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Paleoenvironmental dynamics in Southern Pannonian Basin during Middle Miocene marine flooding (CROSBI ID 572621)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija

Pezelj, Đurđica ; Mandic, Oleg ; Sremac, Jasenka Paleoenvironmental dynamics in Southern Pannonian Basin during Middle Miocene marine flooding // International Symposium on Foraminifera, Forams 2010. Bon, 2010. str. 159-159

Podaci o odgovornosti

Pezelj, Đurđica ; Mandic, Oleg ; Sremac, Jasenka

engleski

Paleoenvironmental dynamics in Southern Pannonian Basin during Middle Miocene marine flooding

Quantitative analysis has been carried out on 42 bulk sediment samples from the coal pit Ugljevik in NE Bosnia and Herzegovina. The outcrop displays the initial transgression of the Central Paratethys Sea in the southern Pannonian Basin. About 60 m thick section starts with Oligocene lacustrine deposits. Initial marine sediments superpose the angular disconformity. They bear assemblages of late Early Badenian Upper Lagenidae Ecozone passing upward into Middle Badenian Spirorutilus carinatus Ecozone, correlating thus with the late Langhian. Data distinguishing 84 benthic foraminifera species were processed by multivariate statistics. Results supported the definition of 5 upward gradually alternating assemblages. Hence the initial marine deposits comprise Cibicidoides ungerianus - Asterigerinata planorbis assemblage that inhabited high oxic environment of the inner shelf. Upward gradual deepening trend and ongoing transgression affected the increase in planctonic foraminifera contributions, the increase of infaunal and opportunistic benthic foraminifera species, and the decrease of bottom water oxygen content. Stable medium oxic conditions on middle to outer shelf install soon. They display the highly diversified Valvulineria complanata - C. ungerianus assemblage. The occasional organic matter input, triggering oxygen fluctuations along with the nutrient quantity and quality variation, is furthermore marked by alternations of V. complanata and V. complanata – Globocassidulina oblonga assemblages. Intensive lamination together with almost continuous presence of low oxic conditions indicates increase in organic matter input during Middle Badenian. The stratification in water column was possibly triggered by fresh water feed likely responsible for increased redeposition of shallow water species. Environmental stress is strongly suggested by increase of dominance and decrease of diversity recorded from Bulimina subulata - B. elongata - Valvulineria complanata - Bolivina dilatata assemblage. The studied marine flooding cycle shows pattern of initial upward deepening, followed by stabile high stand conditions. The small scale environmental disturbances recorded therein, turn than finally to continuously stressed low oxic bottom water conditions.

Middle Miocene; paleoenvironment; Pannonian Basin

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Podaci o prilogu

159-159.

2010.

objavljeno

Podaci o matičnoj publikaciji

International Symposium on Foraminifera, Forams 2010

Bon:

Podaci o skupu

International Symposium on Foraminifera, Forams 2010

poster

05.09.2010-10.09.2010

Bonn, Njemačka

Povezanost rada

Geologija