Dendropithecidae
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Dendropithecidae
The family Dendropithecidae is an extinct family of catarrhine monkeys. They date from the Early Miocene, around 20 - 12 million years ago. Fossils of the two ''Dendropithecus'' species, ''Dendropithecus macinnesi'' and ''Dendropithecus ugandensis'', have been found in East Africa, including several partial skeletons of ''Dendropithecus macinnesi'' on Rusinga Island in Lake Victoria. Other species are ''Simiolus andrewsi'', ''Simiolus cheptumoae'', ''Simiolus enjiessi''. ''Micropithecus clarki'' and ''Micropithecus leakeyorum'' may not be part Dendropithecidae, and may be sister to the crown Catarrhini (or, depending on the definition, the apes and the Cercopithecidae may have emerged in the Dendropithecidae). The later Nyanzapithecinae (including ''Oreopithecus ''Oreopithecus'' (from the Greek , and , , meaning "hill-ape") is an extinct genus of hominoid primate from the Miocene epoch whose fossils have been found in today's Tuscany and Sardinia in Italy. It existed nine to ...
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Hominoidea
Apes (collectively Hominoidea ) are a clade of Old World simians native to sub-Saharan Africa and Southeast Asia (though they were more widespread in Africa, most of Asia, and as well as Europe in prehistory), which together with its sister group Cercopithecidae form the catarrhine clade, cladistically making them monkeys (though this is the subject of much debate). Apes do not have tails due to a mutation of the TBXT gene. In traditional and non-scientific use, the term "ape" can include tailless primates taxonomically considered Cercopithecidae (such as the Barbary ape and black ape), and is thus not equivalent to the scientific taxon Hominoidea. There are two extant branches of the superfamily Hominoidea: the gibbons, or lesser apes; and the hominids, or great apes. * The family Hylobatidae, the lesser apes, include four genera and a total of 20 species of gibbon, including the lar gibbon and the siamang, all native to Asia. They are highly arboreal and bipedal on the gro ...
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Nyanzapithecinae
The Nyanzapithecinae or Nyanzapithecines are a subfamily of extinct Dendropithecidae as sister of '' Simiolus''. The group contains ''Rangwapithecus'', '' Turkanapithecus'', '' Rukwapithecus'', ''Oreopithecus'', and ''Nyanzapithecus''. In the following tree the internal structure of Nyanzapithecinae of Nengo et al. is followed. Nyanzapithecinae Harrison, 2002 * ''Nyanzapithecus'' Harrison, 1986 ** ''Nyanzapithecus harrisoni'' Kunimatsu, 1997 ** ''Nyanzapithecus pickfordi'' Harrison, 1986 ** ''Nyanzapithecus vancouveringorum'' Andrews, 1974 * '' Mabokopithecus'' von Koenigswald, 1969 ** ''Mabokopithecus clarki'' von Koenigswald, 1969 * ''Rangwapithecus ''Rangwapithecus'' is an extinct genus of ape from the Early Miocene of Kenya. Late Miocene phalanges from Hungary have also been assigned to this genus, but were later reclassified as ''Dryopithecus''. Description ''Rangwapithecus'' weighed app ...'' Andrews, 1974 ** ''Rangwapithecus gordoni'' Andrews, 1974 * '' Turkanapithecus ...
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Catarrhine
The parvorder Catarrhini , catarrhine monkeys, Old World anthropoids, or Old World monkeys, consisting of the Cercopithecoidea and apes (Hominoidea). In 1812, Geoffroy grouped those two groups together and established the name Catarrhini, "Old World monkeys", ("''singes de l'Ancien Monde''" in French). Its sister in the infraorder Simiiformes is the parvorder Platyrrhini (New World monkeys). There has been some resistance to directly designate apes (and thus humans) as monkeys despite the scientific evidence, so "Old World monkey" may be taken to mean the Cercopithecoidea or the Catarrhini. That apes are monkeys was already realized by Georges-Louis Leclerc, Comte de Buffon in the 18th century. Linnaeus placed this group in 1758 together with what we now recognise as the tarsiers and the New World monkeys, in a single genus " S''imia''" (sans ''Homo''). The Catarrhini are all native to Africa and Asia. Members of this parvorder are called catarrhines. The Catarrhini are the si ...
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Catarrhini
The parvorder Catarrhini , catarrhine monkeys, Old World anthropoids, or Old World monkeys, consisting of the Cercopithecoidea and apes (Hominoidea). In 1812, Geoffroy grouped those two groups together and established the name Catarrhini, "Old World monkeys", ("''singes de l'Ancien Monde''" in French). Its sister in the infraorder Simiiformes is the parvorder Platyrrhini (New World monkeys). There has been some resistance to directly designate apes (and thus humans) as monkeys despite the scientific evidence, so "Old World monkey" may be taken to mean the Cercopithecoidea or the Catarrhini. That apes are monkeys was already realized by Georges-Louis Leclerc, Comte de Buffon in the 18th century. Linnaeus placed this group in 1758 together with what we now recognise as the tarsiers and the New World monkeys, in a single genus " S''imia''" (sans ''Homo''). The Catarrhini are all native to Africa and Asia. Members of this parvorder are called catarrhines. The Catarrhini are the si ...
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Dendropithecus
''Dendropithecus'' is an extinct genus of apes native to East Africa between 20 and 15 million years ago. ''Dendropithecus'' was originally suggested to be related to modern gibbons, based primarily on similarities in size, dentition, and skeletal adaptations. However, further studies have shown that ''Dendropithecus'' lacks derived hominoid traits. Instead, the traits shared between this taxon and modern primates are primitive for all catarrhines. ''Dendropithecus'' is now considered to be a stem catarrhine, too primitive to be closely related to any modern primates. ''Dendropithecus'' was a slender ape, about in body length. The structure of its arms suggest that it would have been able to brachiate Brachiation (from "brachium", Latin for "arm"), or arm swinging, is a form of arboreal locomotion in which primates swing from tree limb to tree limb using only their arms. During brachiation, the body is alternately supported under each forelimb. ..., swinging between trees b ...
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Prehistoric Apes
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ...
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Miocene Extinctions
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ...
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Pliocene Primates
The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58See the 2014 version of the ICS geologic time scale
million years ago. It is the second and most recent epoch of the Period in the . The Pliocene follows the Epoch and is followed by the

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Miocene Primates
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ...
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Nyanzapithecus Pickfordi
''Nyanzapithecus pickfordi'' is an extinct species of primate from the Middle Miocene of Maboko Island, Nyanza Province, Kenya. It had an average body mass of around . Taxonomy Fifteen cranio-dental specimens of this species were collected from the island between the years 1933-73. During an expedition to Maboko Island in 1982–83, paleoanthropologist Martin Pickford recovered more than a hundred small catarrhine fossils. Among them, described the new genus and species ''Nyanzapithecus pickfordi'', characterized by several dental specializations, and also transferred the '' Rangwapithecus'' species ''R. vancouveringi'' to the genus renaming it ''N. vancouveringorum''. ''Nyanzapithecus'' was considered closely related to ''Rangwapithecus'' and '' Mabokopithecus'' based on dental similarities, and an early relative of ''Oreopithecus bambolii''. ''Nyanzapithecus'' was originally included in Oreopithecidae before being transferred to Proconsulidae. described a new species, ...
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Rangwapithecus
''Rangwapithecus'' is an extinct genus of ape from the Early Miocene of Kenya. Late Miocene phalanges from Hungary have also been assigned to this genus, but were later reclassified as ''Dryopithecus''. Description ''Rangwapithecus'' weighed approximately and the size and shape of the ape's teeth indicate that it was a folivore. An arboreal ape from the earliest Miocene adapted to life in the rainforest, it is associated particularly with Mfangano Island although the species previously inhabited a woodland-bushland environment. Taxonomy ''Rangwapithecus'' was sympatric with ''Proconsul A proconsul was an official of ancient Rome who acted on behalf of a consul. A proconsul was typically a former consul. The term is also used in recent history for officials with delegated authority. In the Roman Republic, military command, or ...'', and may be synonymous with both ''Proconsul gordoni'' and ''Proconsul vancouveringi''. It is also similar to another species found in Africa. ...
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