Results 11 to 20 of about 1,320 (205)

Early and Middle Miocene dinoflagellate cyst stratigraphy of the Central Paratethys, Central Europe [PDF]

Journal of Micropalaeontology, 2006
Abstract. Marine organic-walled dinoflagellate cysts have been studied from the Early and Middle Miocene of the Central Paratethys in Austria (Vienna and eastern Alpine Foreland basins) and Hungary (Pannonian Basin), and compared with assemblages of similar age from the Atlantic Ocean and Mediterranean Sea.
Jiménez-Moreno, Gonzalo, Head, Martin J., Harzhauser, Mathias   +2 more
openaire   +3 more sources

Towards better correlation of the Central Paratethys regional time scale with the standard geological time scale of the Miocene Epoch

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, Halásová Eva, Hudáčková Natália, Holcová Katarína, Hyžný Matúš, Jamrich Michal, Ruman Andrej   +6 more
doaj   +3 more sources

The Eocene-Oligocene climate transition in the Central Paratethys [PDF]

Palaeogeography, Palaeoclimatology, Palaeoecology, 2016
Abstract We studied two boreholes (Cserepvaralja-1 and Kiscell-1) with continuous sedimentary records across the Eocene-Oligocene climate transition from the Central Paratethyan area. Assemblages of benthic foraminifera display a shift in dominance by epifaunal taxa in the late Eocene to shallow and deep infaunal taxa in the early Oligocene.
Péter Ozsvárt, László Kocsis, Anita Nyerges, Orsolya Győri, József Pálfy   +4 more
openaire   +4 more sources

A new Middle Miocene selachian assemblage (Chondrichthyes, Elasmobranchii) from the Central Paratethys (Nyirád, Hungary): implications for temporal turnover and biogeography

Geologica Carpathica, 2016
A new Middle Miocene (Langhian - early Serravallian) assemblage with shark and ray teeth from Nyirád (Hungary, Transdanubia, Veszprém County) consists of nine families, with 15 different species. The assemblage shares many common genera with other Middle
Szabó Márton, Kocsis László
doaj   +2 more sources

The Central Paratethys Sea-rise and demise of a Miocene European marine biodiversity hotspot. [PDF]

Sci Rep
AbstractThe 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, Landau B, Mandic O, Neubauer TA.   +3 more
europepmc   +5 more sources

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, Irina Stanislavovna Patina, Ionuț Șandric, Sergei Lazarev, Iuliana Vasiliev, Marius Stoica, Wout Krijgsman   +6 more
doaj   +2 more sources

Oligocene archaeomonad stomatocysts from the Polish Central Paratethys

Acta Palaeontologica Polonica
An 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, James M. Ehrman, Brajogopal Samanta   +2 more
doaj   +2 more sources

Upper Badenian diatom paleoecolgy of the western part of Central Paratethys

Geologija, 2003
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   +1 more source

Middle and Late Miocene palynological biozonation of the south-western part of Central Paratethys (Croatia)

Geologia Croatica, 2012
Middle and Late Miocene palynological biozonation of the south-western parts of Central Paratethys (Croatia) is presented based on organic-walled phytoplankton.
Koraljka Bakrač, Georg Koch, Jasenka Sremac   +2 more
doaj   +3 more sources

Cretaceous-Paleogene evolution of the proto-Paratethys Sea in Central Asia

, 2020
Unlike today’s prevailing terrestrial features, the geologic past of Central Asia witnessed marine environments and conditions as well. A vast, shallow sea, known as proto-Paratethys, extended across Eurasia from the Mediterranean Tethys to the Tarim Basin in western China during Cretaceous to Paleogene times.
Kaya, Mustafa
core   +4 more sources