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骨质石化症:“大理石骨病”的发现与早期历史

Osteopetrosis: Discovery and early history of "marble bone disease".

作者信息

Whyte Michael P

机构信息

Division of Bone and Mineral Diseases, Department of Internal Medicine, Washington University School of Medicine, St. Louis, MO 63110, USA; Shriners Hospitals for Children-St. Louis, St. Louis, MO 63110, USA.

出版信息

Bone. 2023 Jun;171:116737. doi: 10.1016/j.bone.2023.116737. Epub 2023 Mar 16.

DOI:10.1016/j.bone.2023.116737
PMID:36933855
Abstract

Discovery in 1904 of the disorder initially called "marble bones", then in 1926 more appropriately referred to as "osteopetrosis", is attributed to Heinrich E. Albers-Schönberg (1865-1921), the first radiologist. He used the new technique of "Röntgenographie" to report in a young man the radiographic hallmarks of this osteopathy. Clinical descriptions of lethal forms of osteopetrosis had apparently been published earlier by others. In 1926, "osteopetrosis" (stony or petrified bones) replaced "marble bone disease" because the skeletal fragility resembled limestone more than marble. In 1936, despite fewer than 80 reported patients, a fundamental defect in hematopoiesis, secondarily impacting the entire skeleton, was hypothesized. By 1938, the signature histopathological finding of osteopetrosis was recognized -- persistence of unresorbed calcified growth plate cartilage. Also, it was apparent that besides lethal autosomal recessive osteopetrosis a less severe form was "handed down directly from generation to generation". In 1965, quantitative, but also qualitative, defects in osteoclasts became apparent. Here, I review the discovery and early understanding of osteopetrosis. Characterization of this disorder commencing at the beginning of the past century would support the aphorism of Sir William Osler (1849-1919): "Clinics Are Laboratories; Laboratories Of The Highest Order". As featured in this special issue of Bone, the osteopetroses would prove remarkably informative about the formation and function of the cells responsible for skeletal resorption.

摘要

1904年发现了这种最初被称为“大理石骨病”的病症,1926年更恰当地称为“骨硬化症”,这一发现归功于首位放射科医生海因里希·E·阿尔伯斯-舍恩伯格(1865 - 1921)。他运用“X线摄影术”这项新技术,报告了一名年轻男性身上这种骨病的影像学特征。显然,其他人此前已发表过关于致死性骨硬化症的临床描述。1926年,“骨硬化症”(骨质坚硬如石或石化)取代了“大理石骨病”,因为骨骼的脆弱程度更像石灰石而非大理石。1936年,尽管报告的患者不足80例,但人们推测造血存在根本性缺陷,继而影响整个骨骼。到1938年,骨硬化症标志性的组织病理学发现得到确认——未吸收的钙化生长板软骨持续存在。此外,很明显除了致死性常染色体隐性骨硬化症外,还有一种病情较轻的类型“代代直接遗传”。1965年,破骨细胞的定量及定性缺陷变得明显。在此,我回顾骨硬化症的发现及早期认识。从上世纪初开始对这种病症的特征描述将支持威廉·奥斯勒爵士(1849 - 1919)的格言:“临床即实验室;最高等级的实验室”。正如本期《骨》特刊所展示的,骨硬化症对于负责骨骼吸收的细胞的形成和功能具有显著的启示作用。

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