Isotopic events in the Early/Middle Badenian (Miocene) of the Upper Silesia Basin (Central Paratethys)

• Autorzy: Gonera M. , Bukowski K.

Identyfikatory

DOI

10.7306/gq.1040

• Języki publikacji: EN

Abstrakty

EN

Middle Miocene foraminifera from the Skawina Formation of the Upper Silesia Basin have been analysed. The stable oxygen and carbon isotope signatures in Globigerinoides quadrilobatus (shallow pelagic), Globigerina bulloides (deeperpelagic) and Uvigerina spp. (benthic) tests show a temporal pattern of changes in the sections studied. The foraminiferal assemblage biozones of the Badenian that were identified earlier, on the basis of taxonomic composition, correspond to changes in the foraminiferal ẟ^I8O and ẟ^I3C values. The CPN7/CPN8 transition - as the Moravian/Wielician border - is marked by distinct isotopic events: a ẟ¹⁸O increase (IIAB/IIC boundary) followed by a ẟ¹³C decrease (IIC/IID boundary).

Słowa kluczowe

EN

Middle Miocene; Wielician; Paratethys; foraminifera; stable isotopes

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2012
• Tom: Vol. 56, No 3
• Strony: 561--568
• Opis fizyczny: Biblogr. 35 poz., rys., tab., wykr.

Twórcy

autor

Gonera M.

• Institute of Nature Conservation, Polish Academy of Sciences, A. Mickiewicza 33, 31-120 Kraków, Poland

autor

Bukowski K.

• Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza 30, 30-059 Kraków, Poland

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