Images and Case Reports in Heart Failure |
From the Departments of Internal Medicine Cardiology, (U.M.M., S.G., G.C.S.), and Diagnostic and Interventional Radiology (M.G.), University of Leipzig, Heart Centre, Leipzig, Germany.
Correspondence to Ulrike M. Müller, MD, Department of Internal Medicine/Cardiology, University of Leipzig, Heart Centre, Strümpellstr. 39, D-04289 Leipzig, Germany. E-mail ulrike.mueller@herzzentrum-leipzig.de
An extract of the first 250 words of the full text is provided, because this article has no abstract. |
| Introduction |
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Electrocardiogram showed normofrequent atrial fibrillation. Transthoracic echocardiography indicated moderate biatrial enlargement, although both ventricles had normal dimensions and normal global systolic function. The transmitral prosthetic valve gradient was 14/6 mm Hg. We documented severe tricuspid regurgitation and only mild mitral regurgitation. Nevertheless, echocardiography was difficult to perform because of lack of an adequate acoustic window and metal artifacts of the mitral valve prosthesis. Reflections at the epicardial surface close to the mitral valve were therefore interpreted as calcifications of pericardial layer, and constrictive pericarditis was expected to be the most likely cause of the patients symptoms and diastolic left ventricle dysfunction.
By right heart catheterization, severe postcapillary hypertension was confirmed (systolic/diastolic/mean pulmonary artery pressure, 65/23/43 mm Hg; mean pulmonary wedge pressure, 29 mm Hg). In all cardiac cavities, an end-diastolic pressure equilibration was measured (Figure 1). Pressure curves did not show a dip-plateau phenomenon. Therefore, constrictive pericarditis was excluded. However, in a 64-row multidetector computed tomography scan, the endocardial layer of the left atrium (LA) and the aortic arch were heavily calcified (Figure 2), whereas the pericardium itself did not show any relevant calcifications. As an additional finding, the patient showed tracheobronchopathia osteoplastica (Figure 2A and
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