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牙本质形成过程中的钙转运。对大鼠切牙成牙本质细胞的一项实验研究。

Calcium transport in dentinogenesis. An experimental study in the rat incisor odontoblast.

作者信息

Lundgren T

机构信息

Department of Oral Biochemistry, University of Göteborg, Sweden.

出版信息

Swed Dent J Suppl. 1992;82:1-91.

PMID:1329245
Abstract

Since cellular calcium transport mechanisms during biological calcification are less known, a series of experiments were performed by in vivo as well as in vitro methodologies in the dentinogenically active rat incisor. By means of micro-electrode technique, the pH and pCa (calcium ion activity) in predentin in situ were found to be 7.0 and 2.9, respectively. It was concluded that there exists a Ca2+ion concentrating mechanism over the odontoblast layer in direction towards the mineralization front. The kinetics of this calcium flow was determined in vivo by radiotracer technique. The time for 45Ca2+ uptake into the dentin mineral phase was determined to 10-15 min. Transmembraneous Ca2+ ion pumps and channels in odontoblasts were further analyzed. The resting membrane potential of rat incisor odontoblasts was determined to -24 mV. Using ion-specific mini-electrode technique as well as fluorescence spectrophotometry, calcium channels, Ca(2+)-ATPase and Na+/Ca2+ antiports, responsible for cellular Ca2+ uptake and extrusion, were identified in the odontoblast plasma membrane. Dissected odontoblasts were subjected to subcellular fractionation. An electrophoretic uniporter and a Na2+/Ca2+ exchanger, for Ca2+ release and uptake, respectively, were demonstrated in mitochondria, whereas a Ca(2+)-ATPase was present in the microsomal fraction. Mitochondria, microsomes and whole, digitonin-permeabilized odontoblasts, were able to maintain a steady state Ca2+ activity at pCa = 6.4-6.6 in vitro. In rats treated with colchicine, the incorporation of 45Ca2+ into dentin mineral was severely altered. Similarly, administration to rats of specific calcium channel blockers strongly inhibited 45Ca2+ incorporation. Together, the results indicate that a transcellular pathway is a major route for Ca2+ ion transport during dentinogenesis, and that this may be under a relatively strict cellular control.

摘要

由于生物矿化过程中的细胞钙转运机制尚不为人所知,因此采用体内和体外方法,在具有牙本质生成活性的大鼠切牙上进行了一系列实验。通过微电极技术,发现原位前期牙本质中的pH值和pCa(钙离子活性)分别为7.0和2.9。得出的结论是,在成牙本质细胞层上方朝着矿化前沿的方向存在Ca2+离子浓缩机制。通过放射性示踪技术在体内测定了这种钙流的动力学。45Ca2+摄取到牙本质矿质相中的时间确定为10 - 15分钟。进一步分析了成牙本质细胞中的跨膜Ca2+离子泵和通道。大鼠切牙成牙本质细胞的静息膜电位确定为 - 24 mV。使用离子特异性微电极技术以及荧光分光光度法,在成牙本质细胞质膜中鉴定出负责细胞摄取和排出Ca2+的钙通道、Ca(2+)-ATP酶和Na+/Ca2+反向转运体。对分离出的成牙本质细胞进行亚细胞分级分离。在线粒体中分别证明了一种用于Ca2+释放和摄取的电泳单向转运体和一种Na2+/Ca2+交换体,而在微粒体部分存在一种Ca(2+)-ATP酶。线粒体、微粒体以及经洋地黄皂苷通透处理的完整成牙本质细胞在体外能够在pCa = 6.4 - 6.6维持稳定状态的Ca2+活性。在用秋水仙碱处理的大鼠中,45Ca2+掺入牙本质矿质的情况发生了严重改变。同样,给大鼠施用特定的钙通道阻滞剂会强烈抑制45Ca2+的掺入。总之,结果表明跨细胞途径是牙本质形成过程中Ca2+离子转运的主要途径,并且这可能受到相对严格的细胞控制。

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