Podrobný výpis o publikaci
2014
Early Sarmatian paleoenvironments in the easternmost Pannonian Basin (Borod Depression, Romania) restored from micropaleontological data.
FILIPESCU, S., A. MICLEA, M. GROSS, M. HARZHAUSER, Kamil ZÁGORŠEK et. al.Základní údaje
Originální název
Early Sarmatian paleoenvironments in the easternmost Pannonian Basin (Borod Depression, Romania) restored from micropaleontological data.
Autoři
FILIPESCU, S. (642 Rumunsko), A. MICLEA (642 Rumunsko), M. GROSS (40 Rakousko), M. HARZHAUSER (40 Rakousko), Kamil ZÁGORŠEK (203 Česká republika, garant, domácí) a C. JIPA (642 Rumunsko)
Vydání
Geologica Carpathica, Bratislava, Veda, Publishing House of the Slovak Academy of Sciences, 2014, 1335-0552
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Slovensko
Utajení
není předmětem státního či obchodního tajemství
Kód RIV
RIV/46747885:24510/14:#0001125
Organizace
Fakulta přírodovědně-humanitní a pedagogická – Technická univerzita v Liberci – Repozitář
UT WoS
000332843900005
Klíčová slova anglicky
Sarmatian (late Middle Miocene); Borod Depression (NW-Romania); paleoenvironments; paleogeography; sequence stratigraphy; molluscs; bryozoans; foraminifera; ostracods
Změněno: 26. 3. 2015 14:53, Kamil Zágoršek
Anotace
V originále
The Sarmatian sedimentary record of the Borod Depression (eastern Pannonian Basin) consists of a marine sequence with continental influence. The investigated section, located near Varciorog, was biostratigraphically and paleoenvironmentally analysed. The micro-and macrofossil assemblages include dasycladaceans, characeans, foraminifera, molluscs, polychaetes, ostracods, crabs, bryozoans, fish and vertebrate remains, which are characteristic for a shallow marine setting with local transitions to continental facies. The microfossil assemblages are characteristic for the Elphidium reginum Zone and Mohrensternia Zone of the early Sarmatian (Serravallian). The succession of populations correlates with the sedimentological trend, allowing the separation of several genetic units. The relative sea-level changes and the progradational trend from the top of the section suggest active tectonics in the hinterland (Apuseni Mountains). The shallow seas surrounding the emerging islands (Apuseni Mountains) provided the connections between the Pannonian and Transylvanian basins during the early Sarmatian