Primary hyperoxaluria
Primary hyperoxaluria is a rare genetic condition characterized by the overproduction of oxalate, leading to recurrent kidney stones and potential kidney failure.
Overview
Primary hyperoxaluria results from the overproduction of a substance called oxalate. This leads to abnormally high levels of oxalate in the urine (hyperoxaluria). Oxalate can combine with calcium to form calcium oxalate, which creates hard deposits in the kidneys and bladder. Over time, these deposits can damage the kidneys, leading to end-stage renal disease (ESRD).
Symptoms
- Recurrent kidney and bladder stones.
- Blood in the urine (hematuria).
- Urinary tract infections.
- Kidney damage and potential end-stage renal disease (ESRD).
- Systemic oxalosis: As kidney function declines, oxalate levels in the blood rise and deposit in tissues throughout the body, particularly in bones and blood vessel walls.
- Bone fractures (due to oxalosis in the bones).
Types and Causes
There are three types of primary hyperoxaluria, each caused by mutations in specific genes that provide instructions for enzymes involved in breaking down protein building blocks and other compounds:
- Type 1: Caused by mutations in the AGXT gene. Kidney stones typically appear from childhood to early adulthood.
- Type 2: Caused by mutations in the GRHPR gene. Similar to type 1, but ESRD typically develops later in life.
- Type 3: Caused by mutations in the HOGA1 gene. Affected individuals often develop kidney stones in early childhood.
Inheritance
This condition is inherited in an autosomal recessive pattern, meaning both copies of the gene in each cell have mutations. The parents of an individual with an autosomal recessive condition each carry one copy of the mutated gene but typically do not show signs or symptoms of the condition.
