Tapirus rondoniensis

You can help expand this article with text translated from the corresponding article in Spanish. (November 2016) Click [show] for important translation instructions. Machine translation, like DeepL or Google Translate, is a useful starting point for translations, but translators must revise errors as necessary and confirm that the translation is accurate, rather than simply copy-pasting machine-translated text into the English Wikipedia. Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article. You must provide copyright attribution in the edit summary accompanying your translation by providing an interlanguage link to the source of your translation. A model attribution edit summary is Content in this edit is translated from the existing Spanish Wikipedia article at [[:es:Tapirus rondoniensis]]; see its history for attribution. You may also add the template {{Translated|es|Tapirus rondoniensis}} to the talk page. For more guidance, see Wikipedia:Translation.

Tapirus rondoniensis Temporal range: Pleistocene (Uquian-Ensenadan) ~2–1 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Class:	Mammalia
Order:	Perissodactyla
Family:	Tapiridae
Genus:	Tapirus
Species:	†T. rondoniensis
Binomial name
†Tapirus rondoniensis Holanda, Ribeiro, & Ferigolo 2011

Tapirus rondoniensis is an extinct species of large sized tapir that lived in northwestern parts of Brazil during the Pleistocene. Fossils of the species were found in the Río Madeira Formation of Rondônia, after which the species is named.

This species was originally described by Elizete Celestino Holanda, Ana Maria Ribeiro, and Jorge Ferigolo, in 2011, using materials from the Upper Pleistocene of the Madeira River Formation, in Araras, Nova Mamoré municipality, Rondonia state, Brazil.

The type specimen of Tapirus rondoniensis is an almost complete skull with a unique combination of characteristics that differ from those of current and fossil species of Tapirus described in South America.

It is mainly identified by its broad frontals that support pneumatization that extends to the frontoparietal suture, a high sagittal crest, and a weakly molarized P2. T. rondoniensis is similar in some respects to T. terrestris, but retains some primitive cranial and dental character states like T. pinchaque, such as broad fronts and a weakly molarized P2.^[1]

An extensive study of all the materials collected in the fossil deposits of the Tapirus genus concluded that this is a valid species.^[2]

On the basis of morphometric analysis of its teeth, it is concluded that T. rondoniensis is significantly smaller than most fossil or living tapirs, such as T. indicus, T. oliverasi, T. tarijensis, and T. haysii; and that it was similar in size to T. terrestris and T. mesopotamicus.^[3]

On the basis of cladistic-morphological analysis, it was indicated that T. rondoniensis is the closest species to the living T. kabomani, from which it differs by possessing 3 autapomorphies.^[4]

This prehistoric odd-toed ungulate-related article is a stub. You can help Wikipedia by expanding it.

• v
• t
• e