Anthracobune Temporal range: | |
---|---|
Life restoration | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Family: | †Anthracobunidae |
Genus: | †Anthracobune Pilgrim 1940 |
Species[1] | |
| |
The inferred range of Anthracobune |
Anthracobune ("coal mound") is an extinct genus of stem perissodactyl from the middle Eocene of the Upper Kuldana Formation of Kohat, Punjab, Pakistan.[2]
The size of a small tapir, it lived in a marshy environment and fed on soft aquatic plants. It is the largest known anthracobunid. This group was formerly classified with proboscideans.
Notes
- ↑ Cooper, L. N.; Seiffert, E. R.; Clementz, M.; Madar, S. I.; Bajpai, S.; Hussain, S. T.; Thewissen, J. G. M. (2014-10-08). "Anthracobunids from the Middle Eocene of India and Pakistan Are Stem Perissodactyls". PLOS ONE. 9 (10): e109232. Bibcode:2014PLoSO...9j9232C. doi:10.1371/journal.pone.0109232. PMC 4189980. PMID 25295875.
- ↑ "Fossilworks: Anthracobune". fossilworks.org. Retrieved 17 December 2021.
References
- Kumar, Kishor (1991). "Anthracobune aijiensis nov. sp. (Mammalia: Proboscidea) from the Subathu Formation, Eocene from NW Himalaya, India". Geobios. 24 (2): 221–39. Bibcode:1991Geobi..24..221K. doi:10.1016/s0016-6995(91)80010-w. OCLC 4656806310.
- Pilgrim, G. E. (1940). "Middle Eocene mammals from north-west Pakistan". Proceedings of the Zoological Society. B. London. 110: 127–152. doi:10.1111/j.1469-7998.1940.tb00029.x.
- Sahni, A.; Kumar, K. (1980). "Lower Eocene Sirenia, Ishatherium subathuensis, gen. et sp. nov. from the type area, Subathu Formation, Subathu, Simla Himalayas, H. P." (PDF). Journal of the Palaeontological Society of India. 23&24: 132–5. Retrieved 1 July 2013.
- Wells, N.A.; Gingerich, P.D. (1983). "Review of Eocene Anthracobunidae (Mammalia, Proboscidea) with a new genus and species, Jozaria palustris, from the Kuldana Formation of Kohat (Pakistan)" (PDF). Contrib. Mus. Pal. Univ. Michigan. 26 (7): 117–139. OCLC 742731409.
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