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Biliary cholesterol crystallization characterized by single-crystal cryogenic electron diffraction.

Cholesterol crystals are the building blocks of cholesterol gallstones. The exact structure of early-forming crystals is still controversial. We combined cryogenic-temperature transmission electron microscopy with cryogenic-temperature electron diffraction to sequentially study crystal development and structure in nucleating model and native gallbladder biles. The growth and long-term stability of classic cholesterol monohydrate (ChM) crystals in native and model biles was determined. In solutions of model bile with low phospholipid-to-cholesterol ratio, electron diffraction provided direct proof of a novel transient polymorph that had an elongated habit and unit cell parameters differing from those of classic triclinic ChM. This crystal is exactly the monoclinic ChM phase described by Solomonov and coworkers (Biophysical J., In press) in cholesterol monolayers compressed on the air-water interface. We observed no evidence of anhydrous cholesterol crystallization in any of the biles studied. In conclusion, classic ChM is the predominant and stable form in native and model biles. However, under certain (low phospholipid) conditions, transient intermediate polymorphs may form. These findings, documenting single-crystal analysis in bulk solution, provide an experimental approach to investigating factors influencing biliary cholesterol crystal nucleation and growth as well as other processes of nucleation and crystallization in liquid systems.

Bile↗

Protein crystal growth in microgravity-temperature induced large scale crystallization of insulin.

One of the major stumbling blocks that prevents rapid structure determination using x-ray crystallography is macromolecular crystal growth. There are many examples where crystallization takes longer than structure determination. In some cases, it is impossible to grow useful crystals on earth. Recent experiments conducted in conjunction with NASA on various Space Shuttle missions have demonstrated that protein crystals often grow larger and display better internal molecular order than their earth-grown counterparts. This paper reports results from three Shuttle flights using the Protein Crystallization Facility (PCF). The PCF hardware produced large, high-quality insulin crystals by using a temperature change as the sole means to affect protein solubility and thus, crystallization. The facility consists of cylinders/containers with volumes of 500, 200, 100, and 50 ml. Data from the three Shuttle flights demonstrated that larger, higher resolution crystals (as evidenced by x-ray diffraction data) were obtained from the microgravity experiments when compared to earth-grown crystals.

Animals↗

Observations on structural features and characteristics of biological apatite crystals. 4. Observation on ultrastructure of human bone crystals.

In a series of studies to investigate the structural features of the biological crystals such as the tooth and bone, following the previous observations of the tooth crystal using an electron microscope, we examined the ultrastructure of the human bone crystals at near atomic resolution through the cross and longitudinal sections of the crystals. The materials used for this study were the normal bone tissue obtained from the buccal alveolar compact bone of the human mandible in the portion of the lower first molar. The small cubes of the bone tissue were fixed in glutaraldehyde and osmium tetroxide and embedded in epoxy resin using the routine methods. The ultrathin sections were cut with a diamond knife without decalcification. The sections were examined with the HITACHI H-800 type transmission electron microscope operated at 200 kV. Each crystal was observed at the initial magnification of 300,000 times and at the final magnification of 10,000,000 times and over. Using this approach, we showed the configuration of the hydroxyapatite structure in the cross and longitudinal sections of the bone crystals deposited within and between the collagen fibrils (intrafibrillar and interfibrillar crystals) in the bone tissue. Furthermore, using the same approach, we observed the crystal lattices of the hydroxyapatite structure appearing in the cross and longitudinal sections. We sincerely believe that the electron micrographs shown in this report are the first atomic images from the section obtained from the hydroxyapatite crystal from the human alveolar bone.

Alveolar Process↗

Variation in the inflammatory properties of basic calcium phosphate crystals according to crystal type.

OBJECTIVE: To determine the inflammatory potential of basic calcium phosphate (BCP) crystals, which have been identified in human joints. METHODS: Hydroxyapatite, carbonate apatite, whitlockite, and octacalcium phosphate crystals were injected in rat air pouches. Volume and cellularity of the exudate were measured. Physicochemical properties of the injected BCP crystals were determined, and correlations with the magnitude of induced inflammatory responses were sought. RESULTS: Significant differences were observed among the volumes and white blood cell (WBC) counts of the pouch exudates, based on the various crystal types used to induce inflammation. A strong correlation was demonstrated between the specific surface (SS) area of the injected crystals and the area under the curve for induced WBC count versus time (R2 = 0.88, P = 0.05). This correlation was observed for SS area values below 50 m2/gm, but when SS area increased further, this parameter plateaued. Another parameter of inflammatory response was obtained by dividing the area under the curve figuring WBC counts versus time by the corresponding SS area for each crystal type. This parameter increased linearly with the Ca:P ratio (R2 = 0.97, P = 0.0003). CONCLUSION: The inflammatory potential of BCP crystals appeared to vary according to crystal features. SS area and the Ca:P ratio (which correlates with crystal solubility) influenced inflammatory properties. These results could explain the variable clinical consequences of BCP deposits, and must be taken into account in the choice of apatite ceramics for use as biomaterials.

Animals↗

The crystal structure of indole-3-glycerol phosphate synthase from the hyperthermophilic archaeon Sulfolobus solfataricus in three different crystal forms: effects of ionic strength.

Indole-3-glycerol phosphate synthase from the hyperthermophilic archaeon Sulfolobus solfataricus is a monomeric enzyme with the common (beta/alpha)8-fold. Recently, its three-dimensional structure was solved in an orthorhombic crystal form, grown by using 1.3 M ammonium sulfate as precipitating agent. Here we describe the X-ray structure analysis of two new crystal forms of this enzyme that were obtained at medium and low ionic strength, respectively. Hexagonal crystals with space group P3(1)21 and cell dimensions a = 62.4 A, b = 62.4 A, c = 122.9 A, gamma = 120 degrees grew in 0.1 M Mes buffer at pH 6.0 with 30% polyethylene glycol monomethylether as precipitant and 0.2 M ammonium sulfate as co-precipitant. A second crystal form with space group P2(1)2(1)2(1) and cell constants a = 62.6 A, b = 74.0 A, c = 74.2 A was obtained using polyethylene glycol and ethylene glycol as precipitants in 0.1 M Mes buffer at pH 6.5. Both structures were solved by molecular replacement and refined at 2.5 A and 2.0 A resolution, respectively. Although the global folds are almost identical, alternative conformations are observed in flexible loop regions, mostly stabilized by crystal contacts. In none of the three crystal forms is the so-called phosphate binding site empty, suggesting that this position has high affinity for anions with tetrahedrally arranged oxygen atoms. Differences in ionic strength of the crystallization buffer have only minor effects on number and specificity of intramolecular salt bridges. The crystal packing, on the other hand, seems to be influenced by the ionic strength of the solvent, since the number of intermolecular salt bridges in the low ionic strength crystal forms is significantly higher.

Binding Sites↗

Crystallization of aqueous ammonium sulfate particles internally mixed with soot and kaolinite: crystallization relative humidities and nucleation rates.

Using optical microscopy, we investigated the crystallization of aqueous ammonium sulfate droplets containing soot and kaolinite, as well as the crystallization of aqueous ammonium sulfate droplets free of solid material. Our results show that soot did not influence the crystallization RH of aqueous ammonium sulfate particles under our experimental conditions. In contrast, kaolinite increased the crystallization RH of the aqueous ammonium sulfate droplets by approximately 10%. In addition, our results show that the crystallization RH of aqueous ammonium sulfate droplets free of solid material does not depend strongly on particle size. This is consistent with conclusions made previously in the literature, based on comparisons of results from different laboratories. From the crystallization results we determined the homogeneous nucleation rates of crystalline ammonium sulfate in aqueous ammonium sulfate droplets and the heterogeneous nucleation rates of crystalline ammonium sulfate in aqueous ammonium sulfate particles containing kaolinite. Using classical nucleation theory and our experimental data, we determined that the interfacial tension between an ammonium sulfate critical nucleus and an aqueous ammonium sulfate solution is 0.064 +/- 0.003 J m(-2) (in agreement with our previous measurements), and the contact angle between an ammonium sulfate critical nucleus and a kaolinite surface is 59 +/- 2 degrees. On the basis of our results, we argue that soot will not influence the crystallization RH of aqueous ammonium sulfate droplets in the atmosphere, but kaolinite can significantly modify the crystallization RH of atmospheric ammonium sulfate droplets. As an example, the CRH50 (the relative humidity at which 50% of the droplets crystallize) ranges from about 41 to 51% RH when the diameter of the kaolinite inclusion ranges from 0.1 to 5 microm. For comparison, the CRH50 of aqueous ammonium sulfate droplets (0.5 microm diameter) free of solid material is approximately 34.3% RH under atmospheric conditions.

Journal Article↗

Crystal-to-crystal transformations of a microporous metal-organic laminated framework triggered by guest exchange, dehydration and readsorption.

Single crystals of a neutral, microporous, laminated metal-organic framework (MOF)[Fe(pydc)(4,4'-bipy)]xH(2)O (1xH(2)O)(H(2)pydc = 2,5-dicarboxypyridine, 4,4'-bipy = 4,4'-bipyridine) were generated by hydrothermal synthesis, and its crystal structure was determined. 1xH(2)O retains the framework robustness to ca. 370 degrees C and is insoluble in common organic solvents. By soaking in MeOH and EtOH solutions, 1xH(2)O was transformed directly from the parent single crystals into single crystals of 1xMeOH or 1xEtOH, respectively. Meanwhile, 1xH(2)O shrank to the guest-free framework (h) or (v), respectively, under appropriate heating (up to 160 degrees C in N(2)) or vacuum treatment (10 mmHg) at room temperature. Compared to that of 1xH(2)O, the unit-cell volume of 1xEtOH slightly increases by 2.9%, whereas those of (h) or (v) are reduced by 8.2 and 6.6%, respectively. The anhydrous (v) was found to be highly chemically reactive, taking up ethanol vapor to furnish the solvated crystal structure of an 'expanded' framework 1xEtOH. In a mixture of ethanol-DMF or ethanol-benzene, a selective exchange process was observed, with only ethanol molecules exchanged into the structure due to the limited free size of the channels in the framework of. All the transformed crystals have also been characterized by X-ray single-crystal diffraction to understand the crystal-to-crystal transformation, which have different free volumes (6.5-20.4%).

Journal Article↗

Observations on structural features and characteristics of biological apatite crystals. 5. Three-dimensional observation on ultrastructure of human enamel crystals.

In a series of studies to investigate the structural features of the biological crystals, such as the tooth and bone, using an electron microscope, we examined the ultrastructure of the enamel, dentin, and bone crystals at near atomic resolution and showed the configuration of the hydroxyapatite structure through the cross and longitudinal sections of the crystals. Thereafter, based on the results of the observations by the authors of the ultrastructure of the tooth and bone crystals, thinking that it might be possible to conduct direct three-dimensional observation of the configuration composing the unit cell of the hydroxyapatite crystals, we conducted a study on this. These results indicated that it was possible to sterically observe the configuration of the hydroxyapatite structure composing the enamel crystal. The materials used for this study were the middle layer of the noncarious enamel from the freshly extracted human erupted permanent molars. The small cubes of the enamel were fixed in glutaraldehyde and osmium tetroxide and embedded in epoxy resin using the routine methods. The ultrathin sections were cut with a diamond knife without decalcification and were examined with the HITACHI H-9000 H type transmission electron microscope operated at 300 kV. Each crystal was observed at an initial magnification of 500,000 times and at the final magnification of 10,000,000 times and over. We sincerely believe that the electron micrographs shown in this report are the first to show three-dimensionally the configuration of the hydroxyapatite structure composing the crystal in the cross and longitudinal sections of an enamel crystal.

Dental Enamel↗

Direct preparation of spherically agglomerated salicylic acid crystals during crystallization.

Needle-like salicylic acid crystals were transformed into a spherically shaped dense form during crystallization by the spherical crystallization technique. Agitation of a mixture of ethanol-water-chloroform containing salicylic acid yielded spherically agglomerated salicylic acid crystals. The crystallinity of the agglomerated salicylic acid the amount of ethanol in the solvent mixture was decreased. The wettability of the agglomerated crystals increased when the amount of ethanol in the solvent mixture was decreased, and this enhanced the dissolution rate of the crystals. The remarkable improvements in the flow and packing of the agglomerated crystals enabled the direct compression of the crystals.

Chemical Phenomena↗

Crystal packing interaction that blocks crystallization of a site-specific DNA binding protein-DNA complex.

We present here three high-resolution crystal structures of complexes between the DNA-binding domain of the heat-shock transcription factor (HSF) and DNA oligomers. Although the DNA oligomers contain HSF's specific binding sequence, called a heat-shock element, the crystal structures do not contain the specific protein-DNA complex. In one crystal structure, the 10 base pair DNA oligomer is statically disordered. In the other two related structures, the 12 base pair DNA oligomers are in unique positions, but the protein-DNA contacts in these two crystals are not sequence specific. In all three structures, the DNA appears to act as a rigid, polyanion scaffold to support columns of proteins in a crystalline lattice. A robust crystal packing interface between protein monomers obscures the true DNA-binding surface, known from previous genetic and biochemical studies. By redesigning the protein to interfere with the crystal lattice contacts, we were able to obtain physiologically relevant crystals in a specific protein-DNA complex. Thus, a crystal-packing interface was able to prevent the weak, but physiological relevant interactions between a protein and DNA.

Binding Sites↗

Calcium carbonate crystals promote calcium oxalate crystallization by heterogeneous or epitaxial nucleation: possible involvement in the control of urinary lithogenesis.

A large proportion of urinary stones have calcium oxalate (CaOx) as the major mineral phase. In these stones, CaOx is generally associated with minor amounts of other calcium salts. Several reports showing the presence of calcium carbonate (CaCO3) and calcium phosphate in renal stones suggested that crystals of those salts might be present in the early steps of stone formation. Such crystals might therefore promote CaOx crystallization from supersaturated urine by providing an appropriate substrate for heterogeneous nucleation. That possibility was investigated by seeding a metastable solution of 45Ca oxalate with vaterite or calcite crystallites. Accretion of CaOx was monitored by 45Ca incorporation. We showed that (1) seeds of vaterite (the hexagonal polymorph of CaCO3) and calcite (the rhomboedric form) could initiate calcium oxalate crystal growth; (2) in the presence of lithostathine, an inhibitor of CaCO3 crystal growth, such accretion was not observed. In addition, scanning electron microscopy demonstrated that growth occurred by epitaxy onto calcite seeds whereas no special orientation was observed onto vaterite. It was concluded that calcium carbonate crystals promote crystallization of calcium oxalate and that inhibitors controlling calcium carbonate crystal formation in Henle's loop might play an important role in the prevention of calcium oxalate stone formation.

Calcium Carbonate↗

Membrane interactions with calcium oxalate crystals: variation in hemolytic potentials with crystal morphology.

Crystal-induced membranolysis of human red blood cells has been quantitated for calcium oxalate monohydrate and calcium oxalate dihydrate crystals. Calcium oxalate monohydrate crystals are significantly more membranolytic than calcium oxalate dihydrate crystals at constant surface area. If the crystal morphology of calcium oxalate monohydrate is altered by grinding, the lytic potential at constant surface area is markedly reduced. However, altered calcium oxalate dihydrate crystals are as lytic as natural calcium oxalate dihydrate crystals at constant surface area. Differences in the calcium oxalate monohydrate and dihydrate crystal structures, specifically the structural characteristics of the disordered water channel in calcium oxalate dihydrate, can explain these different membranolytic characteristics.

Calcium Oxalate↗

Crystal-cell interactions: crystal binding to rat renal papillary tip collecting duct cells in culture.

Retention of stone crystallites by urothelium is clearly one of the prime requisites for urinary stone disease. Studies in the literature as early as 1937 have highlighted that the initiation of renal calculi followed the formation of subepithelial calcified plaques in the renal pelvis. The renal papilla is one of the primary sites for crystal fixation and stone maturation. We have developed an in vitro model system for the study of kidney stone crystal retention to tubular epithelium using rat renal papillary collecting tubule (RPCT) cells in primary culture. We have qualitatively and quantitatively analyzed the binding of preformed calcium oxalate monohydrate (COM), hydroxyapatite (HA), and uric acid (UA) crystals to RPCT cells. Our goal was to determine if three common urinary stone crystals evidenced different crystal-cell binding characteristics. Also, since these crystals are frequently observed admixed in stones, we have studied the inhibitive binding characteristics of these crystals with RPCT cells. The RPCT cells in culture grow both as the typical polygonal cells in monolayer and as clumps of aggregated cells. The cells in the aggregates are viable epithelial cells that have lost their attachment to the basement membrane, resulting in the exposure of surface molecules that would not normally be present unless the cells were damaged or if there was a loss of intercellular tight junctions. COM, HA, and UA crystals all preferentially bound to the aggregated cells and all exhibited similar saturable binding patterns.(ABSTRACT TRUNCATED AT 250 WORDS)

Animals↗

Temporomandibular joint osteoarthritis and crystal deposition diseases: a study of crystals in synovial fluid lavages in osteoarthritic temporomandibular joints.

To study the presence of crystals in synovial fluid lavages of osteoarthritic temporomandibular joints (TMJs), in order to evaluate the possible role of these crystals in the osteoarthritic (OA) process, synovial fluid lavage samples of the upper joint compartment from 44 TMJs were obtained prior to arthroscopy. The OA group consisted of 32 TMJs. The control group consisted of 12 TMJs that had been diagnosed with other nonosteoarthritic conditions. The lavage samples were analysed as wet preparations, unstained and stained, with ordinary light, polarized light and compensated polarized light for the presence of crystals and white blood cells. One sample was prepared for subsequent electron microscopic (EM) examination. Synovial fluid lavage analysis of osteoarthritic TMJs did not show any monosodium urate monohydrate or calcium pyrophosphate dihydrate crystals. However, in three lavages, particles which possibly contained calcium were identified with alizarin red S staining. White blood cells were occasionally seen. Synovial fluid analysis of the lavages of the control TMJs did not reveal any crystals. EM examination of synovial fluid lavage from an osteoarthritic TMJ failed to clearly show crystal formation. Concurrence of TMJ crystal deposition and OA appears less prominent than in other synovial joints. We conclude that crystals probably do not play an important role in TMJ OA.

Adult↗

Crystallization and the crystal properties of the oxygen-evolving photosystem II from Synechococcus vulcanus.

A photosystem II (PSII) complex highly active in oxygen evolution was purified and crystallized from a thermophilic cyanobacterium, Synechococcus vulcanus. The PSII complex in the crystals contained the D1/D2 reaction center subunits, CP47 and CP43 (two chlorophyll-binding core antenna proteins of photosystem II), cytochrome b-559 alpha- and beta-subunits, several low molecular weight subunits, and three extrinsic proteins, that is, 33 and 12 kDa proteins and cytochrome c-550. The PSII complex also retained a high rate of oxygen evolution. The apparent molecular mass of the PSII in the crystals was determined to be 580 kDa by gel filtration chromatography, indicating that the PSII crystallized is a dimer. The crystals diffracted to a maximum resolution of 3.5 A at a cryogenic temperature using X-rays from a synchrotron radiation source, SPring-8. The crystals belonged to an orthorhombic system, and the space group was P2(1)2(1)2(1) with unit cell dimensions of a = 129.7 A, b = 226.5 A, and c = 307.8 A. Each asymmetric unit contained one PSII dimer, which gave rise to a specific volume (V(M)) of 3.6 A(3)/Da based on the calculated molecular mass of 310 kDa for a PSII monomer and an estimated solvent content of 66%. Multiple data sets of native crystals have been collected and processed to 4.0 A, indicating that our crystals are suitable for structure analysis at this resolution.

Crystallization↗

Dual roles of brushite crystals in calcium oxalate crystallization provide physicochemical mechanisms underlying renal stone formation.

Calcium oxalate monohydrate (COM) crystals are the major mineral component of most kidney stones, and thus have an important role in chronic human disease. However, the physicochemical mechanisms leading to calcium oxalate (CaOx) stone disease are only partially defined. As spontaneous precipitation of CaOx is rare under renal conditions, an alternative pathway for CaOx crystallization seems necessary to resolve this central issue. We performed kinetic studies using the dual constant composition method to simultaneously analyze the crystallization of COM and brushite, the form of calcium phosphate that is most readily formed in the typical slightly acidic urinary milieu. These studies were supported by parallel analysis by scanning electron and atomic force microscopy. In these studies, mineralization of a thermodynamically stable phase (COM) was induced by the presence of brushite, a more readily precipitated inorganic phase. Furthermore, once formed, the COM crystals grew at the expense of brushite crystals causing the dissolution of the brushite crystals. These studies show that brushite may play crucial roles in the formation of COM crystals. The definition of these two roles for brushite thereby provides physicochemical explanations for the initiation of COM crystallization and also for the relative paucity of calcium phosphate detected in the majority of CaOx renal stones.

Calcium Oxalate↗

Crystal retention capacity of cells in the human nephron: involvement of CD44 and its ligands hyaluronic acid and osteopontin in the transition of a crystal binding- into a nonadherent epithelium.

Nephrolithiasis requires formation of crystals followed by their retention and accumulation in the kidney. Crystal retention can be caused by the association of crystals with the epithelial cells lining the renal tubules. The present study investigated the interaction between calcium oxalate monohydrate (COM) crystals and primary cultures of human proximal (PTC) and distal tubular/collecting duct cells (DTC). Both PTC and DTC were susceptible to crystal binding during the first days post-seeding (4.9 +/- 0.8 micro g COM/cm2), but DTC lost this affinity when the cultures developed into confluent monolayers with functional tight junctions (0.05 +/- 0.02 micro g COM/cm2). Confocal microscopy demonstrated the expression of the transmembrane receptor protein CD44 and its ligands osteopontin (OPN) and hyaluronic acid (HA) at the apical membrane of proliferating tubular cells; at confluence, CD44 was expressed at the basolateral membrane and OPN and HA were no longer detectable. In addition, a particle exclusion technique revealed that proliferating cells were surrounded by HA-rich pericellular matrices or "cell coats" extending several microns from the cell surface. Disintegration of these coats with hyaluronidase significantly decreased the cell surface affinity for crystals. Furthermore, CD44, OPN, and HA were also expressed in vivo at the luminal side of tubular cells in damaged kidneys. These results suggest (1) that the intact distal tubular epithelium of the human kidney does not bind crystals, and (2) that crystal retention in the human kidney may depend on the expression of CD44-, OPN-, and-HA rich cell coats by damaged distal tubular epithelium.

Calcium Oxalate↗

Remarkable features in lattice-parameter ratios of crystals. I. Orthorhombic, tetragonal and hexagonal crystals.

The investigation of the lattice-parameter ratios of tetrahedral and hexagonal-rhombohedral inorganic compounds, as reported by Constant & Shlichta [(2003), Acta Cryst. A59, 281-282], has been extended to the structural data found for organic and metal-organic compounds (CSD), for bio-macromolecular crystals (PDB) and for inorganic materials (ICSD). In this first part of the series, the frequency distribution of orthorhombic, tetragonal and hexagonal crystals is presented. The results obtained confirm the existence of sharp peaks as a function of the ratios of lattice parameters and reveal additional exponential components, decaying for large and small values of these ratios. Practically all the important peaks occur at ratios which correspond to lattices having metric tensors with rational entries, the so-called integral lattices. The exponential component is interpreted as expressing a general statistical distribution which is valid for the generic crystal lattices, i.e. those normally considered. The exponential fraction dominates the peaked component in the organic and metal-organic cases, is less important for bio-macromolecular crystals and is much less important than the sharp peaks for inorganic crystals. Remarkable is the crystallographic relevance of the isometric hexagonal lattice, characterized by the axial ratio c/a = 1 and first observed in the molecular form of a protein. In the frequency distribution of 12 117 inorganic hexagonal crystals, the highest peak of 937 crystals occurs for c = a. In the hexagonal case of the bio-macromolecules the most important peak of 422 crystals is observed near the ideal h.c.p. (hexagonal closed packing) ratio of (8/3)(1/2).

Crystallization↗