Results 61 to 70 of about 1,534 (197)
Sulphur isotopes in anhydrites from Badenian (Middle Miocene) salts of Hrynivka area (Ukrainian Carpathian Foredeep) [PDF]
Ten new determinations of the stable sulphur isotope content of anhydrite from Badenian rock salt in the Hrynivka 525 borehole (Ukrainian Carpathian Foredeep) show that δ34S values in anhydrite range from +20.2 to +22.7‰ and the average value of δ34S is +
Bukowski, K., Meng, F., Galamay, A. R.
core +1 more source
Multiple transitions between realms shape relict lineages of Proteus cave salamanders
Abstract In comparison to biodiversity on Earth's surface, subterranean biodiversity has largely remained concealed. The olm (Proteus anguinus) is one of the most enigmatic extant cave inhabitants, and until now little was known regarding its genetic structure and evolutionary history.
H. Recknagel +4 more
wiley +1 more source
The Badenian/Sarmatian environment on the edge of the Pannonian Basin System [PDF]
The Badenian/Sarmatian succession of Hrvatska Kostajnica, exposed due to a landslide on the eastern slopes of Kubarnovo brdo hill, was investigated for its sedimentological and paleontological features. Marly sediments from the newly formed outcrop originated from the southwestern marginal part of the Pannonian Basin System (PBS), which was one of the ...
Grizelj, Anita +10 more
openaire
Badenian (Middle Miocene) calcareous nannofossils from Paglisa (Cluj district): biostratigraphical importance [PDF]
The calcareous nannofossils from the Middle Miocene (Badenian) formations from Pâglişa (Cluj district) are typical for the Lower and Middle Badenian, respectivelly Moravian and Wielician (or Langhian).
Chira, Carmen +2 more
core +1 more source
Abstract Nubecularia bioherms represent unique bioconstructions that are restricted to the upper Serravallian of the Paratethys and have been reported since the 19th century. They occur in the Central Paratethys in the late Sarmatian and the Eastern Paratethys in the Bessarabian both regional stages of the respective Paratethyan areas.
Werner E. Piller, Mathias Harzhauser
wiley +1 more source
By revisiting three decades of molecular data, we retraced the evolution and mapped the diversity of Pelophylax water frogs, a famous group of Eurasian amphibians. The results highlight the Paratethys Paleo‐sea as a major driver of diversification, implement a new timetree validation approach, emphasize the rare ability of lineages to hybridize despite
Christophe Dufresnes +9 more
wiley +1 more source
In the area of Medvednica Mt., the Upper Badenian and Sarmatiandeposits are divided into four facies associations: (A) deposits of asmall carbonate platform represented by breccia, conglomerates, biocalcirudites,biocalcarenites and biocalclutites; (B ...
Davor Vrsaljko +8 more
doaj +1 more source
Gravity inversion by second order approximation applied to the Styrian Basin (Austria)
Abstract An approximative second order gravity inversion scheme by a truncated power series expansion is applied to derive the thickness of the Neogene, mostly clastic, sedimentary section of the Styrian Basins in South–East Austria, which are sub‐basins of the Pannonian Basin System.
Harald Granser
wiley +1 more source
Middle Miocene Volcanic Flare‐up Preceding and Synchronous with the Langhian/Serravallian Sea Level Decline in the North Pannonian Basin. The top part of the graphical abstract depicts a geological overview of the Pannonian Basin System, featuring the Danube Basin within it.
Samuel Rybár +4 more
wiley +1 more source
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

