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Bacteria are highly organized organisms which are able to adapt to and propagate under a multitude of environmental conditions. Propagation hereby requires reliable chromosome replication and segregation which has to occur cooperatively with other cellular processes such as transcription, translation or signaling. Several mechanisms were proposed for segregation of the Escherichia coli (E. coli) chromosome, for example a mitotic-like active segregation model or entropy-based passive chromosome segregation. Another segregation model suggests coupled transcription, translation and insertion of membrane proteins (termed "transertion"), which links the replicating chromosome (nucleoid) to the growing cell cylinder.
Fluorescence microscopy was widely used to provide evidence for a distinct segregation model. However, the dynamic nature of bacterial chromosomes, the small bacterial size and the optical resolution limit of ~ 200-300 nm impair unveiling the underlying mechanisms. With the emergence of super-resolution fluorescence microscopy techniques and advanced labeling methods, a new toolbox became available enabling scientists to visualize biomolecules and cellular processes in unprecedented detail. Single-molecule localization microscopy (SMLM) represents a set of super-resolution microscopy techniques which relies on the temporal separation of the fluorescence signal and detection of single fluorophores. Separation can be achieved using photoactivatable or -convertible fluorescent proteins (FPs) in photoactivated localization microscopy (PALM), photoswitchable organic dyes in direct stochastic optical reconstruction microscopy (dSTORM) or dynamically binding fluorescent probes in point accumulation for imaging in nanoscale topography (PAINT). In all these techniques, the fluorescence emission pattern of single fluorophores is spatially localized with nanometer-precision. An artificial image is finally reconstructed from the coordinates of all single fluorophores detected. This provides a spatial resolution of ~ 20 nm, which is perfectly suited to investigate cellular processes in bacteria. In this thesis, different SMLM techniques were applied to study fundamental processes in E. coli. This includes determination of protein copy numbers and distributions as well as the nanoscale organization of nucleic acids and lipids.
A novel labeling approach was applied and used for super-resolution imaging of the E. coli nucleoid. It is based on the incorporation of the modified thymidine analogue 5-ethynyl-2’- deoxyuridine (EdU) into the replicating chromosome. Azide-functionalized organic fluorophores can be covalently attached to the ethynyl group of incorporated EdU bases using a copper-catalyzed "click chemistry" reaction. Under the investigated growth condition, E. coli cells exhibited overlapping replication cycles, which is commonly referred to as multi-fork replication and enables cells to divide faster than they can replicate the entire chromosome. dSTORM imaging of such labeled nucleoids revealed chromosome features with diameters of 50 - 200 nm, representing highly condensed DNA filaments. Sorting single E. coli cells by length allowed visualizing structural changes of the nucleoid throughout the cell cycle. Replicating nucleoids segregated and expanded along the bacterial long axis, while constantly covering the entire width of the cell. Measuring cell and nucleoid length revealed a relative nucleoid expansion rate of 78 ± 6 %. At the same time, nucleoids populated 63 ± 8 % of the cell length, almost exclusively being localized to the cylindrical part of the cell. This value was hence normalized to the cylindrical fraction of the cell, yielding a value of 79 ± 10 % (nucleoid-populated fraction of the cell cylinder), which is in good agreement with the observed relative nucleoid expansion rate. These results therefore support a growth-mediated segregation model, in which the chromosome is anchored to the inner membrane and passively segregated into the prospective daughter cells upon cell growth. 3-dimensional dSTORM imaging of labeled nucleoids confirmed that compacted nucleoids helically wrap along the inner membrane. Similar results were obtained by imaging orthogonally aligned E. coli cells using a holographic optical tweezer approach.
In order to visualize particular proteins together with the nucleoid, several correlative imaging workflows were established, facilitating multi-color SMLM imaging in single E. coli cells. These workflows bypass prior limitations of SMLM, including destruction of FPs by reactive oxygen species in copper-catalyzed click reactions or incompatibility of PALM imaging with dSTORM imaging buffers. A sequential SMLM imaging routine was developed which is based on postlabeling and retrieval of previously imaged cells. Optimal imaging conditions can be maintained for each fluorophore, enabling to extract quantitative information from PALM measurements while correlating the protein distribution to the nucleoid ultrastructure within the highly resolved cell envelope. Applying this workflow to an E. coli strain carrying a chromosomal rpoC - photoactivatable mCherry (PAmCh) fusion, transcribing RNA polymerase (RNAP) was found to be localized on the surface of nucleoids, where active genes are exposed towards the cytosol. During growth in nutrient-rich medium, the majority of RNAP molecules was bound to the chromosome, thus ensuring that the RNAP pool is equally distributed to the daughter cells upon cell division. This work represented the first triple-color SMLM study performed in E. coli cells. ...
The East African Rift System (EARS) was initiated in the Eocene epoch between 50 and 21 Ma probably due to the influence of mantle plumes that caused volcanism, flood basalts and rifting extensions in Ethiopa and the Afar region. As a result of magmatic intrusions and adiabatic decompression melting within the lithosphere caused by the impact of the Kenya plume, there was a southward propagation of the EARS of about 30 – 15 Ma from Ethiopia to Kenya, which coincide with the occurrence of volcanism. The EARS developed towards the south along the margins of the Tanzania Craton between 15 and 8 Ma. Previous findings of low-velocity anomalies within the upper mantle and the mantle transition zone indicate an upwelling of hot mantle material in the vicinity of the Afar region and the East African Rift. This study includes the analysis of P- and S-receiver functions in order to determine further impacts on the lithosphere from below. The aim was to determine the topographic undulations of further boundary layers and to identify their variability owing to the rifting processes and the formation of the EARS. The study area included the Tanzania Craton and the surrounding rift branches of the East African Rift System.
The region of the Rwenzori Mountains can be analysed in detail because of the large dataset of the RiftLink project. The use of the P-receiver function technique and the H-K stacking method enabled to determine different vP /vS ratios depending on the tectonic setting in the Rwenzori region: Rift shoulders (vP /vS =1.74), Albert Rift segment (vP /vS =1.80), Edward Rift segment (vP /vS =1.87) and Rwenzori Mountains (vP /vS =1.86). To determine the topography of the Moho, it is necessary to take into account the thickness of the sedimentary layer, the surface topography, the azimuthal variations in crustal thickness and the impact of local anomalies. After correcting these effects on the Moho depths, significant variations in Moho topography could be determined. The Moho depths range from 29 to 39 km beneath the rift shoulders of the Albertine Rift. Within the rift valley, the crustal thickness varies between 25 – 31 km in the Edward Rift segment and 22 – 30 km in the Albert Rift segment. An averaged crustal thickness of about 26 km within the rift valley indicates the lack of the crustal root beneath the Rwenzoris. Similar variations in crustal thickness were determined by using an automatic procedure for analysing S-receiver functions that was developed in this study.
The S-receiver functions are created by applying a rotation criterion in order to rotate the Z, N and E components into the L, Q and T components. It is necessary to perform trial rotations using different incident and azimuth angles to determine the correct rotation angles. The latter are identified by the use of the rotation criterion, including the amplitude ratio of the converted Moho signal to the direct S/SKS-wave signal. The L component is rotated correctly in the direction of the incident shear wave in the case of the maximum amplitude ratio. After analysing the frequency content of the receiver functions in order to sort out harmonic and long-periodic traces, the individual Moho signals are checked for consistency in order to remove atypic signals. To increase the signal-to-noise ratios on the traces, the S-receiver functions are stacked. For this purpose, the signals of the direct shear waves must originate from similar epicenters. On the basis of similar ray paths, the receiver functions show comparable waveforms and converted signals. To perform the stacking procedure, it is necessary to merge the datasets of the adjacent stations in order to obtain a sufficient number of receiver functions. This analysis is based on the assumption that the incident seismic waves arriving at the adjacent stations penetrate to some extent the same underground structures in the case of similar wave propagation paths. This approach accounts for the fact that the converted signals do not result exclusively from the piercing points at the boundary layers. Further signals originate from the conversions at the boundary layer within the Fresnel Zone. The piercing points are derived from the significant signals in the receiver functions. Depending on the order of arrival of the converted phases on the traces, the signals are attributed to the theoretical discontinuities DIS1, DIS2, DIS3 and DIS4. However, partly due to the low signal-to-noise ratios on the traces, it is difficult to identify the real conversions on the traces and to ensure that the converted signals are attributed to the correct boundary layers. For this reason, it is necessary to check the consistency of the conversion depths among each other. In the case of inconsistent conversion depths, the corresponding signals are either adjusted to another seismic boundary layer or removed from the dataset. To verify the functionality of the automatic procedure and to determine the resolvability with respect to two boundary layers, several models are tested including horizontal and dipping discontinuities. To resolve distinct discontinuities, their depths must differ by at least 60 km, otherwise, due to similar depth ranges of the different boundary layers, the converted signals cannot be separated from each other. As a consequence, the converted signals that originate from different discontinuities are attributed to a single one. Further tests including break-off edges of seismic discontinuities are performed to check the attributions of the converted signals to the discontinuities. Owing to the varying number of boundary layers, the converted signals cannot be attributed to the discontinuities according to the order of their arrivals on the traces. It is necessary to correct their attributions to the seismic discontinuities in order to resolve the boundary layers.
The crust-mantle boundary and further discontinuities within the lithospheric mantle are investigated by applying this automatic procedure. Depending on the tectonic setting, the conversion depths of the Moho range from about 30 – 45 km beneath the western rift shoulder to 20 – 35 km within the rift valley up to 30 – 40 km beneath the eastern rift shoulder. The long wavelengths of the shear waves hamper the correct identification of the converted phases in the S-receiver functions. With respect to the relative differences in conversion depth, the topographic undulations of the crust-mantle boundary are consistent with the Moho depths derived from P-receiver functions. In contrast to the Rwenzori region, it is difficult to resolve completely the trend of the Moho in the remaining area of the East African Rift due to the small dataset provided by IRIS. The results exibit an increase in crustal thickness to up to 45 km in the region of the Cenozoic volcanics such as Virunga, Kivu, Rungwe and Kenya. The greatest Moho depths of more than 50 km are located near Mount Kilimanjaro. In addition to the Moho, the analysis of the S-receiver functions revealed two further boundary layers at depths of 60 – 140 km and 110 – 260 km, which are associated with a mid-lithospheric discontinuity and the lithosphere-asthenosphere boundary, respectively. The shallowest conversion depths of the LAB are focussed to small-scale regions within the rift branches, namely the northern Albertine Rift, the Chyulu Hills and the Mozambique Belt, which are located around the Tanzania Craton. The larger thickness of the lithosphere beneath the cratonic terrain indicates that the Tanzania Craton is not significantly eroded. However, there are indications that the lithosphere beneath the craton and the rift branches is penetrated by ascending asthenospheric melts to depths of up to 140 and 60 km, respectively. The top of the ascending melts is associated with the occurrence of the mid-lithospheric discontinuity. The shallowest conversion depths of this boundary layer (60 – 90 km) are related to the rifted areas of the EARS and the Cenozoic volcanic provinces, which are located along the Albertine Rift, the Kenya Rift and the Rukwa-Malawi rift zones. The deepest conversion depths of up to 140 km are related to the Rwenzori Belt, the Ugandan Basement Complex and the interior of the Tanzania Craton.
The small leucine-rich proteoglycan biglycan (Bgn) is a part of the extracellular matrix providing structure and enhancing fibril stability. In its soluble form, biglycan is able to bind and signal via the innate immune receptors Toll-like receptor (TLR) 2 and 4, thereby activating MAP-kinases and the NF-κB pathway. In macrophages soluble biglycan induces the secretion of several cytokines and chemokines, including TNF-α, CCL2, CXCL5 and CXCL13. A unique feature of biglycan is its ability to stimulate the secretion of mature IL-1β. By orchestrating TLR2 and 4 with the purinergic P2X4 and P2X7 receptor signalling biglycan triggers the activation of the NLRP3/ASC inflammasome, which in turn activates caspase-1 to cleave pro-IL-1β to mature IL-1β. Furthermore, in several inflammatory diseases an upregulated biglycan expression is found. Enhanced levels of biglycan could be measured in plasma and inflamed tissue. In mouse models of sepsis, lupus nephritis and renal ischemic reperfusion injury, biglycan-deficiency improved the disease outcome. Overexpression of soluble biglycan on the other hand increased immune cell infiltration into the kidney by inducing cytokine and chemokine expression in a TLR2/4-dependent manner. These studies emphasise its importance in inflammatory processes, especially in the kidney. Furthermore, the pro-inflammatory effects on macrophages and diseases established biglycan as a danger signalling molecule, yet its role as a soluble molecule in plasma was not further investigated.
Although an increase of soluble biglycan in the circulation could be seen in several inflammatory diseases, the source is not fully unravelled. Previously it could be shown that macrophages and dendritic cells secrete soluble biglycan after stimulation with IL-6 and TGF-β1. However, since these cell are resident in organs and do not circulate in the blood stream their contribution to soluble biglycan levels in plasma is likely minor. Therefore, monocytes as precursor of both macrophages and dendritic cells were investigated as a possible source of circulating biglycan. Analysis of blood from septic patients revealed elevated soluble biglycan levels as well as an increased number of monocytes. Isolated monocytes from healthy volunteers incubated with the inflammatory cytokines IL-1β, IL-6 and TGF-β1 displayed increased biglycan mRNA expression and secretion of soluble biglycan into the supernatant, revealing monocytes as a producer of soluble biglycan in blood. Therefore this work was directed to further investigate the influence of soluble biglycan on circulating monocytes, with regard to sepsis.
Monocytes can be classified into three subtypes, while the classical monocytes express CD14 (CD14++CD16low), intermediate monocytes express both CD14 and CD16 (CD14++CD16+) and non-classical monocytes express mainly CD16 (CD14lowCD16++). The intermediate and non-classical monocytes make up about 10 % of all monocytes and are referred to as CD16-positive subtypes. The CD16-positive monocytes express higher levels of TNF-α and IL-1β upon stimulation and display different migration behaviour. In most inflammatory diseases an expansion of CD16-positive monocytes is observed, especially an increased number of intermediate monocytes frequently correlate with disease severity and mortality. Since septic patients had increased circulating biglycan levels and augmented CD16-positive monocytes, a possible correlation between these two parameters was investigated. Using FACS analysis of biglycan-stimulated monocytes from healthy donors revealed a significant shift from classical to intermediate and non-classical monocytes. This shift was mediated by increased expression of CD14 and CD16 on mRNA and protein levels upon biglycan treatment. Furthermore, biglycan induced the mRNA expression of the adhesion molecules ICAM-1, VCAM-1 and ELAM-1 in CD14-positive monocytes. Four hours after biglycan stimulation an increased ICAM-1 protein expression on the cell surface of classical and intermediate monocytes was observed. Additionally, biglycan-treated CD14-positive monocytes rolled and attached to pre-stimulated endothelial cells to a greater extent compared to untreated monocytes. This demonstrates that biglycan not only triggers the expression of CD14 and CD16 but also induces a functional shift of monocytes. ...
Over the last several decades, spinel-structured minerals with the chemical formula AB2O4 (where A and B stand for divalent and trivalent cations, respectively) have attracted more and more attention, particularly with regards to their breakdown at high pressures and temperatures and the nature of the so-called "post-spinel" phases. Spinel-structured phases with different endmember compositions, like magnetite (Fe3O4), hercynite (FeAl2O4) or spinel (MgAl2O4), are known to breakdown differently at high pressure-temperature conditions (e.g., Akaogi et al. 1999; Schollenbruch et al. 2010; Woodland et al. 2012). Such phases are of particular interest when they incorporate ferric (Fe3+) and ferrous (Fe2+) cations as this makes their stability sensitive to redox conditions. Since magnetite and magnesioferrite (MgFe3+ 2O4) have been found as inclusions in diamond (e.g., Stachel et al. 1998; Harte et al. 1999; Wirth et al. 2014; Palot et al. 2016; Jacob et al. 2016), understanding their phase relations is important for setting constraints on the conditions of their formation.
This study aimed to experimentally investigate the phase relations of Fe-Mg spinel-structured phases at conditions of the deep upper mantle and transition zone. Exploring the stability of new post-spinel phases and their characterization were also major goals of this study. Approaching a pyrolitic mantle composition by adding amounts of SiO2 in the system allowed constraints on the relevance of Fe-Mg post-spinel phases coexisting with mantle silicates to be made. ...
A great challenge in life sciences remains the site-specific modification of proteins with minimal perturbation for in vitro as well as in vivo studies. Therefore, different chemoselective reactions and semi-synthetic techniques such as native chemical ligation or intein-mediated protein splicing have been established. They enable a site-specific incorporation of chemical reporters into proteins, such as organic fluorophores or unnatural amino acids. In this PhD Thesis, protein trans-splicing was guided by minimal high-affinity interaction pairs to trace proteins in mammalian cells. In addition, the temporal modulation of cellular processes by photo-cleavable viral immune evasins was achieved.
Protein trans-splicing mediated by split inteins is a powerful technique for site-specific and 'traceless' protein modifications. Despite recent developments there is still an urgent need for ultra-small high-affinity intein tags for in vitro and in vivo approaches. So far, only a very few in-cell applications of protein trans-splicing are reported, all limited to C-terminal protein modifications. Here, a strategy for covalent N-terminal intein-mediated protein labeling at sub-nanomolar probe concentrations was developed. Combined with the minimalistic Ni-trisNTA/His-tag interaction pair, the affinity between the intein fragments was increased 50-fold (KD ~ 10 nM). Site-specific and efficient 'traceless' protein modification by high-affinity trans-splicing is demonstrated at nanomolar concentrations in mammalian cells.
High background originating from non-reacted, 'always-on' fluorescent probes still is a crucial issue in life sciences. Covalent labeling approaches with simultaneous activation of fluorescence are advantageous to increase sensitivity and to reduce background signal. Therefore, high-affinity protein trans-splicing was combined with fluorophore/quencher pairs for online detection of covalent N-terminal protein labeling in cellular environments. Substantial fluorescence enhancement at nanomolar probe concentrations was achieved. This ultra-small fluorogenic high-affinity split intein system is an unprecedented example for real-time monitoring of the trans-splicing reaction in cell-like environments as well as for protein labeling with fluorogenic probes at nanomolar concentrations.
To extend the field of chemical immunology and to address spatiotemporal aspects in adaptive immune response, new tools to control antigen processing are required. Therefore, synthetic photo-conditional viral immune evasins were designed to modulate antigen processing on demand. By using light, the time and dose controlled antigen translocation by the transporter associated with antigen processing (TAP) was triggered with response in the second regime. Peptide delivery and loading by the peptide-loading complex (PLC) was rendered inactive, whereas blocking was abolished in a light-controlled fashion to inactivate the synthetic viral immune evasin ICP47 along with simultaneous activation of the antigen presentation pathway. Lightresponsive peptide translocation by the TAP complex was assayed in vitro by utilizing microsomes isolated from professional antigen presenting B-cell lymphomas (Raji). To extend these studies, suppression and photo-controlled rescue of antigen presentation was examined at single-cell resolution in human primary immune cells.
Native chemical ligation interconnects peptide chemistry with recombinantly expressed proteins. This technique was applied to generate the semi-synthetic full-length ICP47. Although this approach was realized, the low product yield was not sufficient for further functional studies. Therefore, full-length ICP47 was consecutively generated by utilizing a full synthetic four-fragment ligation approach. However, this synthetic viral immune evasin was not able to block peptide translocation in a robust way.
Indian Ocean came into existence with the breakup of Gondwana in the Mesozoic era. The presence of complex aseismic ridges and plateaus in the Indian Ocean makes it the least-understood of all the oceans. Mascarene Plateau, apart from Central Indian Ridge (CIR) running north-south between 2◦N and 25◦S in the Indian Ocean, is one such complex feature in the Indian Ocean that consists of Seychelles microcontinent in the north and the volcanic islands of Mauritius, La Réunion and Rodrigues in the south.
Most of the previous seismological studies on the islands of Mauritius, Rodrigues and Seychelles are restricted as each of them has only one operational permanent station. In the current study, I present the results obtained from the investigations of the seismological data obtained from the deployment of temporary seismic network on Mauritius (November, 2012–August, 2014) and Seychelles (March, 2013–March, 2015) under Réunion Hotspot and Upper Mantle–Réunions Unterer Mantel (RHUM–RUM) project and later in Rodrigues (September, 2014–June, 2016) under a collaborative project between Goethe-Universität, Frankfurt, Germany and Mauritius Oceanography Institute (MOI), Mauritius. Additional data from the permanent stations were also used in this study. The investigations and results are presented under three themes, namely: (1) crustal structure beneath Mauritius, (2) upper mantle anisotropy below Mauritius, Rodrigues and Seychelles and (3) intraplate seismicity in the Rodrigues–CIR region.
Upper mantle anisotropy in south-west Indian Ocean region are very limited, especially from the islands of Mauritius and Rodrigues. With the new data from the seismic stations deployed in Mauritius and Seychelles, under RHUM–RUM, and permanent stations in Rodrigues, I constrain the upper mantle flow pattern beneath these islands. From the joint-splitting analysis, I obtain fast-polarisation direction (φ) dominant in N80◦E and delay time (δt) of ≈0.85 s for Mauritius and φ tending east–west in Rodrigues with δt of ≈1.1 s. Parabolic asthenospheric flow model explains the orientation of the fast-polarisation direction beneath Mauritius, whereas deep mantle circulation patterns best explain the horizontal alignment of the fast-polarisation direction in Rodrigues. From Seychelles data, the results show φ trending NE and δt ≈0.74 s, even for the island close to Amirante Ridge, suggesting an asthenospheric deformation induced by relative motion between the plate and the deep mantle flow.
It has recently been suggested that the volcanic island of Mauritius may be underlain by a remnant of continental origin termed “Mauritia.” To constrain the crustal thickness beneathMauritius, I analysed data from 11 land stations, 10 of which were deployed recently under the RHUM–RUM project. From the recordings, I obtained 382 P-receiver functions. On the obtained receiver functions, I applied the H–κ stacking technique and derived the crustal thickness of ≈10–15 km. I observe a considerable variation in the VP/VS ratio caused by a lack of clear multiples. Using forward modelling of receiver functions, I show that the lack of clear multiples can be explained by a transitional Moho, where the velocity increases gradually. The modelling further indicates that the thickness of this gradient zone is estimated to be ≈10 km. I argue that my findings suggest oceanic crust thickened by crustal underplating due to the mantle plume currently located beneath La Réunion.
Seismicity around Rodrigues Island is generally associated with events recorded by the global networks along the CIR. Using seismological array techniques on the data collected by the temporary deployment of seismic array on Rodrigues Island for a period of 22 months (September, 2014–June 2016), 62 new events were located, which were not reported by any global network. Determination of backazimuth and apparent velocity were performed by applying array methods in the time-domain instead of the more conventional frequency-domain analysis. Event distances were calculated using a 1-D velocity model and the measured travel-time differences between S- and P-wave arrivals. Local magnitudes of the events were obtained by removing the velocity response from the seismographs and then convolving with Wood–Anderson transfer function to obtain ground motion in nanometers. Most of the newly-detected events are located off the ridge axis and can be classified as intraplate events. Three different seismic clusters were observed around the island. Most of the events were localised in the north-east of Rodrigues at a distance of ≈138 km from the reference station. A distinguishable swarm of earthquakes was observed on the west of the spreading segment from March to April 2015. The local magnitudes (ML) of the events varied between 1.6 and 3.7.
Tissue integrity is defined by the composition and connection of cells as a structural and functional unit. It is modulated by a magnitude of processes including differentiation, survival, controlled death and adhesion of cells. Besides, external factors such as physical forces are also involved. A suitable model system to study all modalities of tissue integrity is the mammary gland. Postnatally and within the reproductive phase, the mammary gland undergoes morphological and functional modifications that periodically loosen or strengthen tissue integrity. An important point in the development of the mammary gland is the regression during weaning, also termed involution. The transition from lactation to involution is important for a controlled loss of tissue integrity. In this transition, collective cell death is initiated but not yet prominent enabling the mammary gland to fully recover lactation.
In this thesis, modalities of tissue integrity were investigated using three-dimensional cell cultures (i.e. spheroids) and the mammary gland as model systems. In the context of this thesis, I established (1) an immunofluorescence staining protocol and its detailed evaluation. Furthermore, I studied (2) the role of cell survival during mammary gland development, (3) the effect of physical forces that modulate tissue integrity and (4) the contribution of proteins to cell adhesion and growth.
Since a homogeneous fluorescence stain of the specimen is necessary for quantitative analysis, an immunofluorescence staining protocol was established to stain large spheroids in toto. The evaluation contributes qualitative and quantitative criteria that judge the specificity, intensity and homogeneity of the stain. Based on this approach, it was possible to demonstrate the morphological and functional characteristics that spheroids share with the mammary gland in vivo. These characteristics included the synthesis of extracellular matrix, the development of polarized acinar structures and lactogenic differentiation.
The role of cell survival during mammary gland development was analyzed by means of the expression profile of the pro-survival protein BAG3. The expression of BAG3 differed in the progress of mammary gland development. While the expression was low during pregnancy, it rose in the lactation phase and peaked within the first days of involution, indicating that BAG3 is associated with early involution in the mammary gland. In vitro experiments related the expression of BAG3 to cell survival in mammary epithelial cells.
Physical forces naturally occur during developmental processes influence tissue integrity during the initiation of mammary gland involution. The influence of physical force applied as compression on mammary epithelial spheroids was investigated. A morphological analysis showed that following a lag, the cell nuclei volume changed upon compression. A short-term compression induced the activation of caspases. A prolonged compression reduced the activity of caspases. This suggests the induction of a process that allows cells the adaption to changing environmental conditions. BAG3 is known to be involved in mechanical stress-induced autophagy, also known as chaperone assisted selective autophagy (CASA). Compression of spheroids did not induce CASA. The experimentally applied strain was not comparable to the strain found in the alveolar cells during involution in vivo. Thus, whether or not CASA is activated during mammary gland involution remains elusive. Nevertheless, the methodical approach to apply compression on spheroids in vitro is a model to study the influence of physical forces on cell aggregates.
Apart from cell survival and physical forces, growth and adhesion of cells affect tissue integrity. A spheroid formation assay and subsequent data analysis and computational modeling enabled the investigation of these processes in a non-adhesive environment. The analysis suggested that spheroid formation follows a reaction-controlled process, in which cells do not necessarily form a connection when they collide. The loss of function of either E-cadherin or actin strongly inhibited the formation of a spheroid. The analysis further revealed that neither E-cadherin nor actin influence the chance of the cells to form a connection when they collide. Both molecules are more important in stabilizing established connections. Depolymerization of microtubules still allowed spheroids to form, but the formation was decelerated and growth of the final spheroids was inhibited. The results from computational modeling suggested that microtubules act on cell adhesion through different mechanisms, which also vary among different cell types. The inhibition of FAK phosphorylation at Y397, a downstream target of integrin signaling, and the analysis of FAK protein levels in spheroids showed that integrin-mediated signaling is not prominent in three-dimensional spheroids formed from non-invasive cells. A deletion of BAG3 gene expression increased the number of dead cells in forming spheroids suggesting that BAG3 predominantly affects cell survival.
The results of this thesis identified and characterized adhesion- and survival-associated proteins that are important for tissue integrity. This thesis suggests that a BAG3-dependent cell survival mechanism is prominent at the beginning of mammary gland involution. Future studies will have to identify the related factors and inducers of tissue integrity loss in the mammary gland. This will shed light on the physiology of the organ and could explain the disorders that destroy its integrity. In addition, this thesis contributes to a better understanding of spontaneous cell aggregation, the aggregate organization and implies a role of cell migration in these processes. Future studies that focus on three-dimensional cell migration could explain, how cell migration is promoted and to which extent it supports tissue integrity.
Die Arbeit beschäftigt sich mit der Herstellung sowie der strukturellen und magnetischen Charakterisierung von zwei Materialklassen von kupferbasierten zweidimensionalen Quanten-Spin-Systemen: Quadratische Gitter von Dimeren sowie geometrisch frustrierte Kagomé Gitter. In beiden Systemen werden Substitutionen vorgestellt die zu verbesserten Eigenschaften führen.
Savannas provide essential ecosystem services for human well-being in West Africa. Thus, ecosystem change not only directly affects biodiversity but also human livelihoods. Human land use considerably shaped these savanna ecosystems for millennia, particularly agriculture, livestock grazing, logging and the collection of non-timber forest products (NTFPs). NTFPs are wild plant products and comprise all organic matter from herbaceous plants, shrubs, and trees (excluding timber). Current increasing land use pressure through fast demographic changes is widely esteemed as a severe threat for savanna biodiversity and the socio-economy of rural communities. In consideration of the pivotal role of NTFP species for biodiversity and livelihoods, it is important to evaluate the effect of increasing land use change on savanna vegetation and on its provisioning service for human well-being. Thus, the major aim of this thesis is to investigate the impacts of land use intensification on vegetation composition, diversity and function and its consequences for provisioning ecosystem services (NTFPs) and human well-being in a West African savanna.
The research for this study was conducted in the North Sudanian vegetation zone of south-eastern Burkina Faso, where population growth exceeds the nationwide trend. Generally, Burkina Faso belongs to the worldwide poorest countries, where nearly one quarter of the population suffers from malnutrition (FAO 2014). The integration of NTFPs and particularly wild food species into rural household economies is, thus, an important measure in the national combat against poverty and food insecurity (FAO 2014). Against this background, I focus on vegetation changes, the economic importance of NTFPs as well as the decrease and substitution of wild food species in this study.
Vegetation resurveys of different vegetation types since the early 1990s showed that land use change led to more pronounced changes in the herbaceous than in the woody vegetation layer. Most woody vegetation types stayed stable in species composition and richness, even though some highly useful tree species (Vitellaria paradoxa, Parkia biglobosa) declined in some woody vegetation types. In contrast, in most herbaceous vegetation types species richness increased and species composition considerably changed. This change might be explained by a general ruderalisation process through a pronounced increase of wide-ranging herbaceous species. However, in spite of a general species increase in the herbaceous layer, a decrease of preferred herbaceous fodder species was found. Thus, the decline of useful species in both layers is alarming. Herbaceous vegetation types also showed more pronounced changes in plant functional trait characteristics in comparison to woody vegetation types. However, an increase of smaller plant species and species with a high diaspore terminal velocity (VTerm) was found in both vegetation layers. Since these two trait responses are generally related to grazing and browsing, the strong increase of livestock herds is likely to be responsible for the detected vegetation changes.
In addition to the vegetation study, interviews showed that all useful food species were widely considered to decline. The two economically most important tree species, the shea tree (Vitellaria paradoxa) and the locust bean tree (Parkia biglobosa) that contribute with 70% to wild food income, were considered among the most declining species of all cited wild food species. On this matter, local perceptions of species decline and results from field observations are in accordance. However, a wide range of cited substitutes indicated a great knowledge on alternative plant species in the area. Most wild food species are, however, substituted by other highly valued wild food species. Although our results suggest that rural communities are able to cope with the decrease or absence of wild food species, growing decline of one species would concurrently increase the pressure on other native food species. Therefore, the need to counteract the decrease of highly useful wild food species should be of high priority in management measures. In general, I showed that NTFPs are an essential component in rural households, since it contributed with 45 % to total household income. Significant differences in NTFP dependency between the two investigated villages and across the three main ethnic groups were detected, reflecting different traditional uses and harvesting practices. In general, it was shown that poorer households depend more on NTFP income than wealthier households. Against the background of this study, management strategies for agroforestry systems and poverty alleviation should consider local differences, and ethnicity-dependent NTFP-use patterns.
Overall, the combination of field studies on temporal and functional vegetation change with socio-economic and ethno-botanic interviews increases the knowledge on qualitative and quantitative vegetation changes and on the consequences for rural populations. This thesis gives a thorough insight into decreasing trends of economically valued plant species and thus gives evidence on the consequences of vegetation changes for ecosystem services of West African savanna ecosystems. Further, different NTFP-dependencies and use preferences according to socio-economic and cultural variables, such as ethnicity, present a valuable basis for specific decision-making and should be considered in management plans.
Urn models are simple examples for random growth processes that involve various competing types. In the study of these schemes, one is generally interested in the impact of the specific form of interaction on the allocation of elements to the types. Depending on their reciprocal action, effects of cancellation and self-reinforcement become apparent in the long run of the system. For some urn models, the influencing is of a smoothing nature and the asymptotic allocation to the types is close to being a result of independent and identically distributed growth events. On the contrary, for others, almost sure random tendencies or logarithmically periodic terms emerge in the second growth order. The present thesis is devoted to the derivation of central limit theorems in the latter case. For urns of this kind, we use a "non-classical" normalisation to derive asymptotic joint normality of the types. This normalisation takes random tendencies and phases into account and consequently involves random centering and, also, possibly random scaling.