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.     

A novel matrix protein participating in the nacre framework formation of pearl oyster,Pinctada fucata

Understanding the molecular composition is of great interest for both nacre formation mechanism and biomineralization in mollusk shell. A cDNA clone encoding an MSI31 relative, termed MSI7 because of its estimated molecular mass of 7.3 kDa, was isolated from the pearl oyster, Pinctada fucata. This novel protein shares similarity with MSI31, a prismatic framework protein of P. fucata. It is peculiar that MSI7 is much shorter in size, harboring only the Gly-rich sequence that has been proposed to be critical for Ca(2+) binding. In situ hybridization result showed that MSI7 mRNA was expressed specifically at the folds and outer epithelia of the mantle, indicating that MSI7 participates in the framework formation of both the nacreous layer and prismatic layer. In vitro experiment on the function of MSI7 suggested that it accelerates the nucleation and precipitation of CaCO(3). Taken together, we have identified a novel matrix protein of the pearl oyster, which may play an important role in determining the texture of nacre.     

Identification of genes directly involved in shell formation and their functions in pearl oyster, Pinctada fucata

Mollusk shell formation is a fascinating aspect of biomineralization research. Shell matrix proteins play crucial roles in the control of calcium carbonate crystallization during shell formation in the pearl oyster, Pinctada fucata. Characterization of biomineralization-related genes during larval development could enhance our understanding of shell formation. Genes involved in shell biomineralization were isolated by constructing three suppression subtractive hybridization (SSH) libraries that represented genes expressed at key points during larval shell formation. A total of 2,923 ESTs from these libraries were sequenced and gave 990 unigenes. Unigenes coding for secreted proteins and proteins with tandem-arranged repeat units were screened in the three SSH libraries. A set of sequences coding for genes involved in shell formation was obtained. RT-PCR and in situ hybridization assays were carried out on five genes to investigate their spatial expression in several tissues, especially the mantle tissue. They all showed a different expression pattern from known biomineralization-related genes. Inhibition of the five genes by RNA interference resulted in different defects of the nacreous layer, indicating that they all were involved in aragonite crystallization. Intriguingly, one gene (UD_Cluster94.seq.Singlet1) was restricted to the 'aragonitic line'. The current data has yielded for the first time, to our knowledge, a suite of biomineralization-related genes active during the developmental stages of P. fucata, five of which were responsible for nacreous layer formation. This provides a useful starting point for isolating new genes involved in shell formation. The effects of genes on the formation of the 'aragonitic line', and other areas of the nacreous layer, suggests a different control mechanism for aragonite crystallization initiation from that of mature aragonite growth.     

Characterization of Calcium Deposition and Shell Matrix Protein Secretion in Primary Mantle Tissue Culture from the Marine Pearl Oyster <Emphasis Type="Italic">Pinctada fucata</Emphasis>

In this study, we established and characterized a long-term primary mantle tissue culture from the marine pearl oyster Pinctada fucata for in vitro investigation of nacre biomineralization. In this culture system, the viability of mantle tissue cells lasted up to 2 months. The tissue cells were demonstrated to express nacre matrix proteins by RT-PCR, and a soluble shell matrix protein, nacrein, was detected in the culture medium by Western blot analysis. On the other hand, 15 days after initiating culture, a large amount of calcium deposits with major elements, including calcium, carbon, and oxygen, were generated in the mantle explants and cell outgrowth area. The quantity and size of calcium deposits increased with the prolonged cultivation, and their location and nanogranular structure suggested their biogenic origin. These calcium deposits specifically appeared in mantle tissue cultures, but not in heart tissue cultures. Taken together, these results demonstrate that the mantle tissue culture functions similarly to mantle cells in vivo. This study provides a reliable approach for the further investigation on nacre biomineralization at the cellular level.     

A novel matrix protein family participating in the prismatic layer framework formation of pearl oyster, Pinctada fucata

Understanding the molecular composition and the formation mechanism of shell matrix framework is of great interest for biomineralization in mollusk shell. The cDNAs encoding a novel matrix protein family (KRMP) were cloned from the mantle of pearl oyster, Pinctada fucata. Analysis of the deduced amino acid sequences revealed that KRMP have a high proportion of lysine, glycine, and tyrosine, and their predict isoelectric points are higher than any other identified shell matrix protein to our knowledge. The deduced amino acid sequences of KRMP can be divided into three regions, including an N-terminal signal peptide, a lysine-rich basic region interacting with acidic proteins or CO(3)(2-), and a Gly/Tyr-rich region involved in the protein cross-link via quinone-tanning process. RT-PCR and in situ hybridization demonstrated that KRMP mRNA was specifically expressed in the mantle edge, involved in the prismatic layer formation. Taken together, it seems that KRMP is a matrix protein family participating in the framework formation of prismatic layer.     

cDNA Microarray Analysis Revealing Candidate Biomineralization Genes of the Pearl Oyster, <Emphasis Type="Italic">Pinctada fucata martensii</Emphasis>

Biomineralization is a common biological phenomenon resulting in strong tissue, such as bone, tooth, and shell. Pinctada fucata martensii is an ideal animal for the study of biomineralization. Here, microarray technique was used to identify biomineralization gene in mantle edge (ME), mantle center (MC), and both ME and MC (ME-MC) for this pearl oyster. Results revealed that 804, 306, and 1127 contigs expressed at least three times higher in ME, MC, and ME-MC as those in other tissues. Blast against non-redundant database showed that 130 contigs (16.17 %), 53 contigs (17.32 %), and 248 contigs (22.01 %) hit reference genes (E?≤??10), among which 91 contigs, 48 contigs, and 168 contigs could be assigned to 32, 26, and 63 biomineralization genes in tissue of ME, MC, and ME-MC at a threshold of 3 times upregulated expression level. The ratios of biomineralization contigs to homologous contigs were similar at 3 times, 10 times, and 100 times of upregulated expression level in either ME, MC, or ME-MC. Moreover, the ratio of biomineralization contigs was highest in MC. Although mRNA distribution characters were similar to those in other studies for eight biomineralization genes of PFMG3, Pif, nacrein, MSI7, mantle gene 6, Pfty1, prismin, and the shematrin, most biomineralization genes presented different expression profiles from existing reports. These results provided massive fundamental information for further study of biomineralization gene function, and it may be helpful for revealing gene nets of biomineralization and the molecular mechanisms underlining formation of shell and pearl for the oyster.     

Cloning and characterization of an mRNA encoding a novel G protein alpha-subunit abundant in mantle and gill of pearl oyster Pinctada fucata

Nacre formation is an ideal model to study biomineralization processes. Although much has been done about biomineralization mechanism of nacre, little is known as to how cellular signaling regulates this process. We are interested in whether G protein signaling plays a role in mineralization. Degenerate primers against conserved amino acid regions of G proteins were employed to amplify cDNA from the pearl oyster Pinctada fucata. As a result, the cDNA encoding a novel G(s)alpha (pfG(s)alpha) from the pearl oyster was isolated. The G(s)alpha cDNA encodes a polypeptide of 377 amino acid residues, which shares high similarity to the octopus (Octopus vulgaris) G(s)alpha. The well-conserved A, C, G (switch I), switch II functional domains and the carboxyl terminus that is a critical site for interaction with receptors are completely identical to those from other mollusks. However, pfG(s)alpha has a unique amino acid sequence, which encodes switch III and interaction sites of adenylyl cyclase respectively. In situ hybridization and Northern blotting analysis revealed that the oyster G(s)alpha mRNA is widely expressed in a variety of tissues, with highest levels in the outer fold of mantle and epithelia of gill, the regions essential for biomineralization. We also show that overexpression of the pfG(s)alpha in mammalian MC3T3-E1 cells resulted in increased cAMP levels. Mutant pfG(s)alpha that has impaired CTX substrate diminished its ability to induce cAMP production. Furthermore, the alkaline phosphatase (ALP) activity, an indicator for mineralization, is induced by the G(s)alpha in MC3T3-E1 cells. These results indicated that G(s)alpha may be involved in regulation of physiological function, particularly in biological biomineralization.     

Identification of genes associated with shell color in the black-lipped pearl oyster,Pinctada margaritifera

Background

Color polymorphism in the nacre of pteriomorphian bivalves is of great interest for the pearl culture industry. The nacreous layer of the Polynesian black-lipped pearl oyster Pinctada margaritifera exhibits a large array of color variation among individuals including reflections of blue, green, yellow and pink in all possible gradients. Although the heritability of nacre color variation patterns has been demonstrated by experimental crossing, little is known about the genes involved in these patterns. In this study, we identify a set of genes differentially expressed among extreme color phenotypes of P. margaritifera using a suppressive and subtractive hybridization (SSH) method comparing black phenotypes with full and half albino individuals.

Results

Out of the 358 and 346 expressed sequence tags (ESTs) obtained by conducting two SSH libraries respectively, the expression patterns of 37 genes were tested with a real-time quantitative PCR (RT-qPCR) approach by pooling five individuals of each phenotype. The expression of 11 genes was subsequently estimated for each individual in order to detect inter-individual variation. Our results suggest that the color of the nacre is partially under the influence of genes involved in the biomineralization of the calcitic layer. A few genes involved in the formation of the aragonite tablets of the nacre layer and in the biosynthesis chain of melanin also showed differential expression patterns. Finally, high variability in gene expression levels were observed within the black phenotypes.

Conclusions

Our results revealed that three main genetic processes were involved in color polymorphisms: the biomineralization of the nacreous and calcitic layers and the synthesis of pigments such as melanin, suggesting that color polymorphism takes place at different levels in the shell structure. The high variability of gene expression found within black phenotypes suggests that the present work should serve as a basis for future studies exploring more thoroughly the expression patterns of candidate genes within black phenotypes with different dominant iridescent colors.

Electronic supplementary material

The online version of this article (doi:10.1186/s12864-015-1776-x) contains supplementary material, which is available to authorized users.     

Expression of genes responsible for biomineralization of Pinctada fucata during development

This study compares the expression levels of nacrein, N16, MSI60, Prismalin-14, aspein and MSI31 genes during the ontogeny of Pinctada fucata. Several novel findings were obtained: 1) The early calcitic prismatic layer was distinguished as a thin membrane-like structure. 2) Initial formation of the nacreous layer started from the mantle pallial region at the age of 31 days. 3) 18S rRNA of P. fucata was determined to be more suitable as a real-time PCR reference gene compared with GAPDH and β-actin genes. 4) A relationship was recognized between the expression levels of the above six organic matrix genes and biomineralization of the larval shell. The lack of calcite in the shells of the veliger and pediveliger stages, when MSI31 and Prismalin-14 genes were expressed, makes a role of polymorph control by these genes less likely. The hypothetical involvement of N16 and MSI60 proteins in aragonitic nacreous layer formation was corroborated by the expression levels of N16 and MSI60 genes during ontogeny. Our results are important with respect to the control of CaCO₃ crystal polymorphism and shell microstructures in P. fucata.     

Immunolocalization of matrix proteins in nacre lamellae and their in vivo effects on aragonitic tablet growth

How matrix proteins precisely control the growth of nacre lamellae is an open question in biomineralization research. Using the antibodies against matrix proteins for immunolabeling and in vivo experiments, we investigate the structural and functional roles of EDTA-soluble matrix (SM) and EDTA-insoluble matrix (ISM) proteins in nacre biomineralization of the pearl oyster Pinctada fucata. Immunolabeling reveals that a SM protein, nacrein, distributes within aragonitic tablets and intertabular matrix. An ISM protein, which we named P43, has been specifically recognized by polyclonal antibodies raised against the recombinant protein of P. fucata bone morphogenetic protein 2 in immunoblot analysis. Immunolabeling indicates that P43 is localized to interlamellar sheet, and also embedded within aragonitic tablets. Although nacrein and P43 both distribute within aragonitic tablets, they function differently in aragonitic tablet growth. When nacrein is suppressed by the antibodies against it in vivo, crystal overgrowth occurs, indicating that this SM protein is a negative regulator in aragonitic tablet growth. When P43 is suppressed in vivo, the organo-mineral assemblage is disrupted, suggesting that P43 is a framework matrix. Taken together, SM and ISM proteins are indispensable factors for the growth of nacre lamellae, controlling crystal growth and constructing the framework of aragonitic tablets.     

Purification and characterization of perlucin and perlustrin, two new proteins from the shell of the mollusc Haliotis laevigata

Two new proteins, named perlucin and perlustrin, with M(r) 17,000 and 13,000, respectively, were isolated from the shell of the mollusc Halotis laevigata (abalone) by ion-exchange chromatography and reversed-phase HPLC after demineralization of the shell in 10% acetic acid. The sequence of the first 32 amino acids of perlucin indicated that this protein belonged to a heterogeneous group of proteins consisting of a single C-type lectin domain. Perlucin increased the precipitation of CaCO(3) from a saturated solution, indicating that it may promote the nucleation and/or the growth of CaCO(3) crystals. With pancreatic stone protein (lithostathine) and the eggshell protein ovocleidin 17, this is the third C-type lectin domain protein isolated from CaCO(3) biominerals. This indicates that this type of protein performs an important but at present unrecognized function in biomineralization. Perlustrin was a minor component of the protein mixture and the sequence of the first 33 amino acids indicated a certain similarity to part of the much larger nacre protein lustrin A.     

Characterization and in vitro mineralization function of a soluble protein complex P60 from the nacre of Pinctada fucata

A soluble protein complex P60 from the powdered nacre of Pinctada fucata was extracted and partially characterized. The biological activity of the P60 on pre-osteoblast cell line MC3T3-E1 and bone marrow stroma cells (MSCs) was investigated. The P60 protein from the decalcified powered nacre was solubilized with acetic acid and then purified by liquid chromatography. The P60 protein was a protein complex composed of several subunits with disulfide bridges. The known protein nacrein, and its two derivatives, N28 and N35, were included in the P60 protein complex. The most abundant amino acids in the P60 that account for 68.3% of the total residues are glycine (32.1%), aspartic acid (17.4%), alanine (13.6%), and glutamic acid (5.2%). The in vitro study of the crystallization showed that this protein complex could control the formation and size of calcium carbonate. The assay of biological activity of the P60 protein complex on the pre-osteoblast cell line MC3T3-E1 and MSCs suggested that the P60 could stimulate the formation of mineralized nodules.     

Nautilin-63, a novel acidic glycoprotein from the shell nacre of Nautilus macromphalus

In molluscs, and more generally in metazoan organisms, the production of a calcified skeleton is a complex molecular process that is regulated by the secretion of an extracellular organic matrix. This matrix constitutes a cohesive and functional macromolecular assemblage, containing mainly proteins, glycoproteins and polysaccharides that, together, control the biomineral formation. These macromolecules interact with the extruded precursor mineral ions, mainly calcium and bicarbonate, to form complex organo-mineral composites of well-defined microstructures. For several reasons related to its remarkable mechanical properties and to its high value in jewelry, nacre is by far the most studied molluscan shell microstructure and constitutes a key model in biomineralization research. To understand the molecular mechanism that controls the formation of the shell nacreous layer, we have investigated the biochemistry of Nautilin-63, one of the main nacre matrix proteins of the cephalopod Nautilus macromphalus. After purification of Nautilin-63 by preparative electrophoresis, we demonstrate that this soluble protein is glycine-aspartate-rich, that it is highly glycosylated, that its sugar moieties are acidic, and that it is able to bind chitin in vitro. Interestingly, Nautilin-63 strongly interacts with the morphology of CaCO(3) crystals precipitated in vitro but, unexpectedly, it exhibits an extremely weak ability to inhibit in vitro the precipitation of CaCO(3) . The partial resolution of its amino acid sequence by de novo sequencing of its tryptic peptides indicates that Nautilin-63 exhibits short collagenous-like domains. Owing to specific polyclonal antibodies raised against the purified protein, Nautilin-63 was immunolocalized mainly in the intertabular nacre matrix. In conclusion, Nautilin-63 exhibits 'hybrid' biochemical properties that are found both in the soluble and insoluble proteins, rendering it difficult to classify according to the standard view on nacre proteins. DATABASE: The protein sequences of N63 appear on the UniProt Knowledgebase under accession number P86702.     

Cloning and characterization of an mRNA encoding a novel G protein α-subunit abundant in mantle and gill of pearl oyster Pinctada fucata

Nacre formation is an ideal model to study biomineralization processes. Although much has been done about biomineralization mechanism of nacre, little is known as to how cellular signaling regulates this process. We are interested in whether G protein signaling plays a role in mineralization. Degenerate primers against conserved amino acid regions of G proteins were employed to amplify cDNA from the pearl oyster Pinctada fucata. As a result, the cDNA encoding a novel G_sα (pfG_sα) from the pearl oyster was isolated. The G_sα cDNA encodes a polypeptide of 377 amino acid residues, which shares high similarity to the octopus (Octopus vulgaris) G_sα. The well-conserved A, C, G (switch I), switch II functional domains and the carboxyl terminus that is a critical site for interaction with receptors are completely identical to those from other mollusks. However, pfG_sα has a unique amino acid sequence, which encodes switch III and interaction sites of adenylyl cyclase respectively. In situ hybridization and Northern blotting analysis revealed that the oyster G_sα mRNA is widely expressed in a variety of tissues, with highest levels in the outer fold of mantle and epithelia of gill, the regions essential for biomineralization. We also show that overexpression of the pfG_sα in mammalian MC3T3-E1 cells resulted in increased cAMP levels. Mutant pfG_sα that has impaired CTX substrate diminished its ability to induce cAMP production. Furthermore, the alkaline phosphatase (ALP) activity, an indicator for mineralization, is induced by the G_sα in MC3T3-E1 cells. These results indicated that G_sα may be involved in regulation of physiological function, particularly in biological biomineralization.     

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.