Integrated stratigraphy and palaeoenvironmental interpretation of the Upper Kimmeridgian to Lower Berriasian pelagic sequences of the Velykyi Kamianets section (Pieniny Klippen Belt, Ukraine)

Grabowski, Jacek; Бахмутов, В. Г.; Kdýr, Šimon; Krobicki, Michał; Pruner, Petr; Reháková, Daniela; Schnabl, Petr; Stoykova, Kristalina; Wierzbowski, Hubert

doi:10.1016/j.palaeo.2019.05.038

Cited by 30 publications

(25 citation statements)

References 98 publications

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“…A representative subset of section data are in Fig. 15, focusing on studies across the Tithonian-Kimmeridgian boundary (Ogg et al, 1984;Muttoni et al, 2018;Grabowski et al, 2019). Statistical correlation Option B is supported by the correlation of the normal-polarity-dominated interval of the Platynota Zone and overlying Hypselocycum Zone, to the normal-polarity-dominated interval M25n-M24Bn.…”

Section: Correlation To the Seafloor M-sequence Anomaliesmentioning

confidence: 91%

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The Global Stratotype Section and Point (GSSP) for the base of the Kimmeridgian Stage (Jurassic System), at Flodigarry, Staffin Bay, Isle of Skye, Scotland, UK

et al. 2023

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Section: Correlation To the Seafloor M-sequence Anomaliesmentioning

confidence: 91%

“…However, this position is not universally accepted, with some placing the base Tithonian within the older M23n (Pavia et al, 2004; as shown in Fig. 15), or younger within the lower part or base of M22n (Muttoni et al, 2018;Grabowski et al, 2019).…”

Section: Correlation To the Seafloor M-sequence Anomaliesmentioning

confidence: 99%

The Global Stratotype Section and Point (GSSP) for the base of the Kimmeridgian Stage (Jurassic System), at Flodigarry, Staffin Bay, Isle of Skye, Scotland, UK

et al. 2023

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“…This parameter is the ‐(IRM ‐100mT /IRM 1T ) ratio and is used to determine the ratio of high coercivity minerals to low coercivity minerals (e.g. Grabowski et al ., 2019). The MMPM 10 pulse magnetiser was used to magnetise the samples, and the JR 6‐A spinner magnetometer was used to measure the magnetic remanent.…”

Section: Methodsmentioning

confidence: 99%

Reconstruction of subglacial depositional conditions based on the anisotropy of magnetic susceptibility: an example from Dębe (central Poland)

Teodorski

Dzierżek

Ziółkowski

2021

J Quaternary Science

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The analysis of low‐field anisotropy of magnetic susceptibility (AMS) was used to reconstruct the subglacial deposition conditions during the Main Stadial of the Odranian Glaciation (MIS 6) in till deposits from a site in Dębe (central Poland). Based on the AMS parameters, six till beds were identified (intervals 1–6). The declination of the maximum magnetic susceptibility axis (k1) indicates that the ice sheet was moving in from the northwest. The obtained results confirm the thesis about the preferred direction of ice‐sheet transgression during the Odranian Glaciation (MIS 6) in this part of Poland. This interpretation is also confirmed by data obtained from measurements of the long axis of clasts, which agree with the orientation of k1. Based on the AMS results, a significant part of the profile was deformed through simple shear and direct interaction of the ice sheet with the underlying sediment (beds 2–5). The lowest part of the till (bed 6) may have been deposited on a southeast‐trending slope or post‐depositional deformed by uneven loading of the ice cover. The upper part of the profile (especially in interval 1) could be deposited with an impact of pore water.

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“…In the Velykyi Kamianets section in the Ukraine Carpathians, the Chitinoidella and Praetintinnopsella zones have been detected in the Czorsztyn Limestone Formation (an equivalent of the upper nodular limestones), and the Crassicollaria and Calpionella zones -in the Calpionella-bearing Dursztyn Limestone Formation (Grabowski et al, 2019). The Boneti Subzone is represented by a diverse association, whereas the Dobeni Subzone is only indicated by its index-species as in many other Carpathian sections.…”

Section: Interregional Tethyan Correlationsmentioning

confidence: 99%

“…The Boneti Subzone is represented by a diverse association, whereas the Dobeni Subzone is only indicated by its index-species as in many other Carpathian sections. Grabowski et al (2019) presented a correlation between calpionellid zonation and magnetostratigraphy across the Tithonian/Berriasian boundary in several sections of the Trans-Danubian and Carpathian regions. This direct correlation has revealed that the base of the Boneti Subzone approximates the base of M20r magnetic chron, the top of the Remanei Subzone -the base of M19r magnetic chron, and the base of the Ferasini Subzone correlates well with the M18r chron.…”

Section: Interregional Tethyan Correlationsmentioning

confidence: 99%

Biostratigraphy and microfacies of the pelagic carbonate formations in the Yavorets section (Tithonian–Berriasian), Western Balkan Mts, Bulgaria

Petrova

Koleva-Rekalova

Ivanova

et al. 2019

Geologica Balcanica

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Calpionellid study has provided new evidence of early and late Tithonian age of the top of the Gintsi Formation, and of late Tithonian and early Berriasian age of the Glozhene Formation in the Yavorets section (Western Balkan Mts, Bulgaria). The calpionellid Chitinoidella, Praetintinnopsella, Crassicollaria, and Calpionella zones have been documented in successive order. Three calcareous dinocyst zones – Colomisphaera tenuis, Colomisphaera fortis and Stomiosphaerina proxima, have been determined in this lower Tithonian to lower Berriasian interval. From the base upwards, the following microfacies have been recognized: Saccocoma (Gintsi Formation, lower and upper Tithonian), Globochaete alpina, and calpionellid (Glozhene Formation, upper Tithonian and lower Berriasian). The base of the Berriasian has been traced at the explosion of the uniformly shaped spherical variety of Calpionella alpina. Evolutionary lineages of species of the genus Calpionella are discussed, as well as the vertical distributions and abundance peaks of crassicollarians. The calpionellid zones described herein are correlated with coeval zonations from the Western, Central and Eastern Tethyan domains. The regional correlation with previously studied sections of Tithonian/Berriasian pelagic carbonates in the Western Balkan Mts revealed a transition to hemipelagic deposition of the limestone-marl succession of the Salash Formation and/or sandstone accumulation during the middle to late Berriasian (Elliptica and Simplex calpionellid subzones) due to unstable conditions of the sedimentary environment. From the west to the east in the Western Balkan Unit (i.e., from the Rosomač section in eastern Serbia to the Sarbenitsa, Bov and Yavorets sections in the Iskar River Valley area), there is a trend of slight progressive deepening of the basin. This is manifested in the occurrence of redeposited shallow-carbonate-platform microfossils in the west to greater thickenesses of the Gintsi and Glozhene formations and occurrence of sandstone channel deposits in the east.

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Integrated stratigraphy and palaeoenvironmental interpretation of the Upper Kimmeridgian to Lower Berriasian pelagic sequences of the Velykyi Kamianets section (Pieniny Klippen Belt, Ukraine)

Cited by 30 publications

References 98 publications

The Global Stratotype Section and Point (GSSP) for the base of the Kimmeridgian Stage (Jurassic System), at Flodigarry, Staffin Bay, Isle of Skye, Scotland, UK

The Global Stratotype Section and Point (GSSP) for the base of the Kimmeridgian Stage (Jurassic System), at Flodigarry, Staffin Bay, Isle of Skye, Scotland, UK

Reconstruction of subglacial depositional conditions based on the anisotropy of magnetic susceptibility: an example from Dębe (central Poland)

Biostratigraphy and microfacies of the pelagic carbonate formations in the Yavorets section (Tithonian–Berriasian), Western Balkan Mts, Bulgaria

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