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In the geologic timescale, the Asselian is the earliest geochronologic age or lowermost chronostratigraphic stage of the Permian. It is a subdivision of the Cisuralian epoch or series. The Asselian lasted between and million years ago (Ma). It was preceded by the Gzhelian (the latest or uppermost subdivision in the Carboniferous) and followed by the Sakmarian.〔See Gradstein ''et al.'' (2004) for a detailed geologic timescale〕 ==Stratigraphy== The Asselian stage was introduced into scientific literature in 1954, when the Russian stratigrapher V.E. Ruzhenchev split it from the Artinskian. At that moment the Artinskian still encompassed most of the lower Permian - its current definitions are more restricted. The Asselian is named after the Assel River in the southern Ural Mountains of Kazakhstan. The base of the Asselian stage is at the same time the base of the Cisuralian series and the Permian system. It is defined as the place in the stratigraphic record where fossils of the conodont ''Streptognathodus isolatus'' first appear. The global reference profile for the base (the GSSP or golden spike) is located in the valley of the Aidaralash River, near Aqtöbe in the Ural Mountains of Kazakhstan.〔The GSSP was first proposed by Davydov ''et al.'' (1998)〕 The top of the Asselian stage (the base of the Sakmarian stage) is at the first appearance of conodont species ''Streptognathodus postfusus''. The Asselian contains five conodont biozones: *zone of ''Streptognathodus barskovi'' *zone of ''Streptognathodus postfusus'' *zone of ''Streptognathodus fusus'' *zone of ''Streptognathodus constrictus'' *zone of ''Streptognathodus isolatus'' 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Asselian」の詳細全文を読む スポンサード リンク
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