Rekonstitution des Fumaratsensors DcuS in Liposomen und Transport von Fumarat und Succinat in Escherichia coli

Das Zweikomponentenregulationssystem DcuSR kontrolliert die Expression der wichtigsten fumaratinduzierten Gene in Escherichia coli. Die Gene dcuB und dctA, die fürDicarboxylatcarrier kodieren, sowie das Fumaratreduktase-Operon (frd), sind Zielgene für DcuSR. DcuS ist eine membranständige Sensorkinase mit einer großen periplasmatischen Domäne. NMR-spektroskopische Untersuchungen dieser Domäne zeigen Alpha-Helices und Beta-Faltblätter. Für die Fumaratbindung wichtige Aminosäuren wurden durch Mutagenese identifiziert. Gereinigtes DcuS wurde in Liposomen rekonstituiert. In Anwesenheit von ATP wird DcuS autophosphoryliert. Der Phosphatrest kann dann auf DcuR übertragen werden und beweist somit die Aktivität dieses in vitro Testsystems.Der Transport von C4-Dicarboxylaten erfolgt unter anaeroben Bedingungen durch die sekundären Carrier DcuA, DcuB und DcuC. Es konnte ein weiteres Protein (DcuD) identifiziert werden, das hohe Sequenzähnlichkeit zu DcuC aufweist. Eine dcuD-Mutante zeigte keinen Phänotyp und überproduziertes DcuD konnte den Ausfall der anderen Dcu-Carrier nicht kompensieren. DcuD ist damit ein kryptisches Mitglied der Dcu-Carrierfamilie. Unter aeroben Bedingungen katalysiert DctA den Transport von C4-Dicarboxylaten. Dennoch können dctA-Mutanten noch mit Succinat wachsen. Die Diffusionsrate von Succinat durch Membranen wurde bestimmt. Sie ist um Größenordnungen niedriger als der Transport in der Mutante. Bei dem DctA unabhängigen Transportsystem handelt es sich um einen H+/Succinat2-Symporter, der bei saurem pH aktiv ist und viele Eigenschaften eines Monocarboxylatcarriers aufweist.

Transkriptionskontrolle des nuoA-N Operons (NADH-Dehydrogenase I) von Escherichia coli

Das Elektronentransportsystem von E. coli enthält zwei verschiedene NADH-Dehydrogenasen. Die NADH-DehydrogenaseI (nuoA-N) koppelt im Gegensatz zur NADH-DehydrogenaseII die Oxidation von NADH an eine Protonentranslokation und trägt zur Energiekonservierung bei. Die NADH-DehydrogenaseI wird über die Promotoren P1 und P2 exprimiert und besitzt mehrere Bindestellen für verschiedene Regulatoren.Die separate Klonierung der Promotoren, lacZ-Fusionen, Inaktivierung von Transkriptionsfaktoren, sowie die Nutzung mutierter Regulatorbindestellen in vivo zeigen, dass P1 im wesentlichen die Expressionshöhe bestimmt und ist unter aeroben und anaeroben Bedingungen aktiv. P2 trägt in wesentlich geringerem Maße als P1 zur Expression des Enzyms bei. Er ist stark abhängig von ArcA und IHF. Beide Promotoren wirken nicht additiv.Unter anaeroben Bedingungen wird die Transkription von nuo durch das Zweikomponenten-System ArcB/A reprimiert. ArcA bindet unabhängig und mit unterschiedlicher Affinität an die beiden Bindestellen arc1 und arc2. Von den 8 ArcA-Konsensussequenzen führen nur Mutationen der Konsensussequenzen arc1ab in vitro zu verminderter Bindungsaffinität von ArcA an die Bindestelle arc1. Dieselben führen in vivo unter anaeroben Bedingungen zur Derepression des Promotors P1 bzw. P1+P2. Unter aeroben Bedingungen zeigen nur Mutationen in arc2 eine Derepression, die nicht durch ArcA vermittelt wird. Der veröffentliche ArcA-Konsensus scheint deshalb hier in dieser einfachen Form nicht gültig zu sein.

Application of reactive fluid transport modeling to hydrothermal systems

A one-dimensional multi-component reactive fluid transport algorithm, 1DREACT (Steefel, 1993) was used to investigate different fluid-rock interaction systems. A major short coming of mass transport calculations which include mineral reactions is that solid solutions occurring in many minerals are not treated adequately. Since many thermodynamic models of solid solutions are highly non-linear, this can seriously impact on the stability and efficiency of the solution algorithms used. Phase petrology community saw itself faced with a similar predicament 10 years ago. To improve performance and reliability, phase equilibrium calculations have been using pseudo compounds. The same approach is used here in the first, using the complex plagioclase solid solution as an example. Thermodynamic properties of a varying number of intermediate plagioclase phases were calculated using ideal molecular, Al-avoidance, and non-ideal mixing models. These different mixing models can easily be incorporated into the simulations without modification of the transport code. Simulation results show that as few as nine intermediate compositions are sufficient to characterize the diffusional profile between albite and anorthite. Hence this approach is very efficient, and can be used with little effort. A subsequent chapter reports the results of reactive fluid transport modeling designed to constrain the hydrothermal alteration of Paleoproterozoic sediments of the Southern Lake Superior region. Field observations reveal that quartz-pyrophyllite (or kaolinite) bearing assemblages have been transformed into muscovite-pyrophyllite-diaspore bearing assemblages due to action of fluids migrating along permeable flow channels. Fluid-rock interaction modeling with an initial qtz-prl assemblage and a K-rich fluid simulates the formation of observed mineralogical transformation. The bulk composition of the system evolves from an SiO2-rich one to an Al2O3+K2O-rich one. Simulations show that the fluid flow was up-temperature (e.g. recharge) and that fluid was K-rich. Pseudo compound approach to include solid solutions in reactive transport models was tested in modeling hydrothermal alteration of Icelandic basalts. Solid solutions of chlorites, amphiboles and plagioclase were included as the secondary mineral phases. Saline and fresh water compositions of geothermal fluids were used to investigate the effect of salinity on alteration. Fluid-rock interaction simulations produce the observed mineral transformations. They show that roughly the same alteration minerals are formed due to reactions with both types of fluid which is in agreement with the field observations. A final application is directed towards the remediation of nitrate rich groundwaters. Removal of excess nitrate from groundwater by pyrite oxidation was modeled using the reactive fluid transport algorithm. Model results show that, when a pyrite-bearing, permeable zone is placed in the flow path, nitrate concentration in infiltrating water can be significantly lowered, in agreement with proposals from the literature. This is due to nitrogen reduction. Several simulations investigate the efficiency of systems with different mineral reactive surface areas, reactive barrier zone widths, and flow rates to identify the optimum setup.

Untersuchungen des Keratinfilament-Turnovers in lebenden Zellen

Das Zytoskelett eukaryotischer Zellen besteht aus drei verschiedenen Protein-Netzwerken: den Aktinfilamenten, Mikrotubuli und Intermediärfilamenten. Intermediärfilamente wurden ursprünglich als statische Strukturen angesehen, die die mechanische Stabilisierung der Zellen übernehmen. In den letzten Jahren hat sich dieses Bild jedoch geändert: Intermediärfilament-Netzwerke sind hochdynamisch und unterliegen kontinuierlichen Veränderungen, welche durch Phosphorylierungen reguliert werden. Sie interagieren mit anderen Zytoskelett-Proteinen und greifen in die Regulation von Schlüsselsignalwegen, die Zellwachstum und Zellteilung sowie Apoptose und Stressantwort bestimmen, ein. Die Mechanismen der Filamentplastizität konnten bisher jedoch nicht vollständig aufgeklärt werden. So ist beispielsweise unklar, wo Auf- und Abbau der Filamente stattfindet und welche Faktoren an der Netzwerkmodulation beteiligt sind. Ziel meiner Arbeit war es, einen Beitrag zur Aufklärung dieser Mechanismen am Beispiel der epithelialen Keratin-Intermediärfilamente zu leisten. Mit Hilfe von mikroskopischen Zeitrafferaufnahmen von fluoreszenzmarkierten Zellklonen wurden Nukleationszentren in der Zellperipherie identifiziert, in denen Keratinfilamentvorläufer gebildet werden. Es handelt sich dabei um fokale Adhäsionskomplexe, die als Anheftungsstellen zwischen der extrazellulären Matrix und dem intrazellulären Aktinfilament-System dienen. Es konnte gezeigt werden, dass diese Filamentvorläufer-Entstehung für alle untersuchten Keratinisoformen gültig ist und in epitelialen als auch nicht-epithelialen Zelltypen abläuft. Knock-Down der Adhäsionskomponente Talin verhinderte die Keratinfilamentbildung. Modulation der fokalen Adhäsionskinase, die den Auf- und Abbau der Adhäsionskomplexe koordiniert, beeinflusste ebenso die Bildung der Keratinfilamentnetzwerke. Es konnte weiterhin beobachtet werden, dass die N-terminalen Isoformen IE und IF des Zytolinkers Plectin in fokalen Adhäsionen lokalisieren und damit möglicherweise an der Vernetzung von Keratinfilamentvorläufern, Zelladhäsionen und Aktinfilamenten beteiligt sind. Letztlich stellte sich heraus, dass die Bildung der Keratinfilamentvorläufer unabhängig von Proteintranslation ist. In den mikroskopischen Zeitrafferaufnahmen wurde im Anschluss an die Keratinfilamentbildung ein kontinuierlicher zentripetaler Transport der wachsenden Vorläuferpartikel beobachtet. An Hand von pharmakologischen Experimenten konnte gezeigt werden, dass dieser Transport Aktinfilament-abhängig ist. Zeitgleich kommt es zu Partikelfusion und Integration in das periphere Netzwerk, das sich weiterhin in Richtung auf das Zellzentrum bewegt. Mit Hilfe von Photoaktivierungsversuchen und Zellfusionsexperimenten konnte die Hypothese bestätigt werden, dass der Abbau der einwandernden Keratinfilamente in lösliche, rasch diffusible Zwischenstufen den kontinuierlichen peripheren Neuaufbau ermöglicht. Aus den Beobachtungen und bereits bekannten Ergebnissen wurde ein Modell des Keratin-Zyklus entwickelt, das die folgenden Stadien umfasst: Nukleation von Keratinfilamentvorläufern an fokalen Adhäsionen in der Zellperipherie, Elongation und Fusion der Keratinfilamentvorläufer bei zeitgleichem Aktinfilament-abhängigem zentripetalen Transport, Integration der Keratinfilamentvorläufer in das periphere Netzwerk, Bündelung der Filamente, Filamentabbau in lösliche Untereinheiten und Neubeginn des Zyklus in der Zellperipherie. Eine Störung dieses Zyklus liegt bei mutierten Keratinen vor, welche die Ursache von Blasen-bildenden Hauterkrankungen sind. In der vorliegenden Arbeit wurde am Beispiel von Keratin 6a-Mutanten, welche die Hauterkrankung Pachyonychia congenita verursachen, gezeigt, dass bei diesen Keratinen die Nukleation zwar im Bereich der Adhäsionskomplexe regelrecht abläuft, die anschließende Elongation und Netzwerkbildung aber gestört ist, so dass statt dessen kurzlebige, hyperphosphorylierte Granula entstehen. Der resultierende frustrane Keratin-Zyklus in der Zellperipherie ist stark beschleunigt und kann durch p38-Inhibierung gestoppt werden. Bei Proteasomeninhibierung wird der Zyklus in Richtung der Granulabildung verschoben. In dieser Arbeit wird erstmals das Keratin-Tretmühlen-Modell vorgestellt, das den regulierbaren Auf- und Abbau-Zyklus des Keratinnetzwerks beschreibt. Damit liegen testbare Hypothesen für die Aufklärung der Keratinfilament-Plastizität in physiologischen und pathologischen Situationen vor, die nach unseren ersten Ergebnissen auch von Relevanz für andere Intermediärfilamenttypen sind.

Morphology and charge transport in conjugated polymers

To assist rational compound design of organic semiconductors, two problems need to be addressed. First, the material morphology has to be known at an atomistic level. Second, with the morphology at hand, an appropriate charge transport model needs to be developed in order to link charge carrier mobility to structure.rnrnThe former can be addressed by generating atomistic morphologies using molecular dynamics simulations. However, the accessible range of time- and length-scales is limited. To overcome these limitations, systematic coarse-graining methods can be used. In the first part of the thesis, the Versatile Object-oriented Toolkit for Coarse-graining Applications is introduced, which provides a platform for the implementation of coarse-graining methods. Tools to perform Boltzmann inversion, iterative Boltzmann inversion, inverse Monte Carlo, and force-matching are available and have been tested on a set of model systems (water, methanol, propane and a single hexane chain). Advantages and problems of each specific method are discussed.rnrnIn partially disordered systems, the second issue is closely connected to constructing appropriate diabatic states between which charge transfer occurs. In the second part of the thesis, the description initially used for small conjugated molecules is extended to conjugated polymers. Here, charge transport is modeled by introducing conjugated segments on which charge carriers are localized. Inter-chain transport is then treated within a high temperature non-adiabatic Marcus theory while an adiabatic rate expression is used for intra-chain transport. The charge dynamics is simulated using the kinetic Monte Carlo method.rnrnThe entire framework is finally employed to establish a relation between the morphology and the charge mobility of the neutral and doped states of polypyrrole, a conjugated polymer. It is shown that for short oligomers, charge carrier mobility is insensitive to the orientational molecular ordering and is determined by the threshold transfer integral which connects percolating clusters of molecules that form interconnected networks. The value of this transfer integral can be related to the radial distribution function. Hence, charge mobility is mainly determined by the local molecular packing and is independent of the global morphology, at least in such a non-crystalline state of a polymer.

Charge-transport simulations in organic semiconductors

In this thesis we have extended the methods for microscopic charge-transport simulations for organic semiconductors. In these materials the weak intermolecular interactions lead to spatially localized charge carriers, and the charge transport occurs as an activated hopping process between diabatic states. In addition to weak electronic couplings between these states, different electrostatic environments in the organic material lead to a broadening of the density of states for the charge energies which limits carrier mobilities.rnThe contributions to the method development includern(i) the derivation of a bimolecular charge-transfer rate,rn(ii) the efficient evaluation of intermolecular (outer-sphere) reorganization energies,rn(iii) the investigation of effects of conformational disorder on intramolecular reorganization energies or internal site energiesrnand (iv) the inclusion of self-consistent polarization interactions for calculation of charge energies.These methods were applied to study charge transport in amorphous phases of small molecules used in the emission layer of organic light emitting diodes (OLED).rnWhen bulky substituents are attached to an aromatic core in order to adjust energy levels or prevent crystallization, a small amount of delocalization of the frontier orbital to the substituents can increase electronic couplings between neighboring molecules. This leads to improved charge-transfer rates and, hence, larger charge-mobility. We therefore suggest using the mesomeric effect (as opposed to the inductive effect) when attaching substituents to aromatic cores, which is necessary for example in deep blue OLEDs, where the energy levels of a host molecule have to be adjusted to those of the emitter.rnFurthermore, the energy landscape for charges in an amorphous phase cannot be predicted by mesoscopic models because they approximate the realistic morphology by a lattice and represent molecular charge distributions in a multipole expansion. The microscopic approach shows that a polarization-induced stabilization of a molecule in its charged and neutral states can lead to large shifts, broadening, and traps in the distribution of charge energies. These results are especially important for multi-component systems (the emission layer of an OLED or the donor-acceptor interface of an organic solar cell), if the change in polarizability upon charging (or excitation in case of energy transport) is different for the components. Thus, the polarizability change upon charging or excitation should be added to the set of molecular parameters essential for understanding charge and energy transport in organic semiconductors.rnWe also studied charge transport in self-assembled systems, where intermolecular packing motives induced by side chains can increase electronic couplings between molecules. This leads to larger charge mobility, which is essential to improve devices such as organic field effect transistors, where low carrier mobilities limit the switching frequency.rnHowever, it is not sufficient to match the average local molecular order induced by the sidernchains (such as the pitch angle between consecutive molecules in a discotic mesophase) with maxima of the electronic couplings.rnIt is also important to make the corresponding distributions as narrow as possible compared to the window determined by the closest minima of thernelectronic couplings. This is especially important in one-dimensional systems, where charge transport is limited by the smallest electronic couplings.rnThe immediate implication for compound design is that the side chains should assist the self-assemblingrnprocess not only via soft entropic interactions, but also via stronger specific interactions, such as hydrogen bonding.rnrnrnrn

Mineral dust mobilisation, transport, and deposition in different climate epochs

Mineral dust is an important component of the Earth's climate system and provides essential nutrientsrnto oceans and rain forests. During atmospheric transport, dust particles directly and indirectly influencernweather and climate. The strength of dust sources and characteristics of the transport, in turn, mightrnbe subject to climatic changes. Earth system models help for a better understanding of these complexrnmechanisms.rnrnThis thesis applies the global climate model ECHAM5/MESSy Atmospheric Chemistry (EMAC) for simulationsrnof the mineral dust cycle under different climatic conditions. The prerequisite for suitable modelrnresults is the determination of the model setup reproducing the most realistic dust cycle in the recentrnclimate. Simulations with this setup are used to gain new insights into properties of the transatlanticrndust transport from Africa to the Americas and adaptations of the model's climate forcing factors allowrnfor investigations of the impact of climatic changes on the dust cycle.rnrnIn the first part, the most appropriate model setup is determined through a number of sensitivity experiments.rnIt uses the dust emission parametrisation from Tegen et al. 2002 and a spectral resolutionrnof T85, corresponding to a horizontal grid spacing of about 155 km. Coarser resolutions are not able tornaccurately reproduce emissions from important source regions such as the Bodele Depression in Chad orrnthe Taklamakan Desert in Central Asia. Furthermore, the representation of ageing and wet deposition ofrndust particles in the model requires a basic sulphur chemical mechanism. This setup is recommended forrnfuture simulations with EMAC focusing on mineral dust.rnrnOne major branch of the global dust cycle is the long-range transport from the world's largest dustrnsource, the Sahara, across the Atlantic Ocean. Seasonal variations of the main transport pathways to thernAmazon Basin in boreal winter and to the Caribbean during summer are well known and understood,rnand corroborated in this thesis. Both Eulerian and Lagrangian methods give estimates on the typicalrntransport times from the source regions to the deposition on the order of nine to ten days. Previously, arnhuge proportion of the dust transported across the Atlantic Ocean has been attributed to emissions fromrnthe Bodele Depression. However, the contribution of this hot spot to the total transport is very low inrnthe present results, although the overall emissions from this region are comparable. Both model resultsrnand data sets analysed earlier, such as satellite products, involve uncertainties and this controversy aboutrndust transport from the Bodele Depression calls for future investigations and clarification.rnrnAforementioned characteristics of the transatlantic dust transport just slightly change in simulationsrnrepresenting climatic conditions of the Little Ice Age in the middle of the last millennium with meanrnnear-surface cooling of 0.5 to 1 K. However, intensification of the West African summer monsoon duringrnthe Little Ice Age is associated with higher dust emissions from North African source regions and wetterrnconditions in the Sahel. Furthermore, the Indian Monsoon and dust emissions from the Arabian Peninsula,rnwhich are affected by this circulation, are intensified during the Little Ice Age, whereas the annual globalrndust budget is similar in both climate epochs. Simulated dust emission fluxes are particularly influencedrnby the surface parameters. Modifications of the model do not affect those in this thesis, to be able tornascribe all differences in the results to changed forcing factors, such as greenhouse gas concentrations.rnDue to meagre comparison data sets, the verification of results presented here is problematic. Deeperrnknowledge about the dust cycle during the Little Ice Age can be obtained by future simulations, based onrnthis work, and additionally using improved reconstructions of surface parameters. Better evaluation ofrnsuch simulations would be possible by refining the temporal resolution of reconstructed dust depositionrnfluxes from existing ice and marine sediment cores.