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Foraminifera of the Bohemian Cretaceous Basin
Hašková, Barbora ; Holcová, Katarína (advisor) ; Frank, Jiří (referee)
The thesis deals in the compilation part with systematic classification, biology, morphology of the test, ecology and palaeoecology of the Foraminifera. Next research focuses on the history of Cretaceous Foraminifera in our area and the geology of the Bohemian Cretaceous Basin, focusing on Úpohlavy site in the northwestern part of the Bohemian Cretaceous Basin. Three samples from Úpohlavy section were preliminary micropaleontologically analysed. Plankton / bentos ratio was counted. Genus Heterohelix and Planoheterohelix was described and taxonomically studied. Keywords: Upper Cretaceous, Bohemian Cretaceous Basin, Foraminifera, Heterohelix 1
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Problems of the K/T boudary
Pícha, Štěpán ; Košťák, Martin (advisor) ; Holcová, Katarína (referee)
Mass extinction attracts the attention of scientists for a long time. Particularly examined in detail the extinction at the Cretaceous/Tertiary boundary, took place from 65.9 + -0.4 millionyears. There are numerous theories which try to explain the causes that led to the youngest of the five major extinctions in Earth history. Since 1980, when the iridium anomaly has been recorded in sediments , the theory of extraterrestrial cause of the extinctions caused by meteorite or comet was introducet. This theory has partly been confirmed by the findings impact crater in the Gulf of Mexico. Further examination, however, proved that the crater quite significantly precedes the boundary. Attention therefore has turned in another direction,i . e. the terrestrial cause of extinction. More recent scientists pay attention to present-day India and huge volcanic traps that created the Deccan platform.During the examination of the Deccan traps, the unexpected an impact crater structure, which is several times larger than the crater in the Gulf of Mexico, has been discovered This discovery started anew dispute about the main cause of the extinction at the Cretaceous / Tertiary boundary. Based on modern literature, the three major theories of the K/T extinction are discussed. I have tried to focus their causes,...
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The Quaternary Paleoecological Analysis of the Soos National Nature Reserve
Rajdlová, Hana ; Holcová, Katarína (advisor) ; Novák, Jan (referee)
The Quaternary Paleoecological Analysis of the Soos National Nature Reserve The aim of this proposed diploma thesis is to describe the structure of diatom communities in the diatomite deposits of the Soos National Nature Reserve and compare the finding of this thesis with those of older publications. Another aim was to reconstruct the history of the basin trough with the outputs of diatom analysis accomplished in the 3,4 m long sediment profile. The similarity of diatom communites in individual diatomite types was also tested. Key words: subfossil diatoms, Soos National Nature Reserve, paleolimnology, Late Glacial, Holocene
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Marine microorganisms: the complex project in the learning for geology and biology at grammar schools
Minaříková, Veronika ; Holcová, Katarína (advisor) ; Mourek, Jan (referee)
This thesis deals with incorporating microorganisms into teaching. The main idea was to create guide for teachers at high schools, whereby they could create own excursion. Thesis is divided into didactical and practical part, didactical part of thesis is coping with incorporating into teaching, especially into RVP ZV, RVP G and textbooks. Practical part delas with the creating of metodical guide for teachers. This thesis also contains questionnaire analysis of respondent's relationship to biology and geology. Key words: Inquiry lessons, badenian, excusion, miocene, neogene, Carpathian foredeep, microorganisms, "hands-on" activities
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Early Devonian Foraminifera of the Barrandian area
Vaněčková, Anna ; Holcová, Katarína (advisor) ; Tonarová, Petra (referee)
The first part is devoted to basic information on systematics, general biology of foraminifera, morphology of their tests which is important for taxonomy and also on ecology. The following section relates to characteristic of the Devonian, with the emphasis on the Barrandian area and its stratigraphy plus characteristic of the Na Stydlých vodách quarry where samples were taken for the purpose of this thesis. In the last part, results of the Early Devonian foraminifera of the Barrandian area research are compared with similar studies conducted abroad.
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Early Devonian Foraminifera from the Prague Formation
Vaněčková, Anna ; Holcová, Katarína (advisor) ; Tonarová, Petra (referee)
Lower Devonian foraminifera are known from only a few localities globally and thus are not much investigated. The taxonomy, as well as further use of this group is insufficiently known. One of the main areas of research of foraminifera is the Barrandian area in the Czech Republic. This thesis follows previous studies of this territory but focuses particulary on the Prag formation, which has proven to be rich in foraminifera communities. Taxonomic studies were conducted at two Lower Devonian sites, namely the Na Stydlých vodách quarry and the Požáry quarry. The study showed that foraminifera communities described from the Na Stydlých vodách quarry were dominated by the following genera: Hyperammina, Colonammina and Tolypammina. The highest abundance was recorded at the transition of dvorecko-prokopské limestones and řeporyje limestones and in dvorecko-prokopské limestones. At the Požáry quarry, the communities were dominated by tubular genera of Tolypammina, Hyperammina and Bathysiphon and spherical genera of Lagenammina and Colonammina. The abbundance of Colonammina is unusually high, the genus has been described rarely from other parts of the world so far.
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Planktonic ecosystems of the Upper Jurassic and Cretaceous (calcareous nannoplankton, calpionellids)
Svobodová, Andrea ; Holcová, Katarína (advisor) ; Skupien, Petr (referee) ; Oszczypko-Ciowes, Marta (referee)
The presented PhD thesis is compiled as a commentary to four published papers, which deal with planktonic assamblages of the Upper Jurassic and Cretaceous, namely with calcareous nannofossils and calpionellids. The first part of the dissertation thesis describes the main characteristics of the studied fossil groups with focus on their morphology, palaeoecology, evolution and systematics. The chapter of calcareous nannoplankton gives special attention to the biostratigraphicaly important genus Nannoconus Kampter 1931. Next chapters describe the methods of the laboratory processing of the sediments and the geological settings of the studied areas. The thesis is focused on two areas. At first the selected localities in the Bohemian Cretaceous Basin, i.e. Upper Turonian and Upper Coniacian, are described. Generally, the Upper Cretaceous platform sediments of the middle European basins are rich in calcareous nannoplankton. These fossils represent important marker for biostratigraphical and palaeoecological interpretations. The second part describes carbonate rocks of the Upper Jurassic and Lower Cretaceous of the Tethyan area. In this case, calcareous nannoplankton and calpionellids are an essential part of the modern multidisciplinary form of the Jurassic- Cretaceous (J/K) boundary interval research....
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