Populationsgenetik eisenzeitlicher Reiternomaden der Eurasischen Steppe

Vorliegende Dissertation beschäftigt sich mit der Populationsgenetik eisenzeitlicher Bevölkerungen der Eurasischen Steppe, die mit der skythischen Kultur assoziiert werden. Für die Analysen wurden 30 Fragmente der kodierenden Region und die HVR1 (16040–16400) des mitochondrialen Genoms, sowie 20 phänotypische Marker untersucht. Die Marker wurden durch Multiplex-PCRs angereichert, mit einem probenspezifischen barcode versehen und einer parallelen Sequenzanalyse mit dem 454 GS FLX Sequenzierer unterzogen. 97 Individuen wurden erfolgreich analysiert, von denen 19 aus dem Westen der Eurasischen Steppe und 78 aus dem Bereich des Altai-Gebirges stammen. Die populationsgenetischen Analysen ergaben geringe genetische Distanzen zwischen den skythischen Populationen aus dem Bereich des Altai-Gebirges, die sich vom 9. bis zum 3. Jahrhundert vor Christus erstrecken, was für eine kontinuierliche Bevölkerungsentwicklung sprechen könnte. Weiterhin finden sich geringe genetische Distanzen zwischen den Gruppen im Osten und Westen der Eurasischen Steppe, was auf eine gemeinsame Ursprungspopulation, oder zumindest Genfluss hinweisen kann. Die Ergebnisse aus dem Vergleich mit neolithischen und bronzezeitlichen Referenzpopulationen aus Zentralasien und den angrenzenden Gebieten weisen auf die Möglichkeit eines gemeinsamen zentral-asiatischen Ursprungs hin, zeigen aber auch, dass die östlichen und westlichen Gruppen der Eisenzeit jeweils zusätzlich lokalem Genfluss ausgesetzt waren. Die Allelfrequenzen der phänotypischen Marker deuten auf einen größeren europäischen Einfluss auf das östliche Zentralasien in der Eisenzeit hin, oder ansteigenden Genfluss aus Ostasien nach der Eisenzeit.

Influence of pollination and seed dispersal on the genetic population structure of two Commiphora species in Madagascar and South Africa

Pollination and seed dispersal are important ecological processes for the regeneration of plant populations and both vectors for gene exchange between plant populations. For my thesis, I studied the pollination ecology of the South African tree Commiphora harveyi (Burseraceae) and compared it with C. guillauminii from Madagascar. Both species have low visitation rates and a low number of pollinating insect species, resulting in a low fruit set. While their pollination ecology is very similar, they differ in their seed dispersal with a low seed dispersal rate in the Malagasy and a high seed dispersal rate in the South African species. This should be reflected in a stronger genetic differentiation among populations in the Malagasy than in the South African species. My results, based on AFLP markers, contradict these expectations, the overall differentiation was lower in the Malagasy (FST = 0.05) than in the South African species (FST = 0.16). However, at a smaller spatial scale (below 3 km), the Malagasy species was genetically more strongly differentiated than the South African species, which was reflected by the high inter-population variance within the sample site (C. guillauminii: 72.2 - 85.5 %; C. harveyi: 8.4 - 14.5 %). This strong differentiation could arise from limited gene flow, which was confirmed by spatial autocorrelation analyses. The shape of the autocorrelogram suggested that gene exchange between individuals occurred only up to 3 km in the Malagasy species, whereas up to 30 km in the South African species. These results on the genetic structure correspond to the expectations based on seed dispersal data. Thus, seed dispersal seems to be a key factor for the genetic structure in plant populations on a local scale.

The influence of petrogenetic processes on the composition of Ocean Island Basalts

Ocean Island Basalts (OIB) provide important information on the chemical and physical characteristics of their mantle sources. However, the geochemical composition of a generated magma is significantly affected by partial melting and/or subsequent fractional crystallization processes. In addition, the isotopic composition of an ascending magma may be modified during transport through the oceanic crust. The influence of these different processes on the chemical and isotopic composition of OIB from two different localities, Hawaii and Tubuai in the Pacific Ocean, are investigated here. In a first chapter, the Os-isotope variations in suites of lavas from Kohala Volcano, Hawaii, are examined to constrain the role of melt/crust interactions on the evolution of these lavas. As 187Os/188Os sensitivity to any radiogenic contaminant strongly depend on the Os content in the melt, Os and other PGE variations are investigated first. This study reveals that Os and other PGE behavior change during the Hawaiian magma differentiation. While PGE concentrations are relatively constant in lavas with relatively primitive compositions, all PGE contents strongly decrease in the melt as it evolved through ~ 8% MgO. This likely reflects the sulfur saturation of the Hawaiian magma and the onset of sulfide fractionation at around 8% MgO. Kohala tholeiites with more than 8% MgO and rich in Os have homogeneous 187Os/188Os values likely to represent the mantle signature of Kohala lavas. However, Os isotopic ratios become more radiogenic with decreasing MgO and Os contents in the lavas, which reflects assimilation of local crust material during fractional crystallization processes. Less than 8% upper oceanic crust assimilation could have produced the most radiogenic Os-isotope ratios recorded in the shield lavas. However, these small amounts of upper crust assimilation have only negligible effects on Sr and Nd isotopic ratios and therefore, are not responsible for the Sr and Nd isotopic heterogeneities observed in Kohala lavas. In a second chapter, fractional crystallization and partial melting processes are constrained using major and trace element variations in the same suites of lavas from Kohala Volcano, Hawaii. This inverse modeling approach allows the estimation of most of the trace element composition of the Hawaiian mantle source. The calculated initial trace element pattern shows slight depletion of the concentrations from LREE to the most incompatible elements, which indicates that the incompatible element enrichments described by the Hawaiian melt patterns are entirely produced by partial melting processes. The “Kea trend” signature of lavas from Kohala Volcano is also confirmed, with Kohala lavas having lower Sr/Nd and La/Th ratios than lavas from Mauna Loa Volcano. Finally, the magmatic evolution of Tubuai Island is investigated in a last chapter using the trace element and Sr, Nd, Hf isotopic variations in mafic lava suites. The Sr, Nd and Hf isotopic data are homogeneous and typical for the HIMU-type OIB and confirms the cogenetic nature of the different mafic lavas from Tubuai Island. The trace element patterns show progressive enrichment of incompatible trace elements with increasing alkali content in the lavas, which reflect progressive decrease in the degree of partial melting towards the later volcanic events. In addition, this enrichment of incompatible trace elements is associated with relative depletion of Rb, Ba, K, Nb, Ta and Ti in the lavas, which require the presence of small amount of residual phlogopite and of a Ti-bearing phase (ilmenite or rutile) during formation of the younger analcitic and nephelinitic magmas.

Influence of spatial constraints in non-crystalline regions on the polymer dynamics in semi-crystalline polyethylene: a solid state NMR study

A broad variety of solid state NMR techniques were used to investigate the chain dynamics in several polyethylene (PE) samples, including ultrahigh molecular weight PEs (UHMW-PEs) and low molecular weight PEs (LMW-PEs). Via changing the processing history, i.e. melt/solution crystallization and drawing processes, these samples gain different morphologies, leading to different molecular dynamics. Due to the long chain nature, the molecular dynamics of polyethylene can be distinguished in local fluctuation and long range motion. With the help of NMR these different kinds of molecular dynamics can be monitored separately. In this work the local chain dynamics in non-crystalline regions of polyethylene samples was investigated via measuring 1H-13C heteronuclear dipolar coupling and 13C chemical shift anisotropy (CSA). By analyzing the motionally averaged 1H-13C heteronuclear dipolar coupling and 13C CSA, the information about the local anisotropy and geometry of motion was obtained. Taking advantage of the big difference of the 13C T1 relaxation time in crystalline and non-crystalline regions of PEs, the 1D 13C MAS exchange experiment was used to investigate the cooperative chain motion between these regions. The different chain organizations in non-crystalline regions were used to explain the relationship between the local fluctuation and the long range motion of the samples. In a simple manner the cooperative chain motion between crystalline and non-crystalline regions of PE results in the experimentally observed diffusive behavior of PE chain. The morphological influences on the diffusion motion have been discussed. The morphological factors include lamellar thickness, chain organization in non-crystalline regions and chain entanglements. Thermodynamics of the diffusion motion in melt and solution crystallized UHMW-PEs is discussed, revealing entropy-controlled features of the chain diffusion in PE. This thermodynamic consideration explains the counterintuitive relationship between the local fluctuation and the long range motion of the samples. Using the chain diffusion coefficient, the rates of jump motion in crystals of the melt crystallized PE have been calculated. A concept of "effective" jump motion has been proposed to explain the difference between the values derived from the chain diffusion coefficients and those in literatures. The observations of this thesis give a clear demonstration of the strong relationship between the sample morphology and chain dynamics. The sample morphologies governed by the processing history lead to different spatial constraints for the molecular chains, leading to different features of the local and long range chain dynamics. The knowledge of the morphological influence on the microscopic chain motion has many implications in our understanding of the alpha-relaxation process in PE and the related phenomena such as crystal thickening, drawability of PE, the easy creep of PE fiber, etc.

Factorization and non-local 1/m b corrections in the decay B X s gamma

In this thesis, a systematic analysis of the bar B to X_sgamma photon spectrum in the endpoint region is presented. The endpoint region refers to a kinematic configuration of the final state, in which the photon has a large energy m_b-2E_gamma = O(Lambda_QCD), while the jet has a large energy but small invariant mass. Using methods of soft-collinear effective theory and heavy-quark effective theory, it is shown that the spectrum can be factorized into hard, jet, and soft functions, each encoding the dynamics at a certain scale. The relevant scales in the endpoint region are the heavy-quark mass m_b, the hadronic energy scale Lambda_QCD and an intermediate scale sqrt{Lambda_QCD m_b} associated with the invariant mass of the jet. It is found that the factorization formula contains two different types of contributions, distinguishable by the space-time structure of the underlying diagrams. On the one hand, there are the direct photon contributions which correspond to diagrams with the photon emitted directly from the weak vertex. The resolved photon contributions on the other hand arise at O(1/m_b) whenever the photon couples to light partons. In this work, these contributions will be explicitly defined in terms of convolutions of jet functions with subleading shape functions. While the direct photon contributions can be expressed in terms of a local operator product expansion, when the photon spectrum is integrated over a range larger than the endpoint region, the resolved photon contributions always remain non-local. Thus, they are responsible for a non-perturbative uncertainty on the partonic predictions. In this thesis, the effect of these uncertainties is estimated in two different phenomenological contexts. First, the hadronic uncertainties in the bar B to X_sgamma branching fraction, defined with a cut E_gamma > 1.6 GeV are discussed. It is found, that the resolved photon contributions give rise to an irreducible theory uncertainty of approximately 5 %. As a second application of the formalism, the influence of the long-distance effects on the direct CP asymmetry will be considered. It will be shown that these effects are dominant in the Standard Model and that a range of -0.6 < A_CP^SM < 2.8 % is possible for the asymmetry, if resolved photon contributions are taken into account.

Influence of the chemokine CXCL12 on the progression and the signaling in colorectal cancer

Das Chemokin CXCL12 (auch bekannt als SDF-1) ist ein kleines Protein (8-14) KDa, das in sechs Isoformen exprimiert wird (SDF-1α, SDF-1β, SDF-1γ, SDF- 1δ, SDF-1ε und SDF-1θ) von einem einzigen Gen, dass die Leukozyten-Wanderung regelt und variabel in einer Reihe von normalen und Krebsgeweben exprimiert wird.rnCXCL12 spielt verschiedene Rollen in der Tumorpathogenese. Es wurde nachgewiesen, dass CXCL12 das Tumorwachstum und die Malignität fördert, die Tumorangiogenese stärkt, sich an der Metastasierung beteiligt und zu immunsuppressiven Netzwerken innerhalb des Tumormikromilieus beiträgt. Daher liegt es nahe, dass der CXCL12/CXCR4-Signalweg ein wichtiges Ziel ist für die Entwicklung von neuartigen Krebstherapien.rnUm Licht auf die Rolle der Chemokin CXCL12 Splicevarianten in der Entwicklung von Krebs zu werfen und die mögliche physiologische Relevanz und ihre möglichen funktionellen Unterschiede bei Darmkrebs zu verstehen, haben wir alle CXCL12 Splicevarianten (alpha, beta, gamma, delta, epsilon und theta) in die kolorektalen Zelllinie SW480 und die Melanomzellinie D05 transfiziert und exprimiert.rnrnDiese Arbeit wurde erstellt, um die folgenden Ziele zu erreichen. Untersuchung der Rolle von CXCL12 Splicevarianten bei der Vermittlung von Tumorprogression, Adhäsion, Migration, Invasion und Metastasierung von Darmkrebs. Untersuchung, ob die CXCL12 Variantenwege ein wichtiges Ziel für die Entwicklung von Krebstherapien darstellen.rn• Um eine in vivo Mausmodell zu entwickeln, um die Rolle der CXCL12 Varianten im Rahmen des Tumorwachstums zu verstehen.rnrnUnsere Ergebnisse zeigen, dass:Der CXCL12 G801A Polymorphismus ist ein Low-Penetranz Risikofaktor für die Entwicklung von Darmkrebs. Der CXCL12-Gen-Polymorphismus rs1801157 ist mit dem T-Status (Tumor-node-Metastasen) assoziiert. Es gab keine Beziehung zwischen CXCL12-Gen-Polymorphismus rs1801157 und Fernmetastisen oder LN metastasen. Alle sechs CXCL12 Splicevarianten werden im Darmkrebs und in gesunder Kolon mucosa exprimiert. Die höchste Expression wird bei SDF-1alpha, dann SDF-1 beta gefunden. Alle sechs CXCL12 Varianten zeigen erhöhte Tumorzellproliferation in vitro. SDF-1beta, gefolgt von SDF-1alpha zeigte die größte Aktivität im Proliferationsassay.rn• Alle sechs CXCL12 Varianten induzieren die Tumorzelladhäsion.SDF-1beta dann SDF-1alpha zeigte die größte Aktivität im Rahmen des Adhäsionsassay. Alle sechs CXCL12 Varianten erhöhten die Zellmigration und Invasion von Tumorzellen in vitro. SDF-1theta und SDF-1epsilon 1theta zeigten die größte Aktivität, während die schwächste Aktivität mit SDF-1alpha und SDF-1beta beobachtet wurde. Alle sechs CXCL12 Varianten aktivieren Akt und (MAPK) Mitogen- acktivatedierte Protein kinase Wege und damit die Regulierung viele essentieller Prozesse in Tumorzellen, wie Proliferation, Migration, Invasion und Adhäsion. Es ist interessant festzustellen, dass AMD3100 die CXCL12 Splicevarianten inhibriert, die AKT-MEK-1/2-Phosphorylierung induzieren.rnDer Inhibitor AMD3100 unterdrückt stark die CXCL12 Varianten -delta, -epsilon und theta-und unterdrückt schwach CXCL12-gamma. während es keine signifikante Wirkung auf CXCL12-alpha und beta hatte. Es hat möglicherweise Auswirkungen auf mehrere große Signalwage in Bezug auf Proliferation, Migration und Invasions.rn• Es ist wichtig anzumerken, dass die Hemmung von CXCL12-Varianten durch AMD3100 einen der möglichen Ansaätze in der Krebstherapie darstellen kann.Wir schlagen vor, dass weitere Studien erwogen werden, die wir brauchen, um die biologische Aktivität dieser neuen CXCL12 Varianten bei verschiedenen Arten von Krebs klar zu verstehen.