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A series of ecostratigraphic events across the Langhian/Serravallian boundary in an epicontinental setting: the northern Pannonian Basin

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Abstract

The ŠO-1 core situated in the NE part of the Pannonian Basin represents a parastratotype of the Badenian stage (regional Central Paratethys stage corresponding to the Langhian and Serravallian). A 150-m-thick succession was deposited between ~ 14.2 and 13.5 Ma (dated by the last common occurrence of Helicosphaera waltrans to the last occurrence of Sphenolithus heteromorphus) and spans the Langhian/Serravallian boundary. The section was subdivided into four units: (1) A transgressive carbonate–siliciclastic complex (core depth ~ 150–122 m) deposited in an inner to mid carbonate ramp setting. Carbonate deposition was episodically interrupted by the input of terrigenous phytodetritus as a result of increased precipitation. (2) Tuffaceous siltstone (core depth ~ 122–48 m) corresponding to a sea-level highstand. This unit starts with a Pteropoda immigration event (14.5–14.2 Ma), which could be related to the closing of the Indian-Mediterranean corridor that triggered a change from Indian- to Atlantic-controlled surface circulation in the Mediterranean-Paratethys basin system. An enhanced proportion of high-nutrient markers and a decreased abundance of warm-water plankton might be indicative of eutrophication and cooling of Paratethyan waters at this time. (3) Lowstand sandstone (core depth ~ 48–26 m) indicating stabilization of sea-grass meadows with eutrophic and hypoxic conditions within their root system. A sea-level fall at this time is correlated with the Ser 1 event. (4) A Serravallian transgressive event (core depth ~ 26–5 m) associated with an increase in diversity of benthic assemblages and stabilization of stenohaline assemblages.

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Acknowledgements

This project was supported by programs PROGRESS Q45, VEGA 02/122/18, Ministry of Culture of the Czech Republic (project DKRVO 2019–2023/1.IVa and 2.IIa; National Museum, 00023272). The authors greatly appreciate the reviews of Mihovil Brlek (Zagreb) and one anonymous reviewer as well as constructive comments of the handling editor Maurice Tucker that helped to improve the manuscript significantly. We thank Nela Doláková (Masaryk University, Brno) for her kind and very useful help with palynological analysis.

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Authors and Affiliations

  1. Institute of Geology and Paleontology, Charles University, Albertov 6, 128 43, Prague 2, Czech Republic

    Katarína Holcová & Filip Scheiner

  2. National Museum, Václavské náměstí 68, 110 00, Prague 1, Czech Republic

    Jiřina Dašková & František Vacek

  3. State Geological Institute of Dionýz Štúr, Mlynská dolina 1, 817 04, Bratislava 11, Slovakia

    Klement Fordinál

  4. Earth Sciences Institute of the Slovak Academy of Sciences, Dúbravská cesta 9, 840 05, Bratislava, Slovakia

    Juraj Hrabovský

  5. Earth Sciences Institute of the Slovak Academy of Sciences, Ďumbierska cesta 1, 974 11, Banská Bystrica, Slovakia

    Rastislav Milovský

  6. Institute of Geology, Academy of Sciences of the Czech Republic, Rozvojová 269, 165 00, Prague 6 Lysolaje, Czech Republic

    Jiřina Dašková & Filip Scheiner

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  1. Katarína Holcová
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Correspondence to Katarína Holcová.

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Holcová, K., Dašková, J., Fordinál, K. et al. A series of ecostratigraphic events across the Langhian/Serravallian boundary in an epicontinental setting: the northern Pannonian Basin. Facies 65, 36 (2019). https://doi.org/10.1007/s10347-019-0576-1

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