The Characterization of Intracellular and Extracellular Biomineralization Induced by Synechocystis sp. PCC6803 Cultured under Low Mg/Ca Ratios Conditions

In order to simulate the precipitation process of microbial limestone at the offshore of the ancient ocean, different calcites induced by Synechocystis sp. PCC6803 in culture media with low Mg/Ca ratios (0.01 M Ca²⁺, Mg/Ca = 0, 0.2, 0.4, 0.6) were investigated, and the characteristics of intracellular and extracellular biomineralization were described. Carbonic anhydrase activity of Synechocystis sp. PCC6803 in different culture medium was further detected. The ultrathin slices of Synechocystis sp. PCC6803 cells were analyzed by transmission electron microscope (TEM) and selected area electron diffraction (SAED). Then the precipitates were analyzed by polarizing microscope, scanning electron microscope (SEM), X-ray diffraction (XRD) and energy dispersive spectrometer (EDS). The results showed that the biomineralization precipitates of Synechocystis sp. PCC6803 under low Mg/Ca ratios were mainly calcites with different morphologies. The CA accelerated the pivotal rate limiting step of the calcite precipitation. It was also found that the morphology, microstructure, particle size, preferred orientation, crystallinity and cell volume of calcites changed gradually with the increasing Mg²⁺ concentrations. What is more important, it was found that Synechocystis sp. PCC6803 had the ability of intracellular biomineralization without crystal structure. The intracellular biomineralization product could be divided into two types. This study can provide some useful information for further understanding the characteristics and mechanisms of biomineralization and even the diagenetic environment research of microbial limestone.     

Precipitation of calcite induced by Synechocystis sp. PCC6803

Calcite with laminate structure was successfully prepared by culturing Synechocystis sp. PCC6803 with different concentrations of calcium chloride (CaCl₂) in BG11 media. S. PCC6803 was examined by scanning electron microscopy (SEM), transmission electron microscopy (TEM), laser confocal scanning microscope (LCSM) and energy dispersive spectroscopy (EDS). The effects of Ca²⁺ concentrations and pH values on calcification were investigated and the micro morphs of the CaCO₃ crystals were observed by means of SEM. These results showed that CaCO₃ crystals could be more easily formed with increasing the concentration of CaCl₂ in S. PCC6803 culture solution. S. PCC6803 could largely bind calcium ions, most of which were present in extracellular polymeric substances and on the cell wall. Inside the cells there were a lot of circular areas rich in calcium ions without the crystallization of calcium. Some cells produced a thicker gelatinous sheath outside of the translucent organic thin layer. And the cells inside also produced major changes that the original chloroplasts were almost transformed into starch grains whose sizes were from 0.5 to 1 μm with relatively uniform in sizes. At the same time the cell sizes significantly reduced to only about 8–9 μm almost changing to half of its original diameters. The calcite crystals with a highly preferred orientation induced by S. PCC6803 were observed with X-ray diffraction (XRD). A critical implication was that S. PCC6803 could induce bio-calcification and then mediate the further growth of CaCO₃ crystals in the biological system.     

Non-ureolytic calcium carbonate precipitation by <Emphasis Type="Italic">Lysinibacillus</Emphasis> sp. YS11 isolated from the rhizosphere of <Emphasis Type="Italic">Miscanthus sacchariflorus</Emphasis>

Although microbially induced calcium carbonate precipitation (MICP) through ureolysis has been widely studied in environmental engineering fields, urea utilization might cause environmental problems as a result of ammonia and nitrate production. In this study, many non-ureolytic calcium carbonate-precipitating bacteria that induced an alkaline environment were isolated from the rhizosphere of Miscanthus sacchariflorus near an artificial stream and their ability to precipitate calcium carbonate minerals with the absence of urea was investigated. MICP was observed using a phase-contrast microscope and ion-selective electrode. Only Lysinibacillus sp. YS11 showed MICP in aerobic conditions. Energy dispersive X-ray spectrometry and X-ray diffraction confirmed the presence of calcium carbonate. Field emission scanning electron microscopy analysis indicated the formation of morphologically distinct minerals around cells under these conditions. Monitoring of bacterial growth, pH changes, and Ca²⁺ concentrations under aerobic, hypoxia, and anaerobic conditions suggested that strain YS11 could induce alkaline conditions up to a pH of 8.9 and utilize 95% of free Ca²⁺ only under aerobic conditions. Unusual Ca²⁺ binding and its release from cells were observed under hypoxia conditions. Biofilm and extracellular polymeric substances (EPS) formation were enhanced during MICP. Strain YS11 has resistance at high pH and in high salt concentrations, as well as its spore-forming ability, which supports its potential application for self-healing concrete.     

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.     

Calcium transients in response to salinity and osmotic stress in the nitrogen-fixing cyanobacterium Anabaena sp. PCC7120, expressing cytosolic apoaequorin

We show here that both salinity and osmotic stress trigger transient increases in intracellular free Ca²⁺ concentration ([Ca²⁺]_i) in cells of the nitrogen‐fixing filamentous cyanobacterium Anabaena sp. PCC7120, which constitutively expresses apoaequorin. Isoosmolar concentrations of salt (NaCl) and osmoticum (sucrose) induced calcium transients of similar magnitude and shape, suggesting that cells sense, via Ca²⁺ signalling, mostly osmotic stress. The Ca²⁺ transients induced by NaCl and sucrose were completely blocked by the calcium chelator ethylene glycol‐bis(b‐aminoethylether)N,N,N¢,N¢‐tetraacetic acid (EGTA) and were partially inhibited by the calcium channel blocker verapamil. Increased external Ca²⁺ and the Ca²⁺ ionophore calcimycin (compound A23187) enhanced Ca²⁺ influx further, suggesting the involvement of extracellular Ca²⁺ in the observed response to salinity and osmotic stress. However, the plant hormone abscisic acid (ABA) did not provoke any effect on the Ca²⁺ transients induced by both stresses, indicating that it may not be acting upstream of Ca²⁺ in the signalling of salinity and/or osmotic stress in Anabaena sp. PCC7120.     

Hysteretic activation of the Ca pump revealed by calcium transients in human red cells

The enzymatic basis for the Ca²⁺ pump in human red cells is an ATPase with hysteretic properties. The Ca²⁺-ATPase shifts slowly between a ground state deficient in calmodulin and an active state saturated with calmodulin, and rate constants for the reversible shifts of state were recently determined at different Ca²⁺ concentrations (Scharff, O. and Foder, B. (1982) Biochim. Biophys. Acta 691, 133–143). In order to study whether the Ca²⁺ pump in intact red cells also exhibits hysteretic properties we have analysed transient increases of intracellular calcium concentrations (Ca_i), induced by the divalent cation ionophore A23187. The time-dependent changes of Ca_i were measured by use of radioactive calcium (⁴⁵Ca²⁺) and analysed with the aid of a mathematical model, based partly on the Ca²⁺-dependent parameters obtained from Ca²⁺-ATPase experiments, partly on the A23187-induced Ca²⁺ fluxes determined in experiments with intact red cells. According to the model a delay in the activation of the Ca²⁺ pump is a prerequisite for the occurrence of A23187-induced calcium transients in the red cells, and we conclude that the Ca²⁺ pump in human red cells responds hysteretically. It is suggested that Ca²⁺ pumps in other types of cell also have hysteretic properties.     

The Degradation of Dimethoate and the Mineral Immobilizing Function for Cd2+ by Pseudomonas putida

Organophosphorus pollution and heavy metal pollution are prominent in China and have caused increasingly severe environmental pollution. This research used Pseudomonas putida to degrade dimethoate so as to induce the formation of calcium carbonate (CaCO₃) and calcium phosphate (Ca₃(PO₄)₂) in beef extract peptone medium. In addition, the mineral immobilizing function of the generated Ca₃(PO₄)₂ and CaCO₃ for Cd²⁺ was studied by adding different concentrations of Cd²⁺ to the culture solution. Meanwhile, transmission electron microscopy (TEM), scanning electronic microscopy (SEM), X-ray diffraction, gas chromatography and atomic absorption spectrophotometry were used to investigate the biodegradation of dimethoate, the concentration variation of Ca²⁺ and Cd²⁺, the mineral and chemical compositions of the precipitates. The results showed that the growth of P. Putida could increase the pH value of the culture solution and effectively degrade the organophosphorus pesticide dimethoate. Besides, the concentration of Ca²⁺ in the culture solution decreased significantly in the first four days and then tended to be stable. Moreover, the TEM and SEM results presented that there were large amounts of biogenic sedimentary CaCO₃ and a little Ca₃(PO₄)₂ in the precipitates. Furthermore, in the employed culture system, the removal rates of Cd²⁺, when added at two different concentrations (6 ppm and 15 ppm), reached 100%. Therefore, this study provided a new idea for treating wastewater polluted with organophosphorus pesticide and heavy metals by using microorganisms.     

Bacterial Calcium Carbonate Precipitation in Cave Environments: A Function of Calcium Homeostasis

To determine if microbial species play an active role in the development of calcium carbonate (CaCO ₃ ) deposits (speleothems) in cave environments, we isolated 51 culturable bacteria from a coralloid speleothem and tested their ability to dissolve and precipitate CaCO ₃ . The majority of these isolates could precipitate CaCO ₃ minerals; scanning electron microscopy and X-ray diffractrometry demonstrated that aragonite, calcite and vaterite were produced in this process. Due to the inability of dead cells to precipitate these minerals, this suggested that calcification requires metabolic activity. Given growth of these species on calcium acetate, but the toxicity of Ca ²⁺ ions to bacteria, we created a loss-of-function gene knock-out in the Ca ²⁺ ion efflux protein ChaA. The loss of this protein inhibited growth on media containing calcium, suggesting that the need to remove Ca ²⁺ ions from the cell may drive calcification. With no carbonate in the media used in the calcification studies, we used stable isotope probing with C ¹³ O ₂ to determine whether atmospheric CO ₂ could be the source of these ions. The resultant crystals were significantly enriched in this heavy isotope, suggesting that extracellular CO ₂ does indeed contribute to the mineral structure. The physiological adaptation of removing toxic Ca ²⁺ ions by calcification, while useful in numerous environments, would be particularly beneficial to bacteria in Ca ²⁺ -rich cave environments. Such activity may also create the initial crystal nucleation sites that contribute to the formation of secondary CaCO ₃ deposits within caves.     

The effect of exogenous Ca2+ ions on pollen grain germination and pollen tube growth

Summary The involvement of exogenous calcium ions in the regulation of pollen tube formation has been investigated in Haemanthus albiflos L. and Oenothera biennis L. by following the changes that occur in pollen germination, tube growth, and ⁴⁵⁺Ca²⁺ uptake and distribution upon application of Verapamil (an inhibitor of calcium channels), lanthanum (a Ca²⁺ substitute), and ruthenium red (believed to raise the intracellular calcium level). It was found that exogenous Ca²⁺ takes part in the formation of the calcium gradient present in germinating pollen grains and growing pollen tubes. Ca²⁺ ions enter the cells through calcium channels. Raising or reducing ⁴⁵Ca²⁺ uptake causes disturbances in the germination of the pollen grains and in the growth of the pollen tubes.     

Reduced external calcium or sodium stimulates calcium influx in Pelvetia eggs

The effect of external calcium and sodium ion concentrations on the calcium fluxes on the Pelvetia fastigiata De Toni egg was measured. Decreasing external [Ca²⁺] greatly increased the permeability of the eggs to Ca²⁺; at 1 mM external Ca²⁺ this permeability was 60 times as great as it was at the normal [Ca²⁺] of 10 mM. Lowering the external [Na⁺] also increased Ca²⁺ influx; at 2 mM Na⁺, the Ca²⁺ influx was 2–3 times as great as it was at the normal [Na⁺] if choline was used as a Na⁺ substitute. Lithium was less effective as a Na⁺ substitute in increasing Ca²⁺ influx. The extra Ca²⁺ influx in low [Na⁺] seemed to be dependent on internal [Na⁺]. The Ca²⁺ efflux increased transiently and then declined in low Na⁺ media.     

Subscribed Content Calcium Carbonate Precipitation by Ureolytic Subsurface Bacteria

Coprecipitation in carbonate minerals offers a means of slowing the transport of divalent radionuclides and contaminant metals (e.g.,⁹⁰Sr²⁺, UO²⁺, Co²⁺) in the subsurface. It may be possible to accelerate this process by stimulating the native microbial community to generate chemical conditions favoring carbonate precipitation. In a preliminary evaluation of this approach, we investigated the ability of ureolytic subsurface bacteria to produce alkaline conditions conducive to calcium carbonate precipitation. Groundwater samples from the Eastern Snake River Plain (ESRP) aquifer in Idaho were screened for urea-hydrolyzing microorganisms; three isolates were selected for further evaluation. Analysis of 16S rRNA gene sequences indicated that two of the ESRP isolates were of the genus Pseudomonas , and the other was a Variovorax sp. The specific urease activities of the ESRP isolates appeared to be similar to each other but less than that of Bacillus pasteurii , a known urease-positive organism. However, calcium carbonate was rapidly precipitated in all cultures that were supplied with urea and calcium, and X-ray diffraction analyses indicated that calcite was always the predominant carbonate polymorph produced. The correspondence between measured calcium concentrations and equilibrium predictions suggested that the rate of calcite precipitation was directly linked to the rate of urea hydrolysis. These results are promising with respect to the potential utility of this approach for in situ remediation and indicate that further evaluation of this approach under conditions more closely simulating environmental conditions is warranted.     

Calcium mobilization and muscle contraction induced by acetylcholine in swine trachealis

The roles of Ca²⁺ mobilization in development of tension induced by acetylcholine (ACh, 0.1–100 µM) in swine tracheal smooth muscle strips were studied. Under control conditions, ACh induced a transient increase in free cytosolic calcium concentration ([Ca²⁺]_i) that declined to a steady-state level. The peak increase in [Ca²⁺]_i correlated with the magnitude of tension at each [ACh] after a single exposure to ACh, while the steady-state [Ca²⁺]_i did not. Removal of extracellular Ca²⁺ had little effect on peak [Ca²⁺]_i but greatly reduced steady-state increases in [Ca²⁺]_i and tension. Verapamil inhibited steady-state [Ca²⁺]_i only at [ACh]<1 µM. After depletion of internal Ca²⁺ stores by 10 min exposure to ACh in Ca²⁺-free solution and then washout of ACh for 5 min in Ca²⁺-free solution, simultaneous re-exposure to ACh in the presence of 2.5 mM Ca²⁺ increased [Ca²⁺]_i to the control steady-state level without overshoot. The tension attained was the same as control for each [ACh] used. Continuous exposure to successively increasing [ACh] (0.1–100 µM) also reduced the overshoot of [Ca²⁺]_i at 10 and 100 µM ACh, yet tension reached control levels at each [ACh] used. We conclude that the steady-state increase in [Ca²⁺]_i is necessary for tension maintenance and is dependent on Ca²⁺ influx through voltage-gated calcium channels at 0.1 µM ACh and through a verapamil-insensitive pathway at 10 and 100 µM. The initial transient increase in calcium arises from intracellular stores and is correlated with the magnitude of tension only in muscles that have completely recovered from previous exposure to agonists.     

Sodium/calcium selectivity of cloned calcium T-type channels

We studied the peculiarities of permeability with respect to the main extracellular cations, Na⁺ and Ca²⁺, of cloned low-threshold calcium channels (LTCCs) of three subtypes, Ca_v3.1 (α1G), Ca_v3.2 (α 1H), and Ca_v3.3 (α1I), functionally expressed in Xenopus oocytes. In a calcium-free solution containing 100 mM Na⁺ and 5 mM calcium-chelating EGTA buffer (to eliminate residual concentrations of Ca²⁺) we observed considerable integral currents possessing the kinetics of inactivation typical of LTCCs and characterized by reversion potentials of −10 ± 1, −12 ± 1, and −18 ± 2 mV, respectively, for Ca_v3.1, Ca_v3.2, and Ca_v3.3 channels. The presence of Ca²⁺ in the extracellular solution exerted an ambiguous effect on the examined currents. On the one hand, Ca²⁺ effectively blocked the current of monovalent cations through cloned LTCCs (K _d = 2, 10, and 18 μM for currents through channels Ca_v3.1, Ca_v3.2, and Ca_v3.3, respectively). On the other hand, at the concentration of 1 to 100 mM, Ca²⁺ itself functioned as a carrier of the inward current. Despite the fact that the calcium current reached the level of saturation in the presence of 5 mM Ca²⁺ in the external solution, extracellular Na⁺ influenced the permeability of these channels even in the presence of 10 mM Ca²⁺. The Ca_v3.3 channels were more permeable with respect to Na⁺ (P _Ca/P _Na ∼ 21) than Ca_v3.1 and Ca_v3.2 (P _Ca/P _Na ∼ 66). As a whole, our data indicate that cloned LTCCs form multi-ion Ca²⁺-selective pores, as these ions possess a high affinity for certain binding sites. Monovalent cations present together with Ca²⁺ in the external solution modulate the calcium permeability of these channels. Among the above-mentioned subtypes, Ca_v3.3 channels show the minimum selectivity with respect to Ca²⁺ and are most permeable for monovalent cations. Neirofiziologiya/Neurophysiology, Vol. 38, No. 3, pp. 183–192, May–June, 2006.     

Participation of Intracellular Ca2+ Stores in Ca2+ Signalling in Neurons of the Thalamic Laterodorsal Nucleus of Rats

Experiments were carried out on isolated neurons of the thalamic nucleus lateralis dorsalis (LD) from 12-day-old rats. According to the morphological characteristics, LD neurons were classified as relay thalamo-cortical units and interneurons. The concentration of free Ca²⁺ ions in the cytoplasm ([Ca²⁺] _i ) was measured by a fluorescent calcium indicator, fura-2AM. Application of 30 mM caffeine caused a transient change in the [Ca²⁺] _i in 8 of 15 and in 6 of 11 of the thalamo-cortical units and interneurons under study, respectively. After stimulation of a cell with application of 50 mM KCl, a caffeine-induced increase in the [Ca²⁺] _i was observed in all tested neurons. To study the contribution of Ca²⁺-induced Ca²⁺ release (CICR) to the calcium transient evoked by depolarization of the neuronal membrane, caffeine in a subthreshold concentration was pre-applied. After 50 mM KCl had been added to the medium following pre-application of 0.5 mM caffeine, the calcium transient amplitude in thalamo-cortical neurons increased by 51 ± 7% (n = 16). In interneurons this effect was not observed (n = 11). The data obtained allow us to hypothesize that CICR contributes to the depolarization-evoked calcium transient only in the relay (thalamo-cortical) neurons. Differences in the pattern of calcium signalling, which were detected in two types of neurons of the thalamic LD, can be a factor determining distinctions in the physiological characteristics of these neurons.     

Paenibacillus sp. Strain SB-6 Induces Weathering of Ca-montmorillonite: Illitization and Formation of Calcite

Investigation of the weathering of silicate minerals is helpful to understand the process of soil development, cycling of nutrient elements, and potential applications in fixation of carbon dioxide from the atmosphere through carbonate precipitation. In this study, weathering experiments of calcium-montmorillonite were conducted using Paenibacillus sp. strain SB-6 for 70 days. The results indicated that the Si⁴⁺, Al³⁺, Ca²⁺ and Na⁺ concentrations in the medium of the biotic experiments were evidently higher than those of the abiotic experiments, and that Paenibacillus sp. could help the transformation of partial montmorillonite into an illite–montmorillonite mixed-layer. In the process of illitization, K⁺ went into the interlayer of montmorillonite and hydrated Ca²⁺ and Na⁺ released from it. In the late stage of the experiments, the Ca²⁺ released from montmorillonite combined with carbonate ions generated by the bacterial metabolism, forming calcite.     

Research of the entry of rare earth elements Eu3+ and La3+ into plant cell

Whether rare earth elements can enter into plant cells remains controversial. This article discusses the ultracellular structural localization of lanthanum (La³⁺) and europium (Eu³⁺) in the intact plant cells fed by rare earth elements Eu³⁺ and La³⁺. Eu-TTA fluorescence analysis of the plasmalemma, cytoplast, and mitochondria showed that Eu³⁺ fluorescence intensities in such structures significantly increased. Eu³⁺ can directly enter or be carried by the artificial ion carrier A23187 into plant cells through the calcium ion (Ca²⁺) channel and then partially resume the synthesis of amaranthin in the Amaranthus caudatus growing in the dark. Locations of rare earth elements La³⁺ and Eu³⁺ in all kinds of components of cytoplasmatic organelles were determined with transmission electron microscope, scanning electron microscope, and energy-dispersive X-ray microanalysis. The results of energy-dispersive X-ray microanalysis indicated that Eu³⁺ and La³⁺ can be absorbed into plant cells and bind to the membranes of protoplasm, chloroplast, mitochondrion, cytoplast, and karyon. These results provide experimental evidence that rare earth elements can be absorbed into plant cells, which would be the basis for interpreting physiological and biochemical effects of rare earth elements on plant cells.     

Calcium channels and membrane disorders induced by drought stress in Vicia faba plants supplemented with calcium

Vicia faba plants were grown under drought conditions and variously supplemented with calcium. Drought stress markedly inhibited the growth of Vicia faba plants. Ca²⁺ ameliorated to a large extent this inhibition; fresh weight, dry mass, chlorophyll and water contents were variably improved. Membranes were, also, negatively affected by drought stress and percentage leakage was elevated. Concomitantly, the efflux of K⁺ and Ca²⁺ was enhanced by drought but lowered by supplemental Ca²⁺. In addition, membranes of droughted plants were sensitive to the Ca²⁺ channel blockers lanthanum, nifedipine or verapamil more than those of control plants. These blockers significantly increased the efflux of K⁺ and Ca²⁺ as well as percentage leakage particularly in those of droughted plants. The above results indicated that the functioning of the calcium channels was negatively affected when Vicia faba was grown under drought conditions. However, much of the drought-induced disorders including sensitivity towards the applied calcium channel blockers could be ameliorated by supplemental Ca²⁺.     

Bone tissue incorporates in vitro gallium with a local structure similar to gallium-doped brushite

During mineral growth in rat bone-marrow stromal cell cultures, gallium follows calcium pathways. The dominant phase of the cell culture mineral constitutes the poorly crystalline hydroxyapatite (HAP). This model system mimics bone mineralization in vivo. The structural characterization of the Ga environment was performed by X-ray absorption spectroscopy at the Ga K-edge. These data were compared with Ga-doped synthetic compounds (poorly crystalline hydroxyapatite, amorphous calcium phosphate and brushite) and with strontium-treated bone tissue, obtained from the same culture model. It was found that Sr²⁺ substitutes for Ca²⁺ in the HAP crystal lattice. In contrast, the replacement by Ga³⁺ yielded a much more disordered local environment of the probe atom in all investigated cell culture samples. The coordination of Ga ions in the cell culture minerals was similar to that of Ga³⁺, substituted for Ca²⁺, in the Ga-doped synthetic brushite (Ga-DCPD). The Ga atoms in the Ga-DCPD were coordinated by four oxygen atoms (1.90 Å) of the four phosphate groups and two oxygen atoms at 2.02 Å. Interestingly, the local environment of Ga in the cell culture minerals was not dependent on the onset of Ga treatment, the Ga concentration in the medium or the age of the mineral. Thus, it was concluded that Ga ions were incorporated into the precursor phase to the HAP mineral. Substitution for Ca²⁺ with Ga³⁺ distorted locally this brushite-like environment, which prevented the transformation of the initially deposited phase into the poorly crystalline HAP.Electronic Supplementary Material Supplementary material is available in the online version of this article at Abbreviations ACP amorphous calcium phosphate - DCPD dicalcium phosphate dihydrate (brushite) - HAP hydroxyapatite - ED-XRF energy dispersive X-ray fluorescence - EXAFS extended X-ray absorption fine structure - Ga-ACP gallium-doped amorphous calcium phosphate - Ga-DCPD gallium-doped brushite - Ga-HAP gallium-doped hydroxyapatite - XANES X-ray absorption near edge structure - XAS X-ray absorption spectroscopy - XRD X-ray diffraction     

Cell cycle-related fluctuations in transcellular ionic currents and plasma membrane Ca2+/Mg2+ ATPase activity during early cleavages of Lymnaea stagnalis embryos

Summary During the first four mitotic division cycles of Lymnaea stagnalis embryos, we have detected cell cycle-dependent changes in the pattern of transcellular ionic currents and membrane-bound Ca²⁺-stimulated ATPase activity. Ionic currents ranging from 0.05 to 2.50 A/cm² have been measured using the vibrating probe technique. Enzyme activity was detected using Ando's cytochemical method (Ando et al. 1981) which reveals Ca²⁺/Mg²⁺ ATPase localization at the ultrastructural level, and under high-stringency conditions with respect to calcium availability, it reveals Ca²⁺-stimulated ATPase. The ionic currents and Ca²⁺-stimulated ATPase localization have in common that important changes occur during the M-phase of the cell cycles. Minimal outward current at the vegetal pole coincides with metaphase/anaphase. Maximal inward current at the animal pole coincides with the onset of cytokinesis at that pole. Ca²⁺-stimulated ATPase is absent from one half of the embryo at metaphase/anaphase of the two- and four-cell stage, whereas it is present in all cells during the remaining part of the cell cycle. Since fluctuations of cytosolic free calcium concentrations appear to correlate with both karyokinesis and cytokinesis, we speculate that part of the cyclic pattern of Ca²⁺-stimulated ATPase localization and of the transcellular ionic currents reflects the elevation of cytosolic free calcium concentration during the M-phase. Offprint requests to: D. Zivkovic     

Evidences for Bioprecipitation of Pedogenic Calcite by Calcifying Bacteria from Three Different Soils of L'Aquila Basin (Abruzzi,Central Italy)

To provide further evidences on the role of bacterial soil species in the development of calcium carbonate deposits in soil, we isolated 36 heterotrophic bacterial strains from three soils of L'Aquila basin characterized by different CaCO₃ content and tested their ability to precipitate CaCO₃ when cultured on a Ca-rich medium. We found that the majority (63.89%) of these isolates could precipitate CaCO₃ minerals at 27°C. The aptitude to calcification (time and crystal amount) of each calcifying strains, morphology (SEM) and mineralogy of the formed bioliths were also investigated. X-ray diffraction confirmed the production of calcite. Crystal formation was not observed in the controls. Organic matter, total N and assimilable P, cation exchange capacity and exchangeable Ca²⁺, Mg²⁺, K⁺, Na⁺, pH, total and active calcium carbonate content, electric conductivity, skeleton, sand, silt and clay fractions of each soil sample were determined and related with its microbiological parameters. We found that the CaCO₃ content of soil was significatively related, in particular, to the percentage of calcifying bacterial strains (r = 0.95) and to the heterotrophic bacterial density (r = 0.98), which was found significatively related also with Ca²⁺ content of soil (r = ?0.97) and its CEC (r = ?0.97).