Identification of chitin in the prismatic layer of the shell and a chitin synthase gene from the Japanese pearl oyster, Pinctada fucata

The shell of the Japanese pearl oyster, Pinctada fucata, consists of two layers, the prismatic layer on the outside and the nacreous layer on the inside, both of which comprise calcium carbonate and organic matrices. Previous studies indicate that the nacreous organic matrix of the central layer of the framework surrounding the aragonite tablet is beta-chitin, but it remains unknown whether organic matrices in the prismatic layer contain chitin or not. In the present study, we identified chitin in the prismatic layer of the Japanese pearl oyster, Pinctada fucata, with a combination of Calcofluor White staining with IR and NMR spectral analyses. Furthermore, we cloned a cDNA encoding chitin synthase (PfCHS1) that produces chitin, contributing to the formation of the framework for calcification in the shell.     

The Molecular Evolution of the Pif Family Proteins in Various Species of Mollusks

Various novel proteins have been identified from many kinds of mollusk shells. Although such matrix proteins are believed to play important roles in the calcium carbonate crystal formation of shells, no common proteins that interact with calcium carbonate or that are involved in the molecular mechanisms behind shell formation have been identified. Pif consists of two proteins, Pif 80 and Pif 97, which are encoded by a single mRNA. Pif 80 was identified as a key acidic protein that regulates the formation of the nacreous layer in Pinctada fucata, while Pif 97 has von Willebrand factor type A (VWA) and chitin-binding domains. In this study, we identified Pif homologues from Pinctada margaritifera, Pinctada maxima, Pteria penguin, Mytilus galloprovincialis, and in the genome database of Lottia gigantea in order to compare their primary protein sequences. The VWA and chitin-binding domains are conserved in all Pif 97 homologues, whereas the amino acid sequences of the Pif 80 regions differ markedly among the species. Sequence alignment revealed the presence of a novel significantly conserved sequence between the chitin-binding domain and the C-terminus of Pif 97. Further examination of the Pif 80 regions suggested that they share a sequence that is similar to the laminin G domain. These results indicate that all Pif molecules in bivalves and gastropods may be derived from a common ancestral gene. These comparisons may shed light on the correlation between molecular evolution and morphology in mollusk shell microstructure.     

Purification and structural determination of a phosphorylated peptide with anti-calcification and chitin-binding activities in the exoskeleton of the crayfish, Procambarus clarkii

Organic matrices in calcified hard tissues have been considered to control calcification. A matrix peptide, designated CAP-1, was extracted and purified by anion-exchange and reverse-phase high performance liquid chromatographies from the exoskeleton of the crayfish, Procambarus clarkii. The amino acid sequence of CAP-1 was determined by mass spectral and sequence analyses of the intact peptide and its enzymatically digested peptides. CAP-1 consisted of 78 amino acid residues, including a phosphoserine residue, and was rich in acidic amino acid residues. CAP-1 had a Rebers-Riddiford consensus sequence, which is conserved in cuticle proteins from many arthropods. CAP-1 inhibited precipitation of calcium carbonate in an in vitro anticalcification assay dose-dependently, and completely inhibited it at 3 x 10(-7) M. CAP-1 also showed chitin-binding ability, indicating that this molecule was bifunctional and played an important role in formation of the exoskeleton.     

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.     

The carbonic anhydrase domain protein nacrein is expressed in the epithelial cells of the mantle and acts as a negative regulator in calcification in the mollusc Pinctada fucata

Signals and organic matrix proteins secreted from the mantle are critical for the development of shells in molluscs. Nacrein, which is composed of a carbonic anhydrase domain and a Gly-X-Asn repeat domain, is one of the organic matrix proteins that accumulates in shells. In situ hybridization revealed that nacrein was expressed in the outer epithelial cells of the mantle of the pearl oyster Pinctada fucata. The recombinant nacrein protein inhibited the precipitation of calcium carbonate from a saturated solution containing CaCl2 and NaHCO3, indicating that it can act as a negative regulator for calcification in the shells of molluscs. Because deletion of the Gly-X-Asn repeat domain of nacrein had a significant effect on the ability of nacrein to inhibit the precipitation of calcium carbonate, it is conceivable that the repeat domain has a primary role in the inhibitory function of nacrein in shell formation. Together these studies suggest that nacrein functions as a negative regulator in calcification in the extrapallial space between the shell and the mantle by inhibiting the precipitation of CaCO3.     

A novel calcium-binding peptide from the cuticle of the crayfish, Procambarus clarkii

A novel peptide named calcification-associated peptide (CAP)-2 was isolated from the exoskeleton of the crayfish, Procambarus clarkii. CAP-2 consists of 65 amino acid residues and has a 44% sequence identity with CAP-1 characterized previously. It has a chitin-binding domain observed in many arthropod cuticle proteins. CAP-2 showed inhibitory activity on calcium carbonate precipitation and chitin-binding ability. A CAP-2 cDNA was cloned using RT-PCR and RACE and the open reading frame encoded a precursor peptide consisting of a signal peptide and CAP-2. RT-PCR revealed that CAP-2 mRNA was exclusively expressed in the epidermal tissue during the postmolt stage, the site and stage being associated with calcification. Calcium-binding assay using recombinant CAP-2 revealed that this peptide had affinity for calcium ions with a Kd value of about 1 mM. All these results suggest that CAP-2 serves as a nucleator or a regulator in the calcification of the exoskeleton.     

A Comparative Study of the Shell Matrix Protein Aspein in Pterioid Bivalves

Aspein is one of the unusually acidic shell matrix proteins originally identified from the pearl oyster Pinctada fucata. Aspein is thought to play important roles in the shell formation, especially in calcite precipitation in the prismatic layer. In this study, we identified Aspein homologs from three closely related pterioid species: Pinctada maxima, Isognomon perna, and Pteria penguin. Our immunoassays showed that they are present in the calcitic prismatic layer but not in the aragonitic nacreous layer of the shells. Sequence comparison showed that the Ser-Glu-Pro and the Asp-Ala repeat motifs are conserved among these Aspein homologs, indicating that they are functionally important. All Aspein homologs examined share the Asp-rich D-domain, suggesting that this domain might have a very important function in calcium carbonate formation. However, sequence analyses showed a significantly high level of variation in the arrangement of Asp in the D-domain even among very closely related species. This observation suggests that specific arrangements of Asp are not required for the functions of the D-domain.     

Structural characterization of the N-terminal mineral modification domains from the molluscan crystal-modulating biomineralization proteins, AP7 and AP24

The AP7 and AP24 proteins represent a class of mineral-interaction polypeptides that are found in the aragonite-containing nacre layer of mollusk shell (H. rufescens). These proteins have been shown to preferentially interfere with calcium carbonate mineral growth in vitro. It is believed that both proteins play an important role in aragonite polymorph selection in the mollusk shell. Previously, we demonstrated the 1-30 amino acid (AA) N-terminal sequences of AP7 and AP24 represent mineral interaction/modification domains in both proteins, as evidenced by their ability to frustrate calcium carbonate crystal growth at step edge regions. In this present report, using free N-terminal, C(alpha)-amide "capped" synthetic polypeptides representing the 1-30 AA regions of AP7 (AP7-1 polypeptide) and AP24 (AP24-1 polypeptide) and NMR spectroscopy, we confirm that both N-terminal sequences possess putative Ca (II) interaction polyanionic sequence regions (2 x -DD- in AP7-1, -DDDED- in AP24-1) that are random coil-like in structure. However, with regard to the remaining sequences regions, each polypeptide features unique structural differences. AP7-1 possesses an extended beta-strand or polyproline type II-like structure within the A11-M10, S12-V13, and S28-I27 sequence regions, with the remaining sequence regions adopting a random-coil-like structure, a trait common to other polyelectrolyte mineral-associated polypeptide sequences. Conversely, AP24-1 possesses random coil-like structure within A1-S9 and Q14-N16 sequence regions, and evidence for turn-like, bend, or loop conformation within the G10-N13, Q17-N24, and M29-F30 sequence regions, similar to the structures identified within the putative elastomeric proteins Lustrin A and sea urchin spicule matrix proteins. The similarities and differences in AP7 and AP24 N-terminal domain structure are discussed with regard to joint AP7-AP24 protein modification of calcium carbonate growth.     

A New Method to Extract Matrix Proteins Directly from the Secretion of the Mollusk Mantle and the Role of These Proteins in Shell Biomineralization

Considering the continuous and substantive secretory ability of the mantle in vitro, we report a new technique to produce shell-matrix proteins by inducing the mantle, after removal from the organism's body, to secrete soluble-matrix proteins into phosphate buffer. By this method, a large amount of matrix proteins could be obtained in 2 h. Experiments involving in vitro calcium carbonate crystallization and organic framework calcium carbonate crystallization indicated that these proteins retain high bioactivity and play key roles in shell biomineralization. Phosphate buffer-soluble proteins secreted by the margin of the mantles (MSPs) were used to reconstruct the stages in the growth of the prismatic layer of the decalcified organic frameworks. The MSPs were observed to aggregate calcites in vitro, and this ability enabled the mollusk to form big calcites in the prismatic layer. During shell biomineralization, an important stage after the self-assembly of the biomacromolecules and the formation of crystals is the assembly of the two parts to form a firm structure. Moreover, a new type of matrix protein, functioning as the binding factor between the crystals and the organic frameworks, was shown to exist in the phosphate buffer-soluble proteins secreted by the central part of mantles (CSPs). Nanoscale-sized bowl-like aragonites, with heights of ～800 nm, were induced by CSPs in vitro. This method is a successful example of obtaining functional proteins through secretion by animal tissues.     

Analysis of the chitin recognition mechanism of cuticle proteins from the soft cuticle of the silkworm, Bombyx mori

Insect cuticle is composed mainly of chitin, a polymer of N-acetylglucosamine, and chitin-binding cuticle proteins. Four major cuticle proteins, BMCP30, 22, 18, and 17, have been previously identified and purified from the larval cuticle of silkworm, B. mori. We analyzed the chitin-binding activity of BMCP30 by use of chitin-affinity chromatography. The pH optimum for the binding of BMCP30 to chitin is 6.4, which corresponds to hemolymph pH. Competition experiments using chitooligosaccharides suggested that BMCP30 recognizes 4-6 mer of N-acetylglucosamine in chitin fiber as a unit for binding. The comparison of the binding properties of BMCP30 with those of BMCP18 showed that their binding activities to chitin are similar in a standard buffer but that BMCP30 binds to chitin more stably than BMCP18 in the presence of urea. BMCPs possess the RR-1 form of the R&R consensus, about 70 amino acids region conserved widely among cuticle proteins mainly from the soft cuticle of many insect and arthropod species. Analysis of the binding activity using deletion mutants of BMCPs revealed that this type of conserved region also functions as the chitin-binding domain, similarly to the RR-2 region previously shown to confer chitin binding. Thus, the extended R&R consensus is the general chitin-binding domain of cuticle proteins in Arthropoda.     

SIRT1 contains N- and C-terminal regions that potentiate deacetylase activity

SIRT1 is one of seven mammalian sirtuin (silent information regulator 2-related) proteins that harbor NAD(+)-dependent protein deacetylase activity and is implicated in multiple metabolic and age-associated pathways and disorders. The sirtuin proteins contain a central region of high sequence conservation that is required for catalytic activity, but more variable N- and C-terminal regions have been proposed to mediate protein specific activities. Here we show that the conserved catalytic core domain of SIRT1 has very low catalytic activity toward several known protein substrates, but that regions N- and C-terminal to the catalytic core potentiate catalytic efficiency by between 12- and 45-fold, with the N-terminal domain contributing predominantly to catalytic rate, relatively independent of the nature of the acetyl-lysine protein substrate, and the C-terminal domain contributing significantly to the K(m) for NAD(+). We show that the N- and C-terminal regions stimulate SIRT1 deacetylase activity intramolecularly and that the C-terminal region stably associates with the catalytic core domain to form a SIRT1 holoenzyme. We also demonstrate that the C-terminal region of SIRT1 can influence the inhibitory activity of some sirtuin inhibitors that are known to function through the catalytic core domain. Together, these studies highlight the unique properties of the SIRT1 member of the sirtuin proteins and have implications for the development of SIRT1-specific regulatory molecules.     

Ubiquitylation functions in the calcium carbonate biomineralization in the extracellular matrix

Mollusks shell formation is mediated by matrix proteins and many of these proteins have been identified and characterized. However, the mechanisms of protein control remain unknown. Here, we report the ubiquitylation of matrix proteins in the prismatic layer of the pearl oyster, Pinctada fucata. The presence of ubiquitylated proteins in the prismatic layer of the shell was detected with a combination of western blot and immunogold assays. The coupled ubiquitins were separated and identified by Edman degradation and liquid chromatography/mass spectrometry (LC/MS). Antibody injection in vivo resulted in large amounts of calcium carbonate randomly accumulating on the surface of the nacreous layer. These ubiquitylated proteins could bind to specific faces of calcite and aragonite, which are the two main mineral components of the shell. In the in vitro calcium carbonate crystallization assay, they could reduce the rate of calcium carbonate precipitation and induce the calcite formation. Furthermore, when the attached ubiquitins were removed, the functions of the EDTA-soluble matrix of the prismatic layer were changed. Their potency to inhibit precipitation of calcium carbonate was decreased and their influence on the morphology of calcium carbonate crystals was changed. Taken together, ubiquitylation is involved in shell formation. Although the ubiquitylation is supposed to be involved in every aspect of biophysical processes, our work connected the biomineralization-related proteins and the ubiquitylation mechanism in the extracellular matrix for the first time. This would promote our understanding of the shell biomineralization and the ubiquitylation processes.     

The N-terminal region of an entomopoxvirus fusolin is essential for the enhancement of peroral infection, whereas the C-terminal region is eliminated in digestive juice

The spindles of Anomala cuprea entomopoxvirus (AncuEPV), which are composed of glycoprotein fusolin, are known to enhance the peroral infectivity of AncuEPV itself and of nucleopolyhedroviruses. This has been demonstrated to involve the disruption of intestinal peritrophic membrane (PM), composed of chitin matrix, glycosaminoglycans, and proteins. To identify essential and nonessential regions for this enhancement activity, AncuEPV fusolin and its deletion mutants were expressed in Sf21 cells using a baculovirus system, and their enhancement abilities were analyzed. The recombinant fusolin enhanced the peroral infectivity of Bombyx mori nucleopolyhedrovirus up to 320-fold and facilitated the infection of host insect with AncuEPV. Deletion mutagenesis revealed that the N-terminal region (amino acids 1 to 253), a possible chitin-binding domain, is essential for the enhancement of infection, whereas the C-terminal region is entirely dispensable. The glycosylation-defective mutants N191Q, whose Asn₁₉₁ is replaced with Gln, and ΔSIG, whose signal peptide is deleted, showed considerably reduced and abolished enhancing activities, respectively, indicating that the carbohydrate chain is important in the enhancing activity. Interestingly, the C-terminal dispensable region was digested by a serine protease(s) in insect digestive juice. Moreover, both the N-terminal conserved region and the carbohydrate chain were necessary not only for chitin binding but also for stability in digestive juice. A triple amino acid replacement mutant, IHE (Ile-His-Glu₁₆₁ to Ala-Ala-Ala), was stable in digestive juice and had chitin-binding ability but did not retain its enhancing activity. These results suggest that the enhancement of infectivity involves more than the tolerance to digestive juice and chitin-binding ability.     

A conserved domain in arthropod cuticular proteins binds chitin

Many insect cuticular proteins include a 35-36 amino acid motif known as the R&R consensus. The extensive conservation of this region led to the suggestion that it functions to bind chitin. Provocatively, it has no sequence similarity to the well-known cysteine-containing chitin-binding domain found in chitinases and some peritrophic membrane proteins. Using fusion proteins expressed in E. coli, we show that an extended form of the R&R consensus from proteins of hard cuticles is necessary and sufficient for chitin binding. Recombinant AGCP2b, a putative cuticular protein from the mosquito Anopheles gambiae, was expressed in E. coli and the purified protein shown to bind to chitin beads. A stretch of 65 amino acids from AGCP2b, including the R&R consensus, conferred chitin binding to glutathione-S-transferase (GST). Directed mutagenesis of some conserved amino acids within this extended R&R consensus from hard cuticle eliminated chitin binding. Thus arthropods have two distinct classes of chitin binding proteins, those with the chitin-binding domain found in lectins, chitinases and peritrophic membranes (cysCBD) and those with the cuticular protein chitin-binding domain (non-cysCBD).     

A metalloprotease (MprIII) involved in the chitinolytic system of a marine bacterium,Alteromonas sp. strain O-7

Alteromonas sp. strain O-7 secretes several proteins in addition to chitinolytic enzymes in response to chitin induction. In this paper, we report that one of these proteins, designated MprIII, is a metalloprotease involved in the chitin degradation system of the strain. The gene encoding MprIII was cloned in Escherichia coli. The open reading frame of mprIII encoded a protein of 1,225 amino acids with a calculated molecular mass of 137,016 Da. Analysis of the deduced amino acid sequence of MprIII revealed that the enzyme consisted of four domains: the signal sequence, the N-terminal proregion, the protease region, and the C-terminal extension. The C-terminal extension (PkdDf) was characterized by four polycystic kidney disease domains and two domains of unknown function. Western and real-time quantitative PCR analyses demonstrated that mprIII was induced in the presence of insoluble polysaccharides, such as chitin and cellulose. Native MprIII was purified to homogeneity from the culture supernatant of Alteromonas sp. strain O-7 and characterized. The molecular mass of mature MprIII was estimated by sodium dodecyl sulfate-polyacrylamide gel electrophoresis to be 115 kDa. The optimum pH and temperature of MprIII were 7.5 and 50 degrees C, respectively, when gelatin was used as a substrate. Pretreatment of native chitin with MprIII significantly promoted chitinase activity. Furthermore, the combination of MprIII and a novel chitin-binding protease (AprIV) remarkably promoted the chitin hydrolysis efficiency of chitinase.     

Structural basis for new pattern of conserved amino acid residues related to chitin-binding in the antifungal peptide from the coconut rhinoceros beetle Oryctes rhinoceros

Scarabaecin isolated from hemolymph of the coconut rhinoceros beetle Oryctes rhinoceros is a 36-residue polypeptide that has antifungal activity. The solution structure of scarabaecin has been determined from twodimensional 1H NMR spectroscopic data and hybrid distance geometry-simulated annealing protocol calculation. Based on 492 interproton and 10 hydrogen-bonding distance restraints and 36 dihedral angle restraints, we obtained 20 structures. The average backbone root-mean-square deviation for residues 4-35 is 0.728 +/- 0.217 A from the mean structure. The solution structure consists of a two-stranded antiparallel beta-sheet connected by a type-I beta-turn after a short helical turn. All secondary structures and a conserved disulfide bond are located in the C-terminal half of the peptide, residues 18-36. Overall folding is stabilized by a combination of a disulfide bond, seven hydrogen bonds, and numerous hydrophobic interactions. The structural motif of the C-terminal half shares a significant tertiary structural similarity with chitin-binding domains of plant and invertebrate chitin-binding proteins, even though scarabaecin has no overall sequence similarity to other peptide/polypeptides including chitin-binding proteins. The length of its primary structure, the number of disulfide bonds, and the pattern of conserved functional residues binding to chitin in scarabaecin differ from those of chitin-binding proteins in other invertebrates and plants, suggesting that scarabaecin does not share a common ancestor with them. These results are thought to provide further strong experimental evidence to the hypothesis that chitin-binding proteins of invertebrates and plants are correlated by a convergent evolution process.     

Significance of the N- and C-terminal regions of CAP-1, a cuticle calcification-associated peptide from the exoskeleton of the crayfish, for calcification

Calcification-associated peptide (CAP)-1 is considered to play an important role in calcification of the exoskeleton of the crayfish, Procambarus clarkii. In this study, in order to clarify the molecular mechanism of calcification, we constructed expression systems of recombinant molecules of CAP-1 and its related peptides in Escherichia coli, and verified the structure-activity relationship of these peptides. The inhibitory assay on calcium carbonate precipitation and the calcium-binding assay showed that the C-terminal acidic region was most important for both activities. The CD spectra of these peptides varied depending on calcium concentration and showed that the N-terminal region is associated with the peptide conformation. These results indicate that the C-terminal part of CAP-1 may concentrate calcium ions for nucleation and/or interact with calcium carbonate precipitate to control the growth and that the N-terminal part contribute to maintaining the peptide conformation.     

A Metalloprotease (MprIII) Involved in the Chitinolytic System of a Marine Bacterium, Alteromonas sp. Strain O-7

Alteromonas sp. strain O-7 secretes several proteins in addition to chitinolytic enzymes in response to chitin induction. In this paper, we report that one of these proteins, designated MprIII, is a metalloprotease involved in the chitin degradation system of the strain. The gene encoding MprIII was cloned in Escherichia coli. The open reading frame of mprIII encoded a protein of 1,225 amino acids with a calculated molecular mass of 137,016 Da. Analysis of the deduced amino acid sequence of MprIII revealed that the enzyme consisted of four domains: the signal sequence, the N-terminal proregion, the protease region, and the C-terminal extension. The C-terminal extension (PkdDf) was characterized by four polycystic kidney disease domains and two domains of unknown function. Western and real-time quantitative PCR analyses demonstrated that mprIII was induced in the presence of insoluble polysaccharides, such as chitin and cellulose. Native MprIII was purified to homogeneity from the culture supernatant of Alteromonas sp. strain O-7 and characterized. The molecular mass of mature MprIII was estimated by sodium dodecyl sulfate-polyacrylamide gel electrophoresis to be 115 kDa. The optimum pH and temperature of MprIII were 7.5 and 50°C, respectively, when gelatin was used as a substrate. Pretreatment of native chitin with MprIII significantly promoted chitinase activity. Furthermore, the combination of MprIII and a novel chitin-binding protease (AprIV) remarkably promoted the chitin hydrolysis efficiency of chitinase.     

合浦珠母贝SOX9对Prismalin-14基因的调控研究

目的:研究合浦珠母贝转录因子SOX9对Prismalin-14的转录调控机制。方法:应用在线预测软件PROMO分析Prismalin-14的启动子序列,以预测Prismalin-14启动子上可能的转录因子与其结合位点;运用细胞共转染实验和双荧光素酶报告系统以检测SOX9对Prismalin-14启动子的激活作用;构建Prismalin-14启动子截短体的荧光素酶报告载体,并和SOX9的真核载体共转到HEK-293T细胞中,再进行双荧光素酶报告系统检测Prismalin-14启动子的活性;构建SOX9截短体的真核表达载体,并与Prismalin-14启动子的荧光素酶报告载体共转到HEK-293T细胞中,再进行双荧光素酶报告分析Prismalin-14启动子的活性。结果:SOX9能激活Prismalin-14的启动子的活性,并具有剂量效应;对Prismalin-14启动子进行截短后,不包含结合位点的Prismalin-14启动子的活性是野生型Prismalin-14启动子活性的49%,推测Prismalin-14启动子上的-415bp到-405bp区域是SOX9激活作用的关键区域;对SOX9的SRY-related HMG结构域进行截短后,其对Prismalin-14启动子的激活作用显著减少,因此SOX9结构的完整对Prismalin-14启动子活性的激活作用是必须的。结论:Prismalin-14的转录可能受SOX9调控,为进一步研究合浦珠母贝的转录调控机制提供基础,将有助于从分子水平上理解贝壳形成的上游调控机理。