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Megistotherium
''Megistotherium'' ("greatest beast") is an extinct genus of hyainailourid hyaenodonts from paraphyletic subfamily Hyainailourinae that lived in Africa. Etymology The name of this genus comes and . The name of species ''Megistotherium osteothlastes'' comes and (with ''-es'' being an agent noun: 'bone-crusher'). Description ''Megistotherium osteothlastes'' is the only known species from this genus, and it was a large hyainailourid that lived during the early Miocene. Its remains have been found in the Ngorora and Muruyur Formations of Kenya, Egypt,Morlo, M., Miller, E.R., and El-Barkooky, A.N. 2007. Creodonta and Carnivora from Wadi Moghra, Egypt. Journal of Vertebrate Paleontology 27: 145–159. Namibia, UgandaMorales, J. and M. Pickford. (2008). "Creodonts and carnivores from the Middle Miocene Muruyur Formation at Kipsaraman and Cheparawa, Baringo District, Kenya." ''Comptes Rendus Palevol'' 7 (8): 487-497 and Libya. Named by Robert Savage in 1973, ''Megistotherium'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hyainailouridae
Hyainailouridae ("hyena-cats") is a paraphyletic family of extinct predatory mammals from extinct paraphyletic superfamily Hyainailouroidea within extinct order Hyaenodonta. Hyaenodontids arose during the middle Eocene and persisted well into the middle Miocene. Fossils of this group have been found in Asia, Africa, North America and Europe. General characteristics Hyainailourids are characterized by long skulls, slender jaws, slim bodies, and a plantigrade stance. They generally ranged in size from 30 to 140 cm at the shoulder. While some measured as much as 1.4 m high at the shoulder with head-body length up to 3.2 m and weighed up to 1,500 kg, most were in the 5–15 kg range, equivalent to a mid-sized dog. The anatomy of their skulls show that they had a particularly acute sense of smell, while their teeth were adapted for shearing, rather than crushing. At least one hyainailourid lineage, Apterodontinae, was specialised for aquatic, otter-like habits. Rang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hyainailourinae
Hyainailourinae ("hyena-cats") is an extinct paraphyletic subfamily of hyainailourid hyaenodonts that lived in Africa, Asia, North America and Europe during the middle Eocene to middle Miocene. Classification and phylogeny Taxonomy * Subfamily: †Hyainailourinae (paraphyletic subfamily) ** Genus: †'' Megistotherium'' *** †''Megistotherium osteothlastes'' ** Genus: †'' Mlanyama'' *** †''Mlanyama sugu'' ** Genus: †''Orienspterodon'' *** †''Orienspterodon dahkoensis'' ** Genus: †'' Pakakali'' *** †''Pakakali rukwaensis'' ** Genus: †'' Simbakubwa'' *** †''Simbakubwa kutokaafrika'' ** (unranked): †''Akhnatenavus'' clade *** Genus: †'' Akhnatenavus'' **** †''Akhnatenavus leptognathus'' **** †''Akhnatenavus nefertiticyon'' *** Genus: †'' Hemipsalodon'' **** †''Hemipsalodon grandis'' **** †''Hemipsalodon viejaensis'' *** Genus: †'' Ischnognathus'' **** †''Ischnognathus savagei'' ** Tribe: † Hyainailourini (polyphyletic tribe) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dissopsalis
''Dissopsalis'' ("double scissors") is a genus of teratodontine hyaenodonts of the tribe Dissopsalini. The older species, ''D. pyroclasticus'', lived in Kenya during the middle Miocene, while the type species, ''D. carnifex'', lived in Pakistan and India during the middle to late Miocene.Barry, J. C. (1988.) "''Dissopsalis'', a middle and late Miocene proviverrine creodont (Mammalia) from Pakistan and Kenya." ''Journal of Vertebrate Paleontology'' 48(1): 25–45 ''Dissopsalis'' is the last known hyaenodont genus. It lived alongside its relative ''Hyaenodon weilini'', a member of the very successful genus ''Hyaenodon ''Hyaenodon'' ("hyena-tooth") is an extinct genus of carnivorous hyaenodont mammals from tribe Hyaenodontini, within subfamily Hyaenodontinae in family Hyaenodontidae,Malcolm C. McKenna, Susan K. Bell (1997."Classification of Mammals: Above t ...'', during the Miocene in China. ''Dissopsalis'' survived to the end of the Miocene, whereas ''H. weilini'' did ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngorora Formation
The Ngorora Formation is a geological formation in Kenya preserving fossils dating to the Miocene. The uppermost member of the formation shows sign of a faunal turnover that occurred around 11 to 10.5 million years ago, coinciding with faunal changes elsewhere in the world. This turnover includes the arrival of the horse ''Hipparion'' in East Africa. The Ngorora Formation was initially mapped by G.R. Chapman in collaboration with the East African Geological Research Unit (EAGRU) and formally described by Bishop & Chapman in 1970. Major fossil finds were made in the early 1970s, with expeditions to the area recovering thousands of mammal, fish and mollusc remains alongside less common fossil material of birds and reptiles. Geography The formation is bordered to the west by the Elgeyo Escarpment, the east by the Laikipia Plateau and to the north by the Tiati volcanic center. To the south the formation is limited by the rising floor of the rift. During its deposition the formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hyaenodonta
Hyaenodonta ("hyena teeth") is an extinct order of hypercarnivorous placental pan-carnivoran mammals from mirorder Ferae. Hyaenodonts were important mammalian predators that arose during the early Paleocene in Europe and persisted well into the late Miocene. Characteristics Hyaenodonts are characterized by long skulls, slender jaws, slim bodies and a plantigrade stance. They generally ranged in size from 30 to 140 cm at the shoulder. While '' Simbakubwa kutokaafrika'' may have been up to (surpassing the modern polar bear in size) and ''Hyaenodon gigas'' (the largest species from genus '' Hyaenodon'') was as much as 1.4 m high at the shoulder, 3.0 m long and weighed about 330 kg, most of hyaenodonts were in the 5–15 kg range, equivalent to a mid-sized dog. The anatomy of their skulls show that they had a particularly acute sense of smell, while their teeth were adapted for shearing, rather than crushing. Because of their size range, it is probable tha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hyainailouros
''Hyainailouros'' ("hyena-cat") is an extinct polyphyletic genus of hyainailourid hyaenodont mammal of the polyphyletic tribe Hyainailourini within paraphyletic subfamily Hyainailourinae, that lived during the early to middle Miocene, of which there were at least three species spread across Europe, Africa, and Asia. Closely related to other large African hyaenodonts such as '' Simbakubwa'' and ''Megistotherium'', ''Hyainailouros'' walked with a semi-digitigrade stance and was probably capable of large, leaping bounds. Alongside its African relatives and the last members of the genus ''Hyaenodon ''Hyaenodon'' ("hyena-tooth") is an extinct genus of carnivorous hyaenodont mammals from tribe Hyaenodontini, within subfamily Hyaenodontinae in family Hyaenodontidae,Malcolm C. McKenna, Susan K. Bell (1997."Classification of Mammals: Above t ...'' from Asia, ''Hyainailouros'' was among the largest hyaenodonts that existed. Phylogeny The phylogenetic relationships of genus ''H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robert Savage (palaeontologist)
Robert Joseph Gay Savage (2 July 1927 – 9 May 1998) was a British palaeontologist known as Britain's leading expert on fossil mammals. He worked at the University of Bristol for nearly 40 years and studied fossils around the world, especially in North and East Africa. He produced the 1986 popular science book ''Mammal Evolution: An Illustrated Guide'' and co-edited several technical books in the ''Fossil Vertebrates of Africa'' series with fellow palaeontologist Louis Leakey. Early life Savage was born in Belfast, Northern Ireland on 2 July 1927 to an old family prominent in Ulster. He recalled a large rack of antlers of the extinct Irish elk mounted in the entrance hall of the family home, which colleague Michael Benton writes may have inspired Savage to pursue the study of fossil mammals. He attended grammar school at Methodist College, Belfast and Wesley College, Dublin before and during the period of World War II. He enrolled in Queen's University Belfast, earning a BSc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Junior Synonym
The Botanical and Zoological Codes of nomenclature treat the concept of synonymy differently. * In botanical nomenclature, a synonym is a scientific name that applies to a taxon that (now) goes by a different scientific name. For example, Linnaeus was the first to give a scientific name (under the currently used system of scientific nomenclature) to the Norway spruce, which he called ''Pinus abies''. This name is no longer in use, so it is now a synonym of the current scientific name, '' Picea abies''. * In zoology, moving a species from one genus to another results in a different binomen, but the name is considered an alternative combination rather than a synonym. The concept of synonymy in zoology is reserved for two names at the same rank that refers to a taxon at that rank - for example, the name ''Papilio prorsa'' Linnaeus, 1758 is a junior synonym of ''Papilio levana'' Linnaeus, 1758, being names for different seasonal forms of the species now referred to as ''Araschnia le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene 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" ... Epoch. The Oligocene is the third and final epoch of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carnassial
Carnassials are paired upper and lower teeth modified in such a way as to allow enlarged and often self-sharpening edges to pass by each other in a shearing manner. This adaptation is found in carnivorans, where the carnassials are the modified fourth upper premolar and the first lower molar, however this may vary in family. These teeth are also referred to as sectorial teeth. Taxonomy The name carnivoran is applied to a member of the order Carnivora. Carnivorans possess a common arrangement of teeth called carnassials, in which the first lower molar and the last upper premolar possess blade-like enamel crowns that act similar to a pair of shears for cutting meat. This dental arrangement has been modified by adaptation over the past 60 million years for diets composed of meat, for crushing vegetation, or for the loss of the carnassial function altogether as in seals, sea lions, and walruses. Carnassial dentition Carnassial teeth are modified molars (and in the case of carni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carnivora
Carnivora is a monophyletic order of placental mammals consisting of the most recent common ancestor of all cat-like and dog-like animals, and all descendants of that ancestor. Members of this group are formally referred to as carnivorans, and have evolved to specialize in eating flesh. The order is the fifth largest order of mammals, comprising at least 279 species. Carnivorans live on every major landmass and in a variety of habitats, ranging from the cold polar regions to the hyper-arid region of the Sahara Desert to the open seas. They come in a very large array of different body plans in contrasting shapes and sizes. Carnivora can be divided into two subclades: the cat-like Feliformia and the dog-like Caniformia, which are differentiated based on the structure of their ear bones and cranial features. The feliforms include families such as the cats, the hyenas, the mongooses and the civets. The majority of feliform species are found in the Old World, though the cat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic 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 13C in the atmosphere was exceptionally low in comparison with the more common isotope 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 Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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