A high-resolution, multiproxy stratigraphic analysis of the Devonian-Carboniferous boundary sections in the Moravian Karst (Czech Republic) and a correlation with the Carnic Alps (Austria)

0439374 - ÚACH 2015 GB J - Článek v odborném periodiku
Kumpan, T. - Bábek, O. - Kalvoda, J. - Frýda, J. - Matys Grygar, Tomáš
A high-resolution, multiproxy stratigraphic analysis of the Devonian-Carboniferous boundary sections in the Moravian Karst (Czech Republic) and a correlation with the Carnic Alps (Austria).
Geological Magazine. Roč. 151, č. 2 (2014), s. 201-215. ISSN 0016-7568. E-ISSN 1469-5081
Grant CEP: GA ČR(CZ) GAP210/11/1891
Institucionální podpora: RVO:61388980
Klíčová slova: Hangenberg Event * gamma-ray spectra * carbon isotopes * element geochemistry
Impakt faktor: 2.482, rok: 2014

A multidisciplinary correlation of the Devonian-Carboniferous (D-C) boundary sections from the Moravian Karst (Czech Republic) and the Carnic Alps (Austria), based on conodont and foraminifer biostratigraphy, microfacies analysis, field gamma-ray spectroscopy (GRS), carbon isotopes and element geochemistry, is presented in this paper. The study is focused on the interval from the Middle Palmatolepis gracilis expansa Zone (Late Famennian) to the Siphonodella sandbergi Zone (Early Tournaisian). In Lesni lom (Moravian Karst), a positive C-13 excursion in the Bisphatodus costatus - Protognathodus kockeli Interregnum from a distinct laminated carbonate horizon is correlated with a carbon isotope excursion from the Grune Schneid section of the Carnic Alps and is interpreted as the equivalent of the Hangenberg black shales and a local expression of the global Hangenberg Event sensu stricto. Higher up at both sections, a significant increase in the terrigenous input, which is inferred from the GRS signal and elevated concentrations of terrigenous elements (Si, Ti, Zr, Rb, Al, etc.), provides another correlation tieline and is interpreted as the equivalent of the Hangenberg sandstone. Both horizons are discussed in terms of relative sea-level fluctuations and palaeoceanographic changes. Recent studies show that conodont biostratigraphy is facing serious problems associated with the taxonomy of the first siphonodellids, their dependence on facies and discontinuous occurrences of protognathodids at the D-C boundary. Therefore, the correlative potential of geochemical and petrophysical signatures is high and offers an alternative for the refining of the problematic biostratigraphic division of the D-C boundary.
Trvalý link: http://hdl.handle.net/11104/0242667