Einfluss immunevasiver Strategien des humanen Cytomegalovirus auf die MHC-Klasse-I-Präsentation der viralen Antigene pp65 und IE1

Das Humane Cytomegalovirus (HCMV) stellt eine große Bedrohung für Patienten mit geschwächtem oder unausgereiftem Immunsystem dar. Bei immunkompetenten Personen hingegen werden schwere Erkrankungen insbesondere durch die Wirkung antiviraler zytotoxischer CD8+-T-Lymphozyten (CTL) weitgehend verhindert. Aus Zellkultur-Systemen war bekannt, dass virale Glykoproteine, welche in der US2-US11-Region des HCMV-Genoms kodiert werden, inhibitorisch in den MHC-Klasse-I-Präsentationsweg eingreifen und somit die entsprechende Präsentation durch infizierte Zellen behindern. Über die Bedeutung dieser US2-US11-vermittelten Immunevasion für die Präsentation viraler Antigene im Kontext der Virusinfektion war jedoch nichts bekannt. Im Rahmen der vorliegenden Arbeit sollte daher der Einfluss der Immunevasion auf die MHC-Klasse-I-Präsentation der beiden wichtigsten CTL-Zielstrukturen von HCMV, dem Tegumentprotein pp65 und dem regulatorischen immediate early Protein IE1, untersucht werden. In Ergänzung dazu sollte das immunevasive Potential eines durch HCMV kodierten Homologs des immunmodulatorischen Zytokins Interleukin-10 (cmvIL-10) analysiert werden. Hierzu wurden über Peptidimmunisierung HLA-A2-transgener Mäuse CTL-Klone hergestellt, welche ausgesuchte Peptide aus pp65 und IE1 in Assoziation mit HLA-A2 mit hoher Spezifität und Sensitivität erkannten. Auf diese Weise konnte eine direkte Beeinflussung der MHC-Klasse-I-Präsentation durch cmvIL-10 falsifiziert und somit der Hypothese, dass das von infizierten Zellen freigesetzte Zytokin die MHC-Klasse-I-Präsentation nicht infizierter Nachbarzellen beeinflussen könnte, widersprochen werden. Mit Hilfe einer US2-US11-Deletionsmutante des Virus konnte zum ersten Mal gezeigt werden, dass die Präsentation von sowohl pp65 als auch IE1 durch die Immunevasion beeinträchtigt wird. Dabei war die Präsentation des IE1-Peptids zu jedem untersuchten Zeitpunkt nach Infektion vollständig unterdrückt. Die Präsentation des pp65-Peptids hingegen war noch bis zu 72 Stunden nach Infektion detektierbar. Diese anhaltende Präsentation wurde dabei durch MHC-Klasse-I-Komplexe hervorgerufen, die trotz der Expression der US2-US11-Region an die Zelloberfläche transportiert wurden. Anhand des pp65 konnte somit erstmals gezeigt werden, dass die Immunevasion von HCMV Bildung und Transport bestimmter MHC-Klasse-I-Peptid-Komplexe zwar beeinträchtigen, jedoch nicht vollständig blockieren kann. Weitere Untersuchungen ergaben, dass die Präsentation von IE1-Peptiden durch das Vorhandensein des pp65-Proteins nicht beeinflusst wurde. Damit konnten aus der Literatur bekannte Daten anderer widerlegt werden. Mit Hilfe einer weiteren Virusmutante konnte schließlich gezeigt werden, das die Expression eines der Immunevasine, des gpUS11, hinreichend ist, die IE1-Präsentation vollständig zu unterdrücken, jedoch keinerlei messbaren Einfluss auf die Präsentation von pp65 ausübt. Die vorliegende Arbeit hat wichtige Erkenntnisse erbracht, die die Grundlage für weiterführende Untersuchungen zur Aufklärung der Bedeutung der einzelnen Immunevasionsgene für die Präsentation viraler Antigene im Rahmen der Virusinfektion darstellen.

Isolierung und Charakterisierung der ER-residenten Aminopeptidase ERMP1 und Untersuchung ihrer Funktion in der Prozessierung MHC I restringierter CTL Epitope

Die effiziente Generierung von Peptid-Epitopen aus zelleigenen oder viralen Proteinen für die Präsentation auf „Major Histocompatibility Complex I“ (MHC I) Molekülen ist essentiell für die Aktivierung des adaptiven Immunsystems und die Effektorfunktion der CD8+ zytotoxischen T-Zellen (CTLs). CTLs erkennen diese Peptide in Kontext mit MHC I Molekülen über ihren spezifischen T-Zellrezeptor (TCR). Die Generierung dieser Epitope ist das Resultat eines komplexen proteolytischen Prozesses, der im Zytosol und im endoplasmatischen Retikulum (ER) stattfindet. Im Zytosol generiert das Proteasom N-terminal verlängerte Epitop-Vorläufer. Diese werden durch weitere zytosolische Proteasen abgebaut, es sei denn, sie werden durch den „transporter associated with antigen processing“ (TAP) in das ER transportiert. Dort werden sie durch Aminopeptidasen getrimmt, um den Bindungsvoraussetzungen der MHC I Moleküle zu genügen. Im murinen System ist die „ER aminopeptidase associated with antigen processing“ (ERAAP) die bislang einzige beschriebene Aminopeptidase, die dieses N-terminale Trimming von CTL Epitopen vermitteln kann. Das Profil der proteolytischen Aktivität in angereichertem murinen ER kann jedoch nicht allein durch die Aktivität von ERAAP erklärt werden, was auf die Anwesenheit weiterer Aminopeptidasen mit einer potentiellen Funktion in der Antigenprozessierung hinweist. In dieser Arbeit konnte die immunologisch bislang noch nicht beschriebene Aminopeptidase ERMP1 (endoplasmic reticulum metallopeptidase 1) im murinen ER identifiziert werden. Nach Aufreinigung muriner Mikrosomen und anschließender Anionenaustausch-Chromatographie wurden die gesammelten Fraktionen mit fluorogenen Substraten auf Aminopeptidase-Aktivität getestet. Durch massenspektrometrische Analyse konnten in den beobachteten Peaks die schon beschriebenen Aminopeptidasen ERAAP, die „insulin regulated aminopeptidase“ IRAP und die immunologisch bislang nicht beschriebene Aminopeptidase ERMP1 identifiziert werden. Durch Fluoreszenzmikroskopie konnte die intrazelluläre Lokalisation von ERMP1 im ER durch Kolokalisation mit TAP verifiziert werden. Wie viele Komponenten des MHC I Prozessierungsweges wird auch die Expression von ERMP1 durch IFN-γ stimuliert. Dies macht ERMP1 zu einer potentiellen zweiten trimmenden Aminopeptidase im murinen ER. Überexpression von ERMP1 hat einen allelspezifischen Einfluss auf die globale MHC I Präsentation auf der Zelloberfläche und durch Überexpression und shRNA vermitteltes gene silencing konnte außerdem ein epitopspezifischer Effekt nachgewiesen werden. Da N-terminales Trimming durch ERAAP mit der Evasion von Tumoren und veränderter Immundominanz assoziiert wird, ist die detaillierte Charakterisierung der Aminopeptidase ERMP1 ein wichtiger Schritt zum Verständnis der MHC I Antigen-Prozessierung und der Generierung von CTL Epitopen im ER.

Formation of DNA complexes in aqueous and organic solvents

From a physical-chemical point of view, it is challenging to form complexes with polyelectrolytes, consisting of only molecule of the largest component, i.e. the component with the highest number of charges. In this study, complexes are formed with DNA because of its potential applications as an artificial vector for gene delivery. The aim of this work is to prepare complexes in aqueous solutions as well as in organic solvents containing only one DNA molecule. For this purpose, the topology, equilibrium and conformation of complexes between a supercoiled DNA pUC19 (2686 base pairs) and spermine containing hydrophilic and/or hydrophobic moieties or a polylysine with a hydrophilic block are determined by means of dynamic (DLS) and static light scattering (SLS), atomic force microscopy (AFM), and circular dichroism (CD) spectroscopy. It is demonstrated that all of these complexes consisted of only one molecule of the polyanion. Only the polylysine-b-polyethylene glycol copolymer satisfied the conditions: 1) 100% neutralization of DNA charges and with a small excess of the cation (lower than 30%) and 2) form stable complexes at every charge ratio. rnDNA complex formation is also investigated in organic solvents. Precipitation is induced by neutralizing the charge of the supercoiled DNA pUC19 with the surfactants dodecyltrimethylammonium bromide (DTAB) and tetradecyltrimethylammonium bromide (TTAB). After isolation and drying of the solids, the complexes are dissolved in organic solvents. DNA-TTA complexes are only soluble in methanol and DNA-DTA in DMF. The complexes again consisted of only one DNA molecule. The final topology of the complexes is different in methanol than in DMF. In the former case, DNA seems to be compacted whereas in the latter case, the DNA-DTA complexes seem to have an expanded conformation. Upon complex formation with polycations in organic solvents (with polyvilylpyridine brush (b-PVP) in methanol and with a protected polylysine in DMF), DNA aggregates and precipitates. rnDNA is linearized with an enzyme (SmaI) to investigate the influence of the initial topology of the polyanion on the final conformation of the complexes in organic solvents. Two main differences are evidenced: 1. Complexes in organic solvents formed with linear DNA have in general a more expanded conformation and a higher tendency to aggregate. 2. If a polycation, i.e. the b-PVP, is added to the linear DNA-TTA complexes in methanol, complexes with the polycation are formed at a higher charge ratio. In DMF, the addition of the same b-PVP and of b-PLL did not lead to the formation of complexes.rn

Complexes of polyelectrolytes with defined charge distance and different dendrimer counterions

Complexes of polyelectrolytes with defined charge distance and different dendrimer counterions Magdalena Chelmecka Max Planck Institute for Polymer Research; Ackermannweg 10; D-55128 Mainz ; Tel.: (+49) 06131- 379 – 226 A study of complexes in solution is of interest to investigate whether the formation of well-defined assemblies like in classical surfactant systems is possible. Aim of this thesis is to investigate the electrostatic self-assembly of linear polycations of varying charge distance with “large” counterions of varying architecture. We especially investigate the morphology of objects formed, but also their stability under salt free condition and after low molecular mass salt addition. As polycations, Poly(dialkylimino)-alkylene salts (Ionenes) I65MeBr and I25MeBr were chosen. Ionenes are synthesized via Menschutkin reaction and characterized by standard methods. Counterions are Polyamidoamine (PAMAM) dendrimers of generations G2.5, G5.5, G7.5 with -COONa surface groups and shape-persistent, Polyphenylene dendrimers of generation G1 with surface -COOH groups. A complex interplay of interactions is expected to direct the self assembly via electrostatic interaction, geometric factors, hydrophobic interaction or hydrogen bonds. Methods used for the investigation of complexes are: UV-spectroscopy, pH-metric techniques, dynamic and static light scattering, small angle neutron scattering,  potential measurements and potentiometric titration. Under certain conditions, (i.e. charge ratio of compounds, charge density of ionene and dendrimer also concentration of sample) polyelectrolyte systems composed of ionenes and dendrimers build complexes in solution. System compounds are typical polyelectrolytes, but structures which they build behave not usual for typical polyelectrolytes. In a one diffusion mode regime aggregates of about 100 nm hydrodynamic radius have been found. Such aggregates are core-shell or anisotropic core shell structures in the case of ionenes/PAMAM dendrimers complexes. These complexes are stable even at high ionic strength. In case of ionenes with poly(phenylene) dendrimers, hard sphere-like objects or spherical objects with hairy-like surface have been found in a one diffusion mode regime. Their stability at high ionic strength is lower. For the ionenes/poly(phenylene) dendrimers systems one transition point has been found from one to two diffusion processes, towards increasing ionene concentration, i.e. for the samples with fixed dendrimer concentration towards increasing ionic strength. For the diffusion profile of ionene/PAMAM dendrimers in most cases two transition regimes are observed. One at very low ionene concentration, the second one at high ionene concentrations, which again means for the samples with fixed dendrimer concentration, also at higher ionic strength. Both two mode regimes are separated by the one mode regime. As was confirmed experimentally, the one diffusion mode regime is caused by the motion of well defined assemblies. The two diffusion mode regimes are caused by the movement of different sized species in solution, large aggregates and middle-size aggregates (oligoaggregates). The location and also the number of transition points in the diffusion profiles is dependent on the ionene to dendrimer charge ratio, charge density of the compounds and concentration. No influence of the molecular mass of the ionene has been found. The aggregates are found to be charged on the surface, however this surface charge does not significantly influence the diffusion properties of the system.

Geochemistry, petrogenesis and tectonic setting of ophiolites and mafic-ultramafic complexes in the Northeastern Aegean Region

In this study two ophiolites and a mafic-ultramafic complexes of the northeastern Aegean Sea, Greece, have been investigated to re-evaluate their petrogenetic evolution and tectonic setting. These complexes are: the mafic-ultramafic complex of Lesvos Island and the ophiolites of Samothraki Island and the Evros area. In order to examine these complexes in detail whole-rock major- and trace-elements as well as Sr and Nd isotopes, and minerals were analysed and U-Pb SHRIMP ages on zircons were determined. The mafic-ultramafic complex of Lesvos Island consists of mantle peridotite thrusted over a tectonic mélange containing metasediments, metabasalts and a few metagabbros. This succession had previously been interpreted as an ophiolite of Late Jurassic age. The new field and geochemical data allow a reinterpretation of this complex as representing an incipient continental rift setting that led to the subsequent formation of the Meliata-Maliac-Vardar branches of Neotethys in Upper Permian times (253 ± 6 Ma) and the term “Lesvos ophiolite” should be abandoned. With proceeding subduction and closure of the Maliac Ocean in Late Jurassic times (155 Ma) the Lesvos mafic-ultramafic complex was obducted. Zircon ages of 777, 539 and 338 Ma from a gabbro strongly suggest inheritance from the intruded basement and correspond to ages of distinct terranes recently recognized in the Hellenides (e.g. Florina terrane). Geochemical similar complexes which contain rift associations with Permo-Triassic ages can be found elsewhere in Greece and Turkey, namely the Teke Dere Thrust Sheet below the Lycian Nappes (SW Turkey), the Pindos subophiolitic mélange (W Greece), the Volcanosedimentary Complex on Central Evia Island (Greece) and the Karakaya Complex (NW Turkey). This infers that the rift-related rocks from Lesvos belong to an important Permo-Triassic rifting episode in the eastern Mediterranean. The ‘in-situ’ ophiolite of Samothraki Island comprises gabbros, sparse dykes and basalt flows as well as pillows cut by late dolerite dykes and had conventionally been interpreted as having formed in an ensialic back-arc basin. The results of this study revealed that none of the basalts and dolerites resemble mid-ocean ridge or back-arc basin basalts thus suggesting that the Samothraki ophiolite cannot represent mature back-arc basin crust. The age of the complex is regarded to be 160 ± 5 Ma (i.e. Oxfordian; early Upper Jurassic), which precludes any correlation with the Lesvos mafic-ultramafic complex further south (253 ± 6 Ma; Upper Permian). Restoration of the block configuration in NE Greece, before extensional collapse of the Hellenic hinterland and exhumation of the Rhodope Metamorphic Core Complex (mid-Eocene to mid-Miocene), results in a continuous ophiolite belt from Guevgueli in the NW to Samothraki in the SE, thus assigning the latter to the Innermost Hellenic Ophiolite Belt. In view of the data of this study, the Samothraki ophiolite represents a rift propagation of the Sithonia ophiolite spreading ridge into the Chortiatis calc-alkaline arc. The ophiolite of the Evros area consists of a plutonic sequence comprising cumulate and non-cumulate gabbros with plagiogranite veins, and an extrusive sequence of basalt dykes, massive and pillow lavas as well as pyroclastic rocks. Furthermore, in the Rhodope Massif tectonic lenses of harzburgites and dunites can be found. All rocks are spatially separated. The analytical results of this study revealed an intra-oceanic island arc setting for the Evros ophiolitic rocks. During late Middle Jurassic times (169 ± 2 Ma) an intra-oceanic arc has developed above a northwards directed intra-oceanic subduction zone of the Vardar Ocean in front of the Rhodope Massif. The boninitic, island arc tholeiitic and calc-alkaline rocks reflect the evolution of the Evros island arc. The obduction of the ophiolitic rocks onto the Rhodope basement margin took place during closure of the Vardar ocean basins. The harzburgites and dunites of the Rhodope Massif are strongly depleted and resemble harzburgites from recent oceanic island arcs. After melt extraction they underwent enrichment processes by percolating melts and fluids from the subducted slab. The relationship of the peridotites and the Evros ophiolite is still ambiguous, but the stratigraphic positions of the peridotites and the ophiolitic rocks indicate separated origin. The harzburgites and dunites most probably represent remnants of the mantle wedge of the island arc of the Rhodope terrane formed above subducted slab of the Nestos Ocean in late Middle Jurassic times. During collision of the Thracia terrane with the Rhodope terrane thrusting of the Rhodope terrane onto the Thracia terrane took place, whereas the harzburgites and dunites were pushed between the two terranes now cropping out on top of the Thracia terrane of the Rhodope Massif.

Heteroatom containing polycyclic aromatic hydrocarbons with positive charge - synthesis and characterization

The synthesis and characterization of various heteroatom containing PAHs with positive charge were investigated in this work: 1. A series of 2-phenyl-benzo[8,9]quinolizino[4,5,6,7-fed]phenanthridinylium (PQP) salts with different alkyl chains and anions were synthesized. The synthesis of the extended derivates of PQP salts with two fused benzene rings, 2-phenyl-naphthacene[1,2]quinolizino[3,4,5,6-def]benzo[i]phenanthridinium (DBPQP) tetrafluoroborate was also developed. The self-assembly behavior of these amphiphilic PAHs was investigated in methanolic solution as well as in the bulk. Various aggregates with different morphologies such as fibers, tubes and vesicals were obtained from their solution. All of these morphology changes could be ascribed to the changes in intermolecular interactions which resulting from the difference in the molecular structures such as aromatic cores, alkyl chains and counterions. 2. The synthetic strategy of oxygen containing positively charged PAHs, benzo[5,6]naphthaceno[1,12,11,10-jklmna]xanthylium (BNAX) salts and its dibenzo derivates, DBNAX salts were developed. With a similar method, sulfur containing benzo[5,6]naphthaceno[1,12,11,10-jklmna]thioxanthylium (BNATX) salts were also synthesized. Various BNAX salts with different alkyl chains could be obtained and their supramolecular behavior were investigated. A discotic liquid crystalline behavior was observed for di- (3-25) and tridodecyl (3-27) substituted BNAX salts and both compounds exhibited large unit cell in their 2D-WAXS patterns which could be attributed to the formation of dimer structures. By drop casting their methanolic solution on silicon wafers, similar nanoscaled fibers from monododecyl substituted BNAX bromide 3-24 and DBNAX bromide 3-35 could be observed. 3. A novel synthetic method toward nitrogen containing 14-phenyl-dibenzo[jk,mn]naphtho[2,1,8-fgh]thebenidinium (DBNT) salts was also developed. In this method, the undehydrogenated precursor of DBNT, dibenzoacridinium salt could be produced directly from the reaction between dibenzoxanthenylium derivates and amine/aniline in reasonable yields. Various DBNT salts with different alkyl and alkylphenyl chains on their nitrogen atom were synthesized in this two-step method. The self-assembly behavior of two alkylated DBNT salts, 4-15a and 4-18b was also studied in this work. Compound 4-15a formed nanoscaled fibers and helical aggregates were obtained from 4-18b in their methanolic solutions. 4. Various ionic complexes were derived by complexing PQP and DBPQP cations with different sulfate/sulfonate group containing anionic surfactants. The ionic complexes resulting from the ionic self-assembly (ISA) method exhibited self-assembly behavior which was controllable by the species and shape of cations and anions. Various aggregates such as nanofibers and spherical aggregates could be produced from their methanolic solution in a defined manner conveniently.