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Gigantism of Paleozoic insects and other arthropods
Pecharová, Martina ; Prokop, Jakub (advisor) ; Knor, Stanislav (referee)
Gigantism of insects and other arthropods was rather common in Late Paleozoic. Hypothesis of the oxygen limitation is one the probable explanations caused the phenomenon. Carboniferous insect gigantism was probably directly caused by the higher level of atmospheric oxygen due to direct effectiveness on the tracheal system. Therefore the possibility to grow to large sizes is clearly dependent on the amount of available oxygen. Another fact supporting the hypothesis is the extinction or the change of the giant insect forms at the end of the Permian, when the level of atmospheric oxygen suddenly decreased. This thesis also describes the ecological relationships of the Late Paleozoic arthropods, which is clearly connected to the evolution of giant forms. Gigantism during this period was thus developed by the interplay of several factors related to the global elements cycles. Another part covers major groups and representatives of Palaeozoic gigantic insects and other arthropods. The final part is devoted to describing the physiological experiments related to this topic.
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Palaeocology of plant-arthropod associations from the Lower Miocene of the Most Basin in northern Bohemia (Czech Republic)
Knor, Stanislav
Terrestrial plants and insects account for the majority of the Earth's biodiversity today, and almost half of all insect species are herbivores. Thus, insects and plants share ancient associations date back for more than 400 million years. However, investigation of their interactions stands largely at the beginning in Western Europe. Nearly 4300 plant remains showing various kinds of feeding damages are available for the present study. These trace fossils are classified as so-called functional feeding-groups supply an outstanding example of the complexity, the structure and the changes of terrestrial ecosystems, are not well known during this interval. In Europe, the Neogene is characterized by palaeogeographic re- organization due to the collision of the African with the Eurasian plates. The Neogene plant record in Europe is rich and diverse offering a profound large-scale understanding of the floristic and vegetational development. A database of fossil traces from the Most Basin was compiled and analyzed by various statistical methods in terms of the diversity and intensity of palaeo-herbivory. The primary objective is to present results on the development of insect herbivory through the section of the Bílina Mine in North Bohemia, with the aim of understanding principal factors that caused the...
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Plant - insect interactions in lower Miocene of Central Europe: palaeoclimatological and palaeoecological implications
Knor, Stanislav ; Prokop, Jakub (advisor) ; Kvaček, Jiří (referee) ; Mikuláš, Radek (referee)
The paleoecology of plant - arthropod herbivory associations constitute very important source of knowledge about the phylogeny and co-evolution of both groups. The traces of herbivory interactions between plants and arthropods on the fossil leaves are preserved as so called damaged types (DTs) clustered into distinct functional feeding groups (FFGs). The diversity and frequency of these damage traces also seem to have been strongly influenced by environmental and climatic conditions. This research has been focused on rich fossil plant assemblages from the area of the Most Basin in the north-western Bohemia. The undergoing work has comprised the diagnosis of the individual damages on the basis of their specific morphological traits as their number, size, shape and distributional pattern on the leaf surface. The next issue has involved the statistical analyses concerning the differences in the frequency and diversity of the types of damage and functional feeding groups between two separate fossiliferous layers, namely those of the stratigraphically older Bílina Delta and younger Břešťany Clay. Significant differences were confirmed in this regard, especially in connection with achieved frequency and proportional occurrences of distinct functional feeding groups in the Bílina Delta. The galls were the...
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Palaeocology of plant-arthropod associations from the Lower Miocene of the Most Basin in northern Bohemia (Czech Republic)
Knor, Stanislav
Terrestrial plants and insects account for the majority of the Earth's biodiversity today, and almost half of all insect species are herbivores. Thus, insects and plants share ancient associations date back for more than 400 million years. However, investigation of their interactions stands largely at the beginning in Western Europe. Nearly 4300 plant remains showing various kinds of feeding damages are available for the present study. These trace fossils are classified as so-called functional feeding-groups supply an outstanding example of the complexity, the structure and the changes of terrestrial ecosystems, are not well known during this interval. In Europe, the Neogene is characterized by palaeogeographic re- organization due to the collision of the African with the Eurasian plates. The Neogene plant record in Europe is rich and diverse offering a profound large-scale understanding of the floristic and vegetational development. A database of fossil traces from the Most Basin was compiled and analyzed by various statistical methods in terms of the diversity and intensity of palaeo-herbivory. The primary objective is to present results on the development of insect herbivory through the section of the Bílina Mine in North Bohemia, with the aim of understanding principal factors that caused the...
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Gigantism of Paleozoic insects and other arthropods
Pecharová, Martina ; Prokop, Jakub (advisor) ; Knor, Stanislav (referee)
Gigantism of insects and other arthropods was rather common in Late Paleozoic. Hypothesis of the oxygen limitation is one the probable explanations caused the phenomenon. Carboniferous insect gigantism was probably directly caused by the higher level of atmospheric oxygen due to direct effectiveness on the tracheal system. Therefore the possibility to grow to large sizes is clearly dependent on the amount of available oxygen. Another fact supporting the hypothesis is the extinction or the change of the giant insect forms at the end of the Permian, when the level of atmospheric oxygen suddenly decreased. This thesis also describes the ecological relationships of the Late Paleozoic arthropods, which is clearly connected to the evolution of giant forms. Gigantism during this period was thus developed by the interplay of several factors related to the global elements cycles. Another part covers major groups and representatives of Palaeozoic gigantic insects and other arthropods. The final part is devoted to describing the physiological experiments related to this topic.
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Palaeocology of plant-arthropod associations from the Lower Miocene of the Most Basin in northern Bohemia (Czech Republic)
Knor, Stanislav ; Prokop, Jakub (advisor) ; Teodoridis, Vasilis (referee)
Terrestrial plants and insects account for the majority of the Earth's biodiversity today, and almost half of all insect species are herbivores. Thus, insects and plants share ancient associations date back for more than 400 million years. However, investigation of their interactions stands largely at the beginning in Western Europe. Nearly 4300 plant remains showing various kinds of feeding damages are available for the present study. These trace fossils are classified as so-called functional feeding-groups supply an outstanding example of the complexity, the structure and the changes of terrestrial ecosystems, are not well known during this interval. In Europe, the Neogene is characterized by palaeogeographic re- organization due to the collision of the African with the Eurasian plates. The Neogene plant record in Europe is rich and diverse offering a profound large-scale understanding of the floristic and vegetational development. A database of fossil traces from the Most Basin was compiled and analyzed by various statistical methods in terms of the diversity and intensity of palaeo-herbivory. The primary objective is to present results on the development of insect herbivory through the section of the Bílina Mine in North Bohemia, with the aim of understanding principal factors that caused the...
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