Hostname: page-component-8448b6f56d-xtgtn Total loading time: 0 Render date: 2024-04-23T18:50:43.943Z Has data issue: false hasContentIssue false
  • English
  • Français

Hydrated copper oxalate, moolooite, in lichens

Published online by Cambridge University Press:  05 July 2018

J. E. Chisholm ,
G. C. Jones  and
O. W. Purvis
J. E. Chisholm
Affiliation:
Departments of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD
G. C. Jones
Affiliation:
Departments of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD
O. W. Purvis
Affiliation:
Botany, British Museum (Natural History), Cromwell Road, London SW7 5BD
Get access Rights & Permissions [Opens in a new window]

Abstract

Vivid blue inclusions in white whewellite or weddellite, occurring within the medulla of four lichen species growing on copper-bearing rocks, have been identified as the hydrated copper oxalate, moolooite, CuC2O4. nH2O (n ∼ 0.4–0.7), by infrared spectroscopy and X-ray powder diffraction. The mineral is believed to have been formed by reaction between oxalic acid secreted by the lichen and ground or surface water containing copper.

Keywords

moolooitelichenscopper oxalatewhewelliteweddellite
Type
Mineralogy
Information
Mineralogical Magazine , Volume 51 , Issue 363 , December 1987 , pp. 715 - 718
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Antonovsky, A. (1983) CSIRO Division of Chemical and Wood Technology Research Review 1983.Google Scholar
Ascaso, C, Galvan, J., and Rodriguez-Pascual, C. (1982) Pedobiologi. 24, 219-29.Google Scholar
Bari, H. (1982) Mineralogie des Filons du Neuenberg a Sainte Marie-aux-Mines (Haut-Rhin), Thesis, Universite Louis Pasteur, Strasbourg.Google Scholar
Clarke, R.M., and Williams, I.R. (1986) Mineral. Mag. 50, 295-8.CrossRefGoogle Scholar
Czehura, S.J. (1977) Econ. Geol. 72, 796-803.CrossRefGoogle Scholar
Jones, D., Wilson, M.J., and Tait, J.M. (1980) Lichenologist. 12, 277-89.CrossRefGoogle Scholar
Jones, D., Wilson, M.J., and Tait, J.M. and McHardy, W.J. (1981) J. Microscop. 124, 95-104.CrossRefGoogle Scholar
Palache, C, Berman, H., and Frondel, C. (1951) System of Mineralogy, 7th ed., Vol. 2. John Wiley and Sons Inc., New York, p. 1100.Google Scholar
Poelt, J., and Huneck, S. (1968) Öst. Bot. Zeitschr. 115, 411-22.CrossRefGoogle Scholar
Purvis, O.W. (1984) Lichenologis. 16, 197-204.CrossRefGoogle Scholar
Purvis, O.W. (1985) The Effect of Mineralization on Lichen Communities with Special Reference to Cupriferous Substrata, Ph.D. thesis, Imperial College, London and British Museum (Natural History), London,Google Scholar
Purvis, O.W. and James, P.W. (1985) Lichenologis. 17, 221-37.CrossRefGoogle Scholar
Schmittler, H. (1968) Mber. Dt. Akad. Wiss. Berli. 10, 581-604.Google Scholar
Wadsten, T., and Moberg, R. (1985) Lichenologis. 17, 239-45.CrossRefGoogle Scholar
Wilson, M.J., and Jones, D. (1983) In Residual Deposits: Surface Related Weathering Processes and Materials (Wilson, R.C.L., ed.), Geol. Soc. Spec. Pub. 11, 5-12.CrossRefGoogle Scholar
Wilson, M.J., and Jones, D. (1984) Pedobiologi. 26, 373-9.Google Scholar
Wilson, M.J., and Jones, D. and Russell, J.D. (1980) Mineral. Mag. 43, 837-40.CrossRefGoogle Scholar