Silvia Antolíková Ozdínová

Silvia Antolíková Ozdínová
Slovak Academy of Sciences | SAV · Earth Science Institute of the SAS

RNDr. PhD.

About

6
Publications
2,635
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46
Citations
Introduction
Skills and Expertise
Additional affiliations
January 2005 - July 2021
Slovak Academy of Sciences
Position
  • Editor

Publications

Publications (6)
Article
Early Paleogene events of the Alpine Tethys were considerably upgraded for the Western Carpathians. The Kršteňany KRS-3 core section provides high-resolution data from the Cretaceous-Paleogene (K/Pg) transition to Lutetian/Bartonian boundary. The Upper Cretaceous sequence started from terrestrial red-beds superposed by transgressive sediments with...
Article
Full-text available
Intensively bioturbated hemipelagic limestone of the Fleckenmergel facies is regarded as an equivalent of the Allgäu Formation. Studied outcrops within the sequence of the bioturbated limestone are situated in the westernmost part of Periklippen Zone (respectively Klippen Zone). Mentioned Middle Jurassic bioturbated limestone belongs to the younges...
Article
Full-text available
Outcrops of a thick turbiditic succession are exposed on the northern bank of the Liptovská Mara reservoir near Liptovská Ondrašová and Ráztoky. The section consists of rhythmic, predominantly thin- to medium-bedded turbidites of the Rupelian age. Their biostratigraphy is based on the calcareous nannofossils. Facies associations of these deposits r...
Article
Full-text available
Oligocene and Lower Miocene sediments of the Lučenec Depression were studied to demonstrate the plank-tonic bioevents and climatic proxies from the Číž Formation (Rupelian) and Lučenec Formation (Chattian—Aquitanian) on the basis of quantitative analyses of foraminifers and calcareous nannofossils. The oldest nannofossil assemblages of the Číž Form...

Questions

Question (1)
Question
The object (more objects) was found in the examination of of calcareous nannofossils in the Lower - Middle Jurassic sediments. It can be a part of the nannoplankton body. Thank you for your help :-)

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