Results 31 to 40 of about 4,301,896 (195)
Reproductive phases of Miocene algae from central Paratethys and their bearing on systematics [PDF]
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 +1 more source
Middle Miocene (Badenian) chondrichthyan fossils collected from the Tekeres Schlieren Member of the Baden Formation at Tekeres (southern Hungary, Mecsek Mts) are described here.
M. Szabó +5 more
semanticscholar +1 more source
The Oligocene and Miocene tectonic and biogeographical alterations of the peri-Mediterranean area could strongly impact the speciation processes and migrations of Mediterranean sandfly species.
A. Trájer
semanticscholar +1 more source
Reshaping the understanding of the paratethys using paleogeographic reconstructions and geochronology studies [PDF]
The history of the Paratethys and its inhabiting organisms was profoundly influenced by its connections with the Global Ocean. As the sea‐straits linking Paratethys with the ocean expanded, they integrated the Paratethys with the global ocean, causing ...
Popov Sergey V. +2 more
doaj +1 more source
Litho- and biostratigraphic data are provided of 5 stratigraphic sections in Romania covering the “Badenian” marine flooding that occurred in the Central Paratethys during the middle Miocene (Langhian).
K. Sant +7 more
doaj +1 more source
Geology of the Čoka structure in northern Banat (Central Paratethys, Serbia)
Geology of the Čoka structure in northern Banat (Central Paratethys, Serbia)The Čoka structure is a fault-bounded anticline in northern Banat, in the southern part of the Neogene Pannonian Basin. The structure and its vicinity were explored by 24 wells.
Dejan Radivojević +2 more
openaire +1 more source
Otolith associations have been extensively described from the Badenian (Langhian to early Serravallian) of the Central Paratethys. During the late Badenian (early Serravallian), the basin was strongly segmented, and the faunal composition of its biota ...
Werner Schwarzhans
doaj +1 more source
The middle Miocene foraminifera and ostracod record of the Central Paratethys usually reflects stable normal marine epositional environments for the Badenian and more patchy, less stable restricted marine environments for the Sarmatian.
A. Szuromi-Korecz +6 more
semanticscholar +1 more source
New data on the stratigraphy of Badenian from Krčedin area (Northern Serbia, Central Paratethys) [PDF]
Badenian sediments are found for the first time in the surroundings of the Krcedin village. They represent remnants of the Central Paratethys marginal sea. The sediments are represented by a basal conglomerate unit overlain by pure and sandy marl. Foraminifera and rare ostracods are present, limited to the marls.
Anđelković, Filip +1 more
openaire +2 more sources
Upper Badenian diatom paleoecology of the western part of Central Paratethys
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 moderatelywarm water of depth less than 100 meters and of salinity above 30 ‰.The frequency of resting spores ...
openaire +2 more sources

