Although often supersaturated with mineral salts such as calcium phosphate and calcium oxalate, normal urine possesses an innate ability to keep them from forming harmful crystals. This inhibitory activity has been attributed to the presence of urinary macromolecules, although controversies abound regarding their role, or lack thereof, in preventing renal mineralization. Here, we show that 10% of the mice lacking osteopontin (OPN) and 14.3% of the mice lacking Tamm-Horsfall protein (THP) spontaneously form interstitial deposits of calcium phosphate within the renal papillae, events never seen in wild-type mice. Lack of both proteins causes renal crystallization in 39.3% of the double-null mice. Urinalysis revealed elevated concentrations of urine phosphorus and brushite (calcium phosphate) supersaturation in THP-null and OPN/ THP-double null mice, suggesting that impaired phosphorus handling may be linked to interstitial papillary calcinosis in THP-but not in OPN-null mice. In contrast, experimentally induced hyperoxaluria provokes widespread intratubular calcium oxalate crystallization and stone formation in OPN/THP-double null mice, while completely sparing the wild-type controls. Whole urine from OPN-, THP-, or double-null mice all possessed a dramatically reduced ability to inhibit the adhesion of calcium oxalate monohydrate crystals to renal epithelial cells. These data establish OPN and THP as powerful and functionally synergistic inhibitors of calcium phosphate and calcium oxalate crystallization in vivo and suggest that defects in either molecule may contribute to renal calcinosis and stone formation, an exceedingly common condition that afflicts up to 12% males and 5% females. kidney stone; urolithiasis; uromodulin CLINICAL KIDNEY STONE DISEASE is classified into a number of forms, each requiring a specific plan for medical treatment. It has only been recently demonstrated through a series of biopsy studies of renal papillae from human stone formers that the different stones can develop through different pathways (7,13). Whether the pathogenetic process leading to stone formation involves interstitial plaque or intratubular crystal deposits, a range of host factors appears to be involved, some acting as facilitators and others as inhibitors. Under normal conditions, there is a fine equilibrium between pro-and anticrystallization forces, which helps keep the kidneys stone-free so that they can carry out important physiological functions. However, when the equilibrium breaks down, urine constituents can precipitate out, allowing insoluble crystals to form. Although the mechanisms that mediate retention of urinary crystals into stones remain poorly defined, it is clear that the degree of urinary supersaturation predicts stone risk and type (24,28,38). Furthermore, the urine of most individuals is frequently supersaturated with calcium oxalate and calcium phosphate. These observations suggest a critical role for urinary supersaturation and inhibitors of crystallization. This paradigm of nephrolithiasis has ...