Alces Gallicus
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Alces Gallicus
''Alces gallicus'', also known as the Gallic moose, is an extinct species of moose, which has been found in Europe. It is believed to have lived in Pleistocene The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ... about 2 MYA. This species was smaller than recent moose, but it had longer antlers than it's modern relatives. Antlers structure similar to '' Cervalces'', consisted of very long beams and relatively small palms. It is sometimes included in the genus '' Libralces'' or '' Cervalces''. References gallicus Prehistoric deer Pleistocene Artiodactyla Pleistocene mammals of Europe Pleistocene extinctions Fossil taxa described in 1952 {{Paleo-eventoedungulate-stub ...
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Alces
''Alces'' is a genus of artiodactyl mammals, that includes the largest species of the deer family. There are two species in genus: the moose The moose (: 'moose'; used in North America) or elk (: 'elk' or 'elks'; used in Eurasia) (''Alces alces'') is the world's tallest, largest and heaviest extant species of deer and the only species in the genus ''Alces''. It is also the tal ... (''Alces alces'') and the fossil '' Alces gallicus'' (also known as the Gallic moose), that existed in the Pleistocene about 2 million years ago. Sometimes only one species is included in the genus, the modern moose (''Alces alces''), while the extinct Gallic moose is more often referred to the genus '' Cervalces'', since the structure of their antlers looks similar. "American moose" Sometimes the species ''Alces alces'' is divided into two separate species - European moose (''A. alces),'' and American moose (''A. americanus''). The American moose, contrary to its name, includes all subspecies ...
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Europe
Europe is a continent located entirely in the Northern Hemisphere and mostly in the Eastern Hemisphere. It is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, the Mediterranean Sea to the south, and Asia to the east. Europe shares the landmass of Eurasia with Asia, and of Afro-Eurasia with both Africa and Asia. Europe is commonly considered to be Boundaries between the continents#Asia and Europe, separated from Asia by the Drainage divide, watershed of the Ural Mountains, the Ural (river), Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea, and the waterway of the Bosporus, Bosporus Strait. "Europe" (pp. 68–69); "Asia" (pp. 90–91): "A commonly accepted division between Asia and Europe ... is formed by the Ural Mountains, Ural River, Caspian Sea, Caucasus Mountains, and the Black Sea with its outlets, the Bosporus and Dardanelles." Europe covers approx. , or 2% of Earth#Surface, Earth's surface (6.8% of Earth's land area), making it ...
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Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ...
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Cervalces
''Cervalces'' is an extinct deer genus that lived during the Pliocene and Pleistocene epochs. ''Cervalces gallicus'' is either classified as a species of the related '' Libralces'', or an ancestral species to other members of ''Cervalces''. It lived in Europe from the Pliocene to the Pleistocene. '' Cervalces scotti'', the stag-moose, lived in Pleistocene North America. '' Cervalces latifrons'', the broad-fronted moose, and '' Cervalces carnutorum'' were found in Pleistocene Europe and Asia. The genus has been suggested to be paraphyletic and ancestral with respect to '' Alces'', the genus which contains the modern moose The moose (: 'moose'; used in North America) or elk (: 'elk' or 'elks'; used in Eurasia) (''Alces alces'') is the world's tallest, largest and heaviest extant species of deer and the only species in the genus ''Alces''. It is also the tal ..., and as such, some authors synonymise ''Cervalces'' with ''Alces''. References External linksStag Moose Image ...
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Libralces
''Libralces'' was a genus of Eurasian deer that lived during the Pliocene epoch. It is notable for its 2+ meter wide antlers, comparable in size to those of '' Megaloceros''. ''Libralces'' fossils have been found from France to Tajikistan, with the best-known examples being the French '' L. gallicus''. According to Jordi Agustí, ''Libralces'' was the ancestor of ''Megaloceros'', though most other authorities regard it as a relative of moose, '' Alces''. In the Pleistocene, there were three genera of Holarctic moose-like deer — '' Cervalces'', ''Alces'', and ''Libralces''. In contrast to modern ''Alces'', the Villafranchian ''Libralces gallicus'' had very long-beamed, small-palmed antlers and a generalized skull with moderately reduced nasals; the Nearctic The Nearctic realm is one of the eight biogeographic realms constituting the Earth's land surface. The Nearctic realm covers most of North America, including Greenland, Central Florida, and the highlands of Mexico. ...
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Prehistoric Deer
Prehistory, also called pre-literary history, is the period of human history between the first known use of stone tools by hominins  million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared years ago. It took thousands of years for writing systems to be widely adopted, with writing having spread to almost all cultures by the 19th century. The end of prehistory therefore came at different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. It is based on an old conception of history that without written records there could be no history. The most common conception today is that history is based on evidence, however the concept of prehistory hasn't been completely discarded. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilis ...
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Pleistocene Artiodactyla
The Pleistocene ( ; referred to colloquially as the ''Ice Age'') is the geological epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold glacial periods and warmer interglacials, with the sea levels being up to lower than ...
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Pleistocene Extinctions
The Late Pleistocene to the beginning of the Holocene saw the extinction of the majority of the world's megafauna, typically defined as animal species having body masses over , which resulted in a collapse in faunal density and diversity across the globe. The extinctions during the Late Pleistocene are differentiated from previous extinctions by their extreme size bias towards large animals (with small animals being largely unaffected), and widespread absence of ecological succession to replace these extinct megafaunal species, and the regime shift of previously established faunal relationships and habitats as a consequence. The timing and severity of the extinctions varied by region and are generally thought to have been driven by humans, climatic change, or a combination of both. Human impact on megafauna populations is thought to have been driven by hunting ("overkill"), as well as possibly environmental alteration. The relative importance of human vs climatic factors in th ...
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