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.

Effects of tillage on processes of organic matter sequestration

To increase the organic matter (OM) content in the soil is one main goal in arable soil management. The adoption of tillage systems with reduced tillage depth and/or frequency (reduced tillage) or of no-tillage was found to increase the concentration of soil OM compared to conventional tillage (CT; ploughing to 20-30 cm). However, the underlying processes are not yet clear and are discussed contradictorily. So far, few investigations were conducted on tillage systems with a shallow tillage depth (minimum tillage = MT; maximum tillage depth of 10 cm). A better understanding of the interactions between MT implementation and changes in OM transformation in soils is essential in order to evaluate the possible contribution of MT to a sustainable management of arable soils. The objectives of the present thesis were (i) to compare OM concentrations, microbial biomass, water-stable aggregates, and particulate OM (POM) between CT and MT soils, (ii) to estimate the temporal variability of water-stable aggregate size classes occurring in the field and the dynamics of macroaggregate (>250 µm) formation and disruption under controlled conditions, (iii) to investigate whether a lower disruption or a higher formation rate accounts for a higher occurrence of macroaggregates under MT compared to CT, (iv) to determine which fraction is the major agent for storing the surplus of OM found under MT compared to CT, and (v) to observe the early OM transformation after residue incorporation in different tillage systems simulated. Two experimental sites (Garte-Süd and Hohes Feld) near Göttingen, Germany, were investigated. Soil type of both sites was a Haplic Luvisol. Since about 40 years, both sites receive MT by a rotary harrow (to 5-8 cm depth) and CT by a plough (to 25 cm depth). Surface soils (0-5 cm) and subsoils (10-20 cm) of two sampling dates (after fallow and directly after tillage) were investigated for concentrations of organic C (Corg) and total N (N), different water-stable aggregate size classes, different density fractions (for the sampling date after fallow only), microbial biomass, and for biochemically stabilized Corg and N (by acid hydrolysis; for the sampling date after tillage only). In addition, two laboratory incubations were performed under controlled conditions: Firstly, MT and CT soils were incubated (28 days at 22°C) as bulk soil and with destroyed macroaggregates in order to estimate the importance of macroaggregates for the physical protection of the very labile OM against mineralization. Secondly, in a microcosm experiment simulating MT and CT systems with soil <250 µm and with 15N and 13C labelled maize straw incorporated to different depths, the mineralization, the formation of new macroaggregates, and the partitioning of the recently added C and N were followed (28 days at 15°C). Forty years of MT regime led to higher concentrations of microbial biomass and of Corg and N compared to CT, especially in the surface soil. After fallow and directly after tillage, a higher proportion of water-stable macroaggregates rich in OM was found in the MT (36% and 66%, respectively) than in the CT (19% and 47%, respectively) surface soils of both sites (data shown are of the site Garte-Süd only). The subsoils followed the same trend. For the sampling date after fallow, no differences in the POM fractions were found but there was more OM associated to the mineral fraction detected in the MT soils. A large temporal variability was observed for the abundance of macroaggregates. In the field and in the microcosm simulations, macroaggregates were found to have a higher formation rate after the incorporation of residues under MT than under CT. Thus, the lower occurrence of macroaggregates in CT soils cannot be attributed to a higher disruption but to a lower formation rate. A higher rate of macroaggregate formation in MT soils may be due to (i) the higher concentrated input of residues in the surface soil and/or (ii) a higher abundance of fungal biomass in contrast to CT soils. Overall, as a location of storage of the surplus of OM detected under MT compared to CT, water-stable macroaggregates were found to play a key role. In the incubation experiment, macroaggregates were not found to protect the very labile OM against mineralization. Anyway, the surplus of OM detected after tillage in the MT soil was biochemically degradable. MT simulations in the microcosm experiment showed a lower specific respiration and a less efficient translocation of recently added residues than the CT simulations. Differences in the early processes of OM translocation between CT and MT simulations were attributed to a higher residue to soil ratio and to a higher proportion of fungal biomass in the MT simulations. Overall, MT was found to have several beneficial effects on the soil structure and on the storage of OM, especially in the surface soil. Furthermore, it was concluded that the high concentration of residues in the surface soil of MT may alter the processes of storage and decomposition of OM. In further investigations, especially analysis of the residue-soil-interface and of effects of the depth of residue incorporation should be emphasised. Moreover, further evidence is needed on differences in the microbial community between CT and MT soils.

Characterization of Lipid Droplets and Functional Analysis of Lipid Droplet-Associated Proteins in Dictyostelium discoideum

Lipid droplets (LDs) are the universal storage form of fat as a reservoir of metabolic energy in animals, plants, bacteria and single celled eukaryotes. Dictyostelium LD formation was investigated in response to the addition of different nutrients to the growth medium. LDs were induced by adding exogenous cholesterol, palmitic acid (PA) as well as growth in bacterial suspension, while glucose addition fails to form LDs. Among these nutrients, PA addition is most effective to stimulate LD formation, and depletion of PA from the medium caused LD degradation. The neutral lipids incorporated into the LD-core are composed of triacylglycerol (TAG), steryl esters, and an unknown neutral lipid (UKL) species when the cells were loaded simultaneously with cholesterol and PA. In order to avoid the contamination with other cellular organelles, the LD-purification method was modified. The isolated LD fraction was analysed by mass spectrometry and 100 proteins were identified. Nineteen of these appear to be directly involved in lipid metabolism or function in regulating LD morphology. Together with a previous study, a total of 13 proteins from the LD-proteome were confirmed to localize to LDs after the induction with PA. Among the identified LD-proteins, the localization of Ldp (lipid droplet membrane protein), GPAT3 (glycerol-3-phosphate acyltransferase 3) and AGPAT3 (1-acylglycerol-3-phosphate-acyltransferase 3) were further verified by GFP-tagging at the N-termini or C-termini of the respective proteins. Fluorescence microscopy demonstrated that PA-treatment stimulated the translocation of the three proteins from the ER to LDs. In order to clarify DGAT (diacylglycerol acyltransferase) function in Dictyostelium, the localization of DGAT1, that is not present in LD-proteome, was also investigated. GFP-tagged DGAT1 localized to the ER both, in the presence and absence of PA, which is different from the previously observed localization of GFP-tagged DGAT2, which almost exclusively binds to LDs. The investigation of the cellular neutral lipid level helps to elucidate the mechanism responsible for LD-formation in Dictyostelium cells. Ldp and two short-chain dehydrogenases, ADH (alcohol dehydrogenase) and Ali (ADH-like protein), are not involved in neutral lipid biosynthesis. GPAT, AGPAT and DGAT are three transferases responsible for the three acylation steps of de novo TAG synthesis. Knock-out (KO) of AGPAT3 and DGAT2 did not affect storage-fat formation significantly, whereas cells lacking GPAT3 or DGAT1 decreased TAG and LD accumulation dramatically. Furthermore, DGAT1 is responsible for the accumulation of the unknown lipid UKL. Overexpression of DGAT2 can rescue the reduced TAG content of the DGAT1-KO mutant, but fails to restore UKL content in these cells, indicating that of DGAT1 and DGAT2 have overlapping functions in TAG synthesis, but the role in UKL formation is unique to DGAT1. Both GPAT3 and DGAT1 affect phagocytic activity. Mutation of GPAT3 increases it but a DGAT1-KO decreases phagocytosis. The double knockout of DGAT1 and 2 also impairs the ability to grow on a bacterial lawn, which again can be rescued by overexpression of DGAT2. These and other results are incorporated into a new model, which proposes that up-regulation of phagocytosis serves to replenish precursor molecules of membrane lipid synthesis, whereas phagocytosis is down-regulated when excess fatty acids are used for storage-fat formation.  

Effects of different tillage treatments on labile soil organic matter pools and stabilization processes

An improved understanding of soil organic carbon (Corg) dynamics in interaction with the mechanisms of soil structure formation is important in terms of sustainable agriculture and reduction of environmental costs of agricultural ecosystems. However, information on physical and chemical processes influencing formation and stabilization of water stable aggregates in association with Corg sequestration is scarce. Long term soil experiments are important in evaluating open questions about management induced effects on soil Corg dynamics in interaction with soil structure formation. The objectives of the present thesis were: (i) to determine the long term impacts of different tillage treatments on the interaction between macro aggregation (>250 µm) and light fraction (LF) distribution and on C sequestration in plots differing in soil texture and climatic conditions. (ii) to determine the impact of different tillage treatments on temporal changes in the size distribution of water stable aggregates and on macro aggregate turnover. (iii) to evaluate the macro aggregate rebuilding in soils with varying initial Corg contents, organic matter (OM) amendments and clay contents in a short term incubation experiment. Soil samples were taken in 0-5 cm, 5-25 cm and 25-40 cm depth from up to four commercially used fields located in arable loess regions of eastern and southern Germany after 18-25 years of different tillage treatments with almost identical experimental setups per site. At each site, one large field with spatially homogenous soil properties was divided into three plots. One of the following three tillage treatments was carried in each plot: (i) Conventional tillage (CT) with annual mouldboard ploughing to 25-30 cm (ii) mulch tillage (MT) with a cultivator or disc harrow 10-15 cm deep, and (iii) no tillage (NT) with direct drilling. The crop rotation at each site consisted of sugar beet (Beta vulgaris L.) - winter wheat (Triticum aestivum L.) - winter wheat. Crop residues were left on the field and crop management was carried out following the regional standards of agricultural practice. To investigate the above mentioned research objectives, three experiments were conducted: Experiment (i) was performed with soils sampled from four sites in April 2010 (wheat stand). Experiment (ii) was conducted with soils sampled from three sites in April 2010, September 2011 (after harvest or sugar beet stand), November 2011 (after tillage) and April 2012 (bare soil or wheat stand). An incubation study (experiment (iii)) was performed with soil sampled from one site in April 2010. Based on the aforementioned research objectives and experiments the main findings were: (i) Consistent results were found between the four long term tillage fields, varying in texture and climatic conditions. Correlation analysis of the yields of macro aggregate against the yields of free LF ( ≤1.8 g cm-3) and occluded LF, respectively, suggested that the effective litter translocation in higher soil depths and higher litter input under CT and MT compensated in the long term the higher physical impact by tillage equipment than under NT. The Corg stocks (kg Corg m−2) in 522 kg soil, based on the equivalent soil mass approach (CT: 0–40 cm, MT: 0–38 cm, NT: 0–36 cm) increased in the order CT (5.2) = NT (5.2) < MT (5.7). Significantly (p ≤ 0.05) highest Corg stocks under MT were probably a result of high crop yields in combination with reduced physical tillage impact and effective litter incorporation, resulting in a Corg sequestration rate of 31 g C-2 m-2 yr-1. (ii) Significantly higher yields of macro aggregates (g kg-2 soil) under NT (732-777) and MT (680-726) than under CT (542-631) were generally restricted to the 0-5 cm sampling depth for all sampling dates. Temporal changes on aggregate size distribution were only small and no tillage induced net effect was detectable. Thus, we assume that the physical impact by tillage equipment was only small or the impact was compensated by a higher soil mixing and effective litter translocation into higher soil depths under CT, which probably resulted in a high re aggregation. (iii) The short term incubation study showed that macro aggregate yields (g kg-2 soil) were higher after 28 days in soils receiving OM (121.4-363.0) than in the control soils (22.0-52.0), accompanied by higher contents of microbial biomass carbon and ergosterol. Highest soil respiration rates after OM amendments within the first three days of incubation indicated that macro aggregate formation is a fast process. Most of the rebuilt macro aggregates were formed within the first seven days of incubation (42-75%). Nevertheless, it was ongoing throughout the entire 28 days of incubation, which was indicated by higher soil respiration rates at the end of the incubation period in OM amended soils than in the control soils. At the same time, decreasing carbon contents within macro aggregates over time indicated that newly occluded OM within the rebuilt macro aggregates served as Corg source for microbial biomass. The different clay contents played only minor role in macro aggregate formation under the particular conditions of the incubation study. Overall, no net changes on macro aggregation were identified in the short term. Furthermore, no indications for an effective Corg sequestration on the long term under NT in comparison to CT were found. The interaction of soil disturbance, litter distribution and the fast re aggregation suggested that a distinct steady state per tillage treatment in terms of soil aggregation was established. However, continuous application of MT with a combination of reduced physical tillage impact and effective litter incorporation may offer some potential in improving the soil structure and may therefore prevent incorporated LF from rapid decomposition and result in a higher C sequestration on the long term.

Vom Biofilm zur planktonischen Lebensform

Im ersten Teil dieser Dissertation stand die Analyse der Motilitätsentwicklung bei Vertretern der Gattung Methylobacterium im Vordergrund. Diese zu den pink pigmentierten fakultativ methylotrophen Mikroorganismen (PPFMs) gehörenden Prokaryoten sind in der Umwelt weit verbreitet. Besonders häufig besiedeln die Mikroben pflanzliche Oberflächen und können als so genannte Phytosymbionten in einer wechselseitigen Beziehung zu pflanzlichen Organismen stehen. In aquatischer Umgebung können Methylobakterien Flagellen aufweisen. Hierbei handelt es sich um spezielle Fortbewegungsorganellen, die den Mikroben eine aktive Beweglichkeit ermöglichen. Die Ausbildung polarer Einzelflagellen bei Methylobacterium-Zellen in planktonischer Lebensweise konnte unter Anwendung verschiedener mikroskopischer Techniken dokumentiert werden. Quantitative Beweglichkeitsstudien zeigten einen charakteristischen Entwicklungsverlauf, korreliert mit den Wachstumsphasen der Bakterienkulturen und machten deutlich, dass die Motilitätsrate durch Umweltfaktoren, wie z. B. die Nährstoffversorgung, beeinflusst werden kann. Es konnte gezeigt werden, dass die Pflanzen-assoziierten PPFMs in der Lage sind, zwischen einer sessilen und planktonischen Lebensweise zu wechseln und dass sowohl die zelluläre Beweglichkeit als auch die Biofilm-Bildung der Prokaryoten ein reversibles, reaktivierbares Verhalten darstellt. Weiterhin konnte belegt werden, dass die Motilität der epiphytischen Mikroben bezüglich der Besiedelung von Pflanzen, z. B. bei der Ausbreitung auf Keimblatt-Oberflächen von Sonnenblumen (Helianthus annuus), keine zentrale Rolle spielt und eine endophytische Lebensweise unwahrscheinlich ist. Ziel der Arbeit war weiterhin die Charakterisierung und Identifizierung eines aus der Phyllosphäre der Echten Feige (Ficus carica, Standort Griechenland) isolierten Bakterien-Stammes (Mtb. sp. Fc1). Die fakultativ methylotrophe Stoffwechseleigenschaft, sowie die auffällige rötliche Pigmentierung belegen, dass es sich um einen Vertreter der PPFMs handelt. Die Analyse morphologischer, physiologischer und biochemischer Eigenschaften bestätigte in Übereinstimmung mit molekularphylogenetischen Untersuchungen zur Klassifizierung und taxonomischen Einordnung, dass es sich um Pflanzen-assoziierte Mikroben der Gattung Methylobacterium handelt. Analysen der 16S rDNA sowie partieller Sequenzen der für Methylobakterien etablierten Marker-Gene mxaF und gyrB verdeutlichten die phylogenetische Stellung und die evolutionären Beziehungen des Ficus-Isolates. Obwohl enge Verwandtschaftsverhältnisse zu anderen Methylobacterium-Arten ermittelt werden konnten, war eine Identifizierung als valide beschriebene Spezies nicht möglich. Die Resultate legen den Schluss nahe, dass es sich um eine neue, unbeschriebene Spezies der epiphytisch lebenden Methylobakterien handelt.