Abstract Es braucht nicht immer ein Metall : Massenspektrometrie und quantenchemische Rechnungen liefern für [P 4 O 10 ] .+ – als erstes nichtmetallisches Oxidkation – Belege, dass es in der Lage ist, die C‐H‐Bindung in Methan bei Raumtemperatur zu aktivieren (siehe Bild). Damit wird das Konzept der sauerstoffzentrierten Radikale um ein weiteres Beispiel erweitert. magnified image
Heterochiral self-sorting into only one stereoisomer is observed when metallo-supramolecular squares self-assemble from amino acid-substituted, dynamically interconverting bipyridine stereoisomers and dpppM(OTf)(2) corners (M = Pd, Pt).
An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
The oxidation of small alkanes by the vanadium oxide cation VO2+ in the gas phase has been studied by Fourier transform ion-cyclotron resonance mass spectrometry (FTICR-MS). Sophisticated mass spectrometric experiments in conjunction with investigation of deuterium-labeled substances are used to elucidate the mechanistic details of the reactions. In marked contrast to oxidative dehydrogenation followed by elimination of ethene in the reaction of VO2+ with ethane, the corresponding reaction with propane mainly affords elimination of dihydrogen concomitant with an ionic product assigned to the allyl complex (η3-C3H5)V(O)(OH)+. In the case of n-butane/VO2+, a combined loss of H2 and H2O provides yet another product channel. Branching ratios, reaction rates, and some mechanistic aspects of the oxidation of propane, n-butane, and isobutane by VO2+ are reported. The experiments are complemented by a computational study of the potential energy surface of propane/VO2+ by means of density functional theory.
An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
Abstract For Abstract see ChemInform Abstract in Full Text.
An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
A Leu-Ala-Leu tripeptide, which bears pyridinyl units at the N- as well as C-terminus, is prepared by combination of solid- and solution-phase synthesis. With the Pd(en)2+ fragment it forms a mixture of 1:1 and 2:2 complexes, with the mononuclear complex probably being the dominating species.
This review provides an overview of organic compounds detected in non-avian dinosaur fossils to date. This was enabled by the development of sensitive analytical techniques. Non-destructive methods and procedures restricted to the sample surface, e.g., light and electron microscopy, infrared (IR) and Raman spectroscopy, as well as more invasive approaches including liquid chromatography coupled to tandem mass spectrometry (LC-MS/MS), time-of-flight secondary ion mass spectrometry, and immunological methods were employed. Organic compounds detected in samples of dinosaur fossils include pigments (heme, biliverdin, protoporphyrin IX, melanin), and proteins, such as collagens and keratins. The origin and nature of the observed protein signals is, however, in some cases, controversially discussed. Molecular taphonomy approaches can support the development of suitable analytical methods to confirm reported findings and to identify further organic compounds in dinosaur and other fossils in the future. The chemical properties of the various organic compounds detected in dinosaurs, and the techniques utilized for the identification and analysis of each of the compounds will be discussed.