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Konferencja
5th Micropalaeontological Workshop MIKRO-2005 (8-10.06.2005, Szymbark, Poland)
Języki publikacji
Abstrakty
The Żegocina Tectonic Window is the most eastward located tectonic window of the Lanckorona-Żegocina Zone in the Polish Outer Carpathians and represents the slope parts of the Silesian basin and intrabasinal uplifted zones of the Subsilesian Unit. Upper Cretaceous and Palaeocene variegated marls, typical deposits of the studied part of the basin, are intercalated with the so-called Rybie beds (local sediments of siliciclastic submarine fans). A Middle Cenomanian foraminiferal assemblage (Rotalipora reicheli Zone) is here described from these sediments. The assemblage contains numerous planktonic (epipelagic and bathypelagic) foraminiferids, which is rather unique within the "Flysch" type assemblages. A middle slope palaeodepth is suggested as the depositional environment, based on benthic and planktonic foraminiferal associations.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
249--258
Opis fizyczny
Bibliogr. 21 poz., rys.
Twórcy
autor
- Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland
autor
- Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland
autor
- Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland
autor
- AGH University of Science and Technology, Mickiewicza 30, 30-059 Kraków, Poland
Bibliografia
- [1]. Bąk, K., Bąk, M. & Paul, Z., 2001. Barnasiówka Radiolarian Shale Formation - a new lithostratigraphic unit in the Upper Cenomanian-lowermost Turonian of the Polish Outer Carpathians (Silesian Series). Annales Societatis Geologorum Poloniae, 71: 75-103.
- [2]. Bąk, M., Gedl, E. & Bąk, K., 2000. Assemblages of Radiolaria, foraminiferids and dinocysts on the Cenomanian/Turonian boundary of the Subsilesian Unit (in Polish). In: Zapa³owicz-Bilan et al. (eds). Historia basenów sedymentacyjnych a zapis paleontologiczny. Referaty, komunikaty, postery: 1 Konferencja Paleontologiczna, 21-23.09.2000, Kraków: 12, 13.
- [3]. Birkenmajer, K., 1977. Jurassic and Cretaceous lithostratigraphic units of the Pieniny Klippen Belt. Carpathians. Poland. Studia Geologica Polonica, 45: 1-159.
- [4]. Burtan, J. & Turnau-Morawska, M., 1978. Biochemical siliceous rocks of the West Carpathian Flysch (in Polish with English summary). Prace geologiczne Polskiej Akademii Nauk - Oddział w Krakowie. Komisja Nauk Geologicznych, 111: 1-36.
- [5]. Caron, M., 1985. Cretaceous planktonic foraminifera. In: Bolli H. M., Saunders J., Perch-Nielsen K. (eds). Plankton Stratigraphy. Cambridge University Press, Cambridge: 17-86.
- [6]. Caron, M. & Homewood, P., 1983. Evolution of early planktonic foraminifers. Marine Micropaleontology, 7: 453-462.
- [7]. Gasiński, M. A., 1988. Campanian-Maastrichtian palaecology and palaeobiogeography of Andrychów klippes, Outer Carpathians, Poland. Rozprawy habilitacyjne Uniwersytetu Jagiellońskiego, Kraków, 333: 1-90.
- [8]. Gasiński, M. A., 1997. Tethyan-Boreal connection: influence on the evolution of mid-Cretaceous foraminiferids. Cretaceous Research, 18: 505-514.
- [9]. Gasiński, M. A., Jugowiec, M. & Ślączka, A., 1999. Late Cretaceous foraminiferids and calcareous nannoplankton from the Węglówka Marls (Subsilesian unit, Outer Carpathians, Poland). Geologica Carpathica, 50: 63-73.
- [10]. Gaździcka, E., 2001. Development stages of Skole depositional basin in the Cretaceous and Early Paleogene - nannoplankton documentation (in Polish). Przegląd Geologiczny, 49: 449-451.
- [11]. Gedl, E. & Bąk, M., 2000. Mid-Cretaceous dinocysts and Radiolaria from the Zasań section (Subsilesian Unit, Polish Outer Carpathians) - a CTBE problem. In: Abstracts of 6th International Cretaceous Symposium. August 27 to September 4, 2000 Vienna, Austria, p. 36.
- [12]. Geroch, S., Jednorowska, A., Książkiewicz, M. & Liszkowa J., 1967. Stratigraphy based upon microfauna in the Western Polish Carpathians. Biuletyn Instytutu Geologicznego, 211: 185-282.
- [13]. Geroch, S. & Nowak, W., 1984. Proposal of Zonation for the Late Tithonian-Late Eocene based upon arenaceous foraminifera from the Outer Carpathians, Poland. In: Oerti, H. (ed.). Benthos ‘83, 2nd International Symposium on Benthic Foraminifera, Pau, 225-239.
- [14]. Koszarski, L. & Liszkowa, J., 1963. New data on the Outer Carpathians Cenomanian (in Polish). Kwartalnik Geologiczny, 7: 557-558.
- [15]. Kotlarczyk, J., 1978. Stratigraphy of the Ropianka Formation or of Inoceramian beds in the Skole Unit of the Flysch Carpathians (in Polish with English summary). Kwartalnik Geologiczny, 4: 468-483.
- [16]. Kotlarczyk, J. & Gaździcka, E., 1988. The Dolhe and Ropniaka formations of the hypostratotype area: strtigraphy based on nanoplankton (in Polish). In: Kotlarczyk, J. & Pękala, K. (eds), Przewodnik 59 Zjazdu Polskiego Towarzystwa Geologicznego. Karpaty Przemyskie. 16-18.09.1988. Wydawnictwo AGH. Kraków: 101, 102.
- [17]. Liszkowa, J., 1967. Microfauna of the Upper Cretaceous marls in the Sub-Silesian series in the Wadowice region (Western Carpathians). Biuletyn Instytutu Geologicznego, 211: 341-351.
- [18]. Robaszynski, F. & Caron, M., 1995. Foraminiferes planctoniques du Crétacé: commentaire de la zonation Europe-Méditerranée, Bulletin de la Societe Géologique de France, 6: 681-692.
- [19]. Schlanger, S., O. & Jenkyns, H., C., 1976. Cretaceous Oceanic Anoxic Events: causes and consequences. Geologie en Mijnbouw, 55: 179-184.
- [20]. Skoczylas-Ciszewska, K., 1960. Geology of the Żegocina zone (western Flysch Carpathians). Acta Geologica Polonica, 10: 485-591.
- [21]. Sliter, W. V., 1972. Cretaceous foraminifers, depth habitats and their origin. Nature, 239: 514-515.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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