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<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1987.051.363.12</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Hydrated Copper Oxalate, Moolooite, in Lichens</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Chisholm</surname>
<given-names>J. E.</given-names>
</name>
<xref ref-type="aff" rid="A1">*</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Jones</surname>
<given-names>G. C.</given-names>
</name>
<xref ref-type="aff" rid="A1">*</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Purvis</surname>
<given-names>O. W.</given-names>
</name>
<xref ref-type="aff" rid="A2">&#x2020;</xref></contrib></contrib-group>
<aff id="A1"><label>*</label>Departments of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD</aff>
<aff id="A2"><label>&#x2020;</label>Botany, British Museum (Natural History), Cromwell Road, London SW7 5BD</aff>
<pub-date pub-type="ppub">
<month>12</month>
<year>1987</year>
</pub-date>
<volume>51</volume>
<issue>363</issue>
<fpage>715</fpage>
<lpage>718</lpage>
<history>
<date date-type="received">
<day>12</day>
<month>11</month>
<year>1986</year>
</date>
<date date-type="rev-recd">
<day>12</day>
<month>12</month>
<year>1986</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1987, The Mineralogical Society</copyright-statement>
<copyright-year>1987</copyright-year>
<abstract>
<title>Abstract</title>
<p>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, CuC<sub>2</sub>O<sub>4</sub>. <italic>n</italic>H<sub>2</sub>O (<italic>n</italic> &#x223C; 0.4&#x2013;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.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>moolooite</kwd>
<kwd>lichens</kwd>
<kwd>copper oxalate</kwd>
<kwd>whewellite</kwd>
<kwd>weddellite</kwd>
</kwd-group>
</article-meta>
</front>
</article>
