THE LATE BADENIAN-SARMATIAN (SERRAVALLIAN) ENVIRONMENTAL TRANSITION CALIBRATED BY SEQUENCE STRATIGRAPHY (EASTERN DANUBE BASIN, CENTRAL PARATETHYS)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11410%2F20%3A10414222" target="_blank" >RIV/00216208:11410/20:10414222 - isvavai.cz</a>
Result on the web
<a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=O2N5xdqUMt" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=O2N5xdqUMt</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.31577/GeolCarp.71.4.1" target="_blank" >10.31577/GeolCarp.71.4.1</a>
Alternative languages
Result language
angličtina
Original language name
THE LATE BADENIAN-SARMATIAN (SERRAVALLIAN) ENVIRONMENTAL TRANSITION CALIBRATED BY SEQUENCE STRATIGRAPHY (EASTERN DANUBE BASIN, CENTRAL PARATETHYS)
Original language description
The late Badenian and Sarmatian (Serravallian) evolution of depositional environments in the Danube Basin (Želiezovce Depression) has never been fully explored. Here, we clarify the paleoenvironmental changes which took place in this area during the late Badenian and Sarmatian on the basis of sedimentological, petrographic, biostratigraphic and paleobotanical analyses performed at multiple sections. The combination of these methods with sequence stratigraphy allowed us to divide the sedimentary record into three main intervals: 1) the transgressive late Badenian rocky shore deposits (transgressive and/or highstand system tract), followed by a gap in the stratigraphic record (that can approximately coincide with the latest Badenian falling stage system tract). 2) Earliest Sarmatian terrestrial deposits connected with the beginning of the Sarmatian transgression (synchronous with the lowstand system tract). 3) The early Sarmatian deltaic environment influenced by tidal processes associated with the highstand system tract. The fossil leaf association indicates a climatic turnover from subtropical to temperate conditions between the earliest (lowstand system tract) and the early Sarmatian (highstand system tract). Sediments of the late Sarmatian (falling stage system tract) were not deposited or were later eroded. However, they may be present in the neighbouring depressions, which tectonically opened during the late Sarmatian. The Badenian-Sarmatian boundary in the Želiezovce Depression is developed in transgressive shallow marine to terrestrial volcano-sediments as is typical for this boundary in most other Paratethys depocentres.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/GA18-25057S" target="_blank" >GA18-25057S: Quantifying openness of vegetation by the Integrated Plant Record vegetation analysis</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geologica Carpathica
ISSN
1335-0552
e-ISSN
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Volume of the periodical
71
Issue of the periodical within the volume
4
Country of publishing house
SK - SLOVAKIA
Number of pages
23
Pages from-to
291-313
UT code for WoS article
000565769300001
EID of the result in the Scopus database
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