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For many years, rangeland ecologists have debated about whether the state of semi-arid and arid rangelands is the expression of an ecological equilibrium or non-equilibrium dynamics reached in response to grazing livestock. Since the problem has been considered at different spatial scales, it is recognised that the competing concepts of equilibrium and non-equilibrium dynamics need to be integrated. Furthermore, the role of environmental variables as vegetation driving factors has long been ignored in the discussion on grazing effects on ecosystems. Present thesis, examines the dependence of plant communities on environmental in particular site-ecological conditions in three ecosystems of Western Mongolia established along a precipitation gradient to detect the vegetation-driving ecological factors involved. Furthermore, grazing impact is exemplary assessed in a desert steppe at additional spatial scales of plant communities and population. At the landscape level, a classification of plant communities in dependence on environmental conditions is carried out. Additionally, the investigations focused on the impact of grazing on soil and on the occurrence of grazing-mediated plant communities. Data were sampled along an altitudinal gradient between 1150 m to 3050 m a.s.l. from arid lowland with desert steppe via semi-arid mountain steppe to humid alpine belt. Within each altitudinal belt, data sampling was carried out along grazing gradients, established from grazing hot spots to areas distant from them. By means of an environmentally based vegetation classification, factors with highest explanation values for largest variation in vegetation were identified and considered as most responsible for vegetation patterns. To validate and affirm the classification, three different statistical methods are applied: environmentally adjusted table work of vegetation relevés supported by cluster analysis of species distribution, detrended correspondence analysis of vegetation data separately from environmental data, and the principle component analysis of only environmental data. Vegetation-driving factors change along the altitudinal gradient from abiotic forces in the desert steppe, as e.g. altitude and soil texture, to abiotic and biotic forces in the alpine belt represented by soil texture, soil nutrients and grazing. Vegetation and soil of all ecosystems respond to grazing but with different patterns and to a different extent. While desert steppe does not indicate grazing communities, mountain steppe demonstrates grazing communities at fertilised sites and alpine belt at nutrients depleted sites. Thus, the grazing sensitiveness of the ecosystems is assumed to be linked with plant productivity and the role of vegetation as site-determining factor (Chapter 2). To examine grazing impact at lower spatial scales on desert steppe as the ecosystem with lowest grazing sensitiveness at the landscape scale, at community scale the total number of species, the total vegetation cover, the percentage of annual species, the cover of annual species, and properties of soil nutrient along gradients of grazing intensity within three different communities were assessed. Vegetation parameters respond to grazing in different ways, and the responses of the same parameters vary between plant communities. Correlations with grazing intensity indicate only partly statistical significance. Significant correlations of grazing intensity with concentrations of soil nutrient point to eutrophication in two communities. A comparison of vegetation and soil properties refers to a greater indirect influence of grazing via increased soil nutrients than the direct effect on vegetation (Chapter 4). At the population level, data about stand density, aboveground biomass, individual plant weight, and the proportion of flowering plants of the dominant dwarf semi-shrub Artemisia xerophytica were collected along a grazing gradient. Soil data were used to distinguish between grazing and edaphic influences. All parameters of Artemisia xerophytica reflect the assumed gradient of grazing intensity up to 800 m distance from the grazing hot spot. As grazing pressure decreases, plant density and total biomass per plot increase. The average shrub weight, an indicator of plant vitality, is related to both: distance from the grazing hot spot and stand density, which may be explained by additional intraspecific competition at higher densities. At a longer distance, these effects are masked by variations in soil parameters determining water availability, leading to quite similar degradation forms. These results are in contrast to other studies carried out at the scale of plant communities which did not detect significant changes along a grazing gradient. One explanation is the different map scale: the study took place only within a single plant community comparing populations of one species (Chapter 3). The comparative study demonstrates that even arid desert steppes of western Mongolia display equilibrial and non-equilibrial properties, depending on the observational scale: while no grazing mediated plant communities could be identified at the landscape scale as predicted by the non-equlilibrium model, at the community level vegetation parameters imply an intermediate position between equilibrium and non-equilibrium system. At the population level, the results clearly reflect the grazing gradient as predicted by the equilibrium model (Chapter 4). As a consequence, the assessment of vegetation dynamics and grazing impact in rangelands requires a multiple-scale approach that duly considers different vegetation properties responding differently to grazing, climatic and edaphic variability at different spatial scales. It is further suggested, that future research should draw comparisons between landscapes that co-evolved with herbivory, and those that did without (Chapter 4).
1,1-Bis(trimethylsilyloxy)ketene acetals represent useful synthetic building blocks which can be regarded as masked carboxylic acid dianions. In recent years, a number of cyclization reactions of 1,1-bis(trimethylsilyloxy)ketene acetals have been reported. Functionalized maleic anhydrides represent important synthetic building blocks, which have been employed, for example, in the synthesis of γ-alkylidenebutenolides, maleimides, 5-alkylidene-5H-pyrrol-2-ones. Substituted maleic anhydrides are available by Michael reaction of nucleophiles with parent maleic anhydride and subsequent halogenation and elimination. Oxalyl chloride is an important synthetic tool for the synthesis of O-heterocycles. 3-hydroxymaleic (1-3) anhydrides were synthesised by one-pot cyclization of 1,1-bis(trimethylsilyloxy)ketene acetals with oxalyl chloride using TMSOTf as a catalyst. The Me3SiOTf mediated reaction of 1,1-bis(trimethylsilyloxy)ketene acetals with 3-silyloxyalk-2-en-1-ones, such as (4), afforded 5-ketoacids, such as (5). Treatment of the latter with TFA in CH2Cl2 afforded pyran-2-ones, such as (6-8). It has been found that 1,1-bis(trimethylsilyloxy)ketene acetals can behave as dinucleophile. Functionalized benzo-azoxabicyclo[3.3.1]nonanones (9-12), were prepared by regio- and diastereoselective condensation of 1,1-bis(silyloxy)ketene acetals with isoquinolinium and quinolinium salts and subsequent regioselective and stereospecific iodolactonization. Our next target was the reaction of silyl ketene acetals with pyrazine and quinoxaline. These reactions provide a facile access to a variety of 2,3-benzo-1,4-diaza-7-oxabicyclo[4.3.0]non-2-en-6-ones and 1,4-diaza-7-oxabicyclo[4.3.0]non-2-en-6-ones (13-14). The second part of my research work was concentrated on bis(silyl enol ethers). The TiCl4-mediated [3+3] cyclization of 2,4-bis(trimethylsilyloxy)penta-1,3-diene with 3-silyloxyalk-2-en-1-ones afforded 2-acetylphenols (15), which were transformed into functionalized chromones (16). The Me3SiOTf-mediated condensation of the latter with 1,3-bis(silyl enol ethers) and subsequent domino ′retro-Michael–aldol–lactonization′ reaction afforded 7-hydroxy-6H-benzo[c]chromen-6-ones (17-18). With regard to our on going investigation with bis(silyl enol ethers), we significantly extended the preparative scope of the methodology. We have successfully developed regioselective cyclizations of unsymmetrical 1,1-diacylcyclopentanes, such as 1-acetyl-1-formylcyclopentane, and also studied cyclizations of 2,2-diacetylindane, 1,1-diacetylcyclopent-3-ene and 3,3-dimethylpentane-2,4-dione. In addition, the mechanism of the domino process was studied. We have synthesised spiro[5.4]decenones (19) and that were transfored into bicyclo[4.4.0]deca-1,4-dien-3-ones (20-21), by domino ′Elimination–Double-Wagner-Meerwein-Rearrangement′ reactions. The Lewis acid mediated domino ′[3+3]-cyclization-homo-Michael′ reaction of 1,3-bis-silyl enol ethers with unsymmetrical 1,1-diacylcyclopentanes, such as 1-acetyl-1-formylcyclopentane, allows an efficient one-pot synthesis of functionalized salicylates containing a halogenated side-chain (22-23). A great variety of substitution patterns have been realized by variation of the starting materials and of the Lewis acid. The mechanism of the domino process was studied.
Synthesis and evaluation of pseudosaccharin amine derivatives as potential elastase inhibitions
(2006)
Elastase is a serine protease which by definition is able to solubilize elastin by hydrolytic cleavage.Human Leukocyte Elastase, HLE (EC 3.4.21.37), is involved in deseases such as adult respiatory distress syndrome, pulmonary emphysema, smoking related chronic bronchitits, ischemic-reperfusion injury and rheumatoid arthritis. Hence, the elastase inhibitors have clinical utility in these diseases. Heterocyclic compounds are one of the most important classes of the elastase inhibitiors. In the present work different pseudosaccharin amine derivatives were synthesized and tested against the elastase. The synthesis of pseudosaccharin amine dervatives was carried out from the amines and(1,1-dioxobenzo[d]isothiazol-3-ylsulfanyl)acetonitrile in different solvents. Futhermore, the pseudosaccharin amines were obtained by refluxing the thiosaccarinates in absolute acetic acid. The reaction of 3-ethoxybenzo[d]isothiazole 1,1-dioxide with different amines in dioxane under reflux resulted into the desired pseudosaccharin amine derivatives in higher yields. Pseudosaccharin chloride was also used in the synthesis of these derivatives.A detail study of the synthesis of pseudosaccharin amine dervatives from the above differnt routes is described. Peptides were also synthesized by using the mixed anhydride method. The ester, acid, amide and peptide derivatives were tested against the Porcine Pancreatic Elastase (PPE) and Human Leukocyte Elastase (HLE). The esters were found to be the reversible inhibitors of HLE. The process of the PPE inhibion by cyanomethyl(2S)-2-(1,1-dioxobenzo[d]isothiazol-3-ylamino)-3-methylbutanoate was studied. Michaelis-Menten curve and Lineweaver-Burk double reciprocal plot were constructed in order to study the kinetic of this reaction. The compounds showing high inhibition of HLE were further stuied for determination of their inhibitory constant(Ki). The esters were found to be the higly active compounds against HLE. The cyanomethyl(2S)-2-(1,1-dioxobenzo[d]isothiazol-3-ylamino)-3-methylbutanoate and cyanomethyl(2S,3S)-2-(1,1-dioxobenzo[d]isothiazol-3-ylamino)-3-methylpentanoate showed the competitive reversible inhibition of HLE.The cyanomethyl(2S,3S)-2-(1,1-dioxobenzo[d]isothiazol-3-ylamino)-3-methylpentanoate is highly potent inhibitor of HLE. The possible mechanism of inhibition of elastase by these compounds is discussed. Molecular modelling of some of the ester derivatives is also discussed.
Based on distributions of local Green's functions we present a stochastic approach to disordered systems. specifically we address Anderson localisation and cluster effects in binary alloys. Taking Anderson localisation of Holstein polarons as an example we discuss how this stochastic approach can be used for the investigation of interacting disordered systems.
Recent geochemical and mineralogical alteration processes in tropical coastal sediments of Vietnam
(2006)
The dissertation contains two main parts: (i) Syn-sedimentary hydrodynamic processes & relationship with elemental distribution, clay matter, (ii) Short-term mineral alteration during early diagenes. Samples were taken from the uppermost one metre (<50 year old in RRD, < 300 y old in south central VN). In part one, three principal hydrodynamic factors can be revealed based on End-Member Modelling Algorithm (EMMA), for the polymodal grain-size distribution patterns in coastline of VN (i) Accumulation factor: accumulation of terrigenous sediments linked with a grain size separation (distance dependence), (ii) Erosion factor: synsedimentary erosion by wave activities, (iii) Aeolian factor: deposition from neighbour sand bar by wind (typically only for low sedimentation rate, like in South Central Coast but not to detect in RRD). Distributions of clay matter and chemical elements in the coastal sediments in Vietnam are strongly influenced by hydrodynamic forces (distance from the coastline). In part two, particle-wise analysis by TEM allowed to determined four main mixed layer series: di-Vermiculite/Smectite-ml, Kaolinite/ Expandable-ml, Illite/Smectite-ml, Chlorite/Saponite-ml. Three principal mineral alteration processes can be detected in coastal sediments during early diagenesis: Dissolution, Smectitization, Kaolinitization, based on XRD (CSD, peak area) & TEM-EDX (particle morphology, chemical formula, polytype, particle frequency). Dissolution process of clay matter is typically in the coastal alkaline condition. It is a function of diagenetic time. Dissolution begins with a higher degree of dislocation and is followed by step-wise delamination & dissolution of the first stacks Smectitization (mirrored in diVS-ml series) alters mica-like structures (illite, dioctahedral vermiculite) to smectitic structures (Beidellite, Montmorillonite). Smectitization process occurs in group-wise layer by layer transforming mechanism (mica-like layer to smectitic layer). Each step is indicated by a gauss-like distribution of the octahedral layer charge with K as trigger. Kaolinitization of KE series alters smectitic structure (beidellite, smectitic KE-ml) to kaolinitic structure (kaolinitic KE-ml, kaolinite) "interlayer by interlayer" transformation of KE-ml series is comparable to kaolinitization mechanism discussed by Dudek et al. (2006).OH- groups in ambient could be the trigger. Mangroves biota influences the sediments in two main pathways: Nutrients supply & trapping function (clay matter, heavy metals)Interaction of active root-layer: intensification of dissolution, smectitization & kaolinitization: uptake of K, Na by mangrove root is possible trigger Human activities like shrimp cultivation have stopped the influences of the former active roots.Besides, erosion process related to water discharge gives rise to dispersion of clay species & heavy metals => more toxic for ecosystem.
Proteomic signatures select the physiology state of the cell. By using 2-D technique, proteome signature of Bacillus subtilis under different stresses and starvations are analyzed. Consequently, a proteomic map of Bacillus subtilis in non-growing phase was created. The ammonium and tryptophan as well as phenol and catechol stress are analyzed using both of proteomics and transcriptomics. And the proteomic map represents a good application in the prediction of the mode of action of phenol and catechol stress.
A fluorescent lamp driven with an 'instant start electronic control gear' starts in a glow mode. In the glow mode, which lasts typically for tens of milliseconds, the cathode fall exceeds hundreds of volts. This causes high energy ion bombardment of the electrode which heats the electrode, and induces a transition from glow to arc mode. In the arc mode the electrode emits thermionically and the cathode fall drops to the 12 – 15 V range. Unfortunately, the high energy ion bombardment during the glow mode leads also to intense sputtering of electrode material, including tungsten as well as emitter. Thus, instant started fluorescent lamps often suffer from early failures due to coil fracture. Therefore, the investigation of tungsten erosion during instant start is necessary and was the main goal of this work.
The density of neutral atomic tungsten is determined by laser-induced fluorescence (LIF) and optical emission spectroscopy measurements (OES). Investigations are performed on a low-pressure argon dc discharge and on commercial fluorescent lamps. To include the entire temperature profile along the electrode the diffuse and spot operation modes of the dc lamp are studied experimentally and theoretically. The measured dependencies of the cathode temperature along the coil on the discharge and heating parameters are compared with the calculated results. For the first time the tungsten erosion during instant start of commercial fluorescent lamps was experimentally investigated in this work. The erosion process could be related to sputtering. A reconstruction of the temporal evolution of the absolute tungsten population density of the ground state during the glow mode was presented. The sputtered tungsten density increases immediately with the ignition, reaches a maximum where the discharge contracts at the end of the glow mode, and decreases some milliseconds before the glow-to-arc transition takes place. The maximum tungsten density was observed within a region of a few hundred micrometers only located at the discharge attachment point. The main result achieved in this work is that during the whole glow mode tungsten is sputtered. Therefore, the lifetime of instant started fluorescent lamps can be enhanced by reducing the duration of the glow mode. Additionally, the need for the application of different types of diagnostics for the observation of lamp ignition was shown due to different results of LIF, AAS and OES: The observation of excited tungsten atoms by OES shows the maximum emission signal at the glow-to-arc transition whereas by LIF and AAS measurements of tungsten atoms in the ground state the maximum density is found during the whole glow mode. This can be explained by the fact that the intensity of the spontaneous emitted light is related not only to the density but also to the degree of excitation.
The interaction of partially ionized plasmas with an electromagnetic field is investigated using quantum statistical methods. A general statistical expression for the current density of a plasma in an electromagnetic field is presented and considered in the high field regime. Expressions for the collisional absorption are derived and discussed. Further, partially ionized plasmas are considered. Plasma Bloch equations for the description of bound-free transitions are given and the absorption coefficient as well as rate coefficients for multiphoton ionization are derived and numerical results are presented.
SUMMARY To date, Staphylococcus aureus is the most common cause of nosocomial infections and the species is becoming increasingly resistant to antibiotics. Beyond this, S. aureus colonises the nasal mucosa of circa 35% of the healthy population, so-called carriers. Importantly, S. aureus nasal carriage is a major risk factor for the development of S. aureus infections, which are commonly caused by the colonising strain. This underlines the importance of host factors for the outcome of S. aureus-host interactions. Despite the clinical importance of nasal carriage, little is known about humoral immune responses triggered by colonisation. Therefore, this thesis was focussed on the anti-staphylococcal antibody responses of S. aureus carriers and noncarriers. Staphylococcal superantigens (SAgs) served as indicator antigens for our studies. SAgs are virulence factors with extraordinary variability in the species S aureus and act as extremely potent T cell mitogens. To date, 19 different SAg gene loci are known in the species S. aureus, but molecular-epidemiological studies on the distribution of these genes are limited. Therefore, we established five multiplex PCRs for the detection of all known SAgs. With this robust and high-throughput technique we analysed the SAg gene patterns of more than 300 isolates, including 107 nasal isolates of S. aureus carriers and 88 blood culture isolates of hospital patients from Western Pomerania. The SAg gene patterns were highly heterogeneous, which can be explained by their localisation on mobile genetic elements (MGE), such as genomic islands, pathogenicity islands, phages and plasmids. Most isolates (~80%) harboured SAg genes, on average five to six, and SAgs of the enterotoxin gene cluster (egc) were by far the most prevalent. Additionally, we observed a strict correlation between the presence of SAg genes and the T cell mitogenic potency of clinical isolates. SAg-encoding MGEs can be distributed by two distinct mechanisms: horizontal transfer by bacteriophages and vertical transmission to daughter cells. To investigate the distribution of SAg genes within the S. aureus population, we determined the clonal relationship of our isolates by spa genotyping. Interestingly, SAg-gene encoding MGEs were not randomly distributed, but rather closely linked to clonal lineages. Each clonal lineage was characterised by defined combinations of SAg genes. These data suggest that the simultaneous assessment of virulence gene profiles and the genetic background strongly enhances the discriminatory power of genetic investigations into the mechanisms of S. aureus virulence. Indeed, the comparison of virulence genes within each clonal complex indicated a role in invasiveness for some MGEs, e.g. the exfoliative toxin D-encoding pathogenicity island, while rendering it unlikely for SAgs. It is known that neutralising serum antibodies against the SAgs SEA, SEB, SEC, SED and TSST-1 are frequently present in healthy individuals. However, the neutralising antibody profiles against more recently described SAgs or complex SAg cocktails as secreted by clinical isolates had not been determined so far. Therefore, we screened more than 100 sera for their SAg neutralising capacity with a neutralisation assay. We observed a marked heterogeneity and surprisingly large “gaps” in the neutralising capacity. Interestingly, the egc SAgs were inhibited only rarely (5-10%), whereas between 32 and 86% of the tested sera neutralised “classical” SAgs. This “egc gap” in the SAg-neutralising antibody profiles of healthy individuals was unexpected, since egc SAgs are by far the most prevalent SAgs. We could demonstrate that the “egc gap” is probably not due to different T cell activating properties of egc SAgs compared to classical SAgs, but rather to a differential regulation of SAg gene expression. S. aureus carriers have an increased risk of developing an S. aureus bacteraemia, which is in most cases caused by the colonising strain. Intriguingly, a large prospective clinical trial revealed a considerably higher mortality in noncarriers with invasive S. aureus strains compared to carriers with invasive disease. To explain these paradoxical findings, we hypothesised that in carriers partial immunity against the colonising strain may contribute to their improved outcome. We used SAgs as strain-specific indicator antigens. Importantly, sera from persistent carriers neutralised SAgs of their colonising strain with significantly higher efficiency than sera from noncarriers. This antibody response was strain-specific, since the antibody response of carriers against other SAgs did not differ from that of noncarriers. Thus, colonisation with S. aureus confers a strong and strain-specific antibody response against staphylococcal SAgs. We suggest that in carriers neutralising antibodies directed against SAgs and other staphylococcal virulence factors confer partial protection during systemic infections. This could explain the better prognosis of carriers with S. aureus bacteraemia compared to noncarriers. Moreover, our data imply that the key to understanding the pathogenesis of S. aureus disease may lie in the identification of host factors rather than bacterial factors. Such host factors could be the immune status and gene polymorphisms that contribute to colonisation, susceptibility to infection and outcome of infection. Finally, while the treatment of S. aureus bacteraemia with pooled immunoglobulins was performed in the past without significant success, our findings on strain-specific antibody profiles suggest that therapies with customised cocktails of monoclonal antibodies could have a higher efficacy.
The thesis contains 6 chapter and mentions about the influences of sea level change, climate, tectonic into the sedimentary process. The results show that late Pleistocene facies mostly are weathered facies which content gibbsite-kaolinite, limonite. In transgression, facies assemblage includes lagoon, tidal and estuary. The composition are in-situ reworked minerals like illite, gypsum. In regression, facies are shallow marine, prodelta, delta front, distributary lobe, swamp, tidal and beach, channel infill, flood plain, lake. Abundant minerals are named like smectite, illite, chlorite, quartz, feldspar, rock fragments, gypsum.Gypsum is the evaporited mineral easily to be formed in coastal environment of Red River Delta. It is a good indicative mineral for distinguishing the deposits formed in dry season of monsoon regions. Smectite is good indicative mineral for sea environment which mostly related with the transference and low accumulation and new formed in climate with wet and dry periods. Kaolinite-gibbsite is an indicator of strong chemical weathering with high precipitation. The stratigraphy can be divide into trangressive systems tract (10-8.5 cal. kyr BP) and highstand systems tract with aggradational-progradational parasequence set (8.5-6.5 cal. kyr BP) and progradational parasequence set (6.5 cal. kyr BP-today, with subsets 6.5-4.0; 4.0-1.5; and 1.5-0.0 cal. kyr BP). The subsidence process which reflex in accumulation rate regarded to not only sea level change, tectonics but also human impact - dyke build plays the main role to increased sedimentary thickness. The influence of source variation and climate change are recorded on mineral composition. In late Pleistocene, materials are chemical weathering authigenic components during warm/wet climate. In transgression, dominated materials are reworked terrigenous and chemical weathering components during warm/dry and cool/wet climate. In regression, materials are low maturity, suffered by physical weathering transported from surrounding mountains during 3 warm/dry or wet - cool/dry or wet big climate cycles.