Megacerops

Megacerops ("large-horned face", from méga- "large" + kéras "horn" + ōps "face") is an extinct genus of the prehistoric odd-toed ungulate (hoofed mammal) family Brontotheriidae, an extinct group of rhinoceros-like browsers related to horses. It was endemic to North America during the Late Eocene epoch (38–33.9 mya), existing for approximately 4.1 million years.[1]

Megacerops
Temporal range: Eocene (Priabonian),
Mounted skeleton, Natural History Museum of Los Angeles County
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Perissodactyla
Family: Brontotheriidae
Subfamily: Brontotheriinae
Tribe: Brontotheriini
Subtribe: Brontotheriina
Infratribe: Brontotheriita
Genus: Megacerops
Leidy, 1870
Species
  • M. coloradensis Leidy, 1870 (type species)
  • M. kuwagatarhinus Mader and Alexander, 1995
Synonyms
  • Brontotherium Cope, 1873
  • Brontops
  • Menodus
  • Titanotherium
  • Ateleodon
  • Oreinotherium

Taxonomy

Megacerops was named by Leidy (1870). Its type species is Megacerops coloradensis. It was synonymized subjectively with Menodus by Clark and Beerbower (1967). It was assigned to Brontotheriidae by Leidy (1870), Carroll (1988), Mader (1989), and Mader (1998).[2][3]

According to Mihlbachler and others,[4][5] Megacerops includes the species of the genera Menodus, Brontotherium, Brontops, Menops, Ateleodon, and Oreinotherium.

Description

Restoration of M. coloradensis

All of the species had a pair of blunt horns on their snout (the size varying between species), with the horns of males being much larger than those of the females. This could indicate that they were social animals which butted heads for breeding privileges.

Despite resembling the rhinoceros, it was larger than any living rhinoceros: the living animal easily approached the size of the African forest elephant, the third-largest land animal today. It stood about 2.5 m (8 ft 2 in) tall at the shoulders with an overall length(including tail) of 4.63 m (15.2 ft). [6]:666 Its skull reached 89.5 cm (35.2 in) in greatest length, with some specimens possessing substantial canines, up to 70 mm long.[6]:494,523 Megacerops resembled a large rhinoceros, possessing blunt Y-shaped horn-like protrusions on its nose up to 43 cm in length.[6]:553 Its mass is estimated to be in the range of 3.3–3.8 t (3.6–4.2 short tons) [7][8]

The dorsal vertebrae above the shoulders had extra long spines to support the huge neck muscles needed to carry the heavy skull. The shape of its teeth suggests that it preferred food such as soft stems and leaves, rather than tough vegetation. It may have had fleshy lips and a long tongue for carefully selecting food.

Paleobiology

Skull in Zurich

The skeleton of an adult male was found with partially healed rib fractures, which supports the theory that males used their 'horns' to fight each other. No creature living in Megacerops' time and area except another Megacerops could have inflicted such an injury.[9] The breathing movements prevented the fractures from completely healing. The adults may have also used their horns to defend themselves and their calves from predators, such as hyaenodonts, entelodonts, Bathornis or nimravids.

Distribution

Fossils were uncovered in the northern plains states. Life-sized models of Megacerops families (a male, female, and juvenile) are displayed at the James E. Martin Paleontological Research Laboratory, South Dakota School of Mines & Technology, and a different set at the Canadian Museum of Nature.

Many remains have been found in South Dakota and Nebraska. In the past, specimens exposed by severe rainstorms were found by Native Americans of the Sioux tribes. The Sioux called them "thunder beasts", a name preserved in the ancient Greek translation (bronto-, thunder; therion, beast).[10] Many of the skeletons found by the Sioux belonged to herds which were killed by volcanic eruptions of the Rocky Mountains, which were volcanically active at the time.

See also

References

  1. "Fossilworks: Megacerops".
  2. J. Clark and J. R. Beerbower. 1967. Geology, paleoecology, and paleoclimatology of the Chadron Formation. Fieldiana
  3. Carroll, Robert L. (1988). Vertebrate Paleontology and Evolution. Freeman. ISBN 978-0-7167-1822-2.
  4. Mihlbachler, M.C., Lucas, S.G., and Emry, R.J. (2004). "The holotype specimen of Menodus giganteus, and the "insoluble" problem of Chadronian brontothere taxonomy". New Mexico Museum of Natural History and Science Bulletin. 26: 129–136.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  5. Mihlbachler, Matthew Christian (2005). Phylogenetic systematics of the Brontotheriidae (Mammalia, Perissodactyla) (Thesis). OCLC 79487069. ProQuest 305015315.
  6. Osborn, Henry F. (1929). The titanotheres of ancient Wyoming, Dakota, and Nebraska. Dept. of the Interior, U.S. Geological Survey.
  7. Gregory S., Paul. "Mass estimate table". Archived from the original on 1 November 2014. Retrieved 20 September 2022.
  8. Bales, Gerald S. (1996). "Heterochrony in Brontothere Horn Evolution: Allometric Interpretations and the Effect of Life History Scaling". Paleobiology. 22 (4): 481–495. doi:10.1017/S009483730001647X. S2CID 89214971. Retrieved September 26, 2022.
  9. Palmer, D., ed. (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. pp. 258–259. ISBN 978-1-84028-152-1.
  10. Mayor, Adrienne. "Placenames Describing Fossils in Oral Traditions" (PDF).
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