Articles | Volume 17, issue 7
https://doi.org/10.5194/bg-17-2085-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-2085-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Authigenic formation of Ca–Mg carbonates in the shallow alkaline Lake Neusiedl, Austria
Dario Fussmann
CORRESPONDING AUTHOR
Geobiology, Geoscience Centre,
Georg-August-Universität Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany
Avril Jean Elisabeth von Hoyningen-Huene
Genomic and Applied Microbiology and Göttingen Genomics Laboratory, Institute of
Microbiology and Genetics, Georg-August-Universität
Göttingen, Grisebachstraße 8, 37077 Göttingen, Germany
Andreas Reimer
Geobiology, Geoscience Centre,
Georg-August-Universität Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany
Dominik Schneider
Genomic and Applied Microbiology and Göttingen Genomics Laboratory, Institute of
Microbiology and Genetics, Georg-August-Universität
Göttingen, Grisebachstraße 8, 37077 Göttingen, Germany
Hana Babková
Department of Geodynamics and Sedimentology, University of Vienna,
Althanstraße 14, 1090 Vienna, Austria
Robert Peticzka
Department of Geography and Regional Research, University of Vienna,
Althanstraße 14, 1090 Vienna, Austria
Andreas Maier
Department of Geography and Regional Research, University of Vienna,
Althanstraße 14, 1090 Vienna, Austria
Gernot Arp
Geobiology, Geoscience Centre,
Georg-August-Universität Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany
Rolf Daniel
Genomic and Applied Microbiology and Göttingen Genomics Laboratory, Institute of
Microbiology and Genetics, Georg-August-Universität
Göttingen, Grisebachstraße 8, 37077 Göttingen, Germany
Patrick Meister
Department of Geodynamics and Sedimentology, University of Vienna,
Althanstraße 14, 1090 Vienna, Austria
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Latest update: 20 Nov 2024
Short summary
Dolomite (CaMg(CO3)2) is supersaturated in many aquatic settings (e.g., seawater) on modern Earth but does not precipitate directly from the fluid, a fact known as the dolomite problem. The widely acknowledged concept of dolomite precipitation involves microbial extracellular polymeric substances (EPSs) and anoxic conditions as important drivers. In contrast, results from Lake Neusiedl support an alternative concept of Ca–Mg carbonate precipitation under aerobic and alkaline conditions.
Dolomite (CaMg(CO3)2) is supersaturated in many aquatic settings (e.g., seawater) on modern...
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