Bryoherms from the lower Sarmatian (upper Serravallian, Middle Miocene) of the Central Paratethys. [PDF]
Facies, 2023 AbstractBryozoan–serpulid–algal–thrombolite bioherms of up to 50 cm size are described from the Sarmatian (upper Middle Miocene) of the Central Paratethys. They occur on top of lower Sarmatian carbonate sediments of high-energy conditions and the individual bioherms settle on crests of ripples.
Piller WE, Harzhauser M.
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A 13.06 Ma widespread ignimbrite in the Pannonian Basin captured a snapshot of shallow marine to coastal environment in Central Paratethys [PDF]
Scientific ReportsVoluminous Miocene silicic volcanism sourced mainly from the extensional Pannonian Basin played a major role in the evolution of the Central Paratethys.
Dávid Karátson +21 more
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The Central Paratethys Sea-rise and demise of a Miocene European marine biodiversity hotspot. [PDF]
Sci RepAbstractThe Miocene Climate Optimum (MCO, ~ 17–14 Ma) was a time of extraordinary marine biodiversity in the Circum-Mediterranean Region. This boom is best recorded in the deposits of the vanished Central Paratethys Sea, which covered large parts of central to southeastern Europe.
Harzhauser M +3 more
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Oligocene archaeomonad stomatocysts from the Polish Central Paratethys
Acta Palaeontologica PolonicaAn unanticipated diversity of archaeomonad stomatocysts intermixed with marine plankton including diatoms, silicoflagellates, parmaleans and individual siliceous protistan scales was encountered in Rupelian diatomites from the Central Paratethys. In this
Irena Kaczmarska +2 more
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The middle miocene (Badenian) holoplanktonic mollusks (Euthecosomata - Pteropoda) from Serbia, central paratethys [PDF]
Geološki Anali Balkanskoga PoluostrvaThe present paper deals with holoplanktonic gastropods (Pteropoda) from the Middle Miocene (Badenian) deposits of Serbia. The material for the present study comes from three localities at the southern margin of the Pannonian Basin (Central Paratethys ...
Jovanović Gordana +4 more
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The South-Western Boundary of Central Paratethys
Geologia Croatica, 2002 Small Neogene basins within the Dinarides were never invaded bymarine transgressions during their evolution. The fresh-water sedimentation, endemic fauna and their position between the Adriaticregion and the Pannonian Basin System explain why these ...
Davor Pavelić
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Diversity and distribution patterns of the Oligocene and Miocene decapod crustaceans (Crustacea: Malacostraca) of the Western and Central Paratethys [PDF]
Geologica Carpathica, 2016 Decapod associations have been significant components of marine habitats throughout the Cenozoic when the major diversification of the group occurred.
Hyžný Matúš
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Euryhaline preferences of the decapod crab Mioplax socialis enabled it to survive during the Badenian/Sarmatian extinction (Miocene) in the Central Paratethys [PDF]
Geologica Carpathica, 2016 Although decapod crustaceans of the Central Paratethys were diverse during the Badenian (Langhian-Early Serravallian), a dramatic drop in their diversity occurred at the boundary with the Sarmatian.
Hyžný Matúš +3 more
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Late Miocene megalake regressions in Eurasia [PDF]
Scientific Reports, 2021 The largest megalake in the geological record formed in Eurasia during the late Miocene, when the epicontinental Paratethys Sea became tectonically-trapped and disconnected from the global ocean.
Dan Valentin Palcu +6 more
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Geologica Carpathica, 2018 Depositional sequences originating in semi-enclosed basins with endemic biota, partly or completely isolated from the open ocean, frequently do not allow biostratigraphic correlations with the standard geological time scale (GTS).
Kováč Michal +6 more
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