From polymer precursors to metal oxides

We report on a strategy to prepare metal oxides including binary oxide and mixed metal oxide (MMO) in form of nanometer-sized particles using polymer as precursor. Zinc oxide nanoparticles are prepared as an example. The obtained zinc polyacrylate precursor is amorphous as confirmed by X-ray diffraction (XRD) and transmission electron microscopy (TEM). The conversion from polymer precursor to ZnO nanocrystals by thermal pyrolysis was investigated by means of XRD, thermogravimetric analysis (TGA) and electron microscopy. The as-synthesized ZnO consists of many individual particles with a diameter around 40 nm as shown by scanning electron microscopy (SEM). The photoluminescence (PL) and electron paramagnetic (EPR) properties of the material are investigated, too. Employing this method, ZnO nanocrystalline films are fabricated via pyrolysis of a zinc polyacrylate precursor film on solid substrate like silicon and quartz glass. The results of XRD, absorption spectra as well as TEM prove that both the ZnO nanopowder and film undergo same evolution process. Comparing the PL properties of films fabricated in different gas atmosphere, it is assigned that the blue emission of the ZnO films is due to crystal defect of zinc vacancy and green emission from oxygen vacancy. Two kinds of ZnO-based mixed metal oxide (Zn1-xMgxO and Zn1-xCoxO) particles with very precise stoichiometry are prepared by controlled pyrolysis of the corresponding polymer precursor at 550 oC. The MMO crystal particles are typically 20-50 nm in diameter. Doping of Mg in ZnO lattice causes shrinkage of lattice parameter c, while it remains unchanged with Co incorporation. Effects of bandgap engineering are seen in the Mg:ZnO system. The photoluminescence in the visible is enhanced by incorporation of magnesium on zinc lattice sites, while the emission is suppressed in the Co:ZnO system. Magnetic property of cobalt doped-ZnO is checked too and ferromagnetic ordering was not found in our samples. An alternative way to prepare zinc oxide nanoparticles is presented upon calcination of zinc-loaded polymer precursors, which is synthesized via inverse miniemulsion polymerization of the mixture of the acrylic acid and zinc nitrate. The as-prepared ZnO product is compared with that obtained from polymer-salt complex method. The obtained ZnO nanoparticles undergo surface modification via a phosphate modifier applying ultrasonication. The morphology of the modified particles is checked by SEM. And stability of the ZnO nanoparticles in aqueous dispersion is enhanced as indicated by the zeta-potential results.

Petrogenetic evolution of Uralian-Alaskan-type mafic-ultramafic complexes in the southern and middle Urals, Russia

The PhD thesis at hand consists of three parts and describes the petrogenetic evolution of Uralian-Alaskan-type mafic ultramafic complexes in the Ural Mountains, Russia. Uralian-Alaskan-type mafic-ultramafic complexes are recognized as a distinct class of intrusions. Characteristic petrologic features are the concentric zonation of a central dunite body grading outward into wehrlite, clinopyroxenite and gabbro, the absence of orthopyroxene and frequently occurring platinum group element (PGE) mineralization. In addition, the presence of ferric iron-rich spinel discriminates Uralian-Alaskan-type complexes from most other mafic ultramafic rock assemblages. The studied Uralian-Alaskan-type complexes (Nizhnii Tagil, Kytlym and Svetley Bor) belong to the southern part of a 900 km long, N–S-trending chain of similar intrusions between the Main Uralian Fault to the west and the Serov-Mauk Fault to the east. The first chapter of this thesis studies the evolution of the ultramafic rocks tracing the compositional variations of rock forming and accessory minerals. The comparison of the chemical composition of olivine, clinopyroxene and chromian spinel from the Urals with data from other localities indicates that they are unique intrusions having a characteristic spinel and clinopyroxene chemistry. Laser ablation-ICPMS (LA-ICPMS ) analyses of trace element concentrations in clinopyroxene are used to calculate the composition of their parental melt which is characterized by enriched LREE (0.5-5.2 prim. mantle) and other highly incompatible elements (U, Th, Ba, Rb) relative to the HREE (0.25-2.0 prim. mantle). A subduction-related geotectonic setting is indicated by a positive anomaly for Sr and negative anomalies for Ti, Zr and Hf. The mineral compositions monitor the evolution of the parental magmas and decipher differences between the studied complexes. In addition, the observed variation in LREE/HREE (for example La/Lu = 2-24) can be best explained with the model of an episodically replenished and erupted open magma chamber system with the extensive fractionation of olivine, spinel and clinopyroxene. The data also show that ankaramites in a subduction-related geotectonic setting could represent parental magmas of Uralian-Alaskan-type complexes. The second chapter of the thesis discusses the chemical variation of major and trace elements in rock-forming minerals of the mafic rocks. Electron microprobe and LA-ICPMS analyses are used to quantitatively describe the petrogenetic relationship between the different gabbroic lithologies and their genetic link to the ultramafic rocks. The composition of clinopyroxene identifies the presence of melts with different trace element abundances on the scale of a thin section and suggests the presence of open system crustal magma chambers. Even on a regional scale the large variation of trace element concentrations and ratios in clinopyroxene (e.g. La/Lu = 3-55) is best explained by the interaction of at least two fundamentally different magma types at various stages of fractionation. This requires the existence of a complex magma chamber system fed with multiple pulses of magmas from at least two different coeval sources in a subduction-related environment. One source produces silica saturated Island arc tholeiitic melts. The second source produces silica undersaturated, ultra-calcic, alkaline melts. Taken these data collectively, the mixing of the two different parental magmas is the dominant petrogenetic process explaining the observed chemical variations. The results further imply that this is an intrinsic feature of Uralian-Alaskan-type complexes and probably of many similar mafic-ultramafic complexes world-wide. In the third chapter of this thesis the major element composition of homogeneous and exsolved spinel is used as a petrogenetic indicator. Homogeneous chromian spinel in dunites and wehrlites monitors the fractionation during the early stages of the magma chamber and the onset of clinopyroxene fractionation as well as the reaction of spinel with interstitial liquid. Exsolved spinel is present in mafic and ultramafic rocks from all three studied complexes. Its composition lies along a solvus curve which defines an equilibrium temperature of 600°C, given that spinel coexists with olivine. This temperature is considered to be close to the temperature of the host rocks into which the studied Uralian-Alaskan-type complexes intruded. The similarity of the exsolution temperatures in the different complexes over a distance of several hundred kilometres implies a regional tectonic event that terminated the exsolution process. This event is potentially associated with the final exhumation of the Uralian-Alaskan-type complexes along the Main Uralian Fault and the Serov-Mauk Fault in the Uralian fold belt.

Consequences of DNA damage for gene transcription : direct effects of modified nucleobases and the role of base excision repair = Folgen von DNA-Schäden für die Gentranskription

The presence of damaged nucleobases in DNA can negatively influence transcription of genes. One of the mechanisms by which DNA damage interferes with reading of genetic information is a direct blockage of the elongating RNA polymerase complexes – an effect well described for bulky adducts induced by several chemical substances and UV-irradiation. However, other mechanisms must exist as well because many of the endogenously occurring non-bulky DNA base modifications have transcription-inhibitory properties in cells, whilstrnnot constituting a roadblock for RNA polymerases under cell free conditions. The inhibition of transcription by non-blocking DNA damage was investigated in this work by employing the reporter gene-based assays. Comparison between various types of DNA damage (UV-induced pyrimidine photoproducts, oxidative purine modifications induced by photosensitisation, defined synthetic modified bases such as 8-oxoguanine and uracil, and sequence-specific single-strand breaks) showed that distinct mechanisms of inhibition of transcription can be engaged, and that DNA repair can influence transcription of the affectedrngenes in several different ways.rnQuantitative expression analyses of reporter genes damaged either by the exposure of cells to UV or delivered into cells by transient transfection supported the earlier evidence that transcription arrest at the damage sites is the major mechanism for the inhibition of transcription by this kind of DNA lesions and that recovery of transcription requires a functional nucleotide excision repair gene Csb (ERCC6) in mouse cells. In contrast, oxidisedrnpurines generated by photosensitisation do not cause transcriptional blockage by a direct mechanism, but rather lead to transcriptional repression of the damaged gene which is associated with altered histone acetylation in the promoter region. The whole chain of events leading to transcriptional silencing in response to DNA damage remains to be uncovered. Yet, the data presented here identify repair-induced single-strand breaks – which arise from excision of damaged bases by the DNA repair glycosylases or endonucleases – as arnputative initiatory factor in this process. Such an indirect mechanism was supported by requirement of the 8-oxoguanine DNA glycosylase (OGG1) for the inhibition of transcription by synthetic 8-oxodG incorporated into a reporter gene and by the delays observed for the inhibition of transcription caused by structurally unrelated base modifications (8-oxoguanine and uracil). It is thereby hypothesized that excision of the modified bases could be a generalrnmechanism for inhibition of transcription by DNA damage which is processed by the base excision repair (BER) pathway. Further gene expression analyses of plasmids containing single-strand breaks or abasic sites in the transcribed sequences revealed strong transcription inhibitory potentials of these lesions, in agreement with the presumption that BER intermediates are largely responsible for the observed effects. Experiments with synthetic base modifications positioned within the defined DNA sequences showed thatrninhibition of transcription did not require the localisation of the lesion in the transcribed DNA strand; therefore the damage sensing mechanism has to be different from the direct encounters of transcribing RNA polymerase complexes with DNA damage.rnAltogether, this work provides new evidence that processing of various DNA basernmodifications by BER can perturb transcription of damaged genes by triggering a gene silencing mechanism. As gene expression can be influenced even by a single DNA damage event, this mechanism could have relevance for the endogenous DNA damage induced in cells under normal physiological conditions, with a possible link to gene silencing in general.