Dawn Webber

Sialylation of urinary prothrombin fragment 1 is implicated as a contributory factor in the risk of calcium oxalate kidney stone formation

Urinary glycoproteins are important inhibitors of calcium oxalate crystallization and adhesion of crystals to renal cells, both of which are key mechanisms in kidney stone formation. This has been attributed to glycosylation of the proteins. In South Africa, the black population rarely form stones (incidence < 1%) compared with the white population (incidence 12–15%). A previous study involving urinary prothrombin fragment 1 from both populations demonstrated superior inhibitory activity associated with the protein from the black group. In the present study, we compared N‐linked and O‐linked oligosaccharides released from urinary prothrombin fragment 1 isolated from the urine of healthy and stone‐forming subjects in both populations to elucidate the relationship between glycosylation and calcium oxalate stone pathogenesis. The O‐glycans of both control groups and the N‐glycans of the black control samples were significantly more sialylated than those of the white stone‐formers. This demonstrates a possible association between low‐percentage sialylation and kidney stone disease and provides a potential diagnostic method for a predisposition to kidney stones that could lead to the implementation of a preventative regimen. These results indicate that sialylated glycoforms of urinary prothrombin fragment 1 afford protection against calcium oxalate stone formation, possibly by coating the surface of calcium oxalate crystals. This provides a rationale for the established roles of urinary prothrombin fragment 1, namely reducing the potential for crystal aggregation and inhibiting crystal–cell adhesion by masking the interaction of the calcium ions on the crystal surface with the renal cell surface along the nephron.

Glycosylation of prothrombin fragment 1 governs calcium oxalate crystal nucleation and aggregation, but not crystal growth

Urinary glycoproteins play an important role in the modulation of calcium oxalate crystallisation. In several cases, this has been attributed to glycosylation of the proteins as evidenced by urinary prothrombin fragment 1 where there is a correlation between sialylation and calcium oxalate kidney stone disease. In the present study, plasma-derived prothrombin fragment 1 (PTF1) was enzymatically modified in order to generate its asialo and aglyco forms. The parent glycoprotein and its two glycoforms were used in calcium oxalate crystallisation studies to assess the role of the carbohydrate moeity in PTF1’s potent inhibitory activity. The glycans inhibited crystal aggregation and promoted crystal nucleation, but had no effect on crystal growth. The terminal sialic acid residues had a small effect on inhibition of crystal aggregation whereas they contributed significantly to promotion of nucleation. These results indicate that glycosylation of PTF1 governs calcium oxalate crystal nucleation and aggregation but it does not affect the protein’s role in inhibiting crystal growth. Since promotion of nucleation and inhibition of aggregation are both regarded as protective mechanisms against calcium oxalate urinary stone formation, the kringle domain on which the glycans are located is implicated in PTF1’s inhibitory activity. It is speculated that modifications in the glycosylation of urinary PTF1 in stone-formers may regulate its capacity to protect against calcium urolithiasis.

Experimental determination of multiple thermodynamic and kinetic risk factors for nephrolithiasis in the urine of healthy controls and calcium oxalate stone formers: does a universal discriminator exist?

Nephrolithiasis is thought to be governed by urinary thermodynamic and kinetic risk factors. However, identification of one or more of these factors which consistently and unambiguously differentiates between healthy subjects (N) and calcium oxalate (CaOx) renal stone patients (SF) remains elusive. The present study addresses this challenge. 24 h urines were collected from 15 N and 10 SF. Urine compositions were used to compute thermodynamic risk indices including urinary ratios, quotients and supersaturation (SS) values, while CaOx metastable limits (MSL) were determined experimentally. Crystallisation kinetics was determined by measuring rates of particle formation (number, volume, size) using a Coulter counter multisizer (CC) and a Coulter flow cytometer (FC). Particle shapes were qualitatively differentiated by FC and were viewed directly by scanning electron microscopy. Several urinary composition ratios and risk quotients were significantly different between the groups. However, there were no significant differences between CaOx MSL or SS values. Using transformed FC data, the rate of CaOx crystallisation in SF was significantly greater than in N. This was not supported by CC measurements. There were no significant differences between the groups with respect to particle size or CaOx crystal growth rates. Single and aggregated CaOx dihydrate crystals were observed in both groups with equal frequency and there were no differences in the kinetic properties of these deposits. A few CaOx monohydrate crystals were observed in SF. Although several risk factors were found to be significantly different between the groups, none of them were consistently robust when compared to other cognate factors. Arguments were readily invoked which demonstrated inter-factor inconsistencies and conflicts. We suspect that a unique discriminatory factor, such as any of those which we investigated in the present study, may not exist.

Variability in Kidney Stone Incidence Between Black and White South Africans: AGT Pro11Leu Polymorphism Is Not a Factor

BACKGROUND AND PURPOSE Kidney stone disease is rare in the South African black (B) population and more prevalent in the white (W) population. Genetic studies have not previously examined this anomaly. The AGT Pro11Leu polymorphism in the alanine:glyoxylate aminotransferase (AGT) enzyme has been suggested as possibly playing a role in the pathogenesis of idiopathic calcium oxalate kidney stones. The present study was undertaken to investigate whether differences occur in the frequency of this polymorphism in subjects of both race groups. MATERIALS AND METHODS Healthy B (n=60) and W (n=60) male subjects each provided early morning spot urine, blood, and buccal cell samples. The AGT Pro11Leu locus was amplified using the polymerase chain reaction and polymorphism was genotyped using a restriction fragment length polymorphism. RESULTS There was no difference in the frequency of the AGT Pro11Leu polymorphism, and the major allele (C) was present at a frequency of 0.82 in B and 0.83 in W. Thus, the most common genotype homozygous normal CC genotype was observed at similar frequencies in both groups (0.68 and 0.65 in B and W, respectively), as were the heterozygous CT genotype (CT) and the homozygous variant TT genotype (TT) genotypes (0.33 & 0.02 and 0.28 & 0.03 in B and W, respectively). Neither urinary oxalate nor any other component in the two groups was correlated with the frequency of the AGT Pro11Leu polymorphism. CONCLUSIONS Our data imply that the AGT Pro11Leu polymorphism is not directly responsible for the low incidence of stone formation in B. We conclude that other factors must be instrumental in protecting the B population from urolithiasis.

Proteolysis and partial dissolution of calcium oxalate: a comparative, morphological study of urinary crystals from black and white subjects.

Crystal adherence to the renal epithelium is widely regarded as a probable mechanism of stone formation. Intracrystalline proteins may provide access to the core of urinary crystals and thereby facilitate the dismantling of these crystals after their attachment to and phagocytosis by renal epithelial cells. The present study investigated the role of proteolysis and limited dissolution of urinary calcium oxalate (CaOx) crystals in South Africa’s white and black populations with a view to understanding the remarkably low stone incidence in the black population compared with the whites. CaOx crystals were precipitated from filtered urine or ultrafiltered urine dosed with an intracrystalline protein, urinary prothrombin fragment 1 (UPTF1), isolated from white and black subjects. The crystals were fractured and subjected to proteolysis and/or limited dissolution before examination using field emission scanning electron microscopy (FESEM). FESEM data showed that CaOx crystals from white and black subjects were eroded by treatment with proteases. Cathepsin D caused the most significant crystal erosion, and more noticeable degradation of CaOx monohydrate (COM) crystals compared to CaOx dihydrate (COD). Limited dissolution studies showed the unique ultrastructures and fragmentation processes of COM and COD crystals. COM crystals appeared to be more susceptible to degradation and dissolution than CODs. Since COMs are predominant in blacks, compared with COD crystals from whites, it is speculated that the lower stone rate amongst South African blacks might be attributed partly to their more efficient destruction of retained COM crystals.