Results 51 to 60 of about 4,301,896 (195)
Massive evaporites were discovered in the Soltvadkert Trough (Great Plain, Hungary) correlating to the Badenian Salinity Crisis (13.8 Ma, Middle Miocene) on the basis of nannoplankton and foraminifera biostratigraphy.
Báldi Katalin +5 more
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Upper Badenian diatom paleoecolgy of the western part of Central Paratethys
In the western part of Central Paratethys, on the territory of Slovenia, the Upper Badenian diatoms occur only in the Kr{ko basin. The diatom paleoecology of the Upper Badenian beds suggests their deposition in the marine littoral, in warm to ...
Aleksander Horvat
doaj
Middle and Late Miocene palynological biozonation of the south-western parts of Central Paratethys (Croatia) is presented based on organic-walled phytoplankton.
Koraljka Bakrač +2 more
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Lower Miocene fishes and turtle from Žvarulje near Mlinše, Slovenia (Central Paratethys)
The article discusses fossil finds of Miocene vertebrates from the vicinity of Žvarulje near Mlinše in Central Slovenia. The fossils were found in the Lower Miocene Govce formation. Most common in the assemblage were tooth coronas, usually without their root parts of cartilaginous fishes, belonging to the genera Notorynchus, Carcharias, Cosmopolitodus,
Vasja Mikuž, Aleš Šoster
openaire +2 more sources
Silicified wood remains, especially redeposited driftwood, are relatively abundant in the Central Paratethys upper Oligocene (Egerian) to lower Miocene (Eggenburgian) fluviatile St.
Fritz F. Steininger +2 more
semanticscholar +1 more source
Ar-40/Ar-39 radio-isotopic dating of volcanic tuffs intercalated in sediments can provide high accuracy age control on the deposition of sedimentary rocks.
K. Sant +9 more
semanticscholar +1 more source
Fossils from the Upper Miocene (Pannonian) sands of the Pécsvárad sand pit (Eastern Mecsek Mts., SW Hungary) [PDF]
The Mecsek Mountains in SW Hungary represent an uplifted basement block of the Pannonian Basin. Their Neogene cover includes deposits both from the Middle Miocene Central Paratethys and from its Late Miocene (Pannonian) brackish‐water descendant, Lake ...
Sebe Krisztina +5 more
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The Badenian/Sarmatian boundary in the Central Paratethyan basins is characterised by a change from open marine conditions during the late Badenian to the assumed brackish conditions during the early Sarmatian. The foraminiferal and palynological results
D. Peryt +4 more
semanticscholar +1 more source
The geographic distribution of Crocodylia in Europe throughout the Cenozoic experienced fluctuations in the extension of its northern limit. Whereas crocodylians reached very high latitudes during the early Eocene (78ºN), their northward extension was ...
Marcin Górka +5 more
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In the present paper we report on several new specimens of Jaxea kuemeli Bachmayer, 1954 from the Middle Miocene laminated sandstones from Košiše in Tunjice Hills. New and well-preserved material from shallow water environment of Laško Formation allows
Rok Gašparič, Matúš Hyžný
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