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Conodont and foraminiferal biostratigraphy of the Late Famennian and Early Tournaisian in the Moravian Karst (Moravo-Silesian Zone, Czech Republic)
Autoři | |
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Rok publikování | 2013 |
Druh | Článek v odborném periodiku |
Časopis / Zdroj | Document de l'Institut Scientifique, Rabat |
Fakulta / Pracoviště MU | |
Citace | |
Obor | Geologie a mineralogie |
Klíčová slova | Devonian;Carboniferous;conodont zonation;foraminiferal zonation |
Popis | The conodont succession from the Moravian Karst reveals good correlation with other areas. All of the seven group of early siphonodellids sensu Kaiser-Corradini (2011) have been easily determined. The calciturbidite succession with more shallow water allochems yielded so far richest foraminiferal association at the Devonian-Carboniferous boundary. where the evolution of foraminiferal fauna is calibrated by conodont zonation. |
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