Hammer W J, Roberts W C, deLeon A C
Am J Med. 1978 Mar;64(3):371-6. doi: 10.1016/0002-9343(78)90214-0.
Certain observations are described in four elderly women with massive mitral anular calcific deposits, small thick-walled left ventricles and diastolic gradients between pulmonary artery wedge position (or left atrium) and left ventricle. All four patients had some degree of obstruction to left ventricular outflow. Examination at necropsy (two patients) or at operation (one patient) disclosed only focal fibrous thickening of the mitral leaflets without commissural or chordal fusion. By auscultation, none had mitral opening snaps, only two had loud first heart sounds and only one had a mitral diastolic rumble. Hemodynamic documentation of a diastolic gradient between pulmonary artery wedge position (or left atrium) and left ventricle in the presence of massive mitral anular calcific deposits and in the absence of diffuse disease of the mitral leaflets has not been demonstrated previously. The diastolic gradients are considered to result from the combination of the large mitral anular calcific deposits and the small, thick-walled, noncompliant left ventricles.
在四名老年女性中观察到某些情况,她们有大量二尖瓣环钙化沉积物、小而厚壁的左心室,以及肺动脉楔压位置(或左心房)与左心室之间的舒张期压差。所有四名患者均有一定程度的左心室流出道梗阻。尸检(两名患者)或手术(一名患者)检查发现二尖瓣叶仅有局灶性纤维增厚,无瓣叶联合或腱索融合。听诊时,无人有二尖瓣开瓣音,只有两人有响亮的第一心音,只有一人有二尖瓣舒张期隆隆样杂音。在存在大量二尖瓣环钙化沉积物且无二尖瓣叶弥漫性病变的情况下,肺动脉楔压位置(或左心房)与左心室之间舒张期压差的血流动力学记录此前尚未得到证实。舒张期压差被认为是由大量二尖瓣环钙化沉积物与小而厚壁、顺应性差的左心室共同作用所致。