as far east as South Carolina and North Carolina in Pleistocene rocks dating to 1.81 million to 126,000 years ago. In Florida, remains show both Cuvieronius living from 2 to 0.5 Mya. The most recent findings of Cuvieronius in North America are in Sonora, Mexico, that date to 13,390 years BP at a Clovis culture kill site. As well as remains found near the town of Hockley in Texas near Austin, which date to around 24,000 years BP. According to a group of Brazilian mammalogists, many sites in South America referred to Cuvieronius actually refer to Notiomastodon, with many previous studies simply labeling fossils one or the other depending on location, with only localities definitely identified as Cuvieronius, the range now extends in the high Andes from Ecuador in the north, to Bolivia in the south, with the localities in the southern Andes in Chile and Argentina now thought to belong to Notiomastodon. The same group maintains that all the South American specimens represent the single species C. hyodon, and that no confirmed fossils of Cuvieronius are more recent than 44,000 years ago in South America, so the species would not have been in South America at the time of human arrival. By the end of the Pleistocene, the northern limit of the range of Cuvieronius was in Mexico and Central Texas. Fossils of Cuvieronius have been found in the Ulloma and Tarija Formations of Bolivia, the Sabana Formation of Colombia, Costa Rica, Ecuador, El Salvador, Guatemala, Mexico, Nicaragua, Panama, United States, and Venezuela. An account has Cuvieronius remains being found in Ecuador with human artifacts dated around 200 to 400 AD.
