2186:
118:
2459:
1825:
1915:
1676:
2382:
1312:
1816:
1156:
930:
740:
1147:
1009:
4543:
2086:
147:
2007:
1807:
2267:
2246:. Some Russian authors suggested that the tusks were probably used for breaking twigs, stripping bark and bending high branches and that, because species from the early Oligocene had larger tusks than later ones, they probably had a more bark than leaf based diet. Since the species involved are now known to have been contemporaneous, and the differences in tusks are now thought to be sexually dimorphic, the latter idea is not accepted today. Herds of
1737:
731:
2072:—similar to the running rhinoceroses from which they descended. Some foot bones were almost 50 centimetres (20 in) long. The thigh bones typically measured 1.5 m (4.9 ft), a size only exceeded by those of some elephants and dinosaurs. The thigh bones were pillar-like and much thicker and more robust than those of other rhinoceroses, and the three
1118:, based on remains too fragmentary to identify properly. By analysing alleged differences between named genera and species, Lucas and Sobus found that these most likely represented variation within populations, and that most features were indistinguishable between specimens, as had been pointed out in the 1930s. The fact that the single skull assigned to
702:, and Chinese scientists worked in isolation from each other for much of the 20th century and published research mainly in their respective languages. Scientists from different parts of the world tried to compare their finds to get a more complete picture of these animals, but were hindered by politics and wars. The opposing taxonomic tendencies of "
2486:. Prothero and the zoologist Pavel V. Putshkov have considered these causes unlikely since these animals managed to survive regardless of these issues for millions of years under the harsh conditions of their environment, and were not much larger than the biggest proboscideans, extinct as well as extant, which faced similar challenges.
1755:
because this species is known from the most complete remains. Estimates have been based on skull, teeth, and limb bone measurements, but the known bone elements are represented by individuals of different sizes, so all skeletal reconstructions are composite extrapolations, resulting in several weight
2335:
of
Mongolia represents an arid desert basin, and the environment is thought to have had few tall trees and limited brush cover, as the fauna consisted mainly of animals that fed from tree tops or close to the ground. A study of fossil pollen showed that much of China was woody shrubland, with plants
2241:
Granger and
Gregory argued that the large incisors were used for defence or for loosening shrubs by moving the neck downwards, thereby acting as picks and levers. Tapirs use their proboscis to wrap around branches while stripping off bark with the front teeth; this ability would have been helpful to
1969:
differed from the other species in that the nasal notch was deeper, with the bottom placed above the middle of molar M2, a proportionally higher occipital condyle compared to the occipital surface's height, short muzzle bones and diastema in front of the cheek teeth, and a high zygomatic arch with a
2505:, which would have been their most likely competitors. While cautioning that the true cause of their extinction will never be known for certain, Prothero found it to be more than a coincidence that paraceratheres disappeared just as large predators and other large herbivores entered Asia during the
2120:
would not have been able to run and move quickly, but they would have been able to cross large distances, which would be necessary in an environment with a scarcity of food. They may therefore have had large home ranges and have been migratory. Prothero suggests that animals as big as indricotheres
1644:
as separate genera. In 2016, the
Chinese researchers Haibing Wang and colleagues used the name Paraceratheriidae for the family and Paraceratheriine for the subfamily, and placed them outside of Hyracodontidae. Deng and colleagues confirmed previous studies with their 2021 analysis, suggesting that
2445:
had been able to migrate back north to
Central Asia during this time when that area had become tropical (it was arid during the early Oligocene). This implies the Tibetan region was not yet a high-elevation plateau that could act as a barrier, and large animals may therefore have been able to move
1759:
There are no indications of the colour and skin texture of the animal because no skin impressions or mummies are known. Most life restorations show the creature's skin as thick, folded, grey, and hairless, based on modern rhinoceroses. Because hair retains body heat, modern large mammals such as
995:
from the
Jiaozigou Formation of the Linxia Basin (to which the name refers) of northwestern China. A multitude of other species and genus names—mostly based on differences in size, snout shape, and front tooth arrangement—have been coined for various indricothere remains. Fossils attributable to
1788:
specimens known by then, using the proportions of a modern rhinoceros as a guide. The result was too squat and compact, and Osborn had a more slender version drawn later the same year. Some later life restorations have made the animal too slender, with little regard to the underlying skeleton.
2295:
finds implies that they inhabited a continuous landmass with a similar environment across it, but this is contradicted by palaeogeographic maps that show this area had various marine barriers, so the genus was successful in being widely distributed despite this. The fauna which coexisted with
2039:
were long and formed a long "hump" along the back, where neck muscles and nuchal ligaments for holding up the skull were attached. The ribs were similar to those of modern rhinoceroses, but the ribcage would have looked smaller in proportion to the long legs and large bodies, because modern
2121:
would need very large home ranges or territories of at least 1,000 square kilometres (250,000 acres) and that, because of a scarcity of resources, there would have been little room in Asia for many populations or a multitude of nearly identical species and genera. This principle is called
591:. The shoulder height was about 4.8 metres (15.7 feet), and the length about 7.4 metres (24.3 feet). Its weight is estimated to have been about 15 to 20 tonnes (33,000 to 44,000 lb). The long neck supported a skull that was about 1.3 metres (4.3 ft) long. It had large, tusk-like
1998:. The premolars only partially formed the pi pattern. Each molar was the size of a human fist; among mammals they were only exceeded in size by proboscideans, though they were small relative to the size of the skull. The lower cheek teeth were L-shaped, which is typical of rhinoceroses.
1279:. A 2004 paper by Deng and colleagues also recognised three distinct genera. Some western writers have similarly used names otherwise considered invalid since the 1989 revision, but without providing detailed analysis and justification. Deng and colleagues recognised six
2501:, and as their numbers dwindled, they would have become more vulnerable to other threats. Prothero has pointed out that gomphotheres are not known to have generally coexisted with paraceratheres, and there are no known co-occurrences between paraceratheres and the large
1750:
Early estimates of 30 tonnes (66,000 lb) are now considered exaggerated; it may have been in the range of 15 to 20 tonnes (33,000 to 44,000 lb) at maximum, and as low as 11 tonnes (24,000 lb) on average. Calculations have mainly been based on fossils of
2115:
may be large mammals such as elephants, rhinoceroses and hippopotamuses. To aid in thermoregulation, these animals cool down during the day by resting in the shade or by wallowing in water and mud. They also forage and move mainly at night. Because of its large size,
1699:
that have ever existed, but its precise size is unclear because of the lack of complete specimens. Its total body length was estimated as 8.7 m (28.5 ft) from front to back by
Granger and Gregory in 1936, and 7.4 m (24.3 ft) by the palaeontologist
1977:
were reduced to a single pair of incisors in either jaw, which were large and conical, and have been described as tusks. The upper incisors pointed downwards; the lower ones were shorter and pointed forwards. Among known rhinoceroses, this arrangement is unique to
2140:. Adult individuals would be too large for any land predators to attack, but the young would have been vulnerable. Bite marks on bones from the Bugti beds indicate that even adults may have been preyed on by 10-to-11-metre (33 to 36 ft)-long crocodiles,
2063:
with those of elephants and sauropod dinosaurs with their likewise graviportal (heavy and slow moving) builds. Unlike such animals, which tend to lengthen the upper limb bones while shortening, fusing and compressing the lower limb, hand, and foot bones,
1854:
had a long forehead, which was smooth and lacked the roughened area that serves as attachment point for the horns of other rhinoceroses. The bones above the nasal region are long and the nasal incision goes far into the skull. This indicates that
2185:
2076:
on the sides were much reduced, as this robustness diminished their importance. The limbs were held in a column-like posture instead of bent, as in smaller animals, which reduced the need for large limb muscles. The front limbs had three toes.
117:
1248:, the subfamily name Indricotheriinae is still in use because genus name synonymy does not affect the names of higher level taxa that are derived from these. Members of the subfamily are therefore still commonly referred to as indricotheres.
623:, eating mainly leaves, soft plants, and shrubs. It lived in habitats ranging from arid deserts with a few scattered trees to subtropical forests. The reasons for the animal's extinction are unknown, but various factors have been proposed.
1368:
forms. Most species did not have horns. Rhinoceros fossils are identified as such mainly by characteristics of their teeth, which is the part of the animals most likely to be preserved. The upper molars of most rhinoceroses have a
4123:
Sander, P. M.; Christian, A.; Clauss, M.; Fechner, R.; Gee, C. T.; Griebeler, E. M.; Gunga, H. C.; Hummel, J. R.; Mallison, H.; Perry, S. F.; Preuschoft, H.; Rauhut, O. W. M.; Remes, K.; Tütken, T.; Wings, O.; Witzel, U. (2011).
1898:
appears to have had large, strong neck muscles, which allowed it to sweep its head strongly downwards while foraging from branches. The upper profile of the skull was arched, a distinguishing feature of the genus. One skull of
2473:
and its relatives became extinct after surviving for about 11 million years are unknown, but it is unlikely that there was a single cause. Theories include that their large size was related to the now outdated concept of
2158:
may have lived in small herds, perhaps consisting of females and their calves, which they protected from predators. It has been proposed that 20 tonnes (44,000 lb) may be the maximum weight possible for land mammals, and
2030:
vertebrae of the neck were wider than in most modern rhinoceroses, with space for strong ligaments and muscles that would be needed to hold up the large head. The rest of the vertebrae were also very wide, and had large
1994:(gap). This feature is found in mammals where the incisors and cheek teeth have different specialisations. The upper molars, except for the third upper molar that was V-shaped, had a pi-shaped (π) pattern and a reduced
1783:
fossils, the skeleton of the animal has been reconstructed in several different ways since its discovery. In 1923, Matthew supervised an artist to draw a reconstruction of the skeleton based on the even less complete
2201:
was a browser with a diet consisting of relatively soft leaves and shrubs. Later rhinoceroses were grazers, with high-crowned teeth because their diets contained grit that quickly wore down their teeth. Studies of
1945:, mastoid-paroccipital processes that were relatively thin and placed back on the skull, a lambdoid crest, which extended less back, and an occipital condyle with a horizontal orientation, which it shared with
1890:, which are otherwise found in horned and tusked animals that need strong muscles to push and fight. It also had a deep pit for the attachment of nuchal ligaments, which hold up the skull automatically. The
2282:
have been found in early to late
Oligocene (34–23 million years ago) formations across Eurasia, in modern-day China, Mongolia, India, Pakistan, Kazakhstan, Georgia, Turkey, Romania, Bulgaria, and the
1724:
might have been taller than any proboscidean. Its shoulder height was estimated as 5.25 m (17.2 ft) at the shoulders by
Granger and Gregory, but 4.8 m (15.7 ft) by the palaeontologist
1444:
period, 23 to 34 million years ago. The genus is distinguished from other indricotheres by its large size, nasal incision that would have supported a muscular snout, and its down-turned
2250:
may have migrated while continuously foraging from tall trees, which smaller mammals could not reach. Osborn suggested that its mode of foraging would have been similar to that of the high-browsing
1768:. The ears of elephants enlarge the body's surface area and are filled with blood vessels, making the dissipation of excess heat easier. According to Prothero, this would have been true for
1667:
in the
Oligocene. These researchers did not find Hyracodontidae to form a natural group, and found Paraceratheriidae to be closer to Rhinocerotidae, unlike previous studies.
4173:
Antoine, P. O.; Ibrahim Shah, S. M.; Cheema, I. U.; Crochet, J. Y.; Franceschi, D. D.; Marivaux, L.; Métais, G. G.; Welcomme, J. L. (2004). "New remains of the baluchithere
1228:
from the late
Oligocene of Kazakhstan may be too incomplete for its position to be resolved in relation to the other species; the same applies to proposed species such as
4358:
Wang, Y.; Deng, T. (2005). "A 25 m.y. Isotopic record of paleodiet and environmental change from fossil mammals and paleosols from the NE margin of the Tibetan Plateau".
4225:
1031:
based on a palate and other fragments from Dera Bugti, thought to belong to a giant member of that genus. These fossils are now thought to have belonged to an aberrant
4323:
Martin, C.; Bentaleb, I.; Antoine, P. -O. (2011). "Pakistan mammal tooth stable isotopes show paleoclimatic and paleoenvironmental changes since the early Oligocene".
3187:"New data on Amynodontidae (Mammalia, Perissodactyla) from Eastern Europe: Phylogenetic and palaeobiogeographic implications around the Eocene-Oligocene transition"
2493:
proboscideans from Africa in the late Oligocene (between 28 and 23 million years ago) may have considerably changed the habitats they entered, like
4044:
1846:
are around 1.3 metres (4.3 ft) long, 33 to 38 centimetres (13 to 15 in) at the back of the skull, and 61 centimetres (24 in) wide across by the
1373:-shaped (π) pattern on the crown, and each lower molar has paired L-shapes. Various skull features are also used for identification of fossil rhinoceroses.
2163:
was close to this limit. The reasons mammals cannot reach the much larger size of sauropod dinosaurs are unknown. The reason may be ecological instead of
3494:
3468:
3390:
1400:(natural) grouping. Radinsky's scheme is the prevalent hypothesis today. The hyracodont family contains long-legged members adapted to running, such as
2550:
642:, have been named, but no complete specimens exist, making comparison and classification difficult. Most modern scientists consider these genera to be
839:. His rationale for this reclassification was the species' distinctly down-turned lower tusks. In 1913, Forster-Cooper named a new genus and species,
776:(in modern-day Pakistan) in 1846 by a soldier named Vickary, but these fragments were unidentifiable at the time. The first fossils now recognised as
3062:
4295:
2834:
2787:
1063:
and Forster-Cooper himself had expressed similar doubts few years earlier. Although it had already been declared a junior synonym, the genus name
1000:
continue to be discovered across Eurasia, but the political situation in Pakistan had become too unstable for further excavations to occur there.
4664:
2877:
1485:
3997:
3016:
2421:
dispersed westward to Kazakhstan during the early Oligocene from the ancestral area of Mongolia, where the most primitive member of the genus,
4249:"The maximum attainable body size of herbivorous mammals: Morphophysiological constraints on foregut, and adaptations of hindgut fermenters"
3826:
784:
in Balochistan in 1907–1908. His material consisted of an upper jaw, lower teeth, and the back of a jaw. The fossils were collected in the
2234:; it would extract relatively little nutrition from its food and would have to eat large volumes to survive. Like other large herbivores,
4763:
2370:
1995:
1406:, and were distinguished by incisor characteristics. Indricotheres are distinguished from other hyracodonts by their larger size and the
2458:
1078:
and Jay C. Sobus published a revision of indricothere taxa, which was subsequently followed by western scientists. They concluded that
792:, where Pilgrim had previously been exploring. In 1908, he used the fossils as basis for a new species of the extinct rhinoceros genus
2409:
was the only species of the genus represented in the Oligocene of western Pakistan, while the genus was highly diversified across the
4753:
1384:
in 1966. Previously, they had been regarded as a subfamily within Rhinocerotidea, or even a full family, Indricotheriidae. In a 1999
555:
epoch (34–23 million years ago). The first fossils were discovered in what is now Pakistan, and remains have been found across
4651:
975:, was named by the Chinese palaeontologist Yong-Xiang Li and colleagues based on jaw elements from the Hanjiajing Formation in the
1957:, thick mastoid-paroccipital processes, a lambdoid crest that extended back, and occipital condyles with a vertical orientation.
1923:
4758:
3043:"New fossils of paraceratheres (Perissodactyla, Mammalia) from the Early Oligocene of the Lanzhou Basin, Gansu Province, China"
1911:
shows it was only 8 percent of the skull length, while the brain of the Indian rhinoceros is 17.7 percent of its skull length.
1356:. The diversity within the rhinocerotoid group was much larger in prehistoric times; they ranged from dog-sized to the size of
3685:"Earliest known unequivocal rhinocerotoid sheds new light on the origin of Giant Rhinos and phylogeny of early rhinocerotoids"
714:
that are now known to be contemporaneous were of different ages. Many genera were named on the basis of subtle differences in
4743:
4738:
4566:
4504:
4213:
3351:
2450:, and through lowlands in the area, some of which were possibly under 2,000 m (6,600 ft) in elevation at the time.
1251:
In contrast to the revision by Lucas and Sobus, a 2003 paper by Chinese palaeontologist Jie Ye and colleagues suggested that
2378:
trees, while Siberia and Kazakhstan also had walnut trees. Dera Bugti in Pakistan had dry, temperate to subtropical forest.
1696:
926:
in 1922. Also in 1923, Borissiak created the subfamily Indricotheriinae to include the various related forms known by then.
810:; it included several unrelated species of hornless rhinoceros, many of which have since been moved to other genera. Fossil
4773:
4748:
2815:, a new genus of perissodactyles from the Upper Oligocene deposits of the Bugti hills of Baluchistan. —Preliminary notice"
630:
of the genus and the species within has a long and complicated history. Other genera of Oligocene indricotheres, such as
2056:-like openings (hollow parts of the bone) in their pre-sacral vertebrae, which probably helped to lighten the skeleton.
4768:
3185:
Tissier, J.; Becker, D.; Codrea, V.; Costeur, L.; Fărcaș, C.; Solomon, A.; Venczel, M.; Maridet, O.; Smith, T. (2018).
2463:
953:
134:
4247:
Clauss, M.; Frey, R.; Kiefer, B.; Lechner-Doll, M.; Loehlein, W.; Polster, C.; Rössner, G. E.; Streich, W. J. (2003).
4020:
2479:
902:
in Kazakhstan; it was the most complete indricothere skeleton known, but it lacked the skull. It is mounted in the
2356:), all adapted to arid environments. Trees were rare, and concentrated near groundwater. The parts of China where
1990:
otherwise found behind the incisors were lost. The incisors were separated from the row of cheek teeth by a large
1082:, as the oldest name, was the only valid indricothere genus from the Oligocene, and contained four valid species,
4733:
4397:
and other vertebrates from Oligocene and middle Miocene deposits of the Kağızman-Tuzluca Basin, Eastern Turkey".
1824:
960:, including the legs of a specimen standing in an upright position, indicating that it had died while trapped in
823:
In 1910, more partial fossils were discovered in Dera Bugti during an expedition by the British palaeontologist
3656:, a Middle to Late Eocene hyracodontid (Perissodactyla: Rhinocerotoidea) from Asia and Western North America".
2331:
appears to have varied across its range, based on the types of geological formations it has been found in. The
3855:
3509:
3449:
3375:
847:, based on larger fossils from the same excavations (some of which he had earlier suggested to belong to male
3417:"A giant rhinocerotoid (Mammalia, Perissodactyla) from the Late Oligocene of north-central Anatolia (Turkey)"
903:
130:
1772:, as indicated by the robust bones around the ear openings. The palaeontologists Pierre-Olivier Antoine and
146:
2059:
The limbs were large and robust to support the animal's large weight, and were in some ways similar to and
1914:
1459:
below follows the 1989 analysis of Indricotheriinae by Lucas and Sobus, and shows the closest relatives of
772:
were made through various colonial links to Asia. The first known indricothere fossils were collected from
3042:
2810:
2763:
1760:
elephants and rhinoceroses are largely hairless. Prothero has proposed that, contrary to most depictions,
2226:, which are mainly leaves. Like its perissodactyl relatives, the horses, tapirs, and other rhinoceroses,
1903:
has a domed forehead, whereas others have flat foreheads, possibly because of sexual dimorphism. A brain
891:
4248:
4728:
2168:
4448:
Meng, J.; McKenna, M. C. (1998). "Faunal turnovers of Palaeogene mammals from the Mongolian Plateau".
2857:
2035:
with much room for muscles, tendons, ligaments, and nerves, to support the head, neck, and spine. The
4619:
3969:
3000:
1729:
in 1997. The neck was estimated at 2 to 2.5 m (6.6 to 8.2 ft) long by the palaeontologists
1675:
1836:
skull AMNH 18650 (left), and front views of a cast of same, showing the incisors (center and right).
1380:
belongs, was first classified as part of the family Hyracodontidae by the American palaeontologist
3795:
2971:
Borissiak, A. A. (1924). "Über die Unterfamilie Indricotheriinae Boriss. = Baluchitheriinae Osb".
2040:
rhinoceroses are comparatively short-limbed. The last vertebra of the lower back was fused to the
1410:
structure of their snouts, incisors and canines. The earliest known indricothere is the dog-sized
3343:
1055:, because these specimens were collected at the same locality and were possibly part of the same
2381:
2167:, and perhaps related to reproduction strategies. Movement, sound, and other behaviours seen in
1392:, the American palaeontologist Luke Holbrook found indricotheres to be outside the hyracodontid
4695:
4581:
4491:
Leopold, E. B.; Liu, G.; Clay-Poole, S. (1992), "Low-biomass vegetation in the Oligocene?", in
1060:
876:
4669:
1879:. A distinguishing feature was that the nasal incision was retracted to the P2-P3 premolars.
4705:
4690:
4682:
2122:
703:
20:
4371:
1311:
4638:
4457:
4406:
4367:
4332:
4263:
4186:
3696:
3293:
3198:
2731:
2475:
2332:
2060:
1056:
824:
785:
711:
620:
231:
133:; this is the most completely known skeleton, but the skull is a cast of a specimen at the
3550:
Radinsky, L. B. (1966). "The families of the Rhinocerotoidea (Mammalia, Perissodactyla)".
1815:
1155:
8:
4548:
2689:
2173:
2104:
1381:
945:
781:
260:
4522:
Putshkov, P. V. (2001). ""Proboscidean agent" of some Tertiary megafaunal extinctions".
4461:
4410:
4336:
4267:
4190:
3700:
3297:
3202:
2768:, a new genus of Rhinocerotidae from the Bugti Hills of Baluchistan.—Preliminary notice"
2735:
4492:
4473:
4430:
4393:
Sen, S.; Antoine, P. O.; Varol, B.; Ayyildiz, T.; Sözeri, K. (2011). "Giant rhinoceros
4287:
4150:
4125:
3989:
3950:
3908:
3881:
3818:
3780:
3717:
3684:
3665:
3567:
3495:"Indricotheres (Perissodactyla, Mammalia) from Oligocene in Linxia Basin, Gansu, China"
3249:
Granger, W.; Gregory, W. K. (1936). "Further notes on the gigantic extinct rhinoceros,
3221:
3186:
3127:
3098:
2930:
2589:
2398:
1448:. It had also lost the second and third lower incisors, lower canines, and lower first
1040:
929:
691:
627:
344:
141:
3845:"Dinosaur models: The good, the bad, and using them to estimate the mass of dinosaurs"
4677:
4562:
4500:
4477:
4422:
4291:
4279:
4155:
4141:
3993:
3913:
3722:
3608:
3433:
3416:
3357:
3347:
3226:
3132:
3058:
2593:
2581:
2494:
2483:
2410:
2231:
1891:
1868:
1730:
1127:
1036:
868:
807:
739:
707:
679:
544:
540:
211:
4434:
3954:
2692:(1910). "Notices of new mammalian genera and species from the Tertiaries of India".
1632:
Lucas and colleagues had reached similar conclusions in a previous 1981 analysis of
1008:
906:. In 1916, based on these remains, Aleksei Alekseeivich Borissiak erected the genus
4465:
4414:
4375:
4340:
4271:
4194:
4145:
4137:
4105:
4075:
3981:
3940:
3903:
3893:
3822:
3810:
3776:
3712:
3704:
3598:
3559:
3428:
3301:
3262:
3216:
3206:
3167:
3122:
3114:
3054:
2920:
2869:
2826:
2779:
2739:
2573:
2489:
Putshkov and Andrzej H. Kulczicki instead suggested in 1995 and 2001 that invading
2288:
2258:, rather than to modern rhinoceroses, whose heads are carried close to the ground.
2215:
2147:
2126:
2068:
had short upper limb bones and long hand and foot bones—except for the disc-shaped
1864:
1847:
1765:
1740:
1498:
1146:
1110:
1075:
856:
698:
is complex due to the fragmentary nature of the known fossils and because Western,
616:
1683:(olive green) compared with that of humans, other large mammals, and the dinosaur
4344:
3335:
3211:
2720:: a genus of aberrant rhinoceroses from the Lower Miocene deposits of Dera Bugti"
2414:
2085:
1726:
1513:
1412:
1331:
1213:
867:
were so fragmentary that Foster-Cooper was only able to identify it as a kind of
536:
1965:
only in the anatomy of the rear portion of the jaw, as well as its larger size.
1789:
Gromova published a more complete skeletal reconstruction in 1959, based on the
1067:
remained popular in various media because of the publicity surrounding Osborn's
718:
tooth characteristics—features that vary within populations of other rhinoceros
4379:
4198:
3118:
2438:
2027:
1887:
1793:
skeleton from the Aral Formation, but this also lacked several neck vertebrae.
1713:
1471:
1353:
1349:
1328:
1114:). They considered most other names to be junior synonyms of those taxa, or as
1048:
976:
895:
722:—and are therefore not accepted by most scientists for distinguishing species.
643:
198:
4418:
4275:
4066:
Granger, W.; Gregory, W. K. (1935). "A revised restoration of the skeleton of
3767:
Fortelius, M.; Kappelman, J. (1993). "The largest land mammal ever imagined".
3171:
2873:
2830:
2783:
2577:
2559:: Imperial and International Networks in Early-Twentieth Century Paleontology"
1704:
in 1959, but the former estimate is now considered exaggerated. The weight of
4722:
4604:
3040:
2506:
2142:
2036:
1954:
1563:
1428:
1345:
1192:
from the late Oligocene of Kazakhstan, Mongolia, and northern China included
1115:
980:
919:
769:
715:
299:
75:
3361:
3097:
Deng, T.; Lu, X.; Wang, S.; Flynn, L. J.; Sun, D.; He, W.; Chen, S. (2021).
2006:
1283:
species in 2021, including some that had previously been declared synonyms,
670:, so most reconstructions of the genus are based on it. Differences between
4426:
4283:
4177:
from the Late/latest Oligocene of the Bugti hills, Balochistan, Pakistan".
4159:
3917:
3814:
3726:
3612:
3603:
3587:"The phylogeny and classification of tapiromorph perissodactyls (Mammalia)"
3586:
3306:
3281:
3230:
3136:
2925:
2900:
2744:
2715:
2585:
2305:
2301:
2164:
2032:
1987:
1773:
1701:
1407:
1397:
1389:
1365:
1335:
1174:
1100:
911:
816:
794:
754:
699:
574:
569:
252:
240:
4630:
3945:
3932:
3156:, sp. n., from the Dera Bugti deposits of Baluchistan.—preliminary notice"
1035:
specimen that lacked the M3 molar. In 1936, the American palaeontologists
4613:
2502:
2490:
2313:
2132:
Most terrestrial predators in their habitat were no bigger than a modern
2073:
1942:
1709:
1685:
1445:
1370:
1026:
957:
956:. Various indricothere remains were found in formations of the Mongolian
884:
773:
50:
3985:
4656:
3669:
3571:
2447:
2365:
2349:
2341:
2266:
2053:
1860:
1806:
1655:
992:
860:
789:
596:
95:
60:
3708:
3376:"A new genus of giant rhinoceros from oligocene of Dzungaria, Sinkang"
3286:
Philosophical Transactions of the Royal Society B: Biological Sciences
2724:
Philosophical Transactions of the Royal Society B: Biological Sciences
2111:
due to its size. According to Prothero, the best living analogues for
2107:
suggested in 1988 that overheating may have been a serious problem in
964:, as well as a very complete skull. These remains became the basis of
4524:
Terra Degli Elefanti Congresso Internazionale: The World of Elephants
4109:
4079:
3898:
3652:
Lucas, S. G.; Schoch, R. M.; Manning, E. (1981). "The systematics of
3041:
Yong-Xiang, L.; Yun-Xiang, Z.; Ji, L.; Zhi-Chao, L.; Kun, X. (2017).
2954:
Bulletin de la Société des Naturalistes de Moscou, Section Géologique
2934:
2390:
2375:
2368:, and the most common plant fossils are leaves of the desert-adapted
2361:
2317:
2309:
2223:
2211:
2095:
2069:
2045:
2026:
has yet been found and the tail is completely unknown. The atlas and
2019:
1872:
1456:
1441:
1402:
1385:
1361:
1340:
1180:
from the late Oligocene of Pakistan included junior synonyms such as
961:
612:
600:
552:
158:
100:
44:
37:
4575:
3563:
3266:
3151:
611:
and extant rhinoceroses. Because of its size, it would have had few
4598:
3844:
2437:
in Linxia during the late Oligocene, and it is possible that these
2374:. Trees in Mongolia and China included birch, elm, oaks, and other
2337:
2203:
2154:
may have been lengthy and individuals may have had long lifespans.
1991:
1938:
1904:
1883:
1736:
1449:
1320:
984:
949:
899:
608:
178:
90:
85:
70:
65:
55:
4469:
1973:
Unlike those of most primitive rhinocerotoids, the front teeth of
730:
607:
may have been similar to that of modern large mammals such as the
3882:"Why sauropods had long necks; and why giraffes have short necks"
2284:
2251:
2129:(a grazer) exploit different niches in the same areas of Africa.
2125:; it is used to explain how the black rhinoceros (a browser) and
811:
759:
592:
560:
556:
105:
80:
4643:
4172:
2291:
development of the Alpine-Himalayan mountain belt. The range of
1334:, which includes modern rhinoceroses, can be traced back to the
4126:"Biology of the sauropod dinosaurs: The evolution of gigantism"
3415:
Antoine, P. O.; Karadenizli, L.; Saraç, G. E.; Sen, S. (2008).
2321:
2041:
1417:
1338:—about 50 million years ago—with early precursors such as
1204:
from the middle and late Oligocene of northwest China included
1126:
was domed, while others were flat at the top was attributed to
588:
548:
188:
168:
3970:"There were giants upon the earth in those days (Book Review)"
1953:
had robust maxillae and premaxillae, upturned zygomata, domed
1426:
is known from the middle Eocene; by the late Eocene the genus
603:(trunk). The legs were long and pillar-like. The lifestyle of
2425:, lived, and descendants may have continued to South Asia as
2255:
1876:
1659:
40 million years ago, with the resulting stock evolving into
1538:
1422:
1393:
532:
4246:
4122:
2405:
based on their phylogenetic analys in 2021. They found that
1882:
The back of the skull was low and narrow, without the large
1712:, with the largest complete skeleton known belonging to the
991:, based on a complete skull with an associated mandible and
814:
that Pilgrim had previously assigned to the unrelated genus
4499:, Princeton: Princeton University Press, pp. 399–420,
2133:
719:
3414:
3184:
1220:
may be distinct enough to warrant its original genus name
4214:"All-time giants: the largest animals and their problems"
2913:
Philosophical Transactions of the Royal Society of London
3638:
3636:
3634:
3632:
3630:
3628:
3626:
3624:
3622:
3244:
3242:
3240:
2973:
Zentralblatt für Mineralogie, Geologie und Paläontologie
752:, which was the basis for its separation from the genus
4392:
3796:"Shoulder height, body mass and shape of proboscideans"
2661:
2659:
2657:
2655:
2653:
2651:
2649:
2647:
2210:
teeth confirm the creatures had a diet of soft leaves;
1267:. They also recognised the validity of species such as
551:
that has ever existed and lived from the early to late
3536:
3534:
3532:
3530:
2645:
2643:
2641:
2639:
2637:
2635:
2633:
2631:
2629:
2627:
2509:(between 23 and 16 million years ago).
1933:
are mainly discernible through skull characteristics.
650:, and it is thought to contain the following species;
4559:
Rhinoceros Giants: The Palaeobiology of Indricotheres
4322:
3933:"Estimating body mass from the astragalus in mammals"
3619:
3237:
2675:
2673:
2671:
2617:
2615:
2613:
2611:
2609:
2607:
2605:
2603:
2530:
2528:
2526:
2524:
2522:
871:, but he mentioned the possibility of confusion with
835:, meaning "near the hornless beast", in reference to
16:
Extinct genus of hornless rhinocerotoids from Eurasia
4538:
4490:
3873:
3329:
3327:
3325:
3323:
3321:
3319:
3317:
2757:
2755:
1970:
prominent hind end, and a smaller upper incisor I1.
323:
306:
289:
276:
247:
3527:
2624:
748:1911 illustrations of the down-turned lower jaw of
706:" have also contributed to the problem. Inaccurate
19:"Baluchitherium" redirects here. For the song, see
3766:
3651:
3255:Bulletin of the American Museum of Natural History
2983:
2668:
2600:
2519:
2413:, northwestern China, and Kazakhstan north to the
1986:. The incisors may have been larger in males. The
4325:Palaeogeography, Palaeoclimatology, Palaeoecology
3314:
3099:"An Oligocene giant rhino provides insights into
2752:
2389:species during the early (yellow) and late (red)
2044:, a feature found in advanced rhinoceroses. Like
1420:of western North America and Asia. The cow-sized
1224:, though its exact position requires evaluation.
567:means "near the hornless beast", in reference to
4720:
4318:
4316:
2497:do today. This would have made food scarcer for
2287:. Their distribution may be correlated with the
587:is unknown because of the incompleteness of the
4070:, gigantic fossil rhinoceros of Central Asia".
3682:
3096:
1059:variable species. The American palaeontologist
820:were later shown to belong to the new species.
4497:Eocene-Oligocene Climatic and Biotic Evolution
4100:, a giant hornless rhinoceros from Mongolia".
4091:
4089:
4065:
3745:Trudy Paleontology Institut Akademii Nauk SSSR
3743:Gromova, V. L. (1959). "Gigantskie nosorogi".
3738:
3736:
3683:Wang, H.; Bai, B.; Meng, J.; Wang, Y. (2016).
3486:
3279:
3248:
3149:
3036:
3034:
2898:
2855:
2808:
2761:
2709:
2707:
1764:had large elephant-like ears that it used for
948:led a well-documented expedition to China and
918:, until 1923, but the Russian palaeontologist
827:. Based on these remains, Foster-Cooper moved
4313:
4205:
4041:blogs.scientificamerican.com/tetrapod-zoology
4035:Sea Monsters on Medieval and Renaissance Maps
3645:
3441:
3178:
1776:have expressed scepticism towards this idea.
1024:In 1922 Forster-Cooper named the new species
710:previously led scientists to believe various
3762:
3760:
3758:
3408:
3342:, New York, New York & Oxford, England:
3338:, in Prothero, D. R.; Schoch, R. M. (eds.),
2197:The simple, low-crowned teeth indicate that
855:later that year because the former name was
595:and a nasal incision that suggests it had a
4517:
4515:
4447:
4086:
3879:
3787:
3733:
3492:
3031:
2704:
2261:
1344:. Rhinocerotoidea contains three families;
3793:
3676:
3493:Qui, Z.-X.; Wang, B.-Y.; Deng, T. (2004).
3454:in the northern Junggar Basin of Xinjiang"
3373:
3333:
2952:n. sp. provenant du district de Tourgay".
1020:), in rhinoceros-like and slender versions
682:, which would make them the same species.
116:
4211:
4149:
4018:
3944:
3930:
3907:
3897:
3769:Zoological Journal of the Linnean Society
3755:
3716:
3602:
3432:
3421:Zoological Journal of the Linnean Society
3305:
3282:"The extinct rhinoceroses of Baluchistan"
3220:
3210:
3126:
3092:
3090:
3088:
3086:
3084:
3082:
3080:
2970:
2924:
2743:
2694:Records of the Geological Survey of India
2429:, dispersing through the Tibetan region.
2397:Deng and colleagues speculated about the
1376:The subfamily Indricotheriinae, to which
1138:represents the male of the same species.
937:skull (AMNH 18650), formerly assigned to
780:were discovered by the British geologist
4556:
4521:
4512:
4357:
3836:
3584:
3549:
2544:
2542:
2540:
2457:
2393:, according to Deng and colleagues, 2021
2380:
2265:
2238:would have had a large digestive tract.
2184:
2084:
2005:
1937:had features such as relatively slender
1913:
1735:
1720:). Despite its roughly equivalent mass,
1674:
1310:
1212:. In 2013, the American palaeontologist
1051:(an invalid name for the same taxon) of
1007:
987:and colleague described the new species
979:of China; the name refers to the nearby
928:
883:was named, suggested it may have been a
3967:
3742:
2947:
2688:
2433:existed in Xinjiang and Kazakhstan and
2001:
1779:Due to the fragmentary nature of known
1432:of Asia had almost reached the size of
1074:In 1989, the American palaeontologists
1003:
983:. In 2021, the Chinese palaeontologist
910:named for a mythological monster, the "
666:. The most completely-known species is
4721:
4228:from the original on 27 September 2016
4095:
3447:
3160:Annals and Magazine of Natural History
3077:
2998:
2862:Annals and Magazine of Natural History
2819:Annals and Magazine of Natural History
2772:Annals and Magazine of Natural History
2713:
2548:
2446:freely along the eastern coast of the
1164:Skull (left) and vertebrae (right) of
894:expedition later found fossils in the
4580:
4579:
4561:. Indiana: Indiana University Press.
4000:from the original on 12 November 2014
2790:from the original on 20 November 2015
2537:
1364:forms adapted for running and squat,
914:". He did not assign a species name,
3880:Taylor, M. P.; Wedel, M. J. (2013).
3842:
3832:from the original on 24 August 2016.
3448:Ye, Y.; J., Meng; Yu, W. W. (2003).
3396:from the original on 22 October 2014
3065:from the original on 12 October 2017
1708:was similar to that of some extinct
1134:fossils represent the female, while
859:, as it had already been used for a
4360:Earth and Planetary Science Letters
4047:from the original on 6 October 2014
3334:Lucas, S. G.; Sobus, J. C. (1989),
3253:, from the Oligocene of Mongolia".
2880:from the original on 12 August 2018
2837:from the original on 7 October 2015
2180:
1649:evolved from a clade consisting of
1440:itself lived in Eurasia during the
1396:, and wrote that they may not be a
13:
4764:Taxa named by Clive Forster-Cooper
3852:Dinofest International Proceedings
3781:10.1111/j.1096-3642.1993.tb02560.x
3336:"The systematics of indricotheres"
2464:Pakistan Museum of Natural History
2274:, by Elizabeth Rungius Fulda, 1923
2214:studies have yet to be conducted.
1173:According to Lucas and Sobus, the
954:American Museum of Natural History
424:Forster-Cooper, 1913 (preoccupied)
135:American Museum of Natural History
14:
4785:
3861:from the original on 4 March 2016
3474:from the original on 3 March 2016
3019:from the original on 9 March 2016
2566:Journal of the History of Biology
1924:Musée d'Histoire Naturelle, Paris
1863:upper lip similar to that of the
1012:1923 skeletal reconstructions of
4754:Rupelian genus first appearances
4541:
4301:from the original on 8 June 2019
4142:10.1111/j.1469-185X.2010.00137.x
4021:"Tet Zoo Bookshelf: van Grouw's
3642:Prothero, 2013. pp. 107–121
3434:10.1111/j.1096-3642.2007.00366.x
3059:10.19615/j.cnki.1000-3118.170922
2080:
1886:crests at the top and along the
1823:
1814:
1805:
1319:with other rhinos, according to
1154:
1145:
933:Preparator Otto Falkenbach with
738:
729:
145:
48:
4534:
4484:
4441:
4386:
4351:
4240:
4179:Journal of Asian Earth Sciences
4166:
4116:
4059:
4012:
3961:
3924:
3578:
3543:
3385:. 11 (in Chinese and English).
3367:
3340:The Evolution of Perissodactyls
3273:
3143:
2992:
2964:
2941:
2892:
2849:
2716:"On the skull and dentition of
2665:Prothero, 2013. pp. 87–106
2482:, vegetational change, and low
2300:included other rhinocerotoids,
1043:proposed that Forster-Cooper's
944:In 1922, the American explorer
875:. The American palaeontologist
3540:Prothero, 2013. pp. 53–66
3001:"The extinct giant rhinoceros
2802:
2682:
2679:Prothero, 2013. pp. 35–52
2621:Prothero, 2013. pp. 67–86
2534:Prothero, 2013. pp. 17–34
1670:
1636:, wherein they still retained
1315:Phylogenetic relationships of
762:and part of a mandible (right)
501:Pristinotherium brevicervicale
1:
4759:Fossil taxa described in 1911
3937:Acta Palaeontologica Polonica
3803:Acta Palaeontologica Polonica
2989:Prothero, 2013. pp. 1–16
2950:Indricotherium transouralicum
2512:
2453:
1733:and Mathew J. Wedel in 2013.
904:Moscow Paleontological Museum
461:Indricotherium transouralicum
131:Moscow Paleontological Museum
4744:Prehistoric placental genera
4739:Aquitanian genus extinctions
4345:10.1016/j.palaeo.2011.07.010
3508:(3): 177–192. Archived from
3212:10.1371/journal.pone.0193774
3005:of Western and Central Asia"
2858:"Correction of generic name"
1306:
1259:were valid genera, and that
851:), but he renamed the genus
446:Paraceratherium zhajremensis
7:
4774:Oligocene mammals of Europe
4749:Extinct animals of Pakistan
3280:Forster-Cooper, C. (1934).
3150:Forster-Cooper, C. (1922).
2899:Forster-Cooper, C. (1923).
2856:Forster-Cooper, C. (1913).
2809:Forster-Cooper, C. (1913).
2762:Forster-Cooper, C. (1911).
1352:("true rhinoceroses"), and
1244:is now a junior synonym of
968:, named by Osborn in 1923.
892:Russian Academy of Sciences
685:
10:
4790:
4380:10.1016/j.epsl.2005.05.006
4199:10.1016/j.jaes.2003.09.005
4019:Naish, D. (29 June 2013).
3504:(in Chinese and English).
3463:(in Chinese and English).
3119:10.1038/s42003-021-02170-6
2385:Map showing localities of
2177:are entirely conjectural.
1697:largest known land mammals
1360:. There were long-legged,
1303:as synonyms of the genus.
514:Benaratherium callistratum
18:
4769:Oligocene mammals of Asia
4588:
4495:; Berggren, W.A. (eds.),
4419:10.1007/s00114-011-0786-z
4276:10.1007/s00442-003-1254-z
4212:Alexander, R. M. (1998).
4175:Paraceratherium bugtiense
4102:American Museum Novitates
4072:American Museum Novitates
3172:10.1080/00222932208632717
2874:10.1080/00222931308693431
2831:10.1080/00222931308693412
2784:10.1080/00222931108693085
2766:Paraceratherium bugtiense
2718:Paraceratherium bugtiense
2578:10.1007/s10739-014-9395-y
2462:Life sized model outside
2417:. They hypothesised that
2136:and were not a threat to
1941:and premaxillae, shallow
1577:
1559:
1552:
1534:
1527:
1509:
1502:
1482:
1475:
1416:from the middle and late
1053:Paraceratherium bugtiense
1033:Paraceratherium bugtiense
573:, the genus in which the
350:
343:
273:
268:
246:
239:
142:Scientific classification
140:
124:
115:
30:
4258:(Submitted manuscript).
2907:Indricotherium turgaicum
2813:Thaumastotherium osborni
2568:(Submitted manuscript).
2262:Distribution and habitat
1796:
1240:. Though the genus name
971:In 2017, a new species,
539:belonging to the family
477:Indricotherium asiaticum
422:Thaumastotherium osborni
4372:2005E&PSL.236..322W
4098:Baluchitherium grangeri
4096:Osborn, H. F. (1923). "
3968:Antoine, P. O. (2014).
3794:Larramendi, A. (2016).
3658:Journal of Paleontology
3374:Zhan-Xiang, Q. (1973).
3344:Oxford University Press
2189:Skull and lower jaw of
2146:. As in elephants, the
1663:in the late Eocene and
1236:, as well as the genus
966:Baluchitherium grangeri
863:insect. The fossils of
580:was originally placed.
493:Indricotherium grangeri
469:Baluchitherium grangeri
4734:Oligocene rhinoceroses
3931:Tsubamoto, T. (2012).
3815:10.4202/app.00136.2014
3604:10.1006/clad.1999.0107
3502:Vertebrata PalAsiatica
3461:Vertebrata PalAsiatica
3383:Vertebrata PalAsiatica
3307:10.1098/rstb.1934.0013
3154:Metamynodon bugtiensis
3107:Communications Biology
3047:Vertebrata PalAsiatica
2999:Osborn, H. F. (1923).
2926:10.1098/rstb.1924.0002
2903:Baluchitherium osborni
2745:10.1098/rstb.1924.0009
2714:Cooper, C. F. (1924).
2466:
2394:
2278:Remains assignable to
2275:
2194:
2171:documentaries such as
2100:
2015:
1926:
1842:The largest skulls of
1747:
1718:Mammuthus trogontherii
1689:
1324:
1130:; it is possible that
1061:William Diller Matthew
1045:Baluchitherium osborni
1021:
941:
877:Henry Fairfield Osborn
559:between China and the
438:Metamynodon bugtiensis
432:(Forster-Cooper, 1913)
430:Baluchitherium osborni
414:Aceratherium bugtiense
4691:Paleobiology Database
4557:Prothero, D. (2013).
3946:10.4202/app.2011.0067
3585:Holbrook, L. (1999).
2948:Pavlova, M. (1922). "
2461:
2384:
2269:
2188:
2123:competitive exclusion
2088:
2009:
1917:
1739:
1678:
1314:
1011:
932:
922:had already named it
768:Early discoveries of
712:geological formations
704:lumping and splitting
21:Baluchitherium (song)
3843:Paul, G. S. (1997).
3552:Journal of Mammalogy
3346:, pp. 358–378,
3292:(494–508): 569–616.
2730:(391–401): 369–394.
2476:inadaptive evolution
2333:Hsanda Gol Formation
2002:Postcranial skeleton
1323:and colleagues, 2021
1004:Species and synonyms
843:("wonderful beast")
825:Clive Forster-Cooper
786:Chitarwata Formation
485:Indricotherium minus
440:Forster-Cooper, 1922
365:Forster-Cooper, 1913
4549:Paleontology portal
4462:1998Natur.394..364M
4411:2011NW.....98..407S
4399:Naturwissenschaften
4337:2011PPP...311...19M
4268:2003Oecol.136...14C
4191:2004JAESc..24...71A
3986:10.18563/pv.38.1.e4
3701:2016NatSR...639607W
3298:1934RSPTB.223..569F
3203:2018PLoSO..1393774T
2736:1924RSPTB.212..369F
2549:Manias, C. (2014).
2174:Walking With Beasts
2105:Robert M. Alexander
2018:No complete set of
1382:Leonard B. Radinsky
946:Roy Chapman Andrews
782:Guy Ellcock Pilgrim
543:. It is one of the
4130:Biological Reviews
4027:Eternity of Eagles
3689:Scientific Reports
3515:on 22 October 2014
2919:(391–401): 35–66.
2467:
2399:palaeobiogeography
2395:
2276:
2230:would have been a
2195:
2101:
2046:sauropod dinosaurs
2016:
1927:
1894:was very wide and
1748:
1690:
1679:Estimated size of
1325:
1263:did not belong in
1200:. By this scheme,
1041:William K. Gregory
1022:
942:
583:The exact size of
454:P. transouralicum:
4729:Paraceratheriidae
4716:
4715:
4678:Open Tree of Life
4582:Taxon identifiers
4568:978-0-253-00819-0
4506:978-0-691-02542-1
4456:(6691): 364–367.
3709:10.1038/srep39607
3353:978-0-19-506039-3
2495:African elephants
2484:reproduction rate
2411:Mongolian Plateau
2272:P. transouralicum
2270:Foraging herd of
2232:hindgut fermenter
2191:P. transouralicum
2091:P. transouralicum
2089:Restoration of a
2012:P. transouralicum
1951:P. transouralicum
1920:P. transouralicum
1909:P. transouralicum
1901:P. transouralicum
1892:occipital condyle
1869:Indian rhinoceros
1834:P. transouralicum
1791:P. transouralicum
1786:P. transouralicum
1753:P. transouralicum
1745:P. transouralicum
1731:Michael P. Taylor
1681:P. transouralicum
1629:
1628:
1620:
1619:
1611:
1610:
1602:
1601:
1593:
1592:
1190:P. transouralicum
1136:P. transouralicum
1128:sexual dimorphism
1120:P. transouralicum
1088:P. transouralicum
1018:P. transouralicum
952:sponsored by the
935:P. transouralicum
924:I. transouralicum
869:odd-toed ungulate
831:to the new genus
808:wastebasket taxon
708:geological dating
680:sexual dimorphism
676:P. transouralicum
668:P. transouralicum
656:P. transouralicum
541:Paraceratheriidae
524:
523:
517:
504:
496:
488:
480:
472:
464:
449:
441:
433:
425:
417:
400:
391:
382:
374:
366:
356:
337:
320:
303:
294:P. transouralicum
286:
235:
212:Paraceratheriidae
127:P. transouralicum
4781:
4709:
4708:
4699:
4698:
4686:
4685:
4673:
4672:
4660:
4659:
4647:
4646:
4634:
4633:
4624:
4623:
4622:
4609:
4608:
4607:
4577:
4576:
4572:
4551:
4546:
4545:
4544:
4528:
4527:
4519:
4510:
4509:
4488:
4482:
4481:
4445:
4439:
4438:
4390:
4384:
4383:
4366:(1–2): 322–338.
4355:
4349:
4348:
4320:
4311:
4310:
4308:
4306:
4300:
4253:
4244:
4238:
4237:
4235:
4233:
4224:(6): 1231–1245.
4209:
4203:
4202:
4170:
4164:
4163:
4153:
4120:
4114:
4113:
4093:
4084:
4083:
4063:
4057:
4056:
4054:
4052:
4023:Unfeathered Bird
4016:
4010:
4009:
4007:
4005:
3974:Palaeovertebrata
3965:
3959:
3958:
3948:
3928:
3922:
3921:
3911:
3901:
3899:10.7717/peerj.36
3877:
3871:
3870:
3868:
3866:
3860:
3849:
3840:
3834:
3833:
3831:
3800:
3791:
3785:
3784:
3764:
3753:
3752:
3740:
3731:
3730:
3720:
3680:
3674:
3673:
3649:
3643:
3640:
3617:
3616:
3606:
3582:
3576:
3575:
3547:
3541:
3538:
3525:
3524:
3522:
3520:
3514:
3499:
3490:
3484:
3483:
3481:
3479:
3473:
3458:
3445:
3439:
3438:
3436:
3412:
3406:
3405:
3403:
3401:
3395:
3380:
3371:
3365:
3364:
3331:
3312:
3311:
3309:
3277:
3271:
3270:
3246:
3235:
3234:
3224:
3214:
3182:
3176:
3175:
3147:
3141:
3140:
3130:
3094:
3075:
3074:
3072:
3070:
3038:
3029:
3028:
3026:
3024:
2996:
2990:
2987:
2981:
2980:
2968:
2962:
2961:
2945:
2939:
2938:
2928:
2896:
2890:
2889:
2887:
2885:
2853:
2847:
2846:
2844:
2842:
2806:
2800:
2799:
2797:
2795:
2759:
2750:
2749:
2747:
2711:
2702:
2701:
2686:
2680:
2677:
2666:
2663:
2622:
2619:
2598:
2597:
2563:
2546:
2535:
2532:
2289:palaeogeographic
2216:Isotope analysis
2181:Diet and feeding
2148:gestation period
2127:white rhinoceros
1982:and the related
1947:Dzungariotherium
1918:Upper molars of
1865:black rhinoceros
1848:zygomatic arches
1827:
1818:
1809:
1766:thermoregulation
1741:Life restoration
1555:
1554:
1530:
1529:
1505:
1504:
1499:Indricotheriinae
1478:
1477:
1467:
1466:
1295:, while keeping
1273:P. tienshanensis
1257:Dzungariotherium
1234:P. tienshanensis
1222:Dzungariotherium
1158:
1149:
1111:Dzungariotherium
1076:Spencer G. Lucas
841:Thaumastotherium
742:
733:
617:gestation period
512:
499:
491:
483:
475:
467:
459:
448:Bayshashov, 1988
444:
436:
428:
420:
412:
399:Species synonymy
398:
389:
380:
372:
364:
354:
331:
325:
314:
308:
297:
291:
284:
278:
249:
230:
223:
210:
150:
149:
120:
110:
47:
36:Temporal range:
28:
27:
4789:
4788:
4784:
4783:
4782:
4780:
4779:
4778:
4719:
4718:
4717:
4712:
4704:
4702:
4694:
4689:
4681:
4676:
4668:
4663:
4655:
4650:
4642:
4637:
4629:
4627:
4620:Paraceratherium
4618:
4617:
4612:
4603:
4602:
4597:
4590:Paraceratherium
4584:
4569:
4547:
4542:
4540:
4537:
4532:
4531:
4520:
4513:
4507:
4493:Prothero, D. R.
4489:
4485:
4446:
4442:
4395:Paraceratherium
4391:
4387:
4356:
4352:
4321:
4314:
4304:
4302:
4298:
4251:
4245:
4241:
4231:
4229:
4210:
4206:
4171:
4167:
4121:
4117:
4094:
4087:
4064:
4060:
4050:
4048:
4017:
4013:
4003:
4001:
3966:
3962:
3929:
3925:
3878:
3874:
3864:
3862:
3858:
3847:
3841:
3837:
3829:
3798:
3792:
3788:
3765:
3756:
3741:
3734:
3681:
3677:
3654:Forstercooperia
3650:
3646:
3641:
3620:
3583:
3579:
3564:10.2307/1377893
3548:
3544:
3539:
3528:
3518:
3516:
3512:
3497:
3491:
3487:
3477:
3475:
3471:
3456:
3452:Paraceratherium
3446:
3442:
3413:
3409:
3399:
3397:
3393:
3378:
3372:
3368:
3354:
3332:
3315:
3278:
3274:
3247:
3238:
3197:(4): e0193774.
3183:
3179:
3166:(53): 617–620.
3148:
3144:
3101:Paraceratherium
3095:
3078:
3068:
3066:
3039:
3032:
3022:
3020:
3009:Natural History
2997:
2993:
2988:
2984:
2969:
2965:
2946:
2942:
2897:
2893:
2883:
2881:
2854:
2850:
2840:
2838:
2825:(70): 376–381.
2807:
2803:
2793:
2791:
2778:(48): 711–716.
2760:
2753:
2712:
2705:
2687:
2683:
2678:
2669:
2664:
2625:
2620:
2601:
2561:
2547:
2538:
2533:
2520:
2515:
2499:Paraceratherium
2471:Paraceratherium
2456:
2415:Tibetan Plateau
2403:Paraceratherium
2387:Paraceratherium
2358:Paraceratherium
2329:Paraceratherium
2327:The habitat of
2298:Paraceratherium
2293:Paraceratherium
2280:Paraceratherium
2264:
2248:Paraceratherium
2244:Paraceratherium
2236:Paraceratherium
2228:Paraceratherium
2222:fed chiefly on
2220:Paraceratherium
2208:Paraceratherium
2199:Paraceratherium
2183:
2161:Paraceratherium
2156:Paraceratherium
2152:Paraceratherium
2138:Paraceratherium
2118:Paraceratherium
2113:Paraceratherium
2109:Paraceratherium
2093:pair, with two
2083:
2066:Paraceratherium
2050:Paraceratherium
2024:Paraceratherium
2004:
1980:Paraceratherium
1975:Paraceratherium
1931:Paraceratherium
1929:The species of
1896:Paraceratherium
1857:Paraceratherium
1852:Paraceratherium
1844:Paraceratherium
1840:
1839:
1838:
1837:
1830:
1829:
1828:
1820:
1819:
1811:
1810:
1799:
1781:Paraceratherium
1770:Paraceratherium
1762:Paraceratherium
1727:Gregory S. Paul
1722:Paraceratherium
1706:Paraceratherium
1693:Paraceratherium
1673:
1665:Paraceratherium
1651:Forstercooperia
1638:Paraceratherium
1634:Forstercooperia
1630:
1621:
1612:
1603:
1594:
1582:Paraceratherium
1514:Forstercooperia
1461:Paraceratherium
1438:Paraceratherium
1434:Paraceratherium
1413:Forstercooperia
1378:Paraceratherium
1358:Paraceratherium
1332:Rhinocerotoidea
1317:Paraceratherium
1309:
1281:Paraceratherium
1265:Paraceratherium
1246:Paraceratherium
1216:suggested that
1214:Donald Prothero
1186:P. zhajremensis
1171:
1170:
1169:
1168:
1161:
1160:
1159:
1151:
1150:
1108:(originally in
1098:(originally in
1090:(originally in
1080:Paraceratherium
1057:morphologically
1006:
998:Paraceratherium
873:Paraceratherium
833:Paraceratherium
778:Paraceratherium
766:
765:
764:
763:
758:(left), and an
745:
744:
743:
735:
734:
696:Paraceratherium
688:
648:Paraceratherium
644:junior synonyms
640:Pristinotherium
605:Paraceratherium
585:Paraceratherium
565:Paraceratherium
528:Paraceratherium
520:
487:Borissiak, 1923
479:Borissiak, 1923
402:
401:
394:
381:Birkjukov, 1953
378:Pristinotherium
373:Borissiak, 1916
358:
357:
285:(Pilgrim, 1908)
264:
258:
229:
226:Paraceratherium
221:
208:
144:
111:
109:
108:
103:
98:
93:
88:
83:
78:
73:
68:
63:
58:
53:
42:
41:
34:
32:Paraceratherium
24:
17:
12:
11:
5:
4787:
4777:
4776:
4771:
4766:
4761:
4756:
4751:
4746:
4741:
4736:
4731:
4714:
4713:
4711:
4710:
4700:
4687:
4674:
4661:
4648:
4635:
4625:
4610:
4594:
4592:
4586:
4585:
4574:
4573:
4567:
4553:
4552:
4536:
4533:
4530:
4529:
4511:
4505:
4483:
4440:
4405:(5): 407–423.
4385:
4350:
4331:(1–2): 19–29.
4312:
4239:
4204:
4165:
4136:(1): 117–155.
4115:
4085:
4068:Baluchitherium
4058:
4033:, Van Duzer's
4011:
3960:
3923:
3872:
3835:
3786:
3754:
3747:(in Russian).
3732:
3675:
3664:(4): 826–841.
3644:
3618:
3597:(3): 331–350.
3577:
3558:(4): 631–639.
3542:
3526:
3485:
3450:"Discovery of
3440:
3427:(3): 581–592.
3407:
3366:
3352:
3313:
3272:
3251:Baluchitherium
3236:
3177:
3142:
3076:
3053:(4): 367–381.
3030:
3003:Baluchitherium
2991:
2982:
2963:
2940:
2909:, Borrissyak)"
2891:
2848:
2801:
2751:
2703:
2690:Pilgrim, G. E.
2681:
2667:
2623:
2599:
2557:Indricotherium
2553:Baluchitherium
2536:
2517:
2516:
2514:
2511:
2480:climate change
2455:
2452:
2439:sister species
2263:
2260:
2182:
2179:
2103:The zoologist
2082:
2079:
2003:
2000:
1961:differed from
1959:P. huangheense
1888:sagittal crest
1875:(trunk) as in
1832:
1831:
1822:
1821:
1813:
1812:
1804:
1803:
1802:
1801:
1800:
1798:
1795:
1714:steppe mammoth
1695:is one of the
1672:
1669:
1642:Indricotherium
1627:
1626:
1623:
1622:
1618:
1617:
1614:
1613:
1609:
1608:
1605:
1604:
1600:
1599:
1596:
1595:
1591:
1590:
1587:
1586:
1576:
1573:
1572:
1569:
1568:
1558:
1553:
1551:
1548:
1547:
1544:
1543:
1533:
1528:
1526:
1523:
1522:
1519:
1518:
1508:
1503:
1501:
1494:
1493:
1490:
1489:
1481:
1476:
1474:
1472:Hyracodontidae
1465:
1354:Hyracodontidae
1350:Rhinocerotidae
1308:
1305:
1301:Baluchitherium
1297:Indricotherium
1253:Indricotherium
1242:Indricotherium
1230:I. intermedium
1206:D. turfanensis
1163:
1162:
1153:
1152:
1144:
1143:
1142:
1141:
1140:
1124:Indricotherium
1092:Indricotherium
1065:Baluchitherium
1049:junior synonym
1037:Walter Granger
1005:
1002:
977:Gansu Province
973:P. huangheense
908:Indricotherium
896:Aral Formation
879:, after which
865:Baluchitherium
853:Baluchitherium
806:was by then a
747:
746:
737:
736:
728:
727:
726:
725:
724:
687:
684:
678:may be due to
660:P. huangheense
636:Indricotherium
632:Baluchitherium
537:rhinocerotoids
531:is an extinct
522:
521:
519:
518:
510:
508:Dubious names:
505:
503:Birjukov, 1953
497:
495:(Osborn, 1923)
489:
481:
473:
465:
457:
450:
442:
434:
426:
418:
410:
397:
396:
395:
393:
392:
383:
375:
370:Indricotherium
367:
362:Baluchitherium
355:Genus synonymy
353:
352:
351:
348:
347:
341:
340:
339:
338:
321:
311:P. huangheense
304:
287:
271:
270:
266:
265:
259:
244:
243:
237:
236:
232:Forster-Cooper
219:
215:
214:
206:
202:
201:
199:Perissodactyla
196:
192:
191:
186:
182:
181:
176:
172:
171:
166:
162:
161:
156:
152:
151:
138:
137:
122:
121:
113:
112:
104:
99:
94:
89:
84:
79:
74:
69:
64:
59:
54:
49:
35:
15:
9:
6:
4:
3:
2:
4786:
4775:
4772:
4770:
4767:
4765:
4762:
4760:
4757:
4755:
4752:
4750:
4747:
4745:
4742:
4740:
4737:
4735:
4732:
4730:
4727:
4726:
4724:
4707:
4701:
4697:
4692:
4688:
4684:
4679:
4675:
4671:
4666:
4662:
4658:
4653:
4649:
4645:
4640:
4636:
4632:
4626:
4621:
4615:
4611:
4606:
4600:
4596:
4595:
4593:
4591:
4587:
4583:
4578:
4570:
4564:
4560:
4555:
4554:
4550:
4539:
4525:
4518:
4516:
4508:
4502:
4498:
4494:
4487:
4479:
4475:
4471:
4470:10.1038/28603
4467:
4463:
4459:
4455:
4451:
4444:
4436:
4432:
4428:
4424:
4420:
4416:
4412:
4408:
4404:
4400:
4396:
4389:
4381:
4377:
4373:
4369:
4365:
4361:
4354:
4346:
4342:
4338:
4334:
4330:
4326:
4319:
4317:
4297:
4293:
4289:
4285:
4281:
4277:
4273:
4269:
4265:
4261:
4257:
4250:
4243:
4227:
4223:
4219:
4218:Palaeontology
4215:
4208:
4200:
4196:
4192:
4188:
4184:
4180:
4176:
4169:
4161:
4157:
4152:
4147:
4143:
4139:
4135:
4131:
4127:
4119:
4111:
4107:
4103:
4099:
4092:
4090:
4081:
4077:
4073:
4069:
4062:
4046:
4042:
4038:
4036:
4032:
4028:
4024:
4015:
3999:
3995:
3991:
3987:
3983:
3979:
3975:
3971:
3964:
3956:
3952:
3947:
3942:
3938:
3934:
3927:
3919:
3915:
3910:
3905:
3900:
3895:
3891:
3887:
3883:
3876:
3857:
3853:
3846:
3839:
3828:
3824:
3820:
3816:
3812:
3808:
3804:
3797:
3790:
3782:
3778:
3774:
3770:
3763:
3761:
3759:
3750:
3746:
3739:
3737:
3728:
3724:
3719:
3714:
3710:
3706:
3702:
3698:
3694:
3690:
3686:
3679:
3671:
3667:
3663:
3659:
3655:
3648:
3639:
3637:
3635:
3633:
3631:
3629:
3627:
3625:
3623:
3614:
3610:
3605:
3600:
3596:
3592:
3588:
3581:
3573:
3569:
3565:
3561:
3557:
3553:
3546:
3537:
3535:
3533:
3531:
3511:
3507:
3503:
3496:
3489:
3470:
3466:
3462:
3455:
3453:
3444:
3435:
3430:
3426:
3422:
3418:
3411:
3392:
3388:
3384:
3377:
3370:
3363:
3359:
3355:
3349:
3345:
3341:
3337:
3330:
3328:
3326:
3324:
3322:
3320:
3318:
3308:
3303:
3299:
3295:
3291:
3287:
3283:
3276:
3268:
3264:
3260:
3256:
3252:
3245:
3243:
3241:
3232:
3228:
3223:
3218:
3213:
3208:
3204:
3200:
3196:
3192:
3188:
3181:
3173:
3169:
3165:
3161:
3157:
3155:
3146:
3138:
3134:
3129:
3124:
3120:
3116:
3112:
3108:
3104:
3102:
3093:
3091:
3089:
3087:
3085:
3083:
3081:
3064:
3060:
3056:
3052:
3048:
3044:
3037:
3035:
3018:
3014:
3010:
3006:
3004:
2995:
2986:
2978:
2975:(in German).
2974:
2967:
2959:
2956:(in French).
2955:
2951:
2944:
2936:
2932:
2927:
2922:
2918:
2914:
2910:
2908:
2904:
2895:
2879:
2875:
2871:
2867:
2863:
2859:
2852:
2836:
2832:
2828:
2824:
2820:
2816:
2814:
2805:
2789:
2785:
2781:
2777:
2773:
2769:
2767:
2758:
2756:
2746:
2741:
2737:
2733:
2729:
2725:
2721:
2719:
2710:
2708:
2699:
2695:
2691:
2685:
2676:
2674:
2672:
2662:
2660:
2658:
2656:
2654:
2652:
2650:
2648:
2646:
2644:
2642:
2640:
2638:
2636:
2634:
2632:
2630:
2628:
2618:
2616:
2614:
2612:
2610:
2608:
2606:
2604:
2595:
2591:
2587:
2583:
2579:
2575:
2572:(2): 237–78.
2571:
2567:
2560:
2558:
2554:
2545:
2543:
2541:
2531:
2529:
2527:
2525:
2523:
2518:
2510:
2508:
2507:early Miocene
2504:
2500:
2496:
2492:
2487:
2485:
2481:
2477:
2472:
2465:
2460:
2451:
2449:
2444:
2440:
2436:
2435:P. linxiaense
2432:
2428:
2424:
2420:
2416:
2412:
2408:
2404:
2400:
2392:
2388:
2383:
2379:
2377:
2373:
2372:
2367:
2364:and abundant
2363:
2359:
2355:
2351:
2347:
2343:
2339:
2334:
2330:
2325:
2323:
2319:
2315:
2311:
2307:
2303:
2299:
2294:
2290:
2286:
2281:
2273:
2268:
2259:
2257:
2253:
2249:
2245:
2239:
2237:
2233:
2229:
2225:
2221:
2217:
2213:
2209:
2205:
2200:
2192:
2187:
2178:
2176:
2175:
2170:
2166:
2165:biomechanical
2162:
2157:
2153:
2149:
2145:
2144:
2143:Astorgosuchus
2139:
2135:
2130:
2128:
2124:
2119:
2114:
2110:
2106:
2098:
2097:
2092:
2087:
2081:Palaeobiology
2078:
2075:
2071:
2067:
2062:
2057:
2055:
2051:
2047:
2043:
2038:
2037:neural spines
2034:
2029:
2025:
2021:
2013:
2010:Hind foot of
2008:
1999:
1997:
1993:
1989:
1985:
1984:Urtinotherium
1981:
1976:
1971:
1968:
1967:P. linxiaense
1964:
1960:
1956:
1955:frontal bones
1952:
1948:
1944:
1940:
1936:
1932:
1925:
1921:
1916:
1912:
1910:
1906:
1902:
1897:
1893:
1889:
1885:
1880:
1878:
1874:
1871:, or a short
1870:
1866:
1862:
1858:
1853:
1849:
1845:
1835:
1826:
1817:
1808:
1794:
1792:
1787:
1782:
1777:
1775:
1771:
1767:
1763:
1757:
1754:
1746:
1742:
1738:
1734:
1732:
1728:
1723:
1719:
1715:
1711:
1710:proboscideans
1707:
1703:
1698:
1694:
1688:
1687:
1682:
1677:
1668:
1666:
1662:
1661:Urtinotherium
1658:
1657:
1652:
1648:
1643:
1639:
1635:
1625:
1624:
1616:
1615:
1607:
1606:
1598:
1597:
1589:
1588:
1585:
1584:
1583:
1575:
1574:
1571:
1570:
1567:
1566:
1565:
1564:Urtinotherium
1557:
1556:
1550:
1549:
1546:
1545:
1542:
1541:
1540:
1532:
1531:
1525:
1524:
1521:
1520:
1517:
1516:
1515:
1507:
1506:
1500:
1496:
1495:
1492:
1491:
1488:
1487:
1486:Triplopodinae
1480:
1479:
1473:
1469:
1468:
1464:
1462:
1458:
1453:
1451:
1447:
1443:
1439:
1435:
1431:
1430:
1429:Urtinotherium
1425:
1424:
1419:
1415:
1414:
1409:
1405:
1404:
1399:
1395:
1391:
1387:
1383:
1379:
1374:
1372:
1367:
1363:
1359:
1355:
1351:
1347:
1346:Amynodontidae
1343:
1342:
1337:
1333:
1330:
1322:
1318:
1313:
1304:
1302:
1298:
1294:
1290:
1286:
1282:
1278:
1274:
1270:
1266:
1262:
1258:
1254:
1249:
1247:
1243:
1239:
1238:Benaratherium
1235:
1231:
1227:
1223:
1219:
1218:P. orgosensis
1215:
1211:
1207:
1203:
1202:P. orgosensis
1199:
1195:
1191:
1187:
1183:
1179:
1176:
1167:
1166:P. linxiaense
1157:
1148:
1139:
1137:
1133:
1129:
1125:
1121:
1117:
1116:dubious names
1113:
1112:
1107:
1106:P. orgosensis
1103:
1102:
1097:
1093:
1089:
1085:
1081:
1077:
1072:
1070:
1066:
1062:
1058:
1054:
1050:
1047:was likely a
1046:
1042:
1038:
1034:
1030:
1028:
1019:
1015:
1010:
1001:
999:
994:
990:
989:P. linxiaense
986:
982:
981:Huanghe River
978:
974:
969:
967:
963:
959:
955:
951:
947:
940:
936:
931:
927:
925:
921:
920:Maria Pavlova
917:
913:
909:
905:
901:
897:
893:
888:
886:
882:
878:
874:
870:
866:
862:
858:
854:
850:
846:
842:
838:
834:
830:
826:
821:
819:
818:
813:
809:
805:
801:
797:
796:
791:
787:
783:
779:
775:
771:
770:indricotheres
761:
757:
756:
751:
741:
732:
723:
721:
717:
713:
709:
705:
701:
697:
693:
683:
681:
677:
673:
669:
665:
664:P. linxiaense
661:
657:
653:
649:
645:
641:
637:
633:
629:
624:
622:
618:
614:
610:
606:
602:
599:upper lip or
598:
594:
590:
586:
581:
579:
576:
572:
571:
566:
562:
558:
554:
550:
546:
542:
538:
534:
530:
529:
516:Gabunia, 1955
515:
511:
509:
506:
502:
498:
494:
490:
486:
482:
478:
474:
470:
466:
463:Pavlova, 1922
462:
458:
456:
455:
451:
447:
443:
439:
435:
431:
427:
423:
419:
416:Pilgrim, 1908
415:
411:
409:
408:
407:P. bugtiense:
404:
403:
390:Gabunia, 1955
388:
387:Benaratherium
384:
379:
376:
371:
368:
363:
360:
359:
349:
346:
342:
335:
330:
329:
328:P. linxiaense
322:
318:
313:
312:
305:
301:
296:
295:
288:
283:
282:
275:
274:
272:
267:
262:
257:
256:
254:
245:
242:
238:
233:
228:
227:
220:
217:
216:
213:
207:
204:
203:
200:
197:
194:
193:
190:
187:
184:
183:
180:
177:
174:
173:
170:
167:
164:
163:
160:
157:
154:
153:
148:
143:
139:
136:
132:
128:
123:
119:
114:
107:
102:
97:
92:
87:
82:
77:
72:
67:
62:
57:
52:
46:
39:
33:
29:
26:
22:
4589:
4558:
4535:Bibliography
4523:
4496:
4486:
4453:
4449:
4443:
4402:
4398:
4394:
4388:
4363:
4359:
4353:
4328:
4324:
4303:. Retrieved
4262:(1): 14–27.
4259:
4255:
4242:
4230:. Retrieved
4221:
4217:
4207:
4185:(1): 71–77.
4182:
4178:
4174:
4168:
4133:
4129:
4118:
4104:(78): 1–15.
4101:
4097:
4074:(787): 1–3.
4071:
4067:
4061:
4049:. Retrieved
4040:
4034:
4030:
4026:
4022:
4014:
4002:. Retrieved
3977:
3973:
3963:
3936:
3926:
3889:
3885:
3875:
3863:. Retrieved
3851:
3838:
3806:
3802:
3789:
3772:
3768:
3748:
3744:
3695:(1): 39607.
3692:
3688:
3678:
3661:
3657:
3653:
3647:
3594:
3590:
3580:
3555:
3551:
3545:
3517:. Retrieved
3510:the original
3505:
3501:
3488:
3476:. Retrieved
3464:
3460:
3451:
3443:
3424:
3420:
3410:
3398:. Retrieved
3386:
3382:
3369:
3339:
3289:
3285:
3275:
3258:
3254:
3250:
3194:
3190:
3180:
3163:
3159:
3153:
3145:
3110:
3106:
3100:
3067:. Retrieved
3050:
3046:
3021:. Retrieved
3012:
3008:
3002:
2994:
2985:
2976:
2972:
2966:
2957:
2953:
2949:
2943:
2916:
2912:
2906:
2902:
2894:
2882:. Retrieved
2865:
2864:. Series 8.
2861:
2851:
2839:. Retrieved
2822:
2821:. Series 8.
2818:
2812:
2804:
2792:. Retrieved
2775:
2774:. Series 8.
2771:
2765:
2727:
2723:
2717:
2697:
2693:
2684:
2569:
2565:
2556:
2552:
2498:
2488:
2470:
2469:The reasons
2468:
2443:P. bugtiense
2442:
2434:
2430:
2427:P. bugtiense
2426:
2422:
2419:P, asiaticum
2418:
2407:P. bugtiense
2406:
2402:
2396:
2386:
2369:
2357:
2353:
2345:
2328:
2326:
2306:amphicyonids
2302:artiodactyls
2297:
2292:
2279:
2277:
2271:
2247:
2243:
2240:
2235:
2227:
2219:
2207:
2198:
2196:
2190:
2172:
2160:
2155:
2151:
2141:
2137:
2131:
2117:
2112:
2108:
2102:
2094:
2090:
2065:
2058:
2049:
2033:zygapophyses
2023:
2022:and ribs of
2017:
2011:
1988:canine teeth
1983:
1979:
1974:
1972:
1966:
1963:P. bugtiense
1962:
1958:
1950:
1946:
1935:P. bugtiense
1934:
1930:
1928:
1919:
1908:
1900:
1895:
1881:
1856:
1851:
1843:
1841:
1833:
1790:
1785:
1780:
1778:
1774:Darren Naish
1769:
1761:
1758:
1752:
1749:
1744:
1721:
1717:
1705:
1702:Vera Gromova
1692:
1691:
1684:
1680:
1664:
1660:
1654:
1650:
1646:
1641:
1637:
1633:
1631:
1581:
1580:
1578:
1562:
1560:
1537:
1535:
1512:
1510:
1483:
1460:
1454:
1437:
1433:
1427:
1421:
1411:
1401:
1398:monophyletic
1390:tapiromorphs
1377:
1375:
1366:semi aquatic
1357:
1339:
1336:early Eocene
1326:
1316:
1300:
1296:
1292:
1289:P. asiaticum
1288:
1284:
1280:
1276:
1272:
1268:
1264:
1261:P. prohorovi
1260:
1256:
1252:
1250:
1245:
1241:
1237:
1233:
1229:
1226:P. prohorovi
1225:
1221:
1217:
1209:
1205:
1201:
1197:
1193:
1189:
1185:
1181:
1178:P. bugtiense
1177:
1175:type species
1172:
1165:
1135:
1132:P. bugtiense
1131:
1123:
1119:
1109:
1105:
1101:Aralotherium
1099:
1096:P. prohorovi
1095:
1091:
1087:
1084:P. bugtiense
1083:
1079:
1073:
1068:
1064:
1052:
1044:
1032:
1025:
1023:
1017:
1013:
997:
988:
972:
970:
965:
943:
939:B. grangeri.
938:
934:
923:
916:I. asiaticum
915:
912:Indrik beast
907:
889:
880:
872:
864:
852:
849:P. bugtiense
848:
844:
840:
837:Aceratherium
836:
832:
829:A. bugtiense
828:
822:
817:Bugtitherium
815:
804:Aceratherium
803:
800:A. bugtiense
799:
795:Aceratherium
793:
777:
767:
755:Aceratherium
753:
750:P. bugtiense
749:
695:
689:
675:
672:P. bugtiense
671:
667:
663:
659:
655:
652:P. bugtiense
651:
647:
639:
635:
631:
625:
604:
584:
582:
578:P. bugtiense
577:
575:type species
570:Aceratherium
568:
564:
547:terrestrial
535:of hornless
527:
526:
525:
513:
507:
500:
492:
484:
476:
471:Osborn, 1923
468:
460:
453:
452:
445:
437:
429:
421:
413:
406:
405:
386:
377:
369:
361:
333:
327:
326:
316:
310:
309:
293:
292:
281:P. bugtiense
280:
279:
253:Aceratherium
251:
250:
241:Type species
225:
224:
126:
31:
25:
4614:Wikispecies
4029:, Witton's
3939:: 259–265.
3854:: 129–142.
3467:: 220–229.
3389:: 182–191.
3023:8 September
3015:: 208–228.
2868:(71): 504.
2700:(1): 63–71.
2503:deinotheres
2491:gomphothere
2423:P. grangeri
2314:hyaenodonts
2304:, rodents,
2218:shows that
2074:trochanters
1943:skull roofs
1686:Patagotitan
1671:Description
1446:premaxillae
1329:superfamily
1285:P. grangeri
1194:B. grangeri
1069:B. grangeri
1027:Metamynodon
1014:B. grangeri
958:Gobi Desert
885:titanothere
857:preoccupied
774:Balochistan
694:history of
619:. It was a
615:and a long
43:34–23
4723:Categories
4526:: 133–136.
4031:Pterosaurs
4025:, Bodio's
4004:20 October
3775:: 85–101.
3751:: 154–156.
3591:Cladistics
3519:22 October
3478:22 October
3400:22 October
3113:(1): 639.
3103:evolution"
3069:11 October
2979:: 571–575.
2884:13 January
2764:"LXXVIII.—
2551:"Building
2513:References
2454:Extinction
2448:Tethys sea
2431:P. lepidum
2366:sand dunes
2360:lived had
2350:nitre bush
2342:mormon tea
2061:convergent
2054:pleurocoel
1861:prehensile
1656:Pappaceras
1293:P. lepidum
1269:P. lipidus
1210:P. lipidus
1182:B. osborni
1029:bugtiensis
993:atlas bone
881:B. osborni
861:hemipteran
790:Dera Bugti
597:prehensile
129:skeleton,
4478:204998953
4292:206989975
4256:Oecologia
4110:2246/3262
4080:2246/2123
4051:5 October
3994:203264606
3865:3 January
2960:: 95–116.
2841:28 August
2794:28 August
2594:207150574
2391:Oligocene
2376:deciduous
2371:Palibinia
2362:dry lakes
2318:nimravids
2310:mustelids
2224:C3 plants
2212:microwear
2096:Hyaenodon
2070:phalanges
2020:vertebrae
1996:metastyle
1873:proboscis
1457:cladogram
1450:premolars
1442:Oligocene
1403:Hyracodon
1388:study of
1386:cladistic
1362:cursorial
1341:Hyrachyus
1307:Evolution
962:quicksand
898:near the
692:taxonomic
613:predators
609:elephants
601:proboscis
553:Oligocene
255:bugtiense
165:Kingdom:
159:Eukaryota
38:Oligocene
4628:BioLib:
4599:Wikidata
4435:19968371
4427:21465174
4305:6 August
4296:Archived
4284:12712314
4226:Archived
4160:21251189
4045:Archived
3998:Archived
3955:54686160
3918:23638372
3856:Archived
3827:Archived
3727:28000789
3613:34902952
3469:Archived
3391:Archived
3362:19268080
3267:2246/363
3261:: 1–73.
3231:29668673
3191:PLOS ONE
3152:"LXXIV.—
3137:34140631
3063:Archived
3017:Archived
2905:(? syn.
2878:Archived
2835:Archived
2811:"XLIV.—
2788:Archived
2586:25537636
2354:Nitraria
2338:saltbush
2336:such as
2204:mesowear
2193:, Moscow
1992:diastema
1939:maxillae
1905:endocast
1884:lambdoid
1867:and the
1756:ranges.
1321:Tao Deng
1198:I. minus
985:Tao Deng
950:Mongolia
900:Aral Sea
812:incisors
686:Taxonomy
628:taxonomy
593:incisors
345:Synonyms
269:Species
205:Family:
189:Mammalia
179:Chordata
175:Phylum:
169:Animalia
155:Domain:
125:Mounted
4706:4635272
4683:4942792
4670:1030336
4657:4830663
4644:4528284
4605:Q311212
4458:Bibcode
4407:Bibcode
4368:Bibcode
4333:Bibcode
4264:Bibcode
4232:1 March
4187:Bibcode
4151:3045712
3980:: 1–3.
3909:3628838
3892:: e36.
3823:2092950
3718:5175171
3697:Bibcode
3670:1304430
3572:1377893
3294:Bibcode
3222:5905962
3199:Bibcode
3128:8211792
2732:Bibcode
2348:), and
2346:Ephedra
2285:Balkans
2252:giraffe
1408:derived
1104:), and
845:osborni
760:incisor
621:browser
589:fossils
561:Balkans
557:Eurasia
549:mammals
545:largest
302:, 1922)
300:Pavlova
261:Pilgrim
218:Genus:
195:Order:
185:Class:
4703:uBio:
4631:416754
4565:
4503:
4476:
4450:Nature
4433:
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