Patrycja Wojcik-Tabol

• PhD
• Professor (Assistant) at Jagiellonian University

The provenance of the Numidian Formation deposits remains a matter of debate as to whether the source rock of the detrital material that fed the Maghrebian Flysch Basin is of European or African origin. The Numidian Formation is built mostly of Oligocene to Miocene deep-sea turbiditic sandstones and mudstones, which are widely exposed across the Me...

The Anthracosia Shales are lacustrine deposits within the volcano-sedimentary Pennsylvanian– Lower Permian succession of the Intra-Sudetic Basin. Core from the Rybnica Leśna PIG 1 borehole, which penetrated the Lower Anthracosia Shales, was analysed to explore the influence of climate on the evolution of the palaeolake, as distinct from tectonic an...

The Western Carpathians represent a fold-and-thrust belt that forms the northernmost European Alpides in the Czech Republic, Slovakia, and Poland. They consist of an older range, known as the Inner or Central Carpathians, and a younger range, the Outer or Flysch Carpathians, separated by the Pieniny Klippen Belt. The Inner Carpathians are formed of...

The Oligocene Menilite shales (Silesian Unit, Polish Outer Carpathians), an example of the organic-rich black shale facies of the Paratethys, were sampled in the two sections of Znamirowice and Kobielnik, representing proximal to the land and open-marine environments, respectively. Terrestrial organic matter (OM) imprinted in maceral and biomarker...

Varved clays from a Late Pleistocene proglacial lake in the Pašaminė sections (Lithuania) contain diverse organic matter of different origin, i.e. aquatic and allogenous macerals of the groups of liptinite, vitrinite and inertinite (their average contributions are 55%, 13.5% and 31.5%, respectively). The contents of TOC and TN vary from 0.51% to 1....

Upper Berriasian chemostratigraphic, clay mineral and calcareous nanofossil data are presented from a precisely dated hemipelagic section of Barlya (Western Balkan, Bulgaria). The section covers an interval from the upper part of the lower Berriasian (Calpionella elliptica Subzone, magnetozone M17r) to the lowermost Valanginian (Calpionellites dard...

The Oligocene Menilite shales (Silesian Unit, Polish Outer Carpathians), an example of the organic-rich black shale facies of the Paratethys, were sampled in the two sections of Znamirowice and Kobielnik, representing proximal to the land and open-marine environments, respectively. Terrestrial organic matter (OM) imprinted in maceral and biomarker...

In the Polish sector of the Magura Nappe have long been known and exploited carbonate mineral waters, satu- rated with carbon dioxide, known as the “shchava (szczawa)”. These waters occur mainly in the Krynica Sub- unit of the Magura Nappe, between the Dunajec and Poprad rivers, close to the Pieniny Klippen Belt (PKB). The origin of these waters i...

In the Polish sector of the Magura Nappe have long been known and exploited carbonate mineral waters, saturated with carbon dioxide, known as the “shchava (szczawa)”. These waters occur mainly in the Krynica Subunit of the Magura Nappe, between the Dunajec and Poprad rivers, close to the Pieniny Klippen Belt (PKB). The origin of these waters is sti...

Wójcik-Tabol, P., 2017. Elemental and organic carbon proxies for redox conditions of the Oligocene formations in the Ropa Tectonic Window (Outer Carpathians, Poland): palaeoenvironmental implications. Annales Societatis Geologorum Poloniae, 87: 00–00. Abstract: The Oligocene Grybów Succession is recognized as a counterpart of the anoxic Menilite Fo...

A continuous Late Berriasian sedimentary and stratigraphic record is here presented from a hemipelagic succession from theWestern Balkan (Barlya section, Bulgaria). The section, 39-m-thick,was stratigraphically calibrated using a variety of methods: biostratigraphy (calpionellids, calcareous nannofossils and calcareous dinocysts), magnetostratigrap...

The Ostravice Sandstone Member was identified and described as a lithostratigraphic unit in the Polish part of the Outer Carpathians. This division occurs in the lowermost part of the Godula Formation, is underlain by variegated deposits of the Mazák Formation or directly by the Barnasiówka and Lhoty formations, and overlain by the Czernichów Membe...

Calcareous arenitic rocks exposed in the Dopplerhütte and Tulbingerkogel quarries northwest of Vienna were studied to establish their stratigraphic age. The whole succession is a part of the “Northern Zone” – the Tulbingerkogel thrust sheet – which represents the external part of the Wienerwald Flysch. These rocks were regarded commonly as Neocomia...

This study details the petrology and chemistry of the Oligocene succession of the Grybów Nappe in its stratotype-locality in the Grybów tectonic win dow (Polish Carpathians). The sec tion studied is com posed of the Sub-Grybów Beds, the Grybów Marl For ma tion (GMF), and the Cergowa Beds, representing the middle to upper part of the Oligocene succe...

The study area comprising the cantral part of the Polish Lowlands, termed Mogilno-Łodź Synclinorium. This area could be important petroleum exploration target in Poland, especially for unconventional resources. In this paper, we evaluate organic source facies and the results of basin modelling in order to improve understanding of the regional petro...

The Grybów Unit occurring in the Ropa tectonic window was the subject of micropaleontological and geochemical investigation. Studies, based on calcareous nannofossils, proved that the level of reworked microfossil is not higher than 22 % and it varies between two sections. Quantitative analyses of the reworked assemblages confirmed the domination o...

The role of lithologic discontinuities in forming soil properties is getting increasing recognition, following the allochthonistic approach to soil formation. This approach may be particularly useful in the mountainous areas of Central Europe, where slopes are mantled by layers of cover materials of complex genesis and predominantly Pleistocene age...

14 Waśkowska, A., 2014: The Eocene Hieroglyphic beds and Green shales in the Rożnów Lake area (Silesian Nappe, Outer Carpathians) – facies development and biostratigraphy. Geology, Geophiscics and Environment, in press. Paleogene red beds of the Magura Basin were distinguished as the Łabowa Shale Formation and are mostly developed as variegated hem...

Terminal Triassic environmental changes are characterized by an integrated study of lithology, litho- and cyclostratigraphy, paleontology, mineralogy, geochemistry and rock magnetism in the Tatra Mts. The Carpathian Keuper sequence was deposited in an arid environment with only seasonal rivers, temporal lakes and swamps with scarce vegetation. Comb...

Ab s t r a c t. Most of the craters on the Earth, produced by an impact of meteorite or other space object, have been masked by exogenous processes. Therefore, indirect indicators of the impact such as shocked quartz have been recognized. The impact metamorphism is visibly recorded within quartz by distinctive microstructures. However, only the pla...

The chem i cal com po si tion of the Cre ta ceous de pos its of the Grajcarek thrust-sheets (Pieniny Klippen Belt, Po land) has been in ves ti gated to pro vide in for ma tion on palaeoenvironment and prov e nance of pe lagic and turbiditic par ti cles. The ma te rial stud ied shows large vari a - tions in terrigenous and biogenic con tent. Phyllos...

The turbiditic to hemipelagic, fine-grained deposits of the Hradištì Formation (Hauterivian, 132 Ma) to the Lhoty Formation (Albian–Cenomanian, 99 Ma) in the western part of the Silesian Nappe (Polish Outer Carpathians) were studied mineralogically and geochemically to determine if the main factors controlling the chemistry of the sedimentary mater...

The turbiditic to hemipelagic, fine-grained deposits ofthe Hradiště Formation (Hauterivian, 132 Ma) to the Lhoty Formation (Albian-Cenomanian, 99 Ma) in the western part of the Silesian Nappe (Polish Outer Carpathians) were studied mineralogically and geochemically to determine if the main factors controlling the chemistry of the sedimentary materi...

The chemical composition of the Cretaceous deposits of the Grajcarek thrust-sheets (Pieniny Klippen Belt, Poland) has been investigated to provide information on palaeoenvironment and provenance of pelagic and turbiditic particles. The material studied shows large variations in terrigenous and biogenic content. Phyllosilicates (mirrored in amounts...

Most of the craters on the Earth, produced by an impact of meteorite or other space object, have been masked by exogenous processes. Therefore, indirect indicators of the impact such as shocked quartz have been recognized. The impact metamorphism is visibly recorded within quartz by distinctive microstructures. However, only the planar deformation...

The provenance and diagenesis of the siliciclastic and hemipelagic sediments of three lithostratigraphic units: Lhoty Formation, Barnasiówka Radiolarian Shale Formation (BRSF) and Variegated Shales from Lancko- rona area, Polish Outer Carpathians, was approached by means of petrological and geochemical analysis of the representative samples. Data s...

The studied sediments of the Magierowa Member corespond to the Cenomanian/Turonian OAE 2. A better understanding of the genesis and palaeoenvironmental setting of this unit was achieved by means of geochemical indicators integrated with mineral composition. It suggests a strong influence of palaeoproducti vity/redox cycles. The black shales are cha...

The Cenomanian sequence of marls and marly shales interbedded by black shales (Jaworki Formation) from, the Niedzica Succession was investigated. These organic carbon-rich horizons may correspond to the event of global anoxity OAE 1 d. Major and trace element profiles mirror changing environments of deposition of black shales. In black shales, the...

New petrological and geochemical data lead to a consistent depositional model of the Corg-rich sedimentation within the Pieniny Basin during the mid-Cretaceous. Considerable terrestrial runoff into the Pieniny Basin occurred during the late Albian. Detrital macerals accumulated under aerobic conditions on the shelf and continental slope. Fertilizat...