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Glushinskite, a naturally occurring magnesium oxalate

  • M. J. Wilson (a1), D. Jones (a1) and J. D. Russell (a1)

Summary

Glushinskite, a dihydrate of magnesium oxalate, occurs at the lichen/rock interface on serpentinite colonized by Lecanora atra at Mill of Johnston, near Insch in north-east Scotland. It is found in a creamy white layer intermingled with the hyphae of the lichen fungus. It consists of crystals mainly 2 to 5 µm in size showing a distorted pyramidal form, often with curved and striated faces. X-ray, infrared, and chemical data are given.

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References

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Dubernat, (J.) and Pézérat, (H.), 1974. J. Appl. Cryst. 7, 387-93.
Hey, (M. H.), 1963. Appendix to Chemical Index of Minerals. British Museum (Nat. Hist.).
Jones, (D.), Wilson, (M. J.), and Tait, (J. M.), 1980. Lichenologist (in press).
Lagier, (J.-P.), Pézérat, (H.), and Dubernat, (J.), 1969. Rev. Chim. Mineral. 6, l081-93.
Walter Levy, (L.), Perrotey, (J.), and Visser, (J. W.), 1971. Bull. Soc. Chim. 757-61.
Zhemchuzhnikov, (Y. A.) and Ginzburg, (A. I.), 1960. The Principles of Coal Petrology. Acad. Sci. USSR. [M. A. 16–555].

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