Publication details
Reconstruction of the unusual Middle Miocene (Badenian) palaeoenvironment of the Carpathian Foredeep (Lomnice/Tišnov denudational relict, Czech Republic)
| Authors | |
|---|---|
| Year of publication | 2015 |
| Type | Article in Periodical |
| Magazine / Source | Geological Quarterly |
| MU Faculty or unit | |
| Citation | |
| Doi | http://dx.doi.org/10.7306/gq.1249 |
| Field | Geology and mineralogy |
| Keywords | Badenian-Carpathian Foredeep-lithology-otoliths- foraminifera- calcareous nannoplankton. |
| Description | Multiproxy sedimentological, gammaspectrometric, foraminiferal, calcareous nannoplankton, and otolith data were used for the reconstruction of the Badenian (Middle Miocene) history of the Moravian part of the Carpathian Foredeep. The study material originated from the new bore hole LOM-1, which drilled >20 metres of monotonous clayey siltstones with exceptionally rich and well preserved microfossil assemblages. Distal parts of the Carpathian Foredeep (a forebulge depozone) are exposed in this succession. Generally, a quiet environment of outer shelf to upper bathyal of monotonous clayey silts was interpreted, which is typical for the proximal parts of a peripheral foreland basin. The section studied can be subdivided into six intervals, confirming the cyclical character of Middle Miocene sedimentation in the Central Paratethys. Interannual oscillations of nutrient content, temperature and/or salinity are interpreted based on the oscil aions of geochemical as well as palaeobiological data. The turnover connected with the initiation of the Middle Miocene Climatic Transition is recorded above the LO (last occurrence) of Helicosphaera waltrans in agree ment with previous observations in the Carpathian Foredeep. The changes include cooling a decrease in nutrients, a probable increase of the sa linity of surface water, and increase of seasonality. Seasonal ity was manifested by an alternation of mixed and stratified water columns with a seasonal input of nutrients. Concerning nutrients, sources of seasonal riverine input or seasonal upwelling are both possible. |
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