Egyptian Miocene Jaw Fossil Places Early Ape Radiation in North Africa 17-18 Million Years Ago
The 17-18 Ma Egyptian ape jaw challenges the East-African-only model of early hominoid origins and implies a more northern cradle with flexible diets suited to seasonal environments. Evidence rests on one mandible whose dental traits link it to crown Hominoidea while expanding known Miocene range northward. Additional fossils and dates are needed to confirm the pattern.
The Mansoura-USC team recovered the specimen during 2023-2024 field seasons at Wadi Moghra, a site previously known only for cercopithecoid monkeys. The robust mandible combines large canines, sectorial premolars, and bunodont molars with thick enamel, features that align it with early hominoids while differing from contemporaneous East African taxa such as Proconsul. Dental microwear and enamel thickness suggest a fallback diet of hard objects during seasonal fruit scarcity, consistent with Miocene aridification pulses recorded in North African paleosols. This single specimen fills a geographic gap that previously forced phylogenetic models to route the hominoid stem through southern corridors only.
Earlier phylogenies relied on the absence of definitive apes north of 10° N latitude to argue for an East African cradle. The new morphology forces re-evaluation of dispersal routes across the Tethyan margin and raises the possibility that Middle Eastern and Arabian corridors connected Eurasian and African ape populations earlier than assumed. Comparable dental traits appear in 16-million-year-old Turkish and Pakistani material, hinting at bidirectional exchange rather than unidirectional southward spread.
The find also reframes the timing of crown-group diversification relative to the Middle Miocene Climatic Optimum. If northern latitudes hosted early hominoids, then later European and Asian radiations may represent range expansions from a broader ancestral distribution rather than independent migrations from the south. Future targeted surveys in Libyan and Tunisian Early Miocene basins could test this expanded range within a decade.
The main limitation is the single fragmentary jaw; cranial and postcranial elements are required to anchor its position in character matrices. Larger samples and radiometric dates from additional North African sites would strengthen the geographic claim and allow quantitative biogeographic modeling.
Sallam Lab: Within 36 months, at least one additional North African Early Miocene site will yield postcranial hominoid remains confirming locomotor diversity outside East Africa.
Sources (2)
- [1]Primary Source(https://www.science.org/doi/10.1126/science.adx1234)
- [2]Supporting Source(https://www.nature.com/articles/s41559-025-02789-3)