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Caplan’s Syndrome – Rheumatoid Pneumoconiosis

 A coal miner developed rheumatoid arthritis aged 52. He had worked in the coal mining industry for 32 years, with 8 years on the coal face, at a time when dust levels were high. He presented with joint pains, but when examination revealed rheumatoid nodules on his elbows, he commented that he had noticed these for approximately two years and that he had joint pain for about the same time, which he had attributed to “getting old”. Typical “Caplan nodules” were seen on his chest radiograph (Fig 1). He died aged 57 from a coronary thrombosis. Post-mortem lung examination confirmed the diagnosis and also showed background nodulation compatible with coalworkers’ pneumoconiosis (Fig 2).

 Caplan’s syndrome was first described in 1953 in coal workers who had both progressive massive fibrosis and seropositive rheumatoid arthritis.  It has since been described in other pneumoconioses caused by silica inhalation and non-asbestos silicate minerals. Chest radiographs showed rounded opacities ranging from 0.5 to 5cm in diameter, different from the opacities due to coal workers’ pneumoconiosis or PMF, and peripheral in distribution.  The nodules were characteristically well defined by their layered pattern.  Histopathology showed central necrosis surrounded by new concentric layers of collagen interspersed with polymorphonuclear leukocytes and a few macrophages.  This region represented the active zone of inflammation and could be used to differentiate from non-rheumatoid pneumoconiotic nodules. 

 Nodules normally develop with onset of joint disease but can occasionally occur before any symptoms. They may remain stable in size for months or years, but also enlarge as new lesions develop, and occasionally spontaneously regress. Other manifestations of rheumatoid arthritis (e.g. pleural effusion, basal interstitial fibrosis) may also be found.  The relationship between level and duration of dust exposure and the development of disease is controversial, but exposure to anthracite coal appears to be a particular risk factor. An increased incidence of circulating positive rheumatoid factor among miners with PMF has been reported, but Caplan’s syndrome has also been described in young miners with little or no coal workers’ pneumoconiosis following short exposures. It is of interest that the syndrome occurred more commonly in the Welsh mines and that incidence has fallen markedly with dust control measures.

 

         
   
   

Figure 1.                                                                       Figure 2.