Pinctada Fucata Mantle Research Articles

Purification, crystallization and X-ray analysis of Pf-SCP (sarcoplasmic Ca-binding protein), related to storage and transport of calcium in mantle of Pinctada fucata

Pf-SCP, a 21 kDa protein with two EF-hand motifs and a phosphorylation site, was identified from mantle tissue and binds to calcium ions and transports calcium components from cell to the shell of Pinctada fucata. To reveal the molecular basis of the calcium binding activity of Pf-SCP, we expressed the recombinant protein of full-length Pf-SCP in Escherichia coli. Recombinant Pf-SCP (rPf-SCP) purified by Ni affinity chromatography and size exclusion chromatography appeared as a single band on SDS-PAGE. The circular dichroism spectroscopy showed that the α-helix content decreased when rPf-SCP interacted with both calcium ions and calcium carbonate. Western blotting and immunostaining verified the Pf-SCP expression in the shell and localization most in the mantle epithelial cells. To further understand the structural and functional regulation of Pf-SCP by calcium ions and calcium carbonate, the crystallization experiments of rPf-SCP in the presence of calcium ions were performed. A crystal of rPf-SCP obtained in the presence of calcium ions diffracted X-rays up to a resolution of 1.8 Å. The space group of the crystal is C2 with unit cell parameters of a = 96.828 Å, b = 55.906 Å, c = 102.14 Å and β = 90.009°, indicating that three molecules of rPf-SCP are contained in an asymmetric unit as estimated at the value of the Matthews coefficient. These results suggest that Pf-SCP may play a role in calcium ions transportation and shell mineralization by concentrating calcium ions inside the mantle epithelial cells and interacting with calcium carbonate molecules.

Structural and functional analyses of calcium ion response factors in the mantle of Pinctada fucata.

The pearl oyster, Pinctada fucata, is cultured for pearl production in Japan. The shell of the pearl oyster consists of calcium carbonate and a small amount of organic matrix. Despite many studies of the shell matrix proteins, the mechanism by which calcium elements are transported from the mantle to the shell remains unclear. Investigating the molecular mechanism of calcium transportation, we prepared artificial seawater with a high concentration of calcium ions (10ASW) to induce calcification in the pearl oyster. When pearl oysters were cultured in 10ASW, unusual nanoparticles were precipitated on the surface of the nacreous layer. SDS-PAGE and 2D-PAGE analyses revealed that some calcium-sensing proteins (Sarcoplasmic Ca-binding Protein (Pf-SCP) and Pf-filamin A) might be related to the synthesis of these nanoparticles. The recombinant proteins of Pf-SCP can bind to calcium ions and accumulate nanoparticles of calcium carbonate crystals. However, transcriptomic analysis of the pearl oysters grown in 10ASW showed that the matrix protein genes in the shell did not differ before and after treatment with 10ASW. These results suggest that, despite increasing calcium transportation to the shell, treatment with a high concentration of calcium ions does not induce formation of the organic framework in the shell microstructure. These findings offer meaningful insights into the transportation of calcium elements from the mantle to the shell.

Characterization of pinctada fucata mantle gene 2 (pfmg2) in pearl oyster

ABSTRACTBiomineralization is a complicated process which involves multiple gene products in Pinctada fucata. Here, Pinctada fucata mantle gene 2 (pfmg2) was characterized in P. fucata. The putative PFMG2 protein has a Calponin Homology (CH) domain and an EF hand that can bind calcium. PFMG2 shares homology with transgelin in other species. Multi-tissue reverse transcriptase polymerase chain reaction (RT-PCR) indicates that pfmg2 mRNA is expressed ubiquitously, but its expression is high in the mantle tissue of P. fucata. Furthermore, in situ hybridization shows that pfmg2 localized at the edge of the mantle. Our results suggest that PFMG2 plays an important role in the shell mineralization process in pearl oyster. The analysis and the functional characterization of PFMG2 in P. fucata will provide new insight into the mineralization process.

Calcium carbonate mineralization mediated by in vitro cultured mantle cells from Pinctada fucata

Formation of the molluscan shell is believed to be an extracellular event mediated by matrix proteins. We report calcium carbonate mineralization mediated by Pinctada fucata mantle cells. Crystals only appeared when mantle cells were present in the crystallization solution. These crystals were piled up in highly ordered units and showed the typical characteristics of biomineralization products. A thin organic framework was observed after dissolving the crystals in EDTA. Some crystals had etched surfaces with a much smoother appearance than other parts. Mantle cells were observed to be attached to some of these smooth surfaces. These results suggest that mantle cells may be directly involved in the nucleation and remodeling process of calcium carbonate mineralization. Our result demonstrate the practicability of studying the mantle cell mechanism of biomineralization and contribute to the overall understanding of the shell formation process.

Pinctada fucata mantle gene 4 (PFMG4) from pearl oyster mantle enhances osteoblast differentiation.

The organic matrix of nacre has been reported for its effect on osteogenesis. It was found that PFMG4 (Pinctada fucata mantle gene 4) with an N-terminal signal peptide could be secreted into nacre of Pinctada fucata (P. fucata). Here, we report that PFMG4 is highly expressed in mantle tissue and has high homology with C1q protein in different species. In MC3T3-E1 osteoblast cells, we found that highly expressed PFMG4 could suppress cell proliferation and type I collagen expression, but it could increase alkaline phosphatase activity and mineralized deposition. These results show that PFMG4 has potential ability in enhancing osteoblast differentiation, suggesting a new idea in developing medicine for the therapy of osteoporosis.

A Pearl Protein Self-Assembles To Form Protein Complexes That Amplify Mineralization

The formation of the nacre pearl in marine invertebrates represents an on-demand production of mineralization in response to an irritant or parasite threat to the mantle organ. In the Japanese pearl oyster (Pinctada fucata), this process is mediated by a 12-member protein family known as PFMG (Pinctada fucata mantle gene). One of these proteins, PFGM1, has been implicated in modulating calcium carbonate crystal growth and has been reported to possess an EF-hand-like domain. In this report, we establish that the recombinant PFMG1 (rPFMG1) is an intrinsically disordered "imitator" EF-hand protein that increases the number of calcium carbonate mineral crystals that form relative to control scenarios and does not induce aragonite formation. This protein possesses a modified pseudo-EF-hand sequence at the C-terminal end which exhibits low homology (30-40%) to the pseudo-EF-hand mitochondrial SCaMCs buffering/solute transport proteins. This low sequence homology is the result of the inclusion of disorder-promoting amino acids and short amyloid-like aggregation-prone cross-β-strand sequences within the putative PFMG1 pseudo-EF-hand sequence region. Similar to other nacre proteins, rPFMG1 oligomerizes to form amorphous, heterogeneously sized protein oligomers and films in vitro, and this process is enhanced by Ca(2+), which promotes the formation of aggregation-prone extended β-strand structure within rPFMG1. From these results, we conclude that PFMG1 forms supramolecular assemblies that play an important role in amplifying the nucleation process that is crucial for coating or neutralizing invasive threats to the mantle organ.

Pinctada fucataMantle Gene 5 (PFMG5) from Pearl Oyster Mantle Inhibits Osteoblast Differentiation

PFMG5 (Pinctada fucata mantle gene 5) was identified from mantle tissue of the pearl oyster, Pinctada fucada (P. fucada). Here we report that PFMG5 decreased osteoblast differentiation marker alkaline phosphatase (ALP) activity and the transcript levels of osteoblast differentiation specific marker genes in MC3T3-E1 cells. PFMG5 was identified as a new molecule inhibiting osteoblast differentiation.

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.

Localization of calmodulin and calmodulin-like protein and their functions in biomineralization in P. fucata

Calmodulin (CaM) and calmodulin-like protein (CaLP) are two proteins involved in biomineralization. Their localizations in Pinctada fucata mantle epithelia were studied by Western blot (WB) analysis of the nuclear/cytosol fraction of primary cultured P. fucata mantle cells and immunogold electron microscopy. The results showed a completely different distribution of these two proteins at the subcellular level. CaM was distributed throughout both the nucleus and cytoplasm of the mantle epithelium but CaLP was distributed only in the cytoplasm. The functions of these two proteins in biomineralization were investigated by shell regeneration. During this process, the expressions of CaM and CaLP were greatly enhanced in different organelles of the mantle epithelium. Overexpression of these two proteins and a mutant of calmodulin-like protein (M-CaLP) that lacks an extra C-terminal tail in MC3T3-E1 promoted the mRNA expression of osteopontin, a biomineralization marker for osteoblasts. All of the results indicated that CaM and CaLP have completely different distributions in the mantle epithelium and affect the biomineralization process at different levels. The extra C-terminal tail of CaLP is important for its functions in biomineralization in P. fucata.

Investigation of cell proliferation and differentiation in the mantle of Pinctada fucata (Bivalve, Mollusca)

The mantle of the pearl oyster Pinctada fucata was adopted for the proliferation profile study in our work and a proliferation hot spot was found in the outer epithelia of mantle central zone using the BrdU immunohistochemistry method. This result contradicts the previous research that the mantle has numerous growth centers all over the mantle epithelium, with the same proliferation activity throughout the whole mantle outer epithelial cells. This is the first report on the different proliferation features on the whole mantle where Alcian Blue/PAS staining analysis and ultrastructural observation with the aid of transmission electron microscope (TEM) demonstrated distinct features of the epithelium in four different regions of the mantle. Results from the present investigation displayed that in the outer epithelium of the marginal zone in mantle outer fold, organelles such as mitochondria and endoplasmic reticulum (ER) were well-developed and double membrane bounded vesicles were present; in the outer epithelia of mantle central zone, stem-like cells with a high ratio of nucleus to cytoplasm and comparatively undeveloped organelles were detected. Together with the observations of the cell proliferation profile of different regions of the mantle, a hypothetic model for the proliferation and differentiation of the pearl oyster’s mantle is proposed: there exists a proliferation “hot spot” in the outer epithelial cells of central zone and the proliferation ability decreases progressively from this “hot spot” towards the marginal zone; the whole mantle’s differentiation occurs continuously with its growth and the direction is from the proliferation ‘hot spot’ (central zone) towards the marginal zone. Furthermore, another interesting result was found when the proliferation rate was investigated together with the tidal rhythm: the proliferation activity was found to be closely correlated with the tidal rhythm, indicating that the mantle outer epithelia’s proliferation rhythm might be the impetus of the shell’s daily growth bands.

Different effects of Pb 2+ and Cu 2+ on immune and antioxidant enzyme activities in the mantle of Pinctada fucata

The aim of this study was to investigate the natural role of the mantle in pearl oyster, Pinctada fucata. The mantle is believed to be the tissue responsible for shell and pearl formation. However, our current study on lead and copper accumulation in tissues of the oyster showed that the secondary tissue for lead accumulation was not the digestive gland but the mantle. In view of high lead concentrations in the mantle, its general metabolic condition (including immune and antioxidant defense systems) as affected by the two metals was studied. The results indicated that activities of antioxidant enzymes (superoxide dismutase, SOD; Se-dependent glutathione peroxidase, Se-GPx) were altered by lead and copper in the similar way. However, the immune enzyme activities (acid phosphatase, AcPase; phenoloxidase, PO) were perturbed differently by two metals. Therefore, the mantle of P. fucata was predicted to participate in immune processes and accumulation or detoxification of lead besides shell formation. Our observations described here may also provide important clues to further understanding of the biomarker responses of bivalves.

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.

軟体動物の石灰化組織の鉱物化に関する研究-XVIII

Sulfomucopolysaccharide or acid mucoprotein with sulfate group is detected in mantle mucus of some bivalves4-7), and is considered to act as a calcium carrier and provide calcium concentration high enough for the growth of shell minerals at the site of mineralization4). Histochemical and biochemical studies have suggested that the inner and outer mucus of the mantle of Pinctada fucata show metachromasia on staining with toluidine blue and are very similar to each other in their amino acid compositions1). If the acid mucous substances play the above-mentioned functional role in the calcium metabolism of molluscs, the mucus does not always form a shell. To answer this quesion, biochemical analysis of the acid polysaccharide was made on the inner and outer mucus of the mantle of Pinctada fucata and Chlamys nobilis. Inner mucus adhered on the inner surface of the mantle and outer mucus secreted between the mantle and shell were collected with an injector. In each case the dry mucus obtained by addition of ethyl alcohol was digested with “pronase” at pH 8.0 and 50°C for 72 hours and subsequently with trypsin at pH 7.5 and 37°C for 72 hours. Acid polysaccharide was then separated by the cetyl pyridinium chloride treatment and analysed as described in the preceding paper2). The amount and chemical composition of fraction A containing acid mucopolysaccharide are shown in Tables 1 and 2. The fraction contains a relatively large amount of sulfuric ester and a little amount of protein, but not chondroitine sulfate, as shown by paper electrophoresis. Galactosamine, glucosamine, galactose and glucose are detected in fraction A of both the inner and outer mantle mucus of Pinctada fucata by paper chromatography (Table 3). The fraction seems to be composed of sulfomucopolysaccharide or sulfated polysaccharide-protein complex. From these results, it may be concluded that the presence of the acid mucous substance with sulfate group is necessary to induce shell mineralization though it does not always induce it.