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The present work describes the synthesis of sila-venlafaxine, disila-bexarotene, disila-AG-045572 (disila-CMPD1), a series of silicon-based allosteric modulators of muscarinic receptors, and a partial synthesis of sila-gabapentin. Crystal structure data of rac-sila-venlafaxine hydrochloride, (R)-sila-venlafaxine hydrobromide, bexarotene, disila-bexarotene, and disila-AG-045572 (disila-CMPD1) are included. Studies on the biological activities of sila-venlafaxine and of silicon-based allosteric modulators of muscarinic receptors are discussed. The Si-2,4,6-trimethoxyphenyl (Si-2,4,6-TMOP) moiety is described as a novel, acid-labile protecting group in organosilicon chemistry. The synthesis of chlorotris(chloromethyl)silane and tris(chloromethyl)methoxysilane is described.
Rifting and breakup of Westgondwana in the Late Jurassic/ Early Cretaceous initiated the formation of the South Atlantic and its conjugated pair of passive continental margins. The Walvis Basin offshore NW-Namibia is an Early Cretaceous to recent depositional centre with a typically wedge-shaped postrift sedimentary succession covering an area of 105000km2. A 2D model transect across the central Walvis Basin and adjacent onshore areas is used as a case study to investigate quantitatively the denudational history of the evolving passive margin and the related contemporaneous depositional postrift evolution offshore. The database for both the onshore and offshore part of the model traverse is well constrained by own field work, published data as well as by seismic and well data supported by samples. The ultimate goal of this project is to present an integrated approach towards a quantitative link between surface processes and internal processes in terms of a mass and process balance.
The Upper Cretaceous Ajlun Group (Cenomanian-Turonian) of southern/south-eastern Jordan has been analysed in 15 detailed sections with thicknesses between 40 m and 200 m. Taxonomic, palaeoecological, taphonomic, and sedimentological aspects were taken into account. During the early Upper Cretaceous the study area was situated at the south-eastern margin of the Tethys Ocean, between the palaeo-shoreline in the south-east and an offshore carbonate platform in the west. Thus, the measured sections include a complete facies succession from terrestrial-dominated environments via marginal marine siliciclastics to an area of carbonate precipitation. So far, very little is known about the fauna and the depositional environment of the group, especially of the transitional marginal marine part. Also, in depth studies of the Cretaceous fauna of southern Jordan are very rare. Therefore, the benthic fauna of the area is described in an extensive taxonomic chapter. It consists of 117 taxa, 77 of which are bivalves, 22 gastropods, 9 echinoids, and 4 corals. The phyla Porifera, Bryozoa, and Brachiopoda are represented by 1 species each. Additionally, at least two species of decapod crustaceans were found. One bivalve species is new: Anthonya jordanica from Cenomanian claystones of the eastern study area. 41 quantitative samples of the benthic invertebrate fauna were grouped into nine associations and three assemblages by means of a Q-mode cluster analysis. These are described as remnants of former communities and their environments are discussed. Salinity and substrate consistency are assumed to have been the most important environmental parameters controlling the faunal distribution. The overall palaeo-environment is discussed on the basis of sedimentological and palaeoecological results. It was primarily influenced by the morphology of the sea floor, sediment supply, and salinity of the sea water.
The high-grade metamorphic Epupa Complex (EC) of north-western Namibia constitutes the south-western margin of the Archean to Proterozoic Congo Craton. The north-eastern portion of the EC has been geochemically and petrologically investigated in order to reconstruct its tectono-metamorphic evolution. Two distinct metamorphic units have been recognized, which are separated by ductile shear zones: (1) Upper amphibolite facies rocks (Orue Unit) and (2) ultrahigh-temperature (UHT) granulite facies rocks (Epembe Unit). The rocks of the EC are transsected by a large anorthosite massif, the Kunene Intrusive Complex (KIC). The Orue Unit and the Epembe Unit were affected by two distinct Mesoproterozoic metamorphic events, as is evident from differences in their metamorphic grade, in the P-T paths and in the age of peak-metamorphism: (1) The Orue Unit consists of a Palaeoproterozoic volcano-sedimentary sequence, which was intruded by large masses of I-type granitoids and by rare mafic dykes. During the Mesoproterozoic (1390-1318 Ma) the Orue Unit rocks underwent upper amphibolite facies metamorphism. The volcano-sedimentary sequence is constituted by interlayered basaltic amphibolites and rhyolitic felsic gneisses, with intercalations of migmatitic metagreywackes, migmatitic metapelites, metaarkoses and calc-silicate rocks. The Orue Unit was subdivided into three parts, which record similar heating-cooling paths but represent individual crustal levels: Heating led to the partial replacement of amphibole, biotite and muscovite through dehydration melting reactions. The peak-metamorphic P-T conditions of c. 700°C, 6.5 +/- 1.0 kbar (south-eastern part), c. 820°C, 8 +/- 0.5 kbar (south-western part) and c. 800°C, 6.0 +/- 1.0 kbar (northern part) correlate well with the mineral assemblage in the metapelites, i.e. Grt-Bt-Sil gneisses and schist in the south-eastern and south-western region and (Grt-)Crd-Bt gneisses in the northern part. Peak-metamorphism was followed by retrograde cooling to middle amphibolite facies conditions. Contact metamorphism, related with the intrusion of the anorthosites, is restricted to the direct contact to the KIC and recorded by massive metapelitic Grt-Sil-Crd felses, formed under upper amphibolite facies conditions (c. 750°C, c. 6.5 kbar). (2) The Epembe Unit consists of a Palaeoproterozoic volcano-sedimentary succession, which was intruded by small bodies of S-type granitoids and by andesitic dykes. All these rocks underwent UHT granulite facies metamorphism during the early Mesoproterozoic (1520-1447 Ma). The volcano-sedimentary succession is dominated by interlayered basaltic two-pyroxene granulites and rhyolitic felsic granulites. Migmatitic metapelites and metagreywackes are intercalated in the metavolcanites. Sapphirine-bearing MgAl-rich gneisses occur as restitic schlieren in the migmatitic metagreywackes. Reconstructed anti-clockwise P-T paths are subdivided into several distinct stages: During prograde near-isobaric heating to UHT conditions at c. 7 kbar biotite- or hornblende-bearing mineral assemblages were almost completely replaced by anhydrous mineral assemblages through various dehydration melting reactions. A subsequent pressure increase of 2-3 kbar led to the formation of the peak-metamorphic mineral assemblages Grt-Opx and (Grt-)Opx-Cpx in the orthogneisses and Grt-Opx, Grt-Sil and (Grt-)(Spr-)Opx-Sil-Qtz in the paragneisses. UHT-Metamorphism is proved by conventional geothermobarometry (970 +/- 70°C; 9.5 +/- 2.5 kbar), by the very high Al content of peak-metamorphic orthopyroxene (up to 11.9 wt.% Al2O3) in many paragneisses and by Opx-Sil-Qtz assemblages in the MgAl-rich gneisses. Post-peak decompression is recorded by several corona and symplectite textures, formed at the expense of the peak-metamorphic phases: Initial UHT decompression of about ca. 2 kbar to 940 +/- 60°C at 8 +/- 2 kbar is mainly evident from the formation of sapphirine-bearing symplectites in the Opx-Sil gneisses. Subsequent high-temperature decompression to 6 +/- 2 kbar at 800 +/- 60°C resulted in the formation of Crd-Opx-Spl, Crd-Opx and Spl-Crd symplectites. Subsequent near-isobaric cooling to upper amphibolite conditions of 660 +/- 30°C at 5 +/- 1.5 kbar led to the re-growth of biotite, hornblende, sillimanite and garnet. During continued decompression orthopyroxene and cordierite were formed at the expense of biotite in several paragneisses. In a geodynamic model UHT metamorphism of the Epembe Unit is correlated with the formation of a large magma chamber at the mantle-crust boundary, which forms the source for the anorthosites of the KIC. In contrast, amphibolite facies metamorphism of the Orue Unit is ascribed to a regional contact metamorphic event, caused by the emplacement of the anorthositic crystal mushes in the middle crust.
This work is investigating the electronic structure of organic thin films. A central question in this respect is the influence of the interaction between the molecules in the condensed phase and the interaction at metal-organic interfaces on the electronic properties. For this purpose the experimental methods Photoelectron Spectroscopy (PES) and Near Edge X-ray Absorption Finestructure Spectroscopy (NEXAFS) were applied with highest energy resolution. In addition, ab initio calculations were performed for the theoretical simulation of NEXFAS spectra. The investigation is mainly focussing on thin, vacuum sublimated films of aromatic model molecules with oxygen-containing functional groups (NTCDA, PTCDA, NDCA, BPDCA and ANQ) and Ag(111) surfaces. Due to their large, delocalised p-systems these molecules have very interesting properties for their application in electronic devices. Due to the high energy resolution of third generation synchrotron sources the vibronic fine structure in the NEXAFS spectra of these large molecules could be resolved for the first time in the condensed phase. A comparison of the data of the different molecules provides interesting insight into the coupling between electronic transition and vibronic excitation. Although for these molecules a variety of different vibronic modes exist, the NEXAFS data show that preferentially only on mode couples to each electronic transition. The high-resolution PES spectra of the molecules NTCDA, PTCDA, NDCA, BPDCA and ANQ show distinct differences thus providing a fingerprint for each investigated substance. A comparative analysis of the spectra enabled us to define the 1s binding energies of all chemically different carbon and oxygen atoms. Additional structures in the spectra can be assigned as shake-up satellites. The five molecules are an ideal model system for the investigation of fundamental aspects of core electron spectroscopy, such as initial and final state effects and satellites, that are influenced by the intra- and intermolecular electron distribution in the ground and core ionized state. An important aspect in this thesis is the spectroscopic investigation of structurally different NTCDA monolayer phases on the Ag(111) surface. Marked differences in the electronic structures of the different phases, that can be assigned to differences in the metal-adsorbate interaction, could be demonstrated by XPS and NEXAFS. The substrate bonding can be characterized as chemisorptive for both, the compressed as well as the relaxed NTCDA monolayer, which can be unambiguously deduced from the analysis of satellite structures in the O 1s and C 1s XPS spectra. These satellites are due to dynamic screening by charge transfer from the substrate. The NEXAFS data show consistently, that the NTCDA LUMO becomes partly occupied upon adsorption. Highly interesting phase transitions into disordered low-temperature phases occur upon cooling to 160 K for both, the compressed and the relaxed NTCDA monolayer. Thereby, the adsorbate-substrate bonding is increased and the NTCDA LUMO becomes completely occupied. This can be observed in the NEXAFS data, where transitions involving LUMO final states are quenched. Simultaneously, the XPS data show a distinctly decreased intensity of unscreened photoemission states due to enhanced charge transfer screening. In addition, a hysteresis behaviour could be demonstrated for the phase transition of the relaxed monolayer by temperature dependent NEXAFS experiments and the hysteresis curve was determined. The hysteresis could be quantified to approx. 20 K. From SPA-LEED experiments the activating energy for the phase transition of the relaxed monolayer upon cooling could be determined to 60 meV. Finally, a NEXAFS investigation of polyethylene samples with different comonomer content is presented. Differences in the absorption spectra between samples with different comonomer content could be unambiguously assigned to the different crystallinities of the samples by heating a highly crystalline sample in situ close to the melting temperature. Ab initio calculations on a model matrix of butane molecules show, that the spectra of crystalline and amorphous polyethylene differ distinctly due to the intermolecular interaction, which can be observed best for resonances with strong Rydberg character. Thus, the differences in the PE spectra can be explained by the superposition of the signatures of crystalline and amorphous moieties, that are mixed according to the respective crystallinity.
The transcriptional repressor-Blimp-1 terminates differentiation of B lymphocytes as well as myeloid cells. Our data show that Blimp-1 is highly expressed in freshly isolated murine primary T lymphocytes, particularly its minor splice variant. Ectopic expression of Blimp-1 by retroviral transduction neither dramatically altered secretion of IFN-ã or IL-4 nor did it induce the ability to suppress as regulatory T cells. However, induction of Blimp-1 resulted in not only a significant reduction in the production of IL-2 but also an inability to proliferate as well as in the reduced viability. These results demonstrate that Blimp-1 might mark end stages of lineage differentiation in T cells.
Mechanisms of apoptosis modulation and their contribution to genomic instability in tumor cells
(2004)
The concept of programmed cell death has been increasingly considered from various aspects since early 1970’s. Primarily, knowledge of apoptosis referred to morphological changes in which chromatin is condensed and increasingly fragmented, revealed as small structure in the nucleus. The membrane shrinks and the cell becomes dense as can be seen by flow cytometry. Interestingly, similar modes of cell deletion were observed in nematodes indicating that apoptosis is a highly conserved machinery. Three Caeonorhabditis elegans gene products are found to have high homology with mammalian apoptotic genes: CED-9 inhibits apoptosis and is related to bcl-2; CED-3 and CED-4 promote apoptosis and are related to caspase 9 and APAF-1. Apoptosis is not accidental death, but a highly controlled and medically important molecular process. More general terms such as ‘physiological’ or ‘regulated’ cell death cover different morphologies and sequences. Programmed suicide of cells that were subjected to toxic exogenous and endogenous stimuli plays a key role in understanding cancer development and its treatment. Apoptosis involves sequences of events that may overlap and play contradictory or antagonistic roles in cell death. Generally, the ability to trigger apoptotic processes in cancer cells would benefit an organism by keeping homeostasis intact. Programmed cell death is a regularly present mechanism, for instance, in lymphocyte recruitment in the thymus where immature lymphocytes may recognize host antigens. Therefore, such lymphocytes become apoptotic and are removed by macrophages. Removal prevents possible autoimmune diseases. Unlike apoptosis, necrosis is a passive process of cell death recognizable by membrane morphological changes and accompanied by leakage of intracellular material into intercellular space that may cause inflammation in the organism. Signals that may initiate apoptosis are generally classified into two groups: signals that launch extrinsic apoptotic pathways starting with aggregation of death receptors and intrinsic apoptotic pathways starting with disruption of intracellular homeostasis such as the release of mitochondrial factors or DNA degradation. Early in the process, apoptotic signals may lead to a broad range of signaling mechanisms such as DNA repair and assessment of DNA damage (check points). Thus, failure in any of these steps can cause a defective apoptotic response that plays a decisive role in both tumorigenesis and drug resistance in tumor treatment. More distinctly, the capability of cancer cells to go into apoptosis prevents further neoplastic changes. Generally, the purpose of this study is to investigate the balance between formation of genomic damage and induction of apoptosis under genotoxic stress. After genotoxic insult there are different possibilities for the fate of a cell (Figure 1). The genomic integrity is analyzed at cellular checkpoints, usually leading to a delay in cell cycle progression if DNA was damaged. Mutations in genes such as p53 and p21 change the cellular response to genotoxic stress and may alter the balance between apoptosis and genomic damage. However, p53 is usually mutated or not expressed in 70% of human tumors. Alterations in p53 states that reflect distinct apoptotic response upon induction of DNA damage were examined. In this study, three cell lines with distinct p53 states were used: TK6 harboring wild-type p53, WTK1 with mutated p53 and NH32 with knocked out p53. In the present work we applied different approaches to investigate the correlation between DNA damage and apoptotic responsiveness in cancer cell lines with different p53 states or in hormone responsive cell lines with over expressed bcl-2 gene. We were focused on effects caused by temporary down regulation of the p53 and Bcl-2 activity in human lymphoblastoid cell lines. In addition, we investigated the impact of estradiol-induced proliferation on apoptosis and DNA damage in stably transfected cells with bcl-2gene.
The four-dimensional Minkowski space is known to be a good description for space-time down to the length scales probed by the latest high-energy experiments. Nevertheless, there is the viable and exciting possibility that additional space-time structure will be observable in the next generation of collider experiments. Hence, we discuss different extensions of the standard model of particle physics with an extra dimension at the TeV-scale. We assume that some of the gauge and Higgs bosons propagate in one additional spatial dimension, while matter fields are confined to a four-dimensional subspace, the usual Minkowski space. After compactification on an S^1/Z_2 orbifold, an effective four-dimensional theory is obtained where towers of Kaluza-Klein (KK) modes, in addition to the standard model fields, reflect the higher-dimensional structure of space-time. The models are elaborated from the 5D Lagrangian to the Feynman rules of the KK modes. Special attention is paid to an appropriate generalization of the Rxi-gauge and the interplay between spontaneous symmetry breaking and compactification. Confronting the observables in 5D standard model extensions with combined precision measurements at the Z-boson pole and the latest data from LEP2, we constrain the possible size R of the extra dimension experimentally. A multi-parameter fit of all relevant input parameters leads to bounds for the compactification scale M=1/R in the range 4-6 TeV at the 2 sigma confidence level and shows how the mass of the Higgs boson is correlated with the size of an extra dimension. Considering a future linear e+e- collider, we outline the discovery potential for an extra dimension using the proposed TESLA specifications as an example. As a consistency check for the various models, we analyze Ward identities and the gauge boson equivalence theorem in W-pair production and find that gauge symmetry is preserved by a complex interplay of the Kaluza-Klein modes. In this context, we point out the close analogy between the traditional Higgs mechanism and mass generation for gauge bosons via compactification. Beyond the tree-level, the higher-dimensional models studied extensively in the literature and in the first part of this thesis have to be extended. We modify the models by the inclusion of brane kinetic terms which are required as counter terms. Again, we derive the corresponding 4D theory for the KK towers paying special attention to gauge fixing and spontaneous symmetry breaking. Finally, the phenomenological implications of the new brane kinetic terms are investigated in detail.
Phosphorus and nitrogen containing ligands were examined in terms of their coordination flexibility. Combining these donor atoms of different hardness or softness in one molecule leads to the design of polyfunctional, ambidentate ligand systems with unique properties, because the different features associated with each donor atom confer unique reactivity to their metal complexes. The phosphane Ph2P(CH2Py) (Py = 2-pyridyl) is a very versatile starting material for the preparation of highly flexible, hemilabile, ambident ligands. C-deprotonation of this phosphane yields a Janus head, responding very sensitive to the Lewis-acidity and the charge concentration of the coordinated metal, adapting its coordination mode to the electronic requirements of the cation (electronic differentiation). Thus, bidentate (P,N)-chelating, tridentate (P,N)-chelating together with C-coordination and (C,N)-coordination is observed in the different metal complexes discussed in this work. Additionally, the oxidized derivative of the abovementioned phosphane, the iminophosphorane Ph2P(CH2Py)(NSiMe3), is discussed. The C-deprotonated anion of this iminophosphorane prefers (N,N’)-side arm- rather than C-coordination. The electron deficient pyridyl substituent at the C-atom leads to charge delocalization in the anionic [Ph2P(CHPy)(NSiMe3]-moiety. The bonding parameters of the iminophosphorane and all its derivatives, together with the almost fixed 15N-NMR resonances for the imino nitrogen atoms in these compounds prove that hypervalent central phosphorus is not required to describe the bonding situation in iminophosphoranes.
Complexation properties of 2,2':6',2''-terpyridine (tpy) have been studied with a series of first row transition metal ions by UV-vis, 1H NMR and isothermal titration calorimetry and ƒ´H values for the tpy complexation processes have been determined. These studies reveal that Zn2+ is the best suited metal ion for the reversible coordination of the terpyridine ligand. Thus, supramolecular coordination polymerization of perylene bisimide fluorophores containing terpyridine functionalities have been investigated by using Zn2+ as metal ion. The formation of the dimeric complexes in the case of monotopic model comounds and coordination polymerization of ditopic functional building blocks have been confirmed by 1H NMR studies. The optical properties of dimeric and polymeric complexes have been investigated by UV-vis and fluorescence spectroscopy. The Zn2+ coordination to the terpyridine unit does not effect the advantageous fluorescence properties of perylene bisimide moieties. The reversibility of the formation of coordination polymers has been established by 1H NMR and additionally by DOSY NMR and fluorescence anisotropy measurements. Coordination polymer strands can be visualized by atomic force microscopy (AFM), which also reveals the formation of an ordered monolayer film at higher concentration. The average polymer length has been determined by AFM to 15 repeat units, which correlates well with the value estimated by 1H NMR to >10 repeat units.