A new orang-utan relative from the Late Miocene of Thailand.

Nature

Paleontology Section, Geological Survey Division, Department of Mineral Resources, Bangkok-10400, Thailand.

Published: January 2004

AI Article Synopsis

  • The fossil record for great apes is limited, highlighting the importance of new finds, especially in equatorial forest regions, to deepen our understanding of their evolution.
  • Two main theories exist about orangutan origins: one links them to Lufengpithecus due to dental similarities, while the other points to Sivapithecus based on facial traits; however, other evidence doesn't support these claims.
  • The discovery of a new hominoid species, Khoratpithecus piriyai, from Late Miocene Thailand indicates it shares unique traits with orangutans, suggesting it is their closest known relative and evolved in a tropical environment, unlike those in Southern China and Pakistan.

Article Abstract

The fossil record of the living great apes is poor. New fossils from undocumented areas, particularly the equatorial forested habitats of extant hominoids, are therefore crucial for understanding their origins and evolution. Two main competing hypotheses have been proposed for orang-utan origins: dental similarities support an origin from Lufengpithecus, a South Chinese and Thai Middle Miocene hominoid; facial and palatal similarities support an origin from Sivapithecus, a Miocene hominoid from the Siwaliks of Indo-Pakistan. However, materials other than teeth and faces do not support these hypotheses. Here we describe the lower jaw of a new hominoid from the Late Miocene of Thailand, Khoratpithecus piriyai gen. et sp. nov., which shares unique derived characters with orang-utans and supports a hypothesis of closer relationships with orang-utans than other known Miocene hominoids. It can therefore be considered as the closest known relative of orang-utans. Ancestors of this great ape were therefore evolving in Thailand under tropical conditions similar to those of today, in contrast with Southern China and Pakistan, where temperate or more seasonal climates appeared during the Late Miocene.

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http://dx.doi.org/10.1038/nature02245DOI Listing

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