Ursavus
Temporal range:
Cast skull of Ursavus tedfordi
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Carnivora
Family: Ursidae
Tribe: †Ursavini
Genus: †Ursavus
Schlosser, 1899
Type species
†Ursavus brevirhinus
Hofmann, 1887
Species[1]
  • †Ursavus brevirhinus (Hofmann, 1887)
  • †Ursavus primaevus (Gaillard, 1899)
  • †Ursavus intermedius (Koenigswald, 1925)
  • †Ursavus pawniensis (Frick, 1926)
  • †Ursavus ehrenbergi (Brunner, 1942)
  • †Ursavus sylvestris (Qiu & Qi, 1990)
  • †Ursavus isorei (Ginsburg & Morales, 1998)
  • †Ursavus tedfordi (Zhanxiang et al., 2014)

Ursavus is an extinct genus of bear that existed in North America, Europe, and Asia during the Miocene period, about 23–5.3 million years ago (Mya), existing for roughly 17.7 million years.[2][3] The genus apparently dispersed from Asia into North America about 20 Mya, becoming the earliest member of the subfamily Ursinae in the New World.[4] Qiu points out that if a questionable 29 million-year-old specimen of Ursavus reported in North America is validated, Ursavus may have evolved in North America and dispersed westward into Asia. The higher number of fossils in Europe grading toward eastern Asia make the westward dispersal unlikely.

U. elmensis, also known as the "dawn bear"[5] is generally taken to be the earliest undisputed bear species.[6][7]

Description

Restoration of Ursavus (middle left) and other animals of the Haystack Assemblage

In life, the various species would have been between cat-sized for the smaller species[8] and wolf-sized for the larger members of the genus [9] and were mainly omnivores or hypocarnivores.

Most other species are known from teeth and skull fragments. A complete skull has been found in the Gansu region of China of a new species from the late Miocene, dubbed U. tedfordi.[1] It was about the size of a wolf and – except for the giant panda and the spectacled bear – is believed to be the nearest to the common ancestor of modern bears.

Currently, the only member known from a complete skeleton is U. orientalis, found in the Shanwang diatomite of Early Miocene China.[8][10] However, Qiu et.al. (2014) have suggested reassignment of U. orientalis to the genus Ballusia, in which case it would no longer be considered part of Ursavus.[1]

Fossil distribution

A partial list of find sites and specimen ages:

References

  1. 1 2 3 4 5 Qiu, Zhan-Xiang; et al. (2014). "A Late Miocene Ursavus skull from Guanghe, Gansu, China". Vertebrata PalAsiatica. 52 (3): 265–302.
  2. ↑ Kurten, Bjorn (1966). "Pleistocene bears of North America I: Genus Tremarctos, spectacled bears". Acta Zool. Fenn. 115: 1–120.
  3. ↑ Crusafont, M.; Kurten, B. (1976). "Bears and bear-dogs from the Vallesian of the Valles-Penedes basin, Spain". Acta Zool. Fenn. 144: 1–29.
  4. ↑ Zhanxiang, Qiu (2003). "Dispersals of Neogene carnivorans between Asia and North America". Bulletin of the American Museum of Natural History. 279 (279): 18–31. doi:10.1206/0003-0090(2003)279<0018:C>2.0.CO;2. S2CID 88183435.
  5. ↑ Derocher, Andrew E.; Ian Stirling (February 1989). "Factors affecting the evolution and behavioral ecology of the modern bears". Bears: Their Biology and Management. A selection of papers from the Eighth International Conference on Bear Research and Management (published 1990). 8: 189–204. doi:10.2307/3872919. JSTOR 3872919.
  6. ↑ McLellan, Bruce (1994). "A review of bear evolution" (PDF). [Proceedings of the] International Conference on Bear Research and Management. 9 (1): 85–96.
  7. ↑ Derocher, A. E.; Lynch, W. (2012). Polar Bears: A complete guide to their biology and behavior. Baltimore: Johns Hopkins University Press.
  8. 1 2 3 4 Lindburg, Donald G. (2004). Giant Pandas: Biology and Conservation. University of California Press. p. 46. ISBN 9780520238671.
  9. ↑ phys.org news
  10. 1 2 Yang, Hong; Shipu Yang (December 1994). "The Shanwang fossil biota in eastern China: a Miocene Konservat-Lagerstätte in lacustrine deposits" (PDF). Lethaia. 27 (4): 345–354. doi:10.1111/j.1502-3931.1994.tb01585.x.
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