The Badenian/Sarmatian (Middle Miocene) boundary in the Central Paratethys (Kreminna, western Ukraine) : Foraminiferal and palynological evidence

Peryt, Danuta; Gedl, Przemysław; Jasionowski, Marek; Peryt, Tadeusz Marek; Poberezhskyy, Andriy. V

doi:10.7306/gq.1731

Artykuł - szczegóły

Tytuł artykułu

The Badenian/Sarmatian (Middle Miocene) boundary in the Central Paratethys (Kreminna, western Ukraine) : Foraminiferal and palynological evidence

Autorzy

Peryt Danuta , Gedl Przemysław , Jasionowski Marek , Peryt Tadeusz Marek , Poberezhskyy Andriy. V

Treść / Zawartość

Pełne teksty:

Peryt_D_The Badenian_GQ_Volo. 68_No. 1_2024.pdf

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Identyfikatory

DOI

10.7306/gq.1731

Warianty tytułu

Języki publikacji

Abstrakty

The Badenian/Sarmatian boundary in the Paratethys basin, that marks the transition from normal marine to restricted semi-marine conditions due to isolation of the basin from the world ocean at the onset of Sarmatian time, is still far from being fully understood. The Kreminna section is located at the northeastern margin of the Carpathian Foreland Basin (Central Paratethys) in the Medobory Hills region. The Miocene deposits that overlie here the Upper Cretaceous substratum comprise the >1 m thick upper Badenian marls and clays passing upwards into ~4 m thick Sarmatian marly limestones with intercalations of marls, clays and limestones, and >2 m thick limestones in the uppermost part of the exposure. Fifty-three species of benthic foraminifera and four species of planktonic foraminifera have been recorded. Six benthic foraminiferal assemblages are composed almost exclusively of calcareous forms; agglutinated taxa are practically lacking. Elphidium spp., miliolids, Lobatula lobatula and Ammonia spp. are the most common calcareous benthic foraminifera in the material studied. Planktonic foraminifera are represented only by species of Globigerina and occur rarely in the lowermost part of the section. A characteristic feature of palynofacies is the very low proportion of land-derived elements – sporomorphs and cuticles, which suggests a sedimentary setting without terrestrial influx, and taxonomical impoverishment of dinoflagellate cyst assemblages, which are either monospecific or consist mainly of two to three species: in a majority of samples, assemblages with Polysphaeridium zoharyi and P. subtile occur. Most δ18O values range from –1.5 to ~+0.5‰ VPDB and most δ13C values are between 0 and +2‰ VPDB. In general, the δ13C curve mirrors the δ18O changes in the section. The Badenian/Sarmatian boundary is placed at the level where the Cibicidoides ungerianus Assemblage is replaced by the Elphidium fichtelianum Assemblage. At the boundary, planktonic foraminifers and most abundant stenohaline benthic foraminifera disappeared. Bottom waters were well-oxygenated both in the latest Badenian and earliest Sarmatian in the Kreminna location.

Słowa kluczowe

Middle Miocene Carpathian Foredeep Basin foraminifers palynofacies palaeoenvironments

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2024

Tom

Vol. 68, No. 1

Strony

art. no. 7

Opis fizyczny

Bibliogr. 109 poz., fot., rys., tab., wykr.

Twórcy

autor

Peryt Danuta

Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa

https://orcid.org/0000-0002-5821-1084

autor

Gedl Przemysław

Institute of Geological Sciences, Polish Academy of Sciences, Senacka 1, 31-002 Kraków

https://orcid.org/0000-0003-4319-2658

autor

Jasionowski Marek

Polish Geological Institute - National Research Institute, Rakowiecka 4, 00-975 Warszawa

https://orcid.org/0000-0003-3825-7859

autor

Peryt Tadeusz Marek

Polish Geological Institute - National Research Institute, Rakowiecka 4, 00-975 Warszawa

https://orcid.org/0000-0002-8017-1701

autor

Poberezhskyy Andriy. V

Institute of Geology and Geochemistry, National Academy of Sciences of Ukraine, Naukova 3a, 79060 Lviv

https://orcid.org/0000-0002-4622-0725

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