Teleoceras
| Teleoceras | |
|---|---|
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| Specimen at the Natural History Museum of LA | |
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| 1913 T. fossiger illustration by Robert Bruce Horsfall. | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Order: | Perissodactyla |
| Family: | Rhinocerotidae |
| Subfamily: | †Aceratheriinae |
| Genus: | †Teleoceras Hatcher, 1894 |
| Type species | |
| †Teleoceras major | |
| Species[1] | |
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| Synonyms | |
Teleoceras (Greek: "perfect" (teleos), "horn" (keratos)[4]) is an extinct genus of rhinocerotid. It lived in North America during the Miocene and Pliocene epochs during the Hemingfordian to the end of Hemphillian from around 17.5 to 4.9 million years ago.[5][6] It grew up to lengths of 13 feet (4.0 meters) long.[7]
Teleoceras went extinct in North America alongside Aphelops at the end of the Hemphillian, most likely due to rapid climate cooling, increased seasonality and expansion of C4 grasses, as isotopic evidence suggests that the uptake of C4 plants was far less than that in contemporary horses.[6] The Gray Fossil Site in northeast Tennessee, dated to 4.5-5 million years ago, hosts one of the latest-known populations of Teleoceras, Teleoceras aepysoma.[8]
Description
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Teleoceras had much shorter legs than modern rhinos, and a barrel chest, making its build more like that of a hippopotamus than a modern rhino. Based on this description, Henry Fairfield Osborn suggested in 1898 that it was semi-aquatic and hippo-like in habits. This idea persisted for about a century, but has recently been discounted by isotopic evidence.[6]
Some species of Teleoceras have a small nasal horn, but this appears to be absent in other species such as T. aepysoma.[9] Teleoceras has high crowned (hypsodont) molar teeth, which has historically led to suggestions that the species were grazers. Dental microwear and mesowear analysis alternatively suggest a browsing or mixed feeding (both browsing and grazing) diet.[10] Carbon and oxygen isotope analysis of tooth enamel suggests hippo-like grazing habits, but not aquatic.[11] However, δ18O measurements from Ashfall suggest that the species T. major was semi-aquatic.[12]
Sexual dimorphism
[edit]Teleoceras was sexually dimorphic. Males were larger, with larger tusks (lower incisors), a more massive head and neck, and significantly larger forelimbs. As a result of bimaturism, females matured and stopped growing before males, which is often seen in extant polygynous mammals. Males may have fought for mating rights; healed wounds on skulls have been observed, and healed broken ribs are not uncommon (although not all have their sexes determined). This is further supported by the breeding age female-to-male ratio in the Ashfall Fossil Beds being 4.25:1. There is also a rarity of young adult males preserved at Ashfall, which may be accounted for if they formed bachelor herds away from females and dominant bulls. [11]
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Discovery
[edit]Ashfall Fossil Beds
[edit]Teleoceras major is the most common fossil in the Ashfall Fossil Beds of Nebraska. Over 100 intact T. major skeletons are preserved in ash from the Bruneau-Jarbidge supervolcanic eruption. Of the 20+ taxa present, T. major was buried above the rest, being the last of the animals to succumb (small animals died faster), several weeks or months after the pyroclastic airfall event. Their skeletons show evidence of bone disease, ie hypertrophic pulmonary osteodystrophy (HPOD), as a result of lung failure from the fine volcanic ash.[13]
Most of the skeletons are adult females and young, the breeding age female-to-male ratio being 4.25:1. There is also a rarity of young adult males. If the rhinos at Ashfall represent a herd, this may be accounted for if young adult males formed bachelor herds away from females and dominant bulls. The age demographic is very similar to that of modern hippo herds, as amongst the skeletons, 54% are immature, 30% are young adults, and 16% are older adults. [11]
The greatest concentration of Ashfall fossils is housed in a building called the "Rhino Barn", due to the prevalence of T. major skeletons at the site, of which most were preserved in a nearly complete state. One extraordinary specimen includes the remains of a Teleoceras calf trying to suckle from its mother.[14]
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References
[edit]- ^ Prothero, 2005, p. 94.
- ^ McKenna & Bell, 1997, p. 483.
- ^ Prothero, 2005, p. 122.
- ^ "Glossary. American Museum of Natural History". Archived from the original on 20 November 2021.
- ^ (Prothero, 2005)
- ^ a b c Wang, B.; Secord, R. (2020). "Paleoecology of Aphelops and Teleoceras (Rhinocerotidae) through an interval of changing climate and vegetation in the Neogene of the Great Plains, central United States". Palaeogeography, Palaeoclimatology, Palaeoecology. 542: 109411. Bibcode:2020PPP...54209411W. doi:10.1016/j.palaeo.2019.109411.
- ^ "Region 4: The Great Plains". geology.teacherfriendlyguide.org. Retrieved 2021-06-26.
- ^ Short, Rachel A; Wallace, Steven C. "A New Species of Teleoceras (Mammalia, Rhinocerotidae) from the Late Hemphillian of Tennessee".
{{cite journal}}: Cite journal requires|journal=(help) - ^ Short, Rachel; Wallace, Steven; Emmert, Laura (2019-04-27). "A new species of Teleoceras (Mammalia, Rhinocerotidae) from the late Hemphillian of Tennessee". Bulletin of the Florida Museum of Natural History. 56 (5): 183–260. doi:10.58782/flmnh.kpcf8483. ISSN 2373-9991.
- ^ Mihlbachler, Matthew C.; Campbell, Daniel; Chen, Charlotte; Ayoub, Michael; Kaur, Pawandeep (February 2018). "Microwear–mesowear congruence and mortality bias in rhinoceros mass-death assemblages". Paleobiology. 44 (1): 131–154. Bibcode:2018Pbio...44..131M. doi:10.1017/pab.2017.13. ISSN 0094-8373. S2CID 90987376.
- ^ a b c Mead, Alfred J. (2000). "Sexual dimorphism and paleoecology in Teleoceras , a North American Miocene rhinoceros". Paleobiology. 26 (4): 689–706. doi:10.1666/0094-8373(2000)026<0689:SDAPIT>2.0.CO;2. ISSN 0094-8373.
- ^ Ward, Clark T.; Crowley, Brooke E.; Secord, Ross (15 September 2024). "Home on the range: A multi-isotope investigation of ungulate resource partitioning at Ashfall Fossil Beds, Nebraska, USA". Palaeogeography, Palaeoclimatology, Palaeoecology. 650: 112375. doi:10.1016/j.palaeo.2024.112375. Retrieved 14 November 2024 – via Elsevier Science Direct.
- ^ Tucker, S.T.; Otto, R.E.; Joeckel, R.M.; Voorhies, M.R. (April 2014), "The geology and paleontology of Ashfall Fossil Beds, a late Miocene (Clarendonian) mass-death assemblage, Antelope County and adjacent Knox County, Nebraska, USA", Geologic Field Trips along the Boundary between the Central Lowlands and Great Plains: 2014 Meeting of the GSA North-Central Section, Geological Society of America, pp. 1–22, doi:10.1130/2014.0036(01), ISBN 978-0-8137-0036-6, retrieved 2024-08-13
- ^ "Ashfall Fossil Beds". Archived from the original on 2011-05-18. Retrieved 2005-12-13.
Bibliography
[edit]- McKenna, Malcolm C., and Bell, Susan K. 1997. Classification of Mammals Above the Species Level. Columbia University Press, New York, 631 pp. ISBN 0-231-11013-8
- Prothero, Donald R. 2005. The Evolution of North American Rhinoceroses. Cambridge University Press, Cambridge, 218 pp. ISBN 0-521-83240-3
External links
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Media related to Teleoceras at Wikimedia Commons
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