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Metallorganische Netzwerke (engl. metal-organic frameworks, MOFs) sind eine neuartige Klasse mikro/mesoporöser Materialien, für die eine Vielzahl von möglichen Anwendungen demonstriert werden konnte. Das Ziel dieser Arbeit besteht in der Synthese von MOF Mikro/Nanopartikeln sowie der Herstellung von sogenannten Oberflächen-deponierten MOFs (engl. surface-attached metal-organic frameworks, SURMOFs). MOF Partikel mit kontrollierbarer Morphologie und Größe wurden unter milden Bedingungen synthetisiert. Um MOFs als Sensoren, intelligente Membrane, oder in nanotechnologischen Bauelementen verwenden zu können, ist die Integration auf der jeweiligen Oberfläche wichtig. Daher beschäftigt sich der Großteil dieser Arbeit mit der kontrollierten Abscheidung von SURMOFs auf verschiedenartigen Trägermaterialien. Etliche interessante Eigenschaften (z.B. die Fluoreszenz in Abhängigkeit von der Gegenwart von Gastmolekülen und die dynamische Gasadsorptionskapazität) der SURMOFs wurden untersucht.
This research was conducted in the Rwenzori Region of the Western Branch, East African Rift System (EARS). The EARS is a tectonic structure extending over a length of more than 3000 km from the Afar Triple Junction, in Ethiopia, to Lake Malawi in the south. The Western Rift System is a roughly NE to ENE trending sector of the EARS, which runs along the western boundary of Uganda and the neighboring Democratic Republic of Congo (D.R.C). It stretches 2100 km from Nimule, NW on Uganda-Sudan border, extending to Lake Malawi in the SE of Africa. The unusual uplift of the Rwenzori Mountains within an extensional regime and the mechanisms associated with the high frequency of seismic activity in the region was hardly understood and therefore, had remained a subject of contention that needed to be critically addressed in detail. To my knowledge, this was probably the first study to be performed and documented in great depth within the domains of seismic noise variation, seismic anisotropy and b value analyses beneath the Rwenzori Region. After about six years of operation (2006-2012), the seismology group of the RIFTLINK Research Project (www.riftlink.org) acquired a vast amount of high-quality, digital data that were collected using a seismic network of well calibrated seismic equipment. The project was divided into two phases. Phase I, that operated between February 2006 - September 2007, consisted of thirty-two temporary seismic stations, which were selectively spread out in the Rwenzori Region on the Ugandan side, to detect and record extremely weak as well as strong naturally occurring earthquakes. The seismic equipment used included EDL and REFTEK digitizers, which were coupled with Güralp and MARK sensors respectively (REFTEKS: only short-period MARK sensors, EDLs: short-period MARK plus few broadband Güralp Sensors). Exactly 22375 earthquakes were recorded. The data were processed using the SEISAN software package. About 14413 earthquakes were carefully localized using the velocity model of Bram (1975) that implements a Vp=Vs ratio fixed at 1.74. Phase II, that extended between 2009-2012 consisted of thirty-two seismic stations, which were spread out around the Rwenzori Mountains, both on the Ugandan side and the neighboring D.R.C. Only Taurus digitizers that were coupled with Trillium sensors were used in the D.R.C. On the Ugandan side however, both EDL and Taurus digitizers, which were coupled with Trillium and Güralp sensors were used. ...
Calcium-deficiency rickets (CDR) is a metabolic bone disease in children that is characterized by impaired mineralization and severe bone deformities. As CDR is often an endemic phenomenon that is almost exclusively restricted to tropical areas, environmental conditions are currently considered to be a possible predisposing factor for the CDR. Apart from a lack of macronutrients and micronutrients, an oversupply of potentially toxic elements (PTEs) in the soil-plant pathway of the CDR areas is thought to be involved in the aetiology of CDR. This study is the first to comprehensively analyze the impact of the environment on Ca deficiency and the resulting CDR.
To analyze the impact of the environment on CDR in developing countries, a rural region near Kaduna City, northern Nigeria, was chosen as a study area. From this area, cases of CDR have been reported since the early 2000s with a prevalence rate of 5%. Within this study area, 11 study sites, including areas with a high CDR prevalence (HR), a low CDR prevalence (LR) and no CDR prevalence (NR), were visited. In these HR, LR and NR study sites, the bedrock was investigated and the types of parent materials were identified. Local farmers were interviewed to determine the type and intensity of the land use. The soil types were determined along toposequences. The soil textures as well as the clay mineral fractions were determined. The pH values were measured, and the contents of organic carbon (OC) were determined. The potential cation-exchange capacity (CECpot) and the base saturation (BS) were analyzed. Furthermore, the total and plant-available macronutrient, micronutrient and PTE concentrations were measured in the soils. The drinking water was analyzed for pH values and the concentrations of Ca, Se and F were measured. The maize was analyzed for the Ca, Mg, K and P, Se and phytic acid (PA) contents.
The field and laboratory analyses on the bedrock showed that the HR, LR and NR study sites near Kaduna City, northern Nigeria, were underlain by Older Granites. A direct link between the distribution of the bedrock, the parent materials and the prevalence of CDR was not found. Interviews with the local farmers showed that the land use in the Kaduna study area is dominated by the cultivation of cash crops and food crops. Field analyzes on the soil types in the Kaduna study area showed that the distribution of the soil types is highly dependent on the topography and the distribution of the parent materials. In near vicinity to the inselbergs, Lixisols had developed on grus slope deposits. In the lower pediment and plain positions, Acrisols had developed on grus slope deposits and pisolite slope deposits. In the upper plains, Plinthosols had developed on pisolite slope deposits and in the river valleys, Fluvisols had developed on river deposits. Such soil types and soil type distributions are typical for granite-underlain areas in the northern guinea savanna of West Africa. Similarly, the physical soil conditions were representative for the soils of the northern guinea savanna: sandy topsoils, clayey subsoils and relatively high contents of kaolinite clay minerals in the clay fractions. With regard to the geochemical composition, no significant difference was found between the soils of the Kaduna study area and the soils of other granite-underlain areas in West Africa. Only the concentrations of P were considerably low in the soils of the Kaduna study area. However, P deficiency is a typical phenomenon in West African savanna soils and is not restricted to CDR areas. The micronutrient concentrations in the soils were low, but not critically low. Laboratory analyses on the amounts of PTEs showed that compared to worldwide background levels and international critical limits the PTE concentrations were very low in the soils of the Kaduna study area. In the drinking water, neither a significant lack of macronutrients and micronutrients, nor a noticeable oversupply of PTEs was found. The maize in the HR, LR and NR study sites contained normal contents of Mg, K and P, low contents of Ca and Se as well as slightly elevated concentrations of PA compared to West African food composition tables. Comparisons between the mineral contents of traditional and modern maize cultivars showed that the traditional maize cultivars contained significantly higher contents of Ca and noticeably lower concentrations of PA than the modern maize cultivars.
A direct link between the environmental conditions and the CDR in the Kaduna study area was considered unlikely, as neither a statistically significant lack of macronutrients and micronutrients, nor a statistically significant oversupply of PTEs was found in the environment of this area. Instead, the results indicated that the nutrition rather than the environmental conditions that impacts the prevalence of CDR.
Das Ziel dieser Arbeit ist es, eine authentische Verdeckung eingebetteter virtueller 3D-Objekte in augmentierten Bilderwelten bei einer geringen Anzahl an Fotos innerhalb der Bilderwelt zu erreichen. Für die Verdeckung von realen und virtuellen Anteilen einer Augmented Reality-Szene sind Tiefeninformationen notwendig. Diese stammen üblicherweise aus einer 3D-Rekonstruktion, für deren Erstellung sehr viele Eingangsbilder notwendig sind. Im Gegensatz dazu wurde in dieser Arbeit ein System entwickelt, das eine vollständige 3D-Rekonstruktion umgeht. Dieses beruht auf einem direkten bildbasierten Rendering-Ansatz, welcher auch mit unvollständigen Tiefeninformationen eine hohe Bildqualität in Bezug auf eine authentische Verdeckung erreicht. Daraus erschließen sich neue Anwendungsgebiete, wie z.B. die automatisierte Visualisierung von 3D-Planungsdaten und 3D-Produktpräsentationen in Bildern bzw. Bilderwelten, da in diesen Bereichen oftmals nicht genügend große Bildmengen vorhanden sind. Gerade für diese Anwendungsgebiete sind authentische Verdeckungen für die Nutzerakzeptanz der Augmentierung wichtig. Unter authentischer Verdeckung wird die entsprechend der menschlichen Wahrnehmung visuell korrekte Überlagerung zwischen virtuellen Objekten und einzelnen Bildanteilen eines oder mehrerer Fotos verstanden. Das Ergebnis wird in Form einer Bilderwelt (eine bildbasierte 3D-Welt, die die Fotos entsprechend der Bildinhalte räumlich anordnet) präsentiert, die mit virtuellen Objekten erweitert wurde. Folglich ordnet sich diese Arbeit in das Fachgebiet der Augmented Reality ein. Im Rahmen dieser Arbeit wurde ein Verfahren für die bildbasierte Darstellung mit authentischen Verdeckungen auf der Basis von unvollständigen Tiefeninformationen sowie unterschiedliche Verfahren für die notwendige Berechnung der Tiefeninformationen entwickelt und gegenübergestellt. Das Sliced-Image-Rendering-Verfahren rendert mithilfe unvollständiger Tiefeninformationen ein Bild ohne 3D-Geometrie als dreidimensionale Darstellung und realisiert auf diese Weise eine authentische Verdeckung. Das Berechnen der dafür notwendigen Tiefeninformationen eines 2D-Bildes stellt eine gesonderte Herausforderung dar, da die Bilderwelt nur wenige und unvollständige 3D-Informationen der abgebildeten Szene bereitstellt. Folglich kann eine qualitativ hochwertige 3D-Rekonstruktion nicht durchgeführt werden. Die Fragestellung ist daher, wie einzelne Tiefeninformationen berechnet und diese anschließend größeren Bildbereichen zugeordnet werden können. Für diese Tiefenzuordnung wurden im Rahmen der vorliegenden Arbeit drei verschiedene Verfahren konzipiert, die sich in Bezug auf genutzte Daten und deren Verarbeitung unterscheiden. Das Segment-Depth-Matching-Verfahren ordnet Segmenten eines Bildes mithilfe der 3D-Szeneninformationen der Bilderwelt eine Tiefe zu. Hierfür werden Segmentbilder vorausgesetzt. Als Ergebnis liegt für jedes Foto eine Depth-Map vor. Um eine Tiefenzuordnung auch ohne eine vorangehende Segmentierung zu ermöglichen, wurde das Key-Point-Depth-Matching-Verfahren entwickelt. Bei diesem Verfahren werden die 3D-Szeneninformationen der Bilderwelt auf die Bildebene als kreisförmige Sprites projiziert. Die Distanz zur Kamera wird dabei als Tiefenwert für das Sprite verwendet. Alle projizierten Sprites einer Kamera ergeben die Depth-Map. Beide Verfahren liefern Flächen mit Tiefeninformationen, aber keine pixelgenauen Depth-Maps. Um pixelgenaue Depth-Maps zu erzeugen, wurde das Geometry-Depth-Matching-Verfahren entwickelt. Bei diesem Verfahren wird eine Szenengeometrie des abgebildeten Szenenausschnittes erzeugt und dadurch eine pixelgenaue Depth-Map erstellt. Hierfür wird ein semiautomatischer Skizzierungsschritt vorausgesetzt. Die erzeugte Szenengeometrie stellt keine vollständige 3D-Rekonstruktion der Bilderweltenszene dar, da nur ein Szenenausschnitt aus Sicht einer Kamera rekonstruiert wird. Anhand einer technischen Umsetzung erfolgte eine Validierung der konzeptionellen Verfahren. Die daraus resultierenden Ergebnisse wurden anhand verschiedener Bilderweltenszenen mit unterschiedlichen Eigenschaften (Außen- und Innenraumszenen, detailreich und -arm, unterschiedliche Bildmengen) evaluiert. Die Evaluierung des Sliced-Image-Renderings zeigt, dass mithilfe unvollständiger Tiefeninformationen der entwickelten Depth-Matching-Verfahren und unter Einhaltung der gestellten Anforderungen (wenig Eingabefotos, kleine Szenen, keine 3D-Rekonstruktion) eine authentische Verdeckung eingebetteter virtueller 3D-Objekte in Bilderwelten realisiert werden kann. Mithilfe des entwickelten Systems können bildbasierte Anwendungen auch mit kleinen Fotomengen Augmentierungen mit hoher Bildqualität in Bezug auf eine authentische Verdeckung realisieren.
In der modernen Hochschullehre haben sich eLearning-Elemente als ein Teil des Lehrrepertoires etabliert. Der Einsatz interaktiver webbasierter Selbstlernmodule (Web Based Trainings (WBT)) ist dabei eine Option. Hochschulen und Unternehmen versprechen sich dadurch neue Möglichkeiten des Lehrens und Lernens, um z. B. einen Ausgleich heterogener Vorerfahrungen sowie eine stärkere aktive Beteiligung der Lernenden zu bewirken. Damit die Erstellung und Strukturierung dieser Inhalte mit möglichst geringem Aufwand erfolgen kann, bieten Autorensysteme Unterstützung.
Zu den Grundfunktionen von Autorensystemen gehören unter anderem, das Einbinden gebräuchlicher Medienformate, die einfache Erstellung von Fragen sowie verschiedene Auswertungs- und Feedbackmöglichkeiten. Obwohl Autorensysteme schon vor vielen Jahren ihre erste praktische Anwendung fanden, gibt es nach wie vor Schwachstellen, die sich auf den gesamten Erstellungsprozess wie auch auf einzelne Funktionen beziehen. Im Detail wird bemängelt, dass die Werkzeuge zu komplex und unflexibel sind. Darüber hinaus fehlt häufig eine zufriedenstellende Verknüpfung der vielen Werkzeuge entlang der Prozesskette zu einer Gesamtlösung.
Des Weiteren wird die Konzentration auf die Produktionsphase kritisiert, wodurch andere wichtige Prozesse in den Hintergrund treten bzw. außer Acht gelassen werden.
Im Rahmen der Zusammenarbeit mit einem Automobilhersteller, für den die erste Version des Autorensystems LernBar weiterentwickelt wurde, spielte der Begriff „Lean Production“ inhaltlich in der Umsetzung der WBTs eine wesentliche Rolle. Die Lean Production, die über viele Jahre für die Automobilindustrie entwickelt, verbessert und angepasst wurde, liefert Optimierungsansätze für den Produktionsbereich. Ein wirtschaftlicher Nutzen des Lean-Ansatzes wird auch in anderen Bereichen gesehen wie z. B. in der Softwareentwicklung („Lean Software Development“) oder im Management („Lean Management“). Dabei bietet die Wertschöpfungsorientierung Lösungen für die widersprüchlichen Ziele mehr Leistungen zu geringeren Kosten, schneller und in höherer Qualität zugleich zu liefern. Aus der Grundidee der Lean Production entwickelte sich vorliegendes Dissertationsthema in Bezug darauf, inwiefern sich diese Prinzipien auf den WBT-Produktionsprozess übertragen lassen und die LernBar (das hierfür weiterentwickelnde Autorensystem) dabei Unterstützung bieten kann.
Zunächst wurde analysiert, welche Werkzeuge und Hilfestellungen benötigt werden, um unter dem Aspekt der Lean Production WBTs im universitären Umfeld erstellen zu können. In diesem Zusammenhang wurden Merkmale einer „Lean Media Production“ definiert sowie konzeptionell und technisch umgesetzt. Zur Verbesserung der Prozesse flossen Ergebnisse aus empirischer und praktischer Forschung ein. Im Vergleich zu anderen Entwicklungen bei denen häufig das Hauptziel eine umfangreiche Funktionalität ist, werden u.a. folgende übertragbare Ziele bei der Umsetzung verfolgt: Verschwendung vermeiden, eine starke Einbeziehung der Kunden, Werkzeuge die nahtlos ineinandergreifen, eine hohe Flexibilität und eine stetige Qualitätsverbesserung.
Zur Erreichung dieser Zielsetzungen wurden alle Prozesse kontinuierlich verbessert, sich auf das Wesentliche und die Wertschöpfung konzentriert sowie überflüssige Schritte eliminiert. Demnach ist unter dem Begriff „Lean Media Production“ ein skalierbarer, effizienter und effektiver Produktionsprozess zu verstehen, in dem alle Werkzeuge ineinandergreifen.
Die Realisierung der „Lean Media Production“ erfolgte anhand des Autorensystems LernBar, wobei die typischen Softwareentwicklungsphasen Entwurf, Implementierung und Evaluierung mehrfach durchlaufen wurden. Ausschlaggebend dabei war, dass der „Lean“-Aspekt berücksichtigt wurde und dies somit eine neue Vorgehensweise bei der Umsetzung eines Autorensystems darstellt. Im Verlauf der Entwicklungen ergaben sich, durch eine formative Evaluation, den Einsatz in Projekten und eine empirische Begleitforschung, neue Anforderungen an das System. Ein Vergleich der zwei Produktionssysteme, Automobil vs. WBT-Produktion, zeigt und bestätigt die Erwartung, dass nicht alle Prinzipien der Lean Production übertragbar sind.
Dennoch war diese Untersuchung notwendig, da sie Denkanstöße zur Entwicklung und Optimierung des Erstellungsprozesses eines WBTs gab. Auch die Ergebnisse der abschließenden Online-Befragung ergaben, dass die Ziele der Arbeit erreicht wurden, dass aber weiterer Optimierungsbedarf besteht. Die LernBar Release 3 bietet für alle Produktionsphasen Werkzeuge an, durch die eine effektive und effiziente Erstellung von WBTs von der Idee bis zur Distribution möglich ist.
Stand noch vor fünf Jahren zu Beginn dieser Arbeit das Endprodukt bei der LernBar Entwicklung im Vordergrund, verlagerte sich durch den Einfluss dieser Dissertation der Schwerpunkt auf den gesamten Produktionsprozess. Unter Berücksichtigung der in diesem Zusammenhang entwickelten Prinzipien einer „Lean Media Production“, nehmen bspw. die Wirtschaftlichkeit und die starke Kundenorientierung während des Produktionsprozesses einen wichtigen Stellenwert ein. Dieser Ansatz ist eine neue Vorgehensweise im Bereich der Entwicklung von Autorensystemen, der seine Anerkennung und Professionalität durch die Ergebnisse des selbstentwickelten Evaluationsbogens sowie dem stetig wachsenden Einsatz in Schulen, Hochschulen und Unternehmen belegen kann.
In weiteren Forschungsarbeiten ist zu untersuchen, welche Lean Production Prinzipien zu verwenden oder anzupassen sind, wenn z. B. in größeren Teams oder mobil produziert wird. Des Weiteren sollte überprüft werden, inwieweit die Lernenden mit dem Endprodukt zufrieden sind und in ihrem Lernprozess unterstützt werden. Durch diese Forschungsarbeit wurde ein Beitrag dazu geleistet, die Lehre und Ausbildung zu optimieren, indem die Autoren/Lehrende in der Erstellung ihrer digitalen Lerninhalte im gesamten Prozess von aufeinander abgestimmten Werkzeugen unterstützt werden.
Mantle convection is the process by which heat from the Earth’s core is transferred upwards to the surface and it is accepted to explain the dynamics of the Earth’s interior. On geological time-scales, mantle material flows like a viscous fluid as a consequence of the buoyancy forces arising from thermal expansion. Indeed, mantel convection provides a framework which links together the major disciplines, such as seismology, mineral physics, geochemistry tectonic and geology. The numerical model has been applied to understand the dynamic, structure and evaluation of the Earth, and other terrestrial planets and the investigations continue to explore, different aspects of the mantle convection.
In fact, to model this phenomenon, two complementary approaches are possible. On the one hand, one can solve self-consistently the equations of thermal convection, including parameters and employing physical relationships derived from mineral physics. Our understanding of mantle convection depends ultimately upon the success of such fully self-consistent dynamic models in explaining observable features of the flow. Although, these models presently unable to predict the actual convection pattern of the Earth, they are extremely useful to investigate general characteristics of given physical systems. On the other hand, to permit comparison with specific observables associated with the flow, one can consider a more restricted problem. Instead of focusing on the time evolution of mantle flow, if we know a priori the temperature - and hence presumably the density - anomalies that drive the convection, we can try to build a snapshot of the present-day flow pattern, consistent with those anomalies, that can successfully predict the observables. As matter of fact, the aim of this study is to investigate both approaches in comparison with the main geophysical constraints on mantle structure. These constraints include the geoid anomalies, the dynamic surface and core-mantle boundary topography and tectonic plate motions.
The most appropriate mathematical basis functions for describing a bounded and continuous function on a spherical surface are spherical harmonics. We may therefore expand the geodynamic observables in terms of spherical harmonics. We have investigated two methods of the global spherical harmonic analysis by specific attention to the dynamic geoid computation of the geodynamic models. The first method is the quadrature method in which the loss of the orthogonality of the Legendre functions in transition from continues to discrete case is the major drawback to the method. Particularly, we showed that in the absence of the tesseral harmonics, quadrature formulation leads to obtain inaccurate results. The second method is the least-squares which can be considered as the best linear unbiased estimator that provides the exact results. We showed that even with a low resolution grid data it is possible to reconstruct the data and achieve an accurate result by using this method, which is extremely remarkable in three-dimensional global convection studies. However, special care has to be taken since there is some source of errors that might influence the efficiency of this method.
In general, to better understanding of the properties of the mantle, it is useful to assess observable characteristics of plumes in the mantle, including geoid, topography and heat flow anomalies. However, only few studies exist on geoid and topography for axi-symmetric convection and their models were restricted to isoviscous (or stratified) mantle and low Rayleigh numbers. We studied fully coupled depth and temperature dependent Arrhenius type of viscosity in axi-symmetric spherical shell geometry in order to investigate the shape of geoid anomalies and dynamic topography above a plume. Indeed, the topography and geoid anomalies produced from plumes are sensitive to rheology of the mantle and rheology of the plume; both have effects on shape and amplitude of the geoid anomalies. As results we are able to define different classes of plumes by their geoid signals.
Mainly depth-dependent viscosity models show a geoid with negative sign above the plume which can turn to the positive sign by decrease the viscosity contrast. This can be considered as a transition between the strongly depth dependent and the constant viscosity case. Our results basically support the idea by Morgan [1965] and McKenzie [1977]. They have shown the magnitude and even the sign of the total gravity anomaly depend on the spatial variation in effective viscosity. In addition, Hager [1984] has concluded that the total gravity field is depend on the radial distribution of effective viscosity, and a small change in viscosity contrast leads to varying sign of the response function.
In the case of temperature-dependent viscosity, the formation of an immobile lithosphere is a natural result, and the flow as well as the total geoid becomes strongly time dependent. When we increase the activation energy, all geoids associated with the first arriving plumes look like bell shaped whereas for typical plumes, after reaching a statistical steady state, bell-shaped geoids with decreasing amplitude as well as linear flank shaped geoids are observed. It is surprising that in spite of large differences in lateral and depth varying viscosities, the shapes of the geoid anomalies remained rather similar. We also identified different behaviors in the combined model with temperature-and pressure-dependent viscosity. In fact, in spite of the strongly different rheology, the geoid anomalies in all cases were surprisingly similar. Furthermore, we proposed a scaling law for the geoid which makes our results directly applicable to other planets. Moreover, we can apply the results of our calculation to find relations between different rheology and sub-lid temperature, since we know that the mantle temperature can change significantly with variation in pressure-temperature dependent viscosity. It is also possible to define a range of stagnant lid thickness related to the amplitude of the geoid which can be reasonable for study of the lid thickness in Venus or Mars.
Nevertheless, in these series of models, we simplified a number of complexities within the Earth. One of the most important of such simplification is the Boussinesq approximation. This approximation is valid if the temperature scale height (i.e. the depth over which temperature increases by a factor of “ ” due to adiabatic compression) is much greater than the convection depth. However, a temperature scale height in the Earth’s mantle is at best only slightly greater than the mantle depth. Hence, the Boussinesq approximation could mask some very important stratification and compressibility effects that influence both the spatial and temporal structure of the convection. Therefore, in more advance models we considered compressibility in our mantle convection models, assuming that density vary both radially and laterally, being determined as a function of pressure and temperature through an appropriate equation of the state. Moreover, thermodynamic properties assumed to be a function of depth.
We examined the details of the structure of the spherical axi-symmetric Anelastic Liquid Approximation model (ALA) with special attention to the Arrhenius rheology, and compare it to the cases of compressible convection without depth dependent thermodynamical properties, and to cases of the extended Boussinesq approximation. At the same time, the effects of the interaction between temperature and pressure-dependent viscosity and thermodynamic parameters in the compressible mantle convection on the geoid and topography have been studied. We showed that assuming compressible convection with depth-dependent thermodynamic properties strongly influence the geoid undulations. Using compressible convection with constant thermodynamic properties is physically inconsistent and may lead to spurious results for the geoid and convection pattern. Indeed, by a systematic study of different approaches of compressibility in the spherical shell convection for different Arrhenius viscosity laws we proved that only in the unrealistic case of zero activation energy the different compressibility modes result in comparable convection and geoid patterns. In all other rheological cases, large differences have been obtained, that stressing the important role of consistent compressible thermodynamic properties for mantle convection.
In addition, we examine the impact of compressibility as well as different rheologies on the power law relation that connects the Nusselt number to the Rayleigh number. We have discovered that the power law index of the relationship is controlled by the rheology, independent of which approximation is used. Instead, the bound of this relation is controlled by a combination of different approximation and rheology.
Next, instead of focusing on the time evolution of mantle flow, we have carried out three-dimensional spherical shell models of mantle circulation to investigate the effects of joint radial and lateral viscosity variations on the Earth’s non-hydrostatic geoid, surface and core-mantle boundary topographies. These models include realistic lateral viscosity variations (LVV) in the lithosphere, upper mantle and lower mantle in combination with different stratified viscosity structures. We have demonstrated that the contradictory results concerning the effects of LVV can be clarified by the most straight-forward problem in geoid modeling; namely, rather poorly known stratified viscosity structure. We explored three classes of dynamic geoid models due to lateral viscosity variations. In the first class, the LVV strongly improved the fit to the observed geoid. Indeed, when the viscosity contrast between lower and upper mantles is not large enough to produce a good fit to geoid the LVVs are able to perform this action by adjusting amplitudes, so that it becomes comparable with observation. In the second class, inducing the LVV moderately improved the fit. Actually, when the geoid induced by a stratified viscosity structure already has a good correlation with observation, then the LVV causes its amplitude to further improve. In the last class, if the viscosity contrast between upper and lower mantle would be high enough, inducing LVV deteriorate the fit to the observed geoid.. Indeed, depending on the stratified viscosity, inducing the LVV may take place in one of these categories.
We also quantified the effects of LVV in the mantle and lithosphere individually. We found that the presence of LVV in the mantle (upper and lower) improves the fit to the observed geoid regardless of stratified viscosity. While LVV in the lithosphere is a crucial parameter, and dependent of the stratified viscosity, may increase or decrease the geoid fit. In fact, when the lower mantle considers being viscous enough, it would support the negative buoyancy of subducting slabs. Thus, it transmits some of the stress back to the top boundary and causes a weak coupling between slab and surface. Therefore, by including the low viscous plate boundaries in this model, the slabs and overriding plates decouples and the fit to the observed geoid degrades. In contrast, when the lower mantle viscosity is not sufficiently stiff, the presence of the low viscous plate boundaries assists to weaken the strong mechanical coupling between slab and surface. Hence, a better fit achieved.
In the absence of apparent mutations, alteration of gene expression patterns represents the key mechanism by which normal cells evolve to cancer cells.
Gene expression is tightly regulated by posttranscriptional processes. Within this context, RNA-binding proteins (RBPs) represent fundamental factors, since they control mechanisms, such as mRNA-stabilization, -translation and -degradation. Human antigen R (HuR) was among the first RBPs that have been directly associated to carcinogenesis. HuR modulates the stability and translation of mRNAs which encode proteins facilitating various ‘hallmarks of cancer’, namely proliferation, evasion of growth suppression, angiogenesis, cell death resistance, invasion and metastasis. Furthermore, it is well established that tumor-promoting inflammation contributes to tumorigenesis. In this process, monocytes are attracted to the site of the tumor and educated towards a tumor-promoting macrophage phenotype. While HuR has been extensively studied in various tumor cell types, little is known about HuR in hepatocellular carcinoma (HCC). Thus, the aim of my work was to characterize the contribution of HuR to the development of cancer characteristics in HCC. I was particularly interested to investigate if HuR facilitates tumor-promoting inflammation, since a role for HuR has not been described in this context. To this end, I depleted HuR in HepG2 cells (HuR k/d) and used a co-culture model of HepG2 tumor spheroids and infiltrating monocytes to study the impact of HuR on the tumor microenvironment. I could show that depletion of HuR resulted in the reduction of cell numbers. Additionally, the expression of proliferation marker KI-67 and proto-oncogene c-Myc was reduced, supporting a proliferative role of HuR. Furthermore, exposure to cytotoxic staurosporine elevated apoptosis in HuR k/d cells compared to control cells. Concomitantly, the expression of the anti-apoptotic mediator B-cell lymphoma protein-2 (Bcl-2) was markedly reduced in the HuR k/d cells, pointing to an involvement of HuR in cell survival processes.
Accordingly, a pro-survival function of HuR was also observed in tumor spheroids, since HuR k/d spheroids exhibited a larger necrotic core region at earlier time points and showed elevated numbers of dead cells compared to control (Ctr.) spheroids. Interestingly, HuR k/d spheroids isplayed reduced numbers of infiltrated macrophages, suggesting that HuR contributes to a tumor-promoting, inflammatory microenvironment by recruiting monocytes/macrophages to the tumor site. Aiming at identifying HuR-regulated factors responsible for the recruitment of monocytes, I found reduced levels of the chemokine interleukin 8 (IL-8) in supernatants of HuR k/d spheroids, supporting a critical involvement of HuR in the chemoattraction of monocytes. Analyzing supernatants of co-cultures of macrophages and HuR k/d or Ctr. spheroids revealed additional differences in chemokine secretion patterns. Interestingly, protein levels of many chemokines were elevated in co-cultures of HuR k/d spheroids compared to control co-cultures. Albeit enhanced chemokine secretion was observed, less monocytes are recruited into HuR k/d spheroids, further underlining the necessity of HuR in cancer related monocyte/macrophage attraction and infiltration. Differences between chemokine profiles of mono- and co-cultured spheroids could be attributable to changes in spheroid-derived chemokines as a result of the crosstalk with the immune cells. Provided the chemokines originate from monocytes/macrophages, the different secretion patterns suggest that HuR contributes to the modulation of the functional phenotype of infiltrated macrophages, since the tumorenvironment is critically involved in the shaping of macrophage phenotypes. Regions of low-oxygen (hypoxia) represent another critical feature of tumors. Therefore, I next analyzed the impact of HuR on the hypoxic response. Loss of HuR attenuated hypoxia-inducible factor (HIF) 2α expression after exposure to hypoxia, while HIF-1α protein levels remained unaltered. Considering previous results of our group, showing that HIF-2α depletion (HIF-2α k/d) resulted in the enhanced expression of HIF-1α protein, I aimed to determine the involvement of HuR in the compensatory upregulation of HIF-1α protein in HIF-2α k/d cells. I could demonstrate that not only total HuR protein levels, but specifically cytoplasmic HuR was elevated in HIF-2α depleted cells pointing to enhanced HuR activity. Silencing HuR in HIF-2α deficient cells attenuated enhanced HIF-1α protein expression, thus confirming a direct role of HuR in the compensatory upregulation of HIF-1α. This as also reflected on HIF-1α target gene expression. I further investigated the mechanism underlying the compensatory HIF-1α expression in HIF-2α deficient cells. Analyzing HIF-1α mRNA expression, I excluded enhanced HIF1-α transcription and stability to account for elevated HIF-1α expression in HIF-2α k/d cells. HIF-1α promoter activity assays confirmed the mRNA data. Furthermore, HIF-1α protein half-life was not elevated in HIF-2α k/d cells compared to control cells, indicating that HIF-1α protein stability is not altered in HIF-2α k/d cells. Analysis of the association of HIF-1α with the translational machinery using polysomal fractionation finally revealed an increased istribution of HIF-1α mRNA in the heavier polysomal fractions in HIF-2α k/d cells compared to control cells. Since augmented ribosome occupancy is an indicator for more efficient translation, I propose enhanced HIF-1α translation as underlying principle of the compensatory increase in HIF-1α protein levels in HIF-2α k/d cells. In summary, my results demonstrate that HuR is critical for the development of cancer characteristics in HCC. Future work analyzing the impact of HuR on tumor-promoting inflammation, specifically macrophage attraction and activation could provide new trategies to inhibit macrophage-driven tumor progression. Furthermore, I provide evidence that HuR contributes to the hypoxic response by regulating the expression of HIF-1α and HIF-2α. Targeting single HIF-isoforms for tumor therapy should be carefully considered, because of their compensatory regulation when one α-subunit is depleted. Thus, therapeutic strategies targeting factors such as HuR that control both α-subunits and at the same time prevent compensation might be more promising.
The spider genus Eusparassus Simon, 1903 (Araneae: Sparassidae: Eusparassinae; stone huntsman spider) is revised worldwide to include 30 valid species distributed exclusively in Africa and Eurasia. The type species E. dufouri Simon, 1932 is redescribed and a neotype is designated from Portugal. An extended diagnosis for the genus is presented. Eight new species are described: Eusparassus arabicus Moradmand, 2013 (male, female) from Arabian Peninsula, E. educatus Moradmand, 2013 (male, female) from Namibia, E. reverentia Moradmand, 2013 (male, female) from Burkina Faso and Nigeria, E. jaegeri Moradmand, 2013 (male, female) from South Africa and Botswana, E. jocquei Moradmand, 2013 (male, female) from Zimbabwe, E. borakalalo Moradmand, 2013 (female) from South Africa, E. schoemanae Moradmand, 2013 (male, female) from South Africa and Namibia and E. mesopotamicus Moradmand and Jäger, 2012 (male and female) from Iraq, Iran and Turkey. 22 species are re-described six of them are transferred from the genus Olios Walckenaer, 1837. Six species-groups are proposed: the dufouri-group [8 species: E. dufouri, E. levantinus Urones, 2006, E. barbarus (Lucas, 1846), E. atlanticus Simon, 1909, E. syrticus Simon, 1909, E. oraniensis (Lucas, 1846), E. letourneuxi (Simon, 1874), E. fritschi (Koch, 1873); Iberian Peninsula to parts of north-western Africa], walckenaeri-group [3 species: E. walckenaeri (Audouin, 1826), E. laevatus (Simon, 1897), E. arabicus; eastern Mediterranean to Arabia and parts of north-eastern Africa], doriae-group [7 species: E. doriae (Simon, 1874), E. kronebergi Denis, 1958, E. maynardi (Pocock, 1901), E. potanini (Simon, 1895), E. fuscimanus Denis, 1958, E. oculatus (Kroneberg, 1846) and E. mesopotamicus; Middle East to Central and South Asia], vestigator-group (3 species: E. vestigator (Simon, 1897), E. reverentia, E. pearsoni (Pocock, 1901); central to eastern Africa and an isolated area in NW India], jaegeri-group [4 species: E. jaegeri, E. jocquei, E. borakalalo, E. schoemanae; southern and south-eastern Africa], tuckeri-group [2 species: E. tuckeri (Lawrence, 1927), E. educatus; south-western Africa). Two species, E. pontii Caporiacco, 1935 and E. xerxes (Pocock, 1901) cannot be placed in any of the above groups. Two species are transferred from Eusparassus to Olios: O. flavovittatus (Caporiacco, 1935) and O. quesitio Moradmand, 2013. 14 species are recognized as misplaced in Eusparassus, thus nearly half of the described species prior to this revision were placed mistakenly in this genus. Neotypes are designated for E. walckenaeri from Egypt, E. barbarus, E. oraniensis and E. letourneuxi (all three from Algeria) to establish their identity. The male and female of Cercetius perezi Simon, 1902, which was known only from the immature holotype, are described for the first time. It is recognized that the monotypic and little used generic name Cercetius Simon, 1902 — a species, which had been known only from the immature holotype — as a synonym of the widely used name Eusparassus. The case proposal 3596 (conservation of name Eusparassus) is under consideration by ICZN.
The first comprehensive molecular phylogeny of the family Sparassidae with focus on the genus Eusparassus is investigated using four molecular markers (mitochondrial COI and 16S; nuclear H3 and 28S). The monophyly of Eusparassus and the dufouri, walckenaeri and doriae species-groups are recovered with the latter two groups more closely related. The monophyly of the tuckeri-group is not supported and the position of E. jaegeri as the only available member of the jaegeri-group is not resolved within the Eusparassus clade. DNA samples of the vestigator-group were not accessible for this study. The origination of the genus Eusparassus around 70 million years ago (MA) is estimated according to molecular clock analyses. Using this recent result in combination with some biogeographic and geological data, the Namib Desert is proposed as the place of ancestral origin for Eusparassus and putative Eusparassinae genera.
Further analyses are done on the phylogenetic relationships of Sparassidae and its subfamilies. The Eusparassinae are not confirmed as monophyletic, with the two original genera Eusparassus and Pseudomicrommata in separate clades and only the latter clusters with most other assumed Eusparassinae, here termed the "African clade". Monophyly of the subfamilies Sparianthinae, Heteropodinae sensu stricto, Palystinae and Deleninae is recovered. The Sparianthinae are supported as the most basal clade, diverging considerably early (143 MA) from all other Sparassidae. The Sparassinae and genus Olios are found to be polyphyletic. The Sparassidae are confirmed as monophyletic and as most basal group within the RTA-clade. The divergence time of Sparassidae from the RTA-clade is estimated with 186 MA in the Jurassic. No affiliation of Sparassidae to other members of the "Laterigradae" (Philodromidae, Selenopidae and Thomisidae) is observed, thus the crab-like posture of this group was proposed a result of convergent evolution. Only the families Philodromidae and Selenopidae are found members of a supported clade. Including a considerable amount of RTA-clade representatives, the higher-level clade Dionycha is not but monophyly of the RTA-clade itself is supported.
A stochastic model for the joint evaluation of burstiness and regularity in oscillatory spike trains
(2013)
The thesis provides a stochastic model to quantify and classify neuronal firing patterns of oscillatory spike trains. A spike train is a finite sequence of time points at which a neuron has an electric discharge (spike) which is recorded over a finite time interval. In this work, these spike times are analyzed regarding special firing patterns like the presence or absence of oscillatory activity and clusters (so called bursts). These bursts do not have a clear and unique definition in the literature. They are often fired in response to behaviorally relevant stimuli, e.g., an unexpected reward or a novel stimulus, but may also appear spontaneously. Oscillatory activity has been found to be related to complex information processing such as feature binding or figure ground segregation in the visual cortex. Thus, in the context of neurophysiology, it is important to quantify and classify these firing patterns and their change under certain experimental conditions like pharmacological treatment or genetical manipulation. In neuroscientific practice, the classification is often done by visual inspection criteria without giving reproducible results. Furthermore, descriptive methods are used for the quantification of spike trains without relating the extracted measures to properties of the underlying processes.
For that reason, a doubly stochastic point process model is proposed and termed 'Gaussian Locking to a free Oscillator' - GLO. The model has been developed on the basis of empirical observations in dopaminergic neurons and in cooperation with neurophysiologists. The GLO model uses as a first stage an unobservable oscillatory background rhythm which is represented by a stationary random walk whose increments are normally distributed. Two different model types are used to describe single spike firing or clusters of spikes. For both model types, the distribution of the random number of spikes per beat has different probability distributions (Bernoulli in the single spike case or Poisson in the cluster case). In the second stage, the random spike times are placed around their birth beat according to a normal distribution. These spike times represent the observed point process which has five easily interpretable parameters to describe the regularity and the burstiness of the firing patterns.
It turns out that the point process is stationary, simple and ergodic. It can be characterized as a cluster process and for the bursty firing mode as a Cox process. Furthermore, the distribution of the waiting times between spikes can be derived for some parameter combination. The conditional intensity function of the point process is derived which is also called autocorrelation function (ACF) in the neuroscience literature. This function arises by conditioning on a spike at time zero and measures the intensity of spikes x time units later. The autocorrelation histogram (ACH) is an estimate for the ACF. The parameters of the GLO are estimated by fitting the ACF to the ACH with a nonlinear least squares algorithm. This is a common procedure in neuroscientific practice and has the advantage that the GLO ACF can be computed for all parameter combinations and that its properties are closely related to the burstiness and regularity of the process. The precision of estimation is investigated for different scenarios using Monte-Carlo simulations and bootstrap methods.
The GLO provides the neuroscientist with objective and reproducible classification rules for the firing patterns on the basis of the model ACF. These rules are inspired by visual inspection criteria often used in neuroscientific practice and thus support and complement usual analysis of empirical spike trains. When applied to a sample data set, the model is able to detect significant changes in the regularity and burst behavior of the cells and provides confidence intervals for the parameter estimates.