Chimäre Archonta?: vergleichend-morphologische Studien zur Hyolaryngealregion

Chimäre Archonta? Vergleichend-morphologische Studien zur Hyolaryngealregion. Mit Brevia zur Dental- und Tarsalmorphologie. Die Dissertation greift aus phylogenetisch-systematischer Perspektive das Problem des Primatenursprungs auf. Traditionell wurde die Überordnung Archonta (= Primates + Scandentia + Dermoptera + Chiroptera) angenommen, die aufgrund molekularer Befunde nicht mehr als valide eingestuft wird. Eine Klassifikation anhand der Superordo Euarchontoglires (= Primates + Scandentia + Dermoptera + Glires) wird derzeit bevorzugt. Beide Verwandtschaftshypothesen werden in den taxonomischen Analysen berücksichtigt, um den potentiellen Einfluss der Außengruppenwahl auf die Konstellation der Euarchonta (= Primates + Dermoptera + Scandentia) zu bestimmen. Der Schwerpunkt der Untersuchung liegt in der 3D-Rekonstruktion ontogenetischer Stadien der Hyolaryngealregion diverser Spezies der Ordnungen Artiodactyla, Chiroptera, Dermoptera, Primates, Rodentia, Scandentia und Soricomorpha. Mit AMIRA® 3.1.1 konnten basierend auf histologischen Schnittserien 18 dreidimensionale Modelle der überwiegend spätfetalen Zungenbein- und Kehlkopfregion dargestellt werden. Durch das Studium der Knorpelmorphologie und der Larynx-Myologie wurden 150 Merkmale definiert und in eine MacClade®-Datenmatrix überführt. Die auf dem Parsimonie-Prinzip basierenden PAUP®-Analysen sprechen für eine Schwestergruppenbeziehung der Primates und der Dermoptera (= Primatomorpha). Die als Chimäre titulierte Überordnung Archonta wurde als Vehikel verwendet, um die Integration der Chiropteren zu ermöglichen und die Hyolaryngealforschung zu intensivieren, da auch Echolot-Peilung verwendende Taxa Bestandteil der Untersuchung waren. Die morphologischen Ähnlichkeiten des Zungenbein- und Kehlkopfapparates zwischen der basalen Form Rousettus (Pteropodidae) und dem Dermoptera-Vertreter Cynocephalus wurden als symplesiomorphe Merkmale gedeutet. Bei der Außengruppenwahl eines Rodentia-Repräsentanten hingegen konnte in Übereinstimmung mit den molekularen Befunden und nach dem Gros der Lehrmeinung die Schwestergruppenbeziehung der Primates und der Sundatheria bestätigt werden. Zwecks eines umfassenderen Ansatzes wurden im Rahmen einer „total evidence“-Methodik dental- und tarsalmorphologische Merkmale integriert. Das Resultat der Clusteranalyse, basierend auf 263 Merkmalen, modifiziert das Zwischenergebnis und befürwortet in Übereinstimmung mit molekularen Daten als Schwestergruppe der Primaten das Taxon Sundatheria (= Dermoptera + Scandentia). Damit konnte erstmals mittels eines konsequenten phylogenetisch-systematischen Ansatzes der Primaten-Grundplan hinsichtlich der Merkmalsausstattung der Hyolaryngealregion mit 27 Merkmalen rekonstruiert werden. Der Primatenursprung kann mit dem Euarchonta-Grundplan rekonstruiert werden. Für die Sundatheria wurden 12 Grundplanmerkmale definiert

Dispersion approach to real and virtual Compton scattering

In recent years, new precision experiments have become possible withthe high luminosity accelerator facilities at MAMIand JLab, supplyingphysicists with precision data sets for different hadronic reactions inthe intermediate energy region, such as pion photo- andelectroproduction and real and virtual Compton scattering.By means of the low energy theorem (LET), the global properties of thenucleon (its mass, charge, and magnetic moment) can be separated fromthe effects of the internal structure of the nucleon, which areeffectively described by polarizabilities. Thepolarizabilities quantify the deformation of the charge andmagnetization densities inside the nucleon in an applied quasistaticelectromagnetic field. The present work is dedicated to develop atool for theextraction of the polarizabilities from these precise Compton data withminimum model dependence, making use of the detailed knowledge of pionphotoproduction by means of dispersion relations (DR). Due to thepresence of t-channel poles, the dispersion integrals for two ofthe six Compton amplitudes diverge. Therefore, we have suggested to subtract the s-channel dispersion integrals at zero photon energy($nu=0$). The subtraction functions at $nu=0$ are calculated through DRin the momentum transfer t at fixed $nu=0$, subtracted at t=0. For this calculation, we use the information about the t-channel process, $gammagammatopipito Nbar{N}$. In this way, four of thepolarizabilities can be predicted using the unsubtracted DR in the $s$-channel. The other two, $alpha-beta$ and $gamma_pi$, are free parameters in ourformalism and can be obtained from a fit to the Compton data.We present the results for unpolarized and polarized RCS observables,%in the kinematics of the most recent experiments, and indicate anenhanced sensitivity to the nucleon polarizabilities in theenergy range between pion production threshold and the $Delta(1232)$-resonance.newlineindentFurthermore,we extend the DR formalism to virtual Compton scattering (radiativeelectron scattering off the nucleon), in which the concept of thepolarizabilities is generalized to the case of avirtual initial photon by introducing six generalizedpolarizabilities (GPs). Our formalism provides predictions for the fourspin GPs, while the two scalar GPs $alpha(Q^2)$ and $beta(Q^2)$ have to befitted to the experimental data at each value of $Q^2$.We show that at energies betweenpion threshold and the $Delta(1232)$-resonance position, thesensitivity to the GPs can be increased significantly, as compared tolow energies, where the LEX is applicable. Our DR formalism can be used for analysing VCS experiments over a widerange of energy and virtuality $Q^2$, which allows one to extract theGPs from VCS data in different kinematics with a minimum of model dependence.

Global modeling of pollutant transport and deposition from anthropogenic emission hot spots on global scale

Urban centers significantly contribute to anthropogenic air pollution, although they cover only a minor fraction of the Earth's land surface. Since the worldwide degree of urbanization is steadily increasing, the anthropogenic contribution to air pollution from urban centers is expected to become more substantial in future air quality assessments. The main objective of this thesis was to obtain a more profound insight in the dispersion and the deposition of aerosol particles from 46 individual major population centers (MPCs) as well as the regional and global influence on the atmospheric distribution of several aerosol types. For the first time, this was assessed in one model framework, for which the global model EMAC was applied with different representations of aerosol particles. First, in an approach with passive tracers and a setup in which the results depend only on the source location and the size and the solubility of the tracers, several metrics and a regional climate classification were used to quantify the major outflow pathways, both vertically and horizontally, and to compare the balance between pollution export away from and pollution build-up around the source points. Then in a more comprehensive approach, the anthropogenic emissions of key trace species were changed at the MPC locations to determine the cumulative impact of the MPC emissions on the atmospheric aerosol burdens of black carbon, particulate organic matter, sulfate, and nitrate. Ten different mono-modal passive aerosol tracers were continuously released at the same constant rate at each emission point. The results clearly showed that on average about five times more mass is advected quasi-horizontally at low levels than exported into the upper troposphere. The strength of the low-level export is mainly determined by the location of the source, while the vertical transport is mainly governed by the lifting potential and the solubility of the tracers. Similar to insoluble gas phase tracers, the low-level export of aerosol tracers is strongest at middle and high latitudes, while the regions of strongest vertical export differ between aerosol (temperate winter dry) and gas phase (tropics) tracers. The emitted mass fraction that is kept around MPCs is largest in regions where aerosol tracers have short lifetimes; this mass is also critical for assessing the impact on humans. However, the number of people who live in a strongly polluted region around urban centers depends more on the population density than on the size of the area which is affected by strong air pollution. Another major result was that fine aerosol particles (diameters smaller than 2.5 micrometer) from MPCs undergo substantial long-range transport, with about half of the emitted mass being deposited beyond 1000 km away from the source. In contrast to this diluted remote deposition, there are areas around the MPCs which experience high deposition rates, especially in regions which are frequently affected by heavy precipitation or are situated in poorly ventilated locations. Moreover, most MPC aerosol emissions are removed over land surfaces. In particular, forests experience more deposition from MPC pollutants than other land ecosystems. In addition, it was found that the generic treatment of aerosols has no substantial influence on the major conclusions drawn in this thesis. Moreover, in the more comprehensive approach, it was found that emissions of black carbon, particulate organic matter, sulfur dioxide, and nitrogen oxides from MPCs influence the atmospheric burden of various aerosol types very differently, with impacts generally being larger for secondary species, sulfate and nitrate, than for primary species, black carbon and particulate organic matter. While the changes in the burdens of sulfate, black carbon, and particulate organic matter show an almost linear response for changes in the emission strength, the formation of nitrate was found to be contingent upon many more factors, e.g., the abundance of sulfuric acid, than only upon the strength of the nitrogen oxide emissions. The generic tracer experiments were further extended to conduct the first risk assessment to obtain the cumulative risk of contamination from multiple nuclear reactor accidents on the global scale. For this, many factors had to be taken into account: the probability of major accidents, the cumulative deposition field of the radionuclide cesium-137, and a threshold value that defines contamination. By collecting the necessary data and after accounting for uncertainties, it was found that the risk is highest in western Europe, the eastern US, and in Japan, where on average contamination by major accidents is expected about every 50 years.

Process-based modelling of lichens and bryophytes and their role in global biogeochemical cycles

This thesis presents a process-based modelling approach to quantify carbon uptake by lichens and bryophytes at the global scale. Based on the modelled carbon uptake, potential global rates of nitrogen fixation, phosphorus uptake and chemical weathering by the organisms are estimated. In this way, the significance of lichens and bryophytes for global biogeochemical cycles can be assessed. The model uses gridded climate data and key properties of the habitat (e.g. disturbance intervals) to predict processes which control net carbon uptake, namely photosynthesis, respiration, water uptake and evaporation. It relies on equations used in many dynamical vegetation models, which are combined with concepts specific to lichens and bryophytes, such as poikilohydry or the effect of water content on CO2 diffusivity. To incorporate the great functional variation of lichens and bryophytes at the global scale, the model parameters are characterised by broad ranges of possible values instead of a single, globally uniform value. The predicted terrestrial net uptake of 0.34 to 3.3 Gt / yr of carbon and global patterns of productivity are in accordance with empirically-derived estimates. Based on the simulated estimates of net carbon uptake, further impacts of lichens and bryophytes on biogeochemical cycles are quantified at the global scale. Thereby the focus is on three processes, namely nitrogen fixation, phosphorus uptake and chemical weathering. The presented estimates have the form of potential rates, which means that the amount of nitrogen and phosphorus is quantified which is needed by the organisms to build up biomass, also accounting for resorption and leaching of nutrients. Subsequently, the potential phosphorus uptake on bare ground is used to estimate chemical weathering by the organisms, assuming that they release weathering agents to obtain phosphorus. The predicted requirement for nitrogen ranges from 3.5 to 34 Tg / yr and for phosphorus it ranges from 0.46 to 4.6 Tg / yr. Estimates of chemical weathering are between 0.058 and 1.1 km³ / yr of rock. These values seem to have a realistic order of magnitude and they support the notion that lichens and bryophytes have the potential to play an important role for global biogeochemical cycles.