Megaceroides
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Megaceroides
''Megaceroides algericus'' is an extinct species of deer known from the Late Pleistocene to the Holocene of North Africa. It is one of only two species of deer known to have been native to the African continent, alongside the Barbary stag, a subspecies of red deer. It is considered to be closely related to the giant deer species of Eurasia. Taxonomy The species was first described by Richard Lydekker as ''Cervus algericus'' in 1890 from a maxilla with teeth found near Hammam Maskhoutine in Algeria. The species ''Cervus pachygenys'' was erected for a pachyostotic mandible and an isolated molar found in Algeria by Auguste Pomel in 1892. Léonce Joleaud in two publications in 1914 and 1916 synonymised the two species, and suggested affinities with the giant deer of Europe, and placed it in the newly erected subgenus ''Megaceroides'' within the genus ''Megaceros'' (junior synonym of ''Megaloceros'') as the type species. Camille Arambourg in publications in 1932 and 1938 raised '' ...
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Megaloceros
''Megaloceros'' (from Greek: + , literally "Great Horn"; see also Lister (1987)) is an extinct genus of deer whose members lived throughout Eurasia from the early Pleistocene to the beginning of the Holocene and were important herbivores during the Ice Ages. The largest species, ''Megaloceros giganteus'', vernacularly known as the "Irish elk" or "giant elk", is also the best known. Fallow deer are thought to be their closest living relatives. ''Megaloceros'' is part of the deer family which includes moose, elk, reindeer, and other cervids. Biology Most members of the genus were extremely large animals that favoured meadows or open woodlands. They are the most cursorial deer known, with most species averaging slightly below at the withers. The various species of the Cretan genus ''Candiacervus'' – the smallest of which, ''C. rhopalophorus'' was just high at the shoulder – are sometimes included in ''Megaloceros'' as a subgenus. Despite its name, the Irish elk was neith ...
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Barbary Stag
The Barbary stag (''Cervus elaphus barbarus''), also known as the Atlas deer or African elk, is a subspecies of the red deer that is native to North Africa. It is the only deer known to be native to Africa, aside from '' Megaceroides algericus'', which went extinct approximately 6,000 years ago. Description The Barbary stag is smaller than the typical red deer. Its body is dark brown with some white spots on its flanks and back. The antlers lack the bez (second) tine. Range/habitat The Barbary stag is the only member of the deer family that is native to Africa. It thrives in dense, humid forested areas of Algeria, Tunisia and Morocco. It had initially been hunted to extinction in the latter, but specimens from the Tunisian population were reintroduced in the 1990s.Le programme d'espèces d'UICN et la Commission UICN de la sauvegarde des espèces et TRAFFIC"Résumés des Analyses UICN/TRAFFIC des propositions d'amendement aux Annexes de la CITES pour la Quatorzième session de ...
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Irish Elk
The Irish elk (''Megaloceros giganteus''), also called the giant deer or Irish deer, is an extinct species of deer in the genus ''Megaloceros'' and is one of the largest deer that ever lived. Its range extended across Eurasia during the Pleistocene, from Ireland to Lake Baikal in Siberia. The most recent remains of the species have been carbon dated to about 7,700 years ago in western Russia. /nowiki>International_Code_of_Zoological_Nomenclature.html" ;"title="International Code of Zoological Nomenclature">/nowiki>International Code of Zoological Nomenclature">International Code of Zoological Nomenclature">/nowiki>International Code of Zoological Nomenclature/nowiki> (article 12) to validate ''Megalocerus''." The original spelling of ''Megalocerus'' was never used after its original publication.In 1844 Richard Owen named another synonym of the Irish elk, including it within the newly named subgenus ''Megaceros'', ''Cervus'' (''Megaceros'') ''hibernicus''. This has been suggested ...
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Megaloceros Giganteus Irish Elk Skeleton (Pleistocene; Peat Bog Near Dublin, Eastern Ireland) 3 (15257223660)
''Megaloceros'' (from Greek: + , literally "Great Horn"; see also Lister (1987)) is an extinct genus of deer whose members lived throughout Eurasia from the early Pleistocene to the beginning of the Holocene and were important herbivores during the Ice Ages. The largest species, ''Megaloceros giganteus'', vernacularly known as the "Irish elk" or "giant elk", is also the best known. Fallow deer are thought to be their closest living relatives. ''Megaloceros'' is part of the deer family which includes moose, elk, reindeer, and other cervids. Biology Most members of the genus were extremely large animals that favoured meadows or open woodlands. They are the most cursorial deer known, with most species averaging slightly below at the withers. The various species of the Cretan genus ''Candiacervus'' – the smallest of which, ''C. rhopalophorus'' was just high at the shoulder – are sometimes included in ''Megaloceros'' as a subgenus. Despite its name, the Irish elk was neith ...
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Praemegaceros
''Praemegaceros'' is an extinct genus of deer, known from the Pleistocene and Holocene of Western Eurasia. It contains the subgenera ''Praemegaceros,'' ''Orthogonoceros'' and ''Nesoleipoceros''. It has sometimes been synonymised with ''Megaloceros'' and ''Megaceroides'', however they have been found to be generically distinct. ''P. obscurus'' is the earliest known species from the Early Pleistocene of Europe, and had long, crooked antlers. ''P. verticornis'' is an Early to Mid-Pleistocene species, closely related to ''P. obscurus'', which lived throughout Southern Europe. The genus was widely distributed across Europe, West and Central Asia during the Early-Middle Pleistocene, with fossils having been discovered in France, Georgia, Germany, England, Greece, Israel, Italy, Romania, Russia Spain, Syria, and Tajikistan. The genus was extinct in mainland Europe and Asia by end of the Middle Pleistocene. An insular species, ''P. cazioti'' survived into the Late Pleistocene and Holocen ...
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Late Pleistocene
The Late Pleistocene is an unofficial Age (geology), age in the international geologic timescale in chronostratigraphy, also known as Upper Pleistocene from a Stratigraphy, stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently defined as the time between c. 129,000 and c. 11,700 years ago. The Late Pleistocene equates to the proposed Tarantian Age of the geologic time scale, preceded by the officially ratified Chibanian (formerly known as Middle Pleistocene) and succeeded by the officially ratified Greenlandian. The estimated beginning of the Tarantian is the start of the Eemian interglacial period (Marine Isotope Stage 5). It is held to end with the termination of the Younger Dryas, some 10th millennium BC, 11,700 years ago when the Holocene Epoch began. The term Upper Pleistocene is currently in use as a provisional or "quasi-formal" designation by the International Union of Geological ...
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Before Present
Before Present (BP) years, or "years before present", is a time scale used mainly in archaeology, geology and other scientific disciplines to specify when events occurred relative to the origin of practical radiocarbon dating in the 1950s. Because the "present" time changes, standard practice is to use 1 January 1950 as the commencement date (epoch) of the age scale. The abbreviation "BP" has been interpreted retrospectively as "Before Physics", which refers to the time before nuclear weapons testing artificially altered the proportion of the carbon isotopes in the atmosphere, which scientists must now account for. In a convention that is not always observed, many sources restrict the use of BP dates to those produced with radiocarbon dating; the alternative notation RCYBP stands for the explicit "radio carbon years before present". Usage The BP scale is sometimes used for dates established by means other than radiocarbon dating, such as stratigraphy. This usage differs from t ...
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Fallow Deer
''Dama'' is a genus of deer in the subfamily Cervinae, commonly referred to as fallow deer. Name The name fallow is derived from the deer's pale brown colour. The Latin word ''dāma'' or ''damma'', used for roe deer, gazelles, and antelopes, lies at the root of the modern scientific name, as well as the German ''Damhirsch'', French ''daim'', Dutch ''damhert'', and Italian ''daino''. In Croatian and Serbian, the name for the fallow deer is ''jelen lopatar'' ("shovel deer"), due to the form of its antlers. The Modern Hebrew name of the fallow deer is ''yachmur'' (יחמור). Taxonomy and evolution The genus includes two extant species: Extant species Some taxonomists include the Persian fallow deer as a subspecies In biological classification, subspecies is a rank below species, used for populations that live in different areas and vary in size, shape, or other physical characteristics (morphology), but that can successfully interbreed. Not all species ... (''D. d. me ...
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Aïn Bénian, Algiers
Aïn Benian ( ar, عين البنيان) is a commune in Algiers Province and suburb of the city of Algiers in northern Algeria ) , image_map = Algeria (centered orthographic projection).svg , map_caption = , image_map2 = , capital = Algiers , coordinates = , largest_city = capital , relig .... As of the 2008 census, the commune had a population of 68,354. El-Benian, is a coastal town Ain Benian, Algeria
situated in the region Algiers, Algeria.


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Parietal Bone
The parietal bones () are two bones in the Human skull, skull which, when joined at a fibrous joint, form the sides and roof of the Human skull, cranium. In humans, each bone is roughly quadrilateral in form, and has two surfaces, four borders, and four angles. It is named from the Latin ''paries'' (''-ietis''), wall. Surfaces External The external surface [Fig. 1] is convex, smooth, and marked near the center by an eminence, the parietal eminence (''tuber parietale''), which indicates the point where ossification commenced. Crossing the middle of the bone in an arched direction are two curved lines, the superior and inferior temporal lines; the former gives attachment to the temporal fascia, and the latter indicates the upper limit of the muscular origin of the temporal muscle. Above these lines the bone is covered by a tough layer of fibrous tissue – the epicranial aponeurosis; below them it forms part of the temporal fossa, and affords attachment to the temporal muscle. ...
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Splanchnocranium
The splanchnocranium (or visceral skeleton) is the portion of the cranium that is derived from pharyngeal arches. ''Splanchno'' indicates to the gut because the face forms around the mouth, which is an end of the gut. The splanchnocranium consists of cartilage and endochondral bone. In mammals, the splanchnocranium comprises the three ear ossicles (i.e., incus, malleus, and stapes), as well as the alisphenoid, the styloid process, the hyoid apparatus, and the thyroid cartilage. In other tetrapods, such as amphibians and reptiles, homologous bones to those of mammals, such as the quadrate, articular, columella, and entoglossus are part of the splanchnocranium. See also * Dermatocranium * Endocranium The endocranium in comparative anatomy is a part of the skull base in vertebrates and it represents the basal, inner part of the cranium. The term is also applied to the outer layer of the dura mater in human anatomy. Structure Structurally, t ... References {{anatomy-stub ...
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