Potential role for microbial ureolysis in the rapid formation of carbonate tufa mounds

Modern carbonate tufa towers in the alkaline (~pH 9.5) Big Soda Lake (BSL), Nevada, exhibit rapid precipitation rates (exceeding 3 cm/year) and host diverse microbial communities. Geochemical indicators reveal that carbonate precipitation is, in part, promoted by the mixing of calcium-rich groundwater and carbonate-rich lake water, such that a microbial role for carbonate precipitation is unknown. Here, we characterize the BSL microbial communities and evaluate their potential effects on carbonate precipitation that may influence fast carbonate precipitation rates of the active tufa mounds of BSL. Small subunit rRNA gene surveys indicate a diverse microbial community living endolithically, in interior voids, and on tufa surfaces. Metagenomic DNA sequencing shows that genes associated with metabolisms that are capable of increasing carbonate saturation (e.g., photosynthesis, ureolysis, and bicarbonate transport) are abundant. Enzyme activity assays revealed that urease and carbonic anhydrase, two microbial enzymes that promote carbonate precipitation, are active in situ in BSL tufa biofilms, and urease also increased calcium carbonate precipitation rates in laboratory incubation analyses. We propose that, although BSL tufas form partially as a result of water mixing, tufa-inhabiting microbiota promote rapid carbonate authigenesis via ureolysis, and potentially via bicarbonate dehydration and CO₂ outgassing by carbonic anhydrase. Microbially induced calcium carbonate precipitation in BSL tufas may generate signatures preserved in the carbonate microfabric, such as stromatolitic layers, which could serve as models for developing potential biosignatures on Earth and elsewhere.     

Bio-sequestration of carbon dioxide using carbonic anhydrase enzyme purified from <Emphasis Type="Italic">Citrobacter freundii</Emphasis>

The increase in the atmospheric concentrations of one of the vital green house gasses, carbon dioxide, due to anthropogenic interventions has led to several undesirable consequences such as global warming and related changes. In the global effort to combat the predicted disaster, several CO₂ capture and storage technologies are being deliberated. One of the most promising biological carbon dioxide sequestration technologies is the enzyme catalyzed carbon dioxide sequestration into bicarbonates which was endeavored in this study with a purified C. freundii SW3 β-carbonic anhydrase (CA). An extensive screening process for biological sequestration using CA has been defined. Six bacteria with high CA activity were screened out of 102 colonies based on plate assay and presence of CA in these bacteria was further emphasized by activity staining and Western blot. The identity of selected bacteria was confirmed by 16S rDNA analysis. CA was purified to homogeneity from C. freundii SW3 by subsequent gel filtration and ion exchange chromatography which resulted in a 24 kDa polypeptide and this is in accordance with the Western blot results. The effect of host on metal ions, cations and anions which influence activity of the enzyme in sequestration studies suggests that mercury and HCO₃ ⁻ ion almost completely inhibit the enzyme whereas sulfate ion and zinc enhances carbonic anhydrase activity. Calcium carbonate deposition was observed in calcium chloride solution saturated with carbon dioxide catalyzed by purified enzyme and whereas a sharp decrease in calcium carbonate formation has been noted in purified enzyme samples inhibited by EDTA and acetazolamide.     

Surface Percolation for Soil Improvement by Biocementation Utilizing In Situ Enriched Indigenous Aerobic and Anaerobic Ureolytic Soil Microorganisms

The use of biocementation via microbially induced carbonate precipitation (MICP) for improving the mechanical properties of weak soils in the laboratory has gained increased attention in recent years. This study proposes an approach for applying biocementation in situ, by combining the surface percolation of nutrients and cementation solution (urea/CaCl₂) with in situ cultivation of indigenous soil urease positive microorganisms under non-sterile conditions. The enrichment of indigenous ureolytic soil bacteria was firstly tested in batch reactors. Using selective conditions (i.e., pH of 10 and urea concentrations of 0.17 M), highly active ureolytic microorganisms were enriched from four diverse soil samples under both oxygen-limited (anoxic) and oxygen-free (strictly anaerobic) conditions, providing final urease activities of more than 10 and 5 U/mL, respectively. The enrichment of indigenous ureolytic soil microorganisms was secondly tested in pure silica sand columns (300 and 1000 mm) for biocementation applications using the surface percolation approach. By applying the same selective conditions, the indigenous ureolytic soil microorganisms with high urease activity were also successfully enriched for both the fine and coarse sand columns. However, the in situ enriched urease activity was highly related to the dissolved oxygen of the percolated growth medium. The results showed that the in situ cultivated urease activity may produce non-clogging cementation over the entire 1000-mm columns, with unconfined compressive strength varying between 850–1560 kPa (for coarse sand) and 150–700 kPa (for fine sand), after 10 subsequent applications of cementation solution. The typically observed loss of ureolytic activity during the repeated application of the cementation solution was recovered by providing more growth medium under selective enrichment conditions, enabling the in situ enriched ureolytic microorganisms to increase in numbers and urease activity in such a way that continued cementation was possible.     

Biomineralization Consolidation of Fresco Wall Paintings Samples by Bacillus sphaericus

Bacterial-induced mineralization has been explored for protection and consolidation of degraded limestone, concrete and plaster by precipitation of calcium carbonate. It is the first time that Bacillus sphaericus was used for consolidating the nonsterilized decayed wall paintings samples by immersing them in sterile nutritional media. The B. sphaericus used in this study produced urease, which catalyzes the hydrolysis of urea (CO(NH₂)₂) into ammonium (NH₄) and carbonate (CO₃^?2) leading to the precipitation of calcium carbonate. The effect of B. sphaericus on wall paintings was determined by recording the evolution of culture media chemistry and examining the treated wall paintings under a scanning electron microscope to show the structural and morphological evolution of calcium carbonate that was investigated in wall paintings models.     

IMMOBILIZATION OF CARBONIC ANHYDRASE ENZYME PURIFIED FROM Bacillus subtilis VSG-4 AND ITS APPLICATION AS CO2 SEQUESTERER

The purification, immobilization, and characterization of carbonic anhydrase (CA) secreted by Bacillus subtilis VSG-4 isolated from tropical soil have been investigated in this work. Carbonic anhydrase was purified using ammonium sulfate precipitation, Sephadex-G-75 column chromatography, and DEAE-cellulose chromatography, achieving a 24.6-fold purification. The apparent molecular mass of purified CA obtained by SDS-PAGE was found to be 37 kD. The purified CA was entrapped within a chitosan–alginate polyelectrolyte complex (C-A PEC) hydrogel for potential use as an immobilized enzyme. The optimum pH and temperature for both free and immobilized enzymes were 8.2 and 37°C, respectively. The immobilized enzyme had a much higher storage stability than the free enzyme. Certain metal ions, namely, Co²⁺, Cu²⁺, and Fe³⁺, increased the enzyme activity, whereas CA activity was inhibited by Pb²⁺, Hg²⁺, ethylenediamine tetraacetic acid (EDTA), 5,5′-dithiobis-(2-nitrobenzoic acid (DTNB), and acetazolamide. Free and immobilized CAs were tested further for the targeted application of the carbonation reaction to convert CO₂ to CaCO₃. The maximum CO₂ sequestration potential was achieved with immobilized CA (480 mg CaCO₃/mg protein). These properties suggest that immobilized VSG-4 carbonic anhydrase has the potential to be used for biomimetic CO₂ sequestration.     

Production,purification, and characterization of a fusion protein of carbonic anhydrase from Neisseria gonorrhoeae and cellulose binding domain from Clostridium thermocellum

Carbon dioxide capture technologies have the potential to become an important climate change mitigation option through sequestration of gaseous CO₂. A new concept for CO₂ capture involves use of immobilized carbonic anhydrase (CA) that catalyzes the reversible hydration of CO₂ to HCO₃^? and H⁺. Cost‐efficient production of the enzyme and an inexpensive immobilization system are critical for development of economically feasible CA‐based CO₂ capture processes. An artificial, bifunctional enzyme containing CA from Neisseria gonorrhoeae and a cellulose binding domain (CBD) from Clostridium thermocellum was constructed with a His₆ tag. The chimeric enzyme exhibited both CA activity and CBD binding affinity. This fusion enzyme is of particular interest due to its binding affinity for cellulose and retained CA activity, which could serve as the basis for improved technology to capture CO₂ from flue gasses. © 2009 American Institute of Chemical Engineers Biotechnol. Prog., 2009     

Immobilization of carbonic anhydrase in alginate and its influence on transformation of CO2 to calcite

Present investigation entails carbonic anhydrase (CA) immobilization and its influence on transformation of CO₂ to calcite. CA enzyme was immobilized in alginate beads, subsequently maintained its catalytic efficiency after sequential operational cycles. The immobilized beads showed better operational stability by retaining nearly 67% of its initial activity even after six cycles. Batch scale studies with free and immobilized enzyme revealed that the entrapped CA hydrates CO₂ to bicarbonate and/or carbonate which was then made to react with Ca²⁺ ions to transform into calcite. Calcite was characterized by X-ray diffraction (XRD) and scanning electron microscopy (SEM). The entrapped CA was employed for the performance evaluation with respect to several operational parameters including the influence of enzyme concentration in free and immobilized condition. It was concluded that immobilized CA in alginate beads would have the potential for CO₂ sequestration by biomimetic route.     

Arthrobacter Sp. Strain MF-2 Induces High-Mg Calcite Formation: Mechanism and Implications for Carbon Fixation

To better understand the mechanism of formation of carbonate minerals by microbes, culture experiments with Arthrobacter sp. strain MF-2 were carried out using M2 medium without carbonate ions for 50 days. A series of sterile control experiments without bacteria were run simultaneously. During the incubation, cell density, the quantity of precipitate, the extracellular polysaccharide (EPS) content, the activity of carbonic anhydrase (CA), the low molecular weight organic acid concentration, the pH, the electrical conductivity, and the Ca²⁺ and Mg²⁺ concentrations of the medium were determined. The morphologies of the precipitated carbonates were observed using scanning electron microscopy, and their mineral species were determined by X-ray diffraction. The results demonstrated that the quantity of precipitate in the biotic experiments increased gradually with the incubation time; precipitate was not obtained in the abiotic experiments. The average precipitation rate correlated positively with the cell density and the EPS content, with r = 0.64 and 0.61, respectively. This suggests that bacterial cells and EPS effected carbonate precipitation. Carbonate ion incorporation into minerals results from carbon dioxide hydration, promoted by microbial secretion of CA by bacteria. These findings contribute to the ongoing search for feasible mechanisms for the sequestration of carbon dioxide in the subsurface, in this case mediated by microorganisms.     

A Novel Approach to Enhance the Urease Activity of Sporosarcina pasteurii and its Application on Microbial-Induced Calcium Carbonate Precipitation for Sand

Abstract

Urease is involved in the formation of carbonate sediments by microbial-induced calcium carbonate precipitation (MICP), and Sporosarcina pasteurii used extensively in this technique owing to its high urease production. In this study, a simple two-step culture method with the appropriate medium was developed to enhance the urease activity of S. pasteurii. Urea played an important role in the culture process, particularly during the pre-cultivation step and the newly developed method improved both urease activity and specific urease activity. Furthermore, the increase in urease activity by MICP resulted in increased production of calcium carbonate and better strength of bio-cemented sand.     

Engineered Escherichia coli with Periplasmic Carbonic Anhydrase as a Biocatalyst for CO2 Sequestration

Carbonic anhydrase is an enzyme that reversibly catalyzes the hydration of carbon dioxide (CO₂). It has been suggested recently that this remarkably fast enzyme can be used for sequestration of CO₂, a major greenhouse gas, making this a promising alternative for chemical CO₂ mitigation. To promote the economical use of enzymes, we engineered the carbonic anhydrase from Neisseria gonorrhoeae (ngCA) in the periplasm of Escherichia coli, thereby creating a bacterial whole-cell catalyst. We then investigated the application of this system to CO₂ sequestration by mineral carbonation, a process with the potential to store large quantities of CO₂. ngCA was highly expressed in the periplasm of E. coli in a soluble form, and the recombinant bacterial cell displayed the distinct ability to hydrate CO₂ compared with its cytoplasmic ngCA counterpart and previously reported whole-cell CA systems. The expression of ngCA in the periplasm of E. coli greatly accelerated the rate of calcium carbonate (CaCO₃) formation and exerted a striking impact on the maximal amount of CaCO₃ produced under conditions of relatively low pH. It was also shown that the thermal stability of the periplasmic enzyme was significantly improved. These results demonstrate that the engineered bacterial cell with periplasmic ngCA can successfully serve as an efficient biocatalyst for CO₂ sequestration.     

Crassulacean acid metabolism contributes significantly to the in situ carbon budget in a population of the invasive aquatic macrophyte Crassula helmsii

1. The ecophysiological significance of Crassulacean acid metabolism (CAM) in the invasive aquatic macrophyte Crassula helmsii was studied in an English soft‐water lake. The extent and the contribution of CAM to the carbon budget was examined in spring (April) and summer (July) along a depth gradient (0.5–2.2 m), covering the growth range of C. helmsii in the lake. 2. Significant in situ CAM activity (30–80 meq kg⁻¹ FW) was present in all specimens, although it decreased with depth and hence correlated with the decline in photon irradiance. Potential CAM activity (60–161 meq kg⁻¹ FW), measured after exposure to low concentrations of CO₂ in the day and high concentrations at night, were on average 2.7‐times greater than in situ CAM activity. Overall CAM activity increased from April to July, which is consistent with higher potential carbon limitation caused by increased temperature and light availability. 3. CAM activity in C. helmsii appeared to be carbon‐limited at night because night‐time carbon‐fixation increased at raised, compared to ambient, concentrations of CO₂. 4. The high in situ CAM activity in C. helmsii was reflected in the contribution of CAM to the total carbon budget which, independent of depth and season, ranged from 18% to 42%. The amount of CO₂ taken up in the night via CAM was 0.74 to 2.94 times the amount of CO₂ lost in respiration, thus emphasizing the importance of CAM in refixation of potentially lost respiratory CO₂. 5. The onset of decarboxylation in the morning appeared to be under circadian control as there was a delay of up to 5.5 h between the start of the light period and a decline in cell acidity level. 6. There was little variation in δ¹³C content (−21.69 to 23.49‰) with season or depth suggesting, along with the estimated contribution to the carbon‐budget, that CAM is important for the whole population of C. helmsii. CAM may confer a competitive advantage in relation to growth, which may be one of the reasons for the invasiveness of this species.     

Characterization of marine bacterial carbonic anhydrase and their CO2 sequestration abilities based on a soil microcosm

Abstract

The novel technology of biological carbon sequestration using microbial enzymes have numerous advantages over conventional sequestration strategies. In the present study, extracellular carbonic anhydrase (CA) producing bacteria were isolated from water samples in the Arabian Sea, India. A potential isolate, Bacillus safensis isolate AS-75 was identified based on 16S rDNA sequence analysis. The culture conditions suitable for CA production were 32?°C incubation temperature with 4% NaCl and 10?mM Zn supplementation. Experimental optimization of culture conditions enhanced enzyme activity to 265?U mL^?1. CA specific gene was characterized and based on the analysis, the CA of B. safensis isolate AS-75 was a leucine (11.3%) with α-helices as the dominant component in its secondary structure. Based on soil microcosm studies, CA could sequester CO₂ by 95.4%?±?0.11% in sterilized soil with enzyme microcosm. Hence, the application of enzyme was found to be more effective in removing CO₂.     

Moderate precipitation reduction enhances nitrogen cycling and soil nitrous oxide emissions in a semi-arid grassland

The ongoing climate change is predicted to induce more weather extremes such as frequent drought and high-intensity precipitation events, causing more severe drying-rewetting cycles in soil. However, it remains largely unknown how these changes will affect soil nitrogen (N)-cycling microbes and the emissions of potent greenhouse gas nitrous oxide (N₂O). Utilizing a field precipitation manipulation in a semi-arid grassland on the Loess Plateau, we examined how precipitation reduction (ca. −30%) influenced soil N₂O and carbon dioxide (CO₂) emissions in field, and in a complementary lab-incubation with simulated drying-rewetting cycles. Results obtained showed that precipitation reduction stimulated plant root turnover and N-cycling processes, enhancing soil N₂O and CO₂ emissions in field, particularly after each rainfall event. Also, high-resolution isotopic analyses revealed that field soil N₂O emissions primarily originated from nitrification process. The incubation experiment further showed that in field soils under precipitation reduction, drying-rewetting stimulated N mineralization and ammonia-oxidizing bacteria in favor of genera Nitrosospira and Nitrosovibrio, increasing nitrification and N₂O emissions. These findings suggest that moderate precipitation reduction, accompanied with changes in drying-rewetting cycles under future precipitation scenarios, may enhance N cycling processes and soil N₂O emissions in semi-arid ecosystems, feeding positively back to the ongoing climate change.     

Decrease in Hydraulic Conductivity of a Paddy Field using Biocalcification in situ

The hydraulic conductivity of a paddy field (Anthraquic Dystrustept), a silty clay soil containing more than 29% (w/w) of gravel, in Nagoya University Farm was reduced by in situ treatment of subsurface soil using bentonite and biocalcification (microbial calcium carbonate precipitation) through the addition of CaCl₂, urea, and corn steep liquor (CSL). The treatment decreased the hydraulic conductivity of the field from an average of 10^?3 cm/s to a range of 10^?5 to 10^?7 cm/s during 69 days, with reducing the proportion of pores of subsurface soil larger than 75 µm in diameter. The biocalcification effect was observed at 10-cm thickness from the treated subsurface. Laboratory soil core experiments demonstrated that the decrease in the hydraulic conductivity was not attributed to the effect of bentonite but mainly to the effect of biocalcification. The addition of CSL enhanced the urease activity of soil required for biocalcification, even at 4°C, as indicated by a decrease in urease activation energy temperature sensitivity. These experimental results agreed with the gradual decrease in hydraulic conductivity observed in the field when the average daily temperature was 7°C (days 24–69). It was suggested that the biocalcification is a potential technique to reduce the hydraulic conductivity of paddy field.     

Engineering the genetic components of a whole-cell catalyst for improved enzymatic CO2 capture and utilization

Carbonic anhydrase (CA) is a diffusion-limited enzyme that rapidly catalyzes the hydration of carbon dioxide (CO₂). CA has been proposed as an eco-friendly yet powerful catalyst for CO₂ capture and utilization. A bacterial whole-cell biocatalyst equipped with periplasmic CA provides an option for a cost-effective CO₂-capturing system. However, further utilization of the previously constructed periplasmic system has been limited by its relatively low activity and stability. Herein, we engineered three genetic components of the periplasmic system for the construction of a highly efficient whole-cell catalyst: a CA-coding gene, a signal sequence, and a ribosome-binding site (RBS). A stable and halotolerant CA (hmCA) from the marine bacterium Hydrogenovibrio marinus was employed to improve both the activity and stability of the system. The improved secretion and folding of hmCA and increased membrane permeability were achieved by translocation via the Sec-dependent pathway. The engineering of RBS strength further enhanced whole-cell activity by improving both the secretion and folding of hmCA. The newly engineered biocatalyst displayed 5.7-fold higher activity and 780-fold higher stability at 60°C compared with those of the previously constructed periplasmic system, providing new opportunities for applications in CO₂ capture and utilization.     

The effect of carbonic anhydrase,urea and urease on the calcium carbonate deposition in the shell-repair membrane of the snail,Helix pomatia L.

Summary The effect of carbonic anhydrase (CA), urea and urease on the CaCO₃ deposition in the shell-repair membrane of the snail, Helix pomatia, was studied by injection of CA separately or in combination with urease. This treatment resulted in increased deposits of CaCO₃ and apparent crystal formation within the shell-repair membranes compared with those of the controls. The reactions to CA combined with urea were not uniform. Formation of organic crystalline structures and dendritic spherulites was observed in some of these membranes, whereas the deposition of CaCO₃ crystals was suppressed. Administration of urea alone inhibited the formation of large CaCO₃ crystals, whereas urease stimulated this process. The reaction of young snails was greater compared to adults. The membranes of young snails contained tighly packed, small CaCO₃ crystals and organic crystalline structures, which indicated increase of the calcifying centra and their successive mineralization. The results support the assumption that carbonic anhydrase and urease enhance the rate of calcium carbonate deposition and crystal formation in Helix pomatia.     

ARduino-pH Tracker and screening platform for characterization of recombinant carbonic anhydrase in Escherichia coli

Carbonic anhydrase (CA, EC 4.2.1.1) is an ancient enzyme with zinc ion as its active site, which catalyzes the chemical reaction of carbon dioxide (CO₂) to react with water and form bicarbonate ions. Due to its high catalytic efficiency on CO₂ assimilation, CA is expected to use for carbon sequestration in industry. However, the protein expression level, thermostability and high-throughput screening of an active CA are still with difficulty. In this study, the CA from Sulfurihydrogenibium yellowstonense (denoted as SyCA) was selected for overexpressed in Escherichia coli by different pET vectors. The enzymatic properties including thermo-stability, pH tolerance, effect of metal ion, and kinetic parameters were characterized through a novel ARduino-pH Tracker (ART) for monitoring online effectively. The SyCA is thermophilic and acidophilic as it maintains 100% activity at 50°C, while the residual activity is 34.8% after heating at 80°C for 150 min and the optimal pH is 3–5. The kinetic analysis by ART system showed that the k _cat/K _m of free enzyme was 4.4-folds that that of whole cell. On the other hand, the screening platforms as Wilbur–Anderson unit, phenol red indicator and size of colony forming unit have been established to explore CA with higher activity. The high-throughput screening platform is support in direct evolution of CA and further used in the industry.     

Expression, reconstruction and characterization of codon-optimized carbonic anhydrase from Hahella chejuensis for CO2 sequestration application

The high production of functional carbonic anhydrase (CA) is required for practical CO₂ sequestration application mediated by CA. Here, the synthetic gene based on Escherichia coli codon usage of new α-type CA (HC-aCA) of Hahella chejuensis, a Korea marine microorganism, was highly expressed in E. coli. We obtained a high yield of functional HC-aCA by denaturing/refolding process and incorporating zinc ion into its active site. The refolded HC-aCA displayed a half-deactivation temperature of 60 °C with maximal activity at 50 °C, and had high pH stability in alkali condition with maximal activity at pH 10.0. The esterase activity of HC-aCA almost doubled at high salt concentration ranging from 0.67 to 2.0 M NaCl. HC-aCA catalyzed the conversion of CO₂ to CaCO₃ as calcites form in the presence of Ca²⁺. The refolded HC-aCA could be a promising candidate for the development of efficient CA-based CO₂ sequestration processes.     

An evaluation of abiotic carbon sinks in deserts

Recent field studies have reported anomalous CO₂ uptake using eddy‐covariance techniques in arid and semiarid ecosystems. The rates of CO₂ uptake are incompatible with changes in situ of organic carbon pools. Here, I examine several potential mechanisms of abiotic CO₂ uptake in arid and semiarid soils: atmospheric pressure pumping, carbonate dissolution, and percolation of soil water through the vadose zone. Each mechanism is deemed inadequate to explain the observations of the eddy‐covariance systems, which must now be questioned for their accuracy in desert ecosystems.     

Unravelling the microbial role in ooid formation – results of an in situ experiment in modern freshwater Lake Geneva in Switzerland

The microbial role in the formation of the cortex of low‐Mg calcite freshwater ooids in western part of Lake Geneva in Switzerland has been suggested previously, but not demonstrated conclusively. Early work mostly concentrated in hypersaline milieus, and hence little is known about their genesis in freshwater environments. We designed an in situ experiment to mimic the natural process of low‐Mg calcite precipitation. A special device was placed in the ooid‐rich bank of the lake. It contained frosted glass (SiO₂) slides, while quartz (SiO₂) is the most abundant mineral composition of ooid nuclei that acted as artificial substrates to favour microbial colonization. Microscopic inspection of the slides revealed a clear seasonal pattern of carbonate precipitates, which were always closely associated with biofilms that developed on the surface of the frosted slides containing extracellular polymeric substance, coccoid and filamentous cyanobacteria, diatoms and heterotrophic bacteria. Carbonate precipitation peaks during early spring and late summer, and low‐Mg calcite crystals mostly occur in close association with filamentous and coccoid cyanobacteria (e.g. Tolypothrix, Oscillatoria and Synechococcus, Anacystis, respectively). Further scanning electron microscope inspection of the samples revealed low‐Mg calcite with crystal forms varying from anhedral to euhedral rhombohedra, depending on the seasons. Liquid cultures corroborate the in situ observations and demonstrate that under the same physicochemical conditions the absence of biofilms prevents the precipitation of low‐Mg calcite crystals. These results illustrate that biofilms play a substantial role in low‐Mg calcite ooid cortex formation. It further demonstrates the involvement of microbes in the early stages of ooid development. Combined with ongoing microbial cultures under laboratory‐controlled conditions, the outcome of our investigation favoured the hypothesis of external microbial precipitation of low‐Mg calcite as the main mechanism involved in the early stage of ooid formation in freshwater Lake Geneva.