Wampenite, C18H16, is a new organic mineral from the fossil wood (conifer) locality at Wampen, Fichtelgebirge, Bavaria, Germany. It is monoclinic, space group P2 1/a, with a = 6.7331(19), b = 8.689(3), c = 23.709(7)
Å, β = 90.118(6)°, V = 1387.0(7) Å3 and Z = 4. Its structure was determined by single-crystal X-ray diffraction, which revealed that the molecular structure comprises an aromatic phenanthrene moiety with an axial methyl group at one end and a disordered
propen-2-yl (methylvinyl) terminal group at the other. High resolution mass spectrometry (HRMS) confirmed the molecular formula C18 H16 and the IR spectrum is consistent with the molecular structure found.
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HIGH RESOLUTION MASS SPECTROMETRY;
Document Type: Research Article
Publication date: June 1, 2017
This article was made available online on May 31, 2017 as a Fast Track article with title: "Wampenite, C18H16, a new organic mineral from the fossil conifer locality at Wampen, Bavaria, Germany".
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The European Journal of Mineralogy publishes original papers, review articles and letters dealing with the mineralogical sciences s.l. These include primarily mineralogy, petrology, geochemistry, crystallography and ore deposits, as well as environmental, applied and technical mineralogy. Nevertheless, papers in any related field, including cultural heritage, will be considered.
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