Bádeni foraminiferák kvantitatív paleökológiai vizsgálata és stabil izotópos (d18O, d13C) elemzése: Paratethys paleóceanológia, paleoklíma = The quantitative paleoecological analysis of Badenian foraminifera and its stable isotope composition (d18O, d13C): paleooceanology of the Paratethys, paleoclimate [PDF]
, 2007 A kutatás célja a középső miocén Paratethys paleoóceanológiájának jobb megismerése volt a klímakutatásban használt proxik (angol proxy) segítségével. A levont következtetések nem csupán a foraminiferák kvantitatív vizsgálatára alapultak, hanem független ...
Báldi, Katalin
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The relative roles of CO2 and palaeogeography in determining Late Miocene climate: results from a terrestrial model-data comparison [PDF]
, 2012 The Late Miocene (∼11.6–5.3 Ma) palaeorecord provides evidence for a warmer and wetter climate than that of today and there is uncertainty in the palaeo-CO2 record of at least 150 ppmv.
Bradshaw, Catherine +6 more
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A brachiopodák faunafejlődése Magyarországon a kréta végétől a miocénig (rendszertan, paleoökológia, paleobiogreográfia) = Faunal changes of brachiopods in Hungary from the Late Cretaceous to the Miocene (systematics, paleoecology, paleobiogeography) [PDF]
, 2011 Paleogén és neogén brachiopodákat vizsgáltam különböző hazai és külföldi lelőhelyekről. Monospecifikus paleocén együttest írtunk le Ausztriából (új nemzetség, új faj). Hét hazai eocén felszíni feltárás és 7 mélyfúrás alapján 6 nemzetség 7 faját írtuk le (
Dulai, Alfréd, Tóth, Emőke
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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
Geologica Carpathica, 2017 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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New and little-known Cheilostomata (Bryozoa, Gymnolaemata) from the NE Atlantic [PDF]
, 2013 Based on newly designated type material, four poorly known NE Atlantic cheilostome bryozoan species are redescribed and imaged: Cellaria harmelini d’Hondt from the northern Bay of Biscay, Hippomenella mucronelliformis (Waters) from Madeira, Myriapora ...
Berning, Björn
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Traces of drilling predation in the Badenian Mollusks from the Rakovica stream (Belgrade, Serbia)
Geologia Croatica, 2016 The palaeoecology of fossil molluscs of Serbia is insufficiently studied. Drilling predation indicatesinteractive relationships among Middle Miocene Badenian molluscs from the Rakovicasands. These sands are present in the Rakovica stream valley (southern
Meri Ganić +4 more
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Fish otoliths from the Late Oligocene (Eger and Kiscell Formations) in the Eger area (northeastern Hungary) [PDF]
, 1994 Otoliths collected from the Late Oligocene of the Eger area revealed the presence of 52 teleost taxa from subtropical to warm temperate waters. Two successive faunas, which have only three species in common, are identified: the Kiscell Clay fauna ...
Brzobohaty, R., Nolf, D.
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Geologija, 2015 In this paper we report new specimens of an interesting Paratethyan decapod Styrioplax exiguus Glaessner, 1928, which extend the known palaeogeographic and stratigraphic distribution of the species.
Rok Gašparič, Eva Halásová
doaj +1 more source
The Palaeogeography of Lake Pannon During Deposition of the Congeria rhomboidea Beds [PDF]
, 2001 Lake Pannon covered the area of the Pannonian Basin during the late Miocene. According to the seismic profiles, prograding deltas from the NW and NE resulted in the S-SE migration of the northern palaeoshoreline and the gradual aggradation of the ...
S. Gulyas Jr.
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