scholarly journals Hydrological changes in restricted basins: insights from strontium isotopes on late Miocene‐Pliocene connectivity of the Eastern Paratethys (Dacian Basin, Romania)

2021 ◽  
Author(s):  
Iuliana Vasiliev ◽  
Marius Stoica ◽  
Arjen Grothe ◽  
Sergei Lazarev ◽  
Dan Valentin Palcu ◽  
...  
Keyword(s):  
Late Miocene ◽  
Strontium Isotopes ◽  
Eastern Paratethys ◽  
Hydrological Changes

Late Miocene stratigraphy, palaeoecology and palaeogeography of the Tabriz Basin (NW Iran, Eastern Paratethys)

2011 ◽  
Vol 311 (1-2) ◽  
pp. 1-18 ◽  
Author(s):  
Bettina Reichenbacher ◽  
Habib Alimohammadian ◽  
Jafar Sabouri ◽  
Enayat Haghfarshi ◽  
Mohammad Faridi ◽  
...  
Keyword(s):  
Late Miocene ◽  
Eastern Paratethys ◽  
Nw Iran

scholarly journals The distribution of <i>Triebelina raripila</i> and <i>Carinocythereis carinata</i> (Ostracoda) from the Middle Miocene of the Central Paratethys and their palaeogeographic implications

1998 ◽  
Vol 17 (2) ◽  
pp. 125-130 ◽  
Author(s):  
J. Szczechura
Keyword(s):  
Shallow Water ◽  
Late Miocene ◽  
Middle Miocene ◽  
Early Miocene ◽  
Central Paratethys ◽  
Eastern Paratethys ◽  
Main Species ◽  
Late Middle Miocene ◽  
The Mediterranean

Abstract. Late Middle Miocene (Upper Badenian) strata of the Fore-Carpathian Depression of Poland yield a shallow-water ostracod fauna which contains the species Triebelina raripila (G. W. Müller, 1894) and Carinocythereis carinata (Roemer, 1838). The palaeobiogeographic distribution of the two main species suggests, that in the late Middle Miocene, Central Paratethys was still connected to the Mediterranean, although still separated from the Eastern Paratethys and from southeastern Eurasia. The continuous occurrence of Triebelina raripila and Carinocythereis carinata in the Mediterranean basins, from the Early Miocene to Recent, indicates that marine conditions existed throughout, thereby allowing them to survive the Late Miocene salinity crisis.

scholarly journals Taxonomic revision and new species/subspecies of Middle-Late Miocene (Bessarabian) miliolids of the Family Hauerinidae Schwager from Georgia — Eastern Paratethys

2009 ◽  
Vol 60 (5) ◽  
pp. 419-430
Author(s):  
Lamara Maisuradze ◽  
Kakhaber Koiava ◽  
Silvia Spezzaferri
Keyword(s):  
New Species ◽  
Late Miocene ◽  
Taxonomic Revision ◽  
Eastern Paratethys ◽  
The Family ◽  
Shape And Size

Taxonomic revision and new species/subspecies of Middle-Late Miocene (Bessarabian) miliolids of the Family Hauerinidae Schwager from Georgia — Eastern ParatethysThree new miliolid taxa from Bessarabian sediments from Georgia (Eastern Paratethys) are described following the classification of Łuczkowska (1972), which has never been used before by ex-Soviet micropaleontologists. They are:Varidentella luczkowskae; Varidentella reussi(Bogdanowicz) subsp.costulata; andAffinetrina voloshinovae(Bogdanowicz) subsp.eldarica.This classification takes into account the morphology of the aperture and the shape and size of teeth as criteria to distinguish the species. This study contributes important criteria which will help to unify the taxonomical inconsistencies between the Eastern, Central and Western Paratethyan miliolids.

Application of strontium isotopes to late Miocene-early Pliocene stratigraphy

Geology ◽  
1988 ◽  
Vol 16 (11) ◽  
pp. 1022 ◽  
Author(s):  
Judith A. McKenzie ◽  
David A. Hodell ◽  
Paul A. Mueller ◽  
Daniel W. Mueller
Keyword(s):  
Late Miocene ◽  
Strontium Isotopes ◽  
Early Pliocene

scholarly journals Calcareous nannofossils from the middle/upper Miocene succession of Pécs-Danitzpuszta, southern Hungary: cosmopolitan Paratethys and endemic Lake Pannon assemblages

2021 ◽  
Vol 151 (3) ◽  
pp. 253-265
Author(s):  
Stjepan Ćorić
Keyword(s):  
Late Miocene ◽  
Short Interval ◽  
Drastic Change ◽  
Calcareous Nannofossils ◽  
Lake Pannon ◽  
Central Paratethys ◽  
Eastern Paratethys ◽  
The Family ◽  
Low Diversity ◽  
Quantitative Analyses

Quantitative analyses on calcareous nannofossils were carried out on 109 middle/late Miocene (Sarmatian/ Pannonian) samples from the section at Pécs-Danitzpuszta sand pit (Hungary). The lower part of the section, which can be assigned to the Sarmatian, contains normal marine low-diversity assemblages dominated by Calcidiscus leptoporus, Reticulofenestra pseudoumbilicus, Sphenolithus moriformis and Syracosphaera spp. accompanied by didemnid ascidian spicules (Perforocalcinela fusiformis). The middle/late Miocene (Sarmatian/Pannonian) boundary is characterized by the last occurrences of normal marine calcareous nannofossils. The upper part of the section (Pannonian) can be subdivided into intervals characterized by monospecific endemic nannofossils Isolithus spp. and ascidians, respectively. A short interval with common endemic coccoliths belonging to the family Noelaerhabdaceae (Bekelithella echinata, Noelaerhabdus bozinovicae, N. jerkovici, Praenoelaerhabdus banatensis) in the upper part of the profile was also documented. The drastic change in nannofossil assemblages at the Sarmatian/Pannonian boundary is a result of paleoenvironmental stress caused by the isolation of the Central Paratethys from the Eastern Paratethys.

scholarly journals From Khersonian drying to Pontian “flooding”: late Miocene stratigraphy and palaeoenvironmental evolution of the Dacian Basin (Eastern Paratethys)

2020 ◽  
Vol 192 ◽  
pp. 103224 ◽  
Author(s):  
S. Lazarev ◽  
A. de Leeuw ◽  
M. Stoica ◽  
O. Mandic ◽  
C.G.C. van Baak ◽  
...  
Keyword(s):  
Late Miocene ◽  
Eastern Paratethys
Sign in / Sign up

Export Citation Format

Share Document