Die Rolle des Zelladhäsionsmoleküls L1 in der Tumorprogression

Das neuronale Adhäsionsmolekül L1 wird neben den Zellen des Nervensystems auf vielen humanen Tumoren exprimiert und ist dort mit einer schlechten Prognose für die betroffenen Patienten assoziiert. Zusätzlich zu seiner Funktion als Oberflächenmolekül kann L1 durch membranproximale Spaltung in eine lösliche Form überführt werden. In der vorliegenden Arbeit wurde der Einfluss von L1 auf die Motilität von Tumorzellen untersucht. Lösliches L1 aus Asziten führte zu einer Integrin-vermittelten Zellmigration auf EZM-Substraten. Derselbe Effekt wurde durch Überexpression von L1 in Tumorlinien beobachtet. Weiterhin führt die L1-Expression zu einer erhöhten Invasion, einem verstärkten Tumorwachstum in NOD/SCID Mäusen und zur konstitutiven Aktivierung der MAPK ERK1/2. Eine Mutation in der zytoplasmatischen Domäne von hL1 (Thr1247Ala/Ser1248Ala)(hL1mut) führte hingegen zu einer Blockade dieser Funktionen. Dies weist daraufhin, dass nicht nur lösliches L1, sondern auch die zytoplasmatische Domäne von L1 funktionell aktiv ist. Im zweiten Teil der Arbeit wurde der Mechanismus, der L1-vermittelten Signaltransduktion untersucht. Die zytoplasmatische Domäne von L1 gelangt nach sequenzieller Proteolyse durch ADAM und Presenilin-abhängiger γ-Sekretase Spaltung in den Zellkern. Diese Translokation im Zusammenspiel mit der Aktivierung der MAPK ERK1/2 durch L1-Expression führt zu einer L1-abhängigen Genregulation. Die zytoplasmatische Domäne von hL1mut konnte ebenfalls im Zellkern detektiert werden, vermittelte jedoch keine Genregulation und unterdrückte die ERK1/2 Phosphorylierung. Die L1-abhängige Induktion von ERK1/2-abhängigen Genen wie Cathepsin B, β3 Integrin und IER 3 war in Zellen der L1-Mutante unterdrückt. Die Expression des Retinsäure-bindenden Proteins CRABP-II, welches in hL1 Zellen supprimiert wird, wurde in der L1-Mutante nicht verändert. Weitere biochemische Untersuchungen zeigen, dass die zytoplasmatische Domäne von L1 Komplexe mit Transkriptionsfaktoren bilden kann, die an Promoterregionen binden können. Die dargestellten Ergebnisse belegen, dass L1-Expression in Tumoren an drei Funktionen beteiligt ist; (i) L1 erhöht Zellmotilität, (ii) fördert Tumorprogression durch Hochregulation von pro-invasiven und proliferationsfördernden Genen nach Translokation in den Nukleus und (iii) schützt die Zellen mittels Regulation pro- bzw. anti-apoptotischer Gene vor Apoptose. Die mutierte Phosphorylierungsstelle im L1-Molekül ist essentiell für diese Prozesse. Die Anwendung neuer Therapien für Patienten mit L1-positiven Karzinomen kann mit Hinblick auf die guten Erfolge der Antikörper-basierenden Therapie mit dem mAk L1-11A diskutiert werden.

Changes in amino acid enantiomers and microbial performance in soils from a subtropical mountain oasis in Oman abandoned for different periods

An important feature of maintaining the agricultural stability in millennia-old mountain oases of northern Oman is the temporary abandonment of terraces. To analyse the effects of a fallow period on soil microbial performance, i.e. microbial activity and microbial biomass, samples of eight terrace soils abandoned for different periods were collected in situ, assigned to four fallow age classes and incubated for 30 days in the laboratory after rewetting. The younger fallow age classes of 1 and 5 years were based on the records of the farmers’ recollections, the two older fallow age classes of 10–20 and 25–60 years according to the increase in the D -to- L ratio of valine and leucine enantiomers. The increase in these two ratios was in agreement with that of the D -to- L ratio of lysine. The strongest relationship was observed between the increase in the D -to- L ratio of lysine and the decrease in soil microbial biomass C. However, the most stringent coherence between the increase in fallow age and soil properties was revealed by the decreases in cumulative respiration and net N mineralisation rates with decreasing availability of substrate to soil microorganisms. During the 30-day incubation following rewetting, relative changes in microbial activity (respiration and net N mineralisation) and microbial biomass (C and N)indices were similar in the eight terrace soils on a fallow age-class-specific level, indicating that the same basic processes occurred in all of the sandy terrace soils investigated.

Effect of environmental conditions on the N uptake route of soil microorganisms and adaption of a method to determine amino acid oxidase in soil

Soil microorganisms have evolved two possible mechanisms for their uptake of organic N: the direct route and the mobilization-immobilization-turnover (MIT) route. In the direct route, simple organic molecules are taken up via various mechanisms directly into the cell. In the MIT route, the deamination occurs outside the cell and all N is mineralized to NH4+ before assimilation. A better understanding of the mechanisms controlling the different uptake routes of soil microorganisms under different environmental conditions is crucial for understanding mineralization processes of organic material in soil. For the first experiment we incubated soil samples from the long term trial in Bad Lauchstädt with corn residues with different C to N ratios and inorganic N for 21 days at 20 °C. Under the assumption that all added amino acids were taken up or mineralized, the direct uptake route was more important in soil amended with corn residues with a wide C to N ratio. After 21 days of incubation the direct uptake of added amino acids increased in the order addition of corn residue with a: “C to N ratio of 40 & (NH4)2SO4 and no addition (control)” (69% and 68%, respectively) < “C to N ratio of 20” (73%) < “C to N ratio of 40” (95%). In all treatments the proportion of the added amino acids that were mineralized increased with time, indicating that the MIT route became more important over time. To investigate the effects of soil depth on the N uptake route of soil microorganisms (experiment II), soil samples in two soil depths (0-5 cm; 30-40 cm) were incubated with corn residues with different C to N ratios and inorganic N for 21 days at 20 °C and 60% (WHC). The addition of corn residue resulted in a marked increase of protease activity in both depths due to the induction from the added substrate. Addition of corn residue with a wide C to N ratio resulted in a significantly greater part of the direct uptake (97% and 94%) than without the addition of residues (85% and 80%) or addition of residue with a small C to N ratio (90% and 84%) or inorganic N (91% and 79% in the surface soil and subsoil, respectively), suggesting that under conditions of sufficient mineralizable N (C to N ratio of 20) or increased concentrations of NH4+, the enzyme system involved in the direct uptake is slightly repressed. Substrate additions resulted in an initially significantly higher increase of the direct uptake in the surface soil than in the subsoil. As a large proportion of the organic N input into soil is in form of proteinaceous material, the deamination of amino acids is a key reaction of the MIT route. Therefore the enzyme amino acid oxidase contribute to the extracellular N mineralization in soil. The objective of experiment III was to adapt a method to determine amino acid oxidase in soil. The detection via synthetic fluorescent Lucifer Yellow derivatives of the amino acid lysine is possible in soil. However, it was not possible to find the substrate concentration at which the reaction rate is independent of substrate concentration and therefore we were not able to develop a valid soil enzyme assay.