Oxalate transport in cultured porcine renal epithelial cells

Oxalate binding proteins in calcium oxalate nephrolithiasis

The existence of several oxalate specific binding proteins have been demonstrated in human and rat kidney. These occur in both cortical and medullary cells and are distributed mostly in the subcellular organelles. About 1/3 of the total cellular oxalate binding was localised in the inner mitochondrial membrane while the rest was in the nucleus. The purified mitochondrial oxalate binding protein (62 kDa) was composed, with a higher molar proportion, of basic amino acids, and could accumulate oxalate on incorporation into liposomes. In the nucleus, histone H(1B) (27.5 kDa), nuclear membrane protein (68 kDa) and nuclear pore complex protein (205 kDa) were present with oxalate binding activities. In addition, a 45 kDa calcium oxalate binding protein was identified in most of the subcellular organelles. Both mitochondrial and nuclear oxalate binding proteins and calcium oxalate binding protein have shown the kinetic properties of specificity, saturability, pH and temperature dependency, energy of activation and inhibition by substrate analogues. All oxalate binding proteins were sensitive to the transport inhibitor 4'-4' diisothiocyano stilbene-2-2 disulphonic acid (DIDS), which is known to interact with the lysine moiety of the proteins. Calcium oxalate monohydrate (COM) crystals adsorbed oxalate binding proteins from human and rat kidney, and oxalate binding proteins isolated from human kidney stone matrix also exhibited the above kinetic properties. In experimental hyperoxaluria, all of the renal oxalate binding proteins showed enhanced oxalate binding activity with increased protein concentration. This enhanced oxalate binding activity was also attributed to increased lipid peroxidation, which correlated positively, and to decreased thiol status, which correlated negatively. A positive correlation was observed between the lipid peroxidation and both the oxalate binding activity of the in vitro peroxidised subcellular organelles and the purified protein. Similarly, in an in vivo hyperoxaluric condition, a negative correlation was observed between thiol content and both the oxalate binding activity of the peroxidised subcellular organelles and the purified protein. In the calcium oxalate crystal growth system, the oxalate binding proteins behaved either as promoters or inhibitors of the nucleation and aggregation of crystals. Following the peroxidation of the proteins, the degree of effect of the promoter protein was further stimulated while the degree of inhibition caused by the inhibitor protein further declined. Similar observations were duplicated with the proteins derived from hyperoxaluric rat kidney or kidney homogenate subjected to in vitro lipid peroxidation. The oxalate binding proteins were thought to modulate the crystallisation process in an hyperoxaluric condition similar to calcium specific binding protein modulators.

Pathogenesis of idiopathic calcium nephrolithiasis: update 1997

Idiopathic calcium nephrolithiasis (ICN) is a frequent disease in Western countries. The physicochemical theory of lithogenesis, which explains stone formation by the precipitation, growth, and crystalline aggregation of lithogenic salts in the urine, has contributed greatly to the understanding of the pathogenesis of calcium urolithiasis. However, several aspects are still unexplained; the co-existence of familial occurrence, primary tubular dysfunctions with ICN, and anomalies in the systemic handling of oxalate and calcium led to the development of a cellular hypothesis of ICN. A number of cellular defects in the handling of ions has been reported that involves both anion and cation transport. These anomalies are probably the expression of a still unknown cellular defect in idiopathic calcium stone formers. We suggested that an anomaly in the cell membrane composition might be responsible for the complex array of cell ion flux abnormalities observed in ICN. Recently, a disorder in the n-6 polyunsaturated fatty acid series has been described; it is characterized by a lower linoleic acid content and a higher arachidonic acid concentration in both plasma and erythrocyte membrane phospholipids of renal calcium stone patients. This anomaly could cause an increased activity of ion carriers; furthermore, it may lead to increased prostaglandin synthesis and to secondary phenomena at the kidney, skeletal, and intestinal level. As a consequence, critical conditions for lithogenesis in the kidney may ensue. The data suggest a common pathogenesis for hypercalciuria and hyperoxaluria. The systemic defect in the phospholipid arachidonic acid level may be both of dietary or genetic origin; experimental data suggest that the increase in delta-6 desaturase activity, the limiting enzyme in the metabolic pathway of polyunsaturated fatty acids, might be relevant to the pathogenesis of lipid abnormalities observed in nephrolithiasis and to the pathogenesis of ICN and its related problems (at the kidney, intestinal, and bone level).

Oxalate transport and calcium oxalate renal stone disease

Hyperoxaluria is considered to play a crucial role in calcium oxalate (CaOx) renal stone disease. The amount of oxalate excreted into the urine depends on intestinal absorption, endogenous production, renal clearance and renal tubular transport. Since a primary disorder has not been found so far in most CaOx stone formers and since oxalate is freely filtered at the glomerulus, most studies are presently focussed on alterations in epithelial oxalate transport pathways. Oxalate can be transported across an epithelium by the paracellular (passive) and transcellular (active) pathway. Oxalate transport across cellular membranes is mediated by anion-exchange transport proteins. A defect in the structure of these transport proteins could explain augmented transcellular oxalate transport. Little is known about the physiological regulation of oxalate transport. In this review cellular transport systems for oxalate will be summarized with special attention for the progress that has been made to study oxalate transport in a model of cultured renal tubule cells. Better understanding of the physiological processes that are involved in oxalate transport could yield information on the basis of which it might be possible to design new approaches for an effective treatment of CaOx stone disease.

Cell cultures and nephrolithiasis

While the physical chemistry of stone formation has been intensively studied during the last decade, it has become clear that the pathophysiology of renal stone disease cannot be explained by crystallization processes only. In recent years, evidence has emerged that the cells lining the renal tubules can have an active role in creating the conditions under which stones may develop. Since it is difficult to study these mechanisms in vivo, cultured renal tubular cells have become increasingly popular for the study of physiological and cell biological processes that are possibly linked to stone disease. In this paper, we discuss the possible contribution of cellular processes such as transepithelial oxalate transport and crystal--cell interaction to the formation of renal stones. Experimental studies that have been performed with cultured renal cells to elucidate the mechanisms involved in these processes will be summarized.

Morphological analysis of renal cell culture models of calcium phosphate stone formation

Cell culture models of calcium phosphate renal stone formation were established using the MDCK cell line. Renal microliths were detected within pseudocysts in three-dimensional soft agar cultures, and were also observed in the basal region of cells lining the cell sheet, and immediately beneath domes or blisters in monolayers and collagen gel cultures. Light and scanning electron microscopy indicated that these microliths had a similar lamellated and spherical appearance to those in humans. These microliths were first detected microscopically after 21 days of culture, and were found to be composed of calcium phosphate by X-ray and micro-infrared spectroscopic analyses. These culture models may provide a powerful new tool to study the pathogenesis of renal stone diseases and/or calcium phosphate stone formation in humans and animals.

Oxalate transport and calcium oxalate renal stone disease

Hyperoxaluria is considered to play a crucial role in calcium oxalate (CaOx) renal stone disease. The amount of oxalate excreted into the urine depends on intestinal absorption, endogenous production, renal clearance and renal tubular transport. Since a primary disorder has not been found so far in most CaOx stone formers and since oxalate is freely filtered at the glomerulus, most studies are presently focussed on alterations in epithelial oxalate transport pathways. Oxalate can be transported across an epithelium by the paracellular (passive) and transcellular (active) pathway. Oxalate transport across cellular membranes is mediated by anion-exchange transport proteins. A defect in the structure of these transport proteins could explain augmented transcellular oxalate transport. Little is known about the physiological regulation of oxalate transport. In this review cellular transport systems for oxalate will be summarized with special attention for the progress that has been made to study oxalate transport in a model of cultured renal tubule cells. Better understanding of the physiological processes that are involved in oxalate transport could yield information on the basis of which it might be possible to design new approaches for an effective treatment of CaOx stone disease.

Effect of second messenger systems on oxalate uptake in renal epithelial cells

The oxalate transport system along with protein phosphorylation appears to be deranged in stone formers. This study was undertaken to characterize in LLC-PK1 cells in culture the effect of altering specific intracellular second messenger systems on oxalate uptake. Cellular uptake experiments were performed at 37 degrees C in buffer [265 mM mannitol, 5 mM NaOH, 5 mM KOH, 10 mM Ca-EGTA, 25 mM HEPES/TRIS, pH = 7.4 or in Hank's balanced salt solution (HBSS)] containing 200 microM labeled oxalate (1-14C, 0.3 microCi). Cells were preincubated with DAG (final concentration of 100 microM), phorbol myristate acetate (10 microM), forskolin (50 microM), 8-bromo-cyclic AMP (50 microM), trifluoroperazine (20 microM) and low molecular weight heparin (1 mg/ml) for 10 min in the presence and absence of the anion transport inhibitor DIDS (100 microM) and the effect(s) on oxalate uptake at 10, 25 and 45 min incubation were determined. Chemicals (DAG, forskolin, TPA and 8-bromo-cAMP) which stimulate protein kinase A or C activity resulted in an increased uptake of oxalate while inhibitors of these systems (trifluoroperazine and low molecular weight heparin) resulted in decreased oxalate uptake. The results demonstrate that oxalate uptake in renal tubular cells is modulated by protein kinase C and A dependent mechanisms.

Oxalate transport in a line of porcine renal epithelial cells--LLC-PK1 cells

The present studies examined oxalate handling in LLC-PK1 cells, an epithelial cell line of porcine origin. These cells appear to express transport systems for oxalate, as evidenced by the fact that uptake was saturable, time dependent and sensitive to the anion transport inhibitor DIDS (4,4'-diisothiocyanostilbene-2,2'-disulfonic acid). Oxalate uptake in these cells was also affected by the presence of certain inorganic anions (Cl-, SO4(2-), or HCO3-) but not by organic anions (para-aminohippurate, urate, malate, phenylsuccinate, succinate). This uptake was Na independent and unaffected by changes in membrane potential but was affected by external pH, with acidic pH stimulating and alkaline pH inhibiting oxalate accumulation. These findings suggest that LLC-PK1 cells express oxalate transporters similar to those observed in the mammalian renal cortex. Further studies using these cells may prove useful in defining the conditions that govern transcellular oxalate flux in renal epithelial cells.