Results 1 to 10 of about 1,320 (205)

Abstract: Post-Cimmerian (Jurassic) Petroleum Systems of the Central Paratethys Region

AAPG Bulletin, 1999
openaire   +1 more source

Foraminifera and calcareous nannoplankton from the "Rzehakia (Oncophora) Beds" in the Central Paratethys

Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 2001
openaire   +1 more source

The Central Paratethys Sea – Part of the tropical eastern Atlantic rather than gate into the Indian Ocean

Global and Planetary Change
Mathias Harzhauser, Bernard Landau, Oleg Mandic   +2 more
exaly  

Drilling predation in molluscs from the Early and Middle Miocene of the Central Paratethys.

Palaios, 2011
Sawyer, Jennifer, Zuschin, Martin
openaire   +1 more source

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
doaj   +7 more sources

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
doaj   +3 more sources

Reproductive phases of Miocene algae from central Paratethys and their bearing on systematics [PDF]

Acta Palaeontologica Polonica, 2019
Coralline algae were widespread in shallow-water environments during the middle Miocene in the central Paratethys. Their distribution and diversity patterns are useful in paleoenvironmental and paleoclimatic studies providing that species identifications
Juraj Hrabovský
doaj   +5 more sources

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.
europepmc   +3 more sources

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, Mandic Oleg, Harzhauser Mathias, Ledvák Peter   +3 more
doaj   +2 more sources

A 13.06 Ma widespread ignimbrite in the Pannonian Basin captured a snapshot of shallow marine to coastal environment in Central Paratethys [PDF]

Scientific Reports
Voluminous Miocene silicic volcanism sourced mainly from the extensional Pannonian Basin played a major role in the evolution of the Central Paratethys.
Dávid Karátson, Pierre Lahitte, Maxim Portnyagin, Márton Palotai, Sándor Józsa, Emő Márton, Emőke Tóth, Boglárka Erdei, Sébastien Nomade, Károly Németh, Levente Iván, Márton Krasznai, Fanni Vörös, Tamás Biró, Jean-Louis Paquette, Lilla Hably, János Hír, Péter Prakfalvi, János Kiss, Zoltán Pécskay, Daniel A. Frick, Mátyás Hencz   +21 more
doaj   +2 more sources