The diversity of shell matrix proteins: genome-wide investigation of the pearl oyster, Pinctada fucata.

In molluscs, shell matrix proteins are associated with biomineralization, a biologically controlled process that involves nucleation and growth of calcium carbonate crystals. Identification and characterization of shell matrix proteins are important for better understanding of the adaptive radiation of a large variety of molluscs. We searched the draft genome sequence of the pearl oyster Pinctada fucata and annotated 30 different kinds of shell matrix proteins. Of these, we could identified Perlucin, ependymin-related protein and SPARC as common genes shared by bivalves and gastropods; however, most gastropod shell matrix proteins were not found in the P. fucata genome. Glycinerich proteins were conserved in the genus Pinctada. Another important finding with regard to these annotated genes was that numerous shell matrix proteins are encoded by more than one gene; e.g., three ACCBP-like proteins, three CaLPs, five chitin synthase-like proteins, two N16 proteins (pearlins), 10 N19 proteins, two nacreins, four Pifs, nine shematrins, two prismalin-14 proteins, and 21 tyrosinases. This diversity of shell matrix proteins may be implicated in the morphological diversity of mollusc shells. The annotated genes reported here can be searched in P. fucata gene models version 1.1 and genome assembly version 1.0 ( http://marinegenomics.oist.jp/pinctada_fucata ). These genes should provide a useful resource for studies of the genetic basis of biomineralization and evaluation of the role of shell matrix proteins as an evolutionary toolkit among the molluscs.

Genetic structure and polymorphisms of the N16 gene in Pinctada fucata.

The molluscan shell is a composite of inorganic crystals comprising calcium carbonate and a minute amount of organic matrix. The organic matrix (OM) is intimately involved in every step of shell formation and has consequently received much attention in recent years. However, most of the deposited information has resulted from cDNA analysis, with little analysis of the genome, including the presence and effects of polymorphic genes encoding OM proteins. The current study aimed to clarify the genome structure of the N16 gene from the Japanese pearl oyster, Pinctada fucata, with particular reference to polymorphisms. The N16 gene was analyzed using PCR and DNA sequencing. 23 polymorphic variants were identified from 28 individuals. The variants were analyzed for their relationship to shell formation. All the variations detected by genomic PCR appeared in the cDNAs, implying that all the polymorphisms were transcribed and translated into N16 proteins. Additional genome analysis revealed at least two N16 genes, which were sequentially positioned, each of them comprising four exons and three introns. Further analyses of the transcriptional regulation and function of the N16 genes may provide new insights into their role in molluscan biomineralization.

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 31days. 3) 18S rRNA of P. fucata was determined to be more suitable as a real-time PCR reference gene compared with GAPDH and beta-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 CaCO(3) crystal polymorphism and shell microstructures in P. fucata.

A novel phosphorylated glycoprotein in the shell matrix of the oyster Crassostrea nippona.

We found a novel 52 kDa matrix glycoprotein MPP1 in the shell of Crassostrea nippona that was unusually acidic and heavily phosphorylated. Deduced from the nucleotide sequence of 1.9 kb cDNA, which is likely to encode MPP1 with high probability, the primary structure of this protein shows a modular structure characterized by repeat sequences rich in Asp, Ser and Gly. The most remarkable of these is the DE-rich sequence, in which continuous repeats of Asp are interrupted by a single Cys residue. Disulfide-dependent MPP1 polymers occurring in the form of multimeric insoluble gels are estimated to contain repetitive locations of the anionic molecules of phosphates and acidic amino acids, particularly Asp. Thus, MPP1 and its polymers possess characteristic features of a charged molecule for oyster biomineralization, namely accumulation and trapping of Ca2+. In addition, MPP1 is the first organic matrix component considered to be expressed in both the foliated and prismatic layers of the molluscan shell microstructure. In vitro crystallization assays demonstrate the induction of tabular crystals with a completely different morphology from those formed spontaneously, indicating that MPP1 and its polymers are potentially the agent that controls crystal growth and shell microstructure.

Isolation and characterization of the N-linked oligosaccharides in nacrein from Pinctada fucata.

We analyzed the structure of the N-linked oligosaccharides enzymatically liberated from the organic matrix (OM) component in the nacreous layer of Japanese pearl oyster: Pinctada fucata. The lectin-blot analysis of the soluble OM after separation by SDS-PAGE, four components, with sizes of approximately 55 kDa, 35 kDa, 25 kDa, and 21 kDa were detected with GNA lectin, which recognized terminal mannose of high mannose and hybrid types of N-glycan. The 55-kDa component of the soluble OM detected by lectin blotting was identified as nacrein by using liquid chromatography/mass spectrometry (LC/MS). LC/MS analysis of the N-glycan liberated from nacrein detected a hybrid-type N-glycan, which contained sulfite and sialic acid at its terminus. The data strongly imply that nacrein, a sulfated OM glycoprotein, participates in molluscan biomineralization by creating a favorable environment for calcium ion uptake through sulfonic acid and sialic acid.