THE LATE BADENIAN-SARMATIAN (SERRAVALLIAN) ENVIRONMENTAL TRANSITION CALIBRATED BY SEQUENCE STRATIGRAPHY (EASTERN DANUBE BASIN, CENTRAL PARATETHYS)

Kód výsledku v 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>

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

THE LATE BADENIAN-SARMATIAN (SERRAVALLIAN) ENVIRONMENTAL TRANSITION CALIBRATED BY SEQUENCE STRATIGRAPHY (EASTERN DANUBE BASIN, CENTRAL PARATETHYS)

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

THE LATE BADENIAN-SARMATIAN (SERRAVALLIAN) ENVIRONMENTAL TRANSITION CALIBRATED BY SEQUENCE STRATIGRAPHY (EASTERN DANUBE BASIN, CENTRAL PARATETHYS)

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/GA18-25057S" target="_blank" >GA18-25057S: Kvantifikace “otevřených” vegetačních společenstev přostednictvím Integrated Plant Record vegetační analýzy</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2020

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geologica Carpathica

ISSN

1335-0552

e-ISSN

—

Svazek periodika

71

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

23

Strana od-do

291-313

Kód UT WoS článku

000565769300001

EID výsledku v databázi Scopus

—