Results 1 to 10 of about 393 (133)
Diversity and distribution patterns of the Oligocene and Miocene decapod crustaceans (Crustacea: Malacostraca) of the Western and Central Paratethys. [PDF]
Decapod associations have been significant components of marine habitats throughout the Cenozoic when the major diversification of the group occurred.
Hyžný M.
europepmc +2 more sources
Euryhaline preferences of the decapod crab <i>Mioplax socialis</i> enabled it to survive during the Badenian/Sarmatian extinction (Miocene) in the Central Paratethys. [PDF]
Although decapod crustaceans of the Central Paratethys were diverse during the Badenian (Langhian-Early Serravallian), a dramatic drop in their diversity occurred at the boundary with the Sarmatian.
Hyžný M +3 more
europepmc +2 more sources
A 13.06 Ma widespread ignimbrite in the Pannonian Basin captured a snapshot of shallow marine to coastal environment in Central Paratethys. [PDF]
Voluminous Miocene silicic volcanism sourced mainly from the extensional Pannonian Basin played a major role in the evolution of the Central Paratethys.
Karátson D +21 more
europepmc +2 more sources
Late Miocene megalake regressions in Eurasia. [PDF]
The largest megalake in the geological record formed in Eurasia during the late Miocene, when the epicontinental Paratethys Sea became tectonically-trapped and disconnected from the global ocean.
Palcu DV +6 more
europepmc +2 more sources
Past aridity and dust drove biodiversity crises and altered pollination in the ancient gymnosperm Ephedra (Gnetales). [PDF]
ABSTRACT The long‐term effects of present‐day climate change on pollination are unquantified. However, distinguishing climatic drivers of ancient changes in pollination could provide valuable insights into biotic responses to near‐future climate states.
Barbolini N +9 more
europepmc +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
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
A new Middle Miocene (Langhian - early Serravallian) assemblage with shark and ray teeth from Nyirád (Hungary, Transdanubia, Veszprém County) consists of nine families, with 15 different species. The assemblage shares many common genera with other Middle
Szabó Márton, Kocsis László
doaj +1 more source

