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软骨钙化部位液体中钙化大分子抑制剂和成核因子的展示。

Demonstration of macromolecular inhibitors of calcification and nucleational factors in fluid from calcifying sites in cartilage.

作者信息

Howell D S, Pita J C, Marquez J F, Gatter R A

出版信息

J Clin Invest. 1969 Apr;48(4):630-41. doi: 10.1172/JCI106021.

Abstract

An extracellular fluid phase (C(f1)), aspirated by micropuncture techniques from the hypertrophic cell zone of calcifying epiphyseal certilage, has been characterized in a calcifying system in vitro in respect to the behavior of sedimenting and supernatant fractions after high speed ultracentrifugation. To perform these tests on the starting samples of 20 nl of C(f1), macroscopic analytical methods were scaled down for the identification of relevant organic components, including hexuronic acid and proteinpolysaccharides (PPL). The mineral accretion system was designed to simulate physiologic conditions in the calcifying cartilage septa of normal rats, and the mineral used for seeding was an immature calcium phosphate similar to native cartilage mineral. Normal C(f1) or its dilutions in synthetic lymph up to 1:4 completely prevented mineral accretion in vitro. The inhibitory action was localized to the sedimented fractions after ultracentrifugation and could be destroyed by incubation with trypsin or hyaluronidase. The sediment of C(f1) contained 2 mg of hexuronic acid per ml of C(f1) and gave a strong reaction of identification for a light fraction of PPL by fluorescent antibodies to rat PPL. PPL fractions were tested in the same mineral accretion systems as C(f1) and exhibited responses similar to those of C(f1). Also, there was evidence of a mineral phase in C(f1) of normal rats, in C(f1) of rats with healing rickets, but not in C(f1) of untreated rachitic rats. These results are interpreted to indicate that certain PPLs function as an inhibitor of crystal growth at extracellular sites premonitory to calcification. Evidence for a low density inhibitor of mineral accretion was found in normal serum but not in C(f1).

摘要

通过微穿刺技术从钙化骺软骨肥大细胞区吸出的细胞外液相(C(f1)),已在体外钙化系统中就高速超速离心后沉降和上清部分的行为进行了表征。为了对20 nl C(f1)的起始样品进行这些测试,宏观分析方法被缩小规模以鉴定相关有机成分,包括己糖醛酸和蛋白多糖(PPL)。矿物质沉积系统旨在模拟正常大鼠钙化软骨隔中的生理条件,用于接种的矿物质是一种类似于天然软骨矿物质的未成熟磷酸钙。正常的C(f1)或其在合成淋巴液中高达1:4的稀释液在体外完全阻止了矿物质沉积。抑制作用定位于超速离心后的沉降部分,并且可以通过与胰蛋白酶或透明质酸酶孵育而被破坏。C(f1)的沉淀物每毫升C(f1)含有2 mg己糖醛酸,并通过针对大鼠PPL的荧光抗体对PPL的轻组分产生强烈的鉴定反应。PPL组分在与C(f1)相同的矿物质沉积系统中进行测试,并表现出与C(f1)相似的反应。此外,在正常大鼠的C(f1)、愈合佝偻病大鼠的C(f1)中存在矿物质相的证据,但在未经治疗的佝偻病大鼠的C(f1)中没有。这些结果被解释为表明某些PPL在钙化前期的细胞外部位作为晶体生长的抑制剂起作用。在正常血清中发现了矿物质沉积的低密度抑制剂的证据,但在C(f1)中没有。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/eec8/322268/b104354abbab/jcinvest00210-0076-a.jpg

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