Aluminum tolerance in Pseudomonas fluorescens ATCC 13525: Involvement of a gelatinous lipid-rich residue

Abstract Pseudomonas fluorescens was found to grow in a mineral medium supplemented with up to 50 mM aluminum, complexed to citrate, the sole source of carbon. At stationary phase while virtually no diminution in cellular yield was observed in the presence of 1.0 mM aluminum, only 31% of bacterial yield was recorded in media with 50 mM aluminum. The decrease in soluble aluminum in the culture fluid was concomitant with the formation of a gelatinous residue. At later stages of growth, the trivalent metal was immobilized in this deposit. This bioprecipitate consisted of lipid moieties but was apparently devoid of proteins and carbohydrates. X-ray fluorescence spectroscopy and colorimetric assays also revealed the presence of aluminum and phosphorus. X-ray diffraction spectroscopy indicated that the biomineral was amorphous. Examination of the gelatinous residue by scanning electron microscopy and energy dispersive X-ray microanalysis aided in the identification of aluminum, oxygen and phosphorus rich irregular bodies that were associated with carbon containing thread-like structures.     

Porous Allograft Bone Scaffolds: Doping with Strontium

Strontium (Sr) can promote the process of bone formation. To improve bioactivity, porous allograft bone scaffolds (ABS) were doped with Sr and the mechanical strength and bioactivity of the scaffolds were evaluated. Sr-doped ABS were prepared using the ion exchange method. The density and distribution of Sr in bone scaffolds were investigated by inductively coupled plasma optical emission spectrometry (ICP-OES), X-ray photoelectron spectroscopy (XPS), and energy-dispersive X-ray spectroscopy (EDS). Controlled release of strontium ions was measured and mechanical strength was evaluated by a compressive strength test. The bioactivity of Sr-doped ABS was investigated by a simulated body fluid (SBF) assay, cytotoxicity testing, and an in vivo implantation experiment. The Sr molar concentration [Sr/(Sr+Ca)] in ABS surpassed 5% and Sr was distributed nearly evenly. XPS analyses suggest that Sr combined with oxygen and carbonate radicals. Released Sr ions were detected in the immersion solution at higher concentration than calcium ions until day 30. The compressive strength of the Sr-doped ABS did not change significantly. The bioactivity of Sr-doped material, as measured by the in vitro SBF immersion method, was superior to that of the Sr-free freeze-dried bone and the Sr-doped material did not show cytotoxicity compared with Sr-free culture medium. The rate of bone mineral deposition for Sr-doped ABS was faster than that of the control at 4 weeks (3.28±0.23 µm/day vs. 2.60±0.20 µm/day; p<0.05). Sr can be evenly doped into porous ABS at relevant concentrations to create highly active bone substitutes.     

Strontium ranelate changes the composition and crystal structure of the biological bone-like apatite produced in osteoblast cell cultures

We evaluate the effects of strontium ranelate on the composition and crystal structure of the biological bone-like apatite produced in osteoblast cell cultures, a system that gave us the advantage of obtaining mineral samples produced exclusively during treatment. Cells were treated with strontium ranelate at concentrations of 0.05 and 0.5 mM Sr²⁺. Mineral substances were isolated and analyzed by using a combination of methods: Fourier transform infrared spectroscopy, solid-state ¹H nuclear magnetic resonance, X-ray diffraction, micro-Raman spectroscopy and energy dispersive X-ray spectroscopy. The minerals produced in all cell cultures were typical bone-like apatites. No changes occurred in the local structural order or crystal size of the minerals. However, we noticed several relevant changes in the mineral produced under 0.5 mM Sr²⁺: (1) increase in type-B CO₃ ^2? substitutions, which often lead to the creation of vacancies in Ca²⁺ and OH^? sites; (2) incorporation of Sr²⁺ by substituting slightly less than 10 % of Ca²⁺ in the apatite crystal lattice, resulting in an increase in both lattice parameters a and c; (3) change in the PO₄ ^3? environments, possibly because of the expansion of the lattice; (4) the Ca/P ratio of this mineral was reduced, but its (Ca+Sr)/P ratio was the same as that of the control, indicating that its overall cation/P ratio was preserved. Thus, strontium ranelate changes the composition and crystal structure of the biological bone-like apatite produced in osteoblast cell cultures.     

梭菌MH18 菌株诱导碳酸盐矿物的形成

【目的】研究细菌作用下碳酸盐矿物的形成过程有助于了解微生物成矿的机理。【方法】在LagoaVermelha培养基中(Mg/Ca为6:1)对一株分离自土壤样品的梭菌MH18菌株进行了为期35天的碳酸盐矿物培养实验,同时还完成了一组无菌对照实验。利用X-射线衍射技术对沉淀物的矿物成分进行了测定,利用光学显微镜和扫描电子显微镜对沉淀物的形态进行了系统的观察。【结果】MH18菌株在Lagoa Vermelha培养基中诱导形成了以高镁方解石为主的碳酸盐矿物;这些矿物起初具有哑铃状的外形,后来发展为球状;无菌对照实验中出现少量沉淀物,但X-射线衍射技术图谱显示它们是非晶态物质。【结论】MH18菌株具有促进碳酸盐矿物结晶的功能;碳酸盐矿物的特殊形态(哑铃状和球状)可能与细菌形态存在着某种成因上的联系。     

Mineralogical transformation and neoformation in granite caused by the lichens Tephromela atra and Ochrolechia parella

Tephromela atra and Ochrolechia parella are among the most abundant lichens colonizing granitic monuments in the region of Galicia (northwest Spain). In this work, their interaction with a two-mica granite used in the construction of the Toxosoutos Monastery (Noia, Galicia) was studied, using optical microscopy, scanning electron microscopy (with back-scattered-electron and energy-dispersive X-ray detection), X-ray diffractometry and atomic absorption spectroscopy to evaluate their physical, mineralogical and chemical effects. Both lichens contributed to physical weathering by penetrating intermineral voids and mineral cleavage planes, disaggregating the rock and entrapping the loosened mineral grains in their thalli. Significant chemical and mineralogical weathering also occurred, including depletion of potassium from biotite, transformation of this mica into hydroxyaluminium-vermiculite, and neoformation of whewellite and calcite in the lichen thalli. Neoformation of these calcium minerals on a calcium-poor rock such as granite is noteworthy, and this is the first time calcium carbonate has been detected within a lichen colonizing a granitic rock. Precipitation of the calcium carbonate was attributed to the local pH in the thalli having been raised due to release of sodium from nearby plagioclase during weathering.     

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.     

Physiological characterization of strain DCB-1, a unique dehalogenating sulfidogenic bacterium

Strain DCB-1 is an obligately anaerobic bacterium which carries out the reductive dehalogenation of halobenzoates and was previously known to grow only on pyruvate plus 20% ruminal fluid. When various electron acceptors were supplied, thiosulfate and sulfite were found to stimulate growth. Sulfide was produced from thiosulfate. Cytochrome c and desulfoviridin were detected. The mol% G+C was 49 (at the thermal denaturation temperature). Of 55 carbon sources tested, only pyruvate supported growth as the sole carbon source in mineral medium. Lactate, acetate, L- and D-malate, glycerol, and L- and D-arabinose stimulated growth when supplemented with 10% ruminal fluid and 20 mM thiosulfate. In mineral medium, pyruvate was converted to acetate and lactate, with small amounts of succinate and fumarate accumulating transiently. During growth with thiosulfate, all of these products accumulated transiently. Addition of excess hydrogen to pyruvate-grown cultures resulted in diversion of carbon to formate, lactate, and butyrate, which caused a decrease in cell yield. We conclude that strain DCB-1 is a new type of sulfidogenic bacterium.     

Physiological characterization of strain DCB-1, a unique dehalogenating sulfidogenic bacterium.

Strain DCB-1 is an obligately anaerobic bacterium which carries out the reductive dehalogenation of halobenzoates and was previously known to grow only on pyruvate plus 20% ruminal fluid. When various electron acceptors were supplied, thiosulfate and sulfite were found to stimulate growth. Sulfide was produced from thiosulfate. Cytochrome c and desulfoviridin were detected. The mol% G+C was 49 (at the thermal denaturation temperature). Of 55 carbon sources tested, only pyruvate supported growth as the sole carbon source in mineral medium. Lactate, acetate, L- and D-malate, glycerol, and L- and D-arabinose stimulated growth when supplemented with 10% ruminal fluid and 20 mM thiosulfate. In mineral medium, pyruvate was converted to acetate and lactate, with small amounts of succinate and fumarate accumulating transiently. During growth with thiosulfate, all of these products accumulated transiently. Addition of excess hydrogen to pyruvate-grown cultures resulted in diversion of carbon to formate, lactate, and butyrate, which caused a decrease in cell yield. We conclude that strain DCB-1 is a new type of sulfidogenic bacterium.     

Amorphous and crystalline calcium carbonate distribution in the tergite cuticle of moulting Porcellio scaber (Isopoda, Crustacea)

The main mineral components of the isopod cuticle consists of crystalline magnesium calcite and amorphous calcium carbonate. During moulting isopods moult first the posterior and then the anterior half of the body. In terrestrial species calcium carbonate is subject to resorption, storage and recycling in order to retain significant fractions of the mineral during the moulting cycle. We used synchrotron X-ray powder diffraction, elemental analysis and Raman spectroscopy to quantify the ACC/calcite ratio, the mineral phase distribution and the composition within the anterior and posterior tergite cuticle during eight different stages of the moulting cycle of Porcellio scaber. The results show that most of the amorphous calcium carbonate (ACC) is resorbed from the cuticle, whereas calcite remains in the old cuticle and is shed during moulting. During premoult resorption of ACC from the posterior cuticle is accompanied by an increase within the anterior tergites, and mineralization of the new posterior cuticle by resorption of mineral from the anterior cuticle. This suggests that one reason for using ACC in cuticle mineralization is to facilitate resorption and recycling of cuticular calcium carbonate. Furthermore we show that ACC precedes the formation of calcite in distal layers of the tergite cuticle.     

岩溶洞穴微生物沉积碳酸钙——以贵州石将军洞为例

为探讨洞穴微生物沉积碳酸钙作用对洞穴沉积物的影响,利用传统生物学方法,采集贵州中西部地区石将军洞洞穴沉积物表面的微生物样品,结合洞穴监测数据和理化背景资料,利用B-4培养基和B-4C培养基对洞穴细菌进行筛选和纯化,分离出能沉积碳酸钙的菌种,观察和了解洞穴细菌形成的CaCO3晶体,应用X射线衍射分析仪(XRD)分析细菌形成的CaCO3晶体成分,并利用扫描电子显微镜(SEM)观察晶体结构特征。结果表明:1)在B-4培养基下微生物产生的碳酸钙晶体主要为方解石、球霰石和方解石混合物、球霰石,这种变化与培养基pH值的增幅相关;同时,在添加Mg离子的B-4C培养基下形成的碳酸钙晶体主要为方解石,此外,研究中并未检测到文石晶体。2)通过SEM扫描,发现微生物作用形成的碳酸钙晶体存在不规则六方体、柱状体、四方体层状、半球状等,这些晶体形态在化学作用系统下少见,多见于微生物作用形成的方解石。此外,晶体中微生物作用痕迹明显,微生物作用贯穿于整个沉积过程。     

低Mg/Ca条件下丛毛单胞菌HJ-1菌株诱导文石的形成

【目的】为了探讨细菌对碳酸盐矿物种类和形态的影响。【方法】本文利用丛毛单胞菌HJ-1菌株进行了持续50 d的培养实验。在实验过程中,对细菌数量、沉淀物重量、培养液中Ca2+和Mg2+浓度等进行了动态监测。利用扫描电子显微镜对矿物形态进行了观察,并利用X-射线衍射仪对矿物成分进行测定。【结果】丛毛单胞菌HJ-1菌株具有显著的诱导碳酸盐矿物沉淀的能力,碳酸盐矿物的重量随着培养时间的延长而逐渐增加。X-射线衍射结果表明,形成的碳酸盐沉淀主要由文石和高镁方解石组成,其中文石的最高含量达86%。上述矿物在形态上复杂多样,主要有杆状、柱状、哑铃形、球状和板状以及不规则状和鳞片状集合体。【结论】通常,在Mg/Ca≤2并且有微生物参与的条件下极少形成文石。本文在Mg/Ca为2,不含碳酸根离子的培养基中培养HJ-1菌株的过程中发现了文石。作者认为,低Mg/Ca条件下文石的形成主要与HJ-1菌株分泌较多的胞外多糖有关。     

Investigation of inorganic deposits in selected organic matrices

Inorganic deposits in the wall of human and animal arteries and in experimental tumor (Morris hepatoma 7777) were examined using proton induced X-ray emission (PIXE) and PIXE in combination with proton microprobe (micro-PIXE) techniques. The sections adjacent to the irradiated ones part were submitted to histological investigations and one part of the material was additionally investigated by infrared (IR) spectroscopy. For identification of mineral deposits, the micro-PIXE method appeared the most sensitive. The mineral deposits were detected in the artery samples, even in those without visible morphological changes, as well as in tumor samples. The deposites showed different localization and composition, depending on age and type of vessel. There were also differences between human and animal arteries. IR spectroscopy revealed the presence of carbonate apatite within the artery samples from old individuals. Matching of histological observations with data obtained by micro-PIXE method allows a better correlation of morphological and analytical results.     

An antarctic psychrotrophic bacterium Halomonas sp. ANT-3b, growing on n-hexadecane, produces a new emulsyfying glycolipid

A bacterial strain ANT-3b was isolated at the sea-ice seawater interface from Terra Nova Bay station, Ross Sea, Antarctica. It was isolated on mineral medium supplemented with 2% diesel fuel as a sole carbon and energy source and grown routinely on 2% n-hexadecane. Analysis of 16S rRNA gene sequence indicates that the strain has 99.8% sequence similarity with Halomonas neptunia. The strain ANT-3b was grown in mineral medium supplemented with n-hexadecane between 4 and 20 degrees C, but not at 30 degrees C. The maximum degradation rate of the n-alkane was measured at 15 degrees C, with 5.6+/-1.7 mg O2 microg(-1) protein d(-1). The strain ANT-3b produced emulsifying compounds when grown on n-hexadecane, but not on mineral medium supplemented with D-fructose. A preliminary characterisation of the emulsifier was carried out. The lipid moiety contained a mixture of fatty acids with a following composition in molar ratio: caprylic acid 18.85, myristic acid 1.0, palmitic acid 9.68, palmitoleic acid 5.69 and oleic acid 1.26. The polysaccharide moiety also contained a mixture of sugars with the following molar ratio: mannose 1.71, galactose 1.00 and glucose 2.96. The molecular weight of the glycolipid component determined by gel permeation chromatography was in the 18 kDa range and contained smaller fragments, possibly oligomeric contaminants. Transmission electron microscopy showed contact between the glycolipid secreted by the strain and n-hexadecane broken down to nanodroplets at the water interface, to form a material with mesophase (liquid crystal) organisation.     

The formation of phenol in the degradation ofp-hydroxybenzoic acid byKlebsiella aerogenes (Aerobacter aerogenes)

After growth ofK. aerogenes in chemically defined media consisting of mineral salts andp-hydroxybenzoate with or without glucose, phenol was found in the culture fluid at concentrations inhibiting further growth. Bacteria adapted to mineral salts medium containingp-hydroxybenzoate as sole source of carbon and energy produced small but isolable quantities of 3,4-dihydroxybenzoic acid and catechol and oxidized these substances as rapidly asp-hydroxybenzoate. Bacteria adapted to mineral salts medium containing glucose as sole carbon and energy source did not oxidizep-hydroxybenzoate, 3,4-dihydroxybenzoate or catechol. Bacteria adapted to glucose medium or top-hydroxybenzoate medium did not oxidize or utilize phenol as sole carbon and energy source. A metabolic pathway forp-hydroxybenzoate degradation is proposed and the formation of phenol is attributed to a side reaction.     

Monohydrocalcite in calcareous corpuscles of Mesocestoides corti

Mesocestoides corti (syn. vogae), as many other cestode platyhelminthes, contains abundant mineralized structures called calcareous corpuscles. These concretions may constitute as much as 40% of the dry weight of the organisms, but their function remains poorly understood. In this work, we reviewed the mineral composition of the calcareous corpuscles of M. corti. X-ray diffraction pattern showed that the major mineral component of the corpuscles is a hydrated form of calcium carbonate, monohydrocalcite, also confirmed by infrared spectrometry. The baseline shift of the X-ray diffraction spectra suggested the presence of amorphous calcium carbonate, accordingly to previous reports, and an organic matrix was confirmed by FTIR. Monohydrocalcite is a rare mineral unusually found in biominerals. Although the significance of monohydrocalcite in biominerals has not been determined, the knowledge of corpuscles composition is of relevance to establish their function and for the elucidation of the mechanisms involved in mineralization processes.     

Mineral Distributions at the Developing Tendon Enthesis

Tendon attaches to bone across a functionally graded interface, “the enthesis”. A gradient of mineral content is believed to play an important role for dissipation of stress concentrations at mature fibrocartilaginous interfaces. Surgical repair of injured tendon to bone often fails, suggesting that the enthesis does not regenerate in a healing setting. Understanding the development and the micro/nano-meter structure of this unique interface may provide novel insights for the improvement of repair strategies. This study monitored the development of transitional tissue at the murine supraspinatus tendon enthesis, which begins postnatally and is completed by postnatal day 28. The micrometer-scale distribution of mineral across the developing enthesis was studied by X-ray micro-computed tomography and Raman microprobe spectroscopy. Analyzed regions were identified and further studied by histomorphometry. The nanometer-scale distribution of mineral and collagen fibrils at the developing interface was studied using transmission electron microscopy (TEM). A zone (∼20 µm) exhibiting a gradient in mineral relative to collagen was detected at the leading edge of the hard-soft tissue interface as early as postnatal day 7. Nanocharacterization by TEM suggested that this mineral gradient arose from intrinsic surface roughness on the scale of tens of nanometers at the mineralized front. Microcomputed tomography measurements indicated increases in bone mineral density with time. Raman spectroscopy measurements revealed that the mineral-to-collagen ratio on the mineralized side of the interface was constant throughout postnatal development. An increase in the carbonate concentration of the apatite mineral phase over time suggested possible matrix remodeling during postnatal development. Comparison of Raman-based observations of localized mineral content with histomorphological features indicated that development of the graded mineralized interface is linked to endochondral bone formation near the tendon insertion. These conserved and time-varying aspects of interface composition may have important implications for the growth and mechanical stability of the tendon-to-bone attachment throughout development.     

Microbial metabolism of quinoline and related compounds. VI. Degradation of quinaldine by Arthrobacter sp

Quinaldine catabolism was investigated with the bacterial strain Arthrobacter sp., which is able to grow aerobically in a mineral salt medium with quinaldine as sole source of carbon, nitrogen and energy. The following degradation products of quinaldine were isolated from the culture fluid and identified: 1H-4-oxoquinaldine, N-acetylisatic acid, N-acetylanthranilic acid, anthranilic acid, 3-hydroxy-N-acetylanthranilic acid and catechol. 3-Hydroxy-N-acetylanthranilic acid was not further metabolized by this organism. A degradation pathway is proposed.     

Calcite-forming Bacillus licheniformis Thriving on Underwater Speleothems of a Hydrothermal Cave

The underwater environment of Grotta Giusti (Monsummano Terme, Italy) is a suggestive setting with different types of speleothems including “leafy” and “cauliflower” concretions along the walls and roof, and conical pseudo-stalagmites on the floor. Very high calcium and dissolved CO₂ levels, and massive calcium carbonate precipitation characterize this cave environment. Yet, life thrives on the leafy concretion surfaces with loads of cultivable heterotrophic microorganisms around 10⁵ colony-forming units per cm². Bacillus licheniformis appeared to be the prevalent cultivable microorganism on a low-nutrient medium that was used for screening. 16S rRNA gene-based polymerase chain reaction–single strand conformation polymorphism profiling indicated that Group VI Bacillaceae species was well represented in the bacterial community of underwater speleothems. Interpretation of X-ray diffraction spectra and Raman spectroscopy data indicated that the B. licheniformis isolate produced in vitro abundant calcite microcrystals that were also characterized by scanning electron microscopy coupled with energy dispersive X-ray spectroscopy. Production of calcite microcrystals was analyzed in different media (Christensen’s urea agar and B4 calcium carbonate precipitation medium) and incubation conditions, and it was found to be enhanced by nitrate supplement in B4 medium under low-oxygen conditions. B4 and B4-nitrate media also stimulated antibiotic production by the B. licheniformis isolate, which was analyzed by microbiological assays.     

Uranyl precipitation by Pseudomonas aeruginosa via controlled polyphosphate metabolism

The polyphosphate kinase gene from Pseudomonas aeruginosa was overexpressed in its native host, resulting in the accumulation of 100 times the polyphosphate seen with control strains. Degradation of this polyphosphate was induced by carbon starvation conditions, resulting in phosphate release into the medium. The mechanism of polyphosphate degradation is not clearly understood, but it appears to be associated with glycogen degradation. Upon suspension of the cells in 1 mM uranyl nitrate, nearly all polyphosphate that had accumulated was degraded within 48 h, resulting in the removal of nearly 80% of the uranyl ion and >95% of lesser-concentrated solutions. Electron microscopy, energy-dispersive X-ray spectroscopy, and time-resolved laser-induced fluorescence spectroscopy (TRLFS) suggest that this removal was due to the precipitation of uranyl phosphate at the cell membrane. TRLFS also indicated that uranyl was initially sorbed to the cell as uranyl hydroxide and was then precipitated as uranyl phosphate as phosphate was released from the cell. Lethal doses of radiation did not halt phosphate secretion from polyphosphate-filled cells under carbon starvation conditions.     

Intracellular and Extracellular Biomineralization Induced by Klebsiella pneumoniae LH1 Isolated from Dolomites

Abstract

The interaction between bacteria and minerals is very complicated and has been intensively studied in the laboratory and the field in the last few decades, but the processes and mechanisms of biomineralization and mineral precipitation are still not fully understood and need to be explored further. In the present work, biomineralization experiments were undertaken using Klebsiella pneumoniae LH1, collected from a natural surface environment in an area of outcrops of Cambrian dolomite, in a culture medium with various Mg/Ca molar ratios (0, 3, 6 and 12). The mineral precipitates obtained were analyzed by X-ray diffraction (XRD), scanning electron microscope (SEM), energy dispersive spectrometer (EDS), Fourier transform infrared spectrometer (FTIR), laser scanning confocal microscopy (LSCM) and X-ray photoelectron spectroscopy (XPS). Cells were analyzed with a scanning transmission electron microscope (STEM), high resolution transmission electron microscope (HRTEM) and selected area electron diffraction (SAED). The composition of amino acids in extracellular polymeric substances (EPS) was also determined. In the experiments it was found that the production of ammonia and the presence of carbonate anhydrase promoted the increase of the medium pH and that minerals are nucleated on the EPS, which consist chiefly of amino acids and negatively-charged organic functional groups. With increasing Mg/Ca ratios, the mineral phases changed, including calcite (100%) at Mg/Ca molar ratio of 0, monohydrocalcite (36.05%) + dypingite (63.95%) at Mg/Ca molar ratio of 3, monohydrocalcite (29.72%) + dypingite (15.48%) + nesquehonite (54.80%) at Mg/Ca molar ratio of 6, and monohydrocalcite (14.2%) + dypingite (1.0%) + nesquehonite (84.80%) at Mg/Ca molar ratio of 12. Some intracellular amorphous calcium- and magnesium-rich inclusions were also detected in K. pneumoniae LH1, suggesting intracellular biomineralization accompanying the extracellular mineral precipitation. This study provides further understanding of the biomineralization processes of microorganisms.