TL;DR: Fossils of two previously unknown genera and species of Egyptian early Tertiary Anthropoidea discovered in the Fayum Depression of Egypt appear to be the oldest primates undoubtedly related to humans and their dental anatomy points to a derivation of Anthropoida from Eocene adapids.
Abstract: In 1987 and 1988 fossils of two previously unknown genera and species of Egyptian early Tertiary Anthropoidea were discovered in the Fayum Depression of Egypt These are much older than all other Fayum, Oligocene primates and are believed to be Eocene in age These genera, here named Catopithecus and Proteopithecus, come from a new Fayum site, L-41, and resemble Oligopithecus from the Jebel Qatrani Formation (lower sequence) at quarry E They are here placed with the latter in a subfamily, Oligopithecinae, that is ranked in the Propliopithecidae The level of L-41 is separated from quarry E by at least one major unconformity and 47 m of section Only a maxilla of Proteopithecus is known Its molars and premolars resemble those of later Fayum Propliopithecus and Aegyptopithecus and do not resemble those of Apidium and Parapithecus, all of which come from the Jebel Qatrani Formation, upper sequence The type specimen of Catopithecus confirms a lower dental formula of 2-1-2-3, as in Catarrhini These species appear to be the oldest primates undoubtedly related to humans Their dental anatomy points to a derivation of Anthropoidea from Eocene adapids
TL;DR: Qualitative observations and multivariate morphometric analyses reveal that the astragalar morphology of Proteopithecus is very similar to that of early Oligocene parapithecids and living and extinct small-bodied platyrrhines, and strengthens the hypothesis that the morphological pattern shared by these taxa is primitive within crown Anthropoidea.
TL;DR: A basal African anthropoid dental morphotype is constructed and compared with two of the best-represented proposed basal anthropoids, Eosimias and Djebelemur, with the result that neither appears to be a good candidate to have been ancestral to the African anthropoids.
Abstract: Among the earliest fossil anthropoid primates known are Catopithecus browni, Serapia eocaena, Arsinoea kallimos, and Proteopithecus sylviae, from the late Eocene quarry L-41, Fayum Depression, Egypt. Two of these taxa, C. browni and S. eocaena, may be the oldest known members of the Propliopithecidae and Parapithecidae, respectively, while A. kallimos and P. sylviae are archaic anthropoids of less certain familial affiliation. Dental features of C. browni, S. eocaena, A. kallimos, and P. sylviae are compared with those of younger propliopithecids and parapithecids from the Fayum in order to determine the morphocline polarities of dental features among these early anthropoids. From this, a basal African anthropoid dental morphotype is constructed. Among the features of this morphotype are: dental formula of 2.1.3.3; incisors subvertically implanted and somewhat spatulate; p2 as large as p3, both lacking paraconids; p4 weakly obliquely oriented but not exodaenodont; all lower molars with small paraconids present; upper anterior premolars lacking protocone; upper molars with small, cingular hypocones, all cheek teeth nonbunodont; and canines projecting but not necessarily sexually dimorphic. Comparisons are made between this African anthropoid morphotype and two of the best-represented proposed basal anthropoids, Eosimias and Djebelemur, with the result that neither appears to be a good candidate to have been ancestral to the African anthropoids. Other possible basal simians such as Algeripithecus, Tabelia, and Biretia also are evaluated but are too poorly known for adequate analysis. The larger-bodied Asian primates Pondaungia, Amphipithecus, and Siamopithecus also are not likely ancestors for African anthropoids, but like Eosimias they may share a common ancestry. Despite many recent claims of an Asian origin for anthropoids, the evidence remains far from compelling. The true origins of Anthropoidea remain obscure.
TL;DR: Old World Anthropoidea or Catarrhini can now be traced back to Catopithecus in Egypt, and a set of derived cranial and dental features that first occur in combination in this fossil are shown.
Abstract: Recent finds of Catopithecus browni at an upper Eocene fossil site in the Fayum depression, Egypt, reveal features of the earliest higher primates. This basal anthropoidean shows a set of derived cranial and dental features that first occur in combination in this fossil. Old World Anthropoidea or Catarrhini can now be traced back to Catopithecus in Egypt. Size, shape, orientation of incisors and canines, and other features of the teeth and skull relate Catopithecus both to later Anthropoidea and to the early and middle Eocene cercamoniine adapoids. Most defining characteristics of higher primates cannot be documented earlier than the late Eocene of Africa.
TL;DR: Qualitative and morphometric analyses indicate that humeri of the oligopithecine Catopithecus are more similar to early Oligocene propliopithecines than they are to any other Paleogene anthropoid taxon, and that Proteopitalcus exhibits humeral similarities to parapithecids that may be symplesiomorphies of extant (or "crown") Anthropoidea.
Abstract: A number of recent studies have, by necessity, placed a great deal of emphasis on the dental evidence for Paleogene anthropoid interrelationships, but cladistic analyses of these data have led to the erection of phylogenetic hypotheses that appear to be at odds with biogeographic and stratigraphic considerations. Additional morphological data from the cranium and postcranium of certain poorly understood Paleogene primates are clearly needed to help test whether such hypotheses are tenable. Here we describe humeri attributable to Proteopithecus sylviae and Catopithecus browni, two anthropoids from late Eocene sediments of the Fayum Depression in Egypt. Qualitative and morphometric analyses of these elements indicate that humeri of the oligopithecine Catopithecus are more similar to early Oligocene propliopithecines than they are to any other Paleogene anthropoid taxon, and that Proteopithecus exhibits humeral similarities to parapithecids that may be symplesiomorphies of extant (or “crown”) Anthropoidea. The humeral morphology of Catopithecus is consistent with certain narrowly distributed dental apomorphies—such as the loss of the upper and lower second premolar and the development of a honing blade for the upper canine on the lower third premolar—which suggest that oligopithecines constitute the sister group of a clade containing propliopithecines and Miocene-Recent catarrhines and are not most closely related to Proteopithecus as has recently been proposed.