Palaeo wind system reconstruction of the last glacial period over Europe, using high resolution proxy data and model-data-comparison

The atmosphere is a global influence on the movement of heat and humidity between the continents, and thus significantly affects climate variability. Information about atmospheric circulation are of major importance for the understanding of different climatic conditions. Dust deposits from maar lakes and dry maars from the Eifel Volcanic Field (Germany) are therefore used as proxy data for the reconstruction of past aeolian dynamics.rnrnIn this thesis past two sediment cores from the Eifel region are examined: the core SM3 from Lake Schalkenmehren and the core DE3 from the Dehner dry maar. Both cores contain the tephra of the Laacher See eruption, which is dated to 12,900 before present. Taken together the cores cover the last 60,000 years: SM3 the Holocene and DE3 the marine isotope stages MIS-3 and MIS-2, respectively. The frequencies of glacial dust storm events and their paleo wind direction are detected by high resolution grain size and provenance analysis of the lake sediments. Therefore two different methods are applied: geochemical measurements of the sediment using µXRF-scanning and the particle analysis method RADIUS (rapid particle analysis of digital images by ultra-high-resolution scanning of thin sections).rnIt is shown that single dust layers in the lake sediment are characterized by an increased content of aeolian transported carbonate particles. The limestone-bearing Eifel-North-South zone is the most likely source for the carbonate rich aeolian dust in the lake sediments of the Dehner dry maar. The dry maar is located on the western side of the Eifel-North-South zone. Thus, carbonate rich aeolian sediment is most likely to be transported towards the Dehner dry maar within easterly winds. A methodology is developed which limits the detection to the aeolian transported carbonate particles in the sediment, the RADIUS-carbonate module.rnrnIn summary, during the marine isotope stage MIS-3 the storm frequency and the east wind frequency are both increased in comparison to MIS-2. These results leads to the suggestion that atmospheric circulation was affected by more turbulent conditions during MIS-3 in comparison to the more stable atmospheric circulation during the full glacial conditions of MIS-2.rnThe results of the investigations of the dust records are finally evaluated in relation a study of atmospheric general circulation models for a comprehensive interpretation. Here, AGCM experiments (ECHAM3 and ECHAM4) with different prescribed SST patterns are used to develop a synoptic interpretation of long-persisting east wind conditions and of east wind storm events, which are suggested to lead to an enhanced accumulation of sediment being transported by easterly winds to the proxy site of the Dehner dry maar.rnrnThe basic observations made on the proxy record are also illustrated in the 10 m-wind vectors in the different model experiments under glacial conditions with different prescribed sea surface temperature patterns. Furthermore, the analysis of long-persisting east wind conditions in the AGCM data shows a stronger seasonality under glacial conditions: all the different experiments are characterized by an increase of the relative importance of the LEWIC during spring and summer. The different glacial experiments consistently show a shift from a long-lasting high over the Baltic Sea towards the NW, directly above the Scandinavian Ice Sheet, together with contemporary enhanced westerly circulation over the North Atlantic.rnrnThis thesis is a comprehensive analysis of atmospheric circulation patterns during the last glacial period. It has been possible to reconstruct important elements of the glacial paleo climate in Central Europe. While the proxy data from sediment cores lead to a binary signal of the wind direction changes (east versus west wind), a synoptic interpretation using atmospheric circulation models is successful. This shows a possible distribution of high and low pressure areas and thus the direction and strength of wind fields which have the capacity to transport dust. In conclusion, the combination of numerical models, to enhance understanding of processes in the climate system, with proxy data from the environmental record is the key to a comprehensive approach to paleo climatic reconstruction.rn

Non-equilibrium molecular dynamics study of an amphiphilic model system

Diese Doktorarbeit untersucht das Verhalten von komplexenFluidenunter Scherung, insbesondere den Einfluss von Scherflüssenauf dieStrukturbildung.Dazu wird ein Modell dieser entworfen, welches imRahmen von Molekulardynamiksimulationen verwendet wird.Zunächst werden Gleichgewichtseigenschaften dieses Modellsuntersucht.Hierbei wird unter anderem die Lage desOrdnungs--Unordnungsübergangs von derisotropen zur lamellaren Phase der Dimere bestimmt.Der Einfluss von Scherflüssen auf diese lamellare Phase wirdnununtersucht und mit analytischen Theorien verglichen. Die Scherung einer parallelen lamellaren Phase ruft eineNeuausrichtung des Direktors in Flussrichtung hervor.Das verursacht eine Verminderung der Schichtdicke mitsteigender Scherrateund führt oberhalb eines Schwellwertes zu Ondulationen.Ein vergleichbares Verhalten wird auch in lamellarenSystemengefunden, an denen in Richtung des Direktors gezogen wird.Allerdings wird festgestellt, dass die Art der Bifurkationenin beidenFällen unterschiedlich ist.Unter Scherung wird ein Übergang von Lamellen parallelerAusrichtung zu senkrechter gefunden.Dabei wird beoachtet, dass die Scherspannung in senkrechterOrientierungniedriger als in der parallelen ist.Dies führt unter bestimmten Bedingungen zum Auftreten vonScherbändern, was auch in Simulationen beobachtet wird. Es ist gelungen mit einem einfachen Modell viele Apsekte desVerhalten vonkomplexen Fluiden wiederzugeben. Die Strukturbildung hängt offensichtlich nurbedingt von lokalen Eigenschaften der Moleküle ab.

The role of SENP1 in B cell development and differentiation

SUMOylation is a highly dynamic and reversible posttranslational protein modification closely related to ubiquitination. SUMOylation regulates a vast array of different cellular functions, such as cell cycle, nuclear transport, DNA damage response, proliferation and transcriptional activation. Several groups have shown in in vitro studies how important SUMOylation is for early B cell development and survival as well as for later plasma cell differentiation. This thesis focuses on the deSUMOylation protease SENP1 and its in vivo effects on B cell development and differentiation. For this a conditional SENP1 knockout mouse model was crossed to the CD19-Cre mouse strain to generate a B cell specific SENP1 knockout mouse.rnIn our conditional SENP1ff CD19-Cre mouse model we observed normal numbers of all B cell subsets in the bone marrow. However in the spleen we observed an impairment of B cell survival, based on a 50% reduction of the follicular B cell compartment, whereas the marginal zone B cell compartment was unchanged. T cell numbers were comparable to control mice. rnFurther, impairments of B cell survival in SENP1ff CD19-Cre mice were analysed after in vivo blocking of IL7R signalling. The αIL7R treatment in mature mice blocked new B cell formation in the bone marrow and increased apoptosis rates could be observed in splenic SENP1 KO B cells. Additionally, a higher turnover rate of B cells was measured by in vivo BrdU incorporation.rnSince it is known that the majority of transcription factors that are important for the maintenance of the germinal centre reaction or for induction of plasma cell development are SUMOylated, the question arose, how defective deSUMOylation will manifest itself in these processes. The majority of in vitro cultured splenic B cells, stimulated to undergo class switch recombination and plasma cell differentiation underwent activation induced cell death. However, the surviving cells increasingly differentiated into IgM expressing plasma cells. Class switch recombination to IgG1 was reduced. These observations stood in line with observation made in in vivo sheep red blood cell immunization experiments, which showed increased amounts of germinal centres and germinal centre B cells, as well as increased amounts of plasma cells differentiation in combination with decreased class switch to IgG1.rnThese results lead to the conclusion that SENP1 KO B cells increasingly undergo apoptosis, however, B cells that survive SENP1 deficiency are more prone to undergo plasma cell differentiation. Further, the precursors of these plasma cells either are not as capable of undergoing class switch recombination or they do switch to IgG1 and succumb to activation induced cell death. One possible explanation for both scenarios could be a defective DNA damage response mechanisms during class switch recombination, caused by impaired deSUMOylation. rn