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The phylogeny of the Protaetia Burmeister, 1842 flower beetles in the western palearctic region
Žďárská, Kateřina ; Šípek, Petr (advisor) ; Bezděk, Aleš (referee)
This diploma thesis deals with the phylogeny and phylogeography of flower beetles of the genus Protaetia, especially with the complicated taxonomic complex around the species Protaetia (Potosia) cuprea, P. cuprina and P. caucasica in the western Palearctic region. In light of the results presented by Vondráček et al. (2018), it seems that the classic taxonomic approach, based only on coloration, geographical distribution or poorly analysed morphological characters, is not able to adequately explain the evolution of the taxon, nor correctly identify individual taxa at the species level (i.e. species and subspecies). To understand the evolution of the group and the population structure, it is therefore necessary to use the now standard molecular-phylogenetic approaches as well. Based on analyses of one nuclear (internal transcribed spacer 1) and two mitochondrial genes (cytochrome oxidase I and cytochrome b) from 231 individuals, a phylogenetic hypothesis of the West Palaearctic representatives of the genus Protaetia was compiled. It was found that the currently recognized subgenera of the genus do not correspond to the results of the analyses. The subgenera Eupotosia, Netocia and Potosia proved to be non- monophyletic. Within the species complex of P. cuprea, in addition to the European clade of P....
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Biogeography of the Balkan Peninsula: geological development and recent state of knowledge
Žďárská, Kateřina ; Šípek, Petr (advisor) ; Král, David (referee)
The aim of this study is to summarize history and development of Mediterranean with a following description and comparison of the biogeographical regions of the Balkan peninsula and surrounding areas. Balkan peninsula is located in eastern-central Mediterranean, which is known for its complex paleogeographic evolution. Current presence and distribution of organisms with high rate of endemism is influenced by several factors. For example orogenesis, the fragmentation of the Tethys ocean in Miocene (16 - 18 Ma), the birth and progression of the Paratethys sea and the Messinian salinity crissis (MSC, 5.97 - 5.33 Ma), followed with enormous ecological changes in whole Mediterranean. In this period, landbridges were formed and they allowed migration of species between African, Arabian and Eurasian tectonic plate. Another important period that formed present Mediterranean is Quarternary period in which this area is influenced by climatic oscillations leading to alternation of glacial and interglacial phases. Simultaneously, the sea level oscilations and migrations of species occured, which resulted into the creation of various refugia.
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