The pre-alpine evolution of the basement of the Pelagonian Zone and the Vardar Zone, Greece

The Pelagonian Zone and the Vardar Zone in Greece represent the western part of the Hellenide hinterland (Internal Hellenides). While the Pelagonian Zone comprises predominantly crystalline basement and sedimentary cover rocks, the Vardar Zone has long been regarded as an ophiolite-decorated suture zone separating the Pelagonian Zone from the Serbo-Macedonian Massif to the east. Felsic basement rocks from both areas, with the main focus put on the Pelagonian Zone, were dated in order to identify the major crust-forming episodes and to improve the understanding of the evolutionary history of the region. The interpretation of the single-zircon geochronology results was aided by geochemical investigations. The majority of the basement rocks from the Pelagonian Zone yielded Permo-Carboniferous intrusion ages around 300 Ma, underlining the importance of this crust-forming event for the Internal Hellenides of Greece. Geochemically these basement rocks are classified as subduction-related granitoids, which formed in an active continental margin setting. An important result was the identification of a Precambrian crustal unit within the crystalline basement of the Pelagonian Zone. Orthogneisses from the NW Pelagonian Zone yielded Neoproterozoic ages of c. 700 Ma and are so far the oldest known rocks in Greece. These basement rocks, which are also similar to active margin granitoids, were interpreted as remnants of a terrane, the Florina Terrane, which can be correlated to a Pan-African or Cadomian arc. Since the gneisses contain inherited zircons of Middle to Late Proterozoic ages, the original location of the Florina Terrane was probably at the northwestern margin of Gondwana. In the Vardar Zone an important phase of Upper Jurassic felsic magmatism is documented by igneous formation ages ranging from 155 to 164 Ma. The chemical and isotopic composition of these rocks is also in accord with their formation in a volcanic-arc setting at an active continental margin. Older continental material incorporated in the Vardar Zone is documented by 319-Ma-old gneisses and by inherited zircons of mainly Middle Palaeozoic ages. The prevalence of subduction-related igneous rocks indicates that arc formation and accretion orogeny were the most important processes during the evolution of this part of the Internal Hellenides. The geochronological results demonstrate that most of the Pelagonian Zone and the Vardar Zone crystalline basement formed during distinct pre-Alpine episodes at c. 700, 300 and 160 Ma with a predominance of the Permo-Carboniferous magmatic phase.

Molecular phylogeography of the Woodland Ringlet (Erebia medusa [Denis and Schiffermüller] 1775) in Europe

Phylogeography is a recent field of biological research that links phylogenetics to biogeography through deciphering the imprint that evolutionary history has left on the genetic structure of extant populations. During the cold phases of the successive ice ages, which drastically shaped species’ distributions since the Pliocene, populations of numerous species were isolated in refugia where many of them evolved into different genetic lineages. My dissertation deals with the phylogeography of the Woodland Ringlet (Erebia medusa [Denis and Schiffermüller] 1775) in Central and Eastern Europe. This Palaearctic butterfly species is currently distributed from central France and south eastern Belgium over large parts of Central Europe and southern Siberia to the Pacific. It is absent from those parts of Europe with mediterranean, oceanic and boreal climates. It was supposed to be a Siberian faunal element with a rather homogeneous population structure in Central Europe due to its postglacial expansion out of a single eastern refugium. An already existing evolutionary scenario for the Woodland Ringlet in Central and Eastern Europe is based on nuclear data (allozymes). To know if this is corroborated by organelle evolutionary history, I sequenced two mitochondrial markers (part of the cytochrome oxydase subunit one and the control region) for populations sampled over the same area. Phylogeography largely relies on the construction of networks of uniparentally inherited haplotypes that are compared to geographic haplotype distribution thanks to recent developed methods such as nested clade phylogeographic analysis (NCPA). Several ring-shaped ambiguities (loops) emerged from both haplotype networks in E. medusa. They can be attributed to recombination and homoplasy. Such loops usually avert the straightforward extraction of the phylogeographic signal contained in a gene tree. I developed several new approaches to extract phylogeographic information in the presence of loops, considering either homoplasy or recombination. This allowed me to deduce a consistent evolutionary history for the species from the mitochondrial data and also adds plausibility for the occurrence of recombination in E. medusa mitochondria. Despite the fact that the control region is assumed to have a lack of resolving power in other species, I found a considerable genetic variation of this marker in E. medusa which makes it a useful tool for phylogeographic studies. In combination with the allozyme data, the mitochondrial genome supports the following phylogeographic scenario for E. medusa in Europe: (i) a first vicariance, due to the onset of the Würm glaciation, led to the formation of several major lineages, and is mirrored in the NCPA by restricted gene flow, (ii) later on further vicariances led to the formation of two sub-lineages in the Western lineage and two sub-lineages in the Eastern lineage during the Last Glacial Maximum or Older Dryas; additionally the NCPA supports a restriction of gene flow with isolation by distance, (iii) finally, vicariance resulted in two secondary sub-lineages in the area of Germany and, maybe, to two other secondary sub-lineages in the Czech Republic. The last postglacial warming was accompanied by strong range expansions in most of the genetic lineages. The scenario expected for a presumably Siberian faunal element such as E. medusa is a continuous loss of genetic diversity during postglacial westward expansion. Hence, the pattern found in this thesis contradicts a typical Siberian origin of E. medusa. In contrast, it corroboratess the importance of multiple extra-Mediterranean refugia for European fauna as it was recently assumed for other continental species.

Die Überarbeitung der Fernsehrichtlinie unter Berücksichtigung der EuGH-Entscheidungen zur bisherigen Fassung

Gegenstand der vorliegenden Arbeit ist die Überarbeitung der Richtlinie 89/552/EWG des Rates zur Koordinierung bestimmter Rechts- und Verwaltungsvorschriften der Mitgliedstaaten über die Ausübung der Fernsehtätigkeit, welche aus praktikablen Gründen meist als „(EG-)Fernsehrichtlinie“ bezeichnet wird. Sie bildet den Eckpfeiler der audiovisuellen Politik der EU. Seit Erlass der Fernsehrichtlinie im Jahre 1989 bewirkt der technologische Fortschritt jedoch zunehmend enorme Veränderungen nicht nur im Bereich des klassischen Fernsehens, sondern auch und vor allem im Bereich der neuen Medien. Ausgangspunkt hierfür ist die Verbesserung der Digitaltechnologie, die ihrerseits wiederum technische Konvergenzprozesse begünstigt. Diese Entwicklungen führen nicht nur zu einer Vervielfachung von Übertragungskapazitäten und –techniken, sondern ermöglichen neben neuen Formen audiovisueller Angebote auch die Entstehung neuer Dienste. Unsere Medienlandschaft steht vor „epochalen Umbrüchen“. Im Hinblick auf diese Vorgänge wird seit geraumer Zeit eine Überarbeitung der EG-Fernsehrichtlinie angestrebt, um dem technologischen Fortschritt auch „regulatorisch“ gerecht werden zu können. Diesem Überarbeitungsprozess möchte sich die vorliegende Arbeit widmen, indem sie die Fernsehrichtlinie in einem ersten Teil sowohl inhaltlich wie auch hinsichtlich ihrer Entstehungsgeschichte und der zu ihr ergangenen EuGH-Entscheidungen erläutert. Anschließend werden alle Überarbeitungsvorgänge der Fernsehrichtlinie seit 1997 dargestellt, um sodann die aktuellen Reformansätze analysieren und bewerten zu können. Aus zeitlichen Gründen (der neue Richtlinienvorschlag der Kommission vom 13. Dezember 2005 wurde ca. 2 Wochen vor dem Abgabetermin der Arbeit verabschiedet) sind die Ausführungen zum Entwurf der neuen „Richtlinie über audiovisuelle Mediendienste“ allerdings relativ knapp gehalten.