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The Gzhelian is an age in the ICS geologic timescale or a stage in the stratigraphic column. It is the youngest stage of the Pennsylvanian, the youngest subsystem of the Carboniferous. The Gzhelian lasted from to Ma.〔; 2004: ''A Geologic Time Scale 2004'', Cambridge University Press〕 It follows the Kasimovian age/stage and is followed by the Asselian age/stage, the oldest subdivision of the Permian system. The Gzhelian is more or less coeval with the Stephanian stage of the regional stratigraphy of Europe. ==Name and definition== The Gzhelian is named after the Russian village of Gzhel ((ロシア語:Гжель)), nearby Ramenskoye, not far from Moscow. The name and type locality were defined by Sergei Nikitin (1850–1909) in 1890. The base of the Gzhelian is at the first appearance of the Fusulinida genera ''Daixina'', ''Jigulites'' and ''Rugosofusulina'', or at the first appearance of the conodont ''Streptognathodus zethus''. The top of the stage (the base of the Permian system) is at the first appearance of the conodont ''Streptognathodus isolatus'' within the ''Streptognathus "wabaunsensis"'' chronocline.〔; 1998: ''Proposal of Aidaralash as Global Stratotype Section and Point (GSSP) for base of the Permian System'', Episodes 21(1): pp 11-18, ()〕 Six meters higher in the reference profile, the Fusulinida species ''Sphaeroschwagerina vulgaris aktjubensis'' appears. At the moment (2008), a golden spike for the Gzhelian stage is yet lacking. A candidate is a section along the Ussolka river (a tributary of the Belaya river) at the edge of the hamlet of Krasnoussolsky, about 120 kilometres south-east of Ufa and 60 kilometres north-east of Sterlitamak (in Bashkortostan).〔; 2006: ''Usolka section (southern Urals, Russia): a potential candidate for GSSP to define the base of the Gzhelian Stage in the global chronostratigraphic scale'' Geologija 49(2): pp 205–217, ()〕 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「Gzhelian」の詳細全文を読む スポンサード リンク
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