Spicule matrix protein LSM34 is essential for biomineralization of the sea urchin spicule.

Biomineralized skeletal structures are composite materials containing mineral and matrix protein(s). The cell biological mechanisms that underlie the formation, secretion, and organization of the biomineralized materials are not well understood. Although the matrix proteins influence physical properties of the structures, little is known of the role of these matrix proteins in the actual formation of the biomineralized structure. We present here results using an antisense oligonucleotide directed against a spicule matrix protein, LSM34, present in spicules of embryos of Lytechinus pictus. After injection of anti-LSM34 into the blastocoel of a sea urchin embryo, LSM34 protein in the primary mesenchyme cells decreases and biomineralization ceases, demonstrating that LSM34 function is essential for the formation of the calcareous endoskeletal spicule of the embryo. Since LSM34 is found primarily in a specialized extracellular matrix surrounding the spicule, it is probable that this matrix is important for the biomineralization process.     

Matrix and Mineral in the Sea Urchin Larval Skeleton

The endoskeletal spicules of sea urchin larvae are composed of calcite, a surrounding extracellular matrix, and small amounts of occluded matrix proteins. The spicules are formed by primary mesenchyme cells (PMCs) in the blastocoel of the embryo, where they adopt stereotypical locations, thereby specifying where spicules will form. PMCs also fuse to form cytoplasmic cords connecting the cell bodies, and it is within the cords that spicules arise. The mineral phase contains 5% Mg as well as Ca, and about 0.1% of the mass is protein. The matrix and mineral form concentric plies, and the composite has different physical properties than those of pure calcite. The calcite diffracts as a single crystal and is composed of well-ordered, but not perfectly ordered, microdomains. There is evidence for adsorption of matrix proteins to specific crystal faces at domain boundaries, which may help regulate crystal growth and texture. Immature spicules contain considerable precipitated amorphous CaCO3, and PMCs also have vesicles that contain amorphous CaCO3. This suggests the hypothesis that the cellular precursor to the spicules is actually amorphous CaCO3 stabilized in the cell by protein. The spicule s enveloped by the PMC cord, but is topologically exterior to the cell. The PMC plasmalemma is tightly applied to the developing spicules, except perhaps at the elongating tip. The characteristics, localization, and possible function of the four identified matrix proteins are discussed. SM50, SM37, and PM27 all primarily enclose the mineral, though small amounts are occluded. SM30 is found in cellular vesicles and is probably the principal occluded protein of the spicule.     

Expression of spicule matrix proteins in the sea urchin embryo during normal and experimentally altered spiculogenesis

During its embryonic development, the sea urchin embryo forms an endoskeletal calcitic spicule. This instance of biomineralization is experimentally accessible and also offers the advantage of occurring within a developmental context. Here we investigate the time course of appearance and localization of two proteins among the four dozen that constitute the protein matrix of the skeletal spicule. SM50 and SM30 have been studied in some detail, and polyclonal antisera have been prepared against them (C. E. Killian and F. H. Wilt, 1996, J. Biol. Chem. 271, 9150-9159). Using these antibodies we describe here the localization and time course of accumulation of these two proteins in Strongylocentrotus purpuratus, both in the intact embryo and in micromere cultures. We also investigate the disposition of the matrix proteins, SM50, SM30, and PM27, in the three-dimensional spicule by studying changes in protein localization during experimental manipulation of isolated skeletal spicules. We conclude that SM50, PM27, and SM30 probably play different roles in biomineralization, based on their localization and patterns of expression. It is unlikely that these proteins are solely structural elements within the mineral. SM50 and PM27 may play a role in defining the extracellular space in which spicule deposition occurs, while SM30 may play a role in secretion of spicule components. Finally, we report on the effects of serum on expression of some primary mesenchyme-specific proteins in micromere cultures; withholding serum severely depresses accumulation of SM30 but has only modest effects on the accumulation of other proteins.     

Role of LSM34/SpSM50 proteins in endoskeletal spicule formation in sea urchin embryos

Abstract. Sea urchin embryos form an endoskeletal spicule composed of calcium carbonate and occluded matrix proteins. The accumulation of the LSM34 spicule matrix protein in embryos of Lytechinus pictus (and its ortholog, SpSM50, in Strongylocentrotus purpuratus ) has been inhibited using morpholino antisense oligonucleotides. The inhibition, using relatively high levels of antisense reagent, can result in the complete absence of spicules, and the complete loss of immunoreactive LSM34/SpSM50, as judged by immunostaining and Western blotting. Primary mesenchyme cells (PMCs) do form and express PMC-specific cell surface antigens despite this inhibition. However, these anti-LSM34/SpSM50-treated embryos do not accumulate SM30 protein, another major matrix protein. Hence, both the initiation of spicule formation and subsequent morphogenesis require LSM34 accumulation in L. pictus , and the accumulation of its ortholog, SpSM50, in S. purpuratus .     

The localization of occluded matrix proteins in calcareous spicules of sea urchin larvae

The sea urchin embryo forms calcareous endoskeletal spicules composed of calcite and an occluded protein matrix. Though the latter is approximately 0.1% of of the mass, the composite has substantially altered material properties, e.g., conchoidal fracture planes and increased hardness. Experiments were conducted to examine the localization of matrix proteins occluded in the mineral by use of immunocytochemistry coupled with scanning electron microscopy (SEM). The isolated, unfixed spicules were etched under relatively gentle conditions and exposed to affinity purified antibodies made against two different matrix proteins, as well as an antibody to the entire constellation of matrix proteins. Immunogold tagged secondary antibody was used to observe antibody localization in the back scatter mode of SEM. All proteins examined were very widely distributed throughout the calcite, supporting a model of the structure in which a multiprotein assemblage is woven with fine texture around microcrystalline domains of calcite. Gentle etching revealed a laminar arrangement of calcite solubility, consistent with a stepwise deposition of matrix and mineral to increase girth of the spicule.     

Immunogold detection of glycoprotein antigens in sea urchin embryos

Four developmental stages of sea urchin embryos were labeled with colloidal gold in an attempt to elucidate the intracellular trafficking patterns within the cells that produce the glycoprotein matrix of the embryonic spicule. The primary mesenchyme cells (PMCs) form a syncytium and secrete an organic matrix on which calcium carbonate is laid down to form an endoskeletal spicule. The organic matrix has been isolated and characterized as glycoprotein consisting of four major bands. Polyclonal antibodies to these glycoproteins were used to label embryos from the mesenchyme blastula, early gastrula, late gastrula, and plutei stages of development. The label is concentrated in the Golgi complex and associated vesicles, in secretory vesicles, and in the organic matrix. The density of the labeling increases as development proceeds.     

Spiculogenesis in the sea urchin embryo: Studies on the SM30 spicule matrix protein

When proteins isolated from spicules of Strongylocentrotus purpuratus embryos were examined by western blot analysis, a major protein of approximately 43 kDa was observed to react with the monoclonal antibody, mAb 1223. Previous studies have established that this antibody recognizes an asparagine-linked, anionic carbohydrate epitope on the cell surface glycoprotein, msp130. This protein has been shown to be specifically associated with the primary mesenchyme cells involved in assembly of the spicule. Moreover, several lines of evidence have implicated the carbohydrate epitope in Ca²⁺ deposition into the growing spicule. The 43 kDa, spicule matrix protein detected with mAb 1223 also reacted with a polyclonal antibody to a known spicule matrix protein, SM30. Further characterization experiments, including deglycosylation using PNGaseF, two-dimensional electrophoresis, and immunoprecipitation, verified that the 43 kDa spicule matrix protein had a pl of approximately 4.0, contained the carbohydrate epitope recognized by monoclonal antibody mAb 1223 and reacted with anti-SM30. Electron microscopy confirmed the presence of proteins within the demineralized spicule that reacted with mAb 1223 and anti-SM30. We conclude that the spicule matrix protein, SM30, is a glycoprotein containing carbohydrate chains similar or identical to those on the primary mesenchyme cell membrane glycoprotein, msp130.     

Cellular control over spicule formation in sea urchin embryos: A structural approach

The spicules of the sea urchin embryo form in intracellular membrane-delineated compartments. Each spicule is composed of a single crystal of calcite and amorphous calcium carbonate. The latter transforms with time into calcite by overgrowth of the preexisting crystal. Relationships between the membrane surrounding the spiculogenic compartment and the spicule mineral phase were studied in the transmission electron microscope (TEM) using freeze-fracture. In all the replicas observed the spicules were tightly surrounded by the membrane. Furthermore, a variety of structures that are related to the material exchange process across the membrane were observed. The spiculogenic cells were separated from other cell types of the embryo, frozen, and freeze-dried on the TEM grids. The contents of electron-dense granules in the spiculogenic cells were shown by electron diffraction to be composed of amorphous calcium carbonate. These observations are consistent with the notion that the amorphous calcium carbonate-containing granules contain the precursor mineral phase for spicule formation and that the membrane surrounding the forming spicule is involved both in transport of material and in controlling spicule mineralization.     

Biomineralization of the spicules of sea urchin embryos

The formation of calcareous skeletal elements by various echinoderms, especially sea urchins, offers a splendid opportunity to learn more about some processes involved in the formation of biominerals. The spicules of larvae of euechinoids have been the focus of considerable work, including their developmental origins. The spicules are composed of a single optical crystal of high magnesium calcite and variable amounts of amorphous calcium carbonate. Occluded within the spicule is a proteinaceous matrix, most of which is soluble; this matrix constitutes about 0.1% of the mass. The spicules are also enclosed by an extracellular matrix and are almost completely surrounded by cytoplasmic cords. The spicules are deposited by primary mesenchyme cells (PMCs), which accumulate calcium and secrete calcium carbonate. A number of proteins specific, or highly enriched, in PMCs, have been cloned and studied. Recent work supports the hypothesis that proteins found in the extracellular matrix of the spicule are important for biomineralization.     

Characterization of sea urchin primary mesenchyme cells and spicules during biomineralization in vitro

An in vitro culture system for primary mesenchyme cells of the sea urchin embryo has been used to study the cellular characteristics of skeletal spicule formation. As judged initially by light microscopy, these cells attached to plastic substrata, migrated and fused to form syncytia in which mineral deposits accumulated in the cell bodies and in specialized filopodial templates. Subsequent examination by scanning electron microscopy revealed that the cell bodies and the filopodia and lamellipodia formed spatial associations similar to those seen in the embryo and indicated that the spicule was surrounded by a membrane-limited sheath derived by fusion of the filopodia. The spicules were dissolved from living or fixed cells by a chelator of divalent cations or by lowering the pH of the medium. However, granular deposits found in the cell bodies appeared relatively refractory to such treatments, indicating that they were inaccessible to agents that dissolved the spicules. Use of rapid freezing and an anhydrous fixative to preserve the syncytia for transmission electron microscopy and X-ray microprobe analysis, indicated that electron-dense deposits in the cell bodies contain elements (Ca, Mg and S) common to the spicule. Examination of the spicule cavity after dissolution of the spicule mineral revealed openings in the filopodia-derived sheath, coated pits within the limiting membrane and a residual matrix that stained with ruthenium red. Concanavalin A--gold applied exogenously entered the spicule cavity and bound to matrix glycoproteins. Based on these observations, we conclude that components of the spicule initially are sequestered intracellularly and that spicule elongation occurs in an extracellular cavity. Ca2+ and associated glycoconjugates may be routed in this cavity via a secretory pathway.     

Protein and mineral composition of osteogenic extracellular matrix constructs generated with a flow perfusion bioreactor

This study investigated the temporal composition of an osteogenic extracellular matrix construct generated by culturing mesenchymal stem cells in an electrospun biodegradable poly(ε-caprolactone) fiber mesh scaffold within a flow perfusion bioreactor. Constructs of different extracellular matrix maturities were analyzed for their protein and mineral composition at several culture durations by liquid chromatography-tandem mass spectrometry, scanning electron microscopy, energy-dispersive X-ray diffraction, X-ray diffraction, and calcium and phosphate assays. The analysis revealed that at short culture durations the cells deposited cellular adhesion proteins as a prerequisite protein network for further bone formation. At the later culture durations, the extracellular matrix was composed of collagen 1, hydroxyapatite, matrix remodeling proteins, and regulatory proteins. These results suggest that the later culture duration constructs would allow for improved bone regeneration due to the ability to mineralize and the capabilities for future remodeling.     

Characterization of proteins from the matrix of spicules from the alcyonarian, Lobophytum crassum

The organic matrix of spicules of the alcyonarian coral, Lobophytum crassum, was studied to investigate its molecular characteristics and functional properties. The shape of the spicules was identified using scanning electron microscopy. The soluble organic matrix comprised 0.03% of the spicule weight. The SDS-PAGE analysis of the preparation showed four protein bands with apparent molecular weights of 37, 48, 67 and 102 kDa. The 67- and 102-kDa proteins appeared to be calcium binding proteins, detected as radioactive bands by ⁴⁵Ca autoradiography. The 67-kDa protein appears to be glycosylated. The N-terminal amino acid sequence of the 67 kDa was determined; 7 of 20 residues were acidic. A database search for homologous proteins did not give a clear indication of the function of the 67-kDa protein. The isolated organic matrix possesses carbonic anhydrase activity which functions in calcium carbonate crystal formation, indicating that organic matrix is not only structural protein but also a catalyst. An interpretation of these results is that the spicule of alcyonarian corals has a proteinaceous organic matrix related to the calcification process.     

The organic matrix of the skeletal spicule of sea urchin embryos

The micromeres that arise at the fourth cell division in developing sea urchin embryos give rise to primary mesenchyme, which in turn differentiates and produces calcareous endoskeletal spicules. These spicules have been isolated and purified from pluteus larvae by washing in combinations of ionic and nonionic detergents followed by brief exposure to sodium hypochlorite. The spicules may be demineralized and the integral matrix dissolves. The matrix is composed of a limited number of glycoproteins rich in aspx, glux, gly, ser, and ala, a composition not unlike that found in matrix proteins of biomineralized tissues of molluscs, sponges, and arthropods. There is no evidence for collagen as a component of the matrix. The matrix contains N-linked glycoproteins of the complex type. The matrix arises primarily from proteins synthesized from late gastrulation onward, during the time that spicule deposition occurs. The mixture of proteins binds calcium and is an effective immunogen. Electrophoresis of the glycoproteins on SDS-containing acrylamide gels, followed by blotting and immunocytochemical detection, reveals major components of approximately 47, 50, 57, and 64 kD, and several minor components. These same components may be detected with silver staining or fluorography of amino acid-labeled proteins. In addition to providing convenient molecular marker for the study of the development of the micromere lineage, the spicule matrix glycoproteins provide an interesting system for investigations in biomineralization.     

Development of calcareous skeletal elements in invertebrates

Most metazoans require skeletal support systems. While the formation of bones and teeth in vertebrates has been well studied, endo- and exoskeleton development of non-vertebrates, especially calcification during terminal differentiation, has been neglected. Biomineralization of skeletons in invertebrates presents interesting research opportunities. We undertake here to survey some of the better understood examples of skeletal development in selected invertebrates. The differentiation of the skeletal spicules of euechinoid larvae and other non-vertebrate deuterostomes, the shells of molluscs, and the calcification of crustacean carapaces are surveyed. The diversity of these different kinds of animals and our present limited understanding make it difficult to identify unifying themes, but there certainly are unifying questions: How is the mineral precursor secreted? What is the nature of the interaction of mineral with the matrix proteins of the skeleton? Is there any conservation of protein domains in matrix proteins found in skeletal elements from different phyla? Are there common strategies in the development of organs that form mineralized structures?     

Bone mineralization proceeds through intracellular calcium phosphate loaded vesicles: a cryo-electron microscopy study

Bone is the most widespread mineralized tissue in vertebrates and its formation is orchestrated by specialized cells - the osteoblasts. Crystalline carbonated hydroxyapatite, an inorganic calcium phosphate mineral, constitutes a substantial fraction of mature bone tissue. Yet key aspects of the mineral formation mechanism, transport pathways and deposition in the extracellular matrix remain unidentified. Using cryo-electron microscopy on native frozen-hydrated tissues we show that during mineralization of developing mouse calvaria and long bones, bone-lining cells concentrate membrane-bound mineral granules within intracellular vesicles. Elemental analysis and electron diffraction show that the intracellular mineral granules consist of disordered calcium phosphate, a highly metastable phase and a potential precursor of carbonated hydroxyapatite. The intracellular mineral contains considerably less calcium than expected for synthetic amorphous calcium phosphate, suggesting the presence of a cellular mechanism by which phosphate entities are first formed and thereafter gradually sequester calcium within the vesicles. We thus demonstrate that in vivo osteoblasts actively produce disordered mineral packets within intracellular vesicles for mineralization of the extracellular developing bone tissue. The use of a highly disordered precursor mineral phase that later crystallizes within an extracellular matrix is a strategy employed in the formation of fish fin bones and by various invertebrate phyla. This therefore appears to be a widespread strategy used by many animal phyla, including vertebrates.     

Identification of a "glycine-loop"-like coiled structure in the 34 AA Pro,Gly,Met repeat domain of the biomineral-associated protein,PM27

Fracture resistance in biomineralized structures has been linked to the presence of proteins, some of which possess sequences that are associated with elastic behavior. One such protein superfamily, the Pro,Gly-rich sea urchin intracrystalline spicule matrix proteins, form protein-protein supramolecular assemblies that modify the microstructure and fracture-resistant properties of the calcium carbonate mineral phase within embryonic sea urchin spicules and adult sea urchin spines. In this report, we detail the identification of a repetitive keratin-like "glycine-loop"- or coil-like structure within the 34-AA (AA: amino acid) N-terminal domain, (PGMG)(8)PG, of the spicule matrix protein, PM27. The identification of this repetitive structural motif was accomplished using two capped model peptides: a 9-AA sequence, GPGMGPGMG, and a 34-AA peptide representing the entire motif. Using CD, NMR spectrometry, and molecular dynamics simulated annealing/minimization simulations, we have determined that the 9-AA model peptide adopts a loop-like structure at pH 7.4. The structure of the 34-AA polypeptide resembles a coil structure consisting of repeating loop motifs that do not exhibit long-range ordering. Given that loop structures have been associated with protein elastic behavior and protein motion, it is plausible that the 34-AA Pro,Gly,Met repeat sequence motif in PM27 represents a putative elastic or mobile domain.     

Proteins of calcified endoskeleton: II partial amino acid sequences of endoskeletal proteins and the characterization of proteinaceous organic matrix of spicules from the alcyonarian, Synularia polydactyla

Calcified organic substances in the skeleton contain a protein-polysaccharide complex taking a key role in the regulation of bio-calcification. However, information concerning the matrix proteins in alcyonarian and their effect on calcification process is still unknown. For this reason, we have studied the organic matrix of endoskeletal spicules from the alcyonarian coral, Synularia polydactyla, to analyze the proteins with their sequences and investigate the functional properties by a molecular approach. The separated spicules from the colony were identified by scanning electron microscope (SEM). The soluble organic matrix comprised 0.04% of spicule weight. By recording decline of pH in the experimental design, the inhibitory effect of the matrix on CaCO3 precipitation was revealed. Prior to electrophoresis, our analysis of proteins extracted from the soluble organic matrix of the spicules revealed an abundance of proteins in molecular weight. The sodium dodecyl sulfate-polyacrylamide gel electrophoresis (SDS-PAGE) analysis of the preparations showed seven bands of proteins with an apparent molecular mass of 109, 83, 70, 63, 41, 30 and 22 kDa. The proteins were electrophoresed on Tricine-SDS-PAGE after electro-elution treatment, and then transferred to polyvinylidene difluoride (PVDF) membranes and their N-termini were sequenced. Two bands of proteins of about 70 and 63 kDa successfully underwent N-terminal amino acid sequencing. For the detection of calcium binding proteins, a Ca2+ overlay analysis was conducted on the extract by 45Ca autoradiography. The 109 and 63 kDa calcium binding proteins were found to be radioactive. Periodic acid schiff staining indicated that 83 and 63 kDa proteins were glycosylated. An assay for carbonic anhydrase, which is thought to play an important role in the process of calcification revealed low level of the activity. These findings suggest that the endoskeletal spicules of alcyonarian corals have protein-rich organic matrices, which might be related to the calcification process.     

Spatially and temporally controlled biomineralization is facilitated by interaction between self-assembled dentin matrix protein 1 and calcium phosphate nuclei in solution

Bone and dentin biomineralization are well-regulated processes mediated by extracellular matrix proteins. It is widely believed that specific matrix proteins in these tissues modulate nucleation of apatite nanoparticles and their growth into micrometer-sized crystals via molecular recognition at the protein-mineral interface. However, this assumption has been supported only circumstantially, and the exact mechanism remains unknown. Dentin matrix protein 1 (DMP1) is an acidic matrix protein, present in the mineralized matrix of bone and dentin. In this study, we have demonstrated using synchrotron small-angle X-ray scattering that DMP1 in solution can undergo oligomerization and temporarily stabilize the newly formed calcium phosphate nanoparticle precursors by sequestering them and preventing their further aggregation and precipitation. The solution structure represents the first low-resolution structural information for DMP1. Atomic force microscopy and transmission electron microscopy studies further confirmed that the nascent calcium phosphate nuclei formed in solution were assembled into ordered protein-mineral complexes with the aid of oligomerized DMP1, recombinant and native. This study reveals a novel mechanism by which DMP1 might facilitate initiation of mineral nucleation at specific sites during bone and dentin mineralization and prevent spontaneous calcium phosphate precipitation in areas in which mineralization is not desirable.     

Studies on the Cellular Pathway Involved in Assembly of the Embryonic Sea Urchin Spicule

Micromeres from the 16-cell stage sea urchin embryo were isolated and cultured in vitro in seawater containing 3% horse serum. Under these conditions these cells differentiate into spicule-forming, primary mesenchyme cells. To obtain insight into the route traveled by Ca²⁺ to form the pseudocrystalline spicule composed of CaCO₃ and matrix proteins, studies with various inhibitors were undertaken. Experiments with members of several different classes of Ca²⁺ channel blockers established that the Ca²⁺ utilized for spiculogenesis must be taken up by the cells. Moreover, studies using two agents that disrupt the endomembrane system, monensin and brefeldin A, showed that both blocked spicule formation. Based on these experiments, we conclude that extracellular Ca²⁺ must enter the primary mesenchyme cells prior to being deposited extracellularly as CaCO₃ and that this ion and/or the matrix proteins found in the spicule are routed through the secretory pathway that has been established to exist in a wide variety of other cell types.