Results 151 to 160 of about 4,301,896 (195)
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Geological Journal, 2020
The study of pollen spectra mirrors the evolution of landscape and climatic changes in the northwestern part of Central Paratethys domain during the regional stages Karpatian–Badenian (Late Burdigalian–Langhian to Early Serravalian; NN4‐NN6 biozone ...
N. Doláková +2 more
semanticscholar +1 more source
The study of pollen spectra mirrors the evolution of landscape and climatic changes in the northwestern part of Central Paratethys domain during the regional stages Karpatian–Badenian (Late Burdigalian–Langhian to Early Serravalian; NN4‐NN6 biozone ...
N. Doláková +2 more
semanticscholar +1 more source
Bollettino Malacologico
A new Middle Miocene Central Paratethyan gastropod of the family Architectonicidae Gray, 1850, Heliacus stefanmeszarosi spec. nov. is described. This small-sized architectonicid was recorded from the Upper Badenian (Serravallian) sandy marine deposits of
Radoslav Biskupič
semanticscholar +1 more source
A new Middle Miocene Central Paratethyan gastropod of the family Architectonicidae Gray, 1850, Heliacus stefanmeszarosi spec. nov. is described. This small-sized architectonicid was recorded from the Upper Badenian (Serravallian) sandy marine deposits of
Radoslav Biskupič
semanticscholar +1 more source
Paleogeography of the Central Paratethys during the Karpatian and Badenian
2004The Karpatian and Badenian paleogeography is descibed.
Bajraktarević, Zlatan +2 more
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Miocene vegetation and climate dynamics in Eastern and Central Paratethys (Southeastern Europe)
Palaeogeography, Palaeoclimatology, Palaeoecology, 2011Abstract From the Cretaceous to modern time the earth's climate system has changed repeatedly from a greenhouse to an icehouse. The Miocene appeared as the last warm episode in earth history, prior to the establishment of large Northern Hemisphere ice sheets.
Dimiter Ivanov +5 more
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Provenance of the Miocene Slovenj Gradec Basin sedimentary fill, Western Central Paratethys
Sedimentary Geology, 2018Abstract The Slovenj Gradec Basin represents one of the marginal western basins of the Neogene Pannonian Basin system. Its sedimentary succession is investigated by combination of field, petrographic and geochemical methods. The succession is at least 540 m thick and characterised by frequent alternation of conglomerate, sandstone, siltstone and ...
Kristina Ivančič +3 more
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A Primitive Seal (Mammalia: Phocidae) from Early Middle Miocene of Central Paratethys
2002A well-preserved skull from the early middle Miocene (approximately 15 Ma) at Devinska Nova Ves (formerly Neudorf an der March), Slovakia, herein named <i>Devinophoca claytoni</i>, new genus and new species, is morphologically the closest common ancestor of all true seals. It shows a mixture of subfamilial characters.
Irina A. Koretsky, Peter Holec
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Long-lived brackish water lake in the Central Paratethys backyard
2017Along Mt. Požeška, an inselberg in NE Croatia, the continental Lower to Middle Miocene deposits are widespread. These deposits are present in many outcrops, sections and boreholes, always underlying the Middle Miocene marine series. The present locality provides insight to fossil assemblages and depositional environments of the Mt. Požeška paleolake.
Bakrač, Koraljka +4 more
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Journal of nannoplankton research, 2004
Endemical forms are restricted by changed salimity conditions.
Pavelić, Davor +2 more
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Endemical forms are restricted by changed salimity conditions.
Pavelić, Davor +2 more
openaire +2 more sources
Marine shelled Heterobranchia in part (Gastropoda) of the Miocene Central Paratethys Sea
ZootaxaWe present a revision of the Early and Middle Miocene marine heterobranchs from the European Central Paratethys Sea. We document a surprisingly high diversity of 83 species of which 32 species are described as new species.
M. Harzhauser +2 more
semanticscholar +1 more source
Disintegration of the Central Paratethys and origin of the Lake Pannon
2017U poglavlju je opisan stotinjak metara debeli slijed naslaga na kopu Vranović u cementari u Našicama. Donjih petnaestak metara slijeda pripada najmlađim srednjemiocenskim marinskim sedimentima, a sadrži i sloj tufa. Ostatak slijeda koji je kontinuirano taložen na sarmatske sedimenta, čine vapnenci i lapori mlađeg miocena koji su taloženi u boćatom ...
Bakrač, Koraljka +5 more
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