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Purvis, O. W., Pawlik-Skowrońska, B., Cressey, G., Jones, G. C., Kearsley, A., Spratt, J. (2008) Mineral phases and element composition of the copper hyperaccumulator lichen Lecanora polytropa. Mineralogical Magazine, 72 (2) 607-616 doi:10.1180/minmag.2008.072.2.607

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Reference TypeJournal (article/letter/editorial)
TitleMineral phases and element composition of the copper hyperaccumulator lichen Lecanora polytropa
JournalMineralogical Magazine
AuthorsPurvis, O. W.Author
Pawlik-Skowrońska, B.Author
Cressey, G.Author
Jones, G. C.Author
Kearsley, A.Author
Spratt, J.Author
Year2008 (April)Volume72
Issue2
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2008.072.2.607Search in ResearchGate
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Mindat Ref. ID243911Long-form Identifiermindat:1:5:243911:6
GUID0
Full ReferencePurvis, O. W., Pawlik-Skowrońska, B., Cressey, G., Jones, G. C., Kearsley, A., Spratt, J. (2008) Mineral phases and element composition of the copper hyperaccumulator lichen Lecanora polytropa. Mineralogical Magazine, 72 (2) 607-616 doi:10.1180/minmag.2008.072.2.607
Plain TextPurvis, O. W., Pawlik-Skowrońska, B., Cressey, G., Jones, G. C., Kearsley, A., Spratt, J. (2008) Mineral phases and element composition of the copper hyperaccumulator lichen Lecanora polytropa. Mineralogical Magazine, 72 (2) 607-616 doi:10.1180/minmag.2008.072.2.607
Abstract/NotesAbstractMineral phases and element localization were investigated in the vivid turquoise-coloured lichen, Lecanora polytropa, sampled from a psammite boulder in a wall supporting mine spoil at the abandoned copper mine, Riddarhyttan Kopparverke, southern Sweden. Normally pale yellowish (usnic acid), the lichen is turquoise coloured internally with bluish inclusions. X-ray mapping shows that Cu occurs on and within the lichen and does not coincide with P or S, suggesting that it is indeed associated with carbon or other elements not detected (or reported) using X-ray mapping. Scanning electron microscopy in back-scatter mode confirmed that the greatest Cu concentrations occur in the form of crystalline aggregates in coloured inclusions below the major internal turquoise layer with smaller Cu contents. X-ray diffraction with a position-sensitive detector (XRD-PSD) confirmed coloured crystalline aggregates consisted of the copper oxalate, moolooite. The study confirms the value of XRD-PSD as a non-destructive tool to characterize small (~50 μm) metal oxalate inclusions obtained from within lichen samples.


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