Results 21 to 30 of about 1,320 (205)

Distephanopsis concavus Horvat: a revised silicoflgellate species from the Middle Miocene of the Central Paratethys

Geologija, 2016
The silicoflgellate species Distephanopsis concavus Horvat is revised based on further research of the type material. This species is characterized by having a basal ring with strongly concave sides which reduce the basal ring area and by four symmetry
Aleksander Horvat
doaj   +2 more sources

Badenian discoasters from the section in Lenart (Northeast Slovenia, Central Paratethys)

Geologija, 2005
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

Expansion/shrinkage history of the Paratethys Sea during the Eocene: New insights from eolian Red Clay records in the Altyn Mountains, northern China

Frontiers in Earth Science, 2022
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, Junsheng Nie, Jianxing Li, Wenjiao Xiao, Feng Pan   +4 more
doaj   +1 more source

The Tanais Bay of the Eastern Paratethys Sea at the Sarmatian–Maeotian Transition (Late Miocene): Widespread Desiccations and Local Uplifts in the Light of Historical Information

Journal of Marine Science and Engineering, 2022
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]

Geološki Anali Balkanskoga Poluostrva
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, Kovačić Marijan, Magyar Imre   +2 more
doaj   +1 more source

Hydrological Changes in Restricted Basins: Insights From Strontium Isotopes on Late Miocene‐Pliocene Connectivity of the Eastern Paratethys (Dacian Basin, Romania)

Geochemistry, Geophysics, Geosystems, 2021
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, Marius Stoica, Arjen Grothe, Sergei Lazarev, Dan Valentin Palcu, Christiaan vanBaak, Arjan DeLeeuw, Francesca Sangiorgi, Gert‐Jan Reichart, Gareth R. Davies, Wout Krijgsman   +10 more
doaj   +1 more source

Mediterranean-Paratethys connectivity during the Messinian salinity crisis: The Pontian of Azerbaijan [PDF]

, 2016
Prior to the onset of the Messinian Salinity Crisis, a connection was established between the Mediterranean Sea and the Paratethys region to the north.
Aliyeva, Elmira, van Baak, Christiaan G C, NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia, Stoica, Marius, Grothe, Arjen, Krijgsman, Wout, Paleomagnetism   +6 more
core   +1 more source

The Badenian-Sarmatian Extinction Event in the Carpathian foredeep basin of Romania: Paleogeographic changes in the Paratethys domain [PDF]

, 2015
The Badenian-Sarmatian boundary interval is marked by a major extinction event of marine species in the Central Paratethys. The exact age of the boundary is debated because many successions in marginal basins show erosional features and fauna reworking ...
Krijgsman, Wout,, Kouwenhoven, Tanja J., Bartol, Milos,, Krijgsman, Wout, Stratigraphy and paleontology, Tulbure, Maria, Palcu, Dan V., Tulbure, Maria,, Kouwenhoven, Tanja J.,, NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia, Palcu, Dan V.,, Bartol, Milos, Paleomagnetism   +12 more
core   +1 more source

Mediterranean outflow pump:An alternative mechanism for the Lago-mare and the end of the Messinian Salinity Crisis [PDF]

, 2016
The final stage of the Messinian Salinity Crisis (MSC) is characterized by brackish water “Lago-mare” conditions in the intermediate and marginal basins of the Mediterranean Sea.
Lunt, Daniel J., van Baak, Christiaan G.C., NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia, Marzocchi, Alice, Krijgsman, W, Lunt, Dan, Krijgsman, Wout, Paleomagnetism, Flecker, Rachel   +8 more
core   +1 more source

A MIDDLE MIOCENE BALEEN WHALE FROM BELE VODE IN BELGRADE, SERBIA

Rivista Italiana di Paleontologia e Stratigrafia, 2018
There was a fauna of baleen whales (Cetacea: Mysticeti) in the Central Paratethys, a Miocene water body which covered the area of present-day Central Europe.
PAVEL GOL’DIN, PREDRAG RADOVIĆ
doaj   +1 more source