Self-assembly of Tetraurea Calix[4]arenes

We have elaborated a multistep strategy to synthesize ABAB-type tetraureas. There are overall nine steps but they involve very simple chemistry. The sequence starts with a 1,3-dialkylation and this is the step in which a difference between distal phenolic units is introduced. The selective ipso-nitration in the next step is based on the difference in reactivity between free phenolic units and alkylated ones. The direct reaction of tetraamino calixarene with tolylisocyanate appears not to be an appropriate method to synthesize 1,3-ditolylurea calixarenes but can be used to get tetraureas of ABBB- and AABB-types in two steps with yields of about 60%. A complete regioselective dimerization was obtained with mono-loop derivatives in which two adjacent urea residues are covalently connected. As predicted/expected the loop prevents the formation of one regioisomer, and only the dimer in which the open-chain residue slips through the loop is formed. To synthesize mono-loop tetraureas 1,2-diBoc protected tetraamino calixarene was acylated with activated di-urethanes under high dilution conditions. Di-loop compounds were synthesized by two different ways. In the reaction of tetraamine and di-urethanes the yield is about 30-40%. The second method is based on the metathesis reaction within a suitable heterodimer. For this strategy, tetraurea derivatives with residues which have terminal double bonds were prepared. The exclusive formation of the heterodimer with tetratosylurea as template is the key point in this strategy. Metathesis followed by hydrogenation give exceptionally good yields (> 80%) of the loop compounds. All the NMR data for di-loop compounds confirm that the loops prevent the interaction of the urea residues which are connected and thus, as expected, the di-loop derivatives do not form homodimers. The heterodimer between di-loop compounds and tetratolylurea (open-chain tetraureas) was the only species observed for a 1:1 mixture in benzene or chloroform. The rational synthesis of bis-[2]catenanes was a consequence of the selective formation of one regioisomer of mono-loop derivatives and the exclusive formation of heterodimers by di-loop derivatives. The formation of interlocking-ring in the synthesis of bis-[2]catenanes is an additional evidence that one open-chain residue slips through the loop in mono- or di-loop derivatives. Exceptionally good yields in the synthesis of bis-[2]catenanes are due to the high preorganization in the dimer which undergoes the metathesis. This preorganization decreases the number of the wrong connections and favors the new connections to be formed. Although the procedure for working up the reaction mixture should be still improved, these results are promising. A C2-symmetrical bis-[2]catenane was successfully resolved by column chromatography using a chiral stationary phase. Thus it should be possible to separate a larger amount to obtain pure enantiomers for further studies.

Eduard Study (1862-1930) - ein mathematischer Mephistopheles im geometrischen Gärtchen

Diese Arbeit befasst sich mit Eduard Study (1862-1930), einem der deutschen Geometer um die Jahrhundertwende, der seine Zeit zum Einen durch seine Kontakte zu Klein, Hilbert, Engel, Lie, Gordan, Halphen, Zeuthen, Einstein, Hausdorff und Weyl geprägt hat, zum Anderen in ihr aber auch für seine beißenden und stilistisch ausgefeilten Kritiken ebenso berühmt wie berüchtigt war. Da sich Study mit einer Vielzahl mathematischer Themen beschäftigt hat, führen wir zunächst in die von ihm bearbeiteten Gebiete der Geometrie des 19. Jahrhunderts ein (analytische und synthetische Geometrie im Sinne von Monge, Poncelet, Plücker und Reye, Invariantentheorie Clebsch-Gordan'scher Prägung, abzählende Geometrie von Chasles und Halphen, die Werke Lie's und Grassmann’s, Liniengeometrie sowie Axiomatik und Grundlagenkrise). In seiner darauf folgenden Biographie finden sich als zentrale Stellen seine Habilitation bei Klein über die Chasles’sche Vermutung, sein Streit mit Zeuthen darüber als eine der Debatten der Mathematischen Annalen (aus der er historisch zwar nicht, mathematisch aber tatsächlich als Gewinner hätte herausgehen müssen, wie wir an der Lösung des Problems durch van der Waerden sehen werden) und seine Auseinandersetzungen als etablierter Bonner Professor mit Engel über Lie, Weyl über Invariantentheorie, zahlreichen philosophischen Richtungen über das Raumproblem, Pasch’s Axiomatik, Hilbert’s Formalismus sowie Brouwer’s und Weyl’s Intuitionismus.

Evaluation of a viral vector system, based on a defective interfering RNA of tomato bushy stunt virus, for protein expression and the induction of gene silencing

A viral vector system was developed based on a DI-RNA, a sub-viral particle derived from TBSV-BS3-statice. This newly designed vector system was tested for its applicability in protein expression and induction of gene silencing. Two strategies were pursued. The first strategy was replication of the DI-RNA by a transgenically expressed TBSV replicase and the second was the replication by a so called helper virus. It could be demonstrated by northern blot analysis that the replicase, expressed by the transgenic N. benthamiana plant line TR4 or supplied by the helper virus, is able to replicate DI-RNA introduced into the plant cells. Various genes were inserted into different DI constructs in order to study the vector system with regard to protein expression. However, independent of how the replicase was provided no detectable amounts of protein were produced in the plants. Possible reasons for this failure are identified: the lack of systemic movement of the DI-RNA in the transgenic TR4 plants and the occurrence of deletions in the inserted genes in both systems. As a consequence the two strategies were considered unsuitable for protein expression. The DI-RNA vector system was able to induce silencing of transgenes as well as endogenous genes. Several different p19 deficient helper virus constructs were made to evaluate their silencing efficiency in combination with our DI-RNA constructs. However, it was found that our vector system can not compete with other existing VIGS (virus induced gene silencing) systems in this field. Finally, the influence of DI sequences on mRNA stability on transient GUS expression experiments in GUS silenced plants was evaluated. The GUS reporter gene system was found to be unsuitable for distinguishing between expression levels of wild type plants and GUS silenced transgenic plants. The results indicate a positive effect of the DI sequences on the level of protein expression and therefore further research into this area is recommended.

1,2-Additionen deprotonierter Alpha-Aminonitrile: Umgepolte Imine als vielseitige Synthesebausteine

Von aromatischen Aldehyden abgeleitete α-Aminonitrile können ohne die Anwendung von Schutzgruppen in α-Position deprotoniert werden, wenn keine lithiumhaltigen Basen verwendet werden. Ziel der vorliegenden Arbeit war es, die Reaktionen deprotonierter α-Aminonitrile mit Elektrophilen zu untersuchen. Die Addition von α-Aminocarbanionen an Imine führt unter intramolekularer Eliminierung von HCN zu Endiaminen, die sich in einer Eintopfsynthese abhängig von der Aufarbeitung in 1,2-Diamine oder 1,2-Diimine umwandeln lassen. Die nach Oxidation durch Luftsauerstoff erhaltenen Diimine können mit dem Reduktionsmittel BH3·THF diastereoselektiv reduziert werden. Es hat sich hier gezeigt, dass durch Zugabe einer katalytischen Menge an NaBH4 hauptsächlich die syn-Diamine erhalten werden, der Zusatz von Phthalsäure wiederum liefert bevorzugt die anti-Produkte. In beiden Fällen wird das Produkt in quantitativer Ausbeute erhalten. So konnte also eine effektive diastereoselektive Reduktionsmethode entwickelt werden, die eine freie Wahl der syn- oder anti-Konfiguration ermöglicht. Um enantiomerenreine 1,2-Diamine zu erhalten, wurden verschiedene Methoden getestet. Sowohl auxiliargesteuerte Synthesen mit einem N-Glycosyl-Aminonitril oder mit chiralen Sulfinyliminen als auch die Reduktion durch chirale Borverbindungen (CBS-Katalysatoren, Triacyloxyborhydrid oder Diisopinocamphenylboran), Transferhydrierungen mit chiralen Difluortitanocen-, Noyori- oder Organophosphat-Katalysatoren sowie enantioselektive Hydrierungen mit chiralen Übergangsmetall-katalysatoren waren jedoch nicht erfolgreich. Die Umsetzung der 1,2-Diimine mit Chlormethylethern oder -estern liefert die entsprechenden unsymmetrischen Imidazoliumsalze. Diese konnten zu N-heterocyclischen Carbenen deprotoniert und erfolgreich als Liganden in Suzuki- und Heck-Reaktionen eingesetzt werden. Durch die 1,2-Addition α-deprotonierter Streckerprodukte und anschließende Reduktion im Eintopfverfahren konnten 1,2-Aminoalkohole in mäßigen bis guten Ausbeuten dargestellt werden. Die Umsetzung von α-Aminocarbanionen mit N-Acyliminen erlaubt zudem die Synthese tetrasubstituierter Imidazole und trisubstituierter Oxazole in drei beziehungsweise vier Stufen: Die zunächst gebildeten α-Amino-α-acylaminopropionitrile können isoliert und in Gegenwart von Base einer Retro-Strecker-Reaktion unterworfen werden. Abhängig vom Substitutionsmuster schließt sich in manchen Fällen nach der Eliminierung von HCN direkt die Cyclisierung zum Imidazol an. Nicht cyclisierte Intermediate lassen sich durch Dehydratisierung mit PCl5 zu Imidazolen umsetzen, aber auch unter sauren Bedingungen zu α-Acylaminoketonen hydrolysieren, welche wiederum durch Einwirkung von PCl5 in Oxazole überführt werden können. Auf diese Weise wurden Imidazole und Oxazole in moderaten bis hohen Gesamtausbeuten hergestellt.

Granulite facies metamorphism and partial melting processes in the Ivrea Zone, Northern Italy

The Ivrea Zone in northern Italy has been the focus of numerous petrological, geochemical and structural studies. It is commonly inferred to represent an almost complete section through the mid to lower continental crust, in which metamorphism and partial melting of the abundant metapelites was the result of magmatic underplating by a large volume of mantle-derived magma. This study concerns amphibolite and granulite facies metamorphism in the Ivrea Zone with focus on metapelites and metapsammites/metagreywackes from Val Strona di Omegna and metapelites from Val Sesia and Val Strona di Postua, with the aim to better constrain their metamorphic evolution as well as their pressure and temperature conditions via phase equilibria modelling.rnrnIn Val Strona di Omegna, the metapelites show a structural and mineralogical change from mica-schists with the common assemblage bi-mu-sill-pl-q-ilm ± liq at the lowest grades, through metatexitic migmatites (g-sill-bi-ksp-pl-q-ilm-liq) at intermediate grades, to complex diatexitic migmatites (g-sill-ru-bi-ksp-pl-q-ilm-liq) at the highest grades. Within this section several mappable isograds occur, including the first appearance of K-feldspar in the metapelites, the first appearance of orthopyroxene in the metabasites and the disappearance of prograde biotite from the metapelites. The inferred onset of partial melting in the metapelites occurs around Massiola. The prograde suprasolidus evolution of the metapelites is consistent with melting via the breakdown of first muscovite then biotite. Maximum modelled melt fractions of 30–40 % are predicted at the highest grade. The regional metamorphic field gradient in Val Strona di Omegna is constrained to range from conditions of 3.5–6.5 kbar at T = 650–730 °C to P > 9 kbar at T > 900 °C. The peak P–T estimates, particularly for granulite facies conditions, are significantly higher (around 100 °C) than those of most previous studies. In Val Sesia and Val Strona di Postua to the south the exposure is more restricted. P–T estimates for the metapelites are 750–850 °C and 5–6.5 kbar in Val Sesia and approximately 800–900 °C and 5.5–7 kbar in Val Strona di Postua. These results show similar temperatures but lower pressure than metapelites in Val Strona di Omegna. Metapelites in Val Sesia in contact with the Mafic Complex exhibit a metatexitic structure, while in Val Strona di Postua diatexitic structures occur. Further, metapelites at the contact with the Mafic Complex contain cordierite (± spinel) that overprint the regional metamorphic assemblages and are interpreted to have formed during contact metamorphism related to intrusion of the Mafic Complex. The lower pressures in the high-grade rocks in Val Sesia and Val Strona di Postua are consistent with some decompression from the regional metamorphic peak prior to the intrusion of the Mafic Complex, suggesting the rocks followed a clockwise P–T path. In contrast, the metapelites in Val Strona di Omegna, especially in the granulite facies, do not contain any cordierite or any evidence for a contact metamorphic overprint. The extrapolated granulite facies mineral isograds are cut by the rocks of the Mafic Complex to the south. Therefore, the Mafic Complex cannot have caused the regional metamorphism and it is unlikely that the Mafic Complex occurs in Val Strona di Omegna.