Mechanistic study of the effects of 8-oxo-7,8-dihydroguanine (8-oxoG) on reporter gene expression in mammalian cells

DNA damage causes replication errors, leading to genetic instability or cell death. Besides that, many types of DNA base modifications have been shown to interfere with transcriptional elongation if they are located in the transcribed DNA strand of active genes, acting as roadblocks for RNA polymerases. It is widely assumed that transcription blockage by endogenous DNA damage is responsible for the early cell senescence in organs and accelerated ageing observed in individuals with compromised nucleotide excision repair.rnThe aims of this work were to design new experimental systems for testing transcription blocking potentials of DNA base modifications in an individual gene and to apply these test systems to the investigation of the effects of a frequent endogenously generated base modification, namely 8-oxo-7,8-hydroxyguanine (8-oxoG), on the gene transcription in cells. Several experimental strategies were employed for this purpose. First, I constructed an episomal vector encoding for a short-lived EGFP-ODC fusion protein and measured expression of the reporter gene in permanently transfected clonal cell lines exposed to DNA damaging agents. Second, the expression of plasmid-borne EGFP gene damaged with photosensitisers to obtain one or several oxidative purine modifications per plasmid molecule was determined in transiently transfected human and mouse host cells in an approach known as “host cell reactivation”. As a prerequisite for these experiments, a robust method of precise quantitative measurement of the EGFP gene expression in transiently transfected cells by flow cytometry was developed and validated. Third, I elaborated a very efficient procedure for insertion of synthetic oligonucleotides carrying 8-oxoG into plasmid DNA, avoiding any unwanted base damage and strand breaks. The consequences of 8-oxoG placed in defined positions in opposing DNA strands of the EGFP gene for transcription were measured by host cell reactivation in cells with functional 8-oxoguanine DNA glycosylase (OGG1) gene and in OGG1 null cells.rnThe results obtained in Ogg1-/- cells demonstrated that unrepaired 8-oxoG, even if situated in the transcribed DNA strand, does not have any negative effect on the reporter gene transcription. On the other hand, as few as one 8-oxoG was sufficient to cause a significant decrease of the gene expression in OGG1-proficient cell lines, i.e. in the presence of base excision repair. For two analysed positions of 8-oxoG in the plasmid DNA, the inhibition of gene transcription by the base modification correlated with the efficiency of its excision by purified OGG1 protein under cell-free conditions. Based on these findings, it has to be concluded that the observed decrease of transcription is mediated by excision of the base modification by OGG1 and probably caused by the repair-induced single-strand breaks. The mechanism of transcription inhibition by 8-oxoG is therefore clearly distinct from stalling of elongating RNA polymerase II complexes at the modified base.

Forward modelling of petrological crust-forming processes on the early Earth

Tonalite-trondhjemite-granodiorite (TTG) gneisses form up to two-thirds of the preserved Archean continental crust and there is considerable debate regarding the primary magmatic processes of the generation of these rocks. The popular theories indicate that these rocks were formed by partial melting of basaltic oceanic crust which was previously metamorphosed to garnet-amphibolite and/or eclogite facies conditions either at the base of thick oceanic crust or by subduction processes.rnThis study investigates a new aspect regarding the source rock for Archean continental crust which is inferred to have had a bulk compostion richer in magnesium (picrite) than present-day basaltic oceanic crust. This difference is supposed to originate from a higher geothermal gradient in the early Archean which may have induced higher degrees of partial melting in the mantle, which resulted in a thicker and more magnesian oceanic crust. rnThe methods used to investigate the role of a more MgO-rich source rock in the formation of TTG-like melts in the context of this new approach are mineral equilibria calculations with the software THERMOCALC and high-pressure experiments conducted from 10–20 kbar and 900–1100 °C, both combined in a forward modelling approach. Initially, P–T pseudosections for natural rock compositions with increasing MgO contents were calculated in the system NCFMASHTO (Na2O–CaO–FeO–MgO–Al2O3–SiO2–H2O–TiO2) to ascertain the metamorphic products from rocks with increasing MgO contents from a MORB up to a komatiite. A small number of previous experiments on komatiites showed the development of pyroxenite instead of eclogite and garnet-amphibolite during metamorphism and established that melts of these pyroxenites are of basaltic composition, thus again building oceanic crust instead of continental crust.rnThe P–T pseudosections calculated represent a continuous development of their metamorphic products from amphibolites and eclogites towards pyroxenites. On the basis of these calculations and the changes within the range of compositions, three picritic Models of Archean Oceanic Crust (MAOC) were established with different MgO contents (11, 13 and 15 wt%) ranging between basalt and komatiite. The thermodynamic modelling for MAOC 11, 13 and 15 at supersolidus conditions is imprecise since no appropriate melt model for metabasic rocks is currently available and the melt model for metapelitic rocks resulted in unsatisfactory calculations. The partially molten region is therfore covered by high-pressure experiments. The results of the experiments show a transition from predominantly tonalitic melts in MAOC 11 to basaltic melts in MAOC 15 and a solidus moving towards higher temperatures with increasing magnesium in the bulk composition. Tonalitic melts were generated in MAOC 11 and 13 at pressures up to 12.5 kbar in the presence of garnet, clinopyroxene, plagioclase plus/minus quartz (plus/minus orthopyroxene in the presence of quartz and at lower pressures) in the absence of amphibole but it could not be explicitly indicated whether the tonalitic melts coexisting with an eclogitic residue and rutile at 20 kbar do belong to the Archean TTG suite. Basaltic melts were generated predominantly in the presence of granulite facies residues such as amphibole plus/minus garnet, plagioclase, orthopyroxene that lack quartz in all MAOC compositions at pressures up to 15 kbar. rnThe tonalitic melts generated in MAOC 11 and 13 indicate that thicker oceanic crust with more magnesium than that of a modern basalt is also a viable source for the generation of TTG-like melts and therefore continental crust in the Archean. The experimental results are related to different geologic settings as a function of pressure. The favoured setting for the generation of early TTG-like melts at 15 kbar is the base of an oceanic crust thicker than existing today or by melting of slabs in shallow subduction zones, both without interaction of tonalic melts with the mantle. Tonalitic melts at 20 kbar may have been generated below the plagioclase stability by slab melting in deeper subduction zones that have developed with time during the progressive cooling of the Earth, but it is unlikely that those melts reached lower pressure levels without further mantle interaction.rn

Effects of glucocorticoids on vascular NADPH oxidases and endothelial NO synthase

Glukokortikoide (GCs) stellen wichtige Hormone in der Regulation der metabolischen Homöostase dar. Synthetische GCs, wie Dexamethasone (DEX), spielen eine essentielle Rolle in der Behandlung inflammatorischer Krankheiten. Jedoch sind unter einer Dexamethason-Therapie zahlreiche Nebenwirkungen bekannt, so z.B. auch die Entwicklung einer Hypertonie, in deren Pathogenese oxidativer Stress eine entscheidende Rolle spielt. Obwohl sich in den vergangenen Jahren zahlreiche Studien zum Ziel setzten die GC-induzierte Hypertonie (GC-HT) aufzuklären, sind die genauen Mechanismen bis heute unklar. Eine erhöhte Expression von NADPH Oxidasen (Nox) und eine Entkopplung der endothelialen NO Synthase (eNOS), die Hauptquellen reaktiver Sauerstoffspezies (ROS) im vaskulären System, tragen maßgeblich zur Pathogenese kardiovaskulärer Erkrankungen bei. Daher ist eine Beteiligung dieser Enzyme in GC-induziertem oxidativen Stress sehr wahrscheinlich. Folglich wurde die Hypothese aufgestellt, dass NADPH Oxidasen und eine entkoppelte eNOS die vielversprechendsten unter den zahlreichen involvierten pro- und anti-oxidativen Enzymen sind. Mit Fokus auf die oben genannten Systeme wurde in der vorliegenden Studie der Effekt von DEX mit Hilfe von in vivo (WKY Ratten) ebenso wie in vitro Experimenten (A7r5 und EA.hy 926 Zellen) untersucht. Dabei zeigte sich, dass Nox1, Nox4 und p22phox durch DEX unterschiedlich reguliert wurden. Nox1 wurde hoch-, Nox4 hingegen herunterreguliert, während p22phox unverändert blieb. Die Modufikation schien hierbei auf transkriptioneller und post-transkriptioneller Ebene stattzufinden. Durch die gegensätzliche Regulation von Nox1 und Nox4 bleibt die Nettowirkung der verschiedenen Nox Isoformen unklar. Immer mehr Studien bringen vaskulären oxidativen Stress mit der Pathogenese einer GC-HT in Zusammenhang, welche letztendlich zu einer verminderten Bioverfügbarkeit von Stickstoffmonoxid (NO) führt. Durch die eNOS produziertes NO stellt einen essentiellen Schutzfaktor der Blutgefäße dar. Eine verminderte NO-Bioverfügbarkeit könnte die Folge einer eNOS-Entkopplung darstellen, ausgelöst durch oxidativen Stress. Da die Verfügbarkeit von Tetrahydrobiopterin (BH4) entscheident ist für die Aktivität und enzymatische Kopplung der eNOS, beschäftigt sich die vorliegende Arbeit mit GC-induzierten Veränderungen in der BH4-Versorgung. Die Behandlung von EA.hy 926 Zellen mit DEX führte zu einer zeit- und konzentrationsabhängigen Herunterregulation von eNOS auf mRNA- und Proteinebene. Gleichzeitig wurde die Phosphorylierung an Serine1177 vermindert. Als maßgeblicher “Kopplungs-Schalter” kann BH4 endogen über zwei verschiedene Signalwege synthetisiert werden, welche durch die Enzyme GCH1 und DHFR reguliert werden. DEX führte zu einer zeit- und konzentrationsabhängigen Herunterregulation von BH4, BH2 und Biopterin, wobei ebenso das BH4 / BH2 -Verhältnis vermindert wurde. Beide Enzyme, GCH1 genauso wie DHFR, wurden auf mRNA- und Proteinebene herunterreguliert, was auf einen Effekt von GCs auf beide rnBH4-produzierenden Signalwege schließen lässt. Nach Behandlung mit DEX wurde die Produktion von NO in Endothelzellen maßgeblich vermindert. In ROS-Messungen zeigte sich eine Tendenz hin zu einer eNOS-Entkopplung, jedoch war es mit unserem experimentellen Aufbau nicht möglich, diese endgültig zu beweisen.rnZusammenfassend lässt sich sagen, dass die Behandlung mit GCs zu Veränderungen in beiden untersuchten Systemen, den NADPH Oxidasen ebenso wie dem eNOS-NO System, führte. DEX erhöhte die Expression von Nox1 in glatten Muskelzellen und reduzierte die Nox4-Expression in Endothelzellen. Gleichzeitig verminderte DEX die Verfügbarkeit von BH4 und inhibierte die Phosphorylierung / Aktivität von eNOS. Mithilfe weiterer Studien muss die endgültige Beteiligung von NADPH Oxidasen und einer eNOS-Entkopplung an oxidativem Stress in GC-HT abschließend aufgeklärt werden.rn

Polymer surfaces on small length- and short time-scales

The behaviour of a polymer depends strongly on the length- and time scale as well as on the temperature rnat which it is probed. In this work, I describe investigations of polymer surfaces using scanning probe rnmicroscopy with heatable probes. With these probes, surfaces can be heated within seconds down to rnmicroseconds. I introduce experiments for the local and fast determination of glass transition and melting rntemperatures. I developed a method which allows the determination of glass transition and melting rntemperatures on films with thicknesses below 100 nm: A background measurement on the substrate was rnperformed. The resulting curve was subtracted from the measurement on the polymer film. The rndifferential measurement on polystyrene films with thicknesses between 35 nm and 160 nm showed rncharacteristic signals at 95 ± 1 °C, in accordance with the glass transition of polystyrene. Pressing heated rnprobes into polymer films causes plastic deformation. Nanometer sized deformations are currently rninvestigated in novel concepts for high density data storage. A suitable medium for such a storage system rnhas to be easily indentable on one hand, but on the other hand it also has to be very stable towards rnsurface induced wear. For developing such a medium I investigated a new approach: A comparably soft rnmaterial, namely polystyrene, was protected with a thin but very hard layer made of plasma polymerized rnnorbornene. The resulting bilayered media were tested for surface stability and deformability. I showed rnthat the bilayered material combines the deformability of polystyrene with the surface stability of the rnplasma polymer, and that the material therefore is a very good storage medium. In addition we rninvestigated the glass transition temperature of polystyrene at timescales of 10 µs and found it to be rnapprox. 220 °C. The increase of this characteristic temperature of the polymer results from the short time rnat which the polymer was probed and reflects the well-known time-temperature superposition principle. rnHeatable probes were also used for the characterization of silverazide filled nanocapsules. The use of rnheatable probes allowed determining the decomposition temperature of the capsules from few rnnanograms of material. The measured decomposition temperatures ranged from 180 °C to 225 °C, in rnaccordance with literature values. The investigation of small amounts of sample was necessary due to the rnlimited availability of the material. Furthermore, investigating larger amounts of the capsules using rnconventional thermal gravimetric analysis could lead to contamination or even damage of the instrument. rnBesides the analysis of material parameters I used the heatable probes for the local thermal rndecomposition of pentacene precursor material in order to form nanoscale conductive structures. Here, rnthe thickness of the precursor layer was important for complete thermal decomposition. rnAnother aspect of my work was the investigation of redox active polymers - Poly-10-(4-vinylbenzyl)-10H-rnphenothiazine (PVBPT)- for data storage. Data is stored by changing the local conductivity of the material rnby applying a voltage between tip and surface. The generated structures were stable for more than 16 h. It rnwas shown that the presence of water is essential for succesfull patterning.

Global modeling of pollutant transport and deposition from anthropogenic emission hot spots on global scale

Urban centers significantly contribute to anthropogenic air pollution, although they cover only a minor fraction of the Earth's land surface. Since the worldwide degree of urbanization is steadily increasing, the anthropogenic contribution to air pollution from urban centers is expected to become more substantial in future air quality assessments. The main objective of this thesis was to obtain a more profound insight in the dispersion and the deposition of aerosol particles from 46 individual major population centers (MPCs) as well as the regional and global influence on the atmospheric distribution of several aerosol types. For the first time, this was assessed in one model framework, for which the global model EMAC was applied with different representations of aerosol particles. First, in an approach with passive tracers and a setup in which the results depend only on the source location and the size and the solubility of the tracers, several metrics and a regional climate classification were used to quantify the major outflow pathways, both vertically and horizontally, and to compare the balance between pollution export away from and pollution build-up around the source points. Then in a more comprehensive approach, the anthropogenic emissions of key trace species were changed at the MPC locations to determine the cumulative impact of the MPC emissions on the atmospheric aerosol burdens of black carbon, particulate organic matter, sulfate, and nitrate. Ten different mono-modal passive aerosol tracers were continuously released at the same constant rate at each emission point. The results clearly showed that on average about five times more mass is advected quasi-horizontally at low levels than exported into the upper troposphere. The strength of the low-level export is mainly determined by the location of the source, while the vertical transport is mainly governed by the lifting potential and the solubility of the tracers. Similar to insoluble gas phase tracers, the low-level export of aerosol tracers is strongest at middle and high latitudes, while the regions of strongest vertical export differ between aerosol (temperate winter dry) and gas phase (tropics) tracers. The emitted mass fraction that is kept around MPCs is largest in regions where aerosol tracers have short lifetimes; this mass is also critical for assessing the impact on humans. However, the number of people who live in a strongly polluted region around urban centers depends more on the population density than on the size of the area which is affected by strong air pollution. Another major result was that fine aerosol particles (diameters smaller than 2.5 micrometer) from MPCs undergo substantial long-range transport, with about half of the emitted mass being deposited beyond 1000 km away from the source. In contrast to this diluted remote deposition, there are areas around the MPCs which experience high deposition rates, especially in regions which are frequently affected by heavy precipitation or are situated in poorly ventilated locations. Moreover, most MPC aerosol emissions are removed over land surfaces. In particular, forests experience more deposition from MPC pollutants than other land ecosystems. In addition, it was found that the generic treatment of aerosols has no substantial influence on the major conclusions drawn in this thesis. Moreover, in the more comprehensive approach, it was found that emissions of black carbon, particulate organic matter, sulfur dioxide, and nitrogen oxides from MPCs influence the atmospheric burden of various aerosol types very differently, with impacts generally being larger for secondary species, sulfate and nitrate, than for primary species, black carbon and particulate organic matter. While the changes in the burdens of sulfate, black carbon, and particulate organic matter show an almost linear response for changes in the emission strength, the formation of nitrate was found to be contingent upon many more factors, e.g., the abundance of sulfuric acid, than only upon the strength of the nitrogen oxide emissions. The generic tracer experiments were further extended to conduct the first risk assessment to obtain the cumulative risk of contamination from multiple nuclear reactor accidents on the global scale. For this, many factors had to be taken into account: the probability of major accidents, the cumulative deposition field of the radionuclide cesium-137, and a threshold value that defines contamination. By collecting the necessary data and after accounting for uncertainties, it was found that the risk is highest in western Europe, the eastern US, and in Japan, where on average contamination by major accidents is expected about every 50 years.