Characterization of MRNP34, a novel methionine-rich nacre protein from the pearl oysters

Nacre of the Pinctada pearl oyster shells is composed of 98% CaCO₃ and 2% organic matrix. The relationship between the organic matrix and the mechanism of nacre formation currently constitutes the main focus regarding the biomineralization process. In this study, we isolated a new nacre matrix protein in P. margaritifera and P. maxima, we called Pmarg- and Pmax-MRNP34 (methionine-rich nacre protein). MRNP34 is a secreted hydrophobic protein, which is remarkably rich in methionine, and which is specifically localised in mineralizing the epithelium cells of the mantle and in the nacre matrix. The structure of this protein is drastically different from those of the other nacre proteins already described. This unusual methionine-rich protein is a new member in the growing list of low complexity domain containing proteins that are associated with biocalcifications. These observations offer new insights to the molecular mechanisms of biomineralization.     

Culture of outer epithelial cells from mantle tissue to study shell matrix protein secretion for biomineralization

Mantle tissue plays an important role in shell biomineralization by secreting matrix proteins for shell formation. However, the mechanism by which it regulates matrix protein secretion is poorly understood, largely because of the lack of cellular tools for in vitro study and techniques to evaluate matrix protein secretion. We have isolated the outer epithelial cells of the mantle of the pearl oyster, Pinctada fucata, and evaluated cellular metabolism by measuring the secretion of the matrix protein, nacrein. A novel sensitive sandwich enzyme-linked immunosorbent assay (ELISA) was established to quantify nacrein. Mantle explant culture was demonstrated to provide dissociated tissue cells with high viability. Single dissociated cell types from explant culture were separated by density in a discontinuous Percoll gradient. The outer epithelial cells were isolated from other cell types by their higher density and identified by immunolabeling and ultrastructure analysis. ELISA assays revealed that the outer epithelial cells retained the ability to secrete nacrein in vitro. Moreover, increased nacrein secretion resulted from an increased Ca(2+) concentration in the culture media of the outer epithelial cells, in a concentration-dependent manner. These results confirm that outer epithelial cell culture and the ELISA method are useful tools for studying the regulatory mechanisms of shell biomineralization.     

Amorphous Calcium Carbonate Precipitation by Cellular Biomineralization in Mantle Cell Cultures of Pinctada fucata

The growth of molluscan shell crystals is generally thought to be initiated from the extrapallial fluid by matrix proteins, however, the cellular mechanisms of shell formation pathway remain unknown. Here, we first report amorphous calcium carbonate (ACC) precipitation by cellular biomineralization in primary mantle cell cultures of Pinctada fucata. Through real-time PCR and western blot analyses, we demonstrate that mantle cells retain the ability to synthesize and secrete ACCBP, Pif80 and nacrein in vitro. In addition, the cells also maintained high levels of alkaline phosphatase and carbonic anhydrase activity, enzymes responsible for shell formation. On the basis of polarized light microscopy and scanning electron microscopy, we observed intracellular crystals production by mantle cells in vitro. Fourier transform infrared spectroscopy and X-ray diffraction analyses revealed the crystals to be ACC, and de novo biomineralization was confirmed by following the incorporation of Sr into calcium carbonate. Our results demonstrate the ability of mantle cells to perform fundamental biomineralization processes via amorphous calcium carbonate, and these cells may be directly involved in pearl oyster shell formation.     

Zona Localization of Shell Matrix Proteins in Mantle of <Emphasis Type="Italic">Haliotis tuberculata</Emphasis> (Mollusca,Gastropoda)

Organic matrix from molluscan shells has the potential to regulate calcium carbonate deposition and crystallization. Control of crystal growth thus seems to depend on control of matrix protein secretion or activation processes in the mantle cells, about which little is known. Biomineralization is a highly orchestrated biological process. The aim of this work was to provide information about the source of shell matrix macromolecule production, within the external epithelium of the mantle. An in vivo approach was chosen to describe the histologic changes in the outer epithelium and in blood sinus distribution, associated with mantle cells implicated in shell matrix production. Our results characterized a topographic and time-dependent zonation of matrix proteins involved in shell biomineralization in the mantle of Haliotis.     

不同pH值对三角帆蚌珍珠质分泌的影响

运用多种组织化学方法和透射电镜技术,研究了５种ｐＨ水环境（ｐＨ５、６、７、８、９）对三角帆砷外套膜珍珠质分泌的影响机制,结果表明,在中性水环境中,贝体能积极地从外界水环境中吸收钙,并能旺盛地合成和分泌贝壳珍珠层及珍珠有机基质前体物质,持续的酸性水环境导致贝体的钙严重丢失,并引起珍珠质分泌细胞对有机基质前体物质的合成和分泌能力减弱,持续的碱性水环境虽能导致贝体对钙的积累,但珍珠质分泌细胞合成和分泌珍     

翡翠贻贝外套膜转录组及贝壳珍珠质层和肌棱柱层蛋白质组分析

贝类贝壳在生物材料学及仿生学研究中占据着重要地位。贝壳基质蛋白质是贝壳中的主要有机质成分,对贝壳的形成以及贝壳的力学性能至关重要。翡翠贻贝(Perna viridis)贝壳主要由肌棱柱层和珍珠质层两种微观结构组成,其结构层次较简单,是研究贝壳基质蛋白质及其与贝壳形成关系的极好材料。为深入研究翡翠贻贝贝壳基质蛋白质的分子组成以及分布特点,首先采用扫描电子显微镜,观察翡翠贻贝贝壳内表面珍珠质层和肌棱柱层的微观结构;采用刮取法获得贝壳内表面珍珠质层和肌棱柱层的粉末;对不同层次的贝壳粉末,利用酸溶法去除碳酸钙成分,所获得的有机质组分通过离心将其分为酸可溶性组分和酸不溶性组分。采用Illumina深度测序技术对翡翠贻贝外套膜组织进行大规模测序和序列组装,在此基础上,采用LC-MS/MS质谱技术结合外套膜转录组数据库搜索,对翡翠贻贝肌棱柱层和珍珠质层贝壳基质蛋白质开展组学分析。扫描电镜观察结果表明,翡翠贻贝贝壳有两种不同形貌结构的层次,其中珍珠质层为片状堆叠结构,而肌棱柱层为柱状结构。翡翠贻贝外套膜转录组测序共计获得 69 859 条Unigene。蛋白质组学鉴定结果表明,翡翠贻贝贝壳中总计鉴定到蛋白质54种,其中38种为肌棱柱层所特有蛋白质,3种珍珠质层特有蛋白质,另有13种在珍珠质层和肌棱柱层均被鉴定到。肌棱柱层特有蛋白质的分子多样性明显强于珍珠质层。上述研究为进一步探讨贝壳不同微观层次的形成机制,以及贝壳基质蛋白质对贝壳不同结构层次的调控作用机制奠定了基础。     

A Novel Matrix Protein p10 from the Nacre of Pearl Oyster (Pinctada fucata) and Its Effects on Both CaCO3 Crystal Formation and Mineralogenic Cells

A novel matrix protein, designated as p10 because of its apparent molecular mass of 10 kDa, was isolated from the nacreous layer of pearl oyster (Pinctada fucata) by reverse-phase high-performance liquid chromatography. In vitro crystallization experiments showed that p10 could accelerate the nucleation of calcium carbonate crystals and induce aragonite formation, suggesting that it might play a key role in nacre biomineralization. As nacre is known to contain osteogenic factors, two mineralogenic cell lines, MRC-5 fibroblasts and MC3T3-E1 preosteoblasts, were used to investigate the biological activity of p10. The results showed that p10 could increase alkaline phosphatase activity, an early marker of osteoblast differentiation, while the viability of MRC-5 and MC3T3-E1 remained unchanged after treatment of p10. Taken together, the findings led to identification of a novel matrix protein from the nacre of P. fucata that plays a role in both the mineral phase and in the differentiation of the cells involved in biomineralization.     

Patterns of Expression in the Matrix Proteins Responsible for Nucleation and Growth of Aragonite Crystals in Flat Pearls of Pinctada fucata

The initial growth of the nacreous layer is crucial for comprehending the formation of nacreous aragonite. A flat pearl method in the presence of the inner-shell film was conducted to evaluate the role of matrix proteins in the initial stages of nacre biomineralization in vivo. We examined the crystals deposited on a substrate and the expression patterns of the matrix proteins in the mantle facing the substrate. In this study, the aragonite crystals nucleated on the surface at 5 days in the inner-shell film system. In the film-free system, the calcite crystals nucleated at 5 days, a new organic film covered the calcite, and the aragonite nucleated at 10 days. This meant that the nacre lamellae appeared in the inner-shell film system 5 days earlier than that in the film-free system, timing that was consistent with the maximum level of matrix proteins during the first 20 days. In addition, matrix proteins (Nacrein, MSI60, N19, N16 and Pif80) had similar expression patterns in controlling the sequential morphologies of the nacre growth in the inner-film system, while these proteins in the film-free system also had similar patterns of expression. These results suggest that matrix proteins regulate aragonite nucleation and growth with the inner-shell film in vivo.     

In vitro explant culture of mantle epithelium of freshwater pearl mussel

The in vitro culture of nacre secreting pallial mantle explants of freshwater pearl producing mussel, Lamellidens marginalis (Lamarck) included depuration of pearl mussels with different physical and chemical agents to eradicate various commensals, removal of pallial mantle ribbon, aseptic preparation of explants from the ribbon and transfer of those explants into tissue culture petri dishes. Special synthetic tissue culture media enriched with additives viz., inactivated calf fetal serum and antibiotics were poured into plates with explants. The culture plates were incubated at 30 degrees C in a CO2 incubator at 5%, CO2. The cultures could be maintained for 42-45 days without any contamination. After 12 hr epithelial like cells began to migrate out and formed a complete cell sheet surrounding the explant within 12-15 days. The epithelial cells in the culture indicated functional viability as subsequently after 38-40 days of culture, typical aragonitic 'nacre' crystals of CaCO3 could be observed throughout the culture plates.     

Aragonite precipitation by "proto-polyps" in coral cell cultures

The mechanisms of coral calcification at the molecular, cellular and tissue levels are poorly understood. In this study, we examine calcium carbonate precipitation using novel coral tissue cultures that aggregate to form "proto-polyps". Our goal is to establish an experimental system in which calcification is facilitated at the cellular level, while simultaneously allowing in vitro manipulations of the calcifying fluid. This novel coral culturing technique enables us to study the mechanisms of biomineralization and their implications for geochemical proxies. Viable cell cultures of the hermatypic, zooxanthellate coral, Stylophora pistillata, have been maintained for 6 to 8 weeks. Using an enriched seawater medium with aragonite saturation state similar to open ocean surface waters (Ω(arag)~4), the primary cell cultures assemble into "proto-polyps" which form an extracellular organic matrix (ECM) and precipitate aragonite crystals. These extracellular aragonite crystals, about 10 μm in length, are formed on the external face of the proto-polyps and are identified by their distinctive elongated crystallography and X-ray diffraction pattern. The precipitation of aragonite is independent of photosynthesis by the zooxanthellae, and does not occur in control experiments lacking coral cells or when the coral cells are poisoned with sodium azide. Our results demonstrate that proto-polyps, aggregated from primary coral tissue culture, function (from a biomineralization perspective) similarly to whole corals. This approach provides a novel tool for investigating the biophysical mechanism of calcification in these organisms.     

培养条件对三角帆蚌外套膜离体上皮组织珍珠质分泌能力的影响（简报）

珍珠是由珍珠贝外套膜的上皮细胞受到外源刺激物刺激形成珍珠囊（pearl—sac）,并由珍珠囊产生的钙质分泌物．其分泌物逐渐包围刺激原．使之体积急剧增长而形成的,珍珠质（nacre）是由大于95％的碳酸钙晶体与约5％的角壳蛋白组成的生物矿化产物。因此珍珠贝的外套膜在珍珠形成中起着重要的作用。珍珠贝外套膜的体外培养已开展了一些初步的研究工作。     

Expression of biomineralisation genes in tissues and cultured cells of the abalone Haliotis tuberculata

Mollusc shell biomineralisation involves a variety of organic macromolecules (matrix proteins and enzymes) that control calcium carbonate (CaCO₃) deposition, growth of crystals, the selection of polymorph, and the microstructure of the shell. Since the mantle and the hemocytes play an important role in the control of shell formation, primary cell cultures have been developed to study the expression of three biomineralisation genes recently identified in the abalone Haliotis tuberculata: a matrix protein, Lustrin A, and two carbonic anhydrase enzymes. Mantle cells and hemocytes were successfully maintained in primary cultures and were evaluated for their viability and proliferation over time using a semi-automated assay (XTT). PCR and densitometric analysis were used to semi-quantify the gene expression and compare the level of expression in native tissues and cultured cells. The results demonstrated that the three genes of interest were being expressed in abalone tissues, with expression highest in the mantle and much lower in the hemocytes and the gills. Biomineralisation genes were also expressed significantly in mantle cells, confirming that primary cultures of target tissues are suitable models for in vitro investigation of matrix protein secretion.     

Pinctada fucata mantle gene 3 (PFMG3) promotes differentiation in mouse osteoblasts (MC3T3-E1)

Nacre is secreted from the mantle of pearl oysters. In vivo and in vitro experiments have demonstrated that water-soluble extracts of nacre stimulate osteoblast differentiation and matrix mineralization, but the component responsible for this activity is unclear. It was reported that Pinctada fucata mantle gene 3 (PFMG3) with an N-terminal signal peptide could be secreted into the nacre of P. fucata. Here we report that PFMG3 is specifically expressed at the outer fold of the mantle and could promote calcium carbonate crystal formation in vitro. Consistent with this observation, we found that matrix mineralization of MC3T3-E1 cells, a murine osteoblast cell line, is accelerated upon treatment with PFMG3. Intriguingly, we observed that alkaline phosphatase activity and cell viability are increased after treating MC3T3-E1 cell with PFMG3. mRNA levels of osteoblast-specific marker genes osteocalcin and osteopontin are also increased. We conclude that PFMG3 from the mantle of P. fucata promotes MC3T3-E1 osteoblast cell differentiation, matrix mineralization, and calcium carbonate deposition in vitro. Our findings provide new evidence that PFMG3 may be used as a potential therapeutic molecule for the treatment of osteoporosis.     

Identification and characterization of a biomineralization related gene PFMG1 highly expressed in the mantle of Pinctada fucata

To elucidate the mechanism of nacre biomineralization, the mantle of Pinctada fucata (P. fucata) from the South China Sea was used. Using the mantle cDNA library and the ESTs we have cloned through suppression subtractive hybridization (SSH), ten novel genes including PFMG1 were obtained through nested PCR. Bioinformative results showed that PFMG1 had a high homology (40%) with Onchocerca volvulus calcium-binding protein CBP-1 and had two EF-hand calcium-binding domains from the 81st to the 93rd amino acid and from the 98th to the 133rd amino acid in the deduced amino acid sequence. The results of multitissue RT-PCR and in situ hybridization demonstrated the high expression of PFMG1 in the mantle of P. fucata and confirmed the SSH method. The results of GST-PFMG1 on CaCO3 crystallization showed significant effects on nucleation and precipitation of CaCO3. PFMG1 was cloned into the pcDNA.3.1/myc-HisA vector and was subsequently transfected into MC3T3-E1 cells. RT-PCR revealed upregulation of the marker genes related to cell growth, differentiation, and mineralization, and BMP-2, osterix, and osteopontin were upregulated as a result. This research work suggests that PFMG1 plays an important role in the nacre biomineralization, and the SSH method can pave the way for the bulk cloning and characterization of new genes involved in biomineralization in P. fucata and may accelerate research on the mechanism of pearl formation.     

Calcium phosphate deposits in domes of human pancreatic adenocarcinoma (Capan-1) cell cultures

Human pancreatic cells of the Capan-1 line form domes in culture during the stationary growth stage. The domes are thought to be a result of the transport of water and electrolytes by the Capan-1 cells. In older Capan-1 cultures, the epithelial sheets formed thickenings from several layers of cells of which the outermost ones were joined by tight type junctions. In the intracellular space, deposits of insoluble calcium salts were observed. Culture of Capan-1 cells in the presence of fibroblasts prolonged survival of the cultures with intact domes for more than 80 days. The Capan-1 cells proliferated forming multilayers and closed cavities which we called super-domes. X-ray spectrometry and electron diffraction analysis showed that the abundant deposits inside these cavities consisted of calcium phosphate in an apatite structure. The number of these deposits increased with time in culture, and they appeared to be formed at the sites of contact with an extracellular matrix consisting of cell debris. Deposits were not observed within the culture medium. Cells from domes were stained cytochemically for ATPases and alkaline phosphatases and examined by light and electron microscopy. The Capan-1 cells surrounding the domes were differentiated, polarized cells containing placental type alkaline phosphatases on their apical membranes and Ca2(+)-ATPases on their basolateral membranes. These enzymes were thought to play a role in the accumulation of phosphate and Ca2+ ions in the dome cavities, which then formed crystals in the presence of organic compounds produced by lysis of cells of the deepest layers of the super-domes. The crystals of hydroxyapatite observed in standard Capan-1 cell cultures and those cocultured with fibroblasts were assumed to be a result of transepithelial transport of Ca2+ and phosphate ions by these cells.     

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.     

Cryopreservation of cultured mantle cells of Paphia malabarica for perennial availability

Laboratory friendly, cryopreservation procedures with respect to cryopreservation formulations and cryopreservation temperatures were attempted, in the present study to ensure perennial availability of cultured mantle cells of bivalve (Paphia malabarica). Screening of cryopreservative formulations with different concentrations of DMSO, Propylene glycol and Glycerol was carried out for cryopreservation of freshly dissociated cells of Paphia malabarica. Out of these cryopreservative formulations, 10% DMSO, 10% Propylene glycol and 15% Glycerol were selected for cryopreservation of the mantle cells pooled from 1-day old primary culture and cell line after 3 passages at the end of different cryopreservation periods. Cryopreservative formulation with 15% glycerol, served as a best cryoprotectant for the cryopreservation of cells sourced from freshly dissociated cells as well as from primary cultures and cell cultures after three passages of mantle cells of Paphia malabarica, retaining metabolic activity of resurrected cells. Both, cell cultures established from uncryopreserved cells as well as cryopreserved cells showed similar alkaline phosphatase and carbonic anhydrase activities thus indicating retention of their biomineralization capacity even after cryopreservation at low and ultralow temperatures.