Identification of preferentially targeted tumor-associated antigens in melanoma patients via mRNA stimulation of CD8+ blood lymphocytes

Until now, therapeutic vaccination of cancer patients has mainly relied on rather few T cell epitopes processed from structurally normal shared tumor antigens and presented by frequent HLA alleles. So far the design of these studies has not addressed the individuality of tumor-host interactions, which are not only determined by the antigenic tumor phenotype or the natural HLA polymorphism, but also by the individual T cell repertoire. The procedure described herein was developed to identify the preferential targets of the individual repertoire from a panel of known shared tumor-associated antigens. Lymphocytes were isolated from the peripheral blood of cancer patients or healthy donors and stimulated twice with autologous mRNA-transfected FastDC (Dauer et al., J Immunol. 170:4069, 2003). FastDC were generated from blood monocytes and separately transfected via lipofection with in vitro transcribed mRNAs encoding the panel antigens. Responder lymphocytes were tested on day 12 in a 20-hour IFN-g ELISPOT assay for recognition of 293T cells co-transfected pairwise with plasmids encoding the stimulation antigens and the respective individual’s HLA class I alleles. In a first step, stimulation parameters were optimized for the detection of anti-HCMV pp65 responses. A maximum amplification of pp65-specific CD8+ T cell responses was obtained at a rather low IL-2 concentration (25 IU/ml) and at a minimum APC-to-effector ratio of 1:10. Addition of IL-4, IL-7 or IL-15 did not substantially improve the stimulatory potential. The test was applied to the human melanoma models D05 and MZ2, in both of which multiple T cell-defined antigens had previously been identified by expression screening. Blood lymphocytes were stimulated in parallel with autologous tumor cells and with mRNA-transfected FastDC. In D05, T cell reactivities against three out of eleven epitopes induced by stimulation with tumor cells were also found after stimulation with mRNA-transfected FastDC. Two further T cell target epitopes were identified with mRNA but not with tumor cell stimulation. In MZ2, T cell responses against five distinct epitopes were detected on day 12 after stimulation with mRNA transfectants. The same responses were detectable after stimulation with tumor cells only on day 32. mRNA stimulations against 21 tumor-associated antigens in addition to HCMV pp65 were performed in four healthy individuals. In all cases, CD8+ T cells against HCMV pp65 could be expanded. Among tumor-associated antigens, only reactivity against Melan-A/MART-1 in association with HLA-A*0201 was detectable in one of the donors. The vaccination of patients with targets a priori known to be recognized by their T cell repertoire may help to improve the outcome of therapeutic vaccination.

Aircraft-based in-situ aerosol mass spectrometry: Chemical characterization and source identification of submicron particulate matter in the free and upper troposphere and lower stratosphere

The composition of the atmosphere is frequently perturbed by the emission of gaseous and particulate matter from natural as well as anthropogenic sources. While the impact of trace gases on the radiative forcing of the climate is relatively well understood the role of aerosol is far more uncertain. Therefore, the study of the vertical distribution of particulate matter in the atmosphere and its chemical composition contribute valuable information to bridge this gap of knowledge. The chemical composition of aerosol reveals information on properties such as radiative behavior and hygroscopicity and therefore cloud condensation or ice nucleus potential. rnThis thesis focuses on aerosol pollution plumes observed in 2008 during the POLARCAT (Polar Study using Aircraft, Remote Sensing, Surface Measurements and Models, of Climate, Chemistry, Aerosols, and Transport) campaign over Greenland in June/July and CONCERT (Contrail and Cirrus Experiment) campaign over Central and Western Europe in October/November. Measurements were performed with an Aerodyne compact time-of-flight aerosol mass spectrometer (AMS) capable of online size-resolved chemical characterization of non-refractory submicron particles. In addition, the origins of pollution plumes were determined by means of modeling tools. The characterized pollution episodes originated from a large variety of sources and were encountered at distinct altitudes. They included pure natural emissions from two volcanic eruptions in 2008. By the time of detection over Western Europe between 10 and 12 km altitude the plume was about 3 months old and composed to 71 % of particulate sulfate and 21 % of carbonaceous compounds. Also, biomass burning (BB) plumes were observed over Greenland between 4 and 7 km altitude (free troposphere) originating from Canada and East Siberia. The long-range transport took roughly one and two weeks, respectively. The aerosol was composed of 78 % organic matter and 22 % particulate sulfate. Some Canadian and all Siberian BB plumes were mixed with anthropogenic emissions from fossil fuel combustion (FF) in North America and East Asia. It was found that the contribution of particulate sulfate increased with growing influences from anthropogenic activity and Asia reaching up to 37 % after more than two weeks of transport time. The most exclusively anthropogenic emission source probed in the upper troposphere was engine exhaust from commercial aircraft liners over Germany. However, in-situ characterization of this aerosol type during aircraft chasing was not possible. All long-range transport aerosol was found to have an O:C ratio close to or greater than 1 implying that low-volatility oxygenated organic aerosol was present in each case despite the variety of origins and the large range in age from 3 to 100 days. This leads to the conclusion that organic particulate matter reaches a final and uniform state of oxygenation after at least 3 days in the free troposphere. rnExcept for aircraft exhaust all emission sources mentioned above are surface-bound and thus rely on different types of vertical transport mechanisms, such as direct high altitude injection in the case of a volcanic eruption, or severe BB, or uplift by convection, to reach higher altitudes where particles can travel long distances before removal mainly caused by cloud scavenging. A lifetime for North American mixed BB and FF aerosol of 7 to 11 days was derived. This in consequence means that emission from surface point sources, e.g. volcanoes, or regions, e.g. East Asia, do not only have a relevant impact on the immediate surroundings but rather on a hemispheric scale including such climate sensitive zones as the tropopause or the Arctic.