Palaeontological evidence for an Oligocene divergence between Old World monkeys and apes

• Nancy J. Stevens,
• Erik R. Seiffert,
• Patrick M. O’Connor,
• Eric M. Roberts,
• Mark D. Schmitz,
• Cornelia Krause,
• Eric Gorscak,
• Sifa Ngasala,
• Tobin L. Hieronymus
• & Joseph Temu

• Affiliations
• Contributions
• Corresponding author

Nature

(2013)

doi:10.1038/nature12161

Received

21 February 2013

Accepted

05 April 2013

Published online

15 May 2013

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Apes and Old World monkeys are prominent components of modern African and Asian ecosystems, yet the earliest phases of their evolutionary history have remained largely undocumented¹. The absence of crown catarrhine fossils older than ~20 million years (Myr) has stood in stark contrast to molecular divergence estimates of ~25–30 Myr for the split between Cercopithecoidea (Old World monkeys) and Hominoidea (apes), implying long ghost lineages for both clades^{2, 3, 4}. Here we describe the oldest known fossil ‘ape’, represented by a partial mandible preserving dental features that place it with ‘nyanzapithecine’ stem hominoids. Additionally, we report the oldest stem member of the Old World monkey clade, represented by a lower third molar. Both specimens were recovered from a precisely dated 25.2-Myr-old stratum in the Rukwa Rift, a segment of the western branch of the East African Rift in Tanzania. These finds extend the fossil record of apes and Old World monkeys well into the Oligocene epoch of Africa, suggesting a possible link between diversification of crown catarrhines and changes in the African landscape brought about by previously unrecognized tectonic activity⁵ in the East African rift system.

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