The biosynthetic origin of oxygen functions in phenylphenalenones of Anigozanthos preissii inferred from NMR- and HRMS-based isotopologue analysis |
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Authors: | Munde Tobias Maddula Ravi K Svatos Ales Schneider Bernd |
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Affiliation: | Max Planck Institute for Chemical Ecology, Beutenberg Campus, Hans-Knöll-Straße 8, D-07745 Jena, Germany |
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Abstract: | The biosynthetic origin of 9-phenylphenalenones and the sequence according to which their oxygen functionalities are introduced were studied using nuclear magnetic resonance (NMR) spectroscopy and high-resolution electrospray ionization mass spectrometry (HRESIMS). 13C-labelled precursors were administered to root cultures of Anigozanthos preissii, which were simultaneously incubated in an atmosphere of 18O2. Two major phenylphenalenones, anigorufone and hydroxyanigorufone, were isolated and analyzed by spectroscopic methods. Incorporation of 13C-labelled precursors from the culture medium and 18O from the atmosphere was detected. O-Methylation with 13C-diazomethane was used to attach 13C-labels to each hydroxyl and thereby dramatically enhance the sensitivity with which NMR spectroscopy can detect 18O by means of isotope-induced shifts of 13C signals. The isotopologue patterns inferred from NMR and HRESIMS analyses indicated that the hydroxyl group at C-2 of 9-phenylphenalenones had been introduced on the stage of a linear diarylheptanoid. The oxygen atoms of the carbonyl and lateral aryl ring originated from the hydroxyl group of the 4-coumaroyl moiety, which was incorporated as a unit. |
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Keywords: | Anigozanthos preissii Diarylheptanoids Haemodoraceae Isotope-induced chemical shift Isotope effect Isotopologues Labelling Nuclear magnetic resonance Oxygen-18 Phenylphenalenones |
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