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izvor podataka: crosbi

Foraminifera-based estimation of water depth in epicontinental seas: Badenian deposits from Glavnica Gornja (Medvednica Mt., Croatia), Central Paratethys (CROSBI ID 262751)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Pezelj, Đurđica ; Drobnjak, Lucija Foraminifera-based estimation of water depth in epicontinental seas: Badenian deposits from Glavnica Gornja (Medvednica Mt., Croatia), Central Paratethys // Geologia Croatica, 72 (2019), 2; 93-100. doi: 10.4154/gc.2019.08

Podaci o odgovornosti

Pezelj, Đurđica ; Drobnjak, Lucija

engleski

Foraminifera-based estimation of water depth in epicontinental seas: Badenian deposits from Glavnica Gornja (Medvednica Mt., Croatia), Central Paratethys

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.

Benthic foraminifera ; Paleo-depth estimation ; Badenian ; North Croatian Basin ; Central Paratethys

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Podaci o izdanju

72 (2)

2019.

93-100

objavljeno

1330-030X

1333-4875

10.4154/gc.2019.08

Povezanost rada

Geologija

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