Elektrochemische Desoxygenierung von Carbonsäureamiden und verwandten Verbindungen an der dekorierten Bleikathode

Zusammenfassung der Dissertation, Carolin Edinger, April 2015. Im Rahmen der Dissertation ist eine effiziente und zuverlässige Methode zur elektrochemischen Desoxygenierung von aromatischen Carbonsäureamiden entwickelt worden (Schema 1).[1] Unter galvanostatischen Bedingungen eignet sich das optimierte Elektrolytsystem bestehend aus 2%iger methanolischer H2SO4 und geringen Mengen an Additiv 1 in Kombination mit einer Bleikathode hervorragend in dem gewählten geteilten Zellaufbau. Schema 1: Elektrochemische Desoxygenierung aromatischer Carbonsäureamide. Untersuchungen an verschiedensten Amidsubstraten haben gezeigt, dass ein breites Spektrum an Aminen mit dieser Methode zugänglich ist und durch umfangreiche Studien konnten optimale Elektrolyseparameter gefunden werden. Außerdem wurde die Hochskalierung der Ansatzgröße an einem Testsubstrat mit hohen Aminausbeuten von bis zu 73% gewährleistet. Ein besonderes Merkmal der entwickelten Synthese ist neben milden Bedingungen und hoher Selektivität die Verwendung von Ammoniumsalzadditiven. Der positive Effekt dieser Additive auf die Desoxygenierungsreaktion ist vielfältig: Die Wasserstoffentwicklung als unerwünschte Nebenreaktion wird zu negativeren Potentialen verschoben und die Bleikathode wird durch Zurückdrängung der PbSO4-Bildung effektiv vor Korrosion geschützt. Dies konnte durch experimentelle Werte wie die Erhöhung der Produkt- und Stromausbeute durch Additivzusatz während der Elektrolyse hinreichend bestätigt werden. Aber auch zyklovoltammetrische Untersuchungen und Lichtmikroskopaufnahmen der Elektrodenoberfläche bekräftigen eindeutig diese Aussagen.[2,3] Die entwickelte elektrochemische Methode konnte zusätzlich erfolgreich auf Verbindungen übertragen werden, die mit Carbonsäureamiden verwandt sind. So gelang es, aromatische und aliphatische Sulfoxide in sehr guten Ausbeuten selektiv zu den entsprechenden Sulfiden umzusetzen. Zusätzlich konnten bereits bei weiteren, durch klassische Methoden schwer reduzierbare Stoffklassen erste Erfolge erzielt werden. So gelang es, den Grundstein zur Reduktion von Estern und Triphenylphosphinoxid zu legen und erste, vielversprechende Ergebnisse zu erlangen. Da Elektronen als Reduktionsmittel eingesetzt werden und lediglich Wasser als Nebenprodukt gebildet wird, zeichnet sich die entwickelte Desoxygenierungsmethode vor allem durch milde Bedingungen und hohe Selektivität aus. Da weder Reagenzien noch Katalysatoren verwendet werden müssen, werden Abfälle vermieden. Dadurch ist die gefundene Reduktionsmethode nicht nur kostengünstig, sondern erweist sich auch in der Reaktionsführung als vorteilhaft. Literatur: [1] C. Edinger, S. R. Waldvogel, Eur. J. Org. Chem. 2014, 2014, 5144–5148. [2] C. Edinger, V. Grimaudo, P. Broekmann, S. R. Waldvogel, ChemElectroChem 2014, 1, 1018–1022. [3] C. Edinger, S. R. Waldvogel, PCT Int. Appl. 2013, WO 2013030316A2.

Breakpoint analysis of human chromosome 3 inversions during hominoid evolution

Comparative fluorescence in situ hybridization (FISH) mapping revealed four large DNA segments which have been conserved in their entirety between human chromosome 3 and Bornean orangutan chromosome 2 as well as three evolutionary breakpoints which distinguish between the human and Bornean orangutan chromosome forms. Examination of the structural and functional features of evolutionary breakpoints provides new insights into the possible effects of evolutionary rearrangements on genome function and the relationship between human chromosome pathology and evolution. FISH of human BAC clones which were assesssed in human genomic sequence to primate chromosomes, combined with precise breakpoint localizations by polymerase chain reaction (PCR) analysis of flow-sorted chromosomes and in silico analysis, were used to characterize the evolutionary breakpoints. None of the three breakpoints studied disrupts a validated gene(s), however they are all associated with segmental duplications. At least eleven DNA segments (&a

Jaw mechanics of the pterosaur skull construction and the evolution of toothlessness

In the present study, pterosaur skull constructions were analysed using a combined approach of finite element analysis (FEA), static investigations as well as applying classical beam theory and lever mechanics. The study concentrates on the operating regime „bite“, where loads are distributed via the dentition or a keratinous rhamphotheca into the skull during jaw occlusion. As a first step, pterosaur tooth constructions were analysed. The different morphologies of the tooth construction determine specific operational ranges, in which the teeth perform best (= greatest resistance against failure). The incomplete enamel-covering of the pterosaur tooth constructions thereby leads to a reduction of strain and stress and to a greater lateral elasticity than for a complete enamel cover. This permits the development of high and lateral compressed tooth constructions. Further stress-absorption occurs in the periodontal membrane, although its mechanical properties can not be clarified unambiguously. A three-dimensionally preserved skull of Anhanguera was chosen as a case-study for the investigation of the skull constructions. CT-scans were made to get information about the internal architecture, supplemented by thin-sections of a rostrum of a second Anhanguera specimen. These showed that the rostrum can be approximated as a double-walled triangular tube with a large central vacuity and an average wall-thickness of the bony layers of about 1 mm. On base of the CT-scans, a stereolithography of the skull of Anhanguera was made on which the jaw adductor and abductor muscles were modelled, permitting to determine muscular forces. The values were used for the lever mechanics, cantilever and space frame analysis. These studies and the FEA show, that the jaw reaction forces are critical for the stability of the skull construction. The large jugal area ventral to the orbita and the inclined occipital region act as buttresses against these loads. In contrast to the orbitotemporal region which is subject to varying loading conditions, the pattern in the rostrum is less complex. Here, mainly bending in dorsal direction and torsion occur. The hollow rostrum leads to a reduction of weight of the skull and to a high bending and torsional resistance. Similar to the Anhanguera skull construction, the skulls of those pterosaur taxa were analysed, from which enough skull material is know to permit a reliable reconstruction. Furthermore, FEA were made from five selected taxa. The comparison of the biomechanical behaviour of the different skull constructions results in major transformational processes: elongation of rostra, inclination of the occipital region, variation of tooth morphology, reduction of the dentition and replacement of teeth by a keratinous hook or rhamphotheca, fusion of naris and antorbital fenestra, and the development of bony and soft-tissue crests. These processes are discussed for their biomechanical effects during bite. Certain optional operational ranges for feeding are assigned to the different skull constructions and previous hypotheses (e.g. skimming) are verified. Using the principle of economisation, these processes help to establish irreversible transformations and to define possible evolutionary pathways. The resulting constructional levels and the structural variations within these levels are interpreted in light of a greater feeding efficiency and reduction of bony mass combined with an increased stability against the various loads. The biomechanical conclusive pathways are used for comparison and verification of recent hypothesis of the phylogenetic systematics of pterosaurs.

Petrogenetic evolution of Uralian-Alaskan-type mafic-ultramafic complexes in the southern and middle Urals, Russia

The PhD thesis at hand consists of three parts and describes the petrogenetic evolution of Uralian-Alaskan-type mafic ultramafic complexes in the Ural Mountains, Russia. Uralian-Alaskan-type mafic-ultramafic complexes are recognized as a distinct class of intrusions. Characteristic petrologic features are the concentric zonation of a central dunite body grading outward into wehrlite, clinopyroxenite and gabbro, the absence of orthopyroxene and frequently occurring platinum group element (PGE) mineralization. In addition, the presence of ferric iron-rich spinel discriminates Uralian-Alaskan-type complexes from most other mafic ultramafic rock assemblages. The studied Uralian-Alaskan-type complexes (Nizhnii Tagil, Kytlym and Svetley Bor) belong to the southern part of a 900 km long, N–S-trending chain of similar intrusions between the Main Uralian Fault to the west and the Serov-Mauk Fault to the east. The first chapter of this thesis studies the evolution of the ultramafic rocks tracing the compositional variations of rock forming and accessory minerals. The comparison of the chemical composition of olivine, clinopyroxene and chromian spinel from the Urals with data from other localities indicates that they are unique intrusions having a characteristic spinel and clinopyroxene chemistry. Laser ablation-ICPMS (LA-ICPMS ) analyses of trace element concentrations in clinopyroxene are used to calculate the composition of their parental melt which is characterized by enriched LREE (0.5-5.2 prim. mantle) and other highly incompatible elements (U, Th, Ba, Rb) relative to the HREE (0.25-2.0 prim. mantle). A subduction-related geotectonic setting is indicated by a positive anomaly for Sr and negative anomalies for Ti, Zr and Hf. The mineral compositions monitor the evolution of the parental magmas and decipher differences between the studied complexes. In addition, the observed variation in LREE/HREE (for example La/Lu = 2-24) can be best explained with the model of an episodically replenished and erupted open magma chamber system with the extensive fractionation of olivine, spinel and clinopyroxene. The data also show that ankaramites in a subduction-related geotectonic setting could represent parental magmas of Uralian-Alaskan-type complexes. The second chapter of the thesis discusses the chemical variation of major and trace elements in rock-forming minerals of the mafic rocks. Electron microprobe and LA-ICPMS analyses are used to quantitatively describe the petrogenetic relationship between the different gabbroic lithologies and their genetic link to the ultramafic rocks. The composition of clinopyroxene identifies the presence of melts with different trace element abundances on the scale of a thin section and suggests the presence of open system crustal magma chambers. Even on a regional scale the large variation of trace element concentrations and ratios in clinopyroxene (e.g. La/Lu = 3-55) is best explained by the interaction of at least two fundamentally different magma types at various stages of fractionation. This requires the existence of a complex magma chamber system fed with multiple pulses of magmas from at least two different coeval sources in a subduction-related environment. One source produces silica saturated Island arc tholeiitic melts. The second source produces silica undersaturated, ultra-calcic, alkaline melts. Taken these data collectively, the mixing of the two different parental magmas is the dominant petrogenetic process explaining the observed chemical variations. The results further imply that this is an intrinsic feature of Uralian-Alaskan-type complexes and probably of many similar mafic-ultramafic complexes world-wide. In the third chapter of this thesis the major element composition of homogeneous and exsolved spinel is used as a petrogenetic indicator. Homogeneous chromian spinel in dunites and wehrlites monitors the fractionation during the early stages of the magma chamber and the onset of clinopyroxene fractionation as well as the reaction of spinel with interstitial liquid. Exsolved spinel is present in mafic and ultramafic rocks from all three studied complexes. Its composition lies along a solvus curve which defines an equilibrium temperature of 600°C, given that spinel coexists with olivine. This temperature is considered to be close to the temperature of the host rocks into which the studied Uralian-Alaskan-type complexes intruded. The similarity of the exsolution temperatures in the different complexes over a distance of several hundred kilometres implies a regional tectonic event that terminated the exsolution process. This event is potentially associated with the final exhumation of the Uralian-Alaskan-type complexes along the Main Uralian Fault and the Serov-Mauk Fault in the Uralian fold belt.