Sedimentologic and paleoclimatic reconstructions of carbonate factory evolution in the Alborz Basin (northern Iran) indicate a global response to Early Carboniferous (Tournaisian) glaciations

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• 作者：Mehrdad Sardar Abadi^a ; ^b ; ^{mehrdad.sardarabadi@doct.ulg.ac.be} ; Elena I. Kulagina^c ; ^d ; Dennis F.A.E. Voeten^e ; Fré ; dé ; ric Boulvain^a ; Anne-Christine Da Silva^a ; ^f
• 关键词：Carboniferous ; Tournaisian ; Alborz Basin ; Mobarak Formation ; glaciation ; carbonate factory
• 刊名：Sedimentary Geology
• 出版年：2017
• 出版时间：1 March 2017
• 年：2017
• 卷：348
• 期：Complete
• 页码：19-36
• 全文大小：5162 K
• 卷排序：348

文摘

The Iranian Mobarak Formation recorded Tournaisian events through carbonate factory evolution Local controls, but also continental and global advents are reflected in its facies development Tournaisian glaciations influenced paleoclimate and species distribution on a global scale The Tournaisian Alborz Basin had a subtropical paleoposition rather than a temperate affinity