Genesis of metasomatic sapphirine-corundum-spinel-bearing granulites in Sri Lanka

The goal of the present study is to understand the mechanism of mass transfer, the composition and the role of fluids during crustal metasomatism in high-temperature metamorphic terranes. A well constrained case study, a locality at Rupaha, Sri Lanka was selected. It is located in the Highland Complex of Sri Lanka, which represents a small, but important fragment of the super-continent Gondwana. Excellent exposures of ultramafic rocks, which are embedded in granulites, were found at 10 localities. These provide a unique background for understanding the metasomatic processes. The boundary between the ultramafic and the granulite rocks are lined with metasomatic reaction zones up to 50cm in width. Progressing from the ultramafics to the granulite host rock, three distinct zones with the following mineral assemblages can be distinguished: (1). phlogopite + spinel + sapphirine, (2). spinel + sapphirine and (3). corundum + biotite + plagioclase. In order to assess the P-T-t path, the peak metamorphism and the exhumation history were constrained using different thermobarometers, as well as a diffusion model of garnet zoning. A maximum temperature of 875 ± 20oC (Opx-Cpx thermometer) and at the peak pressure of 9.0 ± 0.1 kbar (Grt-Cpx-Pl-Qtz) was calculated for the silicic granulite. The ultramafic rocks recorded a peak temperature of 840 ± 70oC (Opx-Cpx thermometer) at 9 kbar. Coexisting spinel and sapphirine from the reaction zone yield a temperature of 820 ± 40oC. This is in agreement with the peak-temperatures recorded in the adjacent granulites and ultramafics rocks. The structural concordance of the ultramafic rocks with the siliceous granulite host rock further support the suggestion, that all units have experienced the same peak metamorphism. Diffusion modeling of retrograde zoning in garnets from mafic granulites suggests a three-step cooling history. A maximum cooling rate of 1oC/Ma is estimated during the initial stage of cooling, followed by a cooling rate of ~30oC/Ma. The outermost rims of garnet indicate a slightly slower cooling rate at about 10-15oC/Ma. The sequences of mineral zones, containing a variety of Al-rich, silica undersaturated minerals in the reaction zones separating the ultramafic rocks from the silica-rich rocks can be explained by a diffusion model. This involves the diffusion of Mg from ultramafic rocks across the layers, and K and Si diffuse in opposite direction. Chemical potential of Mg and Si generated continuous monotonic gradient, allowing steady state diffusional transport across the profile. The strong enrichment in Al, and the considerable loss of Si, during the formation of reaction bands can be inferred from isocon diagrams. Some Al was probably added to the reaction zones, while Si was lost. This is most likely due to fluids percolating parallel to the zones at the boundary of the rock units. This study has shown that not only pressure and temperature conditions but most importantly PH2O and the concentration of the chlorine and fluorine in aqueous fluids also control the mass transport in different geological environments.

Untersuchungen zur stereokontrollierten Synthese von 3-Mercaptolysinderivaten und Untersuchungen zur Synthese von Ansa-Seco-Steroiden

Untersuchungen zur stereokontrollierten Synthese von 3-Mercaptolysinderivaten: 3-Mercaptolysin und Peptide mit einer 3-Mercaptolysin-Einheit sind als Liganden für Nukleardiagnostika in der Kontrastmittelforschung von großem Interesse. Für das Screening Gewebe-selektiver Diagnostika sollten Mercaptolysinderivate, die sich für den Einbau in Peptide eignen, stereokontrolliert aufgebaut werden. Als Grundlage wurde im Rahmen dieser Arbeit eine sehr effiziente Synthese von Methoxymethyl-(4-oxo-butyl)-carbaminsäure-tert-butylester aus Pent-4-en-1-ol entwickelt. Nach Olefinierung des Aldehyds konnten Auxiliar-substituierte 6-Amino-hexensäure-derivate in guten Ausbeuten erhalten werden. Diese bildeten die Startmaterialien für auxiliargesteuerte Aziridinierungen mit anschließender Ringöffnung durch Schwefel-Nukleophile. Zudem wurden Azidierungen an Auxiliar-bewehrten Substraten, Michael-Additionen von Schwefel-Nukleophilen an Dehydroaminosäuren und viele weitere Reaktionen untersucht. Es galt dabei auf patentrechtlich geschützte Reaktionen zu verzichten, weil die Produkte ggf. in großem Maßstab kommerziell genutzt werden sollen. Dabei konnten alle vier stereoisomeren 2-Acetylamino-6-(tert-butoxycarbonyl-methoxymethyl-amino)-3-(4-methoxy-benzylsulfanyl)-hexansäurementhylester in guter Ausbeute synthetisiert werden. Nach Herstellung größerer Mengen der entsprechenden am Schwefelatom ungeschützten N-Fmoc-Aminosäurederivate sollen alle vier Stereoisomere in Peptide eingebaut und auf ihre Eignung als Liganden in Nukleardiagnostika untersucht werden. Untersuchungen zur Synthese neuartiger Ansa-Steroide: Über die Synthese von Ansa-Seco-Steroiden mittels eine Kaskade von intermolekularer Diels-Alder-Reaktion und anschließender Retro-Diels-Alder-Reaktion an 5,6,7,8-Tetradehydrosteroiden wurde erstmals 1986 von E. Winterfeldt et al. berichtet. Die damit eröffnete Möglichkeit eines völlig neuen Zugangs zu pharmakologisch interessanten Makrolid-Substraten konnte aber bislang nicht effektiv genutzt werden, weil insbesondere im Zusammenhang mit der Diels-Alder-Reaktion erhebliche präparative Probleme auftraten: Brauchbare Reaktivität nur bei sehr wenigen Dienophilen, Regioselektivitätsprobleme, etc. Hier galt es zu untersuchen, inwiefern sich diese Probleme durch die intramolekulare Reaktionsführung der Cycloaddition unterdrücken lassen können. Für die intramolekulare Diels-Alder-Reaktion zwischen der 5,7-Dien-Einheit des Steroids und einer an das Substrat gebundenen Dienophil-Einheit ist die Möglichkeit einer günstigen Anordnung der beiden Reaktanden-Gruppen entscheidend. Dafür wurden umfangreiche Untersuchungen zur alpha-konfigurierten Anbindung eines Dienophils in die 3-Position an 3-Hydroxy-5,6,7,8-Tetradehydrosteroiden durchgeführt: Mitsunobu-Reaktionen, Oxidations-Reduktions-Sequenzen, Oxidations-Ketalisierungs-Sequenzen, etc. Hierbei wurden zahlreiche neue Steroide synthetisiert. Es gelang jedoch nicht, 5,6,7,8-Tetradehydrosteroide mit axial in Position 3 eingebundenen Dienophilen in präparativ nutzbaren Mengen zu synthetisieren. Bei der Untersuchung intermolekularer Diels-Alder-Reaktionen zwischen Ergosterol und Brommaleinsäureanhydrid wurde vorzugsweise die Bildung der Addukte des 7,8,14,15-Tetradehydroisomers des Ergosterols beobachtet.

Weathering of Fe-bearing minerals under extraterrestrial conditions, investigated by Mössbauer spectroscopy

The weathering of Fe-bearing minerals under extraterrestrial conditions was investigated by Mössbauer (MB) spectroscopy to gain insights into the role of water on the planet Mars. The NASA Mars Exploration Rovers Spirit and Opportunity each carry a miniaturized Mössbauer spectrometer MIMOS II for the in situ investigation of Martian soils and rocks as part of their payload. The MER flight instruments had to be modified in order to work over the Martian diurnal temperature range (180 K – 290 K) and within the unique electronic environment of the rovers. The modification required special calibration procedures. The integration time necessary to obtain a good quality Mössbauer spectrum with the MIMOS II flight instruments was reduced by 30 % through the design of a new collimator. The in situ investigation of rocks along the rover Spirit's traverse in Gusev crater revealed weakly altered olivine basalt on the plains and pervasively altered basalt in the Columbia Hills. Correlation plots of primary Fe-bearing minerals identified by MB spectroscopy such as olivine versus secondary Fe-bearing phases such as nanophase Fe oxides showed that olivine is the mineral which is primarily involved in weathering reactions. This argues for a reduced availability of water. Identification of the Fe-oxyhydroxide goethite in the Columbia Hills is unequivocal evidence for aqueous weathering processes in the Columbia Hills. Experiments in which mineral powders were exposed to components of the Martian atmosphere showed that interaction with the atmosphere alone, in the absence of liquid water, is sufficient to oxidize Martian surface materials. The fine-grained dust suspended in the Martian atmosphere may have been altered solely by gas-solid reactions. Fresh and altered specimens of Martian meteorites were investigated with MIMOS II. The study of Martian meteorites in the lab helped to identify in Bounce Rock the first rock on Mars which is similar in composition to basaltic shergottites, a subgroup of the Martian meteorites. The field of astrobiology includes the study of the origin, evolution and distribution of life in the universe. Water is a prerequisite for life. The MER Mössbauer spectrometers identified aqueous minerals such as jarosite and goethite. The identification of jarosite was crucial to evaluate the habitability of Opportunity's landing site at Meridiani Planum during the formation of the sedimentary outcrop rocks, because jarosite puts strong constrains on pH levels. The identification of olivine in rocks and soils on the Gusev crater plains provide evidence for the sparsity of water under current conditions on Mars. Ratios of Fe2+/Fe3+ were obtained with Mössbauer spectroscopy from basaltic glass samples which were exposed at a deep sea hydrothermal vent. The ratios were used as a measure of potential energy for use by a microbial community. Samples from Mars analogue field sites on Earth exhibiting morphological biosignatures were also investigated.