Catalytic effect of microbially-derived carboxylic acids on the precipitation of Mg-calcite and disordered dolomite: Implications for sedimentary dolomite formation
Open accessAbstract
Abstract The genesis of dolomite is a contentious issue partly due to the difficulty in its synthesis at ambient temperature. Certain types of microorganisms have been demonstrated to be effective in promoting the precipitation of disordered dolomite, an important precursor of sedimentary ordered dolomite. In contrast to a growing body of research on the catalytic role of microbial exopolymers in the crystallization of disordered dolomite, the role of other microbial exudates (e.g., carboxylic acids) remains unknown. To fill in this knowledge gap, precipitation experiments, mimicking the carbonation process within microbial mats, were conducted in saline solutions containing 0–30 mM succinic acid or citric acid, which are commonly produced by microbes. The starting salinities of experiment solutions were set to 35‰ and 70‰, in order to evaluate the effect of solution salinity on dolomite formation. Our results showed that both succinic acid and citric acid enhanced the incorporation of Mg2+ into growing Ca-Mg carbonates. Solution salinity also played a positive role in enhancing Mg signature in Ca-Mg carbonates. Disordered dolomite with 40.92 mol% MgCO3 was detected under the conditions of 30 mM succinic acid and 70‰ salinity, whereas in other reactors with succinic acid, Mg-calcites formed. Citric acid was more effective in loading Mg2+ into Ca-Mg carbonates compared with succinic acid, as evidenced by the predominant occurrence of disordered dolomite with MgCO3 content ranging from 40.91 mol% to 46.75 mol% in most conditions tested. The results of this study have implications for the formation mechanism of sedimentary dolomite.
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Claims the paper makes
13 of 62 cited sources checked · 6 supported · 0 flagged · accuracy not yet measured
- Premisecitation
Disordered dolomite is an important precursor of sedimentary ordered dolomite.
“disordered dolomite, an important precursor of sedimentary ordered dolomite.”
- Also stated in: § 1. Introduction · hedged
“disordered dolomite is considered as the precursor for some ordered dolomites in sedimentary rocks”
Quote in the paperSubstantial claim1 of 3 sources checked- cites Warren, 2000 source
- cites Zhang et al., 2012a, b
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Rodriguez-Blanco et al., 2015 source
The ‘Proto-dolomite to dolomite transformation’ section reports that disordered proto-dolomite transformed into ordered dolomite in the experiments. The section on ancient natural systems proposes a similar pathway for certain ancient dolomite deposits, but does not establish that disordered dolomite is generally an important precursor of sedimentary ordered dolomite. Page numbers are unavailable in our copy. (LLM, conf=0.85)
Experimental — accuracy not yet measured
- Also stated in: § 1. Introduction · hedged
- Premisecitation
Electronegative carboxyl groups bind to [Mg(H2O)6]2+ ion pairs and form a [Mg(H2O)5(R-COO)]+ complex, with ejection of one water molecule.
“Specifically, the electronegative carboxyl groups bind to [Mg(H2O)6] 2+ ion pairs and form a [Mg(H2O)5(R-COO)] + complex, along with the ejection of one water molecule (Roberts et al., 2013).”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Roberts et al., 2013 source
- Premisecitation
Aragonite rather than Ca-Mg carbonates is the dominant carbonate phase when the Mg/Ca molar ratio of saturated solution exceeds 4.0.
“As such, aragonite (a low-Mg calcium carbonate) rather than Ca-Mg carbonates is the dominant carbonate phase when the Mg/Ca molar ratio of saturated solution exceeds 4.0 (Shen et al., 2014(Shen et al., , 2015)).”
Quote in the paperSubstantial claim1 of 2 sources checked- cites Shen et al., 2014 source
- cites Shen et al., 2015 source
The Introduction and Discussion passages address dolomite growth, Mg hydration, and polysaccharides, not which carbonate phase dominates at a given solution Mg/Ca ratio. Searches for aragonite and the 4.0 Mg/Ca threshold found no passage in our copy supporting the claimed phase comparison. (LLM, conf=0.76)
Experimental — accuracy not yet measured
- Premisecitation
The newly formed Mg-carboxyl complex requires significantly lower energy when binding CO3 2- than [Mg(H2O)6]2+.
“Upon the dewatering, the newly formed Mg-carboxyl complex requires significantly lower energy when binding CO3 2-than [Mg(H2O)6] 2+ (Roberts et al., 2013;Shen et al., 2014).”
Quote in the paperSubstantial claim1 of 2 sources checked - Premisecitation
Once oversaturated condition is achieved, the intrinsic chemical property of Mg2+ ion becomes a key factor affecting the growth of Ca-Mg carbonates.
“Once oversaturated condition is achieved, the intrinsic chemical property of Mg 2+ ion becomes a key factor affecting the growth of Ca-Mg carboantes”
Quote in the paperSubstantial claim1 of 3 sources checked
- Premisecitation
Carboxyl moieties within the EPS matrix are major functional groups that accelerate Mg2+ dehydration.
“Furthermore, carboxyl moieties within EPS matrix were identified as the major functional groups to accelerate Mg 2+ dehydration (Wang et al., 2009;Roberts et al., 2013;Zhang et al., 2015).”
Quote in the paperSubstantial claim1 of 3 sources checked- cites Wang et al., 2009 source
- cites Roberts et al., 2013 source
In “Dolomite Identification” (page not supplied), the paper explains that surface-bound carboxyl groups can displace water from Mg²⁺ and proposes this mechanism for EPS-associated dolomite nucleation. Its experiments used carboxylated microspheres, however; it does not identify carboxyl moieties within an EPS matrix as the major functional groups accelerating Mg²⁺ dehydration. (LLM, conf=0.84)
Experimental — accuracy not yet measured - cites Zhang et al., 2015 source
- Premisecitation
Water activity and desolvation energy of cations can be reduced by adding a component with a low dielectric constant.
“It has been well-known that both water activity and desolvation energy of cations can be reduced by adding a component with a lowdielectric constant (Oomori and Kitano, 1987;Zhang et al., 2012a, b).”
Quote in the paperSubstantial claim1 of 2 sources checked- cites Oomori and Kitano, 1987 source
The Introduction (p. 59) says that adding low-dielectric dioxane to seawater can lower water activity. The section on dioxane’s effect on precipitates says it modifies ion hydration, but does not state that it reduces cation desolvation energy; that part of the claim is not established by our copy. (LLM, conf=0.84)
Experimental — accuracy not yet measured - cites Zhang et al., 2012a
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisecitation
Several studies show enhancement of Mg levels in growing Mg-calcite or disordered dolomite by organic additives that exhibit low Mg-binding affinity, such as methanol, alcohol, propanol, dioxane, methane, acetate and agar.
“Furthermore, there have been several studies showing the enhancement of Mg levels in growing Mgcalcite or disordered dolomite by some organic additives that exhibit a low Mg-binding affinity, such as methanol, alcohol, propanol, dioxane, methane, acetate and agar (Oomori and Kitano, 1987;Falini et al., 1996;Xu et al., 2010;Zhang et al., 2010;Zhang et al., 2012a).”
Quote in the paperSubstantial claim1 of 3 sources checked- cites Oomori and Kitano, 1987 source
The ‘Effect of dioxane on the mineralogy of precipitates’ section reports that dioxane favors formation of Mg-bearing calcite–MgCO3 solid solutions and forms no stable complexes with magnesium ions. But it also reports that MgCO3 content decreases as dioxane concentration rises, so this paper does not support an unqualified claim that dioxane enhances Mg levels in the growing solids. The other listed additives are not findings attributed specifically to this paper. (LLM, conf=0.88)
Experimental — accuracy not yet measured - cites Falini et al., 1996 source
- cites Xu et al., 2010
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Findingown data
In other reactors with succinic acid, Mg-calcites formed.
“whereas in other reactors with succinic acid, Mg-calcites formed.”
- Also stated in: § 3.2.1. XRD results · plain
“Mg-calcites with MgCO3 content ranging from 11.08 mol% to 31.82 mol% precipitated in other systems.”
Quote in the paperSubstantial claim - Also stated in: § 3.2.1. XRD results · plain
- Findingown data
Soluble Ca2+ concentrations gradually decreased from ca. 15 mM to near zero by day 14 in reactors with or without carboxylic acids.
“the concentrations of soluble Ca 2+ ions gradually decrease from ca. 15 mM to near zero by day 14.”
Quote in the paperNot a substantial claim - Findingown data
Declines in Mg2+ ions were observed when carboxylic acids were introduced into the precipitation reactors.
“the declines in Mg 2+ ions were observed when carboxylic acids were introduced into the precipitation reactors”
Quote in the paperSubstantial claim - Findingown data
Disordered dolomite with 40.92 mol% MgCO3 was detected under conditions of 30 mM succinic acid and 70‰ salinity.
“Disordered dolomite with 40.92 mol% MgCO3 was detected under the conditions of 30 mM succinic acid and 70‰ salinity”
- Also stated in: § 3.2.1. XRD results · plain
“the highest MgCO3 content of Ca-Mg carbonates produced in the solution with 30 mM succinic acid can reach 40.92 mol%, close to that of dolomite”
Quote in the paperSubstantial claim - Also stated in: § 3.2.1. XRD results · plain
- Findingown data
Both succinic acid and citric acid enhanced the incorporation of Mg2+ into growing Ca-Mg carbonates.
“Our results showed that both succinic acid and citric acid enhanced the incorporation of Mg 2+ into growing Ca-Mg carbonates.”
- Also stated in: § 3.2.1. XRD results · hedged
“these data indicated that (i) both carboxylic acid and salinity had a considerable impact on the Mg 2+ uptake into calcitic structures, leading to the precipitation of Mg-calcite and even disordered dolomite at ambient temperature”
- Also stated in: § 1. Introduction · hedged
“Our results showed that both LMW carboxylic acid and solution salinity could promote the uptake of Mg 2+ into precipitating Ca-Mg carbonates, thus forming Mg-calcite and even disordered dolomite at 25 °C.”
Quote in the paperSubstantial claim - Also stated in: § 3.2.1. XRD results · hedged
- Findingown data
The decreases in Mg2+ were apparently related to increased dosage of carboxylic acid in solution.
“these decreases were apparently related to increased dosage of carboxylic acid in solution.”
Quote in the paperSubstantial claim - Findingown data
Citric acid was more effective in loading Mg2+ into Ca-Mg carbonates compared with succinic acid.
“Citric acid was more effective in loading Mg 2+ into Ca-Mg carbonates compared with succinic acid”
- Also stated in: § 3.2.1. XRD results · plain
“in comparison to succinic acid, citric acid was more effective in enhancing Mg incorporation into Ca-Mg carbonates.”
- Also stated in: § 3.2.1. XRD results · plain
“the MgCO3 contents of synthetic Ca-Mg carbonates facilitated by citric acid were significantly higher than those by succinic acid.”
Quote in the paperSubstantial claim - Also stated in: § 3.2.1. XRD results · plain
- Findingown data
Disordered dolomite with MgCO3 content ranging from 40.91 to 46.75 mol% occurred in most conditions tested with citric acid.
“as evidenced by the predominant occurrence of disordered dolomite with MgCO3 content ranging from 40.91”
- Also stated in: § 3.2.1. XRD results · plain
“Ca-Mg carbonates close to dolomite composition (covering the range 40.91-46.75mol% MgCO3) were produced in the solutions with citric acid over the concentration range of 10-30 mM either at the salinity of 35‰ or at 70‰”
Quote in the paperSubstantial claim - Also stated in: § 3.2.1. XRD results · plain
- Findingown data
Solution salinity played a positive role in enhancing Mg signature in Ca-Mg carbonates.
“Solution salinity also played a positive role in enhancing Mg signature in Ca-Mg carbonates.”
- Also stated in: § 3.2.1. XRD results · hedged
“it seems that the elevated salinity of carboxylic acidbearing solution could also enhance the substitution of Mg for Ca within the resulting carbonate phases, especially those that precipitated from the succinic acid-amended reactors”
Quote in the paperSubstantial claim - Also stated in: § 3.2.1. XRD results · hedged
- Findingown data
There was no appreciable Mg2+ depletion in control sets.
“In general, there was no appreciable Mg 2+ depletion in control sets.”
Quote in the paperSubstantial claim - Findingown data
There were no ordering reflections [e.g., (015), (021), and (101)] in XRD patterns of carboxylic acid-mediated dolomite-like phases.
“there were no ordering reflections [e.g., (015), (021), and (101)] in XRD patterns of carboxylic acid-mediated dolomite-like phases.”
Quote in the paperSubstantial claim - Findingown data
The (104) peak of Ca-Mg carbonate became broader and showed a much higher peak intensity with increasing concentrations of succinic or citric acid.
“the (104) peak of Ca-Mg carbonate became broader and showed a much higher peak intensity with increasing concentrations of succinic (Figs.4B and 4D) or citric acid (Figs.5B and 5D).”
Quote in the paperSubstantial claim - Findingown data
The (104) d-spacing, corresponding to mol% MgCO3 in the crystallites, was significantly correlated with the concentration of succinic or citric acid.
“the (104) d-spacing (corresponding to mol% MgCO3 in the crystallites) was significantly correlated with the concentration of succinic or citric acid”
Quote in the paperSubstantial claim - Findingown data
Crystals formed in control systems with salinities of 35‰ and 70‰ were exclusively aragonite.
“the crystals formed in the control systems with salinities of 35‰ and 70 ‰ were exclusively aragonite (CaCO3)”
Quote in the paperSubstantial claim - Findingown data
MgCO3 contents of synthetic Ca-Mg carbonates facilitated by citric acid were significantly higher than those by succinic acid.
“the MgCO3 contents of synthetic Ca-Mg carbonates facilitated by citric acid were significantly higher than those by succinic acid.”
Quote in the paperSubstantial claim - Findingown data
The XRD pattern and peak position of dolomite-like phases catalyzed by succinic or citric acid were quite similar to those of inorganic disordered dolomite precipitated at 80°C.
“The XRD pattern and peak position of dolomite-like phases catalyzed by succinic or citric acid were quite similar to those of inorganic disordered dolomite precipitated at 80 °C.”
Quote in the paperSubstantial claim - Findingown data
At 70‰ salinity, the highest MgCO3 content of Ca-Mg carbonates produced in solution with 30 mM succinic acid reached 40.92 mol%, close to that of dolomite.
“Once the salinity of succinic acid-bearing solutions increased up to 70‰, the highest MgCO3 content of Ca-Mg carbonates produced in the solution with 30 mM succinic acid can reach 40.92 mol%, close to that of dolomite”
Quote in the paperSubstantial claim - Findingown data
Increment in the concentration of succinic or citric acid led to a progressive decrease in the (104) d-spacing of Ca-Mg carbonate.
“increment in the concentration of these compounds could lead to a progressive decrease in the (104) d-spacing of Ca-Mg carbonate.”
Quote in the paperSubstantial claim - Findingown data
The solid products in reactors with 30 mM citric acid were spherulites with averaged size of 2-4 μm.
“the solid products in the reactors with 30 mM citric acid were spherulites with averaged size of 2-4 μm”
Quote in the paperNot a substantial claim - Findingown data
Ca-Mg carbonates close to dolomite composition (40.91-46.75 mol% MgCO3) were produced in solutions with citric acid over the concentration range of 10-30 mM either at 35‰ or 70‰.
“Ca-Mg carbonates close to dolomite composition (covering the range 40.91-46.75mol% MgCO3) were produced in the solutions with citric acid over the concentration range of 10-30 mM either at the salinity of 35‰ or at 70‰”
Quote in the paperSubstantial claim - Findingown data
Citric acid was more effective in removing Mg2+ from solutions than succinic acid at the same concentration.
“citric acid was more effective in removing Mg 2+ from solutions than succinic acid at the same concentration.”
Quote in the paperSubstantial claim - Findingown data
When succinic or citric acid was introduced, Ca-Mg carbonates of the calcite-dolomite series were identified as the major phases.
“the Ca-Mg carbonates of calcite-dolomite series were identified as the major phases”
Quote in the paperSubstantial claim - Findingown data
Mg-calcites formed when only 5 mM citric acid was used.
“Mg-calcites formed when only 5 mM citric acid was used.”
Quote in the paperSubstantial claim - Findingown data
The disordered dolomite crystal obtained from citric acid-containing groups was identified by its morphology and chemical composition from an EDS spectrum.
“The disordered dolomite crystal obtained from citric acid-containing groups was identified by its morphology and chemical composition from an EDS spectrum”
Quote in the paperSubstantial claim - Findingown data
The occurrence of rod-like aragonite in succinic acid-containing groups was collectively verified by TEM image, SAED pattern and EDS elemental composition.
“The occurrence of rod-like aragonite in succinic acid-containing groups was collectively verified by the results of TEM image, SAED pattern and EDS elemental composition”
Quote in the paperNot a substantial claim - Findingown data
Elevated salinity of carboxylic acid-bearing solution could enhance the substitution of Mg for Ca within the resulting carbonate phases, especially those precipitated from succinic acid-amended reactors.
“the elevated salinity of carboxylic acidbearing solution could also enhance the substitution of Mg for Ca within the resulting carbonate phases, especially those that precipitated from the succinic acid-amended reactors”
Quote in the paperSubstantial claim - Findingcitation
At 35‰ salinity, carbonates with 8.17, 10.35, 28.91, and 33.28 mol% MgCO3 precipitated from solutions with 5, 10, 20, and 30 mM succinic acid, respectively.
“when the solution salinity was 35‰, the carbonates with 8.17, 10.35, 28.91 and 33.28 mol% MgCO3 precipitated from solutions with 5, 10, 20 and 30 mM succinic acid, respectively”
Quote in the paperSubstantial claim - Findingown data
Ca-Mg carbonates formed in 5-30 mM succinic acid-amended systems at 35‰ had MgCO3 composition ranging from 8.17 to 33.28 mol%, corresponding to high-Mg calcite.
“the Ca-Mg carbonates formed in the 5-30 mM succinic acidamended systems with the salinity of 35‰ had MgCO3 composition ranging from 8.17 mol% to 33.28 mol%, corresponding to high-Mg calcite”
Quote in the paperSubstantial claim - Findingown data
In carboxylic acid-amended groups, the concentrations of precipitated Mg were linearly correlated with the concentrations of precipitated Ca.
“in carboxylic acidamended groups, the concentrations of precipitated Mg (depletion of Mg 2+ ) were linearly correlated with the concentrations of precipitated Ca”
Quote in the paperSubstantial claim - Findingown data
The disordered dolomite spherulites were composed of numerous nanoparticles, similar to those obtained in succinic acid-bearing systems.
“disordered dolomite spherulites were composed of numerous nanoparticles (the inserts in Figs.10B and 10D), similar to those obtained in succinic acid-bearing systems.”
Quote in the paperNot a substantial claim - Findingown data
The synthetic disordered dolomite had a dominant spacing of 0.290 nm, corresponding to the d-spacing of (104).
“our synthetic disordered dolomite had a dominant spacing of 0.290 nm, corresponding to the d-spacing of (104)”
Quote in the paperNot a substantial claim - Findingown data
Ca-Mg carbonates occurred in the reactors with succinic acid or citric acid.
“Our present study demonstrated that Ca-Mg carbonates occurred in the reactors with succinic acid or citric acid.”
Quote in the paperSubstantial claim - Findingown data
Incorporation of Mg2+ into growing Ca-Mg carbonates in saline solutions could be enhanced by succinic and citric acid.
“We demonstrated that the incorporation of Mg 2+ into growing Ca-Mg carbonates in saline solutions could be enhanced by succinic and citric acid”
Quote in the paperSubstantial claim - Findingown data
Incorporation amounts of Mg2+ were correlated with the concentration of carboxylic acids and solution salinity.
“and the incorporation amounts of Mg 2+ was correlated with the concentration of carboxylic acids and solution salinity.”
Quote in the paperSubstantial claim - Findingown data
Microbially-derived carboxylic acids were effective in diminishing the hydration effect of Mg2+ and thus promoting incorporation of Mg2+ into growing Ca-Mg carbonates.
“Our results revealed that microbially-derived carboxylic acids were effective in diminishing the hydration effect of Mg 2+ and thus promoting the incorporation of Mg 2+ into growing Ca-Mg carbonates.”
Quote in the paperSubstantial claim - Findingown data
Solution salinity had a considerable influence on the formation of Ca-Mg carbonates in the abiotic reactors.
“Our present results showed that solution salinity had a considerable influence on the formation of Ca-Mg carbonates in the abiotic reactors,”
Quote in the paperNot a substantial claim - Premisecitation
Certain types of microorganisms have been demonstrated to be effective in promoting the precipitation of disordered dolomite.
“Certain types of microorganisms have been demonstrated to be effective in promoting the precipitation of disordered dolomite, an important precursor of sedimentary ordered dolomite.”
- Also stated in: § 1. Introduction · plain
“Laboratory experiments have further shown that the activities of certain types of microorganisms (e.g, sulfate-reducing bacteria, methanogens and halophilic aerobic microbes) are intimately associated with these precipitates”
Quote in the paperSubstantial claim0 of 3 sources checked - Also stated in: § 1. Introduction · plain
- Premisecitation
The inhibitory effect of Mg2+ hydration on the formation of Ca-Mg carbonates has been demonstrated by computational studies.
“Such inhibitory effect of Mg 2+ hydration on the formation of Ca-Mg carbonates has been demonstrated by several computational studies (e.g., de Leeuw and Parker, 2001;Di Tommaso and de Leeuw, 2010).”
Quote in the paperSubstantial claim0 of 2 sources checked - Interpretationown data
Succinic and citric acid are effective in promoting Mg uptake into calcitic structures.
“indicating that these biomolecules are effective in promoting Mg uptake into calcitic structures.”
Quote in the paperSubstantial claim - Premisecitation
Microbial EPS could act as natural catalysts to promote incorporation of Mg2+ into growing Ca-Mg carbonates.
“A growing body of studies has suggested that microbial EPS could act as natural catalysts to promote the incorporation of Mg 2+ into growing Ca-Mg carbonates (Zhang et al., 2012a(Zhang et al., , 2015;;Bontognali et al., 2014;Kenward et al., 2013;Liu et al., 2020).”
Quote in the paperSubstantial claim0 of 3 sources checked - Premisecitation
Hydromagnesite can be easily misidentified as disordered dolomite or dolomite.
“As hydromagnesite [Mg5(CO3)4(OH)2•4H2O] can be easily misidentified as disordered dolomite or dolomite”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Zhang et al., 2012a
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Interpretationown data
Based on EDS analyses and XRD results, the spherulites occurring at salinities of 35‰ or 70‰ were identified as disordered dolomites.
“Based on EDS analyses and XRD results, these spherulites occurring at salinities of 35‰ or 70‰ were identified as disordered dolomites”
Quote in the paperSubstantial claim - Premisecitation
Mg2+ ions are strongly hydrated in solution, forming the Mg2+-H2O complex [Mg(H2O)6]2+.
“Mg 2+ ions are strongly hydrated in solution, forming the Mg 2+ -H2O complex (i.e., [Mg(H2O)6] 2+ )”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Lippman, 1973
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisecitation
Microorganisms secrete copious low-molecular-weight organic acids into solution.
“microorganisms also secrete copious lowmolecular-weight (LMW) organic acids into solution”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Sauer et al., 2008 source
- Interpretationreasoning
It is easier to overcome the hydration barrier surrounding Ca2+ ions than that surrounding Mg2+ ions.
“In contrast, it is easier to overcome the hydration barrier surrounding Ca 2+ ions.”
Quote in the paperSubstantial claim - Premisecitation
Mg2+ has a larger hydration enthalpy than Ca2+ (1926 kJ/mole vs. 1579 kJ/mole).
“However, due to the larger hydration enthalpy of Mg 2+ than that of Ca 2+ (1926 kJ/mole vs. 1579 kJ/mole) (Lippman, 1973),”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Lippman, 1973
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Interpretationreasoning
Even if LMW carboxylic acid concentrations in microbial mats are not as high as those tested, these compounds together with other microbial exudates might play an important role in formation of disordered dolomite.
“Even if the concentration of LMW carboxylic acids in microbial mats are not as high as the ones we tested herein, these compounds, together with other microbial exudates (e.g., EPS), might play an important role in the formation of disordered dolomite.”
Quote in the paperSubstantial claim - Interpretationown data
The metal-chelation mechanism is likely confirmed by the observation that citric acid was more effective in loading Mg2+ into growing carbonate.
“This mechanism is likely confirmed by our observation that citric acid displayed more effective in loading Mg 2+ into growing carbonate, resulting in the formation of disordered dolomite in most conditions tested,”
Quote in the paperSubstantial claim- Rests on an assumption: The metal-binding capacity of carboxylic acids measured in bulk solution governs their effectiveness in loading Mg2+ into growing carbonate.
- Premisecitation
LMW carboxylic acids typically have a lower dielectric constant than water molecules.
“In comparison to water molecules, LMW carboxylic acids typically have a lower dielectric constant (ε).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Kirkwood and Westheimer, 1938 source
- Premisecitation
Citric acid has higher metal-binding capacity than succinic acid in bulk solutions.
“because citric acid has higher metal-binding capacity than succinic acid in bulk solutions (binding constants K of citric acid: KMg=10 3.37 , KCa=10 3.5 ; Ksuccinic acid: (Cannan and Kibrick, 1938;Wang et al., 2009).”
Quote in the paperSubstantial claim0 of 2 sources checked - Premisenone given
The formation of Mg calcite and/or non-stoichiometric dolomite is generally found in hypersaline settings.
“Apart from temperature, the importance of solution salinity has been repeatedly underscored by the fact that the formation of Mg calcite and (or) non-stoichiometric dolomite is generally found in hypersaline settings, as stated earlier.”
Quote in the paperNot a substantial claim - Interpretationreasoning
Succinic and citric acid may function in the same capacity as EPS to catalyze crystallization of Ca-Mg carbonates.
“Given their multicarboxylic status, these two biomolecules may function in the same capacity as EPS through aforementioned model to catalyze the crystallization of Ca-Mg carbonates.”
Quote in the paperSubstantial claim - Premisecitation
Within microbial mats of evaporated saline deposits, the concentration of carboxylic acids should be higher because microorganisms produce carboxyl-rich compounds to maintain metabolic functions in high salt.
“Within microbial mats of evaporated saline deposits (e.g., coastal lagoons, brackish and saline lakes), the concentration of carboxylic acids should be higher, because microorganisms usually produce carboxyl-rich compounds to maintain their metabolic functions in the presence of high concentration of salts (Fukuchi et al., 2003;DasSarma, 2006).”
Quote in the paperSubstantial claim0 of 2 sources checked - Interpretationreasoning
The two-stage model might also explain dolomite formation in the ancient sea.
“Such model might also explain dolomite formation in the ancient sea.”
Quote in the paperNot a substantial claim - Interpretationreasoning
These organic compounds share the same polar behavior, that is, they all have a low dielectric constant.
“These organic compounds share the same polar behavior, that is, they all have a low-dielectric constant.”
Quote in the paperSubstantial claim - Interpretationreasoning
Microbial exudate-mediated dolomite formation offers one overlooked possibility for the occurrence of dolomite in Holocene sediments and sedimentary rocks.
“Considering the wide distribution of carboxylic acids and other microbial exudates (e.g., EPS) in natural environments and high salinity in evaporitic conditions, the microbial exudate-mediated dolomite formation offers one overlooked possibility for the occurrence of dolomite in Holocene sediments and sedimentary rocks.”
Quote in the paperSubstantial claim - Premisecitation
Once disordered dolomite has formed, it undergoes an ageing process upon burial and converts to well-crystallized ordered dolomite.
“Once disordered dolomite has formed, it undergoes an”
Quote in the paperSubstantial claim0 of 3 sources checked - Interpretationreasoning
A two-stage model beginning with precipitation of disordered dolomite via microbial exudates followed by diagenetic transformation to ordered dolomite provides one possible interpretation for the occurrence of dolomite in modern hypersaline environments.
“As such, a two-stage model, which begins with the precipitation of disordered dolomite via microbial exudates (EPS and LMW carboxylic acids) followed by subsequent diagenetic transformation of disordered dolomite to ordered dolomite, provides one possible interpretation on the occurrence of dolomite in modern hypersaline environments.”
Quote in the paperSubstantial claim
- Classified as probably not a substantial claim. 21
- May combine two claims. 20
- The quote only partly states this claim. 2
Probably not a substantial claim: may not pass S3 (load-bearing).
PremisecitationThe dehydration reaction induced by carboxyl moieties proceeds possibly via a metal-chelation mechanism.
“Previous studies also proposed that the dehydration reaction induced by carboxyl moieties proceeds possibly via a metal-chelation mechanism (Romanek et al., 2009;Roberts et al., 2013).”
Quote in the paperNot a substantial claim2 of 2 sources checkedMay combine two claims.
PremisecitationThe more stable inner-sphere hydration shell around Mg2+ hinders adsorption of Mg2+ onto crystal surfaces and blocks subsequent binding of carbonate to surface Mg2+.
“the occurrence of more stable inner-sphere hydration shell around Mg 2+ ions not only hinders the adsorption of Mg 2+ onto crystal surface, but also blocks the subsequent binding of carbonate to surface Mg 2+ (Shen et al., 2014(Shen et al., , 2015)).”
Quote in the paperSubstantial claim1 of 2 sources checked- cites Shen et al., 2014 source
- cites Shen et al., 2015 source
The Introduction describes these as two possible ways Mg hydration may inhibit dolomite growth: making hydrated Mg²⁺ difficult to adsorb and blocking carbonate binding to surface Mg²⁺. The claim states both as established effects, but the Introduction and Discussion say adsorption of hydrated Mg²⁺ is not likely the rate-limiting step; the paper instead focuses on dehydration of surface Mg²⁺. (LLM, conf=0.87)
Experimental — accuracy not yet measured
Classified as probably not a substantial claim. May combine two claims.
PremisecitationA thin Ca-Mg carbonate template could form and its growth will take place when a supersaturated condition is maintained.
“In doing so, it is believed that a thin Ca-Mg carbonate template could form and its growth will take place when a supersaturated condition is maintained (Roberts et al., 2013).”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Roberts et al., 2013 source
May combine two claims.
PremisecitationSolution salinity can regulate microbial community composition, giving rise to a predominance of halophilic microbes involved in crystallization of Ca-Mg carbonates because their cell surface and EPS contain a high density of carboxyl groups.
“Generally, it is suggested that solution salinity can regulate microbial community composition at first, thus giving rise to the predominance of halophilic microbes, which are thought to be involved in the crystallization of Ca-Mg carbonates, as their cell surface and EPS contain high density of carboxyl groups (Rivadeneyra et al., 2000;Sánchez-Román et al., 2008;Balci and Demirel, 2016;Qiu et al.”
Quote in the paperNot a substantial claim1 of 3 sources checkedProbably not a substantial claim: may not pass S3 (load-bearing).
Findingown dataThe pH changes of carboxylic acid-amended systems exhibited a similar trend to control reactors: they rapidly increased within the first 10 days and slightly declined afterwards.
“The pH changes of carboxylic acid-amended systems exhibited a similar trend to those of control reactors (carboxylic acid-free groups): they rapidly increased within the first 10 days and slightly declined afterwards”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Findingown dataHRTEM revealed that nano-sized spheroids were randomly distributed.
“High resolution TEM (HRTEM) image further revealed that these nano-sized spheroids were randomly distributed”
Quote in the paperNot a substantial claimMay combine two claims.
Findingown dataHigh-Mg calcite was detected in succinic acid-containing groups, in good agreement with XRD and SEM results.
“In addition to aragonite, high-Mg calcite was also detected (Figs. 11D-G), in good agreement with XRD and SEM results.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Findingown dataRaman spectra of the samples showed similar patterns with four distinct bands, consistent with previous studies of carbonate minerals.
“similar patterns with four distinct bands were observed in our samples, as consistent with previous studies of carbonate minerals”
Quote in the paperNot a substantial claimMay combine two claims.
Findingown dataEDS revealed that the rod-like microcrystal contained abundant Ca but negligible Mg, whereas the spheroidal phase displayed a relatively high Mg/Ca ratio.
“the rod-like microcrystal (particle a in Fig. 9B) contained abundant Ca but negligible Mg, whereas the spheroidal phase (particle b in Fig. 9B) displayed a relatively high Mg/Ca ratio.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataA representative SAED pattern of the sample showed the presence of (104), (110), (113) and (024) reflections but lacked the typical super-lattice reflections [e.g., (015), (101) and (021)].
“A representative SAED pattern of this sample showed the presence of ( 104), ( 110), ( 113) and ( 024) reflections but lack of the typical super-lattice reflections [e.g., (015), ( 101) and ( 021)]”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Findingown dataThe disordered dolomite spheroid displayed randomly oriented nano-crystals, consistent with SEM observations.
“The disordered dolomite spheroid, when magnified, displayed randomly oriented nano-crystals as shown in Fig. 12B, consistent with the SEM observations”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Findingown dataAragonite and monohydrocalcite were also produced in some cases.
“In addition to these Ca-Mg carbonates, aragonite and monohydrocalcite (CaCO3•H2O) were also produced in some cases.”
Quote in the paperNot a substantial claimThe quote only partly states this claim.
Findingown dataAt 35‰ salinity, citric acid over the same concentration range produced carbonates with average MgCO3 content of 9.62, 40.92, 42.01, and 44.56 mol%, respectively.
“the catalytic effect of citric acid over the same concentration range became more obvious: produced carbonates with an average MgCO3 content of 9.62, 40.92, 42.01 and 44.56 mol%, respectively”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Findingown dataHigh-Mg calcite appeared as spheroid-shaped aggregates.
“high-Mg calcite appeared as spheroid-shaped aggregates.”
Quote in the paperNot a substantial claimThe quote only partly states this claim.
Findingown dataAt 70‰ salinity, Mg-calcites with MgCO3 content ranging from 11.08 to 31.82 mol% precipitated in other succinic acid systems.
“Mg-calcites with MgCO3 content ranging from 11.08 mol% to 31.82 mol% precipitated in other systems.”
Quote in the paperNot a substantial claimMay combine two claims.
FindingreasoningCitric acid was more effective than succinic acid in loading Mg2+ into growing carbonate, resulting in formation of disordered dolomite in most conditions tested.
“This mechanism is likely confirmed by our observation that citric acid displayed more effective in loading Mg 2+ into growing carbonate, resulting in the formation of disordered dolomite in most conditions tested,”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataDisordered dolomites were observed when both 30 mM succinic acid and salinity level of 70‰ were used, in most systems with citric acid, as confirmed by XRD patterns, Raman spectra and TEM-SAED.
“Disordered dolomites were observed when both 30 mM succinic acid and salinity level of 70‰ were used, in most systems with citric acid as confirmed by XRD patterns, Raman spectra and TEM-SAED.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductnone givenAll experiments were run in duplicates.
“All experiments were run in duplicates.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
Study design and conductcitationA hydromagnesite sample, together with inorganic calcite, disordered dolomite and dolomite, was prepared as a standard for inferring the mineralogical composition of solid products.
“a hydromagnesite sample, together with inorganic calcite, disordered dolomite and dolomite, was prepared as a standard for inferring the mineralogical composition of our solid products”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Liu et al., 2019b
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
May combine two claims.
InterpretationreasoningThe crystal structure of the dolomite-like materials was highly disordered and thus they can be identified as disordered dolomite.
“above features indicate that the crystal structure of these dolomite-like materials was highly disordered and thus that they can be identified as disordered dolomite.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Study design and conductcitationThe starting Mg/Ca molar ratio is higher than that of modern seawater (6 vs. 5.2), but lies within the range of values measured in present dolomite-forming environments.
“the starting Mg/Ca molar ratio is higher than that of modern seawater (6 vs. 5.2), but lies within the range of values measured in present dolomite-forming environments (Table 1 in Deng et al., 2010).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Deng et al., 2010 source
May combine two claims.
PremisecitationSuccinic acid and citric acid can be produced by various microorganisms in the tricarboxylic acid cycle and thus be virtually found in most aqueous settings, especially within microbial mats.
“they can be produced by various microorganisms in the tricarboxylic acid cycle (TCA cycle) (Sauer et al., 2008) and thus be virtually found in most aqueous settings, especially within microbial mats where microbial activities are prevalent.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Sauer et al., 2008 source
Classified as probably not a substantial claim.
PremisecitationSeveral studies note the positive role of LMW organic acids (e.g., acetate) in the uptake of Mg into growing Mg-calcites.
“There are several studies that note the positive role of LMW organic acids (e.g., acetate) in the uptake of Mg into growing Mg-calcites”
Quote in the paperSubstantial claim0 of 2 sources checked- cites Xu et al., 2010
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Zhang et al., 2010 source
May combine two claims.
InterpretationreasoningThe mechanism of Mg2+ hydration inhibition helps explain the paucity of dolomite in marine sediment and the predominant occurrence of aragonite in the paper's control sets.
“Such mechanism helps to explain the paucity of dolomite in marine sediment and the predominant occurrence of aragonite in our control sets.”
Quote in the paperSubstantial claimMay combine two claims.
Interpretationown dataCombined with XRD data, the rod-like and spheroidal solid phases were identified as aragonite and high-Mg calcite.
“Combined with XRD data, these two types of solid phases were identified as aragonite and high-Mg calcite.”
Quote in the paperSubstantial claimMay combine two claims.
Interpretationown dataThe micro-spheroidal neoformations consisted of similar Mg and Ca contents and were interpreted as disordered dolomites.
“these micro-spheroidal neoformations consisted of similar Mg and Ca contents (Kα line area), thus were interpreted as disordered dolomites.”
Quote in the paperSubstantial claimClassified as probably not a substantial claim.
Study design and conductcitationThe MgCO3 contents of Ca-Mg carbonates were calculated from the d-spacing of the (104) peak by using the calibration curve of Bischoff et al. (1983).
“The MgCO3 contents of Ca-Mg carbonates were calculated from the d-spacing of the (104) peak by using the calibration curve of Bischoff et al., (1983).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Bischoff et al., 1983
Probably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductnone givenSpectral peak positions were calibrated using the 520.5 cm-1 line of silicon as a standard.
“Spectral peak positions were calibrated using the 520.5 cm -1 line of silicon as a standard.”
Quote in the paperNot a substantial claimMay combine two claims.
Interpretationown dataThe band positions of carboxylic acid-induced precipitates were much close to that of inorganic disordered dolomite, suggesting that the cation occupancy in the carboxylic acid-catalyzed Ca-Mg carbonate was disordered rather than ordered.
“the band positions of our carboxylic acid-induced precipitates were much close to that of inorganic disordered dolomite (Fig. 8B), again suggesting that the cation occupancy in the carboxylic acid-catalyzed Ca-Mg carbonate was disordered rather than ordered.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
PremisecitationThe inorganic synthesis of disordered dolomite or dolomite exhibits a positive temperature dependence.
“Among them, the role of temperature has been long recognized, because the inorganically synthesis of disordered dolomite or dolomite exhibits a positive temperature dependence (e.g., Arvidson and Mackenzie, 1999).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Arvidson and Mackenzie, 1999
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationOcean salinity in the Precambrian was in the range of 40-70‰, significantly higher than that of the modern ocean (~29‰).
“It has been postulated that the ocean salinity in the Precambrian, the”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Knauth, 2005 source
May combine two claims.
PremisecitationHigh salinity can initiate dehydration of Mg-H2O complexes both directly and indirectly, and decrease oxygen solubility in seawater, benefiting preservation of microbial exudates and dolomite precipitation.
“The high salinity is able to not only initiate the dehydration of Mg-H2O complexes both directly and indirectly, but also decrease oxygen solubility in seawater (Knauth, 2005) that benefits the preservation of microbial exudates and dolomite precipitation.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Knauth, 2005 source
May combine two claims.
PremisecitationAuthigenic dolomites in the sabkha of Abu Dhabi exclusively occurred within buried microbial mats, where the concentration of microbial exudates was apparently higher than in non-mat sediments.
“Indeed, a field investigation conducted by Bontognali et al. (2010) showed that authigenic dolomites in the sabkha of Abu Dhabi exclusively occurred within the buried microbial mats, in which the concentration of microbial exudates was apparently higher than that in non-mat sediments.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Bontognali et al., 2010 source
Probably not a substantial claim: may not pass S3 (load-bearing).
PremisecitationHigh salinity itself may directly facilitate the dehydration of Mg2+.
“One explanation for the positive role of salinity in Ca-Mg carbonate formation is that high salinity itself may directly facilitate the dehydration of Mg 2+ (Lippman, 1973;Machel and Mountjoy, 1986).”
Quote in the paperNot a substantial claim0 of 2 sources checked- cites Lippman, 1973
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Machel and Mountjoy, 1986 source
Probably not a substantial claim: may not pass S3 (load-bearing).
PremisecitationOther cations dissolved in saturated solution could interact with water molecules to form metal-H2O clusters, possibly disturbing the existing Mg2+-H2O association.
“Once other cations are dissolved into saturated solution, these cations could also interact with water molecules to form metal-H2O clusters (e.g., [Na(H2O)n] + ) (Tsurusawa and Iwata, 1999), possibly disturbing the existing Mg 2+ -H2O association.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Tsurusawa and Iwata, 1999 source
May combine two claims.
PremisecitationCarboxylic acids are ubiquitous and important components of aquatic systems, detected in some seawaters and marine porewaters at concentrations up to ~3 mM.
“Carboxylic acids are ubiquitous and important components of the aquatic systems, which have been detected in some seawaters and marine porewaters at concentrations of up to ~ 3 mM (Albert and Martens, 1997).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Albert and Martens, 1997 source
Probably not a substantial claim: may not pass S3 (load-bearing).
InterpretationreasoningThe polar behavior of carboxylic acids might also be important for their catalytic role in Ca-Mg carbonate formation.
“In addition to the aforementioned metal-chelation mechanism, the polar behavior of carboxylic acids might also be important for their catalytic role in Ca-Mg carbonate formation.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim. May combine two claims.
PremisecitationPure succinic acid has a dielectric constant of 2.4 at 20 °C, while water has a value of 80.4 at the same temperature.
“For instance, the ε value of pure succinic acid is 2.4 at 20 °C, while water molecular has a value of 80.4 under the same temperature (Kirkwood and Westheimer, 1938).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Kirkwood and Westheimer, 1938 source
Probably not a substantial claim: may not pass S3 (load-bearing).
Interpretationown dataThe influence of salinity on Ca-Mg carbonates in abiotic reactors supports its direct impact on disturbance of the Mg2+-H2O association.
“perhaps supporting its direct impact on the disturbance of Mg 2+ -H2O association.”
Quote in the paperNot a substantial claim
The paper relies on this without support.
It is still unclear whether microbially-derived carboxylic acids can aid in the formation of disordered dolomite.
“However, it is still unclear whether microbially-derived carboxylic acids can aid in the formation of disordered dolomite.”
The paper relies on this without support.
Microbial degradation of organic matter in microbial mats continuously provides NH4+ and CO3^2- that benefit the precipitation of Ca-Mg carbonates.
“mimicking the carbonation process occurring within microbial mats, in which microbial degradation of organic matters (e.g., proteinaceous substances) could continuously provide NH4 + and CO3 2-to benefit the precipitation of Ca-Mg carbonates.”
The paper relies on this without support.
The metal-binding capacity of carboxylic acids measured in bulk solution governs their effectiveness in loading Mg2+ into growing carbonate.
“because citric acid has higher metal-binding capacity than succinic acid in bulk solutions”
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
The main kinetic factors that inhibit the nucleation or precipitation of dolomite at low temperatures are the high hydration energy of the magnesium ion, the presence of sulfate (even in very low concentrations) related to the formation of complex MgSO4^0, and the low activity of CO3 in most natural solutions.
“the main kinetic factors that inhibit the nucleation or precipitation of dolomite at low temperatures are thought to include: (1) the high hydration energy of the magnesium ion [22,45,51,66,[74][75][76][77][78][79][80]; (2) the presence of sulfate (even in very low concentrations), related to the formation of complex MgSO 4 0 [32,74,81,82]; and (3) the low activity of CO 2- 3 in most natural solut”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [45]
The MgCO3 content of high-Mg calcite ranges from 4 mol% to 36 mol%, while calcite with a MgCO3 content ranging from 36 mol% to 55 mol% is called disordered dolomite.
“Liu et al. [45] pointed out that the MgCO 3 content of high-Mg calcite ranges from 4 mol% to 36 mol%, while calcite with a MgCO 3 content ranging from 36 mol% to 55 mol% is called disordered dolomite.”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [45]
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
Each contradiction between two passages listed here was confirmed by an independent check.
The 35‰ succinic-acid product receives conflicting mineral identifications
MinorThe Figure 8 caption calls the product made with 30 mM succinic acid at 35‰ salinity disordered dolomite. The results instead classify every product made with 5-30 mM succinic acid at that salinity as high-Mg calcite, with no more than 33.28 mol% MgCO3.
“carbonate standards: a-c, disordered dolomites synthesized with aid of 30 mM succinic acid (35‰ salinity), 30 mM citric acid and salinity of 35‰, and 30 mM citric acid and salinity of 70‰, respectively; d, inorganic disordered dolomite; e, calcite; f, ordered dolomite.”
“Employing such criteria, the Ca-Mg carbonates formed in the 5-30 mM succinic acidamended systems with the salinity of 35‰ had MgCO3 composition ranging from 8.17 mol% to 33.28 mol%, corresponding to high-Mg calcite (Fig. 6).”
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“meric substance (EPS) negatively charged functional groups (Liu et al., 2020), which is conducive to the formation of dolomites.”
BackgroundCalcification of cell membranes: From ions to minerals
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Dissolved Mn2+ promotes microbially-catalyzed protodolomite precipitation in brackish oxidized water
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Systematic laboratory approach to produce Mg-rich carbonates at low-temperature
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“Other potential organogenic mechanisms that may encourage sedimentary dolomite precipitation, such as selective binding of Ca ions by aqueous organic acids or carboxylic acids diminishing the hydration effect of Mg ions, were also considered (Roberts et al ., 2013; Liu et al ., 2020).”
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“Pr is considered a semicrystalline precursor of dolomite and is a metastable phase with a dolomite-like composition along with a completely disordered arrangement of Ca and Mg in its structure (Tompa et al. 2014; Liu et al. 2020; Müller 1970; Last 1982).”
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“…dolomite precipitation remain a long-standing question in sedimentary geology, often referred to as the ‘dolomite problem’ (Liu, Fan, et al., 2020; Liu, Xu, et al., 2020; McKenzie & Vasconcelos, 2009; Sánchez-Román et al., 2008, 2009; Warren, 2000), as modern dolomite formation is rare and…”
New evidence for normal seawater dolomitization in the middle Permian
Gao, H., Hou, J., Chen, M., Li, X., Li, S., Wang, J., & Zhu, G. (2026) · Chemical Geology · doi:10.1016/j.chemgeo.2026.123599 · Cited by 1 · see citing works
dos Santos, R. F., Nogueira, A. C. R., Pacheco, M. L. A. F., Okubo, J., Callefo, F., Luvizotto, G. L., Sepeda, L. F., Sansjofre, P., Trindade, R. I. F., & Angélica, R. S. (2026) · Geosystems and Geoenvironment · doi:10.1016/j.geogeo.2026.100569
Floating Rafts from Coastal Hypersaline Environments in Brazil
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“The interaction between magnesium ions and water is weakened, allowing magnesium ions to more readily incorporate into the carbonate lattice, thereby promoting the formation of magnesium-rich carbonates [3, 27, 47].”
Han, Y., Zhao, Y., Gao, X. P., Han, C., Wei, X., & Han, Z. (2025) · Geomicrobiology Journal · doi:10.1080/01490451.2025.2547784
“…the physicochemical environment around cells but also bind free metal ions through surface functional groups (Braissant et al. 2007; Dupraz et al. 2009; Liu et al. 2020, 2019), facilitating local enrichment of ions and promoting carbonate precipitation within microscale domains (Zhao et al. 2020).”
Lu, Y., Wang, Y., Hou, S., et al. (2025) · SSRN Electronic Journal · doi:10.2139/ssrn.5358458
朱, 光., 李, 茜., 李, 婷., 周, 磊., 吴, 雨., 沈, 冰., & Ning, M. (2022) · SCIENTIA SINICA Terrae · doi:10.1360/sste-2021-0351
- Authors
- Liu, D., Xu, Y., Yu, Q., Yu, N., Qiu, X., Wang, H., & Papineau, D.
- Affiliations
- China University of Geosciences (CN)
- London Centre for Nanotechnology (GB)
- Corresponding author
- Liu, Deng
- Venue
- Journal of Asian Earth Sciences
- Publisher
- Elsevier BV
- Published
- 2020-05
- Volume
- 193
- Pages
- 104301
- ISSN
- 1367-9120 (ISSN-L)
- OpenAlex
- W3007565420
- Semantic Scholar
- 2726db0ab221ac8446d7d072e5a204d2bffc87f2
- Cited by
- 32
- References
- 89
- Citations by year
- 2026: 5 · 2025: 4 · 2024: 9 · 2023: 4 · 2022: 8 · 2021: 2
- FWCI
- 0.91
- Type
- journal article
- Language
- en
- Open access
- green
- discovery.ucl.ac.uk
- Locations
- Journal of Asian Earth Sciences (publishedVersion)
- UCL Discovery (University College London) (submittedVersion)
- Funders
- National Natural Science Foundation of China
- Topics
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Environmental Science › Environmental Engineering › Microbial Applications in Construction Materials
- Keywords
- dolomite genesis, succinic acid, citric acid, Mg-calcite, magnesium incorporation, microbial mats
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