‘Guanigma’: the revised structure of biogenic anhydrous guanine


  Anna Hirsch [1]  ,  Dvir Gur [2]  ,  Iryna Polishchuk [3]  ,  Davide Levy [3]  ,  Boaz Pokroy [3]  ,  Aurora J. Cruz-Cabeza [4]  ,  Lia Addadi [2]  ,  Leeor Kronik [1]  ,  Leslie Leiserowitz [1]  
[1] Department of Materials and Interfaces, Weizmann Institute of Science, Rehovoth 76100, Israel
[2] Department of Structural Biology, Weizmann Institute of Science, Rehovoth 76100, Israel
[3] Department of Materials science and Engineering, Technion, Haifa 3200003, Israel
[4] School of Chemical Engineering and Analytical Sciences, University of Manchester, The Mill, Sackville Street, Manchester M13 9PL, United Kingdom

Living organisms display a spectrum of wondrous colors, which can be produced by pigmentation, structural coloration, or a combination of the two. A relatively well-studied system, which produces colors via an array of alternating anhydrous guanine crystals and cytoplasm, is responsible for the metallic luster of many fish. The structure of biogenic anhydrous guanine was so far believed to be the same as that of the synthetic one - a monoclinic polymorph (denoted as α). Here we re-examine the structure of biogenic guanine, using detailed experimental X-ray and electron diffraction data, exposing troublesome inconsistencies - namely, a ‘guanigma’. To address this, we sought alternative candidate polymorphs using symmetry and packing considerations, then utilized first principles calculations to determine whether the selected candidates could be energetically stable. We identified theoretically a different monoclinic polymorph (denoted as β), were able to synthesize it, and to confirm using X-ray diffraction that it is this polymorph that occurs in biogenic samples. However, the electron diffraction data was still not consistent with this polymorph, but rather with a theoretically generated orthorhombic polymorph (denoted as γ). This apparent inconsistency was resolved by showing how the electron diffraction pattern could be affected by crystal structural faults composed of offset molecular layers.