Glycopeptidliganden von Zelladhäsionsrezeptoren mit sulfatierter Arabino-Lewis a-Struktur

Selektine sind eine Gruppe von Transmembranglycoproteinen, welche als Adhäsionsmoleküle innerhalb des vaskulären Systems Zelladhäsionsprozesse zwischen Leukozyten und Endothelzellen vermitteln. Das Sialyl-Lewisa Epitop und verwandte Kohlenhydratstrukturen wurden als Liganden der E- und P-Selektine identifiziert. Durch die chemische Synthese verwandter Strukturen verspricht man sich, die im Laufe inflammatorischer Prozesse exprimierten Rezeptoren gezielt blockieren zu können und dadurch pathologische Abläufe wie hämatogene Metastasierungen oder Abstoßungsreaktionen zu bekämpfen. Einige Bereiche der Aminosäuresequenz des E-Selektin-Ligand-1 (ESL-1) treten hochkonservativ auch in anderen Selektinliganden wie MG160 oder PSGL-1 auf und wurden deshalb für die N-Glycosylierung mit einem sulfatierten Oligosaccharid ausgewählt (11). -Val665-Glu-Cys-Arg-Asp-Ile-Val-Gly-Asn(Sulfo-Lea)-Leu-Tyr-Glu-Leu-Glu-Ser-Glu-Asp-Ile682- 11 Im ersten Teil der Arbeit wurde eine Strategie ausgearbeitet, das sulfatierte Trisaccharid 60 im Multigrammaßstab zu synthetisieren. Der endogene Ligand 2 wurde an drei Positionen modifiziert: Austausch der α-L-Fucose gegen die biologisch stabilere α-D-Arabinose, Einführung einer Sulfatgruppe anstelle der N-Acetylneuraminsäure sowie Übergang von O- zu N-glykosidischer Verknüpfung. Die hochregioselektive Einführung der Sulfatgruppe gelingt in sehr guten Ausbeuten durch Vorkomplexierung mit Dibutylzinnoxid und anschließende Umsetzung mit Schwefeltrioxid/Trimethylamin. Durch die Verwendung des anomeren Azids als permanente Schutzgruppe kann das Trisaccharid nach schonender Reduktion zum Amin an ein Asparaginsäurederivat angekuppelt und in einer linearen Synthese nach Fmoc-Strategie als N-Glycosylaminosäure in die Synthese eingebracht werden. Das in der Arbeitsgruppe Kunz entwickelte PTMSEL-Ankersystem 20a erlaubt sowohl die problemlose Synthese als auch die Abspaltung vom polymeren Träger unter sehr milden Bedingungen. Nach dem Entfernen der Benzylester und -ether durch Pd(0) – katalysierte Hydrierung können sulfatierte Glycopeptidsequenzen des Typs 11 über NMR-Spektroskopie (korrelierte Spektren) und Massenspektroskopie (ESI, MALDI) identifiziert werden.

Oligodeoxynucleotide-polypeptide block copolymers

Synthesis and characterization of monodisperse oligonucleotide-polypeptide di- and triblock copolymers are described. These block copolymers are promising building blocks for the formation of defined structures by sequential DNA self-assembly. The oligonucleotide sequences (ODN, 46 bases) obtained from standard solid phase synthesis were designed to form four-arm DNA junctions. The hybridization of the four single stranded oligonucleotides at room temperature to a stable four-arm junction is selective and quantitative. The junctions exhibit good thermal stability as proven by polyacrylamide gel electrophoresis (PAGE) and UV analysis. The second block consists of monodisperse elastin-like polypeptides (ELPs) with a pentapeptide repeat unit of (Val-Pro-Gly-Val-Gly) synthesized by genetic engineering. ODN-ELP diblock copolymers were obtained either by thiol coupling or by activated ester chemistry. Taking advantage of the endgroup control of both components (ODN, ELP), combination of the two different synthetic approaches leads to the synthesis of ODN-ELP-ODN triblock copolymers. Dynamic light scattering measurements of the single components and the synthesized diblock copolymers reveal their monodispersity. Hybridization of four ODN-ELP diblock copolymers carrying the four junction sequences shows quantitative self-assembly. In conclusion, this work provides the first example of the synthesis of perfectly defined ODN-ELP block copolymers and their potential use in DNA self-assembly.

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.