Regulation of CaCO(3) formation in coccolithophores.

Coccolithophores impact the ocean carbon cycle principally through the generation of CO(2) during CaCO(3) production. Coccolithophore biomineralization has been examined most extensively in Pleurochrysis carterae and Emiliania huxleyi both of which produce mineralized scales-coccoliths-composed of elaborate calcite crystals attached to an underlying organic base plate. Calcification of preformed base plates is mediated by acidic polysaccharides and occurs in Golgi-derived structures known as mineralizing vesicles. In Pleurochrysis a high capacity calcium-binding polysaccharide PS2 is required for efficient nucleation of calcitic protocrystals. A galacturonomannan PS3 is required for the growth and transformation of the protocrystals into a massive double disc of calcite. The genes that regulate expression of the glycans have not yet been identified. In addition to the coccolith-bearing diploid phases, Pleurochrysis and Emiliania possess both haploid and diploid non-calcifying stages, which are self-perpetuating via binary fission. One non-calcifying Pleurochrysis phase fails to synthesis PS2 and spontaneously reverts to the mineralizing morphotype in laboratory cultures. As yet, there is little information on environmental factors that effect the expression or silencing of calcifying genes or favor the growth of calcifying over non-calcifying phases. These issues will need extensive investigation, if we are to appreciate the role of coccolithophores in the regulation of atmospheric CO(2) levels.

Galacturonomannan and Golgi-derived membrane linked to growth and shaping of biogenic calcite.

The coccolithophores are valuable models for the design and synthesis of composite materials, because the cellular machinery controlling the nucleation, growth, and patterning of their calcitic scales (coccoliths) can be examined genetically. The coccoliths are formed within the Golgi complex and are the major CaCO(3) component in limestone sediments-particularly those of the Cretaceous period. In this study, we describe mutants lacking a sulfated galacturonomannan and show that this polysaccharide in conjunction with the Golgi-derived membrane is directly linked to the growth and shaping of coccolith calcite but not to the initial orientated nucleation of the mineral phase.

Prisonomics and the use of psychotropic drugs on incarcerated offenders: ethical considerations.

The authors discuss the ethical considerations involved in using psychotropic medications with incarcerated offenders. Medications cannot be used as tool of oppression. Medication cannot be used to justify overpopulation, to quietly terminate prisoners, and must be administered by licensed health professionals. There must be informed consent.

Biomineralization in coccolithophores.

Unicellular marine algae known as coccolithophores are potentially important organisms for the study of gravitational effects on biomineralization. The cells are easily cultured under low maintenance conditions and produce intricately sculpted calcite scales known as coccoliths in specialized Golgi-derived vesicles. Many mutants are available with different types of mineral defects ranging from the complete absence of mineral to the presence of mineral with orientational, morphological, number, and size defects. This short review summarizes what is currently known about the three phases of coccolith mineralization--mineral ion transport, mineral nucleation, and crystal growth--in Pleurochrysis carterae and Emiliania huxleyi in the earth's normal gravitational field.

Mineralization of bone-like extracellular matrix in the absence of functional osteoblasts.

When grown in medium containing ascorbic acid and beta-glycerol phosphate, mouse MC3T3-E1 cells express an osteoblast phenotype and produce a highly mineralized extracellular matrix. The purpose of this study was to independently examine the role of the collagenous matrix and functional osteoblasts on the mineralization process. Cultures with and without an extensive collagenous matrix were prepared by growing MC3T3-E1 cells in the presence and absence of ascorbic acid. Matrix-rich cultures mineralized at much lower calcium phosphate ion products than nonmatrix cultures. At higher ion products, spontaneous precipitation in the medium and cell layers of nonmatrix cultures were observed. In contrast, mineral in matrix-rich cultures was still exclusively associated with collagen fibrils and not with ectopic sites in the cell layer or medium. To examine the effect of cell viability on matrix mineralization, cells were grown 8 or 16 days in the presence of ascorbic acid, then killed and incubated in a mineralizing medium. Significant mineralization was not observed in the collagenous matrix of 8-day killed cultures or age-matched controls. At 16 days mineral was associated with collagen fibrils at specific foci in the matrix of both viable and killed cultures. This observation is consistent with the concept that collagenous matrices must undergo a maturation process before they can support a mineral induction and growth. It further shows that osteoblast-like cells are not required for mineralization of mature matrices, but are required for matrix maturation.

Isolation and characterization of a novel acidic polysaccharide containing tartrate and glyoxylate residues from the mineralized scales of a unicellular coccolithophorid alga Pleurochrysis carterae.

The characterization of mineral-associated polyanions from the unicellular alga Pleurochrysis carterae is described. This species is useful for the study of mineralization, because it produces calcified scales known as coccoliths in homogeneous cell culture. Three acidic polysaccharides (PS-1, PS-2, and PS-3) were extracted from the coccoliths with EDTA and were separated and purified by differential precipitation with magnesium ions and chromatography on DEAE-cellulose. PS-1 and PS-3 are predominantly polymers of galacturonic acid containing lesser amounts of other monosaccharides. PS-2 has an unusual structure. Chemical, enzymatic, and two-dimensional NMR analyses demonstrate that the repeating unit of PS-2 is [----4)D-glucuronate(beta 1----2)meso-tartrate(3----1)glyoxylate(1-]n. Thus PS-2 has a high density of negatively charged groups available for calcium ion binding, similar to the phosphoprotein polyanions of other species. Polysaccharides containing tartrate and/or glyoxylate have not been previously described; these residues may be introduced into PS-2 by a postpolymerization process involving oxidative cleavage of glucuronate or mannuronate residues.

Immunocytochemical localization of a calcium-binding phosphoprotein in hemocytes of heterodont bivalves.

Calcium-binding phosphoprotein particles are the most abundant extracellular proteins in the hemolymph of heterodont bivalves, and granular hemocytes are the most abundant cells in the same fluid. In this study, the hemocytes of Rangia cuneata were examined ultrastructurally and probed with anti-phosphoprotein IgG to demonstrate that the granulocytes are a probable source of the hemolymph phosphoprotein. The granulocyte cytoplasm is laden with large vesicles containing an amorphous homogenous matrix and variable numbers of electron-dense particles; the latter are ultrastructurally similar to the extracellular phosphoprotein. The vesicle particles and matrix are related forms of the hemolymph phosphoprotein as evidenced by heavy gold labeling when Lowicryl sections were sequentially treated with rabbit-anti-phosphoprotein IgG and colloidal gold-anti-rabbit IgG. The vesicles may be the loci for posttranslational phosphorylation and eventual secretion of the calcium-binding phosphoprotein, or alternatively the vesicles may be digestive structures which degrade internalized phosphoprotein.

Binding of calcium and phosphate ions to dentin phosphophoryn.

The concomitant binding of calcium and inorganic phosphate ions by the highly phosphorylated rat dentin phosphophoryn (HP) was measured in the pH range of 7.4-8.5 using an ultrafiltration procedure. HP binds almost exclusively the triply charged PO4(3-)ion, and for each PO4(3-)ion bound, the protein binds about 1.5 additional Ca2+ ions. The protein-mineral ion complex can be described as a protein with two different ligands, Ca2+ ions and calcium phosphate clusters having a stoichiometry of about Ca1.5PO4. The stoichiometry of the bound clusters is similar to amorphous calcium phosphate, indicating that the protein does not sequester crystal embryos of octacalcium phosphate or hydroxyapatite. The protein-mineral ion complex is amorphous by electron diffraction analysis and does not catalyze the formation of a crystalline phase when aged in contact with its solution.

Self-association of calcium and magnesium complexes of dentin phosphophoryn.

Self-association of rat dentin phosphophoryn in the presence of calcium and magnesium ions was examined by chemical cross-linking and electron microscopy. Highly phosphorylated phosphophoryn (HP) binds a maximum of 1.33 calcium ions or 1.07 magnesium ions per organic phosphate residue at pH 7.4-8.0. The Ca-HP complexes are predominantly linear when the calcium content of the complex is less than about 65% of the saturation level. At higher calcium levels, the protein has a folded conformation, and transient protein-protein interactions occur. The equilibrium mixture of monomers and oligomers is predominantly monomeric unless the protein is saturated with calcium. The saturated Ca-HP complex forms discrete high molecular weight particles about 25 nm in diameter. The particles are electrically neutral and generally occur in clusters. Mg-HP complexes appear predominantly linear by electron microscopy at all concentrations of bound magnesium up to about 99% of the saturation level; however, protein-protein interaction is measurable when the magnesium content is as little as 65% of the saturation level. At saturation, Mg-HP complexes form high molecular weight particles which are negatively charged. Because of the negative charge, these particles form a stable colloidal suspension and have a rather stellate configuration.

Binding of calcium and phosphate ions to dentin phosphophoryn.

The concomitant binding of calcium and inorganic phosphate ions by the highly phosphorylated rat dentin phosphophoryn (HP) was measured in the pH range of 7.4-8.5 by an ultrafiltration procedure. HP binds almost exclusively the triply charged PO4(3-) ion, and for each PO4(3-) ion bound, the protein binds about 1.5 additional Ca2+ ions. Therefore, the protein-mineral ion complex can be described as a protein with two different ligands, Ca2+ ions and calcium phosphate clusters having a stoichiometry of about Ca1.5PO4. Empirically the binding of calcium and phosphate can best be described as a function of a neutral ion activity product in which 2.5-10% of the phosphate is HPO4(2-). The stoichiometry of the bound clusters is similar to that of amorphous calcium phosphate, and it is clear that the protein does not sequester crystal embryos of octacalcium phosphate or hydroxyapatite. The protein-mineral ion complex is amorphous by electron diffraction analysis and does not catalyze the formation of a crystalline phase when aged in contact with its solution. About 15% of the bound phosphate is buried in protected domains, and it is stable with respect to dissociation for extended periods in phosphate-free calcium buffers. The buried mineral maintains the protein in an aggregated state even at calcium ion concentrations which are too low for the aggregation of unmineralized HP. In vivo HP should be ineffective in the nucleation of a crystalline mineral phase, if it is secreted in a mineralized aggregated state similar to casein and the bivalve phosphoprotein.

Biomineralization in the presence of calcium-binding phosphoprotein particles.

The innermost shell lamella, which coats the inner surface of the shells in the estuarine clam Rangia cuneata, is a dynamic structure with a variable composition. In some populations the lamella is a phosphoprotein-rich structure devoid of crystalline mineral, and in others it is a glucosamine-rich structure often containing barite (BaSO4) inclusions. Mineral depositions was artificially stimulated in Rangia containing glucosamine-rich lamellae by scratching the inner shell surface. After stimulation, the lamellae were transformed into phosphoprotein-rich structures in which aragonite (CaCO3) was deposited. The mineral grew in spherulitic and dumbbell-shaped clusters characteristic of aragonite precipitated from strictly inorganic solutions. This study demonstrates that phosphoprotein particles accumulate in the innermost shell lamella during stimulated biomineralization but neither inhibit mineral deposition nor influence the crystal habits. Since phosphoprotein particles are high capacity calcium-binding proteins, they may be the source and transport vehicle for the calcium ions utilized in shell mineralization.

Histidinoalanine, a naturally occurring cross-link derived from phosphoserine and histidine residues in mineral-binding phosphoproteins.

Native mineral-containing phosphoprotein particles were isolated from the Heterodont bivalve Macrocallista nimbosa. The native particles are discrete structures about 40 nm in diameter which migrate as a single band during electrophoresis in agarose gels. Removal of the mineral component with ethylenediaminetetraacetic acid dissociates the native protein into nonidentical subunits. The lower molecular weight subunits, representing 8% of the total protein, were obtained by differential centrifugation. The native protein is characterized by a high content of aspartic acid, phosphoserine, phosphothreonine, histidine, and the bifunctional cross-linking residue histidinoalanine. The low molecular weight subunits have the same amino acid composition except for a reduction in histidinoalanine and a corresponding increase in phosphoserine and histidine residues, demonstrating that the alanine portion of the cross-link is derived from phosphoserine residues. Ion-exchange chromatography and molecular sieve chromatography show that the low molecular weight subunits have a similar charge density but differ in molecular weight, and the relative mobilities of the subunits on agarose gels indicate that they are polymers of a single phosphoprotein molecule. The minimum molecular weight of the monomer is about 140 000 on the basis of the amino acid composition. The high molecular weight subunits are rich in histidinoalanine and too large to be resolved by either molecular sieve chromatography or gel electrophoresis. On the basis of the ultrastructural, electrophoretic, chromatographic, and compositional evidence, native phosphoprotein particles are composed of subunits ionically cross-linked via divalent cations. These subunits are variable molecular weight aggregates of a single phosphoprotein molecule covalently cross-linked via histidinoalanine residues. Evidence for a nonenzymatic cross-linking mechanism is discussed.

Controlled studies of a new microprocessor-based portable infusion pump.

A new microprocessor-controlled portable infusion pump, the Pancretec Provider IV 2000 TM was tested in vitro and in vivo in cancer patients. The Provider is a rotary peristaltic, battery-powered pump capable of flow rates of 0.2 to 83 ml/hour with delivery volumes up to 1999 ml. Two programming modes are available: intermittent infusion and continuous infusion. Bench tests showed the flow rate accuracy to be within 96% of the desired rate. Flow rate precision was similarly excellent at +/- 2%. Clinical studies were performed in 14 ambulatory patients receiving continuous infusion antineoplastic or analgesic drugs over 5-60 days as outpatients. The majority of infusions delivered fluoropyrimidines via indwelling central venous access ports. Two of the patients received long term (60 days) continuous infusion of analgesics for pain control. Flow rate accuracy with the pumps was within +/- 5% in 90% of the 27 infusion courses (244 patient-days of continuous infusion therapy). A significant therapy deviation (interruption 10% of the desired course) occurred in three instances. One related to a procedural error (incomplete cartridge insertion into the pump), two were caused by fluid leakage which interrupted pump function. Defect alarms (both visual and audible) operated in both instances. A KVO flow rate of 0.1 ml/hr was also found to be adequate to maintain catheter patency in peripheral veins over a 24-hour period in two normal volunteers. We conclude that the Provider pump is an accurate, reliable and state of the art infusion system with wide clinical applicability.

Distribution and characterization of mineral-binding phosphoprotein particles in Bivalvia.

Representative species of four bivalve subclasses were examined for the presence of mineral-binding phosphoprotein particles in the physiological fluids. The particles were identified in Heterodont bivalves only, and particles from nine different Heterodont species were isolated and characterized. All phosphoprotein particles are internally cross-linked via histidinoalanine residues. In all species over 80% of the amino acid residues in the particles are aspartic acid, phosphoserine (and/or phosphothreonine), and histidine. These amino acids are probably the only residues directly related to mineral ion binding, since all phosphoprotein particles bind mineral irrespective of the minor amino acid content, which is species dependent. In their native state the phosphoprotein particles contain large amounts of calcium, magnesium, and inorganic phosphate ions (up to 45 metal ions and 8 phosphate ions per 100 amino acid residues) and trace amounts of transition elements. Evidence for the presence of calcium phosphate complexes in the native phosphoprotein particles was obtained by observing a concomitant increase in the inorganic phosphate and calcium ion content of the particles with pH in vivo.

Phosphoprotein particles: calcium and inorganic phosphate binding structures.

Phosphoprotein particles were isolated in their native state from the physiological fluid of the estuarine clam Rangia cuneata , and the characteristics of the mineral ion-protein complex which constitutes the native particle were investigated by using mineral ion binding and mineral ion exchange techniques. The particles are aspartic acid rich, highly phosphorylated proteins containing calcium, magnesium, and inorganic phosphate ions and covalently cross-linked via histidinoalanine residues. Twenty-nine percent of the amino acid residues are phosphorylated. In their native state, the particles contain a protected pool of calcium and inorganic phosphate ions and an exchangeable pool of calcium and magnesium ions. The Ca/PO4 ratio in the protected pool is about 2.5. The number of binding sites for the protected mineral is unknown, but on the average, the native particles contain about 0.2 inorganic phosphate ion per organic phosphate residue. There is 1.0 exchangeable metal ion binding site per organic phosphate residue, and there is probably a phosphoserine residue at each site. These sites bind calcium with an apparent binding constant (KCa) of 4 X 10(3) M-1 at 50% saturation under physiological conditions, and KCa/ KMg is about 1.6. In vivo, about 85% of the exchangeable sites are occupied. The total number of calcium ion binding sites (N) in the phosphoprotein particles is related to the number of organic phosphate residues (Po) and the number of bound inorganic phosphate ions (Pi) by the equation N = Po + 2. 5Pi . The phosphoprotein particles probably serve as both the transporter and reserve source of calcium ions for shell development.

Hepatic microsomal activities of cholesterol 7 alpha-hydroxylase and 3-hydroxy-3-methylglutaryl-CoA reductase in the prairie dog. An animal model for cholesterol gallstone disease.

The prairie dog is a useful experimental animal model for studies of cholesterol gallstone pathogenesis. The unique susceptibility to rapid induction of gallstones solely by feeding of a 1.2% cholesterol diet in this species could result from low levels of hepatic cholesterol 7 alpha-hydroxylase. With optimal assay conditions in hepatic microsomes, a basal specific activity of about 25 pmol/min per g protein was found. Administration of diets containing 1.2% cholesterol or 5% cholestyramine caused hydroxylase levels to increase 60 and 250%, respectively. This response pattern is similar to that observed in other species under the same conditions, indicating that abnormally low basal or inappropriately unresponsive hydroxylase levels are not susceptibility factors unique to this model. With optimal assay conditions for hydroxymethylglutaryl-CoA reductase, a Km of 32.5 microM (S-HMG-CoA) and basal specific activities of between 60 and 175 pmol/min per mg protein were found. Following feeding of either sodium chenodeoxycholate or sodium cholate, in reasonable pharmacologic doses, no suppression of hydroxylase and reductase levels was found. These findings undermine the widely held view that the therapeutic effect of oral chenodeoxycholate in man for cholesterol gallstone dissolution is directly mediated by suppression of the activities of these enzymes.

Ntau- and Npi-histidinoalanine: naturally occurring cross-linking amino acids in calcium-binding phosphoproteins.

Two isomeric amino acid cross-links, Ntau-histidinoalanine and Npi-histidinoalanine have been isolated from calcium-binding phosphoprotein particles derived from the extrapallial fluid of the estuarine clam Rangia cuneata. The cross-links were identified and compared by 13C and 1H NMR spectroscopy and mass spectroscopy. In the phosphoprotein particles, 6% of the amino acid residues are involved in cross-linkages. This is the first demonstration of the occurrence of the isomer Npi-histidinoalanine.