Results 181 to 190 of about 2,766 (223)

Trochidae (Gastropoda) from the Sarmatian Basin of the Eastern Paratethys

Paleontological Journal, 2017
The gastropod family Trochidae from the Sarmatian deposits of the Eastern Paratethys is described in detail. Detailed faunal characteristics of 22 Sarmatian sections in Volyn–Podolia, Moldova, southern Ukraine, and Crimea, some of which have yielded the material of this study, are provided.
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Lower miocene sediments of the Maikop group in the Central Eastern Paratethys

Lithology and Mineral Resources, 2006
The composite section of upper Maikop sediments compiled for the central part of the Eastern Paratethys is presented. The section (more than 1000 m) comprises the Karadzhalgan, Sakaraulian, and Kotsakhurian regional stages. The lower boundary of the Miocene drawn at the base of the Karadzhalgan regional stage is unambiguous only in the southern part of
A. S. Stolyarov, E. I. Ivleva
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On the miocene centracanthidae (Teleostei, Perciformes) from the eastern Paratethys

Paleontological Journal, 2006
A new genus, Naslavcea, is erected for the Middle Miocene species Spicara fundata Bannikov, 1990 (Centracanthidae) from the Lower Sarmatian of northern Moldova. This genus is characterized by the relatively small number of rays in the dorsal and anal fins.
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Miocene vegetation and climate dynamics in Eastern and Central Paratethys (Southeastern Europe)

Palaeogeography, Palaeoclimatology, Palaeoecology, 2011
Abstract From the Cretaceous to modern time the earth's climate system has changed repeatedly from a greenhouse to an icehouse. The Miocene appeared as the last warm episode in earth history, prior to the establishment of large Northern Hemisphere ice sheets.
Dimiter Ivanov, Torsten Utescher, Volker Mosbrugger, Svetlana Syabryaj, Desa Djordjević-Milutinović, Serge Molchanoff   +5 more
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Gigantic eruption of a Carpathian volcano marks the largest Miocene transgression of Eastern Paratethys

Earth and Planetary Science Letters, 2021
Abstract Volcanic ash layers (tephras) dispersed over large areas may offer important time markers in the geological record provided their age and geochemical fingerprint can be established. Accurately dated and geochemically characterized tephras are essential in correlation of temporally and spatially discontinuous geological records, which is key ...
Martin Danišík, Vera Ponomareva, Maxim Portnyagin, Sergey Popov, Andrei Zastrozhnov, Christopher L. Kirkland, Noreen J. Evans, Evgeny Konstantinov, Folkmar Hauff, Dieter Garbe-Schönberg   +9 more
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Maeotian mammalian localities of Eastern Paratethys: Magnetochronology and position in European continental scales

Stratigraphy and Geological Correlation, 2008
The Maeotian of Eastern Paratethys corresponds to the interval of the magnetochronological scale from the base of the subchron C4Ar2n to upper parts of the Chron C4n (9.6–7.5 Ma). Fission-track dates of Maeotian deposits are in general agreement with paleomagnetic chronology.
E. A. Vangengeim, A. S. Tesakov
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Morphogenesis of rissoidae in the inland basins of the Eastern Paratethys

Paleontological Journal, 2006
Miocene rissoids from the heterochronous low-salinity seas of the Eastern Paratethys (Early Chokrakian, Karaganian, Late Konkian, Early Sarmatian, and Early Maeotian) were revised. The polyphyletic genus Mohrensternia is subdivided into several generic and subgeneric taxa.
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Middle–Late Miocene Paleogeography of the Eastern Paratethys. Part II. Tarkhanian Basin: Stratigraphy, Facies, Paleogeography and Biota

Stratigraphy and Geological Correlation
Abstract—: The rich benthic fauna and the composition of phyto- and zooplankton, indicate that the Tarkhanian basin had open connections with the World Ocean. These connections existed both in the west of the region–with the Early Badenian Sea, and in Transcaucasia–with the Central Iranian and Anatolian basins.
Popov, S. V., Goncharova, I. A., Golovina, L. A., Pinchuk, T. N., Palcu, D. V., Akhmetiev, M. A., Zastrozhnov, A. S.   +6 more
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Cyclostratigraphy of Pontian deposits of the Eastern Paratethys (Zheleznyi Rog section, Taman Region)

Moscow University Geology Bulletin, 2014
The first data on the cyclostratigraphy of Pontian deposits of the Eastern Paratethys were obtained by studying the magnetic susceptibility of Upper Miocene rocks of the Zheleznyi Rog section in the Taman Region. Based on statistical methods, using the Lomb-Scargle and REDFIT periodograms, cycles related to long-period insolation oscillations ...
Yu. V. Rostovtseva, A. I. Rybkina
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Strontium isotope ratios of the Eastern Paratethys during the Mio-Pliocene transition; Implications for interbasinal connectivity

Earth and Planetary Science Letters, 2010
Paratethys represents the large basin that extended from central Europe to inner Asia, comprising the North Alpine foreland, Pannonian and Dacian basins, the Black Sea and Caspian Sea. Connectivity between these subbasins and the connectivity of Paratethys with the open ocean varied drastically because of pervasive tectono-climatic processes affecting ...
Vasiliev, I., Reichart, G.-J., Davies, G.R., Krijgsman, W., Stoica, M.   +4 more
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