Cystine Nephrolithiasis
Also known as: Cystinuria Stones
Cystine stones result from cystinuria, an autosomal recessive (rarely incomplete dominant) disorder of renal tubular and intestinal transport of the dibasic amino acids cystine, ornithine, lysine and arginine (COLA). It affects about 1 in 7,000 births and accounts for 1 to 2 percent of adult stones and 6 to 8 percent of paediatric stones.
Stones are recurrent, bilateral and often multiple, and the lifetime burden of repeated surgery and chronic kidney disease is high.
Genetics and mechanism:
- Mutations in SLC3A1 (type A, encoding rBAT) or SLC7A9 (type B, encoding b0,+AT) cause the disorder.
- Reabsorption of filtered cystine in the proximal tubule fails. Urinary cystine rises above 400 mg per day in homozygotes (normal below 30 to 60 mg).
- Cystine is poorly soluble at urinary pH below 7.0. Solubility is about 250 mg/L at pH 5 to 7, rising sharply above pH 7.5. It therefore crystallises and forms stones.
Clinical pattern:
- Presentation is usually in the first to third decades.
- Stones are recurrent, bilateral and often multiple. Staghorn calculi form in 10 to 30 percent.
- The stones are hard, waxy, yellow, and faintly radiopaque (due to sulphur content).
- Chronic kidney disease develops in about 17 to 70 percent.













