Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia
<p>Phosphate minerals hydroxylapatite, fluorapatite and crandallite were identified in nodules within phosphorites from Ervenik, Croatia. The minerals were identified using optical microscopy, XRD, SEM and EDX analyses. The presence of fungi was recognized only in association with phosphate-ri...
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Croatian Geological Survey
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doaj-da56f86161764769ae77ec85a0c63e652020-11-25T00:36:57ZengCroatian Geological SurveyGeologia Croatica1330-030X1333-48752012-02-01651677510.4154/GC.2012.05401Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, CroatiaVladimir Bermanec0Hrvoje Posilović1Željka Žigovečki Gobac2Jasna Hrenović3Nevenka Mikac4Goran Kniewald5Faculty of Science, University of Zagreb, Horvatovac 95, 10000 Zagreb, CroatiaFaculty of Science, University of Zagreb, Horvatovac 102a, 10000 Zagreb, CroatiaFaculty of Science, University of Zagreb, Horvatovac 95, 10000 Zagreb, CroatiaFaculty of Science, University of Zagreb, Rooseveltov trg 6, 10000 Zagreb, CroatiaRudjer Bosković Institute, Bijenička 54, 10000 Zagreb, CroatiaRudjer Bosković Institute, Bijenička 54, 10000 Zagreb, Croatia<p>Phosphate minerals hydroxylapatite, fluorapatite and crandallite were identified in nodules within phosphorites from Ervenik, Croatia. The minerals were identified using optical microscopy, XRD, SEM and EDX analyses. The presence of fungi was recognized only in association with phosphate-rich phases. Fungal activity resulted in the dissolution of apatite, producing hollow crystals, particularly in hydroxylapatite – enriched zones. A substantial number of hyphae were observed on the surface of phosphate minerals, in addition to saprophytic bacteria and bacterial spores. Induced activity of phosphate-accumulating bacteria in an aquatic environment caused dissolution of the phosphate minerals. The aqueous phase contained increased concentrations of several elements, including Ca, Sb, U, V and As. These elements are important constituents of minerals of the apatite group. As a consequence of the crystallization of apatite, the concentration of phosphate decreases with a corresponding increase in aluminium concentration, resulting in the prevalence of crandallite as the stable phase, forming the outer sector of the spherulites. </p><p> </p>http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/522phosphorite, hydroxylapatite, fluorapatite, crandallite, fungi, bacteria |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Vladimir Bermanec Hrvoje Posilović Željka Žigovečki Gobac Jasna Hrenović Nevenka Mikac Goran Kniewald |
spellingShingle |
Vladimir Bermanec Hrvoje Posilović Željka Žigovečki Gobac Jasna Hrenović Nevenka Mikac Goran Kniewald Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia Geologia Croatica phosphorite, hydroxylapatite, fluorapatite, crandallite, fungi, bacteria |
author_facet |
Vladimir Bermanec Hrvoje Posilović Željka Žigovečki Gobac Jasna Hrenović Nevenka Mikac Goran Kniewald |
author_sort |
Vladimir Bermanec |
title |
Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia |
title_short |
Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia |
title_full |
Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia |
title_fullStr |
Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia |
title_full_unstemmed |
Mineralogical and geomicrobiological investigation of phosphorite from Ervenik, Croatia |
title_sort |
mineralogical and geomicrobiological investigation of phosphorite from ervenik, croatia |
publisher |
Croatian Geological Survey |
series |
Geologia Croatica |
issn |
1330-030X 1333-4875 |
publishDate |
2012-02-01 |
description |
<p>Phosphate minerals hydroxylapatite, fluorapatite and crandallite were identified in nodules within phosphorites from Ervenik, Croatia. The minerals were identified using optical microscopy, XRD, SEM and EDX analyses. The presence of fungi was recognized only in association with phosphate-rich phases. Fungal activity resulted in the dissolution of apatite, producing hollow crystals, particularly in hydroxylapatite – enriched zones. A substantial number of hyphae were observed on the surface of phosphate minerals, in addition to saprophytic bacteria and bacterial spores. Induced activity of phosphate-accumulating bacteria in an aquatic environment caused dissolution of the phosphate minerals. The aqueous phase contained increased concentrations of several elements, including Ca, Sb, U, V and As. These elements are important constituents of minerals of the apatite group. As a consequence of the crystallization of apatite, the concentration of phosphate decreases with a corresponding increase in aluminium concentration, resulting in the prevalence of crandallite as the stable phase, forming the outer sector of the spherulites. </p><p> </p> |
topic |
phosphorite, hydroxylapatite, fluorapatite, crandallite, fungi, bacteria |
url |
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/522 |
work_keys_str_mv |
AT vladimirbermanec mineralogicalandgeomicrobiologicalinvestigationofphosphoritefromervenikcroatia AT hrvojeposilovic mineralogicalandgeomicrobiologicalinvestigationofphosphoritefromervenikcroatia AT zeljkazigoveckigobac mineralogicalandgeomicrobiologicalinvestigationofphosphoritefromervenikcroatia AT jasnahrenovic mineralogicalandgeomicrobiologicalinvestigationofphosphoritefromervenikcroatia AT nevenkamikac mineralogicalandgeomicrobiologicalinvestigationofphosphoritefromervenikcroatia AT gorankniewald mineralogicalandgeomicrobiologicalinvestigationofphosphoritefromervenikcroatia |
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