Results 161 to 170 of about 1,320 (205)

Self-Pollinated Types and Ecological Adaptations of the Desert Plant <i>Gymnocarpos przewalskii</i>. [PDF]

Plants (Basel)
Jian J, Chai X, Zhao X, Yang Z.
europepmc   +1 more source

A reappraisal of Sarmatosminthus, the earliest member of lophocricetine jerboas (Rodentia, Dipodidae) from Eastern Europe

Delinschi A, Badea D, Vasilyan D, Ratoi B, Sinitsa MV.   +4 more
europepmc   +1 more source

Savanna ecosystems and mammalian adaptations in Mid-Miocene Northern China. [PDF]

Sci Rep
Li C, Wang SQ, Wang Y, Deng T, Ma J, Wang B, Jiangzuo Q, Sun D.   +7 more
europepmc   +1 more source

Middle Pleistocene tectonic events around the SE Aegean Sea: Insights from magnetostratigraphy, (U-Th)/He zircon dating, and fault kinematics in the Datça Graben (SW Türkiye). [PDF]

Sci Rep
İnce MD, Kaymakci N, Langereis C, Uzel B, Gülyüz E, Koralay EO, Stoica M, Sümer Ö.   +7 more
europepmc   +1 more source

Miocene connectivity between the Central and Eastern Paratethys: Constraints from the western Dacian Basin

Palaeogeography, Palaeoclimatology, Palaeoecology, 2014
The Dacian Basin formed an important link between the central and eastern parts of the Paratethys, a chain of late Tertiary inland seas and lakes. This study presents constraints on Miocene sea and lake level fluctuations in the Dacian Basin and on the connectivity between it and other Paratethys basins, based on the interpretation of seismic lines, a ...
Marten Ter Borgh, Marius Stoica, Marinus E Donselaar   +2 more
exaly   +4 more sources

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The age of the Sarmatian–Pannonian transition in the Transylvanian Basin (Central Paratethys)

Palaeogeography, Palaeoclimatology, Palaeoecology, 2010
A marked paleoenvironmental change took place at the beginning of the late Miocene in the Central Paratethys, with dominantly marine Sarmatian successions grading rapidly into mainly brackish Pannonian deposits. A long and excellently exposed section comprising the Sarmatian-Pannonian transition has been investigated at Oarba de Mure?
Iuliana Vasiliev, Sorin Filipescu, Wout Krijgsman   +2 more
exaly   +4 more sources

Tectono-climatic implications of Eocene Paratethys regression in the Tajik basin of central Asia

Earth and Planetary Science Letters, 2015
Plate tectonics and eustatic sea-level changes have fundamental effects on paleoenvironmental conditions and bio-ecological changes. The Paratethys Sea was a large marine seaway that connected the Mediterranean Neotethys Ocean with Central Asia during ...
Barbara Carrapa, Peter G Decelles, Nicoletta Mancin   +2 more
exaly   +2 more sources

Early diagenetic greigite as an indicator of paleosalinity changes in the middle Miocene Paratethys Sea of central Europe

Geochemistry, Geophysics, Geosystems, 2017
The Miocene epicontinental Paratethys Sea of central Eurasia has experienced multiple restriction and reconnection events to the open ocean. Magnetostratigraphy is an important dating tool to better understand the temporal and spatial paleoenvironmental ...
Suzhen Liu, Wout Krijgsman, Mark J Dekkers   +2 more
exaly   +3 more sources

Is there a Messinian unconformity in the Central Paratethys?

Stratigraphy, 2008
Since the conception of the Mediterranean Messinian Salinity Crisis model in the 1970s, regional unconformities as candidates for indicators of a correlative base level drop have been sought in the neighbouring Paratethyan basins. Some authors have suggested that seismic sections and borehole profiles from the Late Miocene to Pliocene lacustrine to ...
Imre Magyar, Orsolya Sztano
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Sarmatian (Late Middle Miocene) gastropod assemblages of the Central Paratethys

Facies, 2002
A rather diverse gastropod fauna from Sarmatian deposits of the Austrian/Hungarian Eisenstadt-Sopron Basin was studied. The fauna derives from two layers of clay and silt within a siliciclastic section at St. Margarethen in Burgenland (Austria). These layers are interpreted as littoral mudflats which formed during the Sarmatian (Late Middle Miocene ...
Mathias Harzhauser, Thorsten Kowalke
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