The Jurassic–Cretaceous transition in the High-Tatric succession (Giewont Unit, Western Tatra Mts, Poland): integrated stratigraphy and microfacies

Lodowski, Damian Gerard; Pszczółkowski, Andrzej; Wilamowski, Andrzej; Grabowski, Jacek

doi:10.24425/agp.2021.137712

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Tytuł artykułu

The Jurassic–Cretaceous transition in the High-Tatric succession (Giewont Unit, Western Tatra Mts, Poland): integrated stratigraphy and microfacies

Autorzy

Lodowski Damian Gerard , Pszczółkowski Andrzej , Wilamowski Andrzej , Grabowski Jacek

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DOI

10.24425/agp.2021.137712

Warianty tytułu

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Abstrakty

Herein are presented the results of detailed bio - (calcareous dinocysts, calpionellids, foraminifers, saccocomids) and chemostratigraphic (δ13C) studies combined with high-resolution microfacies, rock magnetic and gamma-ray spectrometry (GRS) investigations performed on the upper Kimmeridgian-upper Valanginian carbonates of the Giewont succession (Tatricum, Giewont and Mały Giewont sections, Western Tatra Mountains, Poland). The interval studied covers the contact between the Raptawicka Turnia Limestone (RTL) Fm. and the Wysoka Turnia Limestone (WTL) Fm. Their sedimentary sequence is composed of micrites, pseudonodular limestones, cyanoid packstones, lithoclastic packstone and encrinites. A precise correlation with the previously published Mały Giewont section is ensured by biostratigraphy, rock magnetic and GRS logs. The methodology adopted has enabled the recognition of two stratigraphic discontinuities, approximated here as corresponding to the latest Tithonian-early (late?) Berriasian and the early Valanginian. The hiatuses are evidenced by biostratigraphic data and the microfacies succession as well as by perturbations in isotopic compositions and rock magnetic logs; they are thought to result from a conjunction of tectonic activity and eustatic changes. A modified lithostratigraphic scheme for the Giewont and the Osobita High-Tatric successions is proposed. The top of the RTL Fm. falls in the upper Tithonian, where cyanoid packstones disappear. At the base of the WTL Fm. a new Giewont Member is defined as consisting of a basal lithoclastic packstone and following encrinites.

Słowa kluczowe

microfossils rock magnetism carbon isotopes Western Carpathians Tatra Mountains

mikroskamieniałości skała magnetyczna izotopy węgla Karpaty Zachodnie Tatry

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2022

Tom

Vol. 72, no. 1

Strony

107--135

Opis fizyczny

Bibliogr. 93 poz., rys.

Twórcy

autor

Lodowski Damian Gerard

damian.lodowski@uw.edu.pl

Faculty of Geology, University of Warsaw, ul. Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Pszczółkowski Andrzej

apszcz@interia.pl

Institute of Geological Sciences, Polish Academy of Sciences, Warszawa Research Centre, ul. Twarda 51/55, 00-818 Warsaw, Poland

autor

Wilamowski Andrzej

andrzej.wilamowski@pgi.gov.pl

Polish Geological Institute-National Research Institute, ul. Rakowiecka 4, 00-975 Warsaw, Poland

autor

Grabowski Jacek

jacek.grabowski@pgi.gov.pl

Polish Geological Institute-National Research Institute, ul. Rakowiecka 4, 00-975 Warsaw, Poland

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Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).

Typ dokumentu

Bibliografia

Identyfikator YADDA

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