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Impact of volcanic activity on environment and climatic conditions during geological history of the České středohoří Mts.
Zajícová, Jana ; Kvaček, Zlatko (advisor) ; Teodoridis, Vasilis (referee)
The influence of volcanoes on climate is very often debated, not only in the scientific community. However, the question remains, how much may the volcanic activity contribute to the significant ganges, that could cause a response of environment, which lies in the immediate vicinity. These changes could arise as a response on prolonged exposure of the negative influence, which would last much longer than decades, like it is at present. From this reason the situation in the České středohoří Mountains, where the volcanic activity lasted for several million years during the Paleogene period, is studied. This area is extraordinally rich in deposits of so-called volcanic floras, which accompany the neovolcanic activity. The age of the localities are between late Eocene to late Oligocene and it is a long time enough for recognizing some changes in the floristic composition to help elucidate the given problem.
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Palynology of selected coal seams and accompanying sediments of the Laziska and Libiaz Beds (Moscovian) in the Polish part of the Upper Silesian Basin
Bojdová, Lenka ; Opluštil, Stanislav (advisor) ; Kvaček, Zlatko (referee)
This thesis summarizes palynological and paleontological study of the middle part of the Cracow Sandstone Series which is divided into the Łaziska (Bolsovian) and the Libiąz Beds (Asturian). Samples were obtained from the borehole G5 Dab nearby Jaworzno from both coal and non-coal sediments. Palynological study confirmed the stratigraphical gap between these two beds by observation of dissapearance of nine miospore taxons at the bottom of the Libiąz Beds (Torispora, Converrucosisporites, Schulzospora, Gillespieisporites, Schopfites, Convolutispora, Cristatisporites, Tripartites, Cingulizonates). Different ecological demands during the coal and non-coal sedimentation were confirmed. The sedimentation of the Łaziska coal seams is characterized by alternation of lycospore and densospore phases which confirmes alternation of the contrasting plant assamblages with a predominance of the arborescent lycopsids Lepidodendron and Lepidophloios and sub-arborescent lycopsid Omphalophloios. Arborescent lycopsids preferred planar (rheotrophic) mires. Plant assamblages with predominance of the lycopsid Omphalophloios colonized drier peat swamps with fluctuating water level (ombrothrophic). Peat swamp vegetation in Libiąz Beds was damper with localy transitional phase with increased incidence of the genus...
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Carboniferous flora of the Czech part of the Upper Silesian Basin and its stratigraphic importance
Bojdová, Lenka ; Opluštil, Stanislav (advisor) ; Kvaček, Zlatko (referee)
This thesis provides an overview of the Carboniferous flora in the Czech part of the Upper Silesian Basin and its applications in stratigraphy. The sediments of the Upper Silesian Basin with wetland carboniferous vegetation were deposited for about 10 million years. During this period, the floristic character was varying. According to the associations of species we can divide the filling into the stratigraphical units. The basin includes lycopodiophytes, horsetails, ferns, fern-like plants, cordaites, and ginkophytes. The filling began by the Ostrava formation with paralic basin flora with the leading species Sphenopteris adiantoides. Coal seams alternate with non-coal facies with culm flora. Thanks to the paleogeographic changes and marine transgression, the floristic associations changed. Sk. f. h. Enny is the major borderline between middle and upper floristic zones of the lower Namur, in which culm flora disappeared. After the hiatus, Karvinská formation with the important seam Prokop sediments. The formation is characterized by middle Namurian to the Lower Westphalian plants, without non-coal sections. The Upper Namurian plants are located in the sedlové and sušské layers. In the lower sušské layers the biostratigraphical interface of Namur/Westphal is indicated by Lyginopteris hoeninghausii....
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Palaeoclimatic study of the Cenomanian flora of Bohemian Massif
Čepičková, Jana ; Kvaček, Zlatko (advisor) ; Sakala, Jakub (referee)
The aim of this research is to analyse selected plant species from the specific Cenomanian deposits of the Bohemian Cretaceous Basin and their subsequent observation for determining climatic conditions in the Cenomanian age. Fossil plants that will serve to show signs come from two localities, specifically Prague, Slivenec and Prague, Malá Chuchle and are stored in the National Museum in the depository in Horní Počernice. For a more complete view of the Cenomanian in the Bohemian Cretaceous Basin are used the descriptions of the locations Prague, Hloubětín and Vyšehořovice. The default method for detecting the paleoclimatic signal is the CLAMP (Climate Leaf Analysis Multivariate Program) analysis, which sets out the approximate climatic conditions that dominated in the Cenomanian. Key words: palaeoclimatology, Cenomanian flora, Bohemian Massif
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Overview of the fossil bryophytes of the Cretaceous and Tertiary of Bohemian Massif
Veselá, Veronika ; Kvaček, Zlatko (advisor) ; Kvaček, Jiří (referee)
The bachelor thesis summarizes the findings about previously described and published findings of bryophytes from the period of Cretaceous and Tertiary on the territory of the Bohemian Massif. It contains a chapter with current knowledge of taxonomy and life strategies of bryophytes, used to approach the studied groups. Part of the thesis is dedicate to the brief characteristics of the geological settings of locations with known findings of fossil bryophyte. Those locations are situated mainly in the České středohoří Mountains, the Bohemian Cretaceous Basin and the Českobudějovická Basin. For example and comparison are involved also two locations from Outer Western Carpathian. There are only two liverwort species (Notothylacites filiformis and Riccia cf. fluitans) and a few mosses (Hypnum heppii, Muscites sp.) described so far. Because of partial preservation of most of the findings any detailed systematical attribution remains ambiquous. The thesis has purely review character and is supposed to become a basis for further research and study. Key words: Bryophyta, Czech Cretaceous and Tertiary, review
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Impact of volcanic activity on environment and climatic conditions during geological history of the České středohoří Mts.
Zajícová, Jana ; Kvaček, Zlatko (advisor) ; Teodoridis, Vasilis (referee)
The influence of volcanoes on climate is very often debated, not only in the scientific community. However, the question remains, how much may the volcanic activity contribute to the significant ganges, that could cause a response of environment, which lies in the immediate vicinity. These changes could arise as a response on prolonged exposure of the negative influence, which would last much longer than decades, like it is at present. From this reason the situation in the České středohoří Mountains, where the volcanic activity lasted for several million years during the Paleogene period, is studied. This area is extraordinally rich in deposits of so-called volcanic floras, which accompany the neovolcanic activity. The age of the localities are between late Eocene to late Oligocene and it is a long time enough for recognizing some changes in the floristic composition to help elucidate the given problem.
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Palynology of selected coal seams and accompanying sediments of the Laziska and Libiaz Beds (Moscovian) in the Polish part of the Upper Silesian Basin
Bojdová, Lenka ; Opluštil, Stanislav (advisor) ; Kvaček, Zlatko (referee)
This thesis summarizes palynological and paleontological study of the middle part of the Cracow Sandstone Series which is divided into the Łaziska (Bolsovian) and the Libiąz Beds (Asturian). Samples were obtained from the borehole G5 Dab nearby Jaworzno from both coal and non-coal sediments. Palynological study confirmed the stratigraphical gap between these two beds by observation of dissapearance of nine miospore taxons at the bottom of the Libiąz Beds (Torispora, Converrucosisporites, Schulzospora, Gillespieisporites, Schopfites, Convolutispora, Cristatisporites, Tripartites, Cingulizonates). Different ecological demands during the coal and non-coal sedimentation were confirmed. The sedimentation of the Łaziska coal seams is characterized by alternation of lycospore and densospore phases which confirmes alternation of the contrasting plant assamblages with a predominance of the arborescent lycopsids Lepidodendron and Lepidophloios and sub-arborescent lycopsid Omphalophloios. Arborescent lycopsids preferred planar (rheotrophic) mires. Plant assamblages with predominance of the lycopsid Omphalophloios colonized drier peat swamps with fluctuating water level (ombrothrophic). Peat swamp vegetation in Libiąz Beds was damper with localy transitional phase with increased incidence of the genus...
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Carboniferous flora of the Czech part of the Upper Silesian Basin and its stratigraphic importance
Bojdová, Lenka ; Opluštil, Stanislav (advisor) ; Kvaček, Zlatko (referee)
This thesis provides an overview of the Carboniferous flora in the Czech part of the Upper Silesian Basin and its applications in stratigraphy. The sediments of the Upper Silesian Basin with wetland carboniferous vegetation were deposited for about 10 million years. During this period, the floristic character was varying. According to the associations of species we can divide the filling into the stratigraphical units. The basin includes lycopodiophytes, horsetails, ferns, fern-like plants, cordaites, and ginkophytes. The filling began by the Ostrava formation with paralic basin flora with the leading species Sphenopteris adiantoides. Coal seams alternate with non-coal facies with culm flora. Thanks to the paleogeographic changes and marine transgression, the floristic associations changed. Sk. f. h. Enny is the major borderline between middle and upper floristic zones of the lower Namur, in which culm flora disappeared. After the hiatus, Karvinská formation with the important seam Prokop sediments. The formation is characterized by middle Namurian to the Lower Westphalian plants, without non-coal sections. The Upper Namurian plants are located in the sedlové and sušské layers. In the lower sušské layers the biostratigraphical interface of Namur/Westphal is indicated by Lyginopteris hoeninghausii....
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