Geologica Carpathica, 2018 Hydrocarbon exploration in the Bernhardsthal and Bernhardsthal-Sued oil fields documents an up to 2000 m thick succession of middle and upper Badenian deposits in this part of the northern Vienna Basin (Austria).
Harzhauser Mathias +9 more
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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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New data concerning the early middle miocene on the southern slopes of Fruška Gora (Northern Serbia): A case study from the Mutalj quarry [PDF]
Geološki Anali Balkanskoga Poluostrva, 2011 During the last few years, geological research at the southern slopes of Fruška Gora Mt. enabled the discovery of different Miocene units (undivided the Lower Miocene and Middle Miocene Badenian, predominantly). This is primarily thinking of the
Rundić Ljupko +4 more
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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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Tertiary Subsurface Facies, Source Rocks and Hydrocarbon Reservoirs in the SW Part of the Pannonian Basin (Northern Croatia and South-Western Hungary) [PDF]
Geologia Croatica, 2003 The Neogene sedimentary successions of the Drava, Sava and Slavonija–Srijem depressions in the SW part of the Pannonian Basin Systemare built up of three 2nd order megacycles separated by four majorerosional unconformities.
Bruno Saftić +4 more
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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
doaj +2 more sources
The antiquity of the Rhine River: stratigraphic coverage of the dinotheriensande (eppelsheim formation) of the Mainz Basin (Germany). [PDF]
PLoS One, 2012 Background: Mammalian fossils from the Eppelsheim Formation (Dinotheriensande) have been a benchmark for Neogene vertebrate palaeontology since 200 years.
Böhme M +3 more
europepmc +5 more sources
Litho- and biostratigraphic data of lower-middle Miocene sections in the Transylvanian basin and SE Carpathian Foredeep (Romania) [PDF]
Data in Brief, 2019 Litho- and biostratigraphic data are provided of 5 stratigraphic sections in Romania covering the “Badenian” marine flooding that occurred in the Central Paratethys during the middle Miocene (Langhian).
K. Sant +7 more
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Badenian rhodolith in Kozjansko (E Slovenia)
Geologija, 1995 Rhodolith beds are the basal transgressive unit of the several hundred metres thick Badenian succession, and are a pecuharity of the Kozjansko area.Rhodoids are mainly spherical having up to 15 cm in diameter.
Bogoljub Aničić, Bojan Ogorelec
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Miocene Slănic Tuff, Eastern Carpathians, Romania, in the Context of Badenian Salinity Crisis [PDF]
Geosciences, 2018 New geochronological investigations for the Slănic Formation, correlated with previous bio- and lithostratigaphical information, allow for a better succession of events for the Middle Miocene, including the absolute age of the Badenian salinity crisis in
Ana-Voica Bojar +5 more
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