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Mg/Ca Ratio and Salinity: Two Controls over Crystallization of Dolomite
Abstract
Carbonate precipitation is governed by both thermodynamic and kinetic considerations. The concentration and ionic composition of natural solutions influence not only the mineralogy of the precipitate, but also the crystal size and habit of both metastable and stable phases. Under marine conditions sparry calcite does not precipitate because of poisoning of sideward crystal growth by Mg, which forces Mg-calcite and aragonite to assume a micritic, steep-rhombic, or fibrous habit. Blocky calcite can form only in low Mg/Ca waters, either from primary meteoric solutions, or where Mg has been removed from marine water by dolomite or clays. In hypersaline environments precipitation is commonly rapid and, together with the high concentrations of foreign ions, it is difficult for dolomite to form because of the precise Ca-Mg ordering required. Instead, aragonite or Mg-calcite crystallizes. Dolomite can form only if the Mg/Ca ratio exceeds 5-10:1, and even then it is aphanitic and poorly ordered. At progressively reduced salinities dolomite is able to nucleate at still lower Mg/Ca ratios, approaching 1:1 in meteoric waters. The absence of foreign ions and slow crystallization, commonly under phreatic conditions, cause both dolomite and calcite to form exquisitely limpid, euhedral rhombs. Thus, dolomite probably forms most readily by a reduction in salinity, particularly in a schizohaline environment (alternating between hypersaline and near-fresh conditions, as in a floodable sabkha or…
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“Carbonate precipitation is controlled by both kinetic and thermodynamic considerations [12].”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [12]
In the citing paper
“In such environments biogenic proto-dolomite forms at ambient to moderately high temperatures (e.g., alkaline lakes or shabkhas T between 27-50 ° C), high alkalinities (up to 500 mM), and high-Mg:Ca concentration ratios (>1:1 to 100:1) (Folk and Land 1975; Last and De Deckker 1990; Meister et al. 2011 and references therein).”
From A route for the direct crystallization of dolomite (2015) · cites this paper as Folk and Land 1975
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Metadata
- Authors
- Folk, R. L., & Land, L. S.
- Affiliations
- Austin, Texas 78712
- Venue
- AAPG Bulletin
- Published
- 1975-01-01
- Volume
- 59
- Issue
- 1
- Pages
- 60-68
- ISSN
- 0149-1423 (ISSN-L)
- 1558-9153
- OpenAlex
- W2132147684
- Cited by
- 445
- References
- 37
- Citations by year
- 2026: 1 · 2025: 8 · 2024: 8 · 2023: 13 · 2022: 8 · 2021: 17 · 2020: 16 · 2019: 15 · 2018: 8 · 2017: 20 · 2016: 17 · 2015: 13 · 2014: 8 · 2013: 7 · 2012: 7
- FWCI
- 7.97
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- AAPG Bulletin (publishedVersion)
- Topics
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Keywords
- Mg/Ca ratio, salinity, carbonate precipitation, Mg-calcite, aragonite, sparry calcite, crystal morphology, nucleation, sabkha, hypersaline water, meteoric water, coexisting ions
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