Brontotheriidae

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Brontotheres
Temporal range: 56–34  Ma
Brontotherium hatcheri.jpg
Megacerops skeleton at the
National Museum of Natural History, Washington, DC
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Perissodactyla
Family: Brontotheriidae
Marsh, 1873
Genera

See text

Synonyms
  • Menodontidae
  • Titanotheriidae

Brontotheriidae is a family of extinct mammals belonging to the order Perissodactyla, the order that includes horses, rhinoceroses, and tapirs. Superficially, they looked rather like rhinos with some developing bony nose horns, and were some of the earliest mammals to have evolved large body sizes of several tonnes. They lived around 56–34 million years ago, until the very close of the Eocene. Brontotheres had a Holarctic distribution, with the exception of Western Europe: they occupied North America, Asia, and Eastern Europe. [1] They were the first fossilized mammals to be discovered west of the Mississippi, and were first discovered in South Dakota. [2]

Contents

Characteristics and evolution

Megacerops BW.jpg
Life reconstruction of Megacerops
Protitanops NT small.jpg
Life reconstruction of Protitanops curryi
RhinotitanMongoliensis(Skull)-PaleozoologicalMuseumOfChina-May23-08.jpg
Skull of Rhinotitan

This group has also been referred to as "Titanotheres." "Titan" refers to the mythological Greek gods who were symbols of strength and large size, and "theros" is Greek for "wild animal." "Bronto" is Greek for "thunder," which may be how this group got the nickname "thunder beasts." [3]

Brontotheres retain four toes on their front feet and three toes on their hind feet. Their teeth are adapted to shearing (cutting) relatively nonabrasive vegetation. Their molars have a characteristic W-shaped ectoloph (outer shearing blade). The wear patterns observed on brontothere teeth suggests a folivorous diet. Early Brontotheres had brachydont teeth with thick enamel, while later forms evolved a more hypsodont style tooth with thinner enamel. [1]

Brontotheres also shared an elongated postorbital cranium, meaning that their skulls are lengthened between their eyes and ears. They also had anteroposteriorly abbreviated (shortened) faces. [1]

The evolutionary history of this group is well known due to an excellent fossil record in North America. [4] The earliest stem-brontotheres, had an estimated body mass of only 18 kilograms (40 lb) [5]

The earliest brontotheres, such as Eotitanops , were rather small, no more than a meter in height, and hornless.

Brontotheres evolved massive bodies, with some species standing over 2.5 meters (7 feet) tall, [3] with body masses of over a tonne, perhaps exceeding 4,000 kilograms (8,800 lb), in large individuals of Megacerops , [5] although some small species such as Nanotitanops did persist through the Eocene. [5] Some genera, such as Dolichorhinus , evolved highly elongated skulls. Some later brontotheres developed horn-like bony projections of the skull. The North American brontothere Megacerops , for example, evolved large sexually dimorphic paired horns above their noses. The sexually dimorphic horns, along with highly developed neck musculature, suggest that brontotheres were highly gregarious (social) and males may have performed some sort of head-clashing behavior in competition for mates. [6] Females had smaller appendages, which may have been used to ward off predators and protect young. In Asia, another species of brontothere, Embolotherium, evolved a similarly gigantic body size; however, instead of the slingshot-like horns of the Megacerops, they evolved a single elongated bony process that was composed of both nasal and frontal bones. [6] Embolotherium may have used its large nasal cavity to make vocalizations in order to communicate with others of its species. [6] Unlike rhinoceros, in which the horns are made of keratin, however, the horns of brontotheres are composed of bone (the frontal bone and nasal bone) and were placed side-to-side rather than front-to-back. Similarly to Giraffes, their horns were covered in skin and did not have grooves for nutrient blood vessels. There is some evidence of secondary bone growth, likely due to impact from head clashing. [1]

Brontotheres had likely adapted to the warmer and more humid climates of the Eocene, and probably became extinct because they could not adapt to the drier conditions and more open landscapes of the Oligocene. [5]

Discovery

Brontothere model reconstruction (Parvicornis occidentalis) at the San Diego Natural History Museum Brontothere model at SD Natural History Museum.jpg
Brontothere model reconstruction (Parvicornis occidentalis) at the San Diego Natural History Museum

Brontotheres were one of the first fossilized mammals to be discovered west of the Mississippi, with the first fossil being found in 1846 in the Badlands, South Dakota. [2] Joseph Leidy was the first researcher to scientifically describe brontothere fossils, followed by Cope and Marsh, who studied skulls and entire skeletons. [1] Marsh came up with the term "Brontotheridae," identified them as odd-toed ungulates, and identified distinguishing characteristics of the group. [7] [1] [8] Brontotheriidae fossils have been found in eastern Europe, eastern Russia, Kazakstan, Pakistan, southeast Asia, Korea, Japan, the southeastern U.S., and Canada. [1]

Classification

Brontotheres are an early diverging clade within Perissodactyla. Although historically suggested to be closely related to horses, [9] phylogenetic analyses have recovered them to lie outside the clade containing chalicotheres, rhinoceroses, tapirs and horses, [10] or more closely related to chalicotheres, rhinoceroses and tapirs than to horses. [11]

Classification for Brontotheriidae after Mihlbachler 2008 [12] and Mader 2010 [13]
Brontotheriidae

Two classification systems for Brontotheriidae are presented below. The first contains 43 genera and 8 subfamilies, and although it is based on a 1997 publication by McKenna and Bell, it summarizes research that was conducted before 1920 and is badly outdated. The second classification is based on 2004 and 2005 research by Mihlbachler et al., which indicates that many of the previous subfamily names are invalid. Several more recently discovered brontotheres are included in the newer classification.

Although Lambdotherium and Xenicohippus were previously included in Brontotheriidae, they are no longer considered members of this family. Lambdotherium, though excluded, may be the closest known relative to brontotheres. Xenicohippus is now thought to be an early member of the horse family, Equidae.

Old classification (summarized by McKenna and Bell, 1997)New classification (Mihlbachler et al., 2004a, 2004b; Mihlbachler, 2005)

Related Research Articles

<span class="mw-page-title-main">Ancylopoda</span> Extinct suborder of mammals

Ancylopoda is a group of browsing, herbivorous, mammals in the Perissodactyla that show long, curved and cleft claws. Morphological evidence indicates the Ancylopoda diverged from the tapirs, rhinoceroses and horses (Euperissodactyla) after the Brontotheria; however, earlier authorities such as Osborn sometimes considered the Ancylopoda to be outside Perissodactyla or, as was popular more recently, to be related to Brontotheriidae.

<span class="mw-page-title-main">Perissodactyla</span> Order of hoofed mammals

Perissodactyla is an order of ungulates. The order includes about 17 living species divided into three families: Equidae, Rhinocerotidae (rhinoceroses), and Tapiridae (tapirs). They typically have reduced the weight-bearing toes to three or one of the five original toes, though tapirs retain four toes on their front feet. The nonweight-bearing toes are either present, absent, vestigial, or positioned posteriorly. By contrast, artiodactyls bear most of their weight equally on four or two of the five toes: their third and fourth toes. Another difference between the two is that perissodactyls digest plant cellulose in their intestines, rather than in one or more stomach chambers as artiodactyls, with the exception of Suina, do.

<span class="mw-page-title-main">Ungulate</span> Group of animals that walk on the tips of their toes or hooves

Ungulates are members of the diverse clade Euungulata, which primarily consists of large mammals with hooves. Once part of the clade "Ungulata" along with the clade Paenungulata, "Ungulata" has since been determined to be a polyphyletic and thereby invalid clade based on molecular data. As a result, true ungulates had since been reclassified to the newer clade Euungulata in 2001 within the clade Laurasiatheria while Paenungulata has been reclassified to a distant clade Afrotheria. Living ungulates are divided into two orders: Perissodactyla including equines, rhinoceroses, and tapirs; and Artiodactyla including cattle, antelope, pigs, giraffes, camels, sheep, deer, and hippopotamuses, among others. Cetaceans such as whales, dolphins, and porpoises are also classified as artiodactyls, although they do not have hooves. Most terrestrial ungulates use the hoofed tips of their toes to support their body weight while standing or moving. Two other orders of ungulates, Notoungulata and Litopterna, both native to South America, became extinct at the end of the Pleistocene, around 12,000 years ago.

<i>Hyracotherium</i> Extinct genus of mammals

Hyracotherium is an extinct genus of very small perissodactyl ungulates that was found in the London Clay formation. This small, fox-sized animal is considered to be the earliest known member of Equidae before the type species, H. leporinum, was reclassified as a palaeothere, a perissodactyl family related to both horses and brontotheres. The remaining species are now thought to belong to different genera, such as Eohippus, which had previously been synonymised with Hyracotherium.

<i>Embolotherium</i> Extinct genus of mammals

Embolotherium is an extinct genus of brontothere that lived in Mongolia during the late Eocene epoch. It is most easily recognized by a large bony protuberance emanating from the anterior (front) of the skull. This resembles a battering ram, hence the name Embolotherium. The animal is known from about 12 skulls, several jaws, and a variety of other skeletal elements from the Ulan Gochu formation of Inner Mongolia as well as the Ergilin Dzo Formation of Outer Mongolia.

<i>Sarkastodon</i> Oxyaenid genus from upper Eocene Epoch

Sarkastodon is an extinct genus of placental mammals from extinct subfamily Oxyaeninae within extinct family Oxyaenidae, that lived in Asia during the middle Eocene. It was a genus of large, carnivorous animals known only from a skull and jawbones. Sarkastodon was probably a hypercarnivore that preyed on large mammals in its range during the Middle Eocene, such as brontotheres, chalicotheres, and rhinoceroses. Its weight is estimated at 800 kg (1,800 lb), and its length at 3 m (10 ft).

<span class="mw-page-title-main">Chalicotheriidae</span> Family of extinct mammals

Chalicotheriidae is an extinct family of herbivorous, odd-toed ungulate (perissodactyl) mammals that lived in North America, Eurasia, and Africa from the Middle Eocene to the Early Pleistocene. They are often called chalicotheres, a term which is also applied to the broader grouping of Chalicotherioidea. They are noted for their unusual morphology compared to other ungulates, such as their clawed forelimbs. Members of the subfamily Chalicotheriinae developed elongate gorilla-like forelimbs that are thought to have been used to grasp vegetation. They are thought to have been browsers on foliage as well as possibly bark and fruit.

Pakotitanops is a genus of poorly known brontothere represented only by a few tooth fragments. Its fossil dates from the middle Eocene Kuldana Formation, in the Ganda Kas area of Pakistan. Because this species is known only from a few tooth fragments it is difficult to compare it to other species to determine if it is indeed a distinct species and to what other species it is mostly closely related.

<i>Ancylotherium</i> Extinct genus of mammals

Ancylotherium is an extinct genus of the family Chalicotheriidae, subfamily Schizotheriinae, endemic to Europe, Asia, and Africa during the Late Miocene-Early Pleistocene, existing for approximately 9.8 million years.

<i>Eotitanops</i> Extinct genus of mammals

Eotitanops is an extinct genus of brontothere native to North America and Asia.

<i>Megacerops</i> Extinct Perissodactyl ungulate genus from Late Eocene epoch

Megacerops is an extinct genus of the prehistoric odd-toed ungulate family Brontotheriidae, an extinct group of rhinoceros-like browsers related to horses. It was endemic to North America during the Late Eocene epoch, existing for approximately 4.1 million years.

<i>Protitanops</i> Extinct genus of mammals

Protitanops curryi is an extinct species of brontothere that lived during the Eocene, in the Western United States, especially in Death Valley, California, where the best specimens of the species P. curryi have been found. It bore a strong resemblance to Megacerops brontotheres with its knob-shaped horns. However, the position of the horns differed in Protitanops, in that they pointed straight up, rather than more forwards, like in Megacerops.

<span class="mw-page-title-main">Amynodontidae</span> Extinct family of mammals

Amynodontidae is a family of extinct perissodactyls related to true rhinoceroses. They are commonly portrayed as semiaquatic hippo-like rhinos but this description only fits members of the Metamynodontini; other groups of amynodonts like the cadurcodontines had more typical ungulate proportions and convergently evolved a tapir-like proboscis.

<i>Brachydiastematherium</i>

Brachydiastematherium transylvanicum is the westernmost species of brontothere, with the first fossils of it being found in Transylvania, Romania. In comparison with other brontothere fossils, it is suggested that B. transylvanicum would have had an elongated head, not unlike Dolichorhinus, and be about 2 meters at the withers.

<i>Homogalax</i> Genus of odd-toed ungulates

Homogalax is an extinct genus of tapir-like odd-toed ungulate. It was described on the basis of several fossil finds from the northwest of the United States, whereby the majority of the remains come from the state of Wyoming. The finds date to the Lower Eocene between 56 and 48 million years ago. In general, Homogalax was very small, only reaching the weight of today's peccaries, with a maximum of 15 kg. Phylogenetic analysis suggests the genus to be a basal member of the clade that includes today's rhinoceros and tapirs. In contrast to these, Homogalax was adapted to fast locomotion.

<i>Urtinotherium</i> Extinct family of mammals

Urtinotherium is an extinct genus of paracerathere mammals. It was a large animal that was closely related to Paraceratherium, and found in rocks dating from the Late Eocene to Early Oligocene period. The remains were first discovered in the Urtyn Obo region in Inner Mongolia, which the name Urtinotherium is based upon. Other referred specimens are from northern China.

<i>Systemodon</i> Genus of mammals

Systemodon is a genus of early Eocene mammal of Wasatchian age. It was one of many mammals originally considered the earliest horses, long classified in the genus Hyracotherium. These were dog-sized animals that in life would have looked vaguely like a paca, mara, or chevrotain The type species, S. tapirinus, is represented by 24 individuals from a locale called the Castillo pocket in the Huerfano Formation of Colorado. This well-preserved deposit allows researchers to reconstruct aspects of the environment and lifestyle of the species.

Nanotitanops is an extinct genus of Brontothere from the middle Eocene of China. It contains a single species, N. shanghuangensis. It is known only from isolated teeth, the smallest of any known Brontothere.

The Ergilin Dzo Formation, is a geologic formation in southeastern Mongolia. It preserves fossils of a wide variety of animals, which date back to the late Eocene epoch. The type fauna of the Ergilian Asian land mammal age is defined by the mammalian fossils of this formation.

Anatomy of <i>Palaeotherium</i> Studies of a genus of palaeothere

The anatomy of Palaeotherium has been historically well-studied due to at least several of its species being known from common and good fossil material. As the type genus of the Palaeotheriidae, one of two families within the Equoidea, it shares common traits such as orbits that are wide in its back plus located in the skull's midlength, long nasal bones, selenodont form molars, and the presence of diastemata between the canine and other teeth between it. Palaeotherium itself differs from other palaeotheres primarily based on various cranial and dental traits; the subgenus Palaeotherium is likewise distinguished from the other subgenus Franzenitherium based on specialized and specific cranial traits. While not as often studied, Palaeotherium is also known by viable limb bone material, leading to the locomotion of different species being hypothesized. P. magnum, unlike other species, is known by complete skeletal material such as that from Mormoiron in France that is informative about its overall anatomy, sharing similar and different traits from equines and other perissodactyls.

References

  1. 1 2 3 4 5 6 7 Mihlbachler, Matthew C. (June 2008). "Species Taxonomy, Phylogeny, and Biogeography of the Brontotheriidae (Mammalia: Perissodactyla)". Bulletin of the American Museum of Natural History. 2008 (311): 1–475. doi:10.1206/0003-0090(2008)501[1:STPABO]2.0.CO;2. ISSN   0003-0090.
  2. 1 2 "Brontothere: Large beasts of the Badlands (U.S. National Park Service)". www.nps.gov. Retrieved 2024-03-08.
  3. 1 2 "nfd logo fossils - National Fossil Day (U.S. National Park Service)". www.nps.gov. Retrieved 2024-03-08.
  4. Titanotherium
  5. 1 2 3 4 Sanisidro, O.; Mihlbachler, M. C.; Cantalapiedra, J. L. (2023). "A macroevolutionary pathway to megaherbivory". Science. 380 (6645): 616–618. doi:10.1126/science.ade1833.
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  7. Cope, E. D. (1881). "The Systematic Arrangement of the Order Perissodactyla". Proceedings of the American Philosophical Society. 19 (108): 377–401. ISSN   0003-049X.
  8. Marsh, Charles O. (1876). "Principal Characteristics of the Brontotheridae". American Journal of Science and Arts. 11: 335–340.
  9. Koenigswald W von (1994) U-shaped orientation of Hunter-Schreger Bands in the enamel of Moropus (Mammalia: Chalicotheriidae) in comparison to some other Perissodactyla. Ann Carnegie Mus 63:49–65
  10. Hooker, J. J.; Dashzeveg, D. (November 2004). "The origin of chalicotheres (Perissodactyla, Mammalia)". Palaeontology. 47 (6): 1363–1386. doi: 10.1111/j.0031-0239.2004.00421.x . ISSN   0031-0239.
  11. Bai, Bin; Wang, Yuan-Qing; Meng, Jin (2018-08-15). "The divergence and dispersal of early perissodactyls as evidenced by early Eocene equids from Asia". Communications Biology. 1 (1). doi:10.1038/s42003-018-0116-5. ISSN   2399-3642. PMC   6123789 . PMID   30271995.
  12. Mihlbachler, Matthew C. "Species taxonomy, phylogeny and biogeography of the Brontotheriidae (Mammalia, Perissodactyla)". Bulletin of the American Museum of Natural History (311). American Museum of Natural History. hdl:2246/5913 . Retrieved 4 September 2013.
  13. Mader, Bryn J. "A species-level revision of the North American brontotheres Eotitanops and Palaeosyops (Mammalia, Perissodactyla)" (PDF). Department of Biological Sciences and Geology, Queensborough Community College. Retrieved 4 September 2013.

Further reading