Cyclostratigraphic dating in the Lower Badenian (Middle Miocene) of the Vienna Basin (Austria): the Baden-Sooss core |
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Authors: | J Hohenegger S Ćorić M Khatun P Pervesler F Rögl C Rupp A Selge A Uchman M Wagreich |
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Institution: | (1) Department of Palaeontology, University of Vienna, Vienna, Austria;(2) Geological Survey of Austria, Vienna, Austria;(3) Department of Geodynamics and Sedimentology, University of Vienna, Vienna, Austria;(4) Natural History Museum Vienna, Vienna, Austria;(5) Paleomagnetic Laboratory Gams, Institute of Geophysics, MU Leoben, Austria;(6) Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland |
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Abstract: | The scientific borehole Baden-Sooss penetrates a succession of Badenian (Langhian, Middle Miocene) sediments at the type locality
of the Badenian, the old brickyard Baden-Sooss in the Vienna Basin. The sedimentary succession of the 102-m-cored interval
consists of more than 95% bioturbated, medium-to-dark gray marly shales with carbonate contents between 11 and 25% and organic
carbon contents between 0.35 and 0.65%. Biostratigraphic investigations on foraminifera (mainly lower part of Upper Lagenid
Zone) and calcareous nannoplankton (standard zone NN5) indicate an early Badenian (Langhian) age. Cycles in carbonate content,
organic carbon content, and magnetic susceptibility have been identified by power spectra analysis. Correlations between the
three variables are extremely significant. Using cross-correlation, periods around 40 m correlate significantly with the 100 kyr−1 eccentricity cycle, the ∼20 m periods with the obliquity cycle, and the 15 to 11-m periods with both precession cycles. Wavelet
transformation and decomposition of composite periodic functions were used to obtain the position of the cycle peaks in the
profile. Cross-correlation with orbital cycles (La2004) dates the Baden-Sooss core between −14.379 ± 1 and −14.142 my ± 9 kyr. |
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Keywords: | Cylcostratigraphy Middle Miocene Badenian Astronomical tuning |
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