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Wakabayashilite, [(As,Sb)₆S₉][As₄S₅]: Crystal structure, pseudosymmetry, twinning, and revised chemical formula

¹ Dipartimento di Scienze della Terra, Università degli Studi di Firenze, via La Pira 4, I-50121 Firenze, Italy
² Museo di Storia Naturale, sezione di Mineralogia, Università degli Studi di Firenze, via La Pira 4, I-50121 Firenze, Italy
³ Dipartimento di Scienze della Terra, Università degli Studi di Ferrara, Corso Ercole I d Este 32, I-44100 Ferrara, Italy

Correspondence: ^* E-mail: paola.bonazzi{at}geo.unifiit

The crystal structure of the rare mineral wakabayashilite was solved by direct methods using intensity data collected from a twinned crystal. This study revealed that, in spite of the strong hexagonal pseudosymmetry, the structure is orthorhombic (space group Pna2₁) with a_o = 25.262(1), b_o = 14.563(1), c_o = 6.492(1) Å, and V_o = 2388.4(2) ų. The refinement of an anisotropic model led to an R index of 6.08% for 3135 observed reflections [F_o > 4(F_o)] and 8.71% for all 4260 independent reflections. Wakabayashilite is twinned by reticular merohedry [twin plane (110)]. There are two structural units in the structure: (1) [M₆S₉] bundle-like chains running along the [001] axis, consisting of corner-sharing MS₃ trigonal pyramids (M = As, Sb), and (2) rods of As₄S₅ cage-like molecules, located in the space between three bundles and held together by van der Waals forces. The crystal chemical formula was therefore revised according to the structural results, yielding [(As,Sb)₆S₉][As₄S₅] (Z = 4). Both the intramolecular As-S and As-As bond distances and those within the bundle-like units match closely the values commonly observed in the molecule-formed structures of other arsenic sulfides and those found in orpiment, respectively. To contribute to the understanding of the effects of light exposure on the structure of the arsenic sulfides, the crystal was exposed to filtered polychromatic light. The unit-cell parameters were measured after each exposure. The results showed that the As₄S₅ molecules do not undergo any transformations, as previously found by exposing uzonite to light.

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