Dolomite in caves: Recent dolomite formation in oxic, non-sulfate environments. Castañar Cave, Spain |
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| Authors: | Ana M Alonso-Zarza Andrea Martín-Prez |
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| Institution: | aDpto. de Petrología y Geoquímica, Fac. CC. Geológicas—Instituto de Geología Económica, Universidad Complutense-CSIC, 28040 Madrid, Spain |
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| Abstract: | Dolomite is a common mineral in the rock record but rare in recent superficial environments. Where it does occur, it is related to anoxic, sulfate-rich environments and microbial activity. The occurrence of some dolomite deposits in caves, however, indicates that dolomite formation is also possible in oxic, non-sulfate settings. Dolomite is forming at 17 °C and in oxic-vadose conditions on the host rocks and aragonite speleothems of the Castañar Cave, Cáceres, Spain. It appears as spheroids and dumbbells 50–300 μm in diameter that internally consist of micron-sized rhombic to rounded crystals. Initially this dolomite is Ca-rich, non-stoichiometric and poorly ordered. Mg-rich solutions allow the precipitation of metastable Mg-rich carbonates, such as huntite. This soon transforms into this Ca-rich dolomite, which later “ages” to form a more stoichiometric dolomite. These dolomites show similarities to those grown under anoxic, sulfate-rich conditions and their presence in caves provides a different setting that may contribute to the understanding of the “dolomite problem”, including their initial formation and later recrystallization processes. |
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| Keywords: | Dolomite Caves Huntite Low-temperature Recent Castañar Cave Spain |
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