Results 11 to 20 of about 4,301,896 (195)
Stratigraphy revision of upper Badenian of Rakovica stream near Belgrade (Central Paratethys, Serbia) [PDF]
Belgrade area is a region of high paleobiodiversity, being ranked among the best known in Serbia. The prominent position among a number of Middle Miocene (Badenian) fossiliferous sites in the vicinity of Belgrade (southern Pannonian Basin, Central ...
Jovanović Gordana +2 more
doaj +3 more sources
The mid-Langhian flooding in the eastern Central Paratethys: integrated stratigraphic data from the Transylvanian Basin and SE Carpathian Foredeep [PDF]
The mid-Langhian (“Badenian”) flooding fully reconnected the semi-isolated Central Paratethys realm with the Mediterranean and, thereby, drastically changed the middle Miocene paleogeography of Central Europe. Due to the scattered stratigraphic record and scarcity of independent age constraints in some areas, the precise age and underlying mechanism ...
Sant K. +7 more
openaire +4 more sources
Morphometric divergence in Cyprideis (Ostracoda) during the Middle and Late Miocene of the Central Paratethys realm [PDF]
A morphometric outline analysis of the brackish-water ostracod Cyprideis examines a 2.0-million-year period during which the Central Paratethys region underwent significant geographic and environmental transformations.
R. Pipík, M. Gross, D. Starek
doaj +2 more sources
Badenian discoasters from the section in Lenart (Northeast Slovenia, Central Paratethys)
In Slovenske gorice, south of Lenart, a 20 m profile of Middle Miocene strata has been exposed. During previous research numerous discoasters have been found among other coccoliths.
Miloš Bartol, Jernej Pavšič
doaj +2 more sources
Uplift of the Tibetan Plateau, expansion/shrinkage of the Paratethys Sea, and global climate are three major forcings for central-east Asian climatic and environmental variations during the Cenozoic.
Benhong Guo +4 more
doaj +1 more source
The Late Miocene evolution of the Eastern Paratethys Sea was marked by significant palaeogeographical transformations. The knowledge of them should be improved with the information from the peripheral parts of this semi-enclosed marine basin.
Dmitry A. Ruban
doaj +1 more source
The Eocene-Oligocene climate transition in the Central Paratethys [PDF]
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 +4 more
openaire +2 more sources
Early and Middle Miocene dinoflagellate cyst stratigraphy of the Central Paratethys, Central Europe [PDF]
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 +2 more
openaire +2 more sources
Century of Laskarev's landmark contribution to Paratethys Science [PDF]
Laskarev’s seminal contribution to the recognition and elucidation of the Paratethys Sea within geological discourse stands as one of the pivotal milestones in our understanding of Neogene European paleogeography.
Radivojević Dejan +2 more
doaj +1 more source
The Dacian Basin was uniquely situated to record late Miocene hydrological changes that influenced depositional environments and faunal dispersal patterns in Central Eurasia's mega‐lake Paratethys.
Iuliana Vasiliev +10 more
doaj +1 more source

