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Magnesium inhibition controls spherical carbonate precipitation in ultrabasic springwater (Cedars, California) and culture experiments

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Meister,  Patrick
Permanent Research Group Microsensor, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Citation

Meister, P., Johnson, O., Corsetti, F., & Nealson, K. H. (2011). Magnesium inhibition controls spherical carbonate precipitation in ultrabasic springwater (Cedars, California) and culture experiments. In J. Reitner (Ed.), Advances in Stromatolite Geobiology (pp. 101-121). Berlin, Heidelberg: Springer Berlin Heidelberg.


Cite as: http://hdl.handle.net/21.11116/0000-0001-CA37-E
Abstract
The formation of spherical mineral aggregates is commonly observed in nature and well-known from carbonates formed in marine and hypersaline environments and based on their internal structure called ooids, pellets, pisolites, etc. (e.g. Bathurst 1967; Donahue 1969; Davies et al. 1978; Tucker 1984; Tucker and Wright 1990)