Odd-toed ungulate

The main axes of both the front and rear feet pass through the third toe, which is always the largest. The remaining toes have been reduced in size to varying degrees. Tapirs, which are adapted to walking on soft ground, have four toes on their fore feet and three on their hind feet. Living rhinos have three toes on both the front and hind feet. Modern equines possess only a single toe; however, their feet are equipped with hooves, which almost completely cover the toe. Rhinos and tapirs, by contrast, have hooves covering only the leading edge of the toes, with the bottom being soft.

The ulnae and fibulae are reduced in horses. A common feature that clearly distinguishes this group from other mammals is the saddle-shaped ankle between the astragalus and the scaphoid, which greatly restricts the mobility of the foot. The thigh is relatively short, and the clavicle is absent.

Tapirs are the only extant group of perissodactyls with a trunk.

Odd-toed ungulates have a long upper jaw with an extended diastema between the front and cheek teeth, giving them an elongated head. The various forms of snout between families are due to differences in the form of the premaxilla. The lacrimal bone has projecting cusps in the eye sockets and a wide contact with the nasal bone. The temporomandibular joint is high and the mandible is enlarged.

Rhinos have one or two horns made of agglutinated keratin, unlike the horns of even-toed ungulates, which have a bony core.

The number and form of the teeth vary according to diet. The incisors and canines can be very small or completely absent, as in the two African species of rhinoceros. In the horses, usually only the males possess canines. The surface shape and height of the molars is heavily dependent on whether soft leaves or hard grass makes up the main component of their diets. Three or four cheek teeth are present on each jaw half, so the dental formula of odd-toed ungulates is: 0-3 . 0-1 . 2-4 . 31-3 . 1 . 2-4 . 3 × 2 = 30-44

All perissodactyls are hindgut fermenters. In contrast to ruminants, hindgut fermenters store digested food that has left the stomach in an enlarged cecum, where the food is digested by bacteria. No gallbladder is present. The stomach of perissodactyls is simply built, while the cecum accommodates up to 90 l (24 US gal) in horses. The intestine is very long, reaching up to 26 m (85 ft) in horses. Extraction of nutrients from food is relatively inefficient, which probably explains why no odd-toed ungulates are small; for large animals, nutritional requirements per unit of body weight are lower and the surface-area-to-volume ratio is smaller.

Traditionally, the odd-toed ungulates were classified with other mammals such as artiodactyls, hyraxes, mammals with a proboscis, and other "ungulates". A close family relationship with hyraxes was suspected based on similarities in the construction of the ear and the course of the carotid artery.

Recent molecular genetic studies, however, have shown the ungulates to be polyphyletic, meaning that in some cases the similarities are the result of convergent evolution rather than common ancestry. Elephants and hyraxes are now considered to belong to Afrotheria, so are not closely related to the perissodactyls. These, in turn, are in the Laurasiatheria, a superorder that had its origin in the former supercontinent Laurasia. Molecular genetic findings suggest that the cloven Artiodactyla (containing the cetaceans as a deeply nested subclade) are the sister taxon of the Perissodactyla; together, the two groups form the Euungulata.[6] More distant are the bats (Chiroptera) and Ferae (a common taxon of carnivorans, Carnivora, and pangolins, Pholidota).[7] In a discredited alternative scenario, a close relationship exists between perissodactyls, carnivores, and bats, this assembly comprising the Pegasoferae.[8]

According to studies published in March 2015, odd-toed ungulates are in a close family relationship with at least some of the so-called Meridiungulata, a very diverse group of mammals living from the Paleocene to the Pleistocene in South America, whose systematic unity is largely unexplained. Some of these were classified on the basis of their paleogeographic distribution. However, a close relationship can be worked out to perissodactyls by means of protein sequencing and comparison with fossil collagen from remnants of phylogenetically young members of the Meridiungulata (specifically Macrauchenia from the Litopterna and Toxodon from the Notoungulata). Both kinship groups, the odd-toed ungulates and the Litopterna-Notoungulata, are now in the higher-level taxon of Panperissodactyla. This kinship group is included among the Euungulata which also contains the even-toed ungulates and whales (Artiodactyla). The separation of the Litopterna-Notoungulata group from the perissodactyls probably took place before the Cretaceous–Paleogene extinction event. "Condylarths" can probably be considered the starting point for the development of the two groups, as they represent a heterogeneous group of primitive ungulates that mainly inhabited the northern hemisphere in the Paleogene.[9][10]

Odd-toed ungulates (Perissodactyla) comprise three living families with around 17 species—in the horse the exact count is still controversial. Rhinos and tapirs are more closely related to each other than to the horses. The separation of horses from other perissodactyls took place according to molecular genetic analysis in the Paleocene some 56 million years ago, while the rhinos and tapirs split off in the lower-middle Eocene, about 47 million years ago.

• Order Perissodactyla
  • Suborder Hippomorpha
    • Family Equidae: horses and allies, seven species in one genus
      • Equus ferus
        • Tarpan, †Equus ferus ferus
        • Przewalski's horse, Equus ferus przewalskii
        • Domestic horse, Equus ferus caballus
      • African wild ass, Equus africanus
        • Nubian wild ass, Equus africanus africanus
        • Somali wild ass, Equus africanus somaliensis
        • Domesticated ass (donkey), Equus africanus asinus
        • Atlas wild ass, †Equus africanus atlanticus
      • Onager or Asiatic wild ass, Equus hemionus
        • Mongolian wild ass, Equus hemionus hemionus
        • Turkmenian kulan, Equus hemionus kulan
        • Persian onager, Equus hemionus onager
        • Indian wild ass, Equus hemionus khur
        • Syrian wild ass, †Equus hemionus hemippus
      • Kiang or Tibetan wild ass, Equus kiang
        • Western kiang, Equus kiang kiang
        • Eastern kiang, Equus kiang holdereri
        • Southern kiang, Equus kiang polyodon
      • Plains zebra, Equus quagga
        • Quagga, †Equus quagga quagga
        • Burchell's zebra, Equus quagga burchellii
        • Grant's zebra, Equus quagga boehmi
        • Maneless zebra, Equus quagga borensis
        • Chapman's zebra, Equus quagga chapmani
        • Crawshay's zebra, Equus quagga crawshayi
        • Selous' zebra, Equus quagga selousi
      • Mountain zebra, Equus zebra
        • Cape mountain zebra, Equus zebra zebra
        • Hartmann's mountain zebra, Equus zebra hartmannae
      • Grévy's zebra, Equus grevyi
  • Suborder Ceratomorpha
    • Family Tapiridae: tapirs, five species in one genus
      • Brazilian tapir, Tapirus terrestris
      • Mountain tapir, Tapirus pinchaque
      • Baird's tapir, Tapirus bairdii
      • Malayan tapir, Tapirus indicus
      • Kabomani tapir, Tapirus kabomani
    • Family Rhinocerotidae: rhinoceroses, five species in four genera
      • Black rhinoceros, Diceros bicornis
        • Southern black rhinoceros, †Diceros bicornis bicornis
        • North-eastern black rhinoceros, †Diceros bicornis brucii
        • Chobe black rhinoceros, Diceros bicornis chobiensis
        • Uganda black rhinoceros, Diceros bicornis ladoensis
        • Western black rhinoceros, †Diceros bicornis longipes
        • Eastern black rhinoceros, Diceros bicornis michaeli
        • South-central black rhinoceros, Diceros bicornis minor
        • South-western black rhinoceros, Diceros bicornis occidentalis
      • White rhinoceros, Ceratotherium simum
        • Southern white rhinoceros, Ceratotherium simum simum
        • Northern white rhinoceros, Ceratotherium simum cottoni
      • Indian rhinoceros, Rhinoceros unicornis
      • Javan rhinoceros, Rhinoceros sondaicus
        • Indonesian Javan rhinoceros, Rhinoceros sondaicus sondaicus
        • Vietnamese Javan rhinoceros, †Rhinoceros sondaicus annamiticus
        • Indian Javan rhinoceros, †Rhinoceros sondaicus inermis
      • Sumatran rhinoceros, Dicerorhinus sumatrensis
        • Western Sumatran rhinoceros, Dicerorhinus sumatrensis sumatrensis
        • Eastern Sumatran rhinoceros, Dicerorhinus sumatrensis harrissoni
        • Northern Sumatran rhinoceros, †Dicerorhinus sumatrensis lasiotis

Live reconstruction of chalicothere Anisodon grande (formerly Chalicotherium grande)

There are many perissodactyl fossils of multivariant form. The major lines of development include the following groups:

• The Brontotherioidea were among the earliest known large mammals, consisting of the families of Brontotheriidae (synonym Titanotheriidae), the most well known representative being Megacerops and the more basal family Lambdotheriidae. They were generally characterized in their late phase by a bony horn at the transition from the nose to the frontal bone and flat molars suitable for chewing soft plant food. The Brontotheroidea, which were almost exclusively confined to North America and Asia, died out at the beginning of the Upper Eocene.
• The Equoidea (equines) also developed in the Eocene. The Palaeotheriidae are known mainly from Europe; their most famous member is Eohippus, which became extinct in the Oligocene. In contrast, the horse family (Equidae) flourished and spread. Over time this group saw a reduction in toe number, extension of the limbs, and the progressive adjustment of the teeth for eating hard grasses.
• The Chalicotherioidea represented another characteristic group, consisting of the families Chalicotheriidae and Lophiodontidae. The Chalicotheriidae developed claws instead of hooves and considerable extension of the forelegs. The best-known genera include Chalicotherium and Moropus. The Chalicotherioidea died out in the Pleistocene.
• The Rhinocerotoidea (rhino relatives) included a large variety of forms from the Eocene up to the Oligocene, including dog-size leaf feeders, semiaquatic animals, and also huge long-necked animals. Only a few had horns on the nose. The Amynodontidae were hippo-like, aquatic animals. The Hyracodontidae developed long limbs and long necks that were most pronounced in the Paraceratherium (formerly known as Baluchitherium or Indricotherium), the second largest known land mammal ever to have lived (after Palaeoloxodon namadicus[14]). The rhinos (Rhinocerotidae) emerged in the Middle Eocene; five species survive to the present day.
• The Tapiroidea reached their greatest diversity in the Eocene, when more than one class lived in Eurasia and North America. They retained a primitive physique and are noted for the development of a trunk. The extinct families within this group include the Helaletidae.
• Several mammal groups traditionally classified as condylarths, long-understood to be a wastebasket taxon, such as hyopsodontids and phenacodontids, are now understood to be part of the odd-toed ungulate assemblage. Phenacodontids seem to be stem-perissodactyls, while hyopsodontids are closely related to horses and brontotheres, despite their more primitive overall appearance.
• Desmostylia[15] and Anthracobunidae have traditionally been placed among the afrotheres, but they may actually represent stem-perissodactyls. They are an early lineage of mammals that took to the water, spreading across semi-aquatic to fully marine niches in the Tethys Ocean and the northern Pacific. However, later studies have shown that, while anthracobunids are definite perissodactyls, desmostylians have enough mixed characters to suggest that a position among the Afrotheria is not out of the question.[16]
• Order Perissodactyla[17]
  • Suborder Hippomorpha
    • †Hyopsodontidae[18]
    • †Pachynolophidae[19]
    • †Brontotheriidae
    • Superfamily Equoidea
      • †Indolophidae[20]
      • †Palaeotheriidae (might be a basal perissodactyl grade instead)
  • †Suborder Ancylopoda
    • †Isectolophidae (basal ancylopodans and ceratomorphs)
    • †Lophiodontidae
    • Superfamily Chalicotherioidea
      • †Eomoropidae (basal grade of chalicotheroids)
      • †Chalicotheriidae
  • Suborder Ceratomorpha
    • Superfamily Rhinocerotoidea
      • †Amynodontidae
      • †Hyracodontidae
    • Superfamily Tapiroidea
      • †Deperetellidae
      • †Rhodopagidae (sometimes recognized as a subfamily of deperetellids)
      • †Lophialetidae[21]
      • †Eoletidae (sometimes recognized as a subfamily of lophialetids)
  • †Anthracobunidae[22] (a family of stem-perissodactyls; from the Early to Middle Eocene epoch)
  • †Phenacodontidae[22] (a clade of stem-perissodactyls; from the Early Palaeocene to the Middle Eocene epoch)

Relationships within the large group of odd-toed ungulates are not fully understood. Initially, after the establishment of "Perissodactyla" by Richard Owen in 1848, the present-day representatives were considered equal in rank. In the first half of the 20th century, a more systematic differentiation of odd-toed ungulates began, based on a consideration of fossil forms, and they were placed in two major suborders: Hippomorpha and Ceratomorpha. The Hippomorpha comprises today's horses and their extinct members (Equoidea); the Ceratomorpha consist of tapirs and rhinos plus their extinct members (Tapiroidea and Rhinocerotoidea).[24] The names Hippomorpha and Ceratomorpha were introduced in 1937 by Horace Elmer Wood, in response to criticism of the name "Solidungula" that he proposed three years previously. It had been based on the grouping of horses and Tridactyla and on the rhinoceros/tapir complex.[25][26] The extinct brontotheriidae were also classified under Hippomorpha and therefore possess a close relationship to horses. Some researchers accept this assignment because of similar dental features, but there is also the view that a very basal position within the odd-toed ungulates places them rather in the group of Titanotheriomorpha.[23][27]

Originally, the Chalicotheriidae were seen as members of Hippomorpha, and presented as such in 1941. William Berryman Scott thought that, as claw-bearing perissodactyls, they belong in the new suborder Ancylopoda (where Ceratomorpha and Hippomorpha as odd-toed ungulates were combined in the group of Chelopoda).[28] The term Ancylopoda, coined by Edward Drinker Cope in 1889, had been established for chalicotheres. However, further morphological studies from the 1960s showed a middle position of Ancylopoda between Hippomorpha and Ceratomorpha. Leonard Burton Radinsky saw all three major groups of odd-toed ungulates as peers, based on the extremely long and independent phylogenetic development of the three lines.[29] In the 1980s, Jeremy J. Hooker saw a general similarity of Ancylopoda and Ceratomorpha based on dentition, especially in the earliest members, leading to the unification in 1984 of the two submissions in the interim order, Tapiromorpha. At the same time he expanded the Ancylopoda to include the Lophiodontidae. The name "Tapiromorpha" goes back to Ernst Haeckel, who coined it in 1873, but it was long considered synonymous to Ceratomorpha because Wood had not considered it in 1937 when Ceratomorpha were named, since the term had been used quite differently in the past.[30] Also in 1984, Robert M. Schoch used the conceptually similar term Moropomorpha, which today applies synonymously to Tapiromorpha.[31] Included within the Tapiromorpha are the now extinct Isectolophidae, a sister group of the Ancylopoda-Ceratomorpha group and thus the most primitive members of this relationship complex.[27][32]

The evolutionary development of Perissodactyla is well documented in the fossil record. Numerous finds are evidence of the adaptive radiation of this group, which was once much more varied and widely dispersed. Radinskya from the late Paleocene of East Asia is often considered to be one of the oldest close relatives of the ungulates.[33] Its 8 cm skull must have belonged to a very small and primitive animal with a π-shaped crown pattern on the enamel of its rear molars similar to that of perissodactyls and their relatives, especially the rhinos.[34] Finds of Cambaytherium and Kalitherium in the Cambay shale of western India indicate an origin in Asia dating to the Lower Eocene roughly 54.5 million years ago.[35][36] Their teeth also show similarities to Radinskya as well as to the Tethytheria clade.[37][38] The saddle-shaped configuration of the navicular joints and the mesaxonic construction of the front and hind feet also indicates a close relationship to Tethytheria. However, this construction deviates from that of Cambaytherium, indicating that it is actually a member of a sister group. Ancestors of Perissodactyla may have arrived via an island bridge from the Afro-Arab landmass onto the Indian subcontinent as it drifted north towards Asia.[39] A study on Cambaytherium suggests an origin in India prior or near its collision with Asia.[40]

The alignment of hyopsodontids and phenacodontids to Perissodactyla in general suggests an older Laurasian origin and distribution for the clade, dispersed across the northern continents already in the early Paleocene. These forms already show a fairly well-developed molar morphology, with no intermediary forms as evidence of the course of its development.[41] The close relationship between meridiungulate mammals and perissoodactyls in particular is of interest since the latter appear in South America soon after the K–T event, implying rapid ecological radiation and dispersal after the mass extinction.[42]

Eohippus, an early relative of the horse, is one of the oldest-known perissodactyls

The Perissodactyla appear relatively abruptly at the beginning of the Lower Paleocene before about 63 million years ago, both in North America and Asia, in the form of phenacodontids and hyopsodontids. The oldest finds from an extant group originate among other sources from Sifrhippus, an ancestor of the horses from the Willswood lineup in northwestern Wyoming.[43][44] The distant ancestors of tapirs appeared not too long after that in the Ghazij lineup in Balochistan, such as Ganderalophus, as well as Litolophus from the Chalicotheriidae line, or Eotitanops from the group of brontotheriidae.[45][46] Initially, the members of the different lineages looked quite similar with an arched back and generally four toes on the front and three on the hind feet. Eohippus, which is considered a member of the horse family, outwardly resembled Hyrachyus, the first representative of the rhino and tapir line.[47] All were small compared to later forms and lived as fruit and foliage eaters in forests. The first of the megafauna to emerge were the brontotheres, in the Middle and Upper Eocene. Megacerops, known from North America, reached a withers height of 2.5 m (8 ft 2 in) and could have weighed just over 3 metric tons (3.3 short tons). The decline of brontotheres at the end of the Eocene is associated with competition arising from the advent of more successful herbivores.[17][48]

More successful lines of odd-toed ungulates emerged at the end of the Eocene when dense jungles gave way to steppe, such as the chalicotheriid rhinos, and their immediate relatives; their development also began with very small forms. Paraceratherium, one of the largest mammals ever to walk the earth, evolved during this era.[49][50] They weighed up to 20 metric tons (22 short tons) and lived throughout the Oligocene in Eurasia. About 20 million years ago at the onset of the Miocene the perissodactyls first reached Africa when it became connected to Eurasia because of the closing of the Tethys Ocean. For the same reason, however, new animals such as the mammoths also entered the ancient settlement areas of odd-toed ungulates, creating competition that led to the extinction of some of their lines. The rise of ruminants, which occupied similar ecological niches and had a much more efficient digestive system, is also associated with the decline in diversity of odd-toed ungulates. A significant cause for the decline of perissodactyls was climate change during the Miocene, leading to a cooler and drier climate accompanied by the spread of open landscapes. However, some lines flourished, such as the horses and rhinos; anatomical adaptations made it possible for them to consume tougher grass food. This led to open land forms that dominated the newly created landscapes. With the emergence of the Isthmus of Panama in the Pliocene, perissodactyls and other megafauna were given access to one of their last habitable continents: South America.[51][52] However, many perissodactyls became extinct at the end of the ice ages, including American horses and the Elasmotherium. Whether over-hunting by humans (overkill hypothesis), climatic change, or a combination of both factors was responsible for the extinction of ice age mega-fauna, remains controversial.[17]