Giraffokeryx

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Giraffokeryx
Temporal range: Miocene, 14–11  Ma
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Giraffokeryx punjabiensis 2.jpg
Skull of G. punjabiensis (YPM VP 013943)
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Artiodactyla
Family: Giraffidae
Genus: Giraffokeryx
Pilgrim 1910 [1]
Type species
Giraffokeryx punjabiensis
Pilgrim, 1910
Species

Giraffokeryx is an extinct genus of medium-sized giraffids known from the Miocene of the Indian subcontinent and Eurasia. It is distinguished from other giraffids by the four ossicones on its head; one pair in front of the eyes on the anterior aspect of the frontal bone and the other behind the eyes in the frontoparietal region overhanging the temporal fossae. It has a brachydont dentition like in other giraffids and its legs and feet are of medium length. [2] Giraffokeryx is considered monotypic by most authors, in the form of G. punjabiensis, but other species have been assigned to the genus:

Contents

Giraffokeryx resembled either an okapi or a small giraffe. It is a possible ancestor of both. [5]

See also

References

  1. Giraffokeryx in the Paleobiology Database retrieved June 2013
  2. Bhatti, Z.H.; Khan, M.A.; Khan, A.M.; Akhtar, M.; Ghaffar, A.; Iqbal, M.; Ikram, T. (December 2012). "Giraffokeryx (Artiodactyla: Mammalia) remains from the lower Siwaliks of Pakistan" (PDF). Pakistan Journal of Zoology. 44 (6): 1623–1631. 824419715.
  3. Bhatti et al. 2012 , pp. 1628–9
  4. Geraads, D.; Aslan, F. (2003). "Giraffidae from the middle Miocene hominoid locality of Çandır (Turkey)" (PDF). Courier Forschungsinstitut Senckenberg (240). 695125429.
  5. Mitchell, G.; Skinner, J. D. (2003). "On the origin, evolution and phylogeny of giraffes Giraffa camelopardalis" (PDF). Transactions of the Royal Society of South Africa. 58 (1): 51–73. Bibcode:2003TRSSA..58...51M. doi:10.1080/00359190309519935. S2CID   6522531.

Further reading

Pilgrim, G. E. (1910). "Notices of new mammalian genera and species from the Tertiaries of India". Records of the Geological Survey of India. 40 (1): 63–71.