Influences of deep convective cloud systems on tropospheric trace gases and photochemistry over the tropical West Pacific

A numerical model for studying the influences of deep convective cloud systems on photochemistry was developed based on a non-hydrostatic meteorological model and chemistry from a global chemistry transport model. The transport of trace gases, the scavenging of soluble trace gases, and the influences of lightning produced nitrogen oxides (NOx=NO+NO2) on the local ozone-related photochemistry were investigated in a multi-day case study for an oceanic region located in the tropical western Pacific. Model runs considering influences of large scale flows, previously neglected in multi-day cloud resolving and single column model studies of tracer transport, yielded that the influence of the mesoscale subsidence (between clouds) on trace gas transport was considerably overestimated in these studies. The simulated vertical transport and scavenging of highly soluble tracers were found to depend on the initial profiles, reconciling contrasting results from two previous studies. Influences of the modeled uptake of trace gases by hydrometeors in the liquid and the ice phase were studied in some detail for a small number of atmospheric trace gases and novel aspects concerning the role of the retention coefficient (i.e. the fraction of a dissolved trace gas that is retained in the ice phase upon freezing) on the vertical transport of highly soluble gases were illuminated. Including lightning NOx production inside a 500 km 2-D model domain was found to be important for the NOx budget and caused small to moderate changes in the domain averaged ozone concentrations. A number of sensitivity studies yielded that the fraction of lightning associated NOx which was lost through photochemical reactions in the vicinity of the lightning source was considerable, but strongly depended on assumptions about the magnitude and the altitude of the lightning NOx source. In contrast to a suggestion from an earlier study, it was argued that the near zero upper tropospheric ozone mixing ratios which were observed close to the study region were most probably not caused by the formation of NO associated with lightning. Instead, it was argued in agreement with suggestions from other studies that the deep convective transport of ozone-poor air masses from the relatively unpolluted marine boundary layer, which have most likely been advected horizontally over relatively large distances (both before and after encountering deep convection) probably played a role. In particular, it was suggested that the ozone profiles observed during CEPEX (Central Equatorial Pacific Experiment) were strongly influenced by the deep convection and the larger scale flow which are associated with the intra-seasonal oscillation.

Mediterranean-type climate in the South Aegean (Eastern Mediterranean) during the Late Miocene: Evidence from isotope and element proxies

The present-day climate in the Mediterranean region is characterized by mild, wet winters and hot, dry summers. There is contradictory evidence as to whether the present-day conditions (“Mediterranean climate”) already existed in the Late Miocene. This thesis presents seasonally-resolved isotope and element proxy data obtained from Late Miocene reef corals from Crete (Southern Aegean, Eastern Mediterranean) in order to illustrate climate conditions in the Mediterranean region during this time. There was a transition from greenhouse to icehouse conditions without a Greenland ice sheet during the Late Miocene. Since the Greenland ice sheet is predicted to melt fully within the next millennia, Late Miocene climate mechanisms can be considered as useful analogues in evaluating models of Northern Hemispheric climate conditions in the future. So far, high resolution chemical proxy data on Late Miocene environments are limited. In order to enlarge the proxy database for this time span, coral genus Tarbellastraea was evaluated as a new proxy archive, and proved reliable based on consistent oxygen isotope records of Tarbellastraea and the established paleoenvironmental archive of coral genus Porites. In combination with lithostratigraphic data, global 87Sr/86Sr seawater chronostratigraphy was used to constrain the numerical age of the coral sites, assuming the Mediterranean Sea to be equilibrated with global open ocean water. 87Sr/86Sr ratios of Tarbellastraea and Porites from eight stratigraphically different sampling sites were measured by thermal ionization mass spectrometry. The ratios range from 0.708900 to 0.708958 corresponding to ages of 10 to 7 Ma (Tortonian to Early Messinian). Spectral analyses of multi-decadal time-series yield interannual δ18O variability with periods of ~2 and ~5 years, similar to that of modern records, indicating that pressure field systems comparable to those controlling the seasonality of present-day Mediterranean climate existed, at least intermittently, already during the Late Miocene. In addition to sea surface temperature (SST), δ18O composition of coral aragonite is controlled by other parameters such as local seawater composition which as a result of precipitation and evaporation, influences sea surface salinity (SSS). The Sr/Ca ratio is considered to be independent of salinity, and was used, therefore, as an additional proxy to estimate seasonality in SST. Major and trace element concentrations in coral aragonite determined by laser ablation inductively coupled plasma mass spectrometry yield significant variations along a transect perpendicular to coral growth increments, and record varying environmental conditions. The comparison between the average SST seasonality of 7°C and 9°C, derived from average annual δ18O (1.1‰) and Sr/Ca (0.579 mmol/mol) amplitudes, respectively, indicates that the δ18O-derived SST seasonality is biased by seawater composition, reducing the δ18O amplitude by 0.3‰. This value is equivalent to a seasonal SSS variation of 1‰, as observed under present-day Aegean Sea conditions. Concentration patterns of non-lattice bound major and trace elements, related to trapped particles within the coral skeleton, reflect seasonal input of suspended load into the reef environment. δ18O, Sr/Ca and non-lattice bound element proxy records, as well as geochemical compositions of the trapped particles, provide evidence for intense precipitation in the Eastern Mediterranean during winters. Winter rain caused freshwater discharge and transport of weathering products from the hinterland into the reef environment. There is a trend in coral δ18O data to more positive mean δ18O values (–2.7‰ to –1.7‰) coupled with decreased seasonal δ18O amplitudes (1.1‰ to 0.7‰) from 10 to 7 Ma. This relationship is most easily explained in terms of more positive summer δ18O. Since coral diversity and annual growth rates indicate more or less constant average SST for the Mediterranean from the Tortonian to the Early Messinian, more positive mean and summer δ18O indicate increasing aridity during the Late Miocene, and more pronounced during summers. The analytical results implicate that winter rainfall and summer drought, the main characteristics of the present-day Mediterranean climate, were already present in the Mediterranean region during the Late Miocene. Some models have argued that the Mediterranean climate did not exist in this region prior to the Pliocene. However, the data presented here show that conditions comparable to those of the present-day existed either intermittently or permanently since at least about 10 Ma.

Interplay between BDNF,TrkB signalling and GABAergic inhibition in the visual cortex of mice

Der visuelle Kortex ist eine der attraktivsten Modellsysteme zur Untersuchung der molekularen Mechanismen der synaptischen Plastizität im Gehirn. Es hat sich gezeigt, dass der Wachstumsfaktor brain-derived-neurotrophic-factor (BDNF) und die GABAerge Hemmung während der Entwicklung eine essentielle Funktion in der Regulierung der synaptischen Plastizität im visuellen Kortex besitzen. BDNF bindet u.a. an TrkB Rezeptoren, die das Signal intrazellular an unterschiedliche Effektormoleküle weiter vermitteln. Außer BDNF sind auch andere TrkB-Rezeptor Agonisten in der Literatur beschrieben. Einer davon ist das kürzlich identifizierte Flavonoid 7,8-Dihydroxyflavone (7,8-DHF), welchem eine neurotrophe Wirkung zugeschrieben wird. Im ersten Abschnitt der vorliegenden Doktorarbeit wurde der Effekt dieses Agonisten auf die synaptische Übertragung und intrinsischen Zelleigenschaften im visuellen Kortex der Maus untersucht. Dies wurde mit Hilfe der whole-cell patch clamp Methode durchgeführt, wobei die synaptischen Eingänge der Pyramidalzellen der kortikalen Schicht 2/3 von besonderem Interesse waren.rnEine 30 minütige Inkubationszeit der kortikalen Schnitte mit 7,8 DHF (20µM) erzielte eine signifikante Reduktion der GABAergen Hemmung, während die glutamaterge synaptische Übertragung unverändert blieb. Des weiteren konnte in Gegenwart von 7,8 DHF eine Veränderung der intrinsischen neuronalen Zellmembraneigenschaften beobachtet werden. Dies wurde deutlich in der Erhöhung des Eingangwiderstandes und der Frequenz der induzierten Aktionspotentiale. Die chronische Applikation von 7,8 DHF in vivo bestätigte die selektive Wirkung von 7,8 DHF auf das GABAerge System. rnDie Rolle des BDNF-TrkB-Signalweges in der GABAergen Hemmung nach kortikalen Verletzungen ist bisher wenig verstanden. Eine häufig beschriebene elektrophysiologische Veränderung nach kortikaler Verletzung ist eine Reduktion in der GABAergen Hemmung. Im zweiten Abschnitt dieser Doktorarbeit wurde hierzu die Funktion des BDNF-TrkB-Signalweges auf die GABAerge Hemmung nach kortikaler Verletzung untersucht. Es wurde ein "ex-vivo/in-vitro“ Laser-Läsions Modell verwendet, wobei mittels eines Lasers im visuellen Kortex von WT und heterozygoten BDNF (+/−) Mäusen eine definierte, reproduzierbare Läsion induziert wurde. Nachfolgende elektrophysiologische Messungen ergaben, dass die Auswirkung einer Verletzung des visuellen Kortex auf die GABAerge Funktion signifikant von der basalen BDNF Konzentration im Kortex abhängt. Des weiteren konnte beobachtet werden, dass nach kortikaler Verletzung in WT Mäusen sowohl die Frequenz der basalen inhibitorischen, postsynaptischen Potentiale (mIPSCs) reduziert war, als auch ein erhöhtes Paired-Pulse Verhältnis vorlag. Diese Ergebnisse deuten auf Veränderungen der präsynaptischen Funktion inhibitorischer Synapsen auf Pyramidalneurone hin. Im Gegensatz dazu konnte in BDNF (+/−) mice Mäusen eine erhöhte und gleichzeitig verlängerte mIPSC-Amplitude beobachtet werden, induziert durch Reizung afferenter Nervenfasern. Hieraus lässt sich schließen, dass kortikale Verletzungen in BDNF (+/−) mice Mäusen Auswirkungen auf die Eigenschaften von postsynaptischen GABAA-Rezeptoren haben. Die nachfolgende Gabe eines TrkB-Rezeptor Antagonisten bestätigte diese Ergebnisse für das GABAerge System post-Läsion. Dies zeigt auch, dass die Änderungen der synaptischen Hemmung nicht auf eine Reduktion der BDNF-Konzentration zurückzuführen sind. Zusammengefasst zeigen die Ergebnisse der vorliegenden Arbeit, dass der BDNF-TrkB Signalweg eine wichtige Rolle in der Reorganisation der GABAergen Hemmung nach kortikalen Verletzungen spielt. So könnte ein TrkB-Rezeptor Agonist, wie das kürzlich entdeckte 7,8-DHF, über eine Modulation der BDNF-TrB Signalkaskade pharmakologisch die funktionelle Reorganisation des Kortex nach einer fokalen Gehirnverletzung fördern. rnrn

Improving adoptive T cell therapies of cancer by ectopic expression of miR181a to repress inhibitory phosphatases

Adoptive T cell therapy using antigen-specific T lymphocytes is a powerful immunotherapeutic approach against cancer. Nevertheless, many T cells against tumor-antigens exhibit only weak anti-tumoral response. To overcome this barrier it is necessary to improve the potency and anti-tumoral efficacy of these T cells. Activation and activity of T cells are tightly controlled to inhibit unwanted T cell responses and to reduce the risk of autoimmunity. Both are regulated by extrinsic signals and intrinsic mechanisms which suppress T cell activation. The intrinsic mechanisms include the expression of phosphatases that counteract the activation-inducing kinases. Modifying the expression of these phosphatases allows the targeted modulation of T cell reactivity. MicroRNAs (miRNAs) are regulatory small noncoding RNA molecules that control gene expression by targeting messenger RNAs in a sequence specific manner. Gene-specific silencing plays a key role in diverse biological processes, such as development, differentiation, and functionality. miR181a has been shown to be highly expressed in immature T cells that recognize low-affinity antigens.rnThe present study successfully shows that ectopic expression of miR181a is able to enhance the sensitivity of both murine and human T cells. In CD4+ T helper cells as well as in CD8+ cytotoxic T cells the overexpression of miR181a leads to downregulation of multiple phosphatases involved in the T cell receptor signaling pathway. Overexpression of miR181a in human T cells achieves a co-stimulatory independent activation and has an anti-apoptotic effect on CD4+ T helper cells. Additionally, increasing the amount of miR181a enhances the cytolytic activity of murine CD8+ TCRtg T cells in an antigen-specific manner.rnTo test miR181a overexpressing T cells in vivo, a mouse tumor model using a B cell lymphoma cell line (A20-HA) expressing the Influenza hemagglutinin (Infl.-HA) antigen was established. The expression of model antigens in tumor cell lines enables targeted elimination of tumors using TCRtg T cells. The transfer of miR181a overexpressing Infl.-HA TCRtg CD8+ T cells alone has no positive effect neither on tumor control nor on survival of A20-HA tumor-bearing mice. In contrast, the co-transfer of miR181a overexpressing Infl.-HA TCRtg CD8+ and CD4+ T cells leads to improved tumor control and prolongs survival of A20-HA tumor-bearing mice. This effect is characterized by higher amounts of effector T cells and the expansion of Infl.-HA TCRtg CD8+ T cells.rnAll effects were achieved by changes in expression of several genes including molecules involved in T cell differentiation, activation, and regulation, cytotoxic effector molecules, and receptors important for the homing process of T cells in miR181a overexpressing T cells. The present study demonstrates that miR181a is able to enhance the anti-tumoral response of antigen-specific T cells and is a promising candidate for improving adoptive cell therapy.