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.     

Biochemical Composition and Assembly of Biosilica-associated Insoluble Organic Matrices from the Diatom Thalassiosira pseudonana

The nano- and micropatterned biosilica cell walls of diatoms are remarkable examples of biological morphogenesis and possess highly interesting material properties. Only recently has it been demonstrated that biosilica-associated organic structures with specific nanopatterns (termed insoluble organic matrices) are general components of diatom biosilica. The model diatom Thalassiosira pseudonana contains three types of insoluble organic matrices: chitin meshworks, organic microrings, and organic microplates, the latter being described in the present study for the first time. To date, little is known about the molecular composition, intracellular assembly, and biological functions of organic matrices. Here we have performed structural and functional analyses of the organic microrings and organic microplates from T. pseudonana. Proteomics analysis yielded seven proteins of unknown function (termed SiMat proteins) together with five known silica biomineralization proteins (four cingulins and one silaffin). The location of SiMat1-GFP in the insoluble organic microrings and the similarity of tyrosine- and lysine-rich functional domains identifies this protein as a new member of the cingulin protein family. Mass spectrometric analysis indicates that most of the lysine residues of cingulins and the other insoluble organic matrix proteins are post-translationally modified by short polyamine groups, which are known to enhance the silica formation activity of proteins. Studies with recombinant cingulins (rCinY2 and rCinW2) demonstrate that acidic conditions (pH 5.5) trigger the assembly of mixed cingulin aggregates that have silica formation activity. Our results suggest an important role for cingulins in the biogenesis of organic microrings and support the hypothesis that this type of insoluble organic matrix functions in biosilica morphogenesis.     

Analysis of the Proteinaceous Components of the Organic Matrix of Calcitic Sclerites from the Soft Coral Sinularia sp.

An organic matrix consisting of a protein-polysaccharide complex is generally accepted as an important medium for the calcification process. While the role this “calcified organic matrix” plays in the calcification process has long been appreciated, the complex mixture of proteins that is induced and assembled during the mineral phase of calcification remains uncharacterized in many organisms. Thus, we investigated organic matrices from the calcitic sclerites of a soft coral, Sinularia sp., and used a proteomic approach to identify the functional matrix proteins that might be involved in the biocalcification process. We purified eight organic matrix proteins and performed in-gel digestion using trypsin. The tryptic peptides were separated by nano-liquid chromatography (nano-LC) and analyzed by tandem mass spectrometry (MS/MS) using a matrix-assisted laser desorption/ionization (MALDI) – time-of-flight-time-of-flight (TOF-TOF) mass spectrometer. Periodic acid Schiff staining of an SDS-PAGE gel indicated that four proteins were glycosylated. We identified several proteins, including a form of actin, from which we identified a total of 183 potential peptides. Our findings suggest that many of those peptides may contribute to biocalcification in soft corals.     

Soluble organic matrix of two Scleractinian corals: partial and comparative analysis

This study is a biochemical and molecular analysis of the soluble organic matrix (SOM) of two Scleractinian corals differing in their morphological characteristics: Stylophora pistillata, a branched robust coral and Pavona cactus, a leafy complex coral. Soluble organic matrix of both coral species were shown to contain high amounts of potentially acidic amino acids and glycine. However, proportions of glycosaminoglycans and SDS-PAGE analyses of soluble organic matrix proteins were very different. Three proteins of S. pistillata and at least five proteins of P. cactus were detected by silver staining, some of them being able to bind calcium. Internal peptide sequences of two matrix proteins (one from each species) were obtained. One sequence of S. pistillata is unusual because it contains a long poly-aspartate domain, as described in proteins belonging to the calsequestrin family and in proteins from molluscan species. This domain suggests an essential role for this protein in the control of mineralization.     

Hydrophobic proteins of lamellated osmiophilic bodies isolated from pig lung.

1. In addition to proteins that are insoluble in organic solvents, lamellated bodies isolated from pig lung and surfactant prepared from bronchopulmonary lavage fluid contain another group of proteins that are extracted together with lipid into the organic phase. 2. These hydrophobic proteins constitute about 40% of the total protein of lamellated bodies and about 13% of the total protein of surfactant isolated from lavage fluid, whereas less than 1% of the total protein of pig lung microsomal fraction and mitochondria is extracted by organic solvents. 3. The hydrophobic proteins of lamellated bodies were separated into four fractions and freed from phospholipid by chromatographic procedures. Their apparent molecular weights vary between 11 500 and 16 500, they contain 72--79% of hydrophobic residues and 16--22% of sulphur-containing amino-acids, and leucine is the major N-terminal amino acid in each case.     

Die Paläobiochemie,ein neues Arbeitsgebiet der Evolutionsforschung

Attention is focussed on a novel tool to study evolutionary trends in organisms. Emphasis is placed on the comparative biochemistry of shell proteins. It is tentatively concluded that the organic matrix of molluscan shells is predominantly a mixture of “secreted” collagen and k-m-e-f type proteins, and to a lesser extent of mucopolysaccharides. Each species has its characteristic organic pattern. Thus, the heterogeneity of calcified tissues can be related to molluscan phylogeny and evolution.     

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.     

High-energy electron irradiation of proteins and nucleic acids: collisional stopping power and average energy loss

Inactivation of proteins due to the direct action of ionizing radiation and the electron energy loss spectra of organic materials indicate that an average of 60–66 eV of energy is lost from high energy electrons in each inelastic collision with target molecules. The average energy loss per inelastic collision with high energy electrons in solid, carbon-based materials, proteins and nucleic acids is calculated from mass collisional stopping powers and empirical total inelastic cross-sections. Bragg’s Additivity Law is used for the calculation of the mean excitation energy of molecules. For simple organic compounds, the calculated average energy loss is close to that obtained by direct observation of the energy loss suffered by electrons as they pass through thin films of organic material. The density effect correction for the rate of energy loss, important in the more complex case of proteins irradiated with 10 MeV electrons, is determined using the comparable mass collisional stopping power of water and proteins. In this manner, a value is obtained for the average energy per inelastic collision of high energy electrons with proteins, which is similar to the average energy per inactivating event of proteins. Analogous calculations for nucleic acids are also presented.     

Is the “Histone Code” an Organic Code?

Post-translational histone modifications and their biological effects have been described as a ‘histone code’. Independently, Barbieri used the term ‘organic code’ to describe biological codes in addition to the genetic code. He also provided the defining criteria for an organic code, but to date the histone code has not been tested against these criteria. This paper therefore investigates whether the histone code is a bona fide organic code. After introducing the use of the term ‘code’ in biology, the criteria a putative organic code such as the histone code must conform to in order to be recognised as an organic code are described. Our current knowledge of histones and their major post-translational modifications, and the specific protein binding domains that recognise and translate these into specific biological effects, is then reviewed in detail. The histone modification system is then placed in the context of an organic code and it is concluded that it fulfils all the requirements of an organic code. The marks produced on histones by processes such as acetylation and methylation act as organic signs that are translated into unique biological effects, their biological meanings. These translations are accomplished by effector proteins that consist of a binding domain that recognises a specific histone mark and a regulatory domain that mediates the biological effect. Crucially, these domains can be experimentally interchanged between different effector proteins, thus altering the rules that specify the relationships between sign and meaning. The effector proteins therefore fulfil the role of adaptor molecules.     

Denaturation capacity: a new quantitative criterion for selection of organic solvents as reaction media in biocatalysis.

The process of reversible denaturation of several proteins (alpha-chymotrypsin, trypsin, laccase, chymotrypsinogen, cytochrome c and myoglobin) by a broad series of organic solvents of different nature was investigated using both our own and literature data, based on the results of kinetic and spectroscopic measurements. In all systems studied, the denaturation proceeded in a threshold manner, i.e. an abrupt change in catalytic and/or spectroscopic properties of dissolved proteins was observed after a certain threshold concentration of the organic solvent had been reached. To account for the observed features of the denaturation process, a thermodynamic model of the reversible protein denaturation by organic solvents was developed, based on the widely accepted notion that an undisturbed water shell around the protein globule is a prerequisite for the retention of the native state of the protein. The quantitative treatment led to the equation relating the threshold concentration of the organic solvent with its physicochemical characteristics, such as hydrophobicity, solvating ability and molecular geometry. This equation described well the experimental data for all proteins tested. Based on the thermodynamic model of protein denaturation, a novel quantitative parameter characterizing the denaturing strength of organic solvents, called the denaturation capacity (DC), was suggested. Different organic solvents, arranged according to their DC values, form the DC scale of organic solvents which permits theoretical prediction of the threshold concentration of any organic solvent for a given protein. The validity of the DC scale for this kind of prediction was verified for all proteins tested and a large number of organic solvents. The experimental data for a few organic solvents, such as formamide and N-methylformamide, did not comply with equations describing the denaturation model. Such solvents form the group of so-called 'bad' solvents; reasons for the occurrence of 'bad' solvents are not yet clear. The DC scale was further extended to include also highly nonpolar solvents, in order to explain the well-known ability of enzymes to retain catalytic activity and stability in biphasic systems of the type water/water-immiscible organic solvent. It was quantitatively demonstrated that this ability is accounted for by the simple fact that nonpolar solvents are not sufficiently soluble in water to reach the inactivation threshold concentration.     

Comparison of binding of thyroid hormone analogues to hepatic organic anion binding proteins

Dv protein and ligandin are two hepatic cytosolic proteins which bind organic anions, including endogenous thyroid hormones. Binding studies were performed using the ANS displacement technique to compare the binding of a variety of thyroid hormone analogues to purified organic anion binder and ligandin. Inhibition of ANS binding by these compounds was competitive. Both proteins bound L- and D-thyroxine with comparable affinity (Kd 30-45 microM), whereas ligandin bound 3',3',5-triiodo-L-thyronine, 3',3',5-triiodo-L-thyronine and most analogues with greater affinity. Nevertheless, the order of ligand affinities for both binders was highly correlated, suggesting that the nature of the binding site on both proteins is similar. The binding affinities of these organic anion binders are 2-3 orders of magnitude lower than an hepatic cytosolic thyroid binder reported by others, suggesting that ligandin and organic anion binder may not be important in intracellular thyroid hormone transfer.     

Monitoring the Active Conformation of Green Fluorescent Protein (GFP) and β-Glucosidase Adsorbed on Soil Particles

In order to determine the effect of various soil components on the activity of proteins, we monitored the fluorescence and the enzymatic activity of, respectively, green fluorescent protein (GFP) and β-glucosidase adsorbed on fine soil particles. We also monitored the activity of these proteins in the presence of components that are representative of soil colloids: a montmorillonite clay, goethite and organic matter extracted from soil. Upon adsorption on clay and goethite, GFP lost its fluorescence properties while β-glucosidase suffered only a partial loss of its catalytic activity. Extractable organic matter had an inactivating role on GFP while it did not cause inactivation of β-glucosidase. When GFP and β-glucosidase adsorbed on particles from natural soil samples, their behaviour was consistent with the behaviour observed for these proteins in the presence of the separate components, suggesting that the macroscopic activity of proteins adsorbed on soil particles corresponds to an average of the activities of proteins adsorbed on a mixture of surfaces. The monitoring of the proteins on soil particles with different organic matter contents has also shown that organic matter can have different effects (protecting or inactivating) on different proteins.     

Role of proteins in soil carbon and nitrogen storage: controls on persistence

Mechanisms of soil organic carbon (C) and nitrogen (N) stabilization are of great interest, due to the potential for increased CO₂ release from soil organic matter (SOM) to the atmosphere as a result of global warming, and because of the critical role of soil organic N in controlling plant productivity. Soil proteins are recognized increasingly as playing major roles in stabilization and destabilization of soil organic C and N. Two categories of proteins are proposed: detrital proteins that are released upon cell death and functional proteins that are actively released into the soil to fulfill specific functions. The latter include microbial surface-active proteins (e.g., hydrophobins, chaplins, SC15, glomalin), many of which have structures that promote their persistence in the soil, and extracellular enzymes, responsible for many decomposition and nutrient cycling transformations. Here we review information on the nature of soil proteins, particularly those of microbial origin, and on the factors that control protein persistence and turnover in the soil. We discuss first the intrinsic properties of the protein molecule that affect its stability, next possible extrinsic stabilizing influences that arise as the proteins interact with other soil constituents, and lastly controls on accessibility of proteins at coarser spatial scales involving microbial cells, clay particles, and soil aggregates. We conclude that research at the interface between soil science and microbial physiology will yield rapid advances in our understanding of soil proteins. We suggest as research priorities determining the relative abundance and turnover time (age) of microbial versus plant proteins and of functional microbial proteins, including surface-active compounds.     

Interconnection of physico-chemical characteristics of organic solvents and their denaturing ability in relation to proteins]

Reversible denaturation of several proteins (alpha-chymotrypsin, trypsin, laccase, chymotrypsinogen, cytochrome c and myoglobin) by a broad series of organic solvents of different nature was studied. The regularities of this process were analyzed, employing both experimental and literary data based on the results of kinetic and spectroscopic measurements. In all the systems under study denaturation proceeded in a threshold manner, i. e., an abrupt change in the catalytic and/or spectroscopic properties of the dissolved proteins was observed after a certain threshold concentration of the organic solvent had been reached. To account for the observed features of the denaturation process, a thermodynamic model of reversible protein denaturation by organic solvents was proposed. This model is based on the widely accepted viewpoint that the undisturbed water shell around the protein globule is necessary for maintaining the dissolved protein in the native state. Quantitative analysis of the model led to an equation establishing a relationship between the threshold concentration of an organic solvent and its physico-chemical characteristics, such as hydrophobicity, solvating ability and molecular geometry. This equation fits well in the experimental data for all the proteins tested. Based on the above thermodynamic model of protein denaturation, a novel quantitative parameter characterizing the denaturing strength of organic solvents (termed as the denaturation capacity or DC) was proposed. Different organic solvents arranged according to their DC values form the DC scale of organic solvents which permits to predict theoretically the threshold concentration of any organic solvent for a given protein.(ABSTRACT TRUNCATED AT 250 WORDS)     

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.     

Proteomic Strategy for Identifying Mollusc Shell Proteins Using Mild Chemical Degradation and Trypsin Digestion of Insoluble Organic Shell Matrix: A Pilot Study on Haliotis tuberculata

A successful strategy for the identification of shell proteins is based on proteomic analyses where soluble and insoluble fractions isolated from organic shell matrix are digested with trypsin with the aim of generating peptides, which are used to identify novel shell proteins contained in databases. However, using trypsin as a sole degradative agent is limited by the enzyme's cleavage specificity and is dependent upon the occurrence of lysine and arginine in the shell protein sequence. To bypass this limitation, we investigated the ability of trifluoroacetic acid (TFA), a low-specificity chemical degradative agent, to generate clusters of analyzable peptides from organic shell matrix, suitable for database annotation. Acetic acid-insoluble fractions from Haliotis tuberculata shell were processed by trypsin followed by TFA digestion. The hydrolysates were used to annotate an expressed sequence tag library constructed from the mantle tissue of Haliotis asinina, a tropical abalone species. The characterization of sequences with repeat motifs featured in some of the shell matrix proteins benefited from TFA-induced serial cutting, which can result in peptide ladder series. Using the degradative specificities of TFA and trypsin, we were able to identify five novel shell proteins. This pilot study indicates that a mild chemical digestion of organic shell matrix combined with trypsin generates peptides suitable for proteomic analysis for better characterization of mollusc shell matrix proteins.     

Proteomic analysis of the acid-soluble organic matrix of the chicken calcified eggshell layer

The major difference between inorganic minerals and biominerals is the presence of an organic matrix consisting of proteins, glycoproteins, proteoglycans, and polysaccharides, which is synthesized by specialized cells under genetic control before or during mineralization. The organic matrix is thought to play a major role in the assembly of the biomineral and determination of its mechanical properties. The recent elucidation of the chicken genome provided an opportunity to explore the matrix proteome of a biomineral using up-to-date MS-based technology. We identified 520 proteins in this matrix including the ten matrix proteins already known before. The identified proteins were divided into three abundance groups using the exponentially modified protein abundance index described recently which was roughly calibrated with the few known data on protein yield derived from Edman sequence analysis. A small group of 32 highly abundant proteins contained the presently known eggshell-specific proteins and all of the other known eggshell matrix constituents identified before with much less sensitive conventional methods. The present study, which is the first comprehensive proteomic study of a vertebrate biomineral, is intended as a starting point for the detailed molecular characterization of eggshell matrix proteins, their interactions in the matrix network and functional studies.     

Proteomics Analysis of the Nacre Soluble and Insoluble Proteins from the Oyster Pinctada margaritifera

Shell nacre is laid upon an organic cell-free matrix, part of which, paradoxically, is water soluble and displays biological activities. Proteins in the native shell also constitute an insoluble network and offer a model for studying supramolecular organization as a means of self-ordering. Consequently, difficulties are encountered in extraction and purification strategies for protein characterization. In this work, water-soluble proteins and the insoluble conhiolin residue of the nacre of Pinctada margaritifera matrix were analyzed via a proteomics approach. Two sequences homologous to nacre matrix proteins of other Pinctada species were identified in the water-soluble extract. One of them is known as a fundamental component of the insoluble organic matrix of nacre. In the conchiolin, the insoluble residue, four homologs of Pinctada nacre matrix proteins were found. Two of them were the same as the molecules characterized in the water-soluble extract. Results established that soluble and insoluble proteins of the nacre organic matrix share constitutive material. Surprisingly, a peptide in the conchiolin residue was found homologous to a prismatic matrix protein of Pinctada fucata, suggesting that prismatic and nacre matrices may share common proteins. The insoluble properties of shell matrix proteins appear to arise from structural organization via multimerization. The oxidative activity, found in the water-soluble fraction of the nacre matrix, is proposed as a leading process in the transformation of transient soluble proteins into the insoluble network of conchiolin during nacre growth.     

Plant Cellular Osmotica

To cope with the water deficit resulting from saline environment, plant cells accumulate three kinds of osmotica: salts, small organic solutes and hydrophillic, glycine-rich proteins. Salts such as NaCl are cheap and available but has ion toxicity in high concentrations. Small organic solutes are assistant osmotica, their main function is to protect cytoplasmic enzymes from ionic toxicity and maintain the integrity of cellular membranes. Hydrophillic, glycine-rich proteins are the most effective osmotica, they have some characteristics to avoid crystallization even in high concentration, but because they are expensive they are not as commonly used as salts or organic solutes. In addition there is the question of whether the genetic information for growth in saline environment is present in all kinds of plants, both halophytes and nonhalophytes.     

EVIDENCE OF AN ORGANIC MATRIX FROM DIATOM BIOSILICA1

Most biominerals appear to be composites of organic material and mineral. Whether biosilica is such a composite is unresolved because of a lack of evidence for such organic components. We present evidence that organic material exists within diatom biosilica and can be extracted using HF/NH₄F solutions from frustules isolated from Cyclotella meneghiniana Kütz and diatomaceous earth. To eliminate organic casing on the silicified frustules as a source of organic materials, the casing was removed by oxidation of frustules with NaOCl before extraction. The removal of the casing was confirmed in that oxidized frustules no longer displayed the ability to be stained with ruthenium red and fluorescamine. Frustules examined with EDXA showed an emission peak from sulfur before treatment but no peak following treatment, indicating that oxidation removed organic sulfur. The organic material obtained from extracts of fresh frustules contained both soluble and insoluble components. Only soluble material was evident in extracts from diatomaceous earth. The soluble material appears to contain glycoproteins with relatively high levels of serine and glycine. The soluble proteins from fresh frustules also appear to be phosphorylated. Indirect evidence is presented that suggests the soluble proteins may contain regions of primary structure enriched in anionic amino acids. The soluble extracts differ from general cell contents when the two fractions are compared, suggesting that frustules contain specialized organic material. The identification of silica-specific organic material suggests that mineralization in diatoms may be in part matrix-mediated.