Biophysical characterization of lithostathine. Evidences for a polymeric structure at physiological pH and a proteolysis mechanism leading to the formation of fibrils.

Lithostathine is a calcium carbonate crystal habit modifier. It is found precipitated under the form of fibrils in chronic calcifying pancreatitis or Alzheimer's disease. In order to gain better insight into the nature and the formation of fibrils, we have expressed and purified recombinant lithostathine. Analytical ultracentrifugation and quasi-elastic light scattering techniques were used to demonstrate that lithostathine remains essentially monomeric at acidic pH while it aggregates at physiological pH. Analysis of these aggregates by electron microscopy showed an apparently unorganized structure of numerous monomers which tend to precipitate forming regular unbranched fibrils. Aggregated forms seem to occur prior to the apparition of fibrils. In addition, we have demonstrated that these fibrils resulted from a proteolysis mechanism due to a specific cleavage of the Arg(11)-Ile(12) peptide bond. It is deduced that the NH(2)-terminal undecapeptide of lithostathine normally impedes fiber formation but not aggregation. A theoretical model explaining the formation of amyloid plaques in neurodegenerative diseases or stones in lithiasis starting from lithostathine is described. Therefore we propose that lithostathine, whose major function is unknown, defines a new class of molecules which is activated by proteolysis and is not involved in cytoskeleton nor intermediate filament functions.     

Direct observation of the transition from calcite to aragonite growth as induced by abalone shell proteins

The mixture of EDTA-soluble proteins found in abalone nacre are known to cause the nucleation and growth of aragonite on calcite seed crystals in supersaturated solutions of calcium carbonate. Past atomic force microscope studies of the interaction of these proteins with calcite crystals did not observe this transition because no information about the crystal polymorph on the surface was obtained. Here we have used the atomic force microscope to directly observe changes in the atomic lattice on a calcite seed crystal after the introduction of abalone shell proteins. The observed changes are consistent with a transition to (001) aragonite growth on a (1014) calcite surface.     

Characterization of two molluscan crystal-modulating biomineralization proteins and identification of putative mineral binding domains

Ethylenediamine-tetraacetic acid extracted water-soluble matrix proteins in molluscan shells secreted from the mantle epithelia are believed to control crystal nucleation, morphology, orientation, and phase of the deposited mineral. Previously, atomic force microscopy demonstrated that abalone nacre proteins bind to growing step edges and to specific crystallographic faces of calcite, suggesting that inhibition of calcite growth may be one of the molecular processes required for growth of the less thermodynamically stable aragonite phase. Previous experiments were done with protein mixtures. To elucidate the role of single proteins, we have characterized two proteins isolated from the aragonitic component of nacre of the red abalone, Haliotis rufescens. These proteins, purified by hydrophobic interaction chromatography, are designated AP7 and AP24 (aragonitic protein of molecular weight 7 kDa and 24 kDa, respectively). Degenerate oligonucleotide primers corresponding to N-terminal and internal peptide sequences were used to amplify cDNA clones by a polymerase chain reaction from a mantle cDNA library; the deduced primary amino acid sequences are presented. Preliminary crystal growth experiments demonstrate that protein fractions enriched in AP7 and AP24 produced CaCO(3) crystals with morphology distinct from crystals grown in the presence of the total mixture of soluble aragonite-specific proteins. Peptides corresponding to the first 30 residues of the N-terminal sequences of both AP7 and AP24 were generated. The synthetic peptides frustrate the progression of step edges of a growing calcite surface, indicating that sequence features within the N-termini of AP7 and AP24 include domains that interact with CaCO(3). CD analyses demonstrate that the N-terminal peptide sequences do not possess significant percentages of alpha-helix or beta-strand secondary structure in solution. Instead, in both the presence and absence of Ca(II), the peptides retain unfolded conformations that may facilitate protein-mineral interaction.     

Perlwapin, an abalone nacre protein with three four-disulfide core (whey acidic protein) domains, inhibits the growth of calcium carbonate crystals

We have isolated a new protein from the nacreous layer of the shell of the sea snail Haliotis laevigata (abalone). Amino acid sequence analysis showed the protein to consist of 134 amino acids and to contain three sequence repeats of approximately 40 amino acids which were very similar to the well-known whey acidic protein domains of other proteins. The new protein was therefore named perlwapin. In addition to the major sequence, we identified several minor variants. Atomic force microscopy was used to explore the interaction of perlwapin with calcite crystals. Monomolecular layers of calcite crystals dissolve very slowly in deionized water and recrystallize in supersaturated calcium carbonate solution. When perlwapin was dissolved in the supersaturated calcium carbonate solution, growth of the crystal was inhibited immediately. Perlwapin molecules bound tightly to distinct step edges, preventing the crystal layers from growing. Using lower concentrations of perlwapin in a saturated calcium carbonate solution, we could distinguish native, active perlwapin molecules from denaturated ones. These observations showed that perlwapin can act as a growth inhibitor for calcium carbonate crystals in saturated calcium carbonate solution. The function of perlwapin in nacre growth may be to inhibit the growth of certain crystallographic planes in the mineral phase of the polymer/mineral composite nacre.     

Crystal structure of human lithostathine, the pancreatic inhibitor of stone formation.

Human lithostathine (HLIT) is a pancreatic glycoprotein which inhibits the growth and nucleation of calcium carbonate crystals. The crystal structure of the monomeric 17 kDa HLIT, determined to a resolution of 1.55 angstroms, was refined to a crystallographic R-factor of 18.6%. Structural comparison with the carbohydrate-recognition domains of rat mannose-binding protein and E-selectin indicates that the C-terminal domain of HLIT shares a common architecture with the C-type lectins. Nevertheless, HLIT does not bind carbohydrate nor does it contain the characteristic calcium-binding sites of the C-type lectins. In consequence, HLIT represents the first structurally characterized member of this superfamily which is not a lectin. Analysis of the charge distribution and calculation of its dipole moment reveal that HLIT is a strongly polarized molecule. Eight acidic residues which are separated by regular 6 angstrom spacings form a unique and continuous patch on the molecular surface. This arrangement coincides with the distribution of calcium ions on certain planes of the calcium carbonate crystal; the dipole moment of HLIT may play a role in orienting the protein on the crystal surface prior to the more specific interactions of the acidic residues.     

Polysaccharide from coccoliths (CaCO3 biomineral). Influence on crystallization of calcium oxalate monohydrate

A polysaccharide associated with coccoliths of the marine alga Emiliania huxleyi (coccoliths are elaborately shaped calcite biominerals) was isolated and its influence on the crystallization of calcium oxalate monohydrate crystals was studied. Crystallization was monitored in a carefully controlled system by measuring the incorporation of 45Ca tracer from a supersaturated solution into seed crystals of calcium oxalate monohydrate in the absence and in the presence of polysaccharide. The method allowed differentiation between effects on solubility, growth and agglomeration of crystals. At the very low concentrations used in this study, the polysaccharide had no significant effect on the solubility product; it strongly inhibited the growth and strongly stimulated the agglomeration of the crystals. Thus, the two processes of growth and agglomeration, being both crystal-surface-related processes, may react in opposite directions upon surface adhesion of the additive. This finding opens new insights on how a mineralization process may be controlled. The inhibitory effect on growth is shown to proceed through a monolayer type of adsorption of the polysaccharide onto the crystal surface. The portion of the polysaccharide used for the stimulatory effect on agglomeration shows a different type of adsorption, whereby less crystal surface is covered per molecule of polysaccharide. This strongly suggests, that the mechanism whereby agglomeration is stimulated operates through 'viscous binding', with the polysaccharide bridging the gap between two crystal surfaces. In the discussion these findings are related to some possible biological functions of the polysaccharide.     

Three complete turns of a 3(10)-helix at atomic resolution: the crystal structure of Z-(Aib)11-OtBu.

The crystal structure of the synthetic protected oligopeptide Z-(Aib)11-OtBu was determined by x-ray crystallography. The undecapeptide folds in a regular 3(10)-helix with nine consecutive 4 --> 1 hydrogen bonds. At present, this is the largest available structure of a homopeptide (including homopeptides consisting of standard amino acids) and also the longest observed regular 3(10)-helix at atomic resolution. Z-(Aib)11-OtBu crystallizes readily from hot ethanol-water mixture and is one of the crystals in which no solvent molecule is co-crystallized. In the crystal head-to-tail hydrogen bonded columns are formed in the [1 0 1] direction. Each helical column is surrounded by six others, whereby two are packed in parallel and four in antiparallel fashion. Helical columns are packed via apolar crystal contacts. The crystal structure of Z-(Aib)11-OtBu is compared with the crystal structures of Z-(Aib)10-OtBu and Z-(Aib)9-OtBu. The similarities and differences are analysed.     

Helix bending in alamethicin: molecular dynamics simulations and amide hydrogen exchange in methanol

Molecular dynamics simulations of alamethicin in methanol were carried out with either a regular alpha-helical conformation or the x-ray crystal structure as starting structures. The structures rapidly converged to a well-defined hydrogen-bonding pattern with mixed alpha-helical and 3(10)-helical hydrogen bonds, consistent with NMR structural characterization, and did not unfold throughout the 1-ns simulation, despite some sizable backbone fluctuations involving reversible breaking of helical hydrogen bonds. Bending of the helical structure around residues Aib10-Aib13 was associated with reversible flips of the peptide bonds involving G11 (Aib10-G11 or G11-L12 peptide bonds), yielding discrete structural states in which the Aib10 carbonyl or (rarely) the G11 carbonyl was oriented away from the peptide helix. These peptide bond reversals could be accommodated without greatly perturbing the adjacent helical structure, and intramolecular hydrogen bonding was generally maintained in bent states through the formation of new (non-alpha or 3[10]) hydrogen bonds with good geometries: G11 NH-V9 CO (inverse gamma turn), Aib13 NH-Aib8 CO (pi-helix) and, rarely, L12 NH- Q7 NH (pi-helix). These observations may reconcile potentially conflicting NMR structural information for alamethicin in methanol, in which evidence for conformational flexibility in the peptide sequence before P14 (G11-Aib13) contrasts with the stability of backbone amide NH groups to exchange with solvent. Similar reversible reorientation of the Thr11-Gly12 peptide bond of melittin is also observed in dynamics simulations in methanol (R. B. Sessions, N. Gibbs, and C. E. Dempsey, submitted). This phenomenon may have some role in the orientation of the peptide carbonyl in solvating the channel lumen in membrane ion channel states of these peptides.     

Energetics and cooperativity of the hydrogen bonding and anchor interactions that bind peptides to MHC class II protein

The complexity of the interaction between major histocompatibility complex class II (MHC II) proteins and peptide ligands has been revealed through structural studies and crystallographic characterization. Peptides bind through side-chain "anchor" interactions with MHC II pockets and an extensive array of genetically conserved hydrogen bonds to the peptide backbone. Here we quantitatively investigate the kinetic hierarchy of these interactions. We present results detailing the impact of single side-chain mutations of peptide anchor residues on dissociation rates, utilizing two I-A(d)-restricted peptides, one of which has a known crystal structure, and 24 natural and non-natural amino acid mutant variants of these peptides. We find that the N-terminal P1, P4 and P6 anchor-pocket interactions can make significant contributions to binding stability. We also investigate the interactions of these peptides with four I-A(d) MHC II proteins, each mutated to disrupt conserved hydrogen bonds to the peptide backbone. These complexes exhibit kinetic behavior suggesting that binding energy is disproportionately invested near the peptide N terminus for backbone hydrogen bonds. We then evaluate the effects of simultaneously modifying both anchor and hydrogen bonding interactions. A quantitative analysis of 71 double mutant cycles reveals that there is little apparent cooperativity between anchor residue interactions and hydrogen bonds, even when they are directly adjacent (<5A).     

Carbonate crystal growth controlled by interfacial interactions of artificial cell membranes

Morphology of carbonate crystals grown on the surface of artificial cell membranes was controlled by changing the interfacial chemistry. For octadecyltriethoxysilane (OTE) films with terminal methyl groups interacting little with an aqueous calcium carbonate solution, calcite (104) crystals were formed. Polymerized pentacosadiynoic acid (PDA) films with terminal carboxylic acid groups induced deposition of calcite (012) crystals aligned along with each other within a polymer domain. On the other hand, stearyl alcohol (StOH) films with terminal hydroxyl groups induced deposition of aragonite crystals. When PDA was mixed with StOH, the 8∶1 PDA∶StOH (molar ratio) film produced dominating calcite (012) crystals without any crystal alignment, and the 4∶1 mixture film produced minor calcite (012) crystals and major aragonite crystals. For the 2∶1, 1∶1, 1∶2, and 1∶4 mixture films, aragonite crystals were dominating. Hence, it is found that the chemical composition at the interface plays a very important role in controlling the morphology of deposited carbonate crystals.     

Modular design of synthetic protein mimics. Characterization of the helical conformation of a 13-residue peptide in crystals

The incorporation of alpha-aminoisobutyryl (Aib) residues into peptide sequences facilitates helical folding. Aib-containing sequences have been chosen for the design of rigid helical segments in a modular approach to the construction of a synthetic protein mimic. The helical conformation of the synthetic peptide Boc-Aib-(Val-Ala-Leu-Aib)3-OMe in crystals is established by X-ray diffraction. The 13-residue apolar peptide adopts a helical form in the crystal with seven alpha-type hydrogen bonds in the middle and 3(10)-type hydrogen bonds at either end. The helices stack in columns, zigzag rather than linear, by means of direct NH...OC head to tail hydrogen bonds. Leucyl side chains are extended on one side of the helix and valyl side chains on the other side. Water molecules form hydrogen bonds with several backbone carbonyl oxygens that also participate in alpha-helix hydrogen bonds. There is no apparent distortion of the helix caused by hydration. The space group is P2(1)2(1)2(1), with a = 9.964 (3) A, b = 20.117 (3) A, c = 39.311 (6) A, Z = 4, and dx = 1.127 g/cm3 for C64H106N13O16.1.33H2O. The final agreement factor R was 0.089 for 3667 data observed greater than 3 sigma(F) with a resolution of 0.9 A.     

CaCO3 biomineralization: acidic 8-kDa proteins isolated from aragonitic abalone shell nacre can specifically modify calcite crystal morphology

Acidic proteins from many biogenic minerals are implicated in directing the formation of crystal polymorphs and morphologies. We characterize the first extremely acidic proteins purified from biomineralized aragonite. These abalone nacre proteins are two variants of 8.7 and 7.8 kDa designated AP8 (for aragonite proteins of approximately 8 kDa). The AP8 proteins have compositions dominated by Asx ( approximately 35 mol %) and Gly ( approximately 40 mol %) residues, suggesting that their structures have high Ca(2+)-binding capacity and backbone flexibility. The growth of asymmetrically rounded CaCO(3) crystals in the presence of AP8 reveals that both proteins preferentially interact with specific locations on the crystal surface. In contrast, CaCO(3) crystals grown with nacre proteins depleted of AP8 retain the morphology of unmodified calcite rhombohedra. Our observations thus identify sites of protein-mineral interaction and provide evidence to support the long-standing theory that acidic proteins are more effective crystal-modulators than other proteins from the same biomineralized material.     

Effects of branched beta-carbon dehydro-residues on peptide conformations: syntheses, crystal structures and molecular conformations of two tetrapeptides: (a) N-(benzyloxycarbonyl)-DeltaVal-Leu-DeltaPhe-Leu-OCH3 and (b) N-(benzyloxycarbonyl)-DeltaIle-Ala-DeltaPhe-Ala-OCH3.

The roles of branched beta-carbon dehydro-residues in the design of peptide conformations have not been systematically explored so far. In order to determine the effects of branched beta-carbon dehydro-residues on the peptide conformations, two N-protected tetrapeptides containing new combinations of DeltaVal and DeltaPhe in (a) N-(benzyloxycarbonyl)-DeltaVal-Leu-DeltaPhe-Leu-OCH(3) and DeltaIle and DeltaPhe in (b) N-(benzyloxycarbonyl)-DeltaIle-Ala-DeltaPhe-Ala-OCH(3) were synthesized by solution procedure. The crystal structures of these peptides were determined by X-ray diffraction methods. Single crystals of both peptides were grown by slow evaporation method from their solutions in acetone-water mixtures (80 : 20) at 25 degrees C. The crystals of these peptides belong to the orthorhombic space group P2(1)2(1)2(1) with cell dimensions of a = 12.342(1) A, b = 15.659(1) A, c = 18.970(1) A for peptide (a) and a = 8.093(1) A, b = 15.791(1) A, c = 23.816(1) A for peptide (b) having Z = 4 in the unit cells of both peptides. The structures were refined by full-matrix least-squares procedure to R-factors of 0.076 and 0.052 respectively. Both peptides adopt the right-handed 3(10)-helical conformations stabilized by two intramolecular (i + 3-->i) hydrogen bonds between the CO of N-terminal benzyloxycarbonyl (Cbz) group and the NH of residue at position 3, and between the CO of residue at position 1 and NH of the residue at position 4. The two consecutive 10-membered rings formed by the hydrogen bonds have dihedral angles corresponding to the standard values for type III beta-turns. DeltaVal and DeltaIle in peptides (a) and (b) respectively are located at the (i + 1) position of the first beta-turn while DeltaPhe is located at the (i + 2) position of the second beta-turn. In the crystals, the molecules are linked head to tail by intermolecular hydrogen bonds to form long helical chains. The axes of helices are parallel to the b-axes while the neighbouring helices run in the opposite directions. The crystal packings are further stabilized by van der Waals forces between the columns of molecular packings.     

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.     

Conformational characteristics of peptides and unanticipated results from crystal structure analyses

Preferred conformation and types of molecular folding are some of the topics that can be addressed by structure analysis using x-ray diffraction of single crystals. The conformations of small linear peptide molecules with 2-6 residues are affected by polarity of solvent, presence of water molecules, hydrogen bonding with neighboring molecules, and other packing forces. Larger peptides, both cyclic and linear, have many intramolecular hydrogen bonds, the effect of which outweighs any intermolecular attractions. Numerous polymorphs of decapeptides grown from a variety of solvents, with different cocrystallized solvents, show a constant conformation for each peptide. Large conformational changes occur, however, upon complexation with metal ions. A new form of free valinomycin grown from DMSO exhibits near three-fold symmetry with only three intramolecular hydrogen bonds. The peptide is in the form of a shallow bowl with a hydrophobic exterior. Near the bottom of the interior of the bowl are three carbonyl oxygens, spaced and directed so that they are in position to form three ligands to a K+, e.g., complexation can be completed by the three lobes containing the beta-bends closing over and encapsulating the K+ ion. In another example, free antamanide and the biologically inactive perhydro analogue, in which four phenyl groups become cyclic hexyl groups, have essentially the same folding of backbone and side chains. The conformation changes drastically upon complexation with Li+ or Na+. However, the metal ion complex of natural antamanide has a hydrophobic globlar form whereas the metal ion complex of the inactive perhydro analogue has a polar band around the middle. The structure results indicate that the antamanide molecule is in a complexed form during its biological activity. Single crystal x-ray diffraction structure analyses have identified the manner in which water molecules are essential to creating minipolar areas on apolar helices. Completely apolar peptides, such as membrane-active peptides, can acquire amphiphilic character by insertion of a water molecule into the helical backbone of Boc-Aib-Ala-Leu-Aib-Ala-Leu-Aib-Ala-Leu-Aib-OMe, for example. The C-terminal half assumes an alpha-helix conformation, whereas the N-terminal half is distorted by an insertion of a water molecule W(1) between N(Ala5) and O(Ala2), forming hydrogen bonds N(5)H...W(1) and W(1)...O(2). The distortion of the helix exposes C = O(Aib1) and C = O(Aib4) to the outside environment with the consequence of attracting additional water molecules. The leucyl side chains are on the other side of the molecule. Thus a helix with an apolar sequence can mimic an amphiphilic helix.     

Toxicity of Pyroglutaminated Amyloid β-Peptides 3(pE)-40 and -42 Is Similar to That of Aβ1-40 and -42

An N-terminal truncated isoform of the amyloid beta-peptide (A beta) that begins with a pyroglutamate (pE) residue at position 3 [A beta3(pE)-42] is the predominant isoform found in senile plaques. Based upon previous in vitro studies regarding A beta N-terminal truncated isoforms, it has been hypothesized that A beta3(pE)-x isoforms may aggregate more rapidly and become more toxic than corresponding Abeta1-x peptides. However, the toxicity and aggregation properties of A beta3(pE)-42 and A beta3(pE)-40 have not previously been examined. After initial solubilization and 1-week preaggregation of each peptide at 37 degrees C and pH 7.4, the toxicity of 5-50 microM A beta3(pE)-42 was similar to that of A beta1-42. Moreover, the toxicity of A beta3(pE)-40 paralleled that induced by A beta1-40 in both 1 day in vitro (DIV) cortical and 7 DIV hippocampal cells. Circular dichroism spectra did not reveal major differences in secondary structure between aged A beta1-42, A beta3(pE)-42, A beta3(pE)-40, and A beta1-40 or freshly solubilized forms of these peptides. Overall, the data indicate that the loss of the two N-terminal amino acids and the cyclization of glutamate at position 3 do not alter the extracellular toxicity of A beta.     

Molecular structure of L-lysyl-L-tyrosyl-L-serine acetate

The structure of the tripeptide L-lysyl-L-tyrosyl-L-serine acetate was determined by X-ray diffraction. The crystals are triclinic space group P1, with two peptide molecules in the unit cell. The peptides are in zwitterionic form with positive charges both in the amino terminal and epsilon-amino groups of lysine. A negative charge is found in one of the carboxylic groups, whereas the other one is protonated. Both peptides show very similar backbone torsional angles, in the beta pleated sheet region, but different tyrosine and serine side-chain conformations. The two lysine side chains have a similar conformation g + tg + t, which had not been previously found. In the unit cell we also find one water molecule, one isopropanol molecule and four acetic acid molecules, three of them likely to be present as acetate anions. These molecules form layers which separate the beta-pleated sheets. The whole structure looks like an ordered solution of peptides in the beta-sheet conformation. An extensive network of hydrogen bonds stabilizes the crystal structure.     

Eggshell matrix protein mimics: designer peptides to induce the nucleation of calcite crystal aggregates in solution

Ansocalcin is a novel goose eggshell matrix protein with 132 amino acid residues, which induces the formation of polycrystalline calcite aggregates in in vitro crystallization experiments. The central region of ansocalcin is characterized by the presence of multiplets of charged amino acids. To investigate the specific role of charged amino acid multiplets in the crystal nucleation, three short peptides REWD-16, REWDP-17 (containing charged doublets), and RADA-16 (alternating charged residues) were synthesized and characterized. The aggregation of these peptides in solution was investigated using circular dichroism, intrinsic tryptophan fluorescence, and dynamic light scattering experiments. The peptides REWD-16 and REWDP-17 induced the polycrystalline calcite crystal aggregates, whereas RADA-16 did not induce significant changes in calcite crystal morphology or aggregate formation in in vitro crystallization experiments. The lattice and morphology of the calcite crystals were characterized using X-ray diffraction and scanning electron microscope. The results discussed in this paper reveal the importance of multiplets of charged amino acid residues toward the nucleation of polycrystalline calcite crystal aggregates in solution.     

Scanning electron microscopic and X-ray diffraction studies of otoconia in the lizard Podarcis s. sicula

Summary The otoliths of embryos and young animals of the lizard Podarcis s. sicula were studied by X-ray diffraction and scanning electron microscopy. Two types of crystal that give different X-ray diffraction patterns were found in the membranous labyrinth of Podarcis. The crystals consist of calcite or aragonite and are easily distinguished by scanning electron microscopy because of their different morphology. The two calcium carbonate crystal forms are not mixed at random but are present in the embryo from the very beginning in specific sites. The endolymphatic sac contains aragonite crystals while the saccule contains calcite crystals adjacent to the wall, in addition to a preponderance of aragonite crystals. The utricle and lagena contain only calcite crystals. The presence of two crystal forms of calcium carbonate in the membranous labyrinth are discussed in terms of differing genetic and functional significance.