Towards a high-resolution chronostratigraphy and geochronology for the Pannonian Stage: Significance of the Paks cores (Central Pannonian Basin)

  • Imre Magyar Research Group for Paleontology, Hungarian Academy of Sciences-Hungarian Natural History Museum-Eötvös U; MOL Plc., e-mail: immagyar@mol.hu
  • Orsolya Sztanó Department of Geology, Eötvös University, e-mail: sztano@caesar.elte.hu
  • Krisztina Sebe Department of Geology and Meteorology, University of Pécs
  • Lajos Katona MTM Bakony Natural History Museum, Zirc, e-mail: finci@nhmus.hu
  • Vivien Csoma Department of Paleontology, Eötvös University
  • Ágnes Görög Department of Paleontology, Eötvös University
  • Emőke Tóth Department of Paleontology, Eötvös University
  • Andrea Szuromi-Korecz MOL Plc.
  • Michal Šujan Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava
  • Régis Braucher Aix-Marseille University, Aix-en-Provence
  • Zsófia Ruszkiczay-Rüdiger Research Centre for Astronomy and Earth 9 Sciences, Institute for Geological and Geochemical Research (CSFK-FGI)
  • Balázs Koroknai Geomega Ltd.
  • Géza Wórum Geomega Ltd.
  • Karin Sant Paleomagnetic Laboratory ‘Fort Hoofddijk’, Utrecht University
  • Nick Kelder Paleomagnetic Laboratory ‘Fort Hoofddijk’, Utrecht University
  • Wout Krijgsman Paleomagnetic Laboratory ‘Fort Hoofddijk’, Utrecht University
Keywords: Lake Pannon, stratigraphy, lithostratigraphy, biostratigraphy, seismic stratigraphy, sequence stratigraphy, magneto - stratigraphy, authigenic 10Be/9Be dating

Abstract

A new stratigraphic standard for the open lacustrine to deltaic Pannonian Stage is emerging from the combined sedimentological, lithostratigraphical, sequence stratigraphical, biostratigraphical, seismic stratigraphical, geochronological, and magnetostratigraphical investigations of 6 long drill cores. These were drilled by Paks II Nuclear Power Plant Plc. as a preparatory step for the construction of a new power plant near the city of Paks, Central Pannonian Basin, between 2015 and 2016. The boreholes are in a distance of 8-12 km from each other, and five of them fully penetrated the local Pannonian sequence in a thickness of 390 to 662 m. Each core includes offshore clay marl deposited far from sediment entry points (Endrőd Fm), heterolithic, sandy siltstones of a <200 m high shelf-margin slope (Algyő Fm), and several stacked deltaic deposits from prodelta silts to sandy mouth bars, heterolithics, lignite and sandy channel-fills of the delta plain (Újfalu Fm). Magnetostratigraphic investigations from two cores and authigenic 10Be/9Be dating from two others were combined by means of seismic correlation between the boreholes, and thus they provide a solid geochronological and chronostratigraphic basis for the interpretation of the sedimentologial and paleontological records of the cores. The continuous representation of the earliest Pannonian (11.6–9.1 Ma) in the cores needs further investigation, as neither magnetostratigraphy nor authigenic 10Be/9Be dating gave reliable age data from the basal, condensed calcareous marls. The 9.1 to 6.5 Ma interval, however, is represented in the cores by various lithologies and abundant and sometimes excellently preserved fossils. In the deltaic succession, 8 sedimentary sequences were correlated between the cores; as their duration is not more than 400 kyr each, they can be regarded as 4th-order sequences. The paleontological record of the cores shows a very good agreement with the formerly established biochronostratigraphical system. The cores provide an insight into the evolution of the sedimentary environment and the biota of Lake Pannon between 9.1 and 6.5 Ma with a so far unprecedented temporal and spatial resolution.

Published
2019-10-02
How to Cite
MagyarI., SztanóO., SebeK., KatonaL., CsomaV., Görög Ágnes, TóthE., Szuromi-KoreczA., ŠujanM., BraucherR., Ruszkiczay-RüdigerZ., KoroknaiB., WórumG., SantK., KelderN., & KrijgsmanW. (2019). Towards a high-resolution chronostratigraphy and geochronology for the Pannonian Stage: Significance of the Paks cores (Central Pannonian Basin). Földtani Közlöny, 149(3, 4), 351. https://doi.org/10.23928/foldt.kozl.2019.149.4.351

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