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Magnesium Inhibition Controls Spherical Carbonate Precipitation in Ultrabasic Springwater (Cedars, California) and Culture Experiments

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Advances in Stromatolite Geobiology

Part of the book series: Lecture Notes in Earth Sciences ((LNEARTH,volume 131))

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)

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Acknowledgements

We thank Monika Segl (University of Bremen) and Gaute Lavik (MPI, Bremen) for isotope analysis, as well as Peter Schiffman (UC Davis) for allowing us to present his unpublished isotope data. Gail Arnold (MPI, Bremen) and Carolina Reyes (UC Santa Cruz) provided useful comments and improved the clarity of the manuscript. Discussions with Gijs Kuenen, Ana Obraztsova, John Platt, and Rolf Warthmann contributed significantly to the study. We thank Damon Rogers for giving us the opportunity to visit the Cedars Springs and for allowing us to use his camping facility. This study was sponsored by the Agouron Institute and the Swiss National Science Foundation (SNF).

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Authors and Affiliations

  1. Max-Planck-Institute for Marine Microbiology, Celsiusstr. 1, 28359, Bremen, Germany

    Patrick Meister

  2. Department of Earth Sciences, University of Southern California, 3651 Trousdale Parkway, Los Angeles, CA, 90089-0740, USA

    Orion Johnson, Frank Corsetti & Kenneth H. Nealson

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  1. Patrick Meister
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Correspondence to Patrick Meister .

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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: Advances in Stromatolite Geobiology. Lecture Notes in Earth Sciences, vol 131. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-10415-2_6

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