Refine
Year of publication
- 2014 (86) (remove)
Document Type
- Doctoral Thesis (86) (remove)
Language
- English (86) (remove)
Has Fulltext
- yes (86) (remove)
Is part of the Bibliography
- no (86)
Keywords
- Beschleuniger (2)
- Radio Frequenz Quadrupol (2)
- 1,4-dioxane (1)
- ADHD (1)
- Ageing (1)
- Allergie (1)
- Birkenpollen (1)
- Branch and Bound (1)
- Chikungunya (1)
- Chinese river basins, water withdrawals, dam construction, river flow alteration, flow indicators, fish species richness, fish catch, riparian vegetation cover, quantitative analysis (1)
Institute
- Physik (25)
- Biochemie und Chemie (14)
- Biowissenschaften (13)
- Informatik (7)
- Geowissenschaften (6)
- Mathematik (5)
- Pharmazie (4)
- Institut für Ökologie, Evolution und Diversität (3)
- Biochemie, Chemie und Pharmazie (2)
- Psychologie (2)
Drought stress is one of the major abiotic factors diminishing crop productivity world wide. In the course of climate change, regions which already experience dry seasons nowadays will suffer from elongated drought periods and water shortage. These climatic changes will not only have an impact on the regional flora and fauna but also on the people inhabiting these areas. It is therefore of great importance to understand the reactions of plants to drought stress to help breeding and biotechnological approaches for the benefit of new robust cereal cultures growing under low water regimes. In this dissertation four grasses of the genus Panicum, P. bisulcatum (C3), P. laetum, P. miliaceum and P. turgidum (all C4 NAD-ME) were subjected to drought stress. The plants diverse reactions were investigated on a physiological as well as on a molecular level to deepen the understanding of drought stress responses. Drought stress was imposed for a species-specific period until a relative leaf water content (RWC) of ~50 % was reached in each grass. Physiological measurements were conducted on leaves with a RWC of ~50 % investigating chlorophyll a fluorescence parameters with a Plant Efficiency Analyzer (PEA) and gas exchange parameters like the photosynthesis rate and stomatal conductance with a Gas Fluorescence Chamber (GFS-3000). Subsequent molecular analysis were conducted on leaf samples taken (RWC = 50 %) analysing different proteins and the transcriptome of the Panicum species. The physiological measurements revealed a higher photosynthesis rate for the C4 grasses under drought stress with no significant differences between the C4 species. Also the water use efficiency was significantly higher in the C4 species in comparison to the C3 species independent from the water regime supporting results from the literature. The chlorophyll a measurements revealed the strongest adaptation to water shortage in the C4 species P. turgidum followed by the C3 species P. bisulcatum. It has been shown before (GHANNOUM 2009) that the C4 photosynthesis apparatus is more prone to drought stress than the C3 apparatus – despite the higher water use efficiency. Results also suggested that the great adaptation of P. turgidum to drought stress arose from its ability to recover from drought stress (all JIP test parameters showed no significant differences between control and recovery samples). The additional down-regulation of PS II but not of PS I under drought stress also helped the plant to endure times of water shortage and facilitated the recovery when water was available again. Protein analyses on the content of PEPC, OEC and RubisCO (LSU and SSU) revealed no changes. Dehydrin 1 in contrast was strongly up-regulated under drought stress and Summary 108 recovery in all four Panicum species. The stable content of the OEC protein was therefore not the catalyst of rising K peaks measured by chlorophyll a fluorescence and a reduced OEC activity was supposed. Transcriptomic analyses revealed a myriad of differentially regulated tags. Due to unsequenced genomes, tags could only be partially (8 % maximum for P. turgidum) annotated to their specific genes. Diverse methods were therefore used to annotate the most highly regulated tags to their genes and their products. Special emphasis was put on the regulation of five gene products confirming the regulation schemata from the HT-SuperSAGE analyses. Interestingly one protein – the NCED1 – was down-regulated under stress conditions, in contrast to results from the literature. It is therefore of great importance to investigate longer lasting drought to understand the full range of drought stress adaptation. Future genome sequencing projects might also include the Panicum species investigated in this dissertation and important gene candidates with no hits (maybe completely new to the research community) might help breeding and biotechnology approaches to produce more drought resistant crop species.
The PANDA experiment at FAIR will perform world class physics studies using high-intensity cooled antiproton beams with momenta between 1.5 and 15 GeV/c. A rich physics program requires very good particle identification (PID). Charged hadron PID for the barrel section of the target spectrometer has to cover the angular range of 22-140° and separate pions from kaons for momenta up to 3.5 GeV/c with a separation power of at least 3 standard deviations. The system that will provide it has to be thin and operate in a strong magnetic field. A ring imaging Cherenkov detector using the DIRC principle meets those requirements. The design of the PANDA Barrel DIRC is based on the successful BABAR DIRC counter with several important changes to improve the performance and optimize the costs. The design options are being studied in detailed Monte Carlo simulation, and implemented in increasingly complex system prototypes and tested in particle beams. Before building the full system prototypes the radiator bars and lenses are measured on the test benches. The performance of the DIRC prototype was quantified in terms of the single photon Cherenkov angle resolution and the photon yield. Results for two full system prototypes will be presented. The prototype in 2011 aimed at investigating the full size expansion volume. It was found that the resolution for this configuration is at the level of in good agreement with ray tracing simulation results. A more complex prototype, tested in 2012, provided the first experience with a compact fused silica prism expansion volume, a wide radiator plate, and several advanced lens options for the focusing system. The performance of the baseline configuration of the prototype with a standard lens and an air gap met the requirements for the PANDA PID for most of the polar angle range but failed at polar angles around 90° due to photon loss at the air gap. Measurements with a prototype high-refractive index compound lens without an air gap at a polar angle of 128° beam angle showed a good resolution of σΘC = 11.8 ± 0.7 mrad and a high photon yield of Nph = 26.1 ± 0.4. Even at polar angles close to 90° the photon yield with this lens exceeded 15 detected photons per particle, meeting the PANDA Barrel DIRC PID requirements for the entire phase space and demonstrating that the compact focusing DIRC is a very promising option for PANDA.
This study describes the Holocene sedimentary lagoonal deposition history, including event sedimentation and benthic foraminiferal analyzes, from about 10 kyrs BP until today. This is the first study describing the sedimentation of a Maldivian atoll lagoon in such detail. Thirty-nine sediment cores have been recovered from the deep Rasdhoo Atoll lagoon of the Maldives (4°N/73°W). Seventeen sediment cores were opened, described, and 296 sediment samples have been collected and analyzed. Different methods have been used to evaluate the coarse- and fine-grained carbonate components and a total of fifty-eight samples have been dated radiometrically by Beta Analytic Inc., Miami, Florida. In general, the Rasdhoo Atoll lagoon sediments can be divided into (1) a Late Pleistocene soil, (2) an early Holocene peat layer composed of mangrove deposits which mark the beginning inundation of the atoll lagoon by the rising Holocene sea-level at 10,320 ± 100 yrs BP, and (3) carbonate sediments starting to fill up the lagoon 7850 ± 140 yrs BP until today. The transition from peat to carbonate is characterized by a considerable hiatus. Six different carbonate sediment facies are classified by statistical analyses, listed in decreasing abundance:
(1) mollusk-coral-algal floatstone to rudstone (30%)
(2) mollusk-coral-red algae rudstone (23%)
(3) mollusk-coral-algal wackestone to floatstone (23%)
(4) mollusk-coral wackestone (13%)
(5) mollusk-coral mudstone to wackestone (9%)
(6) mollusk mudstone (2%)
Based on grain-sizes in combination with coral identification, the facies represent both lagoonal background sedimentation (mostly fine-grained sediments (matrix >50%)) and event sedimentation (coarse-grained sediment layers composing reefal components).
Six coarser grained layers in muddy background sediments of the Rasdhoo Atoll lagoon were interpreted as Holocene tsunami events, based on the increase of allochthonous skeletal material with shallow-water reef affinity such as fragments of shallow-water coral species, coralline red algae, and reef-dwelling foraminifera in these layers, as well as AMS dating:
• Event 1: 420 - 890 yrs BP (655 yrs BP)
• Event 2: 890 - 1560 yrs BP (1225 yrs BP)
• Event 3: 2040 - 2340 yrs BP (2190 yrs BP)
• Event 4: 2420 - 3380 yrs BP (2900 yrs BP)
• Event 5: 3890 - 4330 yrs BP (4110 yrs BP)
• Event 6: 5480 - 5760 yrs BP (5620 yrs BP)
Five of the six layers may be correlated to previously published tsunami events at adjacent coastal research sites. The mid-late Holocene atoll lagoon archive is incomplete though based on the assumption that major earthquakes at the Indonesian subduction zone generated more than six major tsunamis during the past 6.5 kyrs.
According to Gischler (2006), the sediments of the Rasdhoo Atoll lagoon can be divided into two areas: (1) a central to marginal deep lagoon with a lateral west-to-east gradient of sediment facies distribution, visible in sections <4 kyrs BP with sedimentary facies of mudstone to wackestone in the western part (e.g., cores 16, 18, and 34) and coarse-grained coral and algal-rich sediments in the eastern part of the lagoon (e.g., cores 30 and 31). (2) A northern enclosed and shallow area between the sand apron and the sand spit accumulating “sandy” sediments of wackestone facies (cores 2, 19, 25, and 26).
Comparing the sediment accumulation data of the lagoon with two reconstructed local sea-level curves, three different sequence-stratigraphical systems tracts are visible: (1) a lowstand systems tract (LST) >10 kyrs BP. Pleistocene brownish soil superposing subaerially exposed Pleistocene reef limestone. (2) A transgressive systems tract (TST) 10-6.5 kyrs BP. A peat layer marks the beginning of the inundation, and the carbonate sedimentation starts with very low sedimentation rates of 0.02 m/kyr. (3) A highstand systems tract (HST) 6.5-0 kyrs BP, further divided into three stages (6.5-3, 3-1, 1-0 kyrs BP). The sea-level rise slowed down, sedimentation rates are increasing continuously up to a maximum of 1.4 m/kyr, the sand spit developed some 4 kyrs BP, the lagoonal circulation got restricted, and the lateral west-to-east gradient of grain-size accumulation started. From 1-0 kyrs BP the sedimentation rates slowed down to modern mean sedimentation rates of 0.6 m/kyr.
Two cores, one core from the center of the lagoon (core 16) and one core from the northern margin of the lagoon (core 19), have been analyzed on diversity and assemblages of benthic foraminifera in high-resolution. The transitions of Ammonia spp. to a more even and diverse fauna marks a significant environmental change at 7.0 kyrs BP in core 16 (onset of a stable environment in the deep lagoon after the sea-level rise slowed down at HST stage 1) and at 4.0 kyrs BP in core 19. A continuing environmental change after 1.4 kyrs BP in core 16 caused the fauna to become more even, a recovery of diversity and a permanent decline of foraminiferal accumulation rate. The changes in the faunas at 4.0 kyrs BP and at 1.4 kyrs BP could be explained with the sand spit formation in the northwestern and western lagoon. The sand spit has apparently acted as an obstacle in lagoonal circulation and might have caused unstable environmental conditions due to a more rapid circulation at the shallow marine site of core 19 and a slowdown of bottom water circulation in the main lagoon (core 16) leading to higher residence times and to lower oxygen and higher nutrient concentrations.
Der Radiofrequenzquadrupol (RFQ) wird typischerweise als erstes beschleunigendes Element in Beschleunigeranlagen eingesetzt. Das elektrische Quadrupolfeld ermöglicht die gleichzeitige Fokussierung und Beschleunigung des Ionenstrahls. Zudem ist der RFQ in der Lage den Gleichstromstrahl von der Ionenquelle zu Teilchenpaketen (Bunche) zu formen, die von den nachfolgenden Driftröhrenbeschleunigern benötigt werden. Ziel der vorliegenden Arbeit war die Untersuchung zur Realisierbarkeit eines 325 MHz 4-rod RFQ Beschleunigers. Die Frequenz von 325 MHz stellt eine ungewöhnlich hohe Betriebsfrequenz für die 4-rod Struktur dar und wird z.B. für den Protonenlinac des FAIR Projektes benötigt. Ein Problem hierbei war, dass durch die bauartbedingten unsymmetrischen Elektrodenaufhängung und der hohen Frequenz ein, das Quadrupolfeld überlagerndes, Dipolfeld erzeugt wird. Dieses störende Feld kann z.B. zu einem Versatz der Strahlachse führen. Hierzu wurde die 4-rod Struktur in Simulationen grundlegend auf Einflüsse von verschiedenen Parametern auf die Resonanzfrequenz und das Dipolfeld untersucht. Es wurden Lösungsstrategien erarbeitet das Diopolfeld zu kompensieren und auf einen Prototypen angewendet. Zudem wurde das Verhalten höherer Schwingungsmoden dieser Struktur simuliert. In diesem Rahmen wurden auch Simulationen zu Randfeldern zwischen den 4-rod Elektroden und der Tankwand untersucht, um nachteilige Effekte für die Strahlqualität auszuschließen. Basierend auf den Simulationsergebnissen wurde ein Prototyp angefertigt. Dieser Prototyp wurde zur Demonstration der Betriebseigenschaften mit Leistungen bis 40 kW getestet. Hierbei wurde die Elektrodenspannung mittels Gammaspektroskopie bestimmt und daraus die Shuntimpedanz berechnet. Diese Werte wurden mit anderen Methoden der Shuntimpedanzbes- timmung verglichen. Außerdem wurden alternative RFQ Resonatorkonzepte ebenfalls auf ihre Realisierbarkeit für den Protonenlinac untersucht. Die Einflüsse verschiedener Parameter auf die Betriebsfrequenz, die Möglichkeiten des Frequenztunings und der Einstellung der longitudinalen Spannungsverteilung gefertigter Modelle wurden in einer Diskussion gegenübergestellt.
Evolutionary genetics of bears and red foxes over phylogenetic and phylogeographic time scales
(2014)
Climatic fluctuations during the Pleistocene (2.6-0.01 million years) have played an important role during evolution of many species. Cyclic range contractions and expansions had demographic consequences within species, provided environmental conditions for population divergence and speciation and enabled secondary contact and interspecific hybridization. These and other evolutionary processes have left genetic signatures in the genomes of affected organisms. Comprehensive and unbiased estimates of evolutionary processes can be obtained using genetic markers from different parts of the genome and by integrating population genetic and phylogenetic concepts.
Suitable for studies on evolutionary processes and patterns over different evolutionary time scales are bears (Ursidae) and foxes (Vulpes), which occupy a wide range of habitats and evolved during the past few millions of years. In my thesis, I therefore used bears and red foxes as study species to investigate the genetic variation within and between species and to obtain estimates of evolutionary relationships and divergence times of populations and species that I interpreted in a climatic context. Further, I investigated population genetic processes during the evolution of bears. My thesis includes three publications and one submitted manuscript, spanning different evolutionary time scales - from evolutionary relationships and processes among species (phylogenetic time scales, Publications I & II), among populations and closely related species in a geographical context (phylogeographic time scales, Publications II & III), to ongoing processes within species (population genetic time scales, Publication IV).
In Publication I (Kutschera et al. 2014, Mol Biol Evol 31(8):2004-2017), I studied bears at several nuclear markers from several individuals per species, complemented with markers from the Y chromosome. Using approaches based on a population genetic concept (coalescent theory) I obtained a species tree with divergence time estimates. Further, I studied two evolutionary processes in bears, interspecific gene flow and incomplete lineage sorting (ILS). This study contributed to the growing evidence that population genetic processes can be relevant on time scales up to several millions of years.
In Publication II (Hailer, Kutschera et al. 2012, Science 336(6079):344-347), we complemented previous mitochondrial (mt) DNA-based inference of the evolutionary history of polar and brown bears with nuclear DNA. Coalescence-based species tree analyses of multiple nuclear markers from several individuals per species placed polar bears as sister lineage to brown bears and their divergence time to about 600 thousand years ago (ka). This contrasted previous mtDNA-based inference. We explained this discrepancy between mtDNA and nuclear DNA with interspecific gene flow between polar and brown bears.
In Publication III (Kutschera et al. 2013, BMC Evol Biol 13:114), I studied range-wide phylogeographic events and their timing in red foxes. A synthesis of newly generated and published mtDNA sequences was analyzed using a coalescence-based approach with multiple fossil calibration points. Thereby, I validated the identity and geographic distribution of several red fox lineages and showed that red foxes colonized North America and Japan several times independently during the late Pleistocene (126-11 ka) and around the last glacial maximum (26.5-19 ka). In a comparison of my results from red foxes to brown bears and grey wolves, I identified similar phylogeographic patterns.
In Publication IV (Kutschera et al., submitted to Biol Conserv), I found similar levels of genetic variability in vagrant polar bears that had reached Iceland compared to established subpopulations from across the range. Based on climate projections reported by the Intergovernmental Panel on Climate Change in 2014, polar bear habitat will markedly decline and become increasingly fragmented within the next decades. Dispersal will play an important role by connecting isolated subpopulations, thereby maintaining genetic diversity levels. My results indicate that vagrants could stabilize genetic variability when immigrating into established subpopulations.
In conclusion, my thesis provided a deeper understanding of evolutionary genetic processes and patterns and their timing in bears and red foxes in a climatic context, which can have conservation implications. Further, I showed that processes like ILS and interspecific gene flow can be relevant over different time scales and are important aspects of evolutionary history. Thereby, my thesis contributed to the knowledge on the evolutionary history of several carnivore species and on evolutionary processes acting within and between closely related species.
Understanding major causes of biodiversity and range dynamics requires research on evolutionary processes under consideration of environmental changes. In my thesis, I investigated the spatio-temporal evolution of the Neotropical tree genus Cedrela from the Meliaceae family by studying its genetic diversity, taxonomy, colonization history, climatic niche changes and dynamics of species distributions. My results show that climatic and geological changes are major drivers of biological diversification in Cedrela.
This thesis serves two main purposes:
1. The introduction of a novel experimental method to investigate phase change dynamics of supercooled liquids
2. First-time measurements for the crystallization behaviour for hydrogen isotopes under various conditions
1) The new method is established by the synergy of a liquid microjet of ~ 5 µm diameter and a scattering technique with high spatial resolution, here linear Raman spectroscopy. Due to the high directional stability and the known velocity of the liquid filament, its traveling axis corresponds to a time axis static in space. Utilizing evaporative cooling in a vacuum environment, the propagating liquid cools down rapidly and eventually experiences a phase transition to the crystalline state. This temporal evolution is probed along the filament axis, ultimately resulting in a time resolution of 10 ns. The feasibility of this approach is proven successfully within the following experiments.
2) A main object of study are para-hydrogen liquid filaments. Raman spectra reveal a temperature gradient of the liquid across the filament. This behaviour can quantitatively be reconstructed by numerical simulations using a layered model and is rooted in the effectiveness of evaporative cooling on the surface and a finite thermal conductivity. The deepest supercoolings achieved are ~ 30% below the melting point, at which the filament starts to solidify from the surface towards the core. With a crystal growth velocity extracted from the data the appropriate growth mechanism is identified. The crystal structure that initially forms is metastable and probably the result of Ostwald’s rule of stages. Indications for a transition within the solid towards the stable equilibrium phase support this interpretation.
The analog isotope ortho-deuterium is evidenced to behave qualitatively similar with quantitative differences being mass related.
In further measurements, isotopic mixtures of para-hydrogen and ortho-deuterium are investigated. It is found that the crystallization process starts earlier and lasts significantly longer compared to the pure substances with the maximum values between 20-50% ortho-deuterium content. A solely temperature based explanation for this effect can be excluded. The difference in the quantum character and hence effective size of the isotopes suggests a strong influence of the progressing liquid-solid-interface. Small dilutions of each para-hydrogen and ortho-deuterium with neon show an even more extended crystallization process compared to above isotopic mixtures. Additionally, the crystal is strongly altered in favor of the equilibrium lattice structure of neon.
Die zentralen Objekte der Dissertation sind Translationsflächen. Dabei handelt es sich um Riemann’sche Flächen, die aus in die euklidische Ebene eingebetteten Polygonen durch Verkleben von parallelen gleichlangen Seiten entstehen. Zwei Translationsflächen sind gleich, wenn es möglich ist, die Polygone durch ”Zerschneiden und mittels Translationen neu Zusammenkleben“ ineinander zu überführen. Die Gruppe GL_2(R) operiert auf der Menge der Translationsflächen via der linearen Abbildungen auf den Polygonen. Der Stabilisator einer Translationsfläche X unter dieser Operation wird die Veech-Gruppe von X genannt und mit SL(X) bezeichnet. Die Veech-Gruppe ist eine diskrete Untergruppe von SL_2(R) und damit eine Fuchs’sche Gruppe.
Fuchs’sche Gruppen werden je nach ihrer Limesmenge in elementare und nicht-elementare Gruppen eingeteilt. Letztere wiederum unterteilt man in Gruppen erster oder zweiter Art. Fuchs’sche Gruppen mit endlichem co-Volumen heißen Gitter und sind genau die endlich erzeugten Gruppen erster Art. Translationsflächen, deren Veech-Gruppe ein Gitter ist, heißen Veech-Flächen und sind von besonderem Interesse, da für sie die Veech Alternative gilt.
Ein feineres Maß für die Größe einer Fuchs’schen Gruppe ist der kritische Exponent. Er ist definiert als das Infimum aller reellen Zahlen, für die die Poincaré Reihe konvergiert und liegt für alle unendlichen Fuchs’schen Gruppen zwischen 0 und 1. Hauptziel der Dissertation ist der Beweis von Theorem 1. Es gibt Translationsflächen, für die der kritische Exponent ihrer Veech-Gruppe echt zwischen 1/2 und 1 liegt.
Der kritische Exponent von elementaren Gruppen ist höchstens 1/2, Translationsflächen mit elementaren Veech-Gruppen sind also als Kandidaten für das Theorem ausgeschlossen. Der kritische Exponent von Gittern ist 1. Also scheiden auch Veech-Flächen für das Theorem aus.
Bis zum Jahr 2003 waren Gitter die einzigen bekannten nicht-elementaren Veech-Gruppen. McMullen klassifizierte die Veech-Flächen vom Geschlecht 2 und zeigte, dass jede solche Fläche, die nur eine Singularität besitzt, in der GL_2(R)-Bahn der Fläche L_D liegt, die aus einem L-förmigen Polygon mit geeigneten von D abhängigen Seitenlängen entsteht.
Während auch heute noch keine Translationsfläche mit Veech-Gruppe zweiter Art bekannt ist, fanden McMullen und unabhängig davon Hubert und Schmidt Konstruktionen unendlich erzeugter Veech-Gruppen erster Art. Eine Abschätzung des kritischen Exponenten dieser Gruppen war 10 Jahre lang eine wichtige offene Frage, die nun durch Theorem 1 beantwortet wird.
Zentral in der Konstruktion von Hubert und Schmidt sind spezielle Punkte, nämlich Verbindungspunkte. Hubert und Schmidt konstruieren Translationsflächen, deren Veech-Gruppen kommensurabel zum Stabilisator SL(X;P) von P sind und damit den gleichen kritischen Exponenten haben. Für Verbindungspunkte mit unendlicher SL(X)- Bahn (diese Punkte heißen nicht-periodisch) ist SL(X;P) unendlich erzeugt und von erster Art.
Wir zeigen Theorem 1, indem wir zeigen, dass für jedes D kongruent 0 mod 4, (kein Quadrat), und jeden nicht-periodischen Verbindungspunkt P in L_D der kritische Exponent der Gruppe SL(L_D;P) echt zwischen 1/2 und 1 liegt.
Eine natürliche Frage in diesem Zusammenhang ist die Abhängigkeit von P: Punkte Q in der SL(L_D)-Bahn von P sind auch er nicht-periodische Verbindungspunkte und die zugehö̈rigen Gruppen SL(L_D;P) und SL(L_D;Q) sind konjugiert zueinander. Daher widmen wir uns in Kapitel 4 der Bestimmung der Bahnen nicht-periodischer Verbindungspunkte.
Die Verbindungspunkte haben die Form P=(x_r+x_iw;y_r+y_iw) mit x_r,x_i,y_r,y_i aus Q. Wir zeigen, dass der Hauptnenner N(P) dieser (gekürzten) Brüche eine Invariante der Bahn ist. Daraus folgt:
Theorem 2. Es gibt unendlich viele verschiedene Bahnen von Verbindungspunkten von L_D.
Wir kennen die Operation der horizontalen und der vertikalen Scherungen A und B aus SL(L_D). Im Spezialfall D=8 erzeugen diese beiden Elemente die ganze Gruppe und wir geben je ein Verfahren an, um eine untere und eine obere Schranke an die Anzahl der Bahnen von nicht-periodischen Verbindungspunkten P mit fixiertem Hauptnenner N(P) zu finden. Damit zeigen wir:
Theorem 3. Die Menge der Verbindungspunkte P mit festem Wert N(P) zerfällt in eine endliche Anzahl von SL(L_8)-Bahnen.
Im Beweis von Theorem 1 ist es nötig, die Nicht-Mittelbarkeit eines Graphen zu zeigen. Da wir nur sehr wenige Informationen über dessen Struktur in unserer konkreten Situation haben, entwickeln wir in Kapitel 1 die folgende Methode:
Theorem 4. Sei G ein Graph, den man durch Weglassen von Kanten in einen Wald G′ ohne Blätter überführen kann, bei dem das Supremum der Längen von zusammenhängenden Valenz-2-Teilgraphen von G′ beschränkt ist. Dann ist G nicht mittelbar.
Um diese Methode anzuwenden, ordnen wir jeder Ecke P von G ein Komplexitätsmaß s(P) zu und weisen nach, dass dieser Wert für die Operation von Worten in A- und B-Potenzen mit wachsender Wortlänge ”tendenziell wächst“.
The phylogeny of the genus Gazella and the phylogeography and population genetics of arabian species
(2014)
Biodiversity is caused by a fundamental evolutionary process: speciation. When species can spread into new habitats and are allowed to colonize new ecological niches, speciation can become accelerated and is then called radiation. This can happen, e.g., when formerly separated land masses become connected. A prime example of such a scenario is the Arabian Peninsula that connects Africa and Asia since the Oligocene (approx. 30 Ma ago). Since then, the peninsula promoted several faunal exchanges between both continents. The mammalian genus Gazella is an excellent candidate for investigating this faunal exchange. Species are distributed on both, the African and Asian continent as well as on the Arabian Peninsula that is located in between. The aim of my thesis was to cast new light on the evolution and speciation of the genus and, furthermore, to evaluate the currently problematic taxonomy to infer suggestions for improved conservation actions for threatened gazelle species. Therefore, I investigated the taxon Gazella genetically and identified factors that promoted the speciation of this diverse genus. I assessed intraspecific genetic variability for species that inhabited the Arabian Peninsula to infer the past demography of those species and to estimate the history of species divergence and past population parameters.
In the first part of my thesis I inferred a mitochondrial phylogeny based on cytochrome b gene sequences using samples of all nine extant species of Gazella and also of closely related taxa (chapter 2). Besides the monophyly of the genus Gazella two reciprocally monophyletic clades were detected that evolved in allopatry: one predominantly African and one predominantly Asian clade. Within both clades species pairs could be inferred with species being ecologically adapted to different habitats: one species is a desert-dweller (probably the ancestral character state combination), while the other one is adapted to rather mountainous and humid habitats. These adaptations also correlate with the behavior of the species with the mountainous forms being sedentary, territorial and living in small groups and the desert forms being migratory, non-territorial and living in larger herds.
The second part of my thesis focuses on the Arabian gazelle species. In a study about G. subgutturosa I could show that the Arabian form G. marica (sand gazelle)—previously recognized as a subspecies of G. subgutturosa—is genetically distinct from the nominate form (chapter 3). Moreover, a phylogenetic tree based on cytochrome b gene sequences revealed a polyphyly of G. subgutturosa and G. marica with sand gazelles being more closely related to G. leptoceros and G. cuvieri of North Africa. Consequently, I suggested the restoration to full species level for G. marica corroborating earlier conservation practices of breeding both taxa separately in captivity.
In case of G. dorcas such a genetic differentiation could not be detected (chapter 4). Despite the large distribution range from Mali in the west to Saudi Arabia in the east only low genetic variation was detectable in mitochondrial sequence data. Statistically parsimony network analyses revealed pronounced haplotype sharing across regions. Using a coalescence approach I observed a steep population decline that started about 25,000 years ago and which is still ongoing. The decline could be correlated with human hunting activities in the Sahara. Hence, hunting of G. dorcas (already in ancient times) had a much larger impact on gazelle populations than previously thought and even led to the extinction of the Arabian form of G. dorcas.
In chapter 5 of my thesis I provided a rigorous test to genetically distinguish between the potential species G. gazella and G. arabica. Previously recognized as a single species mitochondrial sequence analyses provided first hints for the separation of both taxa. But without the investigation of nuclear loci the observed pattern could also be the result of male biased dispersal combined with female philopatry. Therefore, I amplified mitochondrial sequence markers and nuclear microsatellite loci for both taxa and found support for the earlier view of two separate species. No signs of recurrent gene flow could be detected between neighboring populations of G. arabica and G. gazella. The split of both species could be estimated one million years ago and the recommendation of breeding both taxa separately in captivity for conservation purposes is fully justified.
Several populations of G. arabica suffer from a severe decline. In chapter 6 I asked whether the population occurring on the Farasan archipelago—being at stable individual numbers for decades—may serve as potential source for future reintroduction on the Arabian mainland, although the gazelles show a reduced body size. Analyzing the genetic differentiation of Farasan gazelles, a genetic cluster could be inferred being endemic to the archipelago. However, only approx. 70% of Farasan individuals were assigned to this specific cluster, while the others showed at least intermediate or even complete assignment to the mainland cluster. This indicates ongoing introgression that is probably mediated by human translocations of gazelles from and onto the islands. Considering the uniform dwarfism of Farasan gazelles, reasons for the smaller body size might be direct consequences of resource limitations, i.e., phenotypic plasticity. If the population decline on the mainland will hold on Farasan gazelles could serve as stocks for future reintroductions.
Myxobacteria are on order of Gram-negative, soil dwelling bacteria that feature an impressive number of properties: they can glide on solid surfaces by using two different motility motors, subsist by preying on other microorganisms, are often producers of multiple natural products, and upon adverse environmental conditions, they are able to form multicellular structures called “fruiting bodies”. The process, in which these macroscopically visible structures arise from independent single cells, has been the predominant subject of myxobacterial research for many decades. More precisely, researchers have strived for the discovery of genes, proteins and small molecules that act as signals, receivers or modulators of this complex process. In this regard, the species Myxococcus xanthus has evolved into the model organism due to its relatively simple and reliable handling in a laboratory environment. The research underlying this thesis focused on the identification and biosynthesis of lipids that may act as intercellular signaling molecules during the course of fruiting body formation of the myxobacterium Myxococcus xanthus as part of the “E-signal” system. In general, lipids containing branched-chain fatty acids with an uneven number of carbon atoms were found to be important players in this particular process. Nevertheless, their exact roles remain largely unknown as of this day. The first publication that is part of this thesis deals with an aspect that even strengthened the importance of role of iso-branched compounds in myxobacteria: myxobacterial metabolism is able to transform precursors of iso-lipids to isoprenoids. It addresses the question whether isoprenoids in general are important for fruiting body formation. Phenotypic analysis of mutants impaired in the biosynthesis of the central isoprenoid precursor 3-hydroxymethylglutaryl-Coenzyme A (3-HMG-CoA) from acetate and/or branched chain keto acids and their genetic and metabolic complementation clearly showed that isoprenoids are essential for fruiting body formation and confirmed that leucine derived isovalerate is an important source for isoprenoid precursors in myxobacteria. The second, and by far and away most tedious and sophisticated study, addressed the question as to how myxobacteria form fatty acid derived iso-branched ether lipids and to what extent they are important for fruiting body formation and sporulation. In a previous study, those unusual lipids were identified as specific biomarkers for myxobacterial development. No biochemical pathways to ether lipids specific for prokaryotes were known by then. In this study, a putative candidate gene that may be in involved in ether lipid biosynthesis was investigated. A combination of gene disruption and complementation experiments, phenotypic analysis and monitoring of ether lipid formation by means of GC-MS demonstrated its involvement in myxobacterial ether lipid biosynthesis and the importance of these lipids for the developmental process. Heterologous expression and biochemical testing of this gene together with in-silico sequence analysis and docking experiments confirmed the functions of its predicted domains. The discussion section provides an additional suggestion on how the ether bond formation is performed. Furthermore and most importantly, iso-branched ether lipids were found to be essential for sporulation but not for fruiting body formation. In summary, one or several molecules derived from an iso-branched alkylglycerol seem to play a role during sporulation in M. xanthus and a multidomain enzyme unique for myxobacteria is involved in their biosynthesis. The last manuscript addresses the complexity of lipid metabolism in myxobacteria. Prior to this work, there was limited knowledge about the exact composition of the myxobacterial lipidome and no method was available to monitor putative changes in the myxobacterial lipidome down to the single molecular species for studying lipid biosynthesis or regulation. An ultra-performance liquid chromatography coupled with mass spectrometry based method with electrospray ionization (UPLC-ESI-MS) utilizing standard equipment and a water/acetonitrile/isopropanol based eluent system proved to be geared for the construction of lipid profiles for wild type and mutant cells of M. xanthus and to show their differences. Fragmentation spectra based structure elucidation of lipid molecular species resulted in the identification of 99 molecular species comprising glycerophosphoethanolamines, glycerophosphoglycerols, glycerolipids, ceramides and ceramide phosphoinositols. The latter have never been described for any prokaryotes before. Three dimensional plots were created from the relative intensity differences of the single molecular ion species between the different samples to provide an efficient and versatile visualization of the data and enable the researcher to quickly detect differences.