Collected Item: “Age And Mode of the Middle Miocene Marine Flooding of the Pannonian Basin—Constraints from Central Serbia”
Врста публикације
Рад у часопису
Верзија рада
објављена верзија
Језик рада
енглески
Аутор/и (Милан Марковић, Никола Николић)
OLEG MANDIC, LJUPKO RUNDIĆ, STJEPAN ĆORIĆ, ÐURÐICA PEZELJ, DÖRTE THEOBALT, KARIN SANT, WOUT KRIJGSMAN
Наслов рада (Наслов - поднаслов)
AGE AND MODE OF THE MIDDLE MIOCENE MARINE FLOODING OF THE PANNONIAN BASIN—CONSTRAINTS FROM CENTRAL SERBIA
Наслов часописа
PALAIOS
Издавач (Београд : Просвета)
Society for Sedimentary Geology
Година издавања
2019
Сажетак на енглеском језику
The timing and mode of the marine flooding of the southern margin of the Pannonian basin in SE Europe
is still a matter of debate. In central Serbia, integrated bio-magnetostratigraphic data and quantified high-resolution
records are completely missing. Here, we provide paleoenvironmental and paleoecological constraints from the Slanci
section located near Belgrade that has an excellent preservation of micro-fauna and flora, i.e., planktonic and benthic
foraminifera and calcareous nannoplankton. We integrate their quantified records with sedimentological, natural
gamma radioactivity and magnetic susceptibility logs and include the non-quantified records of mollusks, corals, and
ostracods to reconstruct the regional depositional history. The section shows upper bathyal to outer shelf depositional
settings and alternating nutrient bottom conditions. The shallowing upwards trend marked by increasing terrestrial
input, attributes it to the early Highstand Systems Tract of the first marine third order sequence in this part of the
Pannonian Basin. We infer that the marine flooding in central Serbia took place at an age of ~ 14 Ma, slightly
predating the Langhian/Serravallian boundary (13.82 Ma) and the Badenian Salinity Crisis (~ 13.8–13.4 Ma) in the
Central Paratethys. Our results support an eastwards directed, tectonically forced, flooding of the southern Pannonian
Basin. This major paleoenvironmental turnover was forced by syn-rift tectonics in the Pannonian Basin system, which
started in the late early Miocene in the Styrian Basin (SE Austria) and ended more than 3 Myr later in the late middle
Miocene in the Morava depression (E Serbia).
is still a matter of debate. In central Serbia, integrated bio-magnetostratigraphic data and quantified high-resolution
records are completely missing. Here, we provide paleoenvironmental and paleoecological constraints from the Slanci
section located near Belgrade that has an excellent preservation of micro-fauna and flora, i.e., planktonic and benthic
foraminifera and calcareous nannoplankton. We integrate their quantified records with sedimentological, natural
gamma radioactivity and magnetic susceptibility logs and include the non-quantified records of mollusks, corals, and
ostracods to reconstruct the regional depositional history. The section shows upper bathyal to outer shelf depositional
settings and alternating nutrient bottom conditions. The shallowing upwards trend marked by increasing terrestrial
input, attributes it to the early Highstand Systems Tract of the first marine third order sequence in this part of the
Pannonian Basin. We infer that the marine flooding in central Serbia took place at an age of ~ 14 Ma, slightly
predating the Langhian/Serravallian boundary (13.82 Ma) and the Badenian Salinity Crisis (~ 13.8–13.4 Ma) in the
Central Paratethys. Our results support an eastwards directed, tectonically forced, flooding of the southern Pannonian
Basin. This major paleoenvironmental turnover was forced by syn-rift tectonics in the Pannonian Basin system, which
started in the late early Miocene in the Styrian Basin (SE Austria) and ended more than 3 Myr later in the late middle
Miocene in the Morava depression (E Serbia).
Волумен/том или годиште часописа
34
Број часописа
2
Почетна страна
71
Завршна страна
95
DOI број
10.2110/palo.2018.052
ISSN број часописа
0883-1351
Кључне речи на српском (одвојене знаком ", ")
Srednji miocen, morska transgresija, Panonski basen, područje Beograda
Кључне речи на енглеском (одвојене знаком ", ")
MIDDLE MIOCENE, MARINE FLOODING, THE PANNONIAN BASIN, BELGRADE AREA
Линк
https://pubs.geoscienceworld.org/sepm/palaios/article-pdf/34/2/71/4638118/i0883-1351-34-2-71.pdf
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Ужа категорија рада према правилнику МПНТ
М21
Пројект у склопу кога је настао рад
Projekti 176015, MNTR RS
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