The late Eocene prosimian Wadilemur elegans from the Jebel Qatrani Formation, northern Egypt, was originally interpreted as an anchomomyin adapiform primate based on limited information from the lower molars and distal premolars. Recently recovered fossils attributable to this species, including a proximal femur, the fourth upper premolar and first and second upper molars, and a mandible preserving the lower second premolar and lower canine and incisor alveoli, reveal a number of derived morphological similarities shared with crown strepsirrhines and, in particular, Miocene-to-Recent stem and crown galagids, to the exclusion of known adapiforms. Phylogenetic analysis of 359 morphological features scored across 95 living and extinct crown primate taxa supports a stem galagid placement for Wadilemur and older Saharagalago, and a close relationship between crown strepsirrhines and the Eocene African taxa ''Anchomomys'' milleri, Djebelemur, and Plesiopithecus (none of which appear to be closely related to European anchomomyins). This scheme of relationships supports the hypothesis that crown Strepsirrhini is of Afro-Arabian origin and that lemuriforms likely colonized Madagascar by crossing the Mozambique Channel. Wadilemur's known dental and postcranial morphology provides additional support for the hypothesis that galagids and lorisids had diverged by the close of the middle Eocene, and, by bolstering the Ϸ37 million-year-old calibration point for crown lorisiform origins provided by Saharagalago, indirect support for the hypothesis of an ancient origin of crown Strepsirrhini and crown Primates.Fayum ͉ Galagidae ͉ Lorisiformes ͉ Strepsirrhini ͉ primates T he time and place of origin of the crown strepsirrhine or ''toothcombed'' prosimian clade, the group containing the Malagasy lemurs, African galagos, and Afro-Asian lorises, has long been a matter of great interest to primatologists (1-4). For many decades, the oldest undoubted fossil members of crown Strepsirrhini were early Miocene [Ϸ20 Megannum (Ma, Megannum ϭ million years old)] lorisiforms from Kenya and Uganda (5-10), but the recent discovery of a Ϸ37 Ma stem galagid (Saharagalago) in northern Egypt (11) has almost doubled this minimum paleontological estimate for the time of origin of both crown lorisiforms and crown strepsirrhines. Independent estimates for the timing of the loris-galago divergence derived from DNA sequence data (12-14) have since come to show remarkable congruence with this fossil evidence in supporting a middle Eocene origin for crown lorisiforms, but this critical new calibration point within crown Strepsirrhini also lends indirect support to the controversial hypothesis of a Ϸ80 Ma origin for crown primates (13,15,16) that is inconsistent with current interpretations of the fossil record documenting early primate evolution (e.g., ref. 17). Given the pivotal role that Saharagalago has come to play in debates surrounding the timing of crown lorisiform, lemuriform, strepsirrhine, and primate origins (13,14,18), it is important that an Eo...