Zhu X L, Ganss B, Goldberg H A, Sodek J
Canadian Institutes of Health Research Group in Matrix Dynamics, Faculty of Dentistry, University of Toronto, ON.
Biochem Cell Biol. 2001;79(6):737-46.
Bone sialoprotein (BSP) and osteopontin (OPN) are sulphated and phosphorylated sialoglycoproteins that regulate the formation of hydroxyapatite crystals during de novo bone formation. To gain insights into the relationship between the synthesis and posttranslational modification of BSP and OPN and the mineralization of bone, pulse-chase studies were conducted on cultures of newly forming bone nodules produced by fetal rat calvarial cells in vitro. Cultures were pulse labelled with 35SO4, or with either 32PO4 or [gamma-32P]ATP to study intracellular and extracellular phosphorylation, respectively, and chased in isotope-free medium for various times up to 24 h. The presence of radiolabelled BSP and OPN was determined in the cells, in culture medium, and in various tissue compartments obtained by dissociative extraction with 4 M GuHCl (G1), 0.5 M EDTA (E), and again with 4 M GuHCl (G2) and a bacterial collagenase digestion of the demineralized collagenous tissue residue. With each isotope employed, radiolabelled BSP and OPN were detected in the E extract within the 1-h chase period and increased in amount with time. Similarly, 35SO4- and 32PO4-labelled BSP increased in the G2 extract, but OPN was not detected. In the G1 extract the 35SO4-labelled BSP decreased with chase time, whereas the 32PO4-labelled BSP increased. No differences were evident in the profiles of BSP labelled with 32PO4 or [gamma-32P]ATP. In the absence of beta-glycerophosphate, which is required for optimal mineralization of the bone nodules, 35SO4-labelled BSP was increased in the medium and G1 extract and decreased in the E extract and G2 extract after 3 h. In addition to differences in the tissue compartmentalization of BSP and OPN, these studies indicate that 35SO4 is lost from BSP during mineralization and that isoforms of BSP exist with a selective affinity for the organic and mineral phases. Moreover, the additional phosphorylation of BSP and OPN catalyzed by ectokinase activity does not appear to alter the distribution of these sialoproteins.
骨唾液蛋白(BSP)和骨桥蛋白(OPN)是硫酸化和磷酸化的唾液糖蛋白,在新生骨形成过程中调节羟基磷灰石晶体的形成。为了深入了解BSP和OPN的合成、翻译后修饰与骨矿化之间的关系,对体外培养的胎鼠颅骨细胞产生的新形成骨结节进行了脉冲追踪研究。分别用35SO4、32PO4或[γ-32P]ATP对培养物进行脉冲标记,以研究细胞内和细胞外磷酸化,然后在无同位素培养基中追踪长达24小时的不同时间。通过用4M盐酸胍(G1)、0.5M乙二胺四乙酸(E)解离提取,然后再次用4M盐酸胍(G2)和对脱矿质胶原组织残渣进行细菌胶原酶消化,测定细胞、培养基以及获得的各种组织部分中放射性标记的BSP和OPN的存在情况。使用每种同位素时,在1小时的追踪期内,在E提取物中检测到放射性标记的BSP和OPN,并且其含量随时间增加。同样,35SO4和32PO4标记的BSP在G2提取物中增加,但未检测到OPN。在G1提取物中,35SO4标记的BSP随追踪时间减少,而32PO4标记的BSP增加。用32PO4或[γ-32P]ATP标记的BSP的图谱没有明显差异。在缺乏骨结节最佳矿化所需的β-甘油磷酸的情况下,35SO4标记的BSP在3小时后在培养基和G1提取物中增加,而在E提取物和G2提取物中减少。除了BSP和OPN在组织分隔上的差异外,这些研究表明,在矿化过程中BSP会丢失35SO4,并且存在对有机相和矿相具有选择性亲和力的BSP同工型。此外,由胞外激酶活性催化的BSP和OPN的额外磷酸化似乎不会改变这些唾液蛋白的分布。