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Bromus racemosus L. is a rather rare grass species of moist meadows. It has strongly decreased in the course of the 20th century due to intensification of agricultural grassland management, and is therefore included in Red Lists of several European countries. Its winter annual life-cycle is remarkable for a species of permanent grasslands.
The aim of this study is to determine the habitat preference and optimal management of B. racemosus in the Netherlands and surrounding countries. Vegetation, soil and hydrological data from 28 sites in the Netherlands have been compared with B. racemosus cover, and with vegetation data from surrounding countries. The results indicate that B. racemosus is characteristic of Molinio-Arrhenatheretea meadows with good mineralisation and aftermath grazing. The optimum lies in grasslands of the alliance Alopecurion pratensis (Deschampsion cespitosae), but the species ranges from wetter Calthion palustris meadows to drier Arrhenatherion elatioris and Cynosurion cristati grasslands. It prefers intermediate nutrient levels and hydrological conditions (mesic sites), but within this range the highest cover is found in relatively nutrient rich and dry sites. Because of the absence of a seedbank and a low dispersal capability, B. racemosus is vulnerable to changes in grassland management. A management of mowing after 15 June and aftermath grazing is most suitable, since it enables fruit ripening and the maintenance of an open sward, needed for germination and development. The risk of extinction is likely to be higher in flat polders than in floodplain sites with natural relief, where the species may shift between belts in different years.
Vegetation patterns of floodplain forests are highly variable across different habitats in European regions. Their plant communities have been well described from the phytosociological point of view, but plant species richness and composition patterns and their underlying environmental factors are still insufficiently known. Sixty-one vegetation plots of black alder-dominated floodplain forests were sampled in central Slovakia in order to find main environmental predictors affecting floristic diversity of their vegetation. For each vegetation plot with a constant size (400m2), vascular plant species and a set of topographic, climatic, soil physical and chemical characteristics were recorded. A generalized linear model was applied to explain relevance of environmental factors on changes of species richness, whereas the relationship between species composition and explanatory variables was tested using ordination methods. Main gradients of species compositional variation were soil moisture, light, elevation and soil chemistry-related variables. Vascular species richness of plots varied between 19 and 59 (mean 38). Herb-layer species richness was positively related to the soil pH, stream power index and negatively to the concentration of soil iron. These linear trends were accompanied by a hump-shaped response to sand content and a U-shaped response to elevation.
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.
Ziel dieser Dissertation war es, die biologische Rolle der Autophagie für die Entwicklung, Alterung und mitochondriale Qualitätskontrolle in dem Ascomyceten Podospora anserina zu untersuchen. Folgende Ergebnisse wurden dabei erzielt:
1. Der Verlust einer funktionalen Autophagie-Maschinerie ist in P. anserina mit einem Defekt der Sporen-Entwicklung bzw. -Keimung charakterisiert.
2. Es konnten drei Methoden zur Untersuchung der Autophagie in P. anserina etabliert werden: 1) Die Verwendung eines Gfp::PaAtg8-Stamms ermöglicht die Fluoreszenzmikroskopische Bestimmung der Autophagosomen-Anzahl; 2) Die phänotypische Charakterisierung des PaAtg1-Deletionsstamms unter verschiedenen Stressbedingungen (z. B. Stickstoffmangel, Rapamycin) liefert Hinweise auf eine mögliche Autophagie-abhängige Stressadaption; 3) Die Verwendung des „GFPcleavage assays“ ermöglicht einen quantitativen Nachweis genereller und selektiver Autophagie (hier: Mitophagie).
3. In zwei voneinander unabhängigen Experimenten wurde ein altersabhängiger Anstieg der Autophagie für P. anserina demonstriert: Das Autophagie-Niveau nimmt in gealterten P. anserina-Kulturen zu. Gleichzeitig resultiert der Verlust der Autophagie in ∆PaAtg1 in eine reduzierte Lebensspanne. Unter Stressbedingungen (hier: Stickstoffmangel) wird dieser positive Einfluss der Autophagie auf die Lebensspanne im Wildtyp sogar noch verstärkt.
4. Der unerwartet „gesunde“ Phänotyp der PaSod3-Deletionsmutante ist abhängig von einer funktionalen Autophagie-Maschinerie. Der Mitophagie wurde eine besondere Rolle als Kompensationsmechanismus für den Verlust von PaSOD3 zugeteilt, da das Mitophagie-Niveau in dieser Mutante erhöht ist. Am Beispiel dieser Mutante, für die ein erhöhter Superoxid-Ausstoß nachgewiesen wurde, konnte eine Dosis-abhängige Wirkung von ROS in P. anserina identifiziert werden. Eine geringe zelluläre ROSMenge verursacht eine mitohormetische Reaktion, die eine Induktion der Mitophagie zur Folge hat und sich positiv auf den Organismus auswirkt. Übersteigt die zelluläre ROS-Dosis einen kritischen Punkt, kommt es zur Induktion des autophagischen Zelltods und damit zum vorzeitigen Tod des Individuums.
5. Der Verlust der PaCLPXP-Protease führt zu Beeinträchtigungen in der Funktion und Zusammensetzung der mitochondrialen Atmungskette. Dieses Defizit im Energiemetabolismus wird über eine Induktion der AOX, vor allem aber über eine ZUSAMMENFASSUNG 127 gesteigerte Autophagie kompensiert. Die deutlich verlängerte Lebensspanne der verschiedenen PaClpXP-Deletionsmutanten (∆PaClpX, ∆PaClpP und ∆PaClpXP) ist abhängig von einer funktionalen Autophagie-Maschinerie. Interessanterweise konnte keine kompensatorische Funktion der Autophagie oder Mitophagie für den Verlust der mitochondrialen i-AAA-Protease PaIAP in P. anserina nachgewiesen werden.
Autophagie/Mitophagie stellt einen übergeordneten Qualitätskontrollmechanismus in P. anserina dar, der den Organismus sehr effektiv vor zellulären Schäden und Dysfunktionen bewahrt und einen positiven Einfluss auf die Alterung, Entwicklung und Energieversorgung einnimmt.
Background: Isolated transient vertigo can be the only symptom of posterior circulation ischemia. Thus, it is important to differentiate isolated vertigo of a cerebrovascular origin from that of more benign origins, as patients with cerebral ischemia have a much higher risk for future stroke than do those with "peripheral" vertigo. The current study aims to identify risk factors for cerebrovascular origin of isolated transient vertigo, and for future cerebrovascular events.
Methods: From the files of 339 outpatients with isolated transient vertigo we extracted history, clinical and technical findings, diagnosis, and follow-up information on subsequent stroke or transient ischemic attack (TIA). Risk factors were analyzed using multivariate regression models (logistic or Cox) and reconfirmed in univariate analyses.
Results: On first presentation, 48 (14.2%) patients received the diagnosis "probable or definite cerebrovascular vertigo". During follow-up, 41 patients suffered stroke or TIA (event rate 7.9 per 100 person years, 95% confidence interval (CI) 5.5–10.4), 26 in the posterior circulation (event rate 4.8 per 100 person years, 95% CI 3.0–6.7). The diagnosis was not associated with follow-up cerebrovascular events. In multivariate models testing multiple potential determinants, only the presentation mode was consistently associated with the diagnosis and stroke risk: patients who presented because of vertigo (rather than reporting vertigo when they presented for other reasons) had a significantly higher risk for future stroke or TIA (p = 0.028, event rate 13.4 vs. 5.4 per 100 person years) and for future posterior circulation stroke or TIA (p = 0.044, event rate 7.8 vs. 3.5 per 100 person years).
Conclusions: We here report for the first time follow-up stroke rates in patients with transient isolated vertigo. In such patients, the identification of those with cerebrovascular origin remains difficult, and presentation mode was found to be the only consistent risk factor. Confirmation in an independent prospective sample is needed.
Functional imaging studies using BOLD contrasts have consistently reported activation of the supplementary motor area (SMA) both during motor and internal timing tasks. Opposing findings, however, have been shown for the modulation of beta oscillations in the SMA. While movement suppresses beta oscillations in the SMA, motor and non-motor tasks that rely on internal timing increase the amplitude of beta oscillations in the SMA. These independent observations suggest that the relationship between beta oscillations and BOLD activation is more complex than previously thought. Here we set out to investigate this rapport by examining beta oscillations in the SMA during movement with varying degrees of internal timing demands. In a simultaneous EEG-fMRI experiment, 20 healthy right-handed subjects performed an auditory-paced finger-tapping task. Internal timing was operationalized by including conditions with taps on every fourth auditory beat, which necessitates generation of a slow internal rhythm, while tapping to every auditory beat reflected simple auditory-motor synchronization. In the SMA, BOLD activity increased and power in both the low and the high beta band decreased expectedly during each condition compared to baseline. Internal timing was associated with a reduced desynchronization of low beta oscillations compared to conditions without internal timing demands. In parallel with this relative beta power increase, internal timing activated the SMA more strongly in terms of BOLD. This documents a task-dependent non-linear relationship between BOLD and beta-oscillations in the SMA. We discuss different roles of beta synchronization and desynchronization in active processing within the same cortical region.
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. ...
Reactive oxygen species are produced transiently in response to cell stimuli, and function as second messengers that oxidize target proteins. Protein-tyrosine phosphatases are important reactive oxygen species targets, whose oxidation results in rapid, reversible, catalytic inactivation. Despite increasing evidence for the importance of protein-tyrosine phosphatase oxidation in signal transduction, the cell biological details of reactive oxygen species-catalyzed protein-tyrosine phosphatase inactivation have remained largely unclear, due to our inability to visualize protein-tyrosine phosphatase oxidation in cells. By combining proximity ligation assay with chemical labeling of cysteine residues in the sulfenic acid state, we visualize oxidized Src homology 2 domain-containing protein-tyrosine phosphatase 2 (SHP2). We find that platelet-derived growth factor evokes transient oxidation on or close to RAB5+/ early endosome antigen 1− endosomes. SHP2 oxidation requires NADPH oxidases (NOXs), and oxidized SHP2 co-localizes with platelet-derived growth factor receptor and NOX1/4. Our data demonstrate spatially and temporally limited protein oxidation within cells, and suggest that platelet-derived growth factor-dependent “redoxosomes,” contribute to proper signal transduction.
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.