Tracing the latest Jurassic–earliest Cretaceous paleoenvironment evolution in swell carbonate facies:a case study of the High-Tatric succession (Central Western Carpathians, Tatra Mts, Poland)

Lodowski, Damian Gerard; Grabowski, Jacek

doi:10.24425/agp.2023.145629

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Tracing the latest Jurassic–earliest Cretaceous paleoenvironment evolution in swell carbonate facies:a case study of the High-Tatric succession (Central Western Carpathians, Tatra Mts, Poland)

Autorzy

Lodowski Damian Gerard , Grabowski Jacek

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Identyfikatory

DOI

10.24425/agp.2023.145629

Warianty tytułu

Języki publikacji

Abstrakty

This paper presents an interpretation of sedimentologic, paleomagnetic, and geochemical data collected in the Upper Kimmeridgian–Valanginian carbonates of the Giewont series (Giewont and Mały Giewont sections, High-Tatric succession, Western Tatra Mountains, Poland). The studied succession provides insight into the sedimentary conditions prevailing in the South Tatric Ridge (Tatricum), a submarine elevation located between the Zliechov Basin (Fatricum) and the Vahic (=South Penninic) Ocean. The sedimentary sequence includes micrites, pseudonodular limestones, cyanoid packstones, lithoclastic packstone, and encrinites. The results are discussed with regards to their significance for detrital input, paleoclimate, and paleoproductivity, which in turn are considered in the context of both local and regional paleoenvironmental trends and events. The greatest depositional depths during the latest Kimmeridgian–earliest Tithonian are documented by the occurrence of pseudonodular limestones. A Tithonian shallowing trend is demonstrated via the increasing size and roundness of cyanoids, while the final (?)emergence and erosion in the South Tatric Ridge is documented by earliest Cretaceous disconformities. This process might have been related to both falling sea-level during the major eustatic regressive cycle and tectonic uplift caused by the mutually related (re)activation in the Neotethyan Collision Belt and rifting in the Ligurian-Penninic-Vahic Oceans. The highest lithogenic influx (although still low; max 0.5% of Al content) during the Late Kimmeridgian is considered as associated with relatively humid climate conditions, whereas a subsequent decreasing trend is thought to result from aridification during the latest Kimmeridgian–earliest Tithonian. Ultimately, deposition in the High-Tatric zone was affected by both large-scale environmental perturbations characteristic of the latest Jurassic (climate changes, variations in sea-water pH, monsoonal upwelling, lithogenic input, etc.), as well as local sedimentary controls, predominantly the oxygenation state of bottom waters and tectonic movements.

Słowa kluczowe

microfacies geochemistry rock magnetism lithogenic input paleoclimate monsoonal upwelling hypoxia paleoproductivity Central Western Carpathians

mikrofacje geochemia skała magnetyczna wkład litogeniczny paleoklimat monsunowe wypiętrzanie niedotlenienie paleoproduktywność zachodnie Karpaty centralne

Wydawca

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

Czasopismo

Acta Geologica Polonica

Rocznik

2023

Tom

Vol. 73, no. 4

Strony

741--772

Opis fizyczny

Bibliogr. 148 poz., rys., wykr., tab

Twórcy

autor

Lodowski Damian Gerard

damian.lodowski@uw.edu.pl; damian.lodowski@pgi.gov.pl

University of Warsaw, Faculty of Geology
Polish Geological Institute-National Research Institute

autor

Grabowski Jacek

jacek.grabowski@pgi.gov.pl

Polish Geological Institute-National Research Institute

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Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2025).

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