Abstract

Submitral calcification or sclerosis was visualized with M mode echocardiography in 84 elderly patients, 35 of whom were also studied with two dimensional echocardiography. Posterior Submitral calcification, commonly referred to as “mitral anulus calcification,” was present in 82 patients and was located in the angle between the posterior mitral leaflet and left ventricular posterior wall, rather than in the mitral anulus proper. M mode scans from the left ventricle to the left atrium showed that posterior submitral calcification ended abruptly in 66 cases, and in these it became contiguous with the posterior atrioventricular junction (true mitral anulus) in only 14 instances. In 16 patients the posterior submitral calcification sloped anteriorly to merge with the posterior aortic root. Anterior submitral calcification was visualized in 12 patients, 10 of whom also had posterior submitral calcification. Anterior submitral calcification was usually located immediately anterior to the base of the anterior mitral cusp. In two cases, it appeared to arise in the region between the aortic and mitral rings; in one instance, it was located in the mid left ventricle, in the mitral chordal region. We suggest that the terms anterior and posterior submitral calcification are more appropriate than “mitral anulus calcification” because in most cases such calcific deposits do not appear to be located in or to arise from the true mitral anulus.

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