Role of matrix vesicles in biomineralization

Background

Matrix vesicles have been implicated in the mineralization of calcified cartilage, bone and dentin for more than 40 years. During this period, their exact role, if any in the nucleation of hydroxyapatite mineral, and its subsequent association with the collagen fibrils in the organic matrix has been debated and remains controversial.

Scope of Review

This review summarizes studies spanning the whole history of matrix vesicles, but emphasizes recent findings and several hypotheses which have been recently introduced to explain in greater detail how matrix vesicles function in biomineralization.

Major Conclusions

It is now generally accepted that matrix vesicles have some role(s) in mineralization; that they are the initial site of mineral formation; that MV bud from the plasma membrane of mineral forming cells, but that they take with them only a subset of the materials found in the parent membrane; that the three proteins, alkaline phosphatase, nucleotide pyrophosphatase phosphodiesterase and annexin V have important roles in the process and that matrix vesicles participate in regulating the concentration of PPi in the matrix. In contrast, many open questions remain to be answered.

General Significance

Understanding the role of matrix vesicles in biomineralization will increase our knowledge of this important process.     

MMS6 protein regulates crystal morphology during nano-sized magnetite biomineralization in vivo

Biomineralization, the process by which minerals are deposited by organisms, has attracted considerable attention because this mechanism has shown great potential to inspire bottom-up material syntheses. To understand the mechanism for morphological regulation that occurs during biomineralization, many regulatory proteins have been isolated from various biominerals. However, the molecular mechanisms that regulate the morphology of biominerals remain unclear because there is a lack of in vivo evidence. Magnetotactic bacteria synthesize intracellular magnetosomes that comprise membrane-enveloped single crystalline magnetite (Fe(3)O(4)). These nano-sized magnetite crystals (<100 nm) are bacterial species dependent in shape and size. Mms6 is a protein that is tightly associated with magnetite crystals. Based on in vitro experiments, this protein was first implicated in morphological regulation during nano-sized magnetite biomineralization. In this study, we analyzed the mms6 gene deletion mutant (Δmms6) of Magnetospirillum magneticum (M. magneticum) AMB-1. Surprisingly, the Δmms6 strain was found to synthesize the smaller magnetite crystals with uncommon crystal faces, while the wild-type and complementation strains synthesized highly ordered cubo-octahedral crystals. Furthermore, deletion of mms6 gene led to drastic changes in the profiles of the proteins tightly bound to magnetite crystals. It was found that Mms6 plays a role in the in vivo regulation of the crystal structure to impart the cubo-octahedral morphology to the crystals during biomineralization in magnetotactic bacteria. Magnetotactic bacteria synthesize magnetite crystals under ambient conditions via a highly controlled morphological regulation system that uses biological molecules.     

Amorphous calcium carbonate biomineralization in the earthworm's calciferous gland: pathways to the formation of crystalline phases

In this study, we investigated the microstructural transformations that take place during carbonate formation in the earthworm’s calciferous gland by analysing the evolution from the precursor fluid of the solid phases (spherulites) to the final carbonate concretions released by the gland. Results from HREM and electron diffraction showed that the spherulithic deposits merely consisted of ACC partially transformed to vaterite. Furthermore, comparisons of the diffraction spectra and microstructural analyses allowed the identification of the transition sequences to more stable carbonates. And thus, transformations of ACC to calcite were observed on the surfaces of these amorphous globular aggregates as their smooth characteristic surface became rougher with time. This transition path was not unique, and the presence of aragonite, as an intermediate phase, has also been found. In this particular case, the transition process followed a completely different pathway with the crystallization starting in the centre of the sphere and progressively extending to the periphery, leading to the formation of radial aggregates. In situ experiments performed on the freshly extracted precursor fluid and analysed by FT-IR spectroscopy showed that ACC is the main constituent and is probably stabilised by macromolecules such as proteins and sugars. Furthermore, the Debye–Scherrer diffraction experiments showed that the carbonate phase present in this fluid remains stable as ACC for more than a week. All these features are indicative of this entire process being biologically controlled by the earthworms. The analysis of the amorphous structure factor of this ACC indicates that these transformations are preceded by short-range order modifications of the amorphous precursor phase.     

Comparison of the long-wave chlorophyll fluorescence in various green and blue-green algae and diatoms

Two types of long-wave fluorescence bands with similar band shape occur at room temperature in various algae: F_II700 and F_I715. F_II700 occurs in a limited number of algae, follows PS II transients, increases with culture age and is moderately increased by cooling to 83 K. F_I715 occurs in most algae, especially Anabaena, but much less in most diatoms and Tribonema. It does not follow PS II transients, does not increase with culture age and is much increased by cooling to 83 K.An interpretation for the characteristics of F_II700 and F_I715 is given.     

Visualization of putative ion-transporting epithelia in Amphibalanus amphitrite using correlative microscopy: Potential function in osmoregulation and biomineralization

Thoracican barnacles are a unique suborder of crustaceans typified by their calcified exterior, which provides protection to the sessile juvenile and adult. Biomineralization is mediated by a mantle epithelium that appears to be involved in calcium uptake and the secretion of calcium laden matrix. Larval and adult intertidal Balanomorph barnacles tolerate a wide range of salinities and it is hypothesized that active ion transport is the primary mechanism for osmoregulation. We observed adult Amphibalanus amphitrite producing an electrolyte-rich secretion emanating from the junction of the basis and parietal plates. Further study of this region using silver staining microscopic techniques, verified by scanning electron microscopy-energy dispersive spectroscopy, revealed a chloride ion rich mantle epithelium. A distinctive pattern of silver chloride stained epithelia was revealed in all A. amphitrite life stages. These epithelia were observed to contain mitochondria rich cells in nauplius and cyprid larvae (as shown by DASPMI staining visualized with confocal laser scanning microscopy) and therefore exhibit potential for active ion transport. Rhod-5 N (a low affinity cellular Ca²⁺ indicator) labeling was also observed in all barnacle life stages, in tissues shown to be chloride positive. We suspect that the observed chloride ion rich epithelia facilitate ionic regulation via active transport, and biomineralization via cellular Ca²⁺ uptake, storage and mobilization.     

Carbonic anhydrase activity and biomineralization process in embryos, larvae and adult blue mussels Mytilus edulis L.

To decide whether a physiological role can be attributed to enzymatic activity with respect to crystal formation and biomineralization of the first larval shell, carbonic anhydrase (CA) activity was measured in embryos and larvae of the blue mussels Mytilus edulis L. Also, CA activity was determined in the mantle edge and gonads of adult mussels with different shell length and condition index. The intention was to find a possible correlation between CA activity and adult shell calcification, i.e. gonadal maturation. The comparison of CA activity in different developmental stages of mussels and the results of an X-ray diffraction study of biomineralization processes in embryonic and larval shells indicate that CA activity is maximal at the end of several developmental stages. Consequently, the increase in CA activity precedes some physiological changes, i.e. the somatoblast 2d formation and the occurrence of the first calcite and quartz crystals in embryos, shell field formation in the gastrula stage, shell gland and periostracum production in trochophores, and rapid aragonite deposition in larval prodissoconch I and prodissoconch II shells. Furthermore, it was found that in adult mussels CA activity was quite variable and that in the mantle edge it was frequently inversely related to the activity in the gonad. Received: 28 November 1998 / Received in revised form: 30 August 1999 / Accepted: 31 August 1999     

Sites of accumulation and composition of hydrocarbons in Botryococcus braunii

Raman spectrometry and electron microscopy show that, in the hydrocarbon-rich alga Botryococcus braunii, hydrocarbons accumulate in two distinct sites; internally in cytoplasmic inclusions and externally in successive outer walls and derived globules. No other classes of lipid are present in noticeable amounts in the cytoplasmic inclusions and in the external globules. The same hydrocarbons are observed in the internal and external pools but with different relative abundances, the shorter hydrocarbons being more abundant in the internal pool. The bulk of B. braunii hydrocarbons (ca 95%) is located in the external pool. Such an extracellular location allows this species to exhibit both an unusually high hydrocarbon content (15% of dry wt) and a normal level (0.75%) within the cells. The hydrocarbon pattern and location of B. braunii were compared with that of other organisms; a close relation appears between higher plant epidermal cells and this green alga. The trilaminar outer walls of B. braunii, at whose contact external hydrocarbon globules accumulate, contain a sporopollenin-like compound.     

Studies on the Localization and Spectral Characteristics of the Fluorescence Emission of Differently Pigmented Wheat Leaves

Intensity, spectral characteristics and localization of the UV-laser (337 nm) induced blue-green and red fluorescence emission of green, etiolated and white primary leaves of wheat seedlings were studied in a combined fluorospectral and fluoromicroscopic investigation. The blue-green fluorescence of the green leaf was characterized by a maximum near 450 nm (blue region) and a shoulder near 530 nm (green region), whereas the red chlorophyll fluorescence exhibited maxima in the near-red (F690) and far-red (F735). The etiolated leaf with some carotenoids and traces of chlorophyll a, in turn, showed a higher intensity of the blue-green fluorescence with a shoulder in the green region and a strong red fluorescence peak near 684 to 690 nm, the far-red chlorophyll fluorescence maximum (F735) was, however, absent. The norfluorazone-treated white leaf, free of chlorophylls and carotenoids, only exhibited blue-green fluorescence of a very high intensity. In green and etiolated leaves the blue-green fluorescence primarily derived from the cell walls of the epidermis and the red fluorescence from the chlorophyll a of the mesophyll cells. In white leaves the blue-green fluorescence emanated from all cell walls of epidermis, mesophyll and leaf vein bundles. The shape and intensity of the blue-green and red fluorescence emission is determined by the reabsorption properties of chlorophylls and carotenoids in the mesophyll, thus giving rise to quite different values of the various fluorescence ratios F450/F690, F450/F530, F450/F735 and F690/F735 in green and etiolated leaves.     

Uptake of magnesium,strontium, barium,and manganese byPlectonema boryanum (Cyanophyceae) with special reference to polyphosphate bodies

Summary The ability of a cyanobacterium to take up and concentrate metals in polyphosphate bodies was tested. It was found that Mg, Ba and Mn are taken up by 3 and 4 week old cultures ofP. boryanum and in all cases the metals were concentrated in the polyphosphate bodies. In the case of Mn it was also detected in the cytoplasm. Strontium was sometimes taken up and incorporated into dense bodies which contained Sr, high S, high K and low Ca. In a number of trials no uptake of Sr could be detected. Polyphosphate bodies, formed as a result of the overplus phenomenon did not incorporate the metal at the time they are being formed. Polyphosphate bodies from 2 and 3 week culture contain P, K, Ca and Mg while bodies from 4 week cultures also possess Zn.It is suggested that sequestering metals in polyphosphate bodies may be a significant mechanism by which heavy metals are concentrated.     

1H, 13C, and 15N resonance assignments of murine amelogenin, an enamel biomineralization protein

Amelogenin is the predominant matrix protein in developing dental enamel. Making extensive use of residue-specific ¹⁵N-labeled amino acids samples, the majority of the main and side chain resonances for murine amelogenin were assigned in 2% aqueous acetic acid at pH 3.0.     

Enzymically accelerated biomineralization of heavy metals: Application to the removal of americium and plutonium from aqueous flows

Abstract: A biological process for the removal of heavy metals from the aqueous flows is described. Metals are precipitated on the surface of immobilized cells of a Citrobacter sp. as cell-bound metal phosphates. This uses phosphate liberated by the activity of a cell-bound phosphatase. Some radionuclides (e.g. 241americium) form metal phosphates readily; efficient removal of ²⁴¹Am on a continuous basis is demonstrated. At low phosphatase activities, the efficiency of uranium removal correlates with enzyme activity. High phosphatase activities are not realised as an increase in metal removal, suggesting that chemical events become rate-limiting. Studies have suggested that maximal metal uptake occurs only after nucleation and the formation of precipitation foci. A model is presented to illustrate how nucleation and crystallization processes could enhance the removal of plutonium and neptunium from dilute solutions.     

白腐菌选择性降解竹基质中木质纤维素的研究

对竹基质白腐菌选择性降解进行了初步研究。结果表明,菌株B1对竹基质中木质素和半纤维素有明显的降解选择性。降解55 d木质素和半纤维素降解率分别达44.4%和47.1%;降解20 d降解选择性最好,木质素和半纤维素降解率选择系数分别是2.08和1.98。从FTIR图谱中木质纤维素相关谱峰(2 924、1 6351、6011、5101、165、1 045、666/cm等)的明显变化也可以得出相同结论。     

Influx of calcium, strontium, and barium in presynaptic nerve endings

Depolarization-induced (potassium-stimulated) influx of 45Ca, 85Sr, and 133Ba was measured in synaptosomes prepared from rat brain. There are two phases of divalent cation entry, "fast" and "slow;" each phase is mediated by channels with distinctive characteristics. The fast channels inactivate (within 1 s) and are blocked by low concentrations (less than 1 micro M) of La. The slow channels do not inactivate (within 10 s), and are blocked by high concentrations (greater than 50 micro M) of La. Divalent cation influx through both channels saturates with increasing concentrations of permeant divalent cation; in addition, each permeant divalent cation species competitively blocks the influx of other permeant species. These results are consistent with the presence of "binding sites" for divalent cations in the fast and slow channels. The Ca:Sr:Ba permeability ratio, determined by measuring the influx of all three species in triple-label experiments, was 6:3:2 for the fast channel and 6:3:1 for the slow channel. A simple model for ion selectivity, based on the presence of a binding site in the channel, could account well for slow and, to some extent, for fast, channel selectivity data.     

Temperature-dependent photoinhibition and recovery of photosynthesis in the green alga Chlamydomonas reinhardtii acclimated to 12 and 27°C

Photoinhibition of photosynthesis and subsequent recovery were studied in cultures of the unicellular green alga Chlamydomonas reinhardtii L. (wt strain 137 c mating type +) acclimated at high (27°C) and low (12°C) temperature, Photoinhibition was assayed by fluorescence kinetics (77K) and oxygen evolution measurements under growth temperature conditions Inhibition of 50% was obtained by exposing cultures acclimated at high temperature to a photosynthetic photon flux density (PPFD) of 1 600 μmol m⁻² S⁻¹ at. 27°C. and cultures acclimated at low temperature to a PPFD of 900 μmol m⁻² s⁻¹ at 12°C When the photoinhibitory conditions were shifted it was revealed that algae acclimated at low temperature had acquired an increased resistance to photoinhibition at both 12 and 27°C. Furthermore, acclimation at low temperature increased the capacity to recover from 50% photoinhibition at both 12 and 27°C Studies of photoinhibition in the presence of the protein synthesis inhibitor, chloramphenicol, revealed that in response to acclimation at low temperature during growth the algae became more dependent on protein synthesis to avoid photoinhibition. It is suggested that acclimation at low temperature rendered C. reinhardtii an increased resistance to photoinhibition by. increasing the rate of turnover of photodamaged proteins in photosystem II (PS II). However, we cannot exclude the possibility that the increased resistance to photoinhibition of C. reinhardtii acclimated at low temperature also involves modifications of the mechanism of photoinhibition.     

High-resolution radioisotopic measurements of calcium, strontium, and barium in heart.

A gamma-ray detector system used in conjunction with isolated vascularly perfused rabbit septa labeled with the Ca-like cations 85Sr and 133Ba has been developed to test the feasibility of constructing a considerably more efficient detector system capable of measuring the highly energetic (Emax congruent to 1.3 MeV) 47Ca radionuclide. In addition an experimental design has been developed to quantify, statistically, perturbations of total tissue Ca, Sr, or Ba should they occur. This project was undertaken because the severe attenuation by living tissue of the beta-emitting radionuclide 45Ca (Emax congruent to 250 keV) limits its usefulness as a Ca tracer during experiments in which total tissue Ca is being measured minute-by-minute by an external detector. Analyses of over 100 experiments conducted on 35Sr- and 133Ba-labeled rabbit septa indicate that a tissue-detector system can be developed having the capacity to resolve perturbations of as little as 2 mumol Ca/kg wet tissue at 1-min sampling times or 6 mumol Ca/kg wet tissue at 0.1-min sampling times.     

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.     

Selectivity and permeation of alkali metal ions in K+-channels

Ion conduction in K⁺-channels is usually described in terms of concerted movements of K⁺ progressing in a single file through a narrow pore. Permeation is driven by an incoming ion knocking on those ions already inside the protein. A fine-tuned balance between high-affinity binding and electrostatic repulsive forces between permeant ions is needed to achieve efficient conduction. While K⁺-channels are known to be highly selective for K⁺ over Na⁺, some K⁺ channels conduct Na⁺ in the absence of K⁺. Other ions are known to permeate K⁺-channels with a more moderate preference and unusual conduction features. We describe an extensive computational study on ion conduction in K⁺-channels rendering free energy profiles for the translocation of three different alkali ions and some of their mixtures. The free energy maps for Rb⁺ translocation show at atomic level why experimental Rb⁺ conductance is slightly lower than that of K⁺. In contrast to K⁺ or Rb⁺, external Na⁺ block K⁺ currents, and the sites where Na⁺ transport is hindered are characterized. Translocation of K⁺/Na⁺ mixtures is energetically unfavorable owing to the absence of equally spaced ion-binding sites for Na⁺, excluding Na⁺ from a channel already loaded with K⁺.