Pregled bibliografske jedinice broj: 76702
Triassic Dasycladales from the reefeal facies: examples from NW Croatia
Triassic Dasycladales from the reefeal facies: examples from NW Croatia // 4th regional symposium of I.F.A.A. (Algae and carbonate platforms in Romania) : Programme and abstracts / Bucur, I.I. ; Tantau, I. (ur.).
Cluj - Napoca, 2001. str. 27-27 (predavanje, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Triassic Dasycladales from the reefeal facies: examples from NW Croatia
Autori
Grgasović, Tonći
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
4th regional symposium of I.F.A.A. (Algae and carbonate platforms in Romania) : Programme and abstracts
/ Bucur, I.I. ; Tantau, I. - Cluj - Napoca, 2001, 27-27
Skup
4th regional symposium of I.F.A.A. (Algae and carbonate platforms in Romania
Mjesto i datum
Cluj-Napoca, Rumunjska, 29.08.2001. - 05.09.2001
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
green algae; Dasycladales; Triassic; reef; paleoecology
Sažetak
Although the majority of fossil (as well as living) Dasycladales inhabited the protected shallow marine environments as lagoons and bays, there are examples of dasyclads that tolerate, and even prefer the reefeal agitated environment. Here are presented some examples from the Anisian of NW Croatia. The first example is reef limestone from the Belski dol quarry, characterised by peculiar "psudooncoidal" reef cements, similar to "Evinosponge" described from the Ladinian Esino Limestone of Lombardia (N Italy) (JADOUL & FRISIA 1988). The species that are usually found in the lagoonal carbonates are present in this limestone: Oligoporella pilosa PIA, Physoporella pauciforata (GÜMBEL) PIA, Physoporella varicans PIA, Teutloporella peniculiformis OTT, Macroporella alpina PIA and foraminifera Meandrospira dinarica KOCHANSKY-DEVIDÉ & PANTIC. Beside them, there is one dasycladal alga that was completely adapted to the reef environment, living attached to the reef rock: Scinderella scopuliformis GRGASOVIC & SOKAC (GRGASOVIC et al., in press). The second example is Ocura quarry, where reefeal limestones are resedimented into deeper-water tuffaceous sediments. The most common reef-organism is sphinctozoan sponge Celyphia zoldana OTT, PISA & FARABEGOLI, acting as framework builder, baffler and encruster. Besides it, there are many other, mainly encrusting microfossils. In several samples, probably from the back-reef facies, dasyclad Diplopora nodosa SCHAFHÄUTL is found together with problematic encrusting fossil (sponge?, alga?) Olangocoelia otti BECHSTÄDT & BRANDNER. Similar reefeal environments from the Ladinian Wetterstein Limestone of the Northern Calcareous Alps has been described by OTT (1972), and from the Anisian of Northern Dolomites by SENOWBARI-DARYAN et al. (1993).
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA