Asymmetric inhibition of spicule formation in sea urchin embryos with low concentrations of gadolinium ion

As gastrulation proceeds during sea urchin embryogenesis, primary mesenchyme cells (PMCs) fuse to form syncytial cables, within which calcium is deposited as CaCO₃, and a pair of spicules is formed. Earlier studies suggested that calcium, previously sequestered by primary mesenchyme cells, is secreted and incorporated into growing spicules. We examined the effects of gadolinium ion (Gd³⁺), a Ca²⁺ channel blocker, on spicule formation. Gd³⁺ did not lead to a retardation of embryogenesis prior to the initiation of gastrulation and did not inhibit the ingression of PMCs from the blastula wall or their migration along the inner blastocoel surface. However, when embryos were raised in seawater containing submicromolar to a few micromolar Gd³⁺, of which levels are considered to be insufficient to block Ca²⁺ channels, a pair of triradiate spicules was formed asymmetrically. At 1–3 μmol/L Gd³⁺, many embryos formed only one spicule on either the left or right side, or embryos formed a very small second spicule. Induction of the spicule abnormality required the presence of Gd³⁺ specifically during late blastula stage prior to spicule formation. An accumulation or adsorption of Gd³⁺ was not detected anywhere in the embryos by X‐ray microanalysis, which suggests that Ca²⁺ channels were not inhibited. These results suggest that Gd³⁺ exerts an inhibitory effect on spicule formation through a mechanism that does not involve inhibition of Ca²⁺ channels.     

A comparison of calcium binding inCallinectes sapidus premolt and postmolt cuticle homogenates: Implications for regulation of biomineralization

Cuticle tissue homogenates (CTHs) fromCallinectes sapidus premolt cuticle bound approximately 367% more Ca²⁺ ions than did those from the postmolt cuticle. ThepH-stat assay which was used to comparein vitro CaCO₃ nucleation times confirmed that the premolt CTHs had greater inhibitory activity than did the postmolt CTHs. This inhibitory activity was indicated by CaCO₃ nucleation times in excess of control values. Premolt nucleation times exceeded those of postmolt samples by approximately 340%. A positive correlation was observed between Ca²⁺ binding and calcification inhibitory activity for both premolt and postmolt CTHs. Heat pretreatment of CTHs at 70°C for a 24-hr period had no significant effect on their Ca²⁺ binding. However, this heat pretreatment decreased their calcification inhibitory activity. Pretreatment of CTHs with Ca²⁺ diminished their calcification inhibitory activity. These results are consistent with a mechanism for inhibition of biocalcification by these proteins which involves their initial reversible binding to nascent calcite nuclei growth steps and kinks, rather than theirin vivo interaction with free Ca²⁺ ions in solution.     

Isolation,culture, and differentiation of echinoid primary mesenchyme cells

Summary Methods are described for isolation and culture of primary mesenchyme cells from echinoid embryos. Ninety-five percentpure primary mesenchyme cells were isolated from early gastrulae ofStrongylocentrotus purpuratus, exploiting the biological segregation of these cells within the blastocoel. When cultured, more than 90% of the isolated cells reached the differentiated state, spicule formation, in synchrony with in vivo controls. Isolated primary mesenchyme cells were cultured with and without various cellular and acellular components of normal embryos in order to study the potential involvement of these components in the morphogenesis of the primary mesenchyme. Our data indicate that: 1. primary mesenchyme cells lack the ability to form the annular pattern of the primary mesenchymal ring autonomously; 2. they autonomously produce spicules of a characteristic morphology that differs from that of embryonic spicules; 3. morphogenesis of the primary mesenchyme is not affected by association with embryonic basal lamina, blastocoel matrix, or loosely aggregated epithelial cells, or by close confinement of each set of primary mesenchyme cells within the blastocoelar space; and 4. reaggregated, tightly associated epithelial cells can promote normal primary mesenchyme ring formation, and modify the primary mesenchyme-intrinsic spicule pattern to produce more normal spicule forms.     

不溶性基质中天冬氨酸丰富的蛋白在珊瑚的钙质骨片形成中的重要作用

一般认为, 酸性蛋白在控制矿物的形成和发展中发挥重要作用。因此, 在不溶性有机基质中鉴定酸性蛋白对于理解珊瑚中个体蛋白的功能是非常重要的一步。在短指多型软珊瑚(Sinularia polydactyla)的可溶性和不溶性基质层中分析蛋白组分表明, 在不溶性基质和可溶性基质层中天冬氨酸的含量分别是61%和29%。利用体外分析法发现, 基质蛋白诱导碳酸钙形成非晶态析出相先于其形成钙质的结晶态。利用X-射线衍射来鉴定骨片上结晶态的碳酸钙, 结果表明钙质的多晶态呈现强反射。傅利叶变换红外光谱分析表明珊瑚基质中富含天冬氨酸的蛋白和多醣的结构。在不溶性基质组分中用钙离子结合分析显示一个分子量为109 kD的蛋白质可以与形成骨片的钙离子结合, 这一过程对骨片形成非常重要。在对生物钙化过程中起重要作用的碳酸酐酶的分析中显示了此酶的新颖的活性。以上结果显示珊瑚中不溶性基质内的富含天冬氨酸的蛋白在生物矿化调控过程中起重要作用。     

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.     

Spiculogenesis in the sea urchin embryo: Studies on the SM30 spicule matrix protein

When proteins isolated from spicules of Strongylocentrotus purpuratus embryos were examined by western blot analysis, a major protein of approximately 43 kDa was observed to react with the monoclonal antibody, mAb 1223. Previous studies have established that this antibody recognizes an asparagine-linked, anionic carbohydrate epitope on the cell surface glycoprotein, msp130. This protein has been shown to be specifically associated with the primary mesenchyme cells involved in assembly of the spicule. Moreover, several lines of evidence have implicated the carbohydrate epitope in Ca²⁺ deposition into the growing spicule. The 43 kDa, spicule matrix protein detected with mAb 1223 also reacted with a polyclonal antibody to a known spicule matrix protein, SM30. Further characterization experiments, including deglycosylation using PNGaseF, two-dimensional electrophoresis, and immunoprecipitation, verified that the 43 kDa spicule matrix protein had a pl of approximately 4.0, contained the carbohydrate epitope recognized by monoclonal antibody mAb 1223 and reacted with anti-SM30. Electron microscopy confirmed the presence of proteins within the demineralized spicule that reacted with mAb 1223 and anti-SM30. We conclude that the spicule matrix protein, SM30, is a glycoprotein containing carbohydrate chains similar or identical to those on the primary mesenchyme cell membrane glycoprotein, msp130.     

Soluble proteins control growth of skeleton crystals in three coralline demosponges

Summary Calcified demosponges (coralline sponges, sclero-sponges), the first metazoa producing a carbonate skeleton, used to be important reef building organisms in the past. The relatives of this group investigated here,Spirastrella (Acanthochaetetes) wellsi, Astrosclera willeyana andVaceletia cf.crypta, are restricted to cryptic niches of modern Pacific coral reefs and may be considered as “living fossils’. They are characterized by a basic biologically controlled metazoan biomineralization process. Each of the investigated taxa forms its calcareous basal skeleton in a highly specialized way. Moreover, each taxon secretes distinct Ca²⁺-binding macromolecules which were entrapped within the calcium carbonate crystals during skeleton formation. Therefore these Ca²⁺-binding macromolecules were also described as intracrystalline macromolecules. When isolated and separated by SDS polyacrylamide gel electrophoresis, the organic skeleton matrix of the three species revealed to be composed of a respective distinct array of EDTA-soluble proteins. A single protein of 41 kDa was detected inS. wellsi, two proteins of 38 and 120 kDa inA. willeyana, and four proteins of 18 kDa, 30 kDa, 33 kDa, and 37 kDa inVaceletia sp. When run on IEF gel, the Ca²⁺-binding proteins gave staining bands at pH values between 5.25 and 5.65. As proved by anin vitro mineralization assay, the extracted proteins effectively inhibit CaCO₃ and SrCO₃ precipitation, respectively, in a saturated solution. Biochemical properties and behavior of the extracted proteins strongly suggest that they are involved in crystal nucleation and skeleton carbonate formation within the calcified sponges studied here.     

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.     

Modulation of Ca Activity in Cardiomyocytes through Caveolae-Gαq Interactions

Cardiomyocytes have a complex Ca²⁺ behavior and changes in this behavior may underlie certain disease states. Intracellular Ca²⁺ activity can be regulated by the phospholipase Cβ–Gα_q pathway localized on the plasma membrane. The plasma membranes of cardiomycoytes are rich in caveolae domains organized by caveolin proteins. Caveolae may indirectly affect cell signals by entrapping and localizing specific proteins. Recently, we found that caveolin may specifically interact with activated Gα_q, which could affect Ca²⁺ signals. Here, using fluorescence imaging and correlation techniques we show that Gα_q-Gβγ subunits localize to caveolae in adult ventricular canine cardiomyoctyes. Carbachol stimulation releases Gβγ subunits from caveolae with a concurrent stabilization of activated Gα_q by caveolin-3 (Cav3). These cells show oscillating Ca²⁺ waves that are not seen in neonatal cells that do not contain Cav3. Microinjection of a peptide that disrupts Cav3-Gα_q association, but not a control peptide, extinguishes the waves. Furthermore, these waves are unchanged with rynaodine treatment, but not seen with treatment of a phospholipase C inhibitor, implying that Cav3-Gα_q is responsible for this Ca²⁺ activity. Taken together, these studies show that caveolae play a direct and active role in regulating basal Ca²⁺ activity in cardiomyocytes.     

A comparison of calcium binding inCallinectes sapidus premolt and postmolt cuticle homogenates: Implications for regulation of biomineralization

Cuticle tissue homogenates (CTHs) fromCallinectes sapidus premolt cuticle bound approximately 367% more Ca²⁺ ions than did those from the postmolt cuticle. ThepH-stat assay which was used to comparein vitro CaCO₃ nucleation times confirmed that the premolt CTHs had greater inhibitory activity than did the postmolt CTHs. This inhibitory activity was indicated by CaCO₃ nucleation times in excess of control values. Premolt nucleation times exceeded those of postmolt samples by approximately 340%. A positive correlation was observed between Ca²⁺ binding and calcification inhibitory activity for both premolt and postmolt CTHs. Heat pretreatment of CTHs at 70°C for a 24-hr period had no significant effect on their Ca²⁺ binding. However, this heat pretreatment decreased their calcification inhibitory activity. Pretreatment of CTHs with Ca²⁺ diminished their calcification inhibitory activity. These results are consistent with a mechanism for inhibition of biocalcification by these proteins which involves their initial reversible binding to nascent calcite nuclei growth steps and kinks, rather than theirin vivo interaction with free Ca²⁺ ions in solution.     

Ca<Superscript>2+</Superscript> increases the specific coenzyme Q<Subscript>10</Subscript> content in <Emphasis Type="Italic">Agrobacterium tumefaciens</Emphasis>

Of various metal ions (Ca²⁺, Cr³⁺, Cu²⁺, Fe²⁺, Mg²⁺, Mn²⁺, Ni²⁺ and Zn²⁺) added to the culture medium of Agrobacterium tumefaciens at 1 mM, only Ca²⁺ increased Coenzyme Q10 (CoQ₁₀) content in cells without the inhibition of cell growth. In a pH-stat fed-batch culture, supplementation with 40 mM of CaCO₃ increased the specific CoQ₁₀ content and oxidative stress by 22.4 and 48%, respectively. Also, the effect of Ca²⁺ on the increase of CoQ₁₀ content was successfully verified in a pilot-scale (300 L) fermentor. In this study, the increased oxidative stress in A. tumefaciens culture by the supplementation of Ca²⁺ is hypothesized to stimulate the increase of specific CoQ₁₀ content in order to protect the membrane against lipid peroxidation. Our results improve the understanding of Ca²⁺ effect on CoQ₁₀ biosynthesis in A. tumefaciens and should contribute to better industrial production of CoQ₁₀ by biological processes.     

Photosynthesis,Respiration and Exopolymer Calcium-Binding in Biofilm Calcification (Westerhöfer and Deinschwanger Creek,Germany)

The impact of microbial activity on biofilm calcification in aquatic environments is still a matter of debate, especially in settings where ambient water has high CaCO₃ mineral supersaturation. In this study, biofilms of two CO₂-degassing karst-water creeks in Germany, which attain high calcite supersaturation during their course downstream, were investigated with regard to water chemistry of the biofilm microenvironment. The biofilms mainly consisted of filamentous cyanobacteria (Phormidium morphotype) and heterotrophic bacteria (including sulfate-reducing bacteria), which affect the microenvironment and produce acidic exopolymers. In situ and ex situ microelectrode measurements showed that a strong pH increase, coupled with Ca^{2 +} consumption, occurred in light conditions at the biofilm surface, while the opposite occurred in the dark. Calcite supersaturation at the biofilm surface, calculated from ex situ Ca^{2 +} and CO₃ ^2? microelectrode measurements, showed that photosynthesis resulted in high omega values during illumination, while respiration slightly lowered supersaturation values in the dark, compared to values in the water column. Dissociation calculation demonstrated that the potential amount of Ca^{2 +} binding by exopolymers would be insufficient to explain the Ca^{2 +} loss observed, although Ca^{2 +} complexation to exopolymers might be crucial for calcite nucleation. No spontaneous precipitation occurred on biofilm-free limestone substrates under the same condition, regardless of high supersaturation. These facts indicate that photosynthesis is a crucial mechanism to overcome the kinetic barrier for CaCO₃ precipitation, even in highly supersaturated settings.     

CaCO3 and SrCO3 bioprecipitation by fungi isolated from calcareous soil

The urease‐positive fungi Pestalotiopsis sp. and Myrothecium gramineum, isolated from calcareous soil, were examined for their properties of CaCO₃ and SrCO₃ biomineralization. After incubation in media amended with urea and CaCl₂ and/or SrCl₂, calcite (CaCO₃), strontianite (SrCO₃), vaterite in different forms [CaCO₃, (Ca_xSr_1?x)CO₃] and olekminskite [Sr(Sr,Ca)(CO₃)₂] were precipitated, and fungal ‘footprints’ were observed on mineral surfaces. The amorphous precipitate mediated by Pestalotiopsis sp. grown with urea and equivalent concentrations of CaCl₂ and SrCl₂ was identified as hydrated Ca and Sr carbonates by Fourier transform infrared spectroscopy. Liquid media experiments showed M. gramineum possessed the highest Sr²⁺ removal ability, and ～ 49% of supplied Sr²⁺ was removed from solution when grown in media amended with urea and 50 mM SrCl₂. Furthermore, this organism could also precipitate 56% of the available Ca²⁺ and 28% of the Sr²⁺ in the form of CaCO₃, SrCO₃ and (Ca_xSr_1?x)CO₃ when incubated in urea‐amended media and equivalent CaCl₂ and SrCl₂ concentrations. This is the first report of biomineralization of olekminskite and coprecipitation of Sr into vaterite mediated by fungi. These findings suggest that urease‐positive fungi could play an important role in the environmental fate, bioremediation or biorecovery of Sr or other metals and radionuclides that form insoluble carbonates.     

Influencing factors and formation mechanism of CaCO3 precipitation induced by microbial carbonic anhydrase

Microbial carbonic anhydrase promotes carbonate deposition, which is important in the formation and evolution of global carbon cycle and geological processes. A kind of bacteria producing extracellular carbonic anhydrase was selected to study the effects of temperature, pH value and Ca²⁺ concentration on bacterial growth, carbonic anhydrase activity and calcification rate in this paper. The results showed that the activity of carbonic anhydrase at 30 °C was the highest, which was beneficial to the calcification reaction, calcification rate of CaCO₃ was the fastest in alkaline environment with the initial pH value of 9.0. When the Ca2+ concentration was 60 mM, compared with other Ca²⁺ concentration, CA bacteria could grow and reproduce best, and the activity of bacteria was the highest, too low Ca²⁺ concentration would affect the generation of CaCO₃, while too high Ca²⁺ concentration would seriously affect the growth of bacteria and reduce the calcification rate. Finally, the mechanism of CaCO₃ precipitation induced by microbial carbonic anhydrase was studied. Carbonic anhydrase can accelerate the hydration of CO₂ into HCO₃⁻, and react with OH⁻ and Ca²⁺ to form CaCO₃ precipitation in alkaline environment and in the presence of calcium source.     

Ca2+ Release from Inositol 1,4,5-Trisphosphate-Sensitive Ca2+ Store by Antidepressant Drugs in Cultured Neurons of Rat Frontal Cortex

Abstract: The ability of antidepressant drugs (ADs) to increase the concentration of intracellular Ca²⁺ ([Ca²⁺]_i) was examined in primary cultured neurons from rat frontal cortices using the Ca²⁺-sensitive fluorescent indicator fura-2. Amitriptyline, imipramine, desipramine, and mianserin elicited transient increases in [Ca²⁺]_i in a concentration-dependent manner (100 μM to 1 mM). These four AD-induced [Ca²⁺]_i increases were not altered by the absence of external Ca²⁺ or by the presence of La³⁺ (30 μM), suggesting that these ADs provoked intracellular Ca²⁺ mobilization rather than Ca²⁺ influx. All four ADs increased inositol 1,4,5-trisphosphate (IP₃) contents by 20–60% in the cultured cells. The potency of the IP₃ production by these ADs closely correlated with the AD-induced [Ca²⁺]_i responses. Pretreatment with neomycin, an inhibitor of IP₃ generation, significantly inhibited amitriptyline- and imipramine-induced [Ca²⁺]_i increases. In addition, by initially perfusing with bradykinin (10 μM) or acetylcholine (10 μM), which can stimulate the IP₃ generation and mobilize the intracellular Ca²⁺, the amitriptyline responses were decreased by 76% and 69%, respectively. The amitriptyline-induced [Ca²⁺]_i increases were unaffected by treatment with pertussis toxin. We conclude that high concentrations of amitriptyline and three other ADs mobilize Ca²⁺ from IP₃-sensitive Ca²⁺ stores and that the responses are pertussis toxin-insensitive. However, it seems unlikely that the effects requiring high concentrations of ADs are related to the therapeutic action.     

Calcium transport and homeostasis in gill cells of a freshwater crab Dilocarcinus pagei

Crustaceans present a very interesting model system to study the process of calcification and calcium (Ca²⁺) transport because of molting-related events and the deposition of CaCO₃ in the new exoskeleton. Dilocarcinus pagei, a freshwater crab endemic to Brazil, was studied to understand Ca²⁺ transport in whole gill cells using a fluorescent probe. Cells were dissociated, all of the gill cell types were loaded with fluo-3 and intracellular Ca²⁺ change was monitored by adding Ca as CaCl₂ (0, 0.1, 0.25, 0.50, 1.0 and 5 mM), with a series of different inhibitors. For control gill cells, Ca²⁺ transport followed Michaelis–Menten kinetics with K _m = 0.42 ± 0.04 mM and V _max = 0.50 ± 0.02 μM (Ca²⁺ change × initial intracellular Ca⁻¹ × 180 s⁻¹; N = 14, r ² = 0.99). Verapamil (a Ca²⁺ channel inhibitor) and amiloride (a Na⁺/Ca²⁺ exchanger [NCX] inhibitor) completely reduced intracellular Ca²⁺ transport, while nifedipine, another Ca²⁺ channel inhibitor, did not. Vanadate, a plasma membrane Ca²⁺-ATPase inhibitor (PMCA), increased intracellular Ca²⁺ in gill cells through a decrease in the efflux of Ca²⁺. Ouabain increased intracellular Ca²⁺, similar to the effect of KB-R, a specific NCX inhibitor for Ca²⁺ in the influx mode. Alterations in extracellular [Na] in the saline did not affect intracellular Ca²⁺ transport. Caffeine, responsible for inducing Ca release from sarcoplasmic reticulum in vertebrate muscle, increased intracellular Ca²⁺ compared to control, suggesting an effect of this inhibitor in gill epithelial cells of Dilocarcinus pagei, probably through release of intracellular stores. We also demonstrate here that intracellular Ca²⁺ in gill cells of Dilocarcinus pagei was kept relatively constant in face of an extracellular Ca concentration of 50-fold, suggesting that crustaceans are able to display Ca²⁺ homeostasis through various Ca²⁺ intracellular sequestration mechanisms and/or plasma membrane Ca²⁺ influx and outflux that are highly regulatory. In summary, studies using whole gill cells are an interesting approach for working with real regulatory Ca²⁺ mechanisms in intact cells under physiological Ca levels (mM range), compared to earlier work using isolated vesicles of various epithelial cells.     

Synaptically Activated Ca<Superscript>2+</Superscript> Release From Internal Stores in CNS Neurons

Synaptically activated postsynaptic [Ca²⁺]_i increases occur through three main pathways: Ca²⁺ entry through voltage-gated Ca²⁺ channels, Ca²⁺ entry through ligand-gated channels, and Ca²⁺ release from internal stores. The first two pathways have been studied intensively; release from stores has been the subject of more recent investigations.Ca²⁺ release from stores in CNS neurons primarily occurs as a result of IP₃ mobilized by activation of metabotropic glutamatergic and/or cholingergic receptors coupled to PLC. Ca²⁺ release is localized near spines in Purkinje cells and occurs as a wave in the primary apical dendrites of pyramidal cells in the hippocampus and cortex. The amplitude of the [Ca²⁺]_i increase can reach several micromolar, significantly larger than the increase due to backpropagating spikes.The large amplitude, long duration, and unique location of the [Ca²⁺]_i increases due to Ca²⁺ release from stores suggests that these increases can affect specific downstream signaling mechanisms in neurons.     

A Prototypic Intracellular Calcium Antagonist, TMB-8, Protects Cultured Cerebellar Granule Cells Against the Delayed, Calcium-Dependent Component of Glutamate Neurotoxicity

Abstract: The effect(s) of a prototypic intracellular Ca²⁺ antagonist, 8-(N,N-diethylamino)octyl-3,4,5-trimethoxybenzoate (TMB-8), on glutamate-induced neurotoxicity was investigated in primary cultures of mouse cerebellar granule cells. Glutamate evoked an increase in cytosolic free-Ca²⁺ levels ([Ca²⁺]_i) that was dependent on the extracellular concentration of Ca²⁺ ([Ca²⁺]_o). In addition, this increase in [Ca²⁺]_i correlated with a decrease in cell viability that was also dependent on [Ca²⁺]_o. Glutamate-induced toxicity, quantified by 3-(4,5-dimethylthiazol-2-yl)-2,5-diphenyltetrazolium bromide (MTT) staining, was shown to comprise two distinct components, an “early” Na⁺/Cl^?-dependent component observed within minutes of glutamate exposure, and a “delayed” Ca²⁺-dependent component (ED₅₀～50 µM) that coincided with progressive degeneration of granule cells 4–24 h after a brief (5–15 min) exposure to 100 µM glutamate. Quantitative analysis of cell viability and morphological observations identify a “window” in which TMB-8 (at >100 µM) protects granule cells from the Ca²⁺-dependent, but not the Na⁺/Cl^?-dependent, component of glutamate-induced neurotoxic damage, and furthermore, where TMB-8 inhibits glutamate-evoked increases in [Ca²⁺]_i. These findings suggest that Ca²⁺ release from a TMB-8-sensitive intracellular store may be a necessary step in the onset of glutamate-induced excitotoxicity in granule cells. However, these conclusions are compromised by additional observations that show that TMB-8 (1) exhibits intrinsic toxicity and (2) is able to reverse its initial inhibitory action on glutamate-evoked increases in [Ca²⁺]_i and subsequently effect a pronounced time-dependent potentiation of glutamate responses. Dantrolene, another putative intracellular Ca²⁺ antagonist, was completely without effect in this system with regard to both glutamate-evoked increases in [Ca²⁺]_i and glutamate-induced neurotoxicity.     

The Signals for Starvation Response Are Transduced through Elevated [Ca]iinDictyosteliumCells

The mechanism by which cells recognize starvation to allow subsequent cellular development was analyzed usingDictyostelium discoideum,with special emphasis on Ca²⁺as a crucial signal transducer in intra- and intercellular communications. As was expected, the cytosolic Ca²⁺concentration ([Ca²⁺]_i) in aequorin-expressing cells (RHI76 derived fromD. discoideumAx-3) was temporarily increased, when 3–5 μM thapsigargin (Tg), a specific inhibitor of the Ca²⁺-ATPase, was added into the cells incubated in semistarvation medium (SS-medium: 1 vol of growth medium plus 7 vol either of 20 mM Na₂/K-phosphate buffer (pH 6.2) or of Bonner's salt solution (BSS)). Essentially the same result was obtained by the application of 5 μM nigericin (Ng), an acid ionophore to cells under the semistarved condition. Here it is of interest to note that in the SS-medium Tg and Ng are capable of enhancing cell differentiation as exemplified well by the earlier acquisition of chemotactic response to cAMP, possibly inducing the starvation response through the [Ca²⁺]_iincrease. From Western blot analysis of phosphotyrosine (pTyr)-containing proteins using anti-pTyr antibody, it was found that the pTyr-phosphorylation levels of 97-, 80-, and 45-kDa proteins increase specifically in response to starvation. Interestingly, Tg and Ng induced such a change of the 80-kDa protein in the cells incubated in the SS-medium. Taken together these results strongly suggest that the temporal increase of [Ca²⁺]_imay be a matter of importance for signal transduction coupled with starvation response.     

Characterization of the 1,25-dihydroxycholecalciferol-stimulated calcium influx pathway in CaCo-2 cells

The present studies were conducted to investigate the mechanisms underlying the 1,25-dihydroxycholecalciferol (1,25(OH)₂D₃)-induced increase in intracellular Ca²⁺ ([Ca²⁺] _i ) in individual CaCo-2 cells. In the presence of 2mm Ca²⁺, 1,25(OH)₂D₃-induced a rapid transient rise in [Ca²⁺] _i in Fura-2-loaded cells in a concentration-dependent manner, which decreased, but did not return to baseline levels. In Ca²⁺-free buffer, this hormone still induced a transient rise in [Ca²⁺] _i , although of lower magnitude, but [Ca²⁺] _i then subsequently fell to baseline. In addition, 1,25(OH)₂D₃ also rapidly induced⁴⁵Ca uptake by these cells, indicating that the sustained rise in [Ca²⁺] _i was due to Ca²⁺ entry. In Mn²⁺-containing solutions, 1,25(OH)₂D₃ increased the rate of Mn²⁺ influx which was temporally preceded by an increase in [Ca²⁺] _i . The sustained rise in [Ca²⁺] _i was inhibited in the presence of external La³⁺ (0.5mm). 1,25(OH)₂D₃ did not increase Ba²⁺ entry into the cells. Moreover, neither high external K⁺ (75mm), nor the addition of Bay K 8644 (1 μm), an L-type, voltage-dependent Ca²⁺ channel agonist, alone or in combination, were found to increase [Ca²⁺] _i , 1,25(OH)₂D₃ did, however, increase intracellular Na⁺ in the absence, but not in the presence of 2mm Ca²⁺, as assessed by the sodium-sensitive dye, sodium-binding benzofuran isophthalate. These data, therefore, indicate that CaCo-2 cells do not express L-type, voltage-dependent Ca²⁺ channels. 1,25(OH)₂D₃ does appear to activate a La³⁺-inhibitable, cation influx pathway in CaCo-2 cells.