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Schizotheriinae
Schizotheriines are one of the two subfamilies of the extinct family Chalicotheriidae, a group of herbivorous odd-toed ungulate (perissodactyl) mammals that lived from the Eocene to the Pleistoscene. The other clade is the Chalicotheriinae. Both clades had claws rather than hooves on their front feet, an adaptation understood as related to feeding. Schizotheriines also had claws on their hind feet. The fossils of both groups are found in environments that had trees and shrubs. While chalicotheriines developed very derived body forms, schizotheriines remained basically similar in shape to other perissodactyls such as horses and tapirs. Like most forest-dwelling ungulates, they had long necks and forelimbs longer than their hindlimbs. Schizotheriines had longer, higher-crowned cheek teeth than chalicotheriines, which indicates they typically fed on tougher vegetation. The sediments where their fossils are found show they also lived in a wider range of environments, from moist forest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalicotheres
Chalicotheres (from Greek language, Greek ''wikt:χάλιξ, chalix'', "gravel" and ''wikt:θηρίον, therion'', "beast") are an extinct clade of herbivorous, odd-toed ungulate (perissodactyl) mammals that lived in North America, Eurasia, and Africa from the Eocene, Middle Eocene until the Early Pleistocene, existing from 48.6 to 1.806 Annum, mya. They are one of the five major Evolutionary radiation, radiations of perissodactyls, with three groups living (Equidae, horses, plus the extinct Palaeotheriidae, paleotheres; Rhinoceros, rhinoceroses; Tapiroidea, tapirs), and two extinct (Brontotheriidae, brontotheres and chalicotheres). Description Unlike modern perissodactyls, chalicotheres had clawed feet. They had longer forelimbs and shorter hind limbs, lower incisors that cropped food against a toothless pad in the upper jaw, low-crowned molar teeth, and were browsers on trees and shrubs throughout their history. They evolved in two different directions, which became separate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalicotheriidae
Chalicotheres (from Greek '' chalix'', "gravel" and '' therion'', "beast") are an extinct clade of herbivorous, odd-toed ungulate (perissodactyl) mammals that lived in North America, Eurasia, and Africa from the Middle Eocene until the Early Pleistocene, existing from 48.6 to 1.806 mya. They are one of the five major radiations of perissodactyls, with three groups living ( horses, plus the extinct paleotheres; rhinoceroses; tapirs), and two extinct (brontotheres and chalicotheres). Description Unlike modern perissodactyls, chalicotheres had clawed feet. They had longer forelimbs and shorter hind limbs, lower incisors that cropped food against a toothless pad in the upper jaw, low-crowned molar teeth, and were browsers on trees and shrubs throughout their history. They evolved in two different directions, which became separate subfamilies, the Schizotheriinae and the Chalicotheriinae. Schizotherine chalicotheres such as ''Moropus'' lived in a variety of forest, woodland, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalicotheriinae
Chalicotheriines are one of the two subfamilies of the extinct family Chalicotheriidae, a group of herbivorous, odd-toed ungulate ''(perissodactyl)'' mammals that lived from the Eocene to the Pleistocene. The other subfamily is the Schizotheriinae. Chalcotheriines evolved unique characteristics for ungulates, with very long forelimbs, short hindlimbs, and a relatively gorilla-like physique, including knuckle-walking on their flexible forelimbs, which bore long curved claws. Members of this subfamily possessed some of the longest forelimbs and shortest hindlimbs in relation to each other out of all extinct animals. Analysis of dental wear implies that most chalicotheriines fed on seeds and fruit. Their claws were likely used in a hook-like manner to pull down branches, suggesting they lived as bipedal browsers. Presence of chalicothere fossils is generally regarded as an indicator of forested environments. Unlike schizotheriines, chalicotheriines were typically confined to moist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moropus
''Moropus'' (meaning "slow foot") is an extinct genus of large perissodactyl ("odd-toed" ungulate) mammal in the chalicothere family. They were endemic to North America during the Miocene from ~20.4—13.6 Mya, existing for approximately . ''Moropus'' belonged to the schizotheriine subfamily of chalicotheres, and has the best fossil record of any member of this group; numbers of individuals, including complete skeletons, have been found. The closest extant relatives of ''Moropus'' are other perissodactyls: Equus (genus), horses, Rhinoceros, rhinos, and tapirs. Description Like other chalicothere Chalicotheres (from Greek '' chalix'', "gravel" and '' therion'', "beast") are an extinct clade of herbivorous, odd-toed ungulate (perissodactyl) mammals that lived in North America, Eurasia, and Africa from the Middle Eocene until the Early Plei ...s, ''Moropus'' differed from typical ungulates in having large claws, rather than hooves, on the feet. Three large, highly compress ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancylotherium
''Ancylotherium'' (from Greek, meaning "hooked beast") is an extinct genus of the family Chalicotheriidae, subfamily Schizotheriinae, endemic to Europe, Asia, and Africa during the Late Miocene-Early Pleistocene (9.0—1.8 mya), existing for approximately . Taxonomy ''Ancylotherium'' was named by Gaudry (1863) and was assigned to Chalicotheriidae by Carroll (1988); and to Schizotheriinae by Geraads et al. (2007). Description With some individuals reaching high at the shoulder and a weight of , ''Ancylotherium'' was relatively large, and was built rather like a goat. Individuals varied considerably in size, and the genus may have been sexually dimorphic, like many other chalicotheres. While it had the typical long forelimbs and short hind limbs of a chalicothere, like other schizotheriines, it did not walk on its knuckles. It was similar to the North American genus ''Moropus''. In at least some individuals of ''A. pentelicum'' the frontal bone of the skull is inflated to form a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borissiakia
''Borissiakia'' is an extinct genus of chalicothere, a group of herbivorous, odd-toed ungulate (perissodactyl) mammals, that lived during the late Oligocene in Kazakhstan. They had claws that were likely used in a hook-like manner to pull down branches, suggesting they lived as bipedal browsers Browse, browser or browsing may refer to: Programs *Web browser, a program used to access the World Wide Web *Code browser, a program for navigating source code *File browser or file manager, a program used to manage files and related objects *Ha .... References Sources * Classification of Mammals by Malcolm C. McKenna and Susan K. Bell Chalicotheres Oligocene mammals of Asia Fossil taxa described in 1946 {{paleo-oddtoedungulate-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chemositia
''Chemositia'' is an extinct genus of chalicothere, a group of herbivorous, odd-toed ungulate ''(perissodactyl)'' mammals. They lived in Africa, and had claws that were likely used in a hook-like manner to pull down branches, suggesting they lived as bipedal browsers. Many authorities do not believe that ''Chemositia'' is a valid genus and synonymize it with ''Ancylotherium ''Ancylotherium'' (from Greek, meaning "hooked beast") is an extinct genus of the family Chalicotheriidae, subfamily Schizotheriinae, endemic to Europe, Asia, and Africa during the Late Miocene-Early Pleistocene (9.0—1.8 mya), existing for app ...'' or '' Metaschizotherium''. References Sources * Classification of Mammals by Malcolm C. McKenna and Susan K. Bell Chalicotheres Miocene mammals of Africa Miocene odd-toed ungulates Fossil taxa described in 1979 {{paleo-oddtoedungulate-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metaschizotherium
''Metaschizotherium'' is an extinct genus that belongs to the family Chalicotheriidae, which was a group of herbivorous perissodactyl ("odd-toed") mammals. Though found primarily in Europe, fragmentary remains suggest that their range extended into Asia. Several other species have been described under ''Metaschizotherium'' in the past, including the African ''M. transvaalensis'', but they have been transferred to other genera, such as ''Ancylotherium''. The entire genus has been considered synonymous with ''Ancylotherium'' in the past, but nowadays the two are generally found to be distinct. This genus is typically associated with areas of closed, moist forest, where it fed on relatively soft leaves and shoots compared to a more abrasive diet of twigs and bark. See also *''Moropus'' *''Ancylotherium ''Ancylotherium'' (from Greek, meaning "hooked beast") is an extinct genus of the family Chalicotheriidae, subfamily Schizotheriinae, endemic to Europe, Asia, and Africa during th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Odd-toed Ungulate
Odd-toed ungulates, mammals which constitute the taxonomic order Perissodactyla (, ), are animals—ungulates—who have reduced the weight-bearing toes to three (rhinoceroses and tapirs, with tapirs still using four toes on the front legs) or one (equines, third toe) of the five original toes. The non-weight-bearing toes are either present, absent, vestigial, or positioned posteriorly. By contrast, the even-toed ungulates bear most of their weight equally on four or two (an even number) of the five toes: their third and fourth toes. Another difference between the two is that odd-toed ungulates digest plant cellulose in their intestines rather than in one or more stomach chambers as even-toed ungulates, with the exception of Suina, do. The order includes about 17 species divided into three families: Equidae (horses, asses, and zebras), Rhinocerotidae (rhinoceroses), and Tapiridae (tapirs). Despite their very different appearances, they were recognized as related families in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene First Appearances
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene Extinctions
The Quaternary period (from 2.588 ± 0.005 million years ago to the present) has seen the extinctions of numerous predominantly megafaunal species, which have resulted in a collapse in faunal density and diversity and the extinction of key ecological strata across the globe. The most prominent event in the Late Pleistocene is differentiated from previous Quaternary pulse extinctions by the widespread absence of ecological succession to replace these extinct species, and the regime shift of previously established faunal relationships and habitats as a consequence. The earliest casualties were incurred at 130,000 BCE (the start of the Late Pleistocene), in Australia ~ 60,000 years ago, in Americas ~ 15,000 years ago, coinciding in time with the early human migrations. However, the great majority of extinctions in Afro-Eurasia and the Americas occurred during the transition from the Pleistocene to the Holocene epoch (13,000 BCE to 8,000 BCE). This extinction wave di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
