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Prolibytherium
''Prolibytherium'' is an extinct genus of prolibytheriid artiodactyl ungulate native to Middle Miocene North Africa and Pakistan, from around 16.9 to 15.97 million years ago. Fossils of ''Prolibytherium'' were found in the Marada Formation of Libya, Vihowa Formation of Pakistan, and the Moghara Formation of Egypt. Description The long creature would have superficially resembled an okapi or a deer. Unlike these, however, ''Prolibytherium'' displayed dramatic sexual dimorphism, in that the male had a set of large, leaf-shaped ossicones with a width of , while the female had a set of slender, horn-like ossicones. The taxonomic status of ''Prolibytherium'' remains in flux. At one time, it was described as a relative of ''Sivatherium'' (as a precursor to "Libytherium maurusium" (''S. maurusium'')). Later, it would be regarded as a palaeomerycid, or either as a climacoceratid, or as a basal member of Giraffoidea Giraffoidea is a superfamily that includes the families Clim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climacoceratidae
Climacoceratidae is a family of superficially deer-like artiodactyl ungulates which lived in the Miocene epoch in Africa. They are close to the ancestry of giraffes, with some genera, such as ''Prolibytherium'', originally classified as giraffes. The climacoceratids, namely members of what is now the type genus ''Climacoceras'', were originally placed within the family Palaeomerycidae, and then within Giraffidae. In 1978, W. R. Hamilton erected a new family, placing it close to Giraffidae within the superfamily Giraffoidea. They differ from giraffes in that their antler-like ossicone Ossicones are columnar or conical skin-covered bone structures on the heads of giraffes, male okapi, and some of their extinct relatives. Ossicones are distinguished from the superficially similar structures of horns and antlers by their unique ...s are derived from different bones. References * MacInnes, D. G. 1936, "A new genus of fossil deer from the Miocene of Africa", Journal of the Linne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ossicone
Ossicones are columnar or conical skin-covered bone structures on the heads of giraffes, male okapi, and some of their extinct relatives. Ossicones are distinguished from the superficially similar structures of horns and antlers by their unique development and a permanent covering of skin and fur. Structure Giraffe ossicones consist of a highly vascularized and innervated bone core covered with vascularized and innervated skin. The base of an ossicone is attached to the skull with vascularized innervated connective tissue. Ossicones are formed at late gestation, but in early development they are not bony and not fused to the skull yet. Ossicones usually fuse to the skull at sexual maturity. All male and female giraffes have a pair of parietal ossicones on the parietal bones of the skull. Males also usually have a single median ossicone on the frontal bone that is larger in northern animals and smaller in southern giraffes. Giraffes can also have small additional paired occipi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giraffoidea
Giraffoidea is a superfamily that includes the families Climacoceratidae, Antilocapridae, and Giraffidae. The only extant members in the superfamily are the pronghorn, giraffe, and okapi. The Climacoceratidae are also placed in the superfamily, but were originally placed within the family Palaeomerycidae. Classification * Superfamily Giraffoidea ** Family † Climacoceratidae *** †'' Climacoceras'' *** †'' Orangemeryx'' *** †'' Prolibytherium'' *** †'' Propalaeoryx'' *** †'' Nyanzameryx'' *** †'' Sperrgebietomeryx'' ** Family Antilocapridae *** '' Antilocapra'' *** †'' Capromeryx'' *** †'' Ceratomeryx'' *** †'' Cosoryx'' *** †'' Hayoceros'' *** †'' Hexameryx'' *** †'' Hexobelomeryx'' *** †'' Ilingoceros'' *** †'' Meryceros'' *** †'' Merycodus'' *** †'' Osbornoceros'' *** †'' Ottoceros'' *** †'' Paracosoryx'' *** †'' Plioceros'' *** †'' Proantilocapra'' *** †'' Ramoceros'' *** †'' Sphenophalos'' *** †'' Stockoceros'' *** †'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sivatherium
''Sivatherium'' ("Shiva's beast", from Shiva and ''therium'', Latinized form of Ancient Greek θηρίον -'' thēríon'') is an extinct genus of giraffids that ranged throughout Africa to the Indian subcontinent. The species ''Sivatherium giganteum'' is, by weight, one of the largest giraffid known, and also one of the largest ruminants of all time. ''Sivatherium'' originated during the Late Miocene (around 7 million years ago) in Africa and survived through to the late Early Pleistocene ( Calabrian) ''S. giganteum'' remains have been recovered from the Himalayan foothills, dating around 1 million years ago. Suggestions have been made that ''S. maurusium'' may have gone extinct as recently as 8,000 years ago, as depictions that resemble it are known from ancient rock paintings in the Sahara and Central West India. But these claims are not substantiated by fossil evidence, and the depictions likely represent other animals. Description ''Sivatherium'' resembled the modern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burdigalian
The Burdigalian is, in the geologic timescale, an age or stage in the early Miocene. It spans the time between 20.43 ± 0.05 Ma and 15.97 ± 0.05 Ma (million years ago). Preceded by the Aquitanian, the Burdigalian was the first and longest warming period of the MioceneEdward Petuch, Ph.D. Florida Atlantic University, Department of Geosciences. and is succeeded by the Langhian. Stratigraphic definition The name Burdigalian comes from ''Burdigala'', the Latin name for the city of Bordeaux, France. The Burdigalian Stage was introduced in scientific literature by Charles Depéret in 1892. The base of the Burdigalian is at the first appearance of foram species ''Globigerinoides altiaperturus'' and the top of magnetic chronozone C6An. , an official GSSP for the Burdigalian had not yet been assigned. The top of the Burdigalian (the base of the Langhian) is defined by the first appearance of foram species ''Praeorbulina glomerosa'' and is also coeval with the top of magnetic chronozo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leaf
A leaf (plural, : leaves) is any of the principal appendages of a vascular plant plant stem, stem, usually borne laterally aboveground and specialized for photosynthesis. Leaves are collectively called foliage, as in "autumn foliage", while the leaves, stem, flower, and fruit collectively form the shoot system. In most leaves, the primary photosynthesis, photosynthetic tissue is the palisade mesophyll and is located on the upper side of the blade or lamina of the leaf but in some species, including the mature foliage of ''Eucalyptus'', palisade mesophyll is present on both sides and the leaves are said to be isobilateral. Most leaves are flattened and have distinct upper (Glossary of botanical terms#adaxial, adaxial) and lower (Glossary of botanical terms#abaxial, abaxial) surfaces that differ in color, hairiness, the number of stomata (pores that intake and output gases), the amount and structure of epicuticular wax and other features. Leaves are mostly green in color due ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossils Of Libya
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 abso ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossils Of Egypt
Egypt has many fossil-bearing geologic formations, in which many dinosaurs have been discovered. Scientists * Ernst Stromer * Richard Markgraf, early 1900s, (he died in Sinnuris of Giza in 1916) * A. B. Orlebar, Fayoum 1845 * George Schweinfurth, Geziret al-Qarn in Lake Qarun 1879 & Qasr al-Sagha Formation ancient whale fossils named Zeuglodom osiris. * Hugh Beadnell, Fayoum 1898 * Charles Andrews, 1901, they unearthed a wealth of fossils Palaeomastodon, the oldest known elephant * Eberhard Frass, Fayoum 1905 * Walter Granger & Henry F. Osborn, Fayoum 1907 * Wendell Phillips, 1947 * Elwyn L. Simons, Fayoum 1961–1986 * Thomas M. Bown and David Tab Rasmussen, 1980s Fossils Petrified Wood Fayoum, Petrified wood protectorate in New-Cairo Area/ Cairo-Suez desert road & entire Western Desert of Egypt is covered in Petrified wood. This is one of the clues that the region was a tropical climate. The petrified wood is very diverse and many samples are very beautiful, of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 late ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mammal Enigmatic Taxa
Mammals () are a group of vertebrate animals constituting the class Mammalia (), characterized by the presence of mammary glands which in females produce milk for feeding (nursing) their young, a neocortex (a region of the brain), fur or hair, and three middle ear bones. These characteristics distinguish them from reptiles (including birds) from which they diverged in the Carboniferous, over 300 million years ago. Around 6,400 extant species of mammals have been described divided into 29 orders. The largest orders, in terms of number of species, are the rodents, bats, and Eulipotyphla (hedgehogs, moles, shrews, and others). The next three are the Primates (including humans, apes, monkeys, and others), the Artiodactyla (cetaceans and even-toed ungulates), and the Carnivora (cats, dogs, seals, and others). In terms of cladistics, which reflects evolutionary history, mammals are the only living members of the Synapsida (synapsids); this clade, together with Sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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