Results 41 to 50 of about 4,301,896 (195)

Revised Middle Miocene datum for initial marine flooding of North Croatian Basins (Pannonian Basin System, Central Paratethys)The Pannonian Basin System (PBS) originated during the Early Miocene as a result of extensional processes between the Alpine-Carp

Geologia Croatica, 2011
The Pannonian Basin System (PBS) originated during the Early Miocene as a result of extensional processes between the Alpine-Carpathian and the Dinaride Orogenic Belts.
Stjepan Ćorić, Davor Pavelić, Fred Rögl, Oleg Mandic, Sejfudin Vrabac, Radovan Avanić, Lazar Jerković, Alan Vranjković   +7 more
doaj   +1 more source

Timing of the Middle Miocene Badenian Stage of the Central Paratethys

Geologica Carpathica, 2014
Abstract A new and precisely defined chronometric subdivision of the Badenian (Middle Miocene, regional stage of Central Paratethys) is proposed. This uses global events, mainly geomagnetic polarity reversals as correlated chronometric boundaries, supported by climatic and sea-level changes in addition to isotope events and biostratigraphic data ...
Hohenegger, Johann, Coric, Stjepan, Wagreich, Michael   +2 more
openaire   +1 more source

Tidal deposits in the Early Miocene Central Paratethys: the Vučji Jarek and Čemernica members of the Macelj formation (NW Croatia)

, 2021
The Macelj formation is an informal Eggenburgian-early Ottnangian lithostratigraphic unit that is established in the area of the Hrvatsko Zagorje Basin, which represented a marginal zone of the Early Miocene Central Paratethys Sea.
Radovan Avanić, D. Pavelić, Z. Pécskay, Mirjana Miknić, D. Tibljaš, L. Wacha   +5 more
semanticscholar   +1 more source

Porgy fish teeth in Miocene marl from Mastni hrib near Škocjan, Slovenia

Geologija, 2014
The article discusses fossil porgy fish teeth found in Middle Miocene (Badenian) sandy marl from Mastni hrib near Škocjan in Dolenjska. The teeth belong to the species Pagrus cinctus (Agassiz, 1836) and represent the first find in the Krka basin.
Vasja Mikuž, Miloš Bartol, Aleš Šoster   +2 more
doaj   +1 more source

A new clupeoid genus from the Oligocene of Central Paratethys (Menilite Formation, Poland)

Acta geologica Polonica
The Suborder Clupeoidei Bleeker, 1859 comprises mostly marine fishes, which form large schools feeding on plankton. The fossil record of the suborder in the Late Paleogene reveals that clupeoids were abundant in the Western, Central, as well as Eastern ...
Mateusz Granica, M. Bienkowska-Wasiluk, M. Pałdyna   +2 more
semanticscholar   +1 more source

Sarmatian molluscs from site Osek-1 in Slovenske gorice, Slovenia

Geologija, 2015
This article is a contribution to the taxonomical investigation of Middle Miocene (Sarmatian) molluscs from section (fossil site) Osek-1 at Spodnji Osek (Slovenske gorice) in the Mura-Zala basin on western margin of Central Paratethys.
Vasja Mikuž, Matija Križnar
doaj   +1 more source

The Badenian/Sarmatian (Middle Miocene) boundary in the Central Paratethys (Kreminna, western Ukraine): Foraminiferal and palynological evidence

Geological Quarterly
The Badenian/Sarmatian boundary in the Paratethys basin, that marks the transition from normal marine to restricted semi-marine conditions due to isolation of the basin from the world ocean at the onset of Sarmatian time, is still far from being fully ...
D. Peryt, P. Gedl, M. Jasionowski, T. Peryt, A. Poberezhskyy   +4 more
semanticscholar   +1 more source

FISH OTOLITHS AND FORAMINIFERA FROM THE BORSKÝ MIKULÁŠ SECTION (SLOVAKIA, MIDDLE MIOCENE, UPPER BADENIAN, VIENNA BASIN) AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE

Rivista Italiana di Paleontologia e Stratigrafia, 2022
Thirty-eight otolith-based species of fishes and 41 foraminifera species have been recorded in the Borský Mikuláš-Vinohrádky section in the upper Badenian deposits in the eastern part of the Vienna Basin, in West Slovakia.
Rostislav Brzobohaty, BARBARA ZAHRADNÍKOVÁ, NATÁLIA HUDÁČKOVÁ   +2 more
doaj   +1 more source

Silicoflagellates and other siliceous micro- and nannofossils from Rupelian diatomites, southeastern Poland

Plant and Fungal Systematics
The Eocene-Oligocene Transition is one of the major stages of the Cenozoic reshaping of the world oceans with associated changes in climate, of ocean coastlines and circulation patterns.
Irena Kaczmarska, James M. Ehrman
doaj   +1 more source

REEFS AND BIOACCUMULATIONS IN THE MIOCENE DEPOSITS OF THE NORTH CROATIAN BASIN – AMAZING DIVERSITY YET TO BE DESCRIBED

Rudarsko-geološko-naftni Zbornik, 2016
During the early stages of the Middle Miocene transgression marine biota invaded the newly formed Paratethys Sea. Reefs and reef-like structures particularly flourished with life, supported by the favourable climate conditions.
Jasenka Sremac, Marija Bošnjak Makovec, Davor Vrsaljko, Bojan Karaica, Kristina Tripalo, Karmen Fio Firi, Ana Majstorović Bušić, Tihomir Marjanac   +7 more
doaj   +1 more source