Conodont and foraminiferal biostratigraphy of the Late Famennian and Early Tournaisian in the Moravian Karst (Moravo-Silesian Zone, Czech Republic)
| Authors | |
|---|---|
| Year of publication | 2013 |
| Type | Article in Periodical |
| Magazine / Source | Document de l'Institut Scientifique, Rabat |
| MU Faculty or unit | |
| Citation | |
| Field | Geology and mineralogy |
| Keywords | Devonian;Carboniferous;conodont zonation;foraminiferal zonation |
| Description | 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. |
| Related projects: |