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Anaptomorphinae
Anaptomorphinae is a pre-historic group of primates known from Eocene fossils in North America and Europe and later periods of Paleocene Asia, and are a sub-family of omomyids. The anaptomorphines is a paraphyletic group consisting of the two tribes Trogolemurini and Anaptomorphini. Anaptomorphine radiation in Wyoming, one of the most detailed records of changes within populations and between species in the fossil record, has provided remarkable evidence of transitional fossils. Description '' Teilhardina'' is the most primitive of the anaptomorphines with respect a number of dental features (e.g. four premolars and relatively unreduced canine). Most scientists recognize at least fourteen ''genera'' of anaptomorphine. The probable lineages of ''Tetonius'', ''Absarokius'' and ''Anemorhysis'' evolved from ''Teilhardinia'' or a closely related form from North America. ''Tetonius'' and ''Shoshonius'' have been classified as belonging to the Tarsiiformes, and are therefore not close ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Omomyidae
Omomyidae is a group of early primates that radiated during the Eocene epoch between about (mya). Fossil omomyids are found in North America, Europe & Asia making it one of two groups of Eocene primates with a geographic distribution spanning holarctic continents, the other being the adapids (family Adapidae). Early representatives of the Omomyidae and Adapidae appear suddenly at the beginning of the Eocene (56 mya) in North America, Europe, and Asia, and are the earliest known crown primates. Etymology The Omomyidae are named after the type genus '' Omomys''. While the etymology of this genus is uncertain, it most likely derives from the Ancient Greek ὠμός (ōmós), "raw, crude" + μῦς (mûs), "mouse". Characteristics Features that characterize many omomyids include large orbits (eye sockets), shortened rostra and dental arcades, loss of anterior premolars, cheek teeth adapted for insectivorous or frugivorous diets, and relatively small body mass (i.e., less than 500 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teilhardina
''Teilhardina'' (, ) was an early marmoset-like primate that lived in Europe, North America and Asia during the Early Eocene epoch, about 56-47 million years ago. The paleontologist George Gaylord Simpson is credited with naming it after the French paleontologist, Jesuit and philosopher Teilhard de Chardin. Paleobiology Carbon isotope excursion suggests that the Asian ''Teilhardina asiatica'' is the oldest member of the genus; the youngest is the North American ''Teilhardina brandti''. However finds in Wyoming suggest ''Teilhardina'' may have originated in North America. There are four hypotheses that have been proposed to try and explain the geographic distribution: # Africa was the origination of the primates and then they dispersed to Europe- Greenland and finally North America. # Primates originated in North America then dispersed to Asia through the Bering route and later passed through Greenland to finally reach Europe. # Primates originated in Asia or Africa and disper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bownomomys
''Bownomomys'' was an early marmoset-like primate that lived in North America during the Early Eocene epoch, about 56-50 million years ago. Taxonomy ''Teilhardina americana'' and ''T. crassidens'' were originally named as species of ''Teilhardina'', usually considered a member of Omomyidae. However, phylogenetic analysis by Ni et al. (2004) recovered ''Teilhardina'' as polyphyletic, with ''Teilhardina belgica'' and ''T. asiatica'' nested as the basalmost haplorrhines, and ''T. americana'' and ''T. crassidens'' being recovered as anaptomorphine omomyids (and thus more closely related to the tarsiers than to simians The simians, anthropoids, or higher primates are an infraorder (Simiiformes ) of primates containing all animals traditionally called monkeys and apes. More precisely, they consist of the parvorders New World monkeys (Platyrrhini) and Catarrhi ...). ''Teilhardina crassidens'' was later referred to the genus '' Baataromomys'' by Ni et al. (2007). A paper by Mors ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Paleocene
The Thanetian is, in the International Commission on Stratigraphy, ICS Geologic timescale, the latest age (geology), age or uppermost stage (stratigraphy), stratigraphic stage of the Paleocene epoch (geology), Epoch or series (stratigraphy), Series. It spans the time between . The Thanetian is preceded by the Selandian Age and followed by the Ypresian Age (part of the Eocene). The Thanetian is sometimes referred to as the Late Paleocene. Stratigraphic definition The Thanetian was established by Switzerland, Swiss geologist Eugène Renevier in 1873. The Thanetian is named after the Thanet Formation, the oldest Cenozoic deposit of the London Basin, which was first identified in the area of Kent (southern England) known as the Isle of Thanet. The base of the Thanetian Stage is laid at the base of magnetic chronozone C26n. The references profile (Global Boundary Stratotype Section and Point) is in the Zumaia section (43° 18'N, 2° 16'W) at the beach of Itzurun, Pais Vasco, northern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
