Abstract
The monoclinic mineral ikaite (CaCO3 center dot 6H(2)O) and itspseudomorphs are potentially important archives for palaeoenvironmentalreconstructions. Natural ikaite occurs in a small temperature range nearfreezing point and is reported mainly from marine and only rarely fromcontinental aquatic environments. Ikaite transforms to more stableanhydrous forms of CaCO3 after an increase in temperature or whenexposed to atmospheric conditions. The knowledge about conditions fornatural ikaite formation, its stable isotope fractionation factors andisotopic changes during transformation to calcite is very restricted.Here, for the first time, primary precipitation of idiomorphic ikaiteand its calcite pseudomorphs are reported from a subsaline lake, LagunaPotrok Aike, in southern Argentina. The calculated stable oxygen isotopefractionation factor between lake water and ikaite-derived calcite
Dokumententyp: | Zeitschriftenartikel |
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Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften > Kristallographie und Materialwissenschaft |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
Sprache: | Englisch |
Dokumenten ID: | 18797 |
Datum der Veröffentlichung auf Open Access LMU: | 10. Mrz. 2014, 14:14 |
Letzte Änderungen: | 04. Nov. 2020, 13:00 |