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Fossils and microfacies of Bellerophon Formation from the Vojsko Plateau (CROSBI ID 623600)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | domaća recenzija

Sremac, Jasenka ; Jurkovšek, Bogdan ; Aljinović, Dunja ; Kolar Jurkovšek, Tea Fossils and microfacies of Bellerophon Formation from the Vojsko Plateau // Međunarodni znanstveni skup 100-ta obljetnica rođenja akademkinje Vande Kochansky-Devidé/International scientific meeting 100th birth anniversary of Vanda Kochansky-Devidé, full member of Academy. Knjiga sažetaka / Abstracts / Mauch Lenardić, Jadranka ; Hernitz Kučenjak, Morana ; Premec Fućek, Vlasta et al. (ur.). Zagreb: Hrvatska akademija znanosti i umjetnosti (HAZU), 2015. str. 78-79

Podaci o odgovornosti

Sremac, Jasenka ; Jurkovšek, Bogdan ; Aljinović, Dunja ; Kolar Jurkovšek, Tea

engleski

Fossils and microfacies of Bellerophon Formation from the Vojsko Plateau

Late Permian Bellerophon Formation in Western Slovenia is exposed at the Vojsko plateau. It is ca. 130 m thick sequence composed of dolomites and limestones. The uppermost limestone interval is particularly interesting due to the sponge buildups situated just below the Permian/Triassic boundary. Small sponge biolithites represent a local facies variety within the bioclastic wackestones and packstones. Generally, three microfacies types appear within these deposits: Facies A: sponge bafflestone with large chambered demosponges (Colospongia, Amblysiphonella), smaller Demospongea and Calcarea. Sponges are preserved in situ but fine skeleton microstructure is partly destroyed by recrystallization (SREMAC et al., 2014). Facies B: packstone composed of bioclastic material and large biomicrite lithoclasts or coated bioclasts. Bioclasts are irregularly shaped and poorly sorted. Fossil fragments are more diverse than in the Facies C (echinoderms, foraminifers, algae, brachiopods and gastropods). Algal lithoclasts are particularly common. These sediments were probably deposited close to the sponge buildups. Facies C: packstone/wackestone limestone type composed mainly of echinoderm fragments and foraminifers. Brachiopod shells, bivalves and algal fragments are rarely present. Micritic matrix is often intensively recrystallized and dolomitized. These deposits indicate a lagoonal or shallow marine restricted environment, away from sponge buildups. Sponge fragments are generally scarce in Facies B and C, which confirms their limited occurrence and quick burial. The whole sequence was deposited on a shallow inner shelf/ramp in equatorial part of the Western Palaeotethys. Sedimentary basin was partly isolated from the main ocean currents, which enabled the survival of sensitive filter feeders during the stress events at the Guadalupian/Lopingian Boundary and in the Late Permian.

fossils; microfacies; Late Permian; Bellerophon Formation; Slovenia

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Podaci o prilogu

78-79.

2015.

objavljeno

Podaci o matičnoj publikaciji

Međunarodni znanstveni skup 100-ta obljetnica rođenja akademkinje Vande Kochansky-Devidé/International scientific meeting 100th birth anniversary of Vanda Kochansky-Devidé, full member of Academy. Knjiga sažetaka / Abstracts

Mauch Lenardić, Jadranka ; Hernitz Kučenjak, Morana ; Premec Fućek, Vlasta ; Sremac, Jasenka

Zagreb: Hrvatska akademija znanosti i umjetnosti (HAZU)

978-953-347-023-8

Podaci o skupu

Međunarodni znanstveni skup 100-ta obljetnica rođenja akademkinje Vande Kochansky- Devidé/International scientific meeting 100th birth anniversary of Vanda Kochansky-Devidé, full member of Academy

predavanje

09.04.2015-11.04.2015

Zagreb, Hrvatska

Povezanost rada

Geologija