Ursus rossicus (the Pleistocene small cave bear)[1] is an extinct species of bear that lived in the steppe regions of northern Eurasia and Siberia during the Pleistocene.
| Ursus rossicus Temporal range: Middle to Late Pleistocene,
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| Skeleton in Zoological Museum, Saint Petersburg | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Order: | Carnivora |
| Family: | Ursidae |
| Genus: | Ursus |
| Species: | †U. rossicus
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| Binomial name | |
| †Ursus rossicus Borissiak, 1930
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Discovery edit
Vereshchagin discovered the first U. rossicus remains in the Altai Mountains in 1973. Mandibles of the bear were found in Bachatsk Quarry, Krasni Yar (in Tomsk Province) and Mokhovo Quarry; skull fragments were found in Krasni Yar.[1] More fossil remains of U. rossicus were discovered in the famous Denisova Cave.[2]
Description edit
The small cave bear had a very broad, domed skull with a steep forehead. Its stout body had long thighs, massive shins and in-turning feet, making it similar in skeletal structure to the brown bear.[3] Cave bears were comparable in size to the largest modern-day bears.[4]
Diet edit
Cave bear teeth show greater wear than most modern bear species, suggesting a diet of tough materials. However, tubers and other gritty food, which cause distinctive tooth wear in modern brown bears, do not appear to have constituted a major part of cave bears' diets on the basis of dental microwear analysis.[5]
The morphological features of the cave bear chewing apparatus, including loss of premolars, have long been suggested to indicate their diets displayed a higher degree of herbivory than the Eurasian brown bear. Indeed, a solely vegetarian diet has been inferred on the basis of tooth morphology. Results obtained on the stable isotopes of cave bear bones also point to a largely vegetarian diet in having low levels of nitrogen-15 and carbon-13,[6] which are accumulated at a faster rate by carnivores as opposed to herbivores.
Cave bears of the last ice age lacked the usual two or three premolars present in other bears; to compensate, the last molar is very elongated, with supplementary cusps.[7]
References edit
- ^ a b Baryshnikov, G.; Foronova, I. (2001). "Pleistocene small cave bear (Ursus rossicus) from the South Siberia, Russia" (PDF). Cadernos Lab. Xeolóxico de Laxe. 26: 373–398. Archived from the original (PDF) on 8 March 2021. Retrieved 15 April 2015.
- ^ Puzachenko, A.Yu.; Titov, V.V.; Kosintsev, P.A. (20 December 2021). "Evolution of the European regional large mammals assemblages in the end of the Middle Pleistocene – The first half of the Late Pleistocene (MIS 6–MIS 4)". Quaternary International. 605–606: 155–191. doi:10.1016/j.quaint.2020.08.038. Retrieved 22 January 2024 – via Elsevier Science Direct.
- ^ Brown, Gary (1996). Great Bear Almanac. Lyons & Burford. p. 340. ISBN 1-55821-474-7.
- ^ Macdonald, David (1992). The Velvet Claw. New York: Parkwest. p. 256. ISBN 0-563-20844-9.
- ^ Pinto Llona, A. C., Andrews, P. & Etxeberrı´a, P. 2005: Taphonomy and Palaeoecology of Cave Bears from the Quaternary of Cantabrian Spain. Fondacio´n de Asturias/Du Pont Ibe´rica/The Natural History Museum, Grafinsa, Oviedo.
- ^ Bocherens, H.; et al. (2006). "Bears and humans in Chauvet Cave (Vallon-Pont-d'Arc, Ardeche, France): Insights from stable isotopes and radiocarbon dating of bone collagen". Journal of Human Evolution. 50 (3): 370–376. doi:10.1016/j.jhevol.2005.12.002. PMID 16442587.
- ^ Gli orsi spelèi delle Conturines/ Ursus Spelaeus. Altabadia.it. Retrieved on 2011-09-26.
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