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Abstrakty
Turbiditic silty and sandy intercalations in the Turonian Variegated Shale from the Silesian Nappe (Polish Outer Carpathians) contain numerous sponge spicules among siliciclastic fine-grained particles. The highest amount of spicule admixture is nearly 50%. In such layers, they create spiculitic sublitharenite microfacies. These sponge spicules contain forms belonging mostly to the Lithistida group (97% of morphotypes), with a small admixture of spicules from the Hexactinellidae group. Tetraclones with a high content of different types of triaenes dominate among desmas, what indicates the dominance of sponges from subfamily Tetracladina. The preservation state of spicules is generally poor. The Variegated Shale deposits that contain the sponge spicules were accumulated in a deep sea basin, below the calcium compensation depth. Most probably, the spicules were derived from loose material accumulated earlier in various parts of the basin slopes, from which they were exhumed and again redeposited by turbidity currents during the Turonian times.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
33--48
Opis fizyczny
Bibliogr. 50 poz., rys.
Twórcy
autor
- Institute of Geography, Pedagogical University of Cracow; ul. Podchorążych 2, 30-084 Krakow, Poland
autor
- Institute of Geological Sciences, Jagiellonian University; ul. Oleandry 2a, 30-063 Krakow, Poland
autor
- AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection; al. Mickiewicza 30, 30-059 Krakow, Poland
autor
- Institute of Geography, Pedagogical University of Cracow; ul. Podchorążych 2, 30-084 Krakow, Poland
Bibliografia
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-89d9fc3a-d3fe-4956-b83a-dfbfd0af7cc6