Pathophysiology
According to the World Health Organization "Evidence suggests that podoconiosis is the result of a genetically determined abnormal inflammatory reaction to mineral particles in irritant red clay soils derived from volcanic deposits".The pathophysiology of podoconiosis is a combination of genetic susceptibility, possibly through associations with HLA-DQA1, HLA-DQB1, and HLA-DRB1 variants, and a cumulative exposure to irritant soil. In susceptible individuals, irritant soil particles penetrate the feet and collect in lymphatic vessels. Over time, chronic inflammation within the lymphatic vessels leads to fibrosis and occlusion. Diagnosis
Differential diagnosis
The differential diagnosis for podoconiosis includes other causes of tropical lymphedema, such as filariasis or leprosy, and mycetoma pedis.While filariasis is generally unilateral, podoconiosis affects the legs bilaterally albeit asymmetrically and in an ascending manner. Podoconiosis very rarely affects the groin while filariasis frequently involves the groin: a high ratio of lymphoedema/hydrocele cases in an area suggests podoconiosis as the dominant cause of lymphedema. In some cases, the history and clinical presentation alone are unable to differentiate between the two causes of tropical lymphedema. Local epidemiology can also be a clue to diagnosis, as podoconiosis is typically found in higher altitude areas with volcanic soils while filariasis is common in low-lying areas where mosquitos are prevalent. Blood smears for identification of microfilariae and antigen detection techniques can be helpful in the diagnosis of lymphatic filariasis.Lepromatous lymphedema can also mimic podoconiosis clinically, but the former will have loss of sensation in the toes and feet, thickened nerves, and trophic ulcers. Other causes of lymphedema include Kaposi sarcoma, mycetoma, and elephantiasis nostras verrucosa.
A recent review has summarized the global distribution of podoconiosis. In some areas of Ethiopia, the prevalence is as high as 4%. The incidence of podoconiosis increases with age, likely due to cumulative exposure to irritant soil. It is very rare to see podoconiosis in the 0–5 year old age group, and the incidence rapidly rises from 6 to 20 years of age, with the highest prevalence after 45 years of age. Podoconiosis is most commonly seen in higher altitude areas with volcanic soil, and it is estimated to affect 4 million people worldwide. Productivity losses associated with the disease are significant. In Ethiopia (where 1.6 million people are estimated to be affected), the condition is thought to have caused US $200 million in lost productivity per year in 2004. History
After parasitic filariae were discovered to be an important cause of tropical lymphedema in the 19th century, early investigators assumed that filariae were the sole cause of lymphedema in the tropics. It was later discovered that the distribution of tropical lymphedema and filariasis did not perfectly overlap, and researchers began to recognize that some forms of tropical lymphedema were not associated with filariasis. Ernest W Price, a British surgeon living in Ethiopia, discovered the true etiology of podoconiosis in the 1970s and 1980s by studying the lymph nodes and vessels of those afflicted with the disease. Using light microscopy, he observed macrophage cells laden with micro-particles in lymph nodes of the affected extremity.