Femtosecond imaging-mode laser-induced breakdown spectroscopy

Many nonlinear optical microscopy techniques based on the high-intensity nonlinear phenomena were developed recent years. A new technique based on the minimal-invasive in-situ analysis of the specific bound elements in biological samples is described in the present work. The imaging-mode Laser-Induced Breakdown Spectroscopy (LIBS) is proposed as a combination of LIBS, femtosecond laser material processing and microscopy. The Calcium distribution in the peripheral cell wall of the sunflower seedling (Helianthus Annuus L.) stem is studied as a first application of the imaging-mode LIBS. At first, several nonlinear optical microscopy techniques are overviewed. The spatial resolution of the imaging-mode LIBS microscope is discussed basing on the Point-Spread Function (PSF) concept. The primary processes of the Laser-Induced Breakdown (LIB) are overviewed. We consider ionization, breakdown, plasma formation and ablation processes. Water with defined Calcium salt concentration is used as a model of the biological object in the preliminary experiments. The transient LIB spectra are measured and analysed for both nanosecond and femtosecond laser excitation. The experiment on the local Calcium concentration measurements in the peripheral cell wall of the sunflower seedling stem employing nanosecond LIBS shows, that nanosecond laser is not a suitable excitation source for the biological applications. In case of the nanosecond laser the ablation craters have random shape and depth over 20 µm. The analysis of the femtosecond laser ablation craters shows the reproducible circle form. At 3.5 µJ laser pulse energy the diameter of the crater is 4 µm and depth 140 nm for single laser pulse, which results in 1 femtoliter analytical volume. The experimental result of the 2 dimensional and surface sectioning of the bound Calcium concentrations is presented in the work.

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.

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.