TL;DR: Cantius torresi has premolars reminiscent of those in Omomyidae, suggesting that earlier lemuriform and tarsiiform primates were closely related and little differentiated at the beginning of the Eocene as discussed by the authors.
Abstract: The oldest primates of modern aspect (primates of prosimian tarsiiform-lemuriform or higher grade) are known from Lower Eocene strata of Sparnacian age in Europe1,2, Bumbanian age in Asia3,4, and Wasatchian age in North America5. These first appearances coincide on all three northern continents with initial records of Artiodactyla, Perissodactyla and other modern mammalian groups appearing approximately 53 Myr BP6,7. Here I report that a newly discovered basal Wasatchian f aunal assemblage older than any known previously includes the well-preserved dental remains of a new species of Cantius, the earliest representative of Eocene Adapidae and the oldest evidence of primates of modern aspect known from North America. This new Cantius is possibly ancestral to all later adapids, including the European Donrussellia and North American Pelycodus. Cantius torresi has premolars reminiscent of those in Omomyidae, suggesting that earlier lemuriform and tarsiiform primates were closely related and little differentiated at the beginning of the Eocene.
TL;DR: More than one hundred undescribed foot elements of Cantius and other closely related notharctine adapids (7 species in all) from throughout the early Eocene (Wasatchian) Willwood Formation of the Bighorn Basin, Wyoming, have been analyzed as discussed by the authors.
Abstract: More than one hundred undescribed foot elements of Cantius and other closely related notharctine adapids (7 species in all) from throughout the early Eocene (Wasatchian) Willwood Formation of the Bighorn Basin, Wyoming, have been analyzed. For four species (Cantius ralstoni, “Copelemur” feretutus, Cantius frugivorus, and? Pelycodus jarrovii) these represent the first described postcranial material. The clade of Cantius and allied genera in the Bighorn Basin includes several speciation events and both increases and decreases in body size. The largest species represented by tarsal remains (? Pelycodus jarrovii) is several times larger than the smallest, Cantius ralstoni. However, despite the number of species, temporal duration, and range of body size represented, there are no obvious changes in foot morphology as measured by various indices or by observation of qualitative features. This contrasts with the more obvious changes in dental features (e.g., development of hypocone and mesostyle) in the same group of species described by earlier authors. The fossil record of Cantius thus illustrates different kinds of evolutionary change in the dentition and tarsus. The dentition changes in both size and shape while the tarsus changes only in size. We describe significant differences in foot anatomy which distinguish notharctines from extant strepsirhines, including the nature of the articulations between the navicular and cuboid and the distal tarsus with the metatarsus. These features indicate that the fossil taxa are not particularly closely allied phylogenetically to either extant strepsirhines in general or lemurids in particular.
TL;DR: Newly discovered later Eocene (Uintan) primates (adapids, omomyids, and microsyopids) from San Diego Co., California are described and compared with those of other Eocene faunas in Ventura Co..
Abstract: Newly discovered later Eocene (Uintan) primates (adapids, omomyids, and microsyopids) from San Diego Co., California are described and compared with those of other Eocene faunas in Ventura Co. (Sespe Formation) and the North American western interior. The 11 species of primates from San Diego Co. lived in coastal lowland riparian and deltaic environments; their remains are preserved in the Friars and Mission Valley formations (early Uintan, greater San Diego area) and Santiago Formation (later Uintan, northwestern San Diego Co.). Genera previously known from the western interior but recorded for the first time from the west coast include Pelycodus, Notharctus, Hemiacodon , and ? Macrotarsius ; to these is added Omomys , as I consider Stockia powayensis a species of Omomys . Range extensions into the early Uintan include Pelycodus, Notharctus , and Hemiacodon . The southerly climes of the Californian later Eocene coastal areas may have served as temporary havens for species that became extirpated earlier in the western interior. All nine primate species recorded from the early Uintan of the west coast had close relatives in the western interior, a faunal similarity shared by other vertebrates. Late in the Uintan, west coastal endemism increased as barriers to faunal interchange developed between the two areas.