Funktionsanalysen der Domänen des Vacuolin B und die Rolle des filamentösen Actins am Vacuolin B-positiven Kompartiment im endocytotischen Transit in Dictyostelium discoideum

Ähnlich wie in Säugerzellen ist das neutrale Postlysosom in Dictyostelium discoideum von einem Coat aus filamentösem Actin umgeben. In dieser Arbeit wurde der Frage nach der Funktion dieses Actin-Cytoskeletts am späten Endosom nachgegangen. Hierzu wurde zunächst eine Analyse der Domänen des Vacuolin B durchgeführt, das als bisher spätester bekannter Marker im Endocytoseweg in Dictyostelium discoideum das neutrale, postlysosomale Kompartiment dekoriert. In einer Yeast Two Hybrid-Analyse wurden die Bereiche des Vacuolin B identifiziert, die für eine Selbst-Interaktion des Proteins notwendig und ausreichend sind. Es handelt sich dabei um die coiled-coil-Domäne und einen daran anschließenden, 18 Aminosäuren langen, alpha-helicalen Abschnitt. Diesem helicalen Bereich scheint die Funktion einer modifizierenden, die coiled-coil-Ausbildung vermittelnden oder initiierenden Faltungseinheit zuzukommen. Sie weist jedoch nicht die typischen Merkmale einer trigger-Helix auf. Lokalisationsuntersuchungen mit GFP-Deletionskonstrukten zeigten, dass es einen Zusammenhang zwischen Interaktionsfähigkeit und Bindung des Vacuolin an die Oberfläche später Endosomen gibt: Eine korrekte Lokalisation und Membranassoziation waren nur dann zu beobachten, wenn in der Yeast Two Hybrid-Analyse eine Interaktion nachgewiesen werden konnte. Es wurden die für die Lokalisation und Assoziation mit der vacuolären Membran notwendigen Sequenzbereiche identifiziert; diese waren jedoch nicht hinreichend. Vermutlich sind hierfür auch Sequenzen des N-Terminus notwendig. Die erhobenen Daten legen weiterhin eine Bedeutung der hydrophoben Domäne des Vacuolin B für die korrekte Faltung des Proteins nahe. Im Anschluss an die Domänenanalyse wurde Vacuolin dazu benutzt, durch Herstellung von Hybridproteinen Actin-interagierende Proteine gezielt an das späte Endosom zu transportieren. Es wurde deren Einfluss auf den lokalen Actin Coat und den endocytotischen Transit untersucht. Zwei Actin-bindende Proteine mit depolymerisierender Wirkung konnten im Rahmen dieser Arbeit getestet werden, nämlich Severin und Cofilin. Die Schwächung des lokalen Actin Coats durch das Vorhandensein von Severin an der späten Vacuole war nicht eindeutig festzustellen. Severin am Postlysosom führte nicht zu einer Veränderung der Transitkinetik von Flüssigphasenmarker. Allerdings konnte ein Defekt in der Phagocytose festgestellt werden. Es könnte hierbei ein Zusammenhang zwischen der Mobilisierung von intrazellulärem Calcium während der Partikelaufnahme und der Calcium-abhängigen Regulation der Severin-Aktivität bestehen. Das Hybridprotein aus Vacuolin und Cofilin zeigte neben einer Assoziation mit der vacuolären Membran auch eine Lokalisation im Cytoplasma und Cortex der Zellen. Mit der Lokalisation im Cytoplasma und Cortex korrelierte eine Veränderung der endocytotischen Aktivität. Das Vacuolin-Cofilin-Fusionsprotein am Postlysosom rief einen Verlust des lokalen Actin Coats hervor. Dies führte zu einer traubenförmigen Assoziation der späten Endosomen; exocytotische Parameter blieben jedoch unbeeinflusst. Aufgrund der hier erhobenen Daten kann vermutet werden, dass der Actin Coat am Postlysosom dazu dient, eine Agglutination dieser Endosomen zu inhibieren. Dies könnte ein Schutzmechanismus zum Ausschluss von Docking- und Fusionsereignissen sein.

Funktionelle Analyse der LC-FACS in Dictyostelium discoideum

"Funktionelle Analyse der LC-FACS in Dictyostelium discoideum" Das Dictyostelium discoideum Gen fcsA kodiert für ein 75 kDa großes Protein. Es kann durch Homologieanyalysen der Amino-säuresequenz zu den "long-chain fatty acyl-CoA"-Synthetasen ge-rechnet werden, die lang-kettige Fettsäuren durch die kovalente Bindung von Coenzym A akti-vie-ren und damit für diverse Reak-tionen in Stoffwechsel und Molekül-Synthese der Zelle verfügbar machen. Die hier untersuchte D. discoideum LC-FACS lokalisiert als peripher assoziiertes Protein an der cytosolischen Seite der Membran von Endo-somen und kleiner Vesikel. Bereits kurz nach der Bildung in der frühen sauren Phase kann die Lokalisation der LC-FACS auf Endosomen ge-zeigt werden. Sie dissoziiert im Laufe ihrer Neutra-li-sierung und kann auf späten Endosomen, die vor ihrer Exocytose stehen nicht mehr nach-gewiesen werden. Ein Teil der kleinen die in der gesamte Zelle verteilten kleinen Vesikel zeigt eine Kolokalisation mit lysosomalen Enzymen. Trotz des intrazellulären Verteilungs-mus-ters, das eine Beteiligung dieses Pro-teins an der Endocytose nahe-legt, konnte kein signifikanter Rückgang der Pino- und Phagocytose-Rate in LC-FACS Nullmutanten beobachtet werden. Der endo-cy-to-ti-sche Transit ist in diesen Zellen etwas verlängert, außerdem zeigen die Endosomen einen deutlich erhöhten pH-Wert, was zu einer weniger effektiven Prozessierung eines lysosomalen Enzyms führt (a-Mannosidase). Die Funktion der LC-FACS ist die Aufnahme von langkettigen Fettsäuren aus dem Lumen der Endosomen.

Salinity-induced changes in the microbial use of sugarcane filter cake added to soil

Five laboratory incubation experiments were carried out to assess the salinity-induced changes in the microbial use of sugarcane filter cake added to soil. The first laboratory experiment was carried out to prove the hypothesis that the lower content of fungal biomass in a saline soil reduces the decomposition of a complex organic substrate in comparison to a non-saline soil under acidic conditions. Three different rates (0.5, 1.0, and 2.0%) of sugarcane filter cake were added to both soils and incubated for 63 days at 30°C. In the saline control soil without amendment, cumulative CO2 production was 70% greater than in the corresponding non-saline control soil, but the formation of inorganic N did not differ between these two soils. However, nitrification was inhibited in the saline soil. The increase in cumulative CO2 production by adding filter cake was similar in both soils, corresponding to 29% of the filter cake C at all three addition rates. Also the increases in microbial biomass C and biomass N were linearly related to the amount of filter cake added, but this increase was slightly higher for both properties in the saline soil. In contrast to microbial biomass, the absolute increase in ergosterol content in the saline soil was on average only half that in the non-saline soil and it showed also strong temporal changes during the incubation: A strong initial increase after adding the filter cake was followed by a rapid decline. The addition of filter cake led to immobilisation of inorganic N in both soils. This immobilisation was not expected, because the total C-to-total N ratio of the filter cake was below 13 and the organic C-to-organic N ratio in the 0.5 M K2SO4 extract of this material was even lower at 9.2. The immobilisation was considerably higher in the saline soil than in the non-saline soil. The N immobilisation capacity of sugarcane filter cake should be considered when this material is applied to arable sites at high rations. The second incubation experiment was carried out to examine the N immobilizing effect of sugarcane filter cake (C/N ratio of 12.4) and to investigate whether mixing it with compost (C/N ratio of 10.5) has any synergistic effects on C and N mineralization after incorporation into the soil. Approximately 19% of the compost C added and 37% of the filter cake C were evolved as CO2, assuming that the amendments had no effects on the decomposition of soil organic C. However, only 28% of the added filter cake was lost according to the total C and d13C values. Filter cake and compost contained initially significant concentrations of inorganic N, which was nearly completely immobilized between day 7 and 14 of the incubation in most cases. After day 14, N re-mineralization occurred at an average rate of 0.73 µg N g-1 soil d-1 in most amendment treatments, paralleling the N mineralization rate of the non-amended control without significant difference. No significant net N mineralization from the amendment N occurred in any of the amendment treatments in comparison to the control. The addition of compost and filter cake resulted in a linear increase in microbial biomass C with increasing amounts of C added. This increase was not affected by differences in substrate quality, especially the three times larger content of K2SO4 extractable organic C in the sugarcane filter cake. In most amendment treatments, microbial biomass C and biomass N increased until the end of the incubation. No synergistic effects could be observed in the mixture treatments of compost and sugarcane filter cake. The third 42-day incubation experiment was conducted to answer the questions whether the decomposition of sugarcane filter cake also result in immobilization of nitrogen in a saline alkaline soil and whether the mixing of sugarcane filter cake with glucose (adjusted to a C/N ratio of 12.5 with (NH4)2SO4) change its decomposition. The relative percentage CO2 evolved increased from 35% of the added C in the pure 0.5% filter cake treatment to 41% in the 0.5% filter cake +0.25% glucose treatment to 48% in the 0.5% filter cake +0.5% glucose treatment. The three different amendment treatments led to immediate increases in microbial biomass C and biomass N within 6 h that persisted only in the pure filter cake treatment until the end of the incubation. The fungal cell-membrane component ergosterol showed initially an over-proportionate increase in relation to microbial biomass C that fully disappeared at the end of the incubation. The cellulase activity showed a 5-fold increase after filter cake addition, which was not further increased by the additional glucose amendment. The cellulase activity showed an exponential decline to values around 4% of the initial value in all treatments. The amount of inorganic N immobilized from day 0 to day 14 increased with increasing amount of C added in comparison to the control treatment. Since day 14, the immobilized N was re-mineralized at rates between 1.31 and 1.51 µg N g-1 soil d-1 in the amendment treatments and was thus more than doubled in comparison with the control treatment. This means that the re-mineralization rate is independent from the actual size of the microbial residues pool and also independent from the size of the soil microbial biomass. Other unknown soil properties seem to form a soil-specific gate for the release of inorganic N. The fourth incubation experiment was carried out with the objective of assessing the effects of salt additions containing different anions (Cl-, SO42-, HCO3-) on the microbial use of sugarcane filter cake and dhancha leaves amended to inoculated sterile quartz sand. In the subsequent fifth experiment, the objective was to assess the effects of inoculum and temperature on the decomposition of sugar cane filter cake. In the fourth experiment, sugarcane filter cake led to significantly lower respiration rates, lower contents of extractable C and N, and lower contents of microbial biomass C and N than dhancha leaves, but to a higher respiratory quotient RQ and to a higher content of the fungal biomarker ergosterol. The RQ was significantly increased after salt addition, when comparing the average of all salinity treatments with the control. Differences in anion composition had no clear effects on the RQ values. In experiment 2, the rise in temperature from 20 to 40°C increased the CO2 production rate by a factor of 1.6, the O2 consumption rate by a factor of 1.9 and the ergosterol content by 60%. In contrast, the contents of microbial biomass N decreased by 60% and the RQ by 13%. The effects of the inoculation with a saline soil were in most cases negative and did not indicate a better adaptation of these organisms to salinity. The general effects of anion composition on microbial biomass and activity indices were small and inconsistent. Only the fraction of 0.5 M K2SO4 extractable C and N in non-fumigated soil was consistently increased in the 1.2 M NaHCO3 treatment of both experiments. In contrast to the small salinity effects, the quality of the substrate has overwhelming effects on microbial biomass and activity indices, especially on the fungal part of the microbial community.

Redox reactions of group 5 elements, including element 105, in aqueous solutions

Standard redox potentials E^0(M^z+x/M^z+) in acidic solutions for group 5 elements including element 105 (Ha) and the actinide, Pa, have been estimated on the basis of the ionization potentials calculated via the multiconfiguration Dirac-Fock method. Stability of the pentavalent state was shown to increase along the group from V to Ha, while that of the tetra- and trivalent states decreases in this direction. Our estimates have shown no extra stability of the trivalent state of hahnium. Element 105 should form mixed-valence complexes by analogy with Nb due to the similar values of their potentials E^0(M^3+/M^2+). The stability of the maximumoxidation state of the elements decreases in the direction 103 > 104 > 105.