Results 21 to 30 of about 3,307 (160)

Geology of the Čoka structure in northern Banat (Central Paratethys, Serbia)

Geologica Carpathica, 2010
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, Ljupko Rundić, Slobodan Knežević   +2 more
openaire   +1 more source

First occurrences of Trionychidae (Testudines, Cryptodira) from the Miocene of Poland: Detailed cranial anatomy and biogeographic implications

Journal of Anatomy, EarlyView.
Fossil finds from three Middle Miocene sites in Poland reveal the northernmost known presence of trionychid turtles in Europe, tentatively identified as Trionyx cf. vindobonensis, suggesting a warmer climate that supported thermophilic species in Central Europe during this period. Abstract Modern trionychids (Testudines, Cryptodira) have a pan‐tropical
Yohan Pochat‐Cottilloux, Sergi López‐Torres, Milan Chroust, Georgios L. Georgalis, Marcin Górka, Mateusz Tałanda   +5 more
wiley   +1 more source

New data on the stratigraphy of Badenian from Krčedin area (Northern Serbia, Central Paratethys) [PDF]

Bulletin of the Natural History Museum, 2020
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, Batoćanin, Natalija   +1 more
openaire   +2 more sources

Depositional and stratigraphic evolution of a Permian megalake system: Implications for seiche‐influenced models

The Depositional Record, Volume 12, Issue 2, April 2026.
During the Late Permian, the rise of the Gondwanides Belt trapped marine waters, giving birth to a vast megalake. This lake shifted between overfilled, balanced‐fill and underfilled stages that are recorded by high‐frequency accommodation changes, while meteorological seiches shaped the sedimentary dynamic and produced heterolithic beds.
B. Christofoletti, L. V. Warren, F. G. Varejão, M. G. Rodrigues, M. G. Simões, D. V. Palcu, M. L. Assine   +6 more
wiley   +1 more source

Late Eocene bryozoan faunas in the Alpine-Carpathian region - a comparison [PDF]

, 1999
Twelve Priabonian (Late Eocene) bryozoan faunas of the Alps and Carpathians, collected from shallow to deep marine sediments, are compared by similarity indices.
Kázmér, Miklós, Zágorsek, Kamil
core  

The Messinian Salinity Crisis in the Dacic Basin (SW Romania) and early Zanclean Mediterranean-Eastern Paratethys high sea-level connection [PDF]

, 2011
International audienceNew field observations and fossil analyses complete and clarify the strong impact of the Mediterranean sea-level changes linked to the peak of the Messinian Salinity Crisis on the Dacic Basin in southwestern Romania.
Clauzon, Georges, Csato, Istvan, Do Couto, Damien, Macalet, Rodica, Melinte-Dobrinescu, M.C., Popescu, Speranta-Maria, Quillévéré, Frédéric, Rubino, Jean-Loup, Suc, Jean-Pierre   +8 more
core   +3 more sources

The Messinian Salinity Crisis Between Italy and Albania: The Peri‐Adriatic Depression and Southern Adriatic Basin Records

Basin Research, Volume 38, Issue 2, March/April 2026.
Basin‐scale correlation of Messinian salinity crisis (MSC) deposits across the Apennine–Albanide foreland basin system integrating outcrop and subsurface data. ABSTRACT We reconstructed the geological evolution of the Albanides during the Messinian salinity crisis (MSC), based on the integration of outcrop and subsurface data from both onshore (peri ...
Bigi Diego, Lugli Stefano, Manzi Vinicio, Roveri Marco, Milushi Ibrahim   +4 more
wiley   +1 more source

Palynomorphs of brackish and marine species in cores from the freshwater Lake Sapanca, NW Turkey [PDF]

, 2010
Lake Sapanca, which is located on the Sakarya–Sapanca–İzmit corridor in NW Turkey, is a freshwater lake with numerous fish farms in its catchment. Palynological analyses including non-pollen palynomorphs of a short (38.5 cm) and a longer sediment core ...
Aksu, Akçaalan, Albay, Albay, Anderson, Atkinson, Aykulu, Balık, Balon, Baykal, Bobat, Boettger, Gürbüz, Innal, İslamoğlu, Kouli, Kristiansen, Leroy, Leroy, Leroy, Leroy, Marret, Marret, Marret, McAndrews, Meriç Albay, Mertens, Morkoç, Mudie, Mudie, Mudie, Pfannenstiel, Polat, Rathje, Ryan, Ryan, Santamaría, Schwab, Schütt, Sorrel, Suzanne A.G. Leroy, Tanik, Traverse, Uğurlu, Vasiliev, Wall, Çelikkale, Özuluğ, Şahin, Şaşı   +49 more
core   +1 more source

Upper Badenian diatom paleoecology of the western part of Central Paratethys

Geologija, 2003
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

Sea Surface Temperature and Salinity Changes in the Easternmost Mediterranean During the Pre‐Evaporitic Messinian Controlled by the Restriction at Gibraltar

Paleoceanography and Paleoclimatology, Volume 41, Issue 1, January 2026.
Abstract During the latest Miocene, the Mediterranean Basin was affected by extreme paleoceanographic and paleoenvironmental changes culminating with evaporite (gypsum and halite) formation during the Messinian Salinity Crisis (MSC: 5.97–5.33 Ma).
F. Lanterna, W. Krijgsman, L. Lourens, A. Mulch, I. Vasiliev   +4 more
wiley   +1 more source