Camelops

History of research Camelops was first named by Joseph Leidy in 1854, based on a partial maxilla (upper jawbone), that was found in a gravel drift somewhere in the Kansas Territory, with Leidy naming the type species Camelops kansanus in the same publication based on the maxilla. Later authors have judged that while the jawbone undoubtedly represents Camelops, it is too fragmentary to be diagnostic to species, making C. kansanus a nomen dubium. Later in 1874, Leidy named the species Camelops hesternus, based on teeth found in a gravel deposit in Arroyo Las Positas in Livermore Valley, Alameda County in the southern Bay Area of California. Several other species, including Camelops sulcatus named by Edward Drinker Cope in 1893 based on a partial left mandible, found at Rock Creek, Texas, as well as Camelops huerfanensis, named by Francis Whittemore Cragin in 1892 based on remains found along the Huerfano River in Colorado (as well as its claimed subspecies Camelops huerfanensis dallasi named by Richard Swann Lull in 1921 for remains collected along the Trinity River in northeast Texas), Camelops aransas named by Oliver Perry Hay in 1926 for remains including a partial right mandible found on a bank of the Aransas River in southeast Texas, and Camelops traviswhitei named by Mooser and Dalquist in 1975 from remains found in Aguascalientes in central Mexico, are now regarded as junior synonyms of C. hesternus. Another species, C. minidokiae, named by Hay in 1927 for jaw and teeth remains found in a gravel bed near Minidoka, Idaho, has been suggested to also be potentially valid, given its apparently smaller size than C. hesternus, though other authors have suggested that it is another synonym for C. hesternus. This species is primarily recorded during the Irvingtonian (Early-Middle Pleistocene), though some remains of the species have been reported from the Rancholabrean (late Middle-Late Pleistocene). Evolution The family Camelidae, which contains the living camels, as well as lamines (the tribe Lamini, which includes the llama, guanaco, alpaca and vicuña), first emerged in North America during the Eocene, around 46-42 million years ago, reaching its apex of diversity during the Miocene epoch (23-5.3 million years ago). The two modern tribes of Camelidae, Camelini and Lamini, are suggested to have diverged during this period, around 17.5-16 million years ago. Living camels are thought to descend from Paracamelus, which crossed the Bering Land Bridge into Eurasia from North America during the Late Miocene, around 6 million years ago. Although historically often assigned to Lamini,}}}}|label1=Camelidae}}The oldest fossils of Camelops are known from southern North America, dating to around 4-3.2 million years ago during the Pliocene epoch. but by the Late Pleistocene (Rancholabrean), Camelops represented the last remaining camel in the Americas. ==Description==

Camelops hesternus was a large camel with a bodyform similar to a living dromedary, reaching a shoulder height of with body mass estimates ranging from to , to around , Whether Camelops had humps or not like living camels is uncertain. The skull has 1 incisor, 1 canine, 2 premolars and 3 molars in each half of the upper jaw, and 3 incisors, 1 canine, 1 premolar and 3 molars in each half of the lower jaw. The upper first premolar and both upper and lower second premolars are absent, with the lower first premolar usually absent and only occasionally present. The molar and premolar teeth are very high-crowned (hypsodont), with the molars being slender relative to their length, with the canines, upper third premolar and lower fourth premolar being reduced in size. The premaxilla bone is robust, with the rostrum of the skull being elongate, with the facial region of the skull not exhibiting considerable shortening. The nasal bones are strongly arched. The brain is relatively large, estimated at . The mandible is relatively deep. The limbs are relatively elongate (around 20% longer than those of living dromedaries) but robust. The metapodial bones are robust and relatively short. == Distribution, habitat and ecology ==

of C. hesternus During the Pleistocene, Camelops is known from fossils across western North America, ranging from California, Oregon and Washington State, eastwards to South Dakota, Nebraska, Kansas, Oklahoma and Texas, with rarer records further east, including near the Missouri-Illinois border. The northernmost records of Camelops are known from Alaska and Yukon, but it probably only occupied this region during warm interglacial intervals, before becoming extirpated from the region during glacial periods, as is thought for some other species whose remains are also rarely found in the region, such as the ground sloth Megalonyx jeffersoni, mastodons and Castoroides giant beavers. Across its range it inhabited a wide variety of habitats, from subtropical environments, In parts of its range Camelops hesternus co-occurred alongside the lamines Hemiauchenia and Palaeolama. a plant also commonly found in the diet of living camels. but a 2021 dental wear analysis study suggested that in some locations such as in Nebraska, Camelops hesternus engaged in grazing, sometimes predominantly so, suggesting that Camelops hesternus was a flexible feeder. Isotopic analysis suggests that Camelops may have engaged in seasonal migrations. the sabertooth cat Smilodon fatalis, the scimitar-toothed cat (Homotherium serum) and the American lion (Panthera atrox). Specimens of Camelops have been found exhibiting signs of disease like osteoarthritis. == Relationship with humans and extinction ==

Camelops went extinct around 13-12,000 years ago as part of the end-Pleistocene extinction event along with most other large mammals across the Americas. These extinctions followed the arrival of humans to the Americas, and it is suggested that human hunting may have had a contributory role in the extinctions (though some authors have argued that climatic change was the most important factor Some authors have suggested that fractured bones of Camelops found near Casper, Wyoming (which also represent the youngest well-dated remains of the species, dating to around 13,060 years Before Present Other possible, but not definitive sites where Camelops remains may be associated with human activity include Carter/Kerr-McGee and Colby sites in Wyoming (the latter of which is associated with a Clovis point) and the Lehner site in Arizona. A sacrum of Camelops found near Tequixquiac in central Mexico has been suggested to have been shaped to resemble an animal head. ==See also==