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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.1986.050.356.14</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Spheniscidite, a New Phosphate Mineral from Elephant Island, British Antarctic Territory</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Wilson</surname>
<given-names>M. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Bain</surname>
<given-names>D. C.</given-names>
</name></contrib>
<aff>Department of Mineral Soils, the Macaulay Institute for Soil Research, Craigiebuckler, Aberdeen</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1986</year>
</pub-date>
<volume>50</volume>
<issue>356</issue>
<fpage>291</fpage>
<lpage>293</lpage>
<history>
<date date-type="received">
<day>22</day>
<month>11</month>
<year>1985</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1986, The Mineralogical Society</copyright-statement>
<copyright-year>1986</copyright-year>
<abstract>
<title>Abstract</title>
<p>Spheniscidite is a new phosphate mineral occurring in a soil profile in an area of nesting penguins on Elephant Island. It is the NH<sub>4</sub>-dominant analogue of leucophosphite and has the formula (NH<sub>4</sub>,K)(Fe<sup>3+</sup>,Al)<sub>2</sub> (PO<sub>4</sub>)<sub>2</sub>(OH) &#x00B7; 2H<sub>2</sub>O. It is monoclinic, <italic>P2<sub>1</sub>/n</italic> with unit cell parameters <italic>a</italic> = 9.75, <italic>b</italic> = 9.63, <italic>c</italic> = 9.70 &#x00C5;, &#x03B2; = 102&#x00B0; 34&#x2032;, and Z = 4. The strongest X-ray lines are 6.79(100), 5.99(90), 3.05(45), 7.62(40) &#x00C5;. Spheniscidite is thought to have formed by the interaction of ammonium phosphate solutions from penguin guano with micaceous and chloritic minerals in the soil. The name is for Sphenisciformes, the order name for penguins, and has been approved by the IMA Commission on New Minerals and Mineral Names.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>spheniscidite</kwd>
<kwd>phosphate minerals</kwd>
<kwd>new minerals</kwd>
<kwd>Elephant Island</kwd>
<kwd>Antarctica</kwd>
</kwd-group>
</article-meta>
</front>
</article>
