Dicrocerus Furcatus
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Dicrocerus Furcatus
''Dicrocerus elegans'' (Its name is Greek for "fork antler") is an extinct species of deer found in France, Europe (related species in Asia). ''Dicrocerus'' probably came from Asia, from the region where true deer are believed to have originated and evolved. It inhabited forests in the temperate belt and in Europe it was typical of the Miocene (15-5 million years ago). It died out at the beginning of Pliocene without leaving any descendants. Description ''Dicrocerus'' stood tall at the shoulder - the same size as the modern roe deer. Its long skull sported a set of antlers with a thickened base - the first known member of cervids to possess them. The antlers were still quite primitive and had no tines; they were worn only by the males. Like modern deer, ''Dicrocerus'' shed its antlers every year. The main stem was shorter in each new set. The same is seen in modern muntjacs. Gallery Dicrocerus elegans MHNT.PRE.2012.0.jpg, ''Dicrocerus elegans'' Collection Lartet MHNT Dicro ...
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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" 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 ...
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