Uwarunkowania stratygraficzno-środowiskowe występowania nagromadzeń złożowych bursztynu na północnej Lubelszczyźnie

Słodkowska, Barbara; Kasiński, Jacek Robert; Żarski, Marcin

doi:10.7306/2022.3

Cited by 2 publications

(4 citation statements)

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“…This MPLS-1 is characterised by a maximum thickness of ~20 m, on average 6.3-8.1 m (Bechtel et al 2019(Bechtel et al , 2020Widera et al 2021). Most likely, its deposition started during the last peak of the Mid-Miocene Climatic Optimum (MMCO) and continued when the climate started to cool (Kasiński and Słodkowska 2016;Słodkowska and Kasiński 2016;Słodkowska and Widera 2021). This is supported by tuff dating and calculations of the maximum peat accumulation time.…”

Section: Lithostratigraphymentioning

confidence: 71%

“…This has been well documented palynologically and paleontologically (Planderová et al 1993;Böhme 2003;Holcová et al 2018;Doláková et al 2021). Thus, under conditions of both global and regional cooling, the reduction of air humidity and the increased seasonality of the climate in the foreland of the Alpine-Carpathian orogenic belt, including the Konin Basin area, increased over time (Piwocki and Ziembińska-Tworzydło 1997;Mosbrugger et al 2005;Słodkowska and Kasiński 2016;Utescher et al 2021). At that time (after ~13.8 Ma), the slow tectonic subsidence of the sedimentary basin continued in central Poland, and the rivers flowed to one or more endorheic 'terminal floodplain' basins with a centripetal drainage pattern (Czapowski and Kasiński 2002;Widera 2013a;Widera et al 2017aWidera et al , 2019b.…”

Section: Tectonic and Climatic Changesmentioning

confidence: 81%

“…Most likely, their deposition commenced ~13.8-13.5 Ma, when the Mid-Miocene Climatic Optimum in a broad sense finished (Böhme 2003). At that time the climate become cooler and drier compared to the climatic optimum, with clearly marked seasonality (Kasiński and Słodkowska 2016;Słodkowska and Kasiński 2016). Finally, the Neogene succession is capped by the glaciogenic Quaternary.…”

Section: Lithostratigraphymentioning

confidence: 99%

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Acta Geologica Polonica

Widera

Zieliński

Chomiak

et al. 2020

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Many geological problems have not been convincingly explained so far and are debatable, for instance the origin and changes of the Neogene depositional environments in central Poland. Therefore, these changes have been reconstructed in terms of global to local tectonic and climatic fluctuations. The examined Neogene deposits are divided into a sub-lignite unit (Koźmin Formation), a lignite-bearing unit (Grey Clays Member), and a supra-lignite unit (Wielkopolska Member). The two lithostratigraphic members constitute the Poznań Formation. The results of facies analysis show that the Koźmin Formation was deposited by relatively high-gradient and well-drained braided rivers. Most likely, they encompassed widespread alluvial plains. In the case of the Grey Clays Member, the type of river in close proximity to which the mid-Miocene low-lying mires existed and then were transformed into the first Mid-Miocene Lignite Seam (MPLS-1), has not been resolved. The obtained results confirm the formation of the Wielkopolska Member by low-gradient, but mostly well-drained anastomosing or anastomosing-to-meandering rivers. The depositional evolution of the examined successions depended on tectonic and climatic changes that may be closely related to the mid-Miocene great tectonic remodelling of the Alpine-Carpathian orogen. This resulted in palaeogeographic changes in its foreland in the form of limiting the flow of wet air and water masses from the south and vertical tectonic movements.

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Section: Lithostratigraphymentioning

confidence: 71%

Section: Tectonic and Climatic Changesmentioning

confidence: 81%

Section: Lithostratigraphymentioning

confidence: 99%

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Acta Geologica Polonica

Widera

Zieliński

Chomiak

et al. 2020

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“…In the Eocene deposits, she identified palynologically amber-bearing strata. She also distinguished characteristic dinocyst communities in prospective amber-bearing sediments in the northern Lublin region (Słodkowska & Kasiński, 2016b;Słodkowska et al, 2022). Marzena Kłusek, currently employed at the Silesian University of Technology, studies the anatomy of fossil angiosperm wood (Kłusek, 2012) as well as wood of some coniferous taxa (Kłusek, 2014).…”

Section: History Of the Last Hundred Years Of Polish Palaeobotanical ...mentioning

confidence: 99%

Polish Palaeobotany: 750 Million Years of Plant History as Revealed in a Century of Studies. Research on the Paleogene and Neogene (Tertiary)

Słodkowska

Ziembinska-Tworzydlo

2022

Acta Soc Bot Pol

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On overview of over a hundred years of history of Polish palaeobotanical research on the Paleogene and Neogene (formerly Tertiary) is provided. Profiles of the researchers who laid the foundations for the development of paleofloristic research are presented. In particular, we describe individuals who have made significant research contributions, including M. Raciborski, J. Zabłocki, M. Kostyniuk, H. Czeczott, and W. Szafer. Research centers that were revived after World War II gathered scientists who continued and extended work in the field, including M. Łańucka-Środońowa, J. Oszast, A. Skirgiełło, J. Doktorowicz-Hrebnicka, J. Stachurska, and J. Mamczar. This tradition was maintained and developed by researchers of the next generation: L. Stuchlik, E. Zastawniak, A. Sadowska, M. Ziembińska-Tworzydło, I. Grabowska, H. Ważyńska, A. Hummel, Z. Baranowska-Zarzycka, and A. Kohlman-Adamska. Currently, the fourth generation of Polish palaeobotanists, including B. Słodkowska, E. Worobiec, G. Worobiec, P. Gedl, M. Garecka, E. Durska, and R. Kowalski, conduct multifaceted palaeobotanical research, with links to various fields of knowledge, including botany, geology, and palaeoclimatology. Studies of past changes in plant cover provide important insight current climate change.

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Uwarunkowania stratygraficzno-środowiskowe występowania nagromadzeń złożowych bursztynu na północnej Lubelszczyźnie

Cited by 2 publications

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Acta Geologica Polonica

Acta Geologica Polonica

Polish Palaeobotany: 750 Million Years of Plant History as Revealed in a Century of Studies. Research on the Paleogene and Neogene (Tertiary)

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