ArticleRSC advances2021
Systematic laboratory approach to produce Mg-rich carbonates at low temperature.
Article in RSC advances, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.
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2 citing papers in PubMed.
- Formation and stabilisation of nesquehonite in the presence of glucose and xanthan gum.RSC advances · 2026Article
- Characterizing carbonate mineral-forming bacterial strains and their carbonic anhydrase activities in two coastal sabkhas.Biochemistry and biophysics reports · 2025Article
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Authors and funding
8 authors.
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Abstract
Dolomite is a common Mg-rich carbonate in the geological record, but the mechanism of its formation remains unclear. At low temperature, the incorporation of magnesium ions into the carbonate minerals necessary to form dolomite is kinetically inhibited. Over the decades, several factors that possibly allow for overcoming this kinetic barrier have been proposed, and their effectiveness debated. Here, we present the results of a large number of laboratory precipitation experiments that have been designed to identify and compare the factors that promote the formation of Mg-rich carbonates. Under the tested conditions, the most interesting observations include: (1) from solutions that mimic evaporitic seawater, the maximum mol% of Mg incorporated in high Mg calcite is 35, (2) carbonates with a mol% of Mg above 40 were obtained exclusively in the presence of organic molecules, (3) no correlation was observed between the charge of the organic molecules and the incorporation of Mg, (4) the mode (
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