Pregled bibliografske jedinice broj: 993335
Foraminifera-based estimation of water depth in epicontinental seas: Badenian deposits from Glavnica Gornja (Medvednica Mt., Croatia), Central Paratethys
Foraminifera-based estimation of water depth in epicontinental seas: Badenian deposits from Glavnica Gornja (Medvednica Mt., Croatia), Central Paratethys // Geologia Croatica : journal of the Croatian Geological Survey and the Croatian Geological Society, 72 (2019), 2; 93-100 doi:10.4154/gc.2019.08 (međunarodna recenzija, članak, znanstveni)
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Naslov
Foraminifera-based estimation of water depth in
epicontinental seas: Badenian deposits from
Glavnica Gornja (Medvednica Mt., Croatia),
Central Paratethys
Autori
Pezelj, Đurđica ; Drobnjak, Lucija
Izvornik
Geologia Croatica : journal of the Croatian Geological Survey and the Croatian Geological Society (1330-030X) 72
(2019), 2;
93-100
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Benthic foraminifera ; Paleo-depth estimation ; Badenian ; North Croatian Basin ; Central Paratethys
Sažetak
This study presents the first attempt to estimate the paleo-depth, and to assess the environmental conditions at the sea bottom, by means of foraminifers during the deposition of earlier Badenian deposits in the North Croatian Basin. The studied stratigraphic record, the Glavnica Gornja section is located in Mt. Medvednica, in the southwestern part of the Pannonian Basin System, and it belongs to the Upper Lagenidae Zone (Moravian substage of the Badenian). Three methods were tested to estimate the paleo-depth ; the plankton/benthos (P/B) ratio indicated the lower to upper bathyal zone, the modified P/B ratio indicated 886-987 m depth of the bathyal zone, whereas the Hohenegger method indicated 142-204 m depth of the outer shelf. Of the three estimates, the last one is considered as best fitting the general environmental demands of the dominant and common small benthic forams. The well oxygenated sea bottom was temporarily replaced by more stressful conditions in the middle part of the studied interval, pointing to occasional fluctuations of the organic flux.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Đurđica Pezelj
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus