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Kubanochoerus
''Kubanochoerus'' is an extinct genus of large, long-legged suid artiodactyl mammal from the Miocene of Eurasia and Africa. Taxonomy The genera ''Libycochoerus'' and ''Megalochoerus ''Megalochoerus'' is an extinct genus of large and long-legged pig-like animals from the Miocene of Africa. Taxonomy The species ''M. khinzikebirus'' and ''M. marymuunguae'' were once considered to belong to the related ''Kubanochoerus ''Kub ...'' were once assigned to ''Kubanochoerus'' but are now considered distinct based on dental and minor cranial details. The putative paraceratheriid genus ''Caucasotherium'', described from the Caucasus on the basis of a bone fragment with four incisors, is actually a synonym of the Middle Miocene ''Kubanochoerus gigas''. Description The largest species, the aptly named ''K. gigas'', grew to be around at the shoulder, and probably weighed up to in life.
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Kubanochoerus Robustus A6 Digital
''Kubanochoerus'' is an extinct genus of large, long-legged suid artiodactyl mammal from the Miocene of Eurasia and Africa. Taxonomy The genera ''Libycochoerus'' and ''Megalochoerus ''Megalochoerus'' is an extinct genus of large and long-legged pig-like animals from the Miocene of Africa. Taxonomy The species ''M. khinzikebirus'' and ''M. marymuunguae'' were once considered to belong to the related ''Kubanochoerus ''Kub ...'' were once assigned to ''Kubanochoerus'' but are now considered distinct based on dental and minor cranial details. The putative paraceratheriid genus ''Caucasotherium'', described from the Caucasus on the basis of a bone fragment with four incisors, is actually a synonym of the Middle Miocene ''Kubanochoerus gigas''. Description The largest species, the aptly named ''K. gigas'', grew to be around at the shoulder, and probably weighed up to in life.
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Kubanochoerus Gigas
''Kubanochoerus'' is an extinct genus of large, long-legged suid artiodactyl mammal from the Miocene of Eurasia and Africa. Taxonomy The genera ''Libycochoerus'' and ''Megalochoerus ''Megalochoerus'' is an extinct genus of large and long-legged pig-like animals from the Miocene of Africa. Taxonomy The species ''M. khinzikebirus'' and ''M. marymuunguae'' were once considered to belong to the related ''Kubanochoerus ''Kub ...'' were once assigned to ''Kubanochoerus'' but are now considered distinct based on dental and minor cranial details. The putative paraceratheriid genus ''Caucasotherium'', described from the Caucasus on the basis of a bone fragment with four incisors, is actually a synonym of the Middle Miocene ''Kubanochoerus gigas''. Description The largest species, the aptly named ''K. gigas'', grew to be around at the shoulder, and probably weighed up to in life.
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Kubanochoerus Gigas NMNS
''Kubanochoerus'' is an extinct genus of large, long-legged suid artiodactyl mammal from the Miocene of Eurasia and Africa. Taxonomy The genera ''Libycochoerus'' and ''Megalochoerus ''Megalochoerus'' is an extinct genus of large and long-legged pig-like animals from the Miocene of Africa. Taxonomy The species ''M. khinzikebirus'' and ''M. marymuunguae'' were once considered to belong to the related ''Kubanochoerus ''Kub ...'' were once assigned to ''Kubanochoerus'' but are now considered distinct based on dental and minor cranial details. The putative paraceratheriid genus ''Caucasotherium'', described from the Caucasus on the basis of a bone fragment with four incisors, is actually a synonym of the Middle Miocene ''Kubanochoerus gigas''. Description The largest species, the aptly named ''K. gigas'', grew to be around at the shoulder, and probably weighed up to in life.
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Megalochoerus
''Megalochoerus'' is an extinct genus of large and long-legged pig-like animals from the Miocene of Africa. Taxonomy The species ''M. khinzikebirus'' and ''M. marymuunguae'' were once considered to belong to the related ''Kubanochoerus'' or ''Libycochoerus'', but have since been reassigned to ''Megalochoerus''. ''Megalochoerus marymuuguae'' was the smallest and earliest of the three species, while ''M. humungous'' was the latest occurring and largest. Description ''Megalochoerus'' contained some of the largest suids ever known to exist. Weight estimates of ''M. khinzikebirus'', intermediate in size between the other two species, have been as high as based on dental morphology, easily larger than other giant fossil pigs such as ''Kubanochoerus'' and '' Notochoerus''. Other calculations based on molar and humerus measurements have yielded lower estimates for ''M. khinzikebirus''; based on measurements of the lower molar (m/1), and based on articulation of the distal humerus ...
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Suidae
Suidae is a family of artiodactyl mammals which are commonly called pigs, hogs or swine. In addition to numerous fossil species, 18 extant species are currently recognized (or 19 counting domestic pigs and wild boars separately), classified into between four and eight genera. Within this family, the genus ''Sus'' includes the domestic pig, ''Sus scrofa domesticus'' or ''Sus domesticus'', and many species of wild pig from Europe to the Pacific. Other genera include babirusas and warthogs. All suids, or swine, are native to the Old World, ranging from Asia to Europe and Africa. The earliest fossil suids date from the Oligocene epoch in Asia, and their descendants reached Europe during the Miocene. Several fossil species are known and show adaptations to a wide range of different diets, from strict herbivory to possible carrion-eating (in Tetraconodontinae). Physical characteristics Suids belong to the order Artiodactyla, and are generally regarded as the living members of that or ...
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Libycochoerus
''Libycochoerus'' is an extinct genus of large and long-legged animals in the pig family from the Miocene of Africa. Taxonomy ''Libycochoerus'' was at one point sunk as a junior synonym of ''Kubanochoerus ''Kubanochoerus'' is an extinct genus of large, long-legged suid artiodactyl mammal from the Miocene of Eurasia and Africa. Taxonomy The genera ''Libycochoerus'' and ''Megalochoerus ''Megalochoerus'' is an extinct genus of large and long-l ...'' but is now considered a distinct genus. All species of this species have very robust teeth that are mesiodistally long, but also stout canines and simple molars.Bishop LC (2010) Suoidea. In: Werdelin L, Sanders WJ, editors. Cenozoic Mammals of Africa. Berkeley: University of California Press. pp. 821–842. References * Prehistoric Suidae Miocene mammals of Africa Miocene even-toed ungulates Fossil taxa described in 1961 Prehistoric even-toed ungulate genera {{paleo-eventoedungulate-stub ...
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Fossils Of Russia
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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Miocene Mammals Of Europe
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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Fossils Of China
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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Miocene Mammals Of Asia
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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Fossils Of Kenya
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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Miocene Mammals Of Africa
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 ...
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