
104 Shah, Holmes, and Assimos
human diets. It is a metabolic end product in humans that is linked to a variety of vital
pathways, including gluconeogenesis, glycolysis, ureagenesis, pentose–phosphate path-
way, glyoxylate pathway, serine pathway, and xylulose pathway (1).
Oxalate is freely filtered through the glomerulus and secretory fluxes may also occur
(2–5). Oxalate transport in proximal tubular cells may be complex because it seem to
plays a role as a recycling substrate that functionally links the transcellular absorption
of chloride to that of other anions such as bicarbonate and sulfate (6,7). At the basolateral
membrane, oxalate enters the cell in exchange for sulfate or bicarbonate (6–8). At the
luminal brush border membrane, oxalate can be transported out of the cell in exchange
for chloride and may be transported back into the cell in exchange for sulfate (6, 7).
There is also evidence that oxalate exchange may occur in the distal tubule (9). Various
anion exchange proteins mediate these processes (10,11).
Oxalate is absorbed all along the gastrointestinal tract, including the stomach (12).
Absorptive and secretory pathways for oxalic acid regulated by substances that direct the
net oxalate ion flux have been identified in the proximal and distal segments of rat colon
(13–16). Cations such as calcium and magnesium complex with oxalate in the alimen-
tary tract and limit its absorption. The free anionic form of oxalate is thought to be the
one that is absorbed. Recent oxalate loading studies in healthy volunteers have demon-
strated that oxalate absorption varies tremendously, with 2–18% of a dietary oxalate load
in normal individuals being absorbed (17). In addition, the time sequences of absorption
studies suggest that a significant amount of oxalate is absorbed in the small intestine in
humans. Oxalate is also degraded in the colon by oxalate-degrading bacteria such as
Oxalobacter formigenes and other organisms (18). The actual role that this bacterium
plays in altering intestinal oxalate content and oxalate absorption has not been well
characterized.
A role for the intestinal absorption of dietary oxalate in stone formation was suggested
by the studies of Curhan and associates (19,20). A low-calcium intake was shown to be
a significant risk factor for stone development. The explanation for this finding is that
calcium complexes with oxalate in the alimentary tract thus limiting oxalate absorption.
Metabolic studies in humans support this theory. We demonstrated a 34% increase in
urinary oxalate excretion in normal adult subjects when dietary calcium is reduced from
1002 mg to 391 mg/d while other dietary constituents are unchanged, which is consistent
with this theory (21). In addition, Liebman and Chai found that supplemental calcium
decreased the absorption of an oxalate load in humans by more than 50% (22).
Studies have shown that supraphysiologic concentrations of oxalate can damage
cultured renal tubular cells through free-radical-induced oxidative stress (23–27). Expo-
sure of a line of human renal epithelial cells, HK-2, to oxalate resulted in a programmed
sequence of events that led to an increase in membrane permeability, alterations in cell
morphology and viability, and the re-initiation of DNA synthesis (23). It has been
hypothesized that this concentration-dependent damage promotes a release of lipid-
rich cellular membranes that act as a nidus for crystal nucleation and retention, which
likely leads to lithogenesis (28–31). Although there is currently no evidence that such
events occur in human stone formers, stones do contain lipids in their matrix (32).
The roles of oxalate and calcium in the lithogenic process have nearly always been
attributed to their impact on the supersaturation of urine with calcium oxalate. Some
studies have demonstrated that supersaturation of calcium oxalate in stone formers does
not differ significantly from that in nonstone formers (33,34). However, Borghi et al.
have shown that oxalate-loading in calcium oxalate stone formers was associated with