Elasmotherium
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Elasmotherium (from Ancient Greek ἔλασμα (élasma), meaning "metal plate" with the intended meaning "lamina" in reference to the tooth enamel, and θηρίον (theríon), meaning "beast") is an extinct genus of very large rhinoceros that lived in Eastern Europe, Central Asia and East Asia from the late Miocene through to the Late Pleistocene, until at least 39,000 years ago. It was the last surviving member of the subfamily Elasmotheriinae, a formerly diverse group of rhinoceroses separate from the subfamily Rhinocerotinae, that contains all living rhinoceroses.
Five species are recognised. The genus first appeared in the Late Miocene in present-day China, likely having evolved from Sinotherium, before spreading to the Pontic–Caspian steppe, the Caucasus and Central Asia. Species of Elasmotherium are the largest known true rhinoceroses, reaching body lengths of at least Template:Convert, shoulder heights of over Template:Convert, and estimated body masses of Template:Convert, comparable to an elephant. The skull exhibits a large dome on the top of the skull roof, which is hollow and forms an enlargement of the nasal cavity. No remains of a horn of Elasmotherium have ever been found and the appearance of the horn, if any, has been subject to considerable speculation. Elasmotherium sibericum has often been conjectured and depicted as having borne an enormous nearly Template:Convert long straight horn projecting from the dome. However, a 2021 study found that such a horn was implausible due to the thinness of the outer wall of the dome and the lack of attachment points for a horn on the dome itself, and suggested that the dome (which they proposed was primarily for enhancing the sense of smell) was instead covered by a hard keratinous pad (comparable to the bosses of muskox and African buffalo) and that may have resembled a small horn in mature males.
Elasmotherium is thought to have had a relatively narrow and specialised ecological niche as an inhabitant of the central Eurasian steppe. The high crowned (becoming evergrowing/hypselodont in E. sibiricum, uniquely among rhinoceroses) and complicated enamel pattern of Elasmotherium teeth indicate that they had an abrasive diet of low growing vegetation. Elasmotherium may have fed on grass and/or used its well muscled head to turn over the soil to feed on roots and other subterranean parts of plants.
Elasmotherium has sometimes been claimed to be the basis of the mythical unicorn, though the evidence in support of this hypothesis is highly speculative.
Taxonomy
Elasmotherium was first described in 1808-1809 by German/Russian palaeontologist Gotthelf Fischer von Waldheim based on a left lower jaw, four molars, and the tooth root of the third premolar, which was gifted to Moscow University by princess Ekaterina Dashkova in 1807. He first announced the genus name at an 1808 presentation before the Moscow Society of Naturalists, and named the type species E. sibiricum a year later in 1809.<ref>Template:Cite journal</ref><ref name="Zhegallo2005">Template:Cite journal</ref>
The genus name derives from Ancient Greek ἔλασμα (élasma), meaning "metal plate", with the intended meaning "lamina", in reference to the laminated folding of the tooth enamel; and θηρίον (theríon), meaning "beast" and the species name sibericum is probably a reference to the predominantly Siberian origin of Princess Dashkova's collection. However, the specimen's exact origins are unknown. The specimen narrowly escaped destruction by being evacuated to Nizhny Novgorod during the French invasion of Russia in 1812, when most of the rest of Dashkova's collection was destroyed. The specimen was transferred to the Palaeontological Institute of the Academy of Sciences of the USSR (now the Russian Academy of Sciences) in Moscow during the mid-20th century.<ref name="Zhegallo2005" />
Due to the initially limited known remains and the unique morphology of Elasmotherium, for much of the 19th century its affinities to other mammals were the subject of considerable speculation. Fischer suggested in his original description that Elasmotherium was a "pachyderm which finds a place between elephants and rhinoceroses", while others such as Georges Cuvier in 1817, Anselme Gaëtan Desmarest in 1820, and Richard Owen in 1845 saw it as a "missing link" between rhinoceroses and horses, Henri Marie Ducrotay de Blainville in publications from 1839-1864 suggested that it was an "edentate", and Henri Milne-Edwards in 1868 proposed that it was an aquatic, possibly even marine mammal. Johann Jakob Kaup in 1840-41 was the first author to recognise that Elasmotherium was a rhinoceros, a view followed by Charles Lucien Bonaparte in 1845, who created the group Elasmotheriina to house it. Other authors supporting Elasmotherium as a rhinoceros include George Louis Duvernoy in 1852, who in 1855 erroneously assigned a partial skull correctly attributed to Elasmotherium by Kaup to the new genus and species Stereoceros galli. In 1877, Johann Friedrich von Brandt described the first complete skull of Elasmotherium sibiricum, which put to rest the debate about its affinities and demonstrated unequivocally that Elasmotherium was a rhinoceros.<ref name="Zhegallo2005" /><ref name=":4">Antoine, P. O. Phylogénie et évolution des Elasmotheriina (Mammalia, Rhinocerotidae) (Muséum national d'Histoire naturelle, 2002). (In French with English abstract)</ref>24-25 In 1916, a new genus, Enigmatherium and species E. stavropolitanum were named by Pavlova based on a single tooth found in the Northern Caucasus. This species was later recognised as a synonym of E. fischeri, named by Desmarest in 1820, which itself is now considered a synonym of the type species E. sibiricum.<ref name="Zhegallo2005" />
Evolution
Elasmotherium belongs to the subfamily Elasmotheriinae, distinct from the subfamily which includes all living rhinoceroses, Rhinocerotinae. The depth of the split between Elasmotheriinae and Rhinocerotinae is disputed. Older estimates place the age of divergence around 47 million years ago, during the Eocene,<ref name="Kosintsev2018">Template:Cite journal</ref> while younger estimates place the split during the Oligocene, around 35-23 million years ago.<ref name=":5">Template:Cite journal</ref><ref name=":3">Template:Cite journal</ref> Unambiguous members of Elasmotheriinae first appeared during the Early Miocene, and the subfamily was speciose and widespread across Europe, Africa and Asia during the Miocene epoch.<ref>Template:Cite journal</ref>
Cladogram of Rhinocerotidae after Borrani et al. 2025 (note: only a limited selection of elasmothere genera were included in the tree).<ref>Template:Cite journal</ref> Template:CladeCladogram of Elasmotheriina (the subgroup including core members of Elasmotheriinae) after Sun et al. 2023:<ref>Template:Cite journal</ref>Template:Clade Elasmotherium is the only known member of Elasmotheriinae to haved survived after the Early Pliocene.<ref name="Antoine-20252">Template:Citation</ref> with elasmotheriines declining as part of a broader decline of rhinocerotids and many other species of mammals during the late Miocene period.<ref>Template:Cite journal</ref> After originating and initially evolving in China (likely from Sinotherium) during the latest Miocene and Pliocene,<ref name=":6">Template:Cite journal</ref> Elasmotherium migrated westwards into Central Asia and Eastern Europe around 2.6 million years ago, during the earliest part of the Pleistocene epoch.<ref name=":8">Template:Cite journal</ref><ref name=":7" /> Elasmotherium became extinct in China by the end of the Early Pleistocene, around 1 million years ago.<ref name=":7" />
Elasmotherium is the only known member of Elasmotheriinae to haved survived after the Early Pliocene.<ref name="Antoine-20252">Template:Citation</ref> with elasmotheriines declining as part of a broader decline of rhinocerotids and many other species of mammals during the late Miocene period.<ref>Template:Cite journal</ref> After originating and initially evolving in China (likely from Sinotherium) during the latest Miocene and Pliocene,<ref name=":6">Template:Cite journal</ref> Elasmotherium migrated westwards into Central Asia and Eastern Europe around 2.6 million years ago, during the earliest part of the Pleistocene epoch.<ref name=":8">Template:Cite journal</ref><ref name=":7" /> Elasmotherium became extinct in China by the end of the Early Pleistocene, around 1 million years ago.<ref name=":7" />
Species
The oldest known species of Elasmotherium is Elasmotherium primigenium from the late Miocene (sometime between around 9 and 5.3 million years ago) of Dingbian County in Shaanxi, China,<ref name=":6" /> though some authors have doubted the attribution of this species to Elasmotherium.<ref name=":1" /> This species is distinguished from later Elasmotherium species by its more primitive tooth morphology. Like later species, it has the characteristic dome on the skull roof.<ref name=":6" />
There are four largely successive species of Elasmotherium aside from the aforementioned E. primigenium, which are—from oldest to youngest—E. chaprovicum, E. peii, E. caucasicum and E. sibiricum, and which together span from the Late Pliocene to the Late Pleistocene.<ref name=":02">Template:Cite journal</ref> Elasmotherium species are largely distinguished by differences in their tooth anatomy.<ref name=":7" />
Remains of Elasmotherium from the Khaprovian or Khaprov Faunal Complex, which was at first taken to be E. caucasicum,<ref>Template:Cite web</ref> and then on the basis of the dentition was redefined as a new species, E. chaprovicum (Shvyreva, 2004), named after the Khaprov Faunal Complex.<ref name="titov226">Template:Cite book</ref> The Khaprov is in the Middle Villafranchian, MN17, which spans the Piacenzian of the Late Pliocene and the Gelasian of the Early Pleistocene of Northern Caucasus, Moldova and Asia and has been dated to 2.6–2.2 Ma.<ref>Template:Cite web</ref> This species is characterised by the relative thickness and roughness of its irregularly folded tooth enamel, its massive metapodial bones, and the morphology of the talus bone of the foot, which are relatively low, have a narrow trochlea and a wide part closest to the (distal) tip of the foot.<ref name=":7" /> E. chaprovicum may have existed at the same time as early members of E. peii lived in China.<ref name=":7" />
E. peii was first described by Chow, 1958 for remains found in Shaanxi, China.<ref>Chow, M.C., 1958. New elasmotherine Rhinoceroses from Shansi. Vertebrato PalA-siatica 2, 135-142.</ref> The species is also known from numerous remains from the classical range of Elasmotherium, and some sources have considered this species to be a synonym of E. caucasicum, but it is currently considered distinct.<ref name=":02" /> In the western part of its range, it is mainly found in the Psekups faunal complex between 2.2 and 1.6 Ma.<ref name=":02" /> In China, E. peii is considered to be the only Pleistocene species of Elasmotherium, spanning from around 2.6 Ma until at least 1.36 Ma, though its remains in China are rare and only known from a handful of localities.<ref name=":7">Template:Cite journal</ref> This species is distinguished from other Elasmotherium species by several aspects of its dental anatomy, with the teeth being characterised by early closure of the roots, though the roots remain distinct from the crown of the tooth, and several morphological characters of the teeth, including the persistent presence of a postfossette (a depression of the tooth surface), as well as the shape of the protoloph and metaloph (which are raised areas of teeth).<ref name=":7" />
E. caucasicum was first described by Russian palaeontologist Aleksei Borissiak in 1914. It is placed as part of the Early Pleistocene Tamanian Faunal Unit (1.55–0.8 Ma, named after the Taman Peninsula). E. caucasicum is more primitive than E. sibiricum and likely represents its direct ancestor.<ref name=":8" /><ref name=":7" /> The teeth of E. caucasicum are distinguished from earlier species by their more complex enamel folding, and from E. sibiricum by having larger teeth and a relatively elongate tooth row.<ref name=":7" /> E. caucasicum also differs from the later E. sibiricum in some aspects of its limb bone morphology.<ref name=":0">Deng, T. & Zheng, M. Limb bones of Elasmotherium (Rhinocerotidae, Perissodactyla) from Nihewan (Hebei, China). Vert. PalAs. 43, 110–121 (2005).</ref>
E. sibiricum, described by Johann Fischer von Waldheim in 1808 and chronologically the latest species of the sequence appeared in the Middle Pleistocene, ranging northwards to southern-central Russia, westwards into Ukraine and Moldova in Eastern Europe,<ref>Template:Cite book</ref> eastwards into eastern Kazakhstan and southwards to Uzbekistan in Central Asia, and into Azerbaijan in the Caucasus.<ref name="Kosintsev2018" /> This species is distinguished from earlier Elasmotherium by having smaller teeth, a reduced number of premolars, open rooted (evergrowing) molars, as well as very thin and highly complicated enamel folding in the cheek teeth.<ref name=":7" />
Description
Elasmotherium is the largest known rhinocerotid,<ref>Template:Cite journal</ref> and one of the largest members of Rhinocerotoidea, excluding the largest paraceratheres like Paraceratherium.<ref name=":2">Template:Cite journal</ref>supplementary material The largest known specimens of E. sibiricum reach up to Template:Convert in length, with shoulder heights of over Template:Convert,<ref name="Zhegallo2005" /> with a 2018 study estimating a body mass of around Template:Convert,<ref name="Kosintsev2018" /> while extrapolations based on isolated teeth of E. caucasicum, which are larger than those of E. sibiricum, suggest the largest E. caucasicum individuals may have reached Template:Convert in body length and a body mass of Template:Convert.<ref name="Zhegallo2005" /><ref>Template:Cite book</ref> These make Elasmotherium comparable in size to the woolly mammoth (Mammuthus primigenius) and larger than the contemporary woolly rhinoceros (Coelodonta antiquitatis).<ref>Template:Cite journal</ref><ref name="Cerdeno1998">Template:Cite journal</ref>
The cervical vertebrae of the neck were very robust,<ref name="Zhegallo2005" /> with the atlas (the first neck vertebra that articulates with the skull) in particular having broad wings up to Template:Convert across, exceeding the width of the skull.<ref name=":1" /> The posterior neck vertebrae,<ref name=":1" /> as well as the thoracic vertebrae of the back have elongate neural spines, reaching up to Template:Convert in length.<ref name="Zhegallo2005" /> The neck of Elasmotherium is thought to have been heavily muscled.<ref name=":1" /> Compared to living rhinoceroses, a number of bones of the limbs, including the radius, tibia, astragalus (talus) and metapodials are relatively elongate, though the humerus and ulna are proportionally similar in size to living rhinoceroses.<ref name=":7" /> The feet were unguligrade, the front larger than the rear, with three digits at the front and rear, with a vestigial fifth metacarpal.<ref>Template:Cite journal</ref>
Elasmotherium is typically reconstructed covered in a considerable layer of fur, generally based on the woolliness exemplified in contemporary megafauna such as woolly mammoths and the woolly rhinoceros. However, it is sometimes depicted as bare-skinned like modern rhinoceroses.<ref name="Zhegallo2005" />
Skull
The skulls of E. sibiricum were large and relatively elongate, reaching a length of Template:Convert in mature male individuals. The skull is less than half as wide at maximum width as it is long. The nasal septum is heavily ossified (bony) rather than cartilaginous.<ref name=":1" /> The forward, upper and lower rims of the orbits (eye sockets) are distinctly protuberant, with the back part of the orbit being open. The skull has large areas for the attachment of the neck muscles, including two paired growths on the occipital bone at the back of the skull, which extend further back than the occipital condyles (where the skull articulates with the neck vertebrae).<ref name=":1" />
The most conspicuous feature of the skull of Elasmotherium is the large dome on the top of the frontal bone of the skull roof, generally around Template:Convert in diameter. The development of the dome depended on age and sex, being more developed in adult and especially in male individuals. The dome is covered in a rough hummocky texture of uniformly spaced tubercules, though the degree to which this roughness was developed varies considerably between individuals, with some individuals, assume to be female, exhibiting relatively little roughness on the dome. Unlike living rhinoceroses, these tubercules were not arranged into ring-like structures. Along the side of the domes ran sulci grooves, which in life would have supported arterial blood vessels. The interior of the dome was largely hollow, and formed an extension of the nasal cavity, and the sinuses, with the interior of the dome being divided into two halves by the bony nasal septum, with the hollow space being filled with numerous thin walls which would have been covered in mucous membranes, with the outer wall of the dome being relatively thin, varying from Template:Convert thick across the dome.<ref name=":1" />
Elasmotherium sibiricum had two premolars and three molars in each half of both the upper and lower jaws, and lacked any incisors or canines.<ref name="Zhegallo2005" /> These teeth were very high crowned (hypsodont), the highest crowned among ungulates, and the molars of E. sibiricum were evergrowing (hypselodont) similar to those of many rodents but uniquely among rhinoceroses (ever growing cheek teeth also evolved in South American notoungulates).<ref>Template:Cite journal</ref><ref name=":1" /> In E. sibiricum, the teeth completely lacked roots in adult teeth, though some earlier Elasmotherium species had roots in their adult teeth.<ref name=":1" /> The cheek teeth exhibit highly complex laminated enamel folding,<ref name="Zhegallo2005" /> which is more pronouncedly developed in later species.<ref name=":7" /> The roughness of the nasal bone and the interior of the nasal septum suggests that Elasmotherium had a relatively mobile prehensile upper lip.<ref name=":1" />
Cranial ornamentation
No preserved soft tissue remains surrounding the dome of Elasmotherium have been found, resulting in a number of different hypotheses regarding its life appearance. Beginning with the first reconstructions of Elasmotherium by Rashevsky under Brant's guidance in 1878, many authors have contended that the dome in Elasmotherium served as the base for a large keratinous horn,<ref name="Zhegallo2005" /> often conjectured to be around Template:Convert long.<ref name=":2" />supplementary material This interpretation, while widely popularised in encyclopedias and other works,<ref name="Zhegallo2005" /> has not been without its critics, such as Valentin Teryaev in 1948, who argued that a much smaller covering of the dome was present instead.<ref name=":1" />
A 2021 study by Vadim Titov and colleagues supported Teryaev's view, and found that the cranial dome was quite fragile because it was largely hollow, and only had a thin outer wall, and was therefore ill suited for a large horn, and the pattern of the rugosity of the skull did not match the structure found at the base of the horns of living rhinoceroses, and was instead indicative of a smaller cornified (hard) keratinous covering, likely similar to the keratinous bosses present on the heads of muskox (Ovibos moschatus) and African buffalo (Syncerus caffer), that may have resembled a small horn in mature male individuals, which served primarily to protect the fragile dome, and that the dome, as an enlargement of the nasal cavity, primarily functioned to enhance the sense of smell, and possibly secondarily as a resonating chamber for vocalisation in males. They also proposed, based on the roughness of the bone in the area, that the front tip of the snout had another keratinous pad that was used for scraping the ground.<ref name=":1">Template:Cite journal</ref>
Palaeobiology
The angle made by the intersection of the plane of the occipital bone with the skull base is around 105–115°, indicating that the head was habitually held low,<ref name=":1" /> even lower than the living white rhinoceros (Ceratotherium simum),<ref name="Kosintsev2018" /> which has resulted in it being widely agreed among researchers that Elasmotherium predominantly fed on low-growing vegetation.<ref name=":1" /><ref name="Made2010">Template:Cite book</ref>
Valentin Teryaev in 1948 argued that Elasmotherium was a semi-aquatic animal that lived within and in close proximity to water including riverbanks and ponds, feeding on aquatic and nearshore plants with an ecology and physical appearance similar to a hippopotamus. Part of Teryaev's argument was based on the supposed presence of a fourth functional digit in the forefeet of Elasmotherium, similar to tapirs which predominantly inhabit wet environments, but this idea was later shown to be incorrect. Some other authors, while not necessarily agreeing with Teryaev's idea of a semi-aquatic Elasmotherium, have suggested that it predominantly lived near water, such as along river valleys, and foraged on aquatic and semi-aquatic plants.<ref name="Zhegallo2005" /><ref name=":1" /> However, other researchers have disagreed with this assessment, and argued that Elasmotherium primarily inhabited open terrestrial environments, including steppe, forest steppe and meadows.<ref name=":1" /><ref name="Kosintsev2018" /> Analysis of carbon and nitrogen isotopes, which resemble those of other steppe dwelling animals, has been argued to support the idea of a steppe-dwelling niche for Elasmotherium.<ref name="Kosintsev2018" /> Elasmotherium sibiricum frequently co-occurs with other steppe-dwelling animals in the fossil record, such as the saiga antelope (Saiga tatarica), the extinct large camel Camelus knoblochi, Irish elk (Megaloceros giganteus), steppe bison (Bison priscus), and mammoths (Mammuthus chosaricus).<ref>Template:Cite journal</ref>
Modern high crowned (hypsodont) hoofed mammals are generally grazers of open environments,<ref>Template:Cite journal</ref> with the wrinkled enamel of Elasmotherium teeth suggested to possibly be an adaptation to feeding on tough, fibrous grass.<ref>Template:Cite journal</ref> The high crowned teeth of Elasmotherium have either been suggested to an adaptation for feeding on grass or to compensate from the wear caused by the intake of grit on the food it was eating.<ref name="Kosintsev2018" /> Dental wear analysis indicates that E. caucasicum and E. sibiricum had a highly abrasive diet, suggested to be the result of a high amount of sandy grit in the soil covering the food they ingested.<ref name=":1" />
The morphology of skull and neck vertebrae suggest that Elasmotherium had the ability to powerfully move its head from side to side (laterally), and combined side to side and upwards motion (dorsolaterally). A number of authors have argued based on multiple lines of evidence, including skull morphology (such as the protuberant eyesocket rims, heavily ossified snout, and enlarged nasal cavity) and carbon and nitrogen isotope ratios (which are highly distinct from those of other rhinoceroses), that Elasmotherium likely heavily fed on roots and other underground parts of plants such as rhizomes, bulbs and tubers, perhaps to an even greater degree than above-ground parts of plants, using their keratinous pad near the front of the snout (rather than the one on the dome), in combination with their powerful neck muscles, to disturb and turn over soil in search of food. Elasmotherium may have moved between different habitats, such as forest, steppe and meadows, seasonally to feed on different plant resources.<ref name=":1" /><ref name="Zhegallo2005" />
If the dome functioned as a resonating chamber, it may have been used to amplify loud vocalisations by males, perhaps to attract females and/or to indicate/assert control of territory.<ref name=":1" /> Analysis of the limb bones of Elasmotherium suggests that despite its large size, it was probably capable of moving at considerable speed.<ref name="Kosintsev2018" />
At the latest Middle Pleistocene-early Late Pleistocene Irgiz 1 site in European Russia, 7 Elasmotherium sibiricum individuals, ranging from adults to juveniles, appear to have died together in a catastrophic event. Dental microwear analysis, which records an animals diet in their last days/weeks of life, suggests they switched from a low-growing vegetation/grazing diet typical for Elasmotherium (as indicated by their tooth mesowear, which records their long-term diet spanning months to years before death), towards an atypical browsing diet shortly before their death. This may suggest that the Elasmotherium individuals died due to starvation as a result of the ground being covered in an abnormally thick layer of snow, forcing them to attempt to feed on shrubs and other vegetation above the snow layer.<ref>Template:Cite journal</ref>
Relationship with humans and extinction
Elasmotherium sibiricum was previously thought to have gone extinct during the late Middle Pleistocene, around 200,000 years ago as a background extinction, but radiocarbon dates obtained from specimens found in southern European Russia shows its persistence in the region until at least 39,000 and possibly as late as 35,000 years ago, indicating that Elasmotherium survived well into the Last Glacial Period.<ref name="Kosintsev2018" /> A claimed later radiocarbon date of around 29,000 years ago from Pavlodar, in northern Kazakhstan is not considered credible.<ref name="Kosintsev2018" /> These late dates place Elasmotherium's extinction within the timeframe of the late Quaternary extinction event, when most large terrestrial animals became extinct, generally thought to be the result of climate change, hunting by the globally expanding population of modern humans, or the combination of both. However, there is very little evidence of human interaction with Elasmotherium, and their remains have never been found in any confirmed archaeological context. The last records of Elasmotherium, which date to Marine Isotope Stage 3, correspond to a period of pronounced climatic and environmental change induced by the oscillation between relatively warm interstadial and cool stadial periods, with the last records dating to around the onset of Heinrich stadial 4/Greenland stadial 8, caused by a Heinrich event (a large group of icebergs simultaneously breaking off the North American Laurentide Ice Sheet and travelling into the North Atlantic), corresponding with pronounced cooling, the disruption of grass and herb dominated ecosystems and the spread of the mammoth steppe-tundra across northern Eurasia. The specialised ecology and restricted geographical distribution of Elasmotherium may have contributed to its extinction.<ref name="Kosintsev2018" />
A claimed Late Pleistocene presence in Western Europe, based on a cave painting in Rouffignac Cave in France, which depicts a rhinoceros with a large single horn, has been doubted, because of the complete lack of any Western European remains of Elasmotherium,<ref name=":4" />46-47 and other authors have considered this to be a depiction of the woolly rhinoceros.<ref name="Zhegallo2005" /> Other claimed depictions of Elasmotherium have been reported from Shulgan-Tash Cave in the southern Russian Urals, though other authors have considered the claims to be unproven, due to the ambiguous nature of the ochre drawings, and these could again be depictions of the woolly rhinoceros.<ref name="Zhegallo2005" />
Since the 19th century, Elasmotherium has been claimed to be the origin of folkloric creatures, particularly the unicorn, though the evidence in support of this hypothesis is conjectural, and Elasmotherium does not appear to have inhabited the areas where the mythological unicorn is thought to have originated, and the depiction of the unicorn may have been influenced by living rhinoceroses rather than Elasmotherium.<ref name="Zhegallo2005" /> As a consequence, E. sibiricum has sometimes been nicknamed the "Siberian Unicorn".<ref name="Kosintsev2018" />
See also
References
Further reading
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