Results 41 to 50 of about 2,766 (223)

The mid-Langhian flooding in the eastern Central Paratethys: integrated stratigraphic data from the Transylvanian Basin and SE Carpathian Foredeep [PDF]

International Journal of Earth Sciences, 2019
The mid-Langhian (“Badenian”) flooding fully reconnected the semi-isolated Central Paratethys realm with the Mediterranean and, thereby, drastically changed the middle Miocene paleogeography of Central Europe. Due to the scattered stratigraphic record and scarcity of independent age constraints in some areas, the precise age and underlying mechanism ...
Sant K., Palcu D. V., Turco E., Di Stefano A., Baldassini N., Kouwenhoven T., Kuiper K. F., Krijgsman W.   +7 more
openaire   +3 more sources

New data concerning the early middle miocene on the southern slopes of Fruška Gora (Northern Serbia): A case study from the Mutalj quarry [PDF]

, 2011
During the last few years, geological research at the southern slopes of Fruška Gora Mt. enabled the discovery of different Miocene units (undivided the Lower Miocene and Middle Miocene Badenian, predominantly). This is primarily thinking of the
Cvetkov Vesna, Knežević Slobodan, Rakijaš Milovan, Rundić Ljupko, Vasić Nebojša   +4 more
core   +1 more source

Rediscovering Globigerina bollii Cita and Premoli Silva 1960 [PDF]

Journal of Micropalaeontology
Globigerina bollii Cita and Premoli Silva was described from the historical Langhian-type section in Langhe, Piedmont (Italy). Due to its peculiar compact morphology, it was set apart from all the other globigerinids typical of the coeval Mediterranean ...
A. Fabbrini, A. Fabbrini, M. R. Petrizzo, I. P. Silva, L. M. Foresi, B. S. Wade   +5 more
doaj   +1 more source

Paleoenvironmental evolution of the Eastern Paratethys: Tracing the Tethys Ocean legacy through geochemical proxies

Chemical Geology
During the Oligocene to Miocene, the Paratethys Sea emerged as the northern offshoot of the Tethys Ocean, separated from the Mediterranean by the Alpine-Himalayan mountain range. Its history was characterized by the opening, restriction and closure of marine gateways, resulting in significant paleoenvironmental changes, including episodes of anoxia and
Palcu Rolier, Dan V., Liu, Zhanhong, Wei, Wei, Popov, Sergey, Golovina, Larisa, Vasiliev, Iuliana, Krijgsman, Wout, Algeo, Thomas   +7 more
openaire   +2 more sources

Quaternary time scales for the Pontocaspian domain: interbasinal connectivity and faunal evolution [PDF]

, 2019
The Pontocaspian (Black Sea - Caspian Sea) region has a very dynamic history of basin development and biotic evolution. The region is the remnant of a once vast Paratethys Sea.
Agustí, J., Aliyeva, E., Alçiçek, M. C., Bista, D., Bruch, A., Bukhsianidze, M., Büyükmeriç, Y., Danukalova, G., Flecker, R., Frolov, P., Hoyle, T. M., Jorissen, E. L., Kirscher, U., Koriche, S. A., Krijgsman, W., Kroonenberg, S. B., Lazarev, S., Lordkipanidze, D., Oms, O., Paleomagnetism, Paleomagnetism, Rausch, L., Singarayer, J., Stoica, M., Stratigraphy & paleontology, Stratigraphy and paleontology, Tesakov, A., Titov, V. V., Van Baak, C.G.C., van de Velde, S., Wesselingh, F. P., Yanina, T.   +31 more
core   +4 more sources

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

ON NEOGENE BIOSTRATIGRAPHY OF THE BORISPHEN GULF OF THE EASTERN PARATETHYS

Geological Journal, 2012
  New data about paleontological composition of Neogene deposits of Borisphen gulf (the Southern Ukraine, Zaporozhian and Cherssonian regions) are adduced. The Middle-, Upper Miocene and Pliocene presence is confirmed by macro- and microfauna; the Lower Miocene deposits (Mayachkian suite) have not fauna in situ.
BARG, I. M., IVANOVA, T. A., BONDAR, O. V., STARIN, D. A., SAPRONOVA, D. A.   +4 more
openaire   +3 more sources

Offshore Neopycnodonte oyster reefs in the Mediterranean Sea [PDF]

, 2020
© The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Angeletti, L., & Taviani, M. Offshore Neopycnodonte oyster reefs in the Mediterranean Sea. Diversity,
Angeletti, Lorenzo, Taviani, Marco
core   +1 more source

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

Караганский и конкский региоярусы Восточного Паратетиса: вопросы их объема и стратиграфической самостоятельности [PDF]

, 1994
Аналіз поглядів дослідників на об'єм та розчленування караганського і конкського регіоярусів Східного Паратетіса дозволив визначити взаємовідношення варненських (мелітопольських, ервілієвих), картвельських (фоладових), сартаганських, веселянських верств.
Вернигорова, Ю.В.
core   +6 more sources