Untersuchungen zur Lymphozytotoxizität gegen Tumoren in Nierenzellkarzinom-Patienten und HLA-kompatiblen gesunden Spendern

In der vorliegenden Arbeit wurden Blutlymphozyten, die aus allogenen, serologisch HLA (humanes Leukozytenantigen)-identischen gesunden Geschwisterspendern von Nierenzellkarzinom (RCC, engl. renal cell carcinoma)-Patienten isoliert wurden, auf ihre antitumorale Reaktivität in vitro untersucht. Dazu war die vorangehende Generierung von stabil in vitro wachsenden Tumorzelllinien der Patienten zwingende Voraussetzung. Insgesamt wurden aus primärem Tumorgewebe von 65 Nierenzellkarzinom-Patienten Tumorzellen isoliert und daraus Zellkulturen angelegt. In 28 % der Fälle gelang es, eine konstant in Zellkultur wachsende Tumorzelllinie zu etablieren. Daneben wurden aus 56 Tumorpatienten auch die aus dem angrenzenden Nierengewebe gewonnenen nicht-malignen Nierenzellen über wenige Zellkultur-Passagen expandiert. In vier Patienten mit stabil in vitro wachsender Tumorzelllinie war ein allogener HLA-identischer Geschwisterspender verfügbar. In diesen Modellsystemen wurden in gemischten Lymphozyten-Tumorzell-Kulturen (MLTCs, engl. mixed lymphocyte tumor cell cultures) die Blutlymphozyten der Patienten und der gesunden Geschwisterspender mit der jeweiligen Nierenzellkarzinom-Zelllinie stimuliert und tumorreaktive CD8+ zytotoxische T-Lymphozyten (CTLs, engl. cytotoxic T-lymphocytes) generiert. Wenn möglich wurden aus den so gewonnenen „Responder“-Massenkulturen CD8+ T-Zellklone isoliert und hinsichtlich ihrer Funktionalität in IFN-γ-ELISpot-Assays und 51Chrom-Zytotoxizitätstests untersucht. Durch Blockade der HLA-Moleküle mit monoklonalen Antikörpern wurden die HLA-Restriktionselemente sowie weitere an der Erkennung beteiligte Oberflächenmoleküle analysiert. Kreuzreaktivitätsuntersuchungen mit einem breiten Zielzell-„Panel“ gaben Aufschluss über die Reaktivität der CTLs gegen RCC, nicht-maligne Nierenzellen, hämatopoetische Zielzellen von Patient und Geschwisterspender und weitere Tumorzelllinien aus Nierenzellkarzinomen und anderen Tumorentitäten. Interessanterweise zeigten die Geschwister-MLTC-„Responder“-Lymphozyten im Vergleich zu den autologen MLTC-„Responder“-Lymphozyten eine stärkere Proliferation und Zytotoxizität nach Stimulation mit Tumorzellen. Die allogenen tumorreaktiven „Responder“-Lymphozyten entstammten der CD8+ CD62L(high)+ Subpopulation, die naive Vorläufer- und „central memory“-T-Zellen enthält. Im Gegensatz zu autologen MLTC-Lymphozyten und tumorinfiltrierenden Lymphozyten konnte aus nahezu allen allogenen MLTCs mithilfe des Grenzverdünnungsverfahrens ein breites Spektrum an tumorreaktiven CTL-Klonen expandiert werden. Diese lysierten entweder ausschließlich die autologe RCC-Zelllinie oder kreuzreagierten mit autologen nicht-malignen Nierenzellen. Eine Minderheit der CTL-Klone erkannte außerdem hämatopoetische Zellen des Patienten oder allogene Tumorzellen. Als HLA-Restriktionselemente der allogenen tumorreaktiven CD8+ CTL-Klone wurden HLA-A2, -A3, -A11, -A24 und -B7 identifiziert. Weiterhin wurden in einem Modellsystem bisher unbekannte, stark proliferierende CD3+ CD16+ CD57+ CTL-Klone mit nicht-HLA-restringierter Tumorreaktivität isoliert. Zusammenfassend zeigt diese Arbeit erstmals, dass allogene Blutlymphozyten von HLA-identischen gesunden Geschwistern eine Vielfalt von tumorreaktiven CD8+ CTL-Klonen enthalten. Im direkten Vergleich mit autologen Blutlymphozyten der betroffenen Patienten besitzen allogene Blutlymphozyten der Geschwister eine stärkere proliferative und zytotoxische Tumorreaktivität. Die Ergebnisse dieser Arbeit ermutigen weitere Bemühungen, tumorreaktive T-Zellen aus dem Blut von HLA-identischen gesunden Geschwisterspendern in vitro zu generieren. Solche T-Zellen wären in zweierlei Hinsicht von Interesse: Zum einen ermöglichen sie die Identifizierung der Zielantigene, die von T-Zellen aus gesunden Individuen auf Tumoren erkannt werden und als Zielstrukturen von antigenspezifischen Immuntherapien (z. B. Vakzination) dienen könnten. Zum anderen könnten diese T-Zellen möglicherweise für eine adoptive Immuntherapie der betroffenen Tumorpatienten verwendet werden.

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.

Forward modelling of petrological crust-forming processes on the early Earth

Tonalite-trondhjemite-granodiorite (TTG) gneisses form up to two-thirds of the preserved Archean continental crust and there is considerable debate regarding the primary magmatic processes of the generation of these rocks. The popular theories indicate that these rocks were formed by partial melting of basaltic oceanic crust which was previously metamorphosed to garnet-amphibolite and/or eclogite facies conditions either at the base of thick oceanic crust or by subduction processes.rnThis study investigates a new aspect regarding the source rock for Archean continental crust which is inferred to have had a bulk compostion richer in magnesium (picrite) than present-day basaltic oceanic crust. This difference is supposed to originate from a higher geothermal gradient in the early Archean which may have induced higher degrees of partial melting in the mantle, which resulted in a thicker and more magnesian oceanic crust. rnThe methods used to investigate the role of a more MgO-rich source rock in the formation of TTG-like melts in the context of this new approach are mineral equilibria calculations with the software THERMOCALC and high-pressure experiments conducted from 10–20 kbar and 900–1100 °C, both combined in a forward modelling approach. Initially, P–T pseudosections for natural rock compositions with increasing MgO contents were calculated in the system NCFMASHTO (Na2O–CaO–FeO–MgO–Al2O3–SiO2–H2O–TiO2) to ascertain the metamorphic products from rocks with increasing MgO contents from a MORB up to a komatiite. A small number of previous experiments on komatiites showed the development of pyroxenite instead of eclogite and garnet-amphibolite during metamorphism and established that melts of these pyroxenites are of basaltic composition, thus again building oceanic crust instead of continental crust.rnThe P–T pseudosections calculated represent a continuous development of their metamorphic products from amphibolites and eclogites towards pyroxenites. On the basis of these calculations and the changes within the range of compositions, three picritic Models of Archean Oceanic Crust (MAOC) were established with different MgO contents (11, 13 and 15 wt%) ranging between basalt and komatiite. The thermodynamic modelling for MAOC 11, 13 and 15 at supersolidus conditions is imprecise since no appropriate melt model for metabasic rocks is currently available and the melt model for metapelitic rocks resulted in unsatisfactory calculations. The partially molten region is therfore covered by high-pressure experiments. The results of the experiments show a transition from predominantly tonalitic melts in MAOC 11 to basaltic melts in MAOC 15 and a solidus moving towards higher temperatures with increasing magnesium in the bulk composition. Tonalitic melts were generated in MAOC 11 and 13 at pressures up to 12.5 kbar in the presence of garnet, clinopyroxene, plagioclase plus/minus quartz (plus/minus orthopyroxene in the presence of quartz and at lower pressures) in the absence of amphibole but it could not be explicitly indicated whether the tonalitic melts coexisting with an eclogitic residue and rutile at 20 kbar do belong to the Archean TTG suite. Basaltic melts were generated predominantly in the presence of granulite facies residues such as amphibole plus/minus garnet, plagioclase, orthopyroxene that lack quartz in all MAOC compositions at pressures up to 15 kbar. rnThe tonalitic melts generated in MAOC 11 and 13 indicate that thicker oceanic crust with more magnesium than that of a modern basalt is also a viable source for the generation of TTG-like melts and therefore continental crust in the Archean. The experimental results are related to different geologic settings as a function of pressure. The favoured setting for the generation of early TTG-like melts at 15 kbar is the base of an oceanic crust thicker than existing today or by melting of slabs in shallow subduction zones, both without interaction of tonalic melts with the mantle. Tonalitic melts at 20 kbar may have been generated below the plagioclase stability by slab melting in deeper subduction zones that have developed with time during the progressive cooling of the Earth, but it is unlikely that those melts reached lower pressure levels without further mantle interaction.rn