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.     

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.     

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.     

CRYSTAL PROPERTY OF THE LARVAL SEA URCHIN SPICULE*

A pair of pluteus skeletal spicules arises from a pair of calcareous granules via the triradiate form. In polarized light, each spicule behaves as though carved out of a single crystal of magnesian calcite. The optic axis lies perpendicular to the plane of the triradiate and parallel to the body rod of the pluteus. However, in the scanning electron microscope, the spicule surface appeared smooth or somewhat spongy and manifested no crystal faces. Neither etching nor fracturing revealed underlying crystalline texture. Nevertheless, rhombohedral calcite crystals could be grown epitaxially onto isolated spicules immersed in a medium containing CaCl₂ and NaHCO₃. The optic axes of all crystals coincided with the optic axis of the spicule on which they were grown. Corresponding faces of the crystals were all aligned parallel to each other despite the complex shape of each spicule. Where the left and right spicules joined, two mutually tilted sets of crystals were observed but not crystals of intermediate orientation. Thus, the sea urchin larval spicule is built from a stack of molecularly contiguous microcrystals but its overall shape is generated by the mesenchyme cells independent of the magnesian calcite crystal habit.     

Ultrastructural localization of spicule matrix proteins in normal and metalloproteinase inhibitor-treated sea urchin primary mesenchyme cells

Studies of the sea urchin larval skeleton have contributed greatly to our understanding of the process of biomineralization. In this study we have undertaken an investigation of the morphology of skeleton formation and the localization of proteins involved in the process of spicule formation at the electron microscope level. Sea urchin primary mesenchyme cells undergo a number of morphological changes as they synthesize the larval skeleton. They form a large spicule compartment that surrounds the growing spicule and, as spicule formation comes to an end, the density of the cytoplasm decreases. Inhibition of spicule formation by specific matrix metalloproteinase inhibitors or serum deprivation has some subtle effects on the morphology of cells and causes the accumulation of specific classes of vesicles. We have localized proteins of the organic matrix of the spicule and found that one protein, SM30, is localized to the Golgi apparatus and transport vesicles in the cytoplasm as well as throughout the occluded protein matrix of the spicule itself. This localization suggests that SM30 is an important structural protein in the spicule. Another spicule matrix protein, SM50, has a similar cytoplasmic localization, but in the spicule much of it is localized at the periphery of the spicule compartment, and consequently it may play a role in the assembly of new material onto the growing spicule or in the maintenance of the integrity of the matrix surrounding the spicule.     

Skeletogenesis in sea urchin interordinal hybrid embryos

Reciprocal interordinal crosses were made between the sea urchins Strongylocentrotus purpuratus and Lytechinus pictus. Previous research indicated that the expression of many L. pictus genes is reduced in the hybrid embryos. The S. purpuratus gene encoding the spicule matrix protein SM50 and the L. pictus gene encoding its orthologue LSM34 were both expressed at normal levels per gene copy in hybrid embryos, and in about 32 skeletogenic primary mesenchyme cells (PMCs) in hybrid and natural gastrulae. In many embryos of all crosses, 16 PMCs initially ingressed, while 32-64 PMCs were present in gastrulae. The skeletal spicules of most hybrid plutei were predominantly like those of S. purpuratus, consistent with the predominance of expression of S. purpuratus genes in hybrid embryos. The spicules of some hybrid plutei showed features characteristic of L. pictus, such as recurrent rods, branched body rod tips, or convergent ventral transverse rods; a few hybrid spicules were predominantly like those of L. pictus. Based on our observations and the literature, we propose the following. Cues from the ectodermal epithelium position the PMCs as they elaborate the initial triradiate spicules. Their orientation and outgrowth appears to be responsible for the convergence of the tips of body rods in most S. purpuratus and hybrid embryos, unlike in most L. pictus embryos. Variations among hybrid and natural embryos in skeletal branching pattern reflect differences in interpretation by PMCs of patterning cues produced by the ectodermal epithelium that probably have similar spatial distributions in the two species.     

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.     

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 .     

Analysis of competence in cultured sea urchin micromeres.

Sea urchin embryo micromeres form the primary mesenchyme, the skeleton-producing cells of the embryo. Almost nothing is known about nature and timing of the embryonic cues which induce or initiate spicule formation by these cells. A related question concerns the competence of the micromeres to respond to the cues. To examine competence in this system we have exposed cultured sea urchin micromeres to an inducing medium containing horse serum for various periods of time and have identified a period when micromeres are competent to respond to serum and form spicules. This window, between 30 and 50 h after fertilization, corresponds to the time when mesenchyme cells in vivo are aggregating and beginning to form the syncytium in which the spicule will be deposited. The loss of competence after 50 h is not due to impaired cell health since protein synthesis at this time is not significantly different from controls. Likewise the accumulation of a spicule matrix mRNA (SM 50) and a cell surface glycoprotein (msp 130), both indices of micromere/mesenchyme differentiation, still occurs in cells that have lost competence to respond to serum by forming spicules. These experiments demonstrate that the acquisition and loss of competence in these cells are regulated developmental events and establish an in vitro system for the identification of the molecular basis for inductive signal recognition and signal transduction.     

Model peptide studies of sequence repeats derived from the intracrystalline biomineralization protein, SM50. II. Pro,Asn-rich tandem repeats

In the biomineralization process, a number of Pro-rich proteins participate in the formation of three-dimensional supramolecular structures. One such protein superfamily, the Pro,Gly-rich sea urchin intracrystalline spicule matrix proteins, form protein-protein supramolecular assemblies that modify the microstructure of the inorganic mineral phase (calcite) within embryonic sea urchin spicules and adult sea urchin spines. These proteins represent a useful model for understanding Pro sequence usage and the resulting generation of extended or "open" structures for protein-protein and/or protein-crystal recognition. In the sea urchin spicule matrix protein, SM50 (Strongylocentrotus purpuratus), there exists an unusual 20-residue Pro,Asn-containing repeat, &bond;PNNPNNPNPNNPNNPNNPNPbond which links the upstream 15-residue C-terminal domain and the downstream 211-residue beta-spiral repeat domain. To define the structural preferences of this 20-residue repeat, we created a 20-residue N- and C-terminal "capped" peptidomimetic of this sequence. Using far-uv CD dichroism, CH(alpha) and alpha-(15)N conformational shifts, (3)J(NH-CHalpha) coupling constants, sequential d(NN(i, i + 1)) rotating frame nuclear Overhauser effect connectivities, d(alphaN(i, i + 1))/d(NN(i, i + 1)) intensity ratios, amide temperature shift coefficients, amide solvent exchange, and simulated annealing refinement protocols, we have determined that this 20-residue repeat motif adopts an extended "twist" structure consisting of turn- and coil-like regions. These findings are consistent with previous studies, which have shown that Pro-rich tandem repeats adopt extended, flexible structures in solution. We hypothesize that this 20-residue repeat may fulfill the role of a mineral-binding domain, a protein-protein docking domain, or as an internal "molecular spacer" for the SM50 protein during spicule biocomposite formation.     

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.     

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.     

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.     

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.     

Silica deposition in Demosponges: spiculogenesis in Crambe crambe

Transmission electron-microscopy images coupled with dispersive X-ray analysis of the species Crambe crambe have provided information on the process of silica deposition in Demosponges. Sclerocytes (megasclerocytes) lie close to spicules or surround them at different stages of growth by means of long thin enveloping pseudopodia. Axial filaments occur free in the mesohyl, in close contact with sclerocytes, and are triangular in cross section, with an internal silicified core. The unit-type membrane surrounding the growing spicule coalesces with the plasmalemma. The axial filament of a growing spicule and that of a mature spicule contain 50%-70% Si and 30%-40% Si relative to that contained in the spicule wall, respectively. The extracellular space between the sclerocyte and the growing spicule contains 50%-65%. Mitochondria, vesicles and dense inclusions of sclerocytes exhibit less than 10%. The cytoplasm close to the growing spicule and that far from the growing spicule contain up to 50% and less than 10%, respectively. No Si has been detected in other parts of the sponge. The megascleres are formed extracellularly. Once the axial filament is extruded to the mesohyl, silicification is accomplished in an extracellular space formed by the enveloping pseudopodia of the sclerocyte. Si deposition starts at regularly distributed sites along the axial filament; this may be related to the highly hydroxylated zones of the silicatein-alpha protein. Si is concentrated in the cytoplasm of the sclerocyte close to the plasmalemma that surrounds the growing spicules. Orthosilicic acid seems to be pumped, both from the mesohyl to the sclerocyte and from the sclerocyte to the extracellular pocket containing the growing spicule, via the plasmalemma.     

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.