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Palynostratigraphy and palynofacies of the Upper Silesian Keuper (southern Poland)

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Palynostratigraphy and palynofacies of the Upper Silesian Keuper (southern Poland)

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dc.contributor.author Fijałkowska-Mader, Anna pl
dc.contributor.author Heunisch, Carmen pl
dc.contributor.author Szulc, Joachim [SAP11010265] pl
dc.date.accessioned 2016-01-28T07:22:10Z
dc.date.available 2016-01-28T07:22:10Z
dc.date.issued 2015 pl
dc.identifier.issn 0208-9068 pl
dc.identifier.uri http://ruj.uj.edu.pl/xmlui/handle/item/20238
dc.language eng pl
dc.rights Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa *
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/4.0/pl/legalcode *
dc.title Palynostratigraphy and palynofacies of the Upper Silesian Keuper (southern Poland) pl
dc.type JournalArticle pl
dc.description.physical 637-661 pl
dc.description.additional Bibliogr. s. 657-659 pl
dc.abstract.en The results of the palynostratigraphical studies presented in this paper come from five boreholes Patoka 1, Czarny Las, Woźniki Śląskie K1, Kobylarz 1 and Poręba as well as from four outcrops at Lipie Śląskie, Patoka, Zawiercie and Poręba, in Upper Silesia (southern Poland). The palynostratigraphical zonation presented by Orłowska-Zwolińska (1983) for the epicontinental Upper Triassic of Poland was applied. The palynomorph spectra are marked by different preservation states, combined with the frequent occurrence of reworked specimens, probably even from Palaeozoic strata. The spore-pollen assemblage recognized in the “Chrzanów Formation” belongs to the early Carnian verrucata Subzone of the palynological longdonensis Zone. The spectrum from the Stuttgart Formation represents the Carnian astigmosus Zone. Spectra in the Patoka Marly Mudstone-Sandstone Member (Grabowa Mudstone-Carbonate Formation), with the Lisowice bone-bearing horizon, represent the middle and late Norian meyeriana b Subzone. The Rhaetian age of the bone-bearing succession in the Lisowice–Lipie Śląskie clay-pit suggested in the literature was not confirmed. The age of assemblages from the “Połomia Formation”, which overlies the Patoka Member, was not determined, owing to the poor state of miospore preservation. Moreover, three types of palynofacies were recognized as being characteristic for a fluvial channel (1), a flood plain (2), and lacustrine and playa environments (3) as well as for an undetermined milieu. Type 1 was found in the deposits of the Stuttgart Formation, the Patoka Member and the “Połomia Formation”, type 2 in the Patoka Member and the “Połomia Formation”, type 3 in the “Chrzanów Formation”, the Stuttgart Formation and the Patoka Member. pl
dc.subject.en miospores pl
dc.subject.en palynostratigraphy pl
dc.subject.en palynofacies pl
dc.subject.en Upper Triassic pl
dc.subject.en Upper Silesia pl
dc.description.volume 85 pl
dc.description.number 4 pl
dc.identifier.doi 10.14241/asgp.2015.025 pl
dc.identifier.eissn 2300-8512 pl
dc.title.journal Annales Societatis Geologorum Poloniae pl
dc.language.container eng pl
dc.affiliation Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych pl
dc.subtype Article pl
dc.rights.original OTHER; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0; pl
dc.identifier.project ROD UJ / P pl
.pointsMNiSW [2015 A]: 15


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Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa Except where otherwise noted, this item's license is described as Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa