Odontoblast phosphate and calcium transport in dentinogenesis.

Swedish dental journal. Supplement Pub Date : 2002-01-01
Patrik Lundquist
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Abstract

It has been suggested that odontoblasts are instrumental in translocating Ca2+ and inorganic phosphate (Pi) ions during the mineralization of dentin. The aim of this thesis was, therefore, to study the expression of components of the transcellular ion transport system, Na+/Ca2+ exchangers and Na(+)-Pi contransporters, in odontoblastic and osteoblastic cells. Their activity was assayed in osteoblast-like cells and in the recently developed MRPC-1 odontoblast-like cell line. To assess the relationship between ion transport and mineralization, Ca2+ and Pi uptake activities were determined in mineralizing cultures of MRPC-1 cells. Osteoblastic and odontoblastic cells showed an identical expression pattern of Na+/Ca2+ exchanger splice-variants, NCX1.3, NCX1.7 and NCX1.10, derived from the NCX1 gene, while NCX2 was not expressed. The cells showed a high sodium-dependent calcium extrusion activity. Regarding Na(+)-Pi cotransporter expression, Glvr-1, Ram-1 and the two high capacity cotransporters Npt-2a and Npt-2b were found to be expressed in odontoblasts and MRPC-1 cells. Osteoblast-like cells differed from this in expressing the Npt-1 but not the Ram-1 gene but were otherwise identical to the odontoblastic cells. Odontoblast-like cells exhibited almost twice the sodium-dependent Pi uptake activity of osteoblast-like cells. The presence of NaPi-2a and NaPi-2b, gene products of Npt-2a and Npt-2b, was verified in vivo by immunohistochemistry on mouse teeth. Both cotransporters could be detected in fully differentiated, polarized odontoblasts but not in preodontoblasts prior to dentin formation. Both cotransporters were detected in adjacent bone and in ameloblasts. Studying ion uptake in mineralizing MRPC-1 cultures, large changes were detected concomitant with the onset of mineral formation, when phosphate uptake increased by 400% while calcium uptake started to decline. The increase in Pi uptake was found to be due to activation of the NaPi-2a cotransporter. MRPC-1 cells expressed an odontoblast-like phenotype already at the onset of culture, but in order to form mineral a differentiation involving their ion transporters seems necessary. Calculating the theoretical rate of ion transport needed for dentin formation and comparing with data from the studies in this thesis showed that transcellular ion transport is both possible and sufficient to meet the phosphate and calcium demands of dentinogenesis.

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牙本质形成过程中成牙本质细胞的磷酸盐和钙转运。
在牙本质矿化过程中,成牙细胞在钙离子和无机磷酸盐(Pi)离子的转运中起着重要作用。因此,本论文的目的是研究跨细胞离子运输系统的组成部分,Na+/Ca2+交换器和Na(+)-Pi共转运体在成牙细胞和成骨细胞中的表达。在成骨细胞样细胞和最近发展的MRPC-1成牙细胞样细胞系中测定了它们的活性。为了评估离子运输和矿化之间的关系,在矿化培养的MRPC-1细胞中测定了Ca2+和Pi摄取活性。成骨细胞和成牙细胞显示出相同的Na+/Ca2+交换器剪接变体NCX1.3、NCX1.7和NCX1.10的表达模式,来源于NCX1基因,而NCX2不表达。细胞表现出高钠依赖性钙挤压活性。在Na(+)-Pi共转运体表达方面,发现Glvr-1、Ram-1和两种高容量共转运体Npt-2a和Npt-2b在成牙细胞和MRPC-1细胞中均有表达。成骨细胞样细胞在表达nt -1基因而非Ram-1基因方面与此不同,但在其他方面与成牙细胞相同。成骨细胞样细胞表现出几乎是成骨细胞样细胞钠依赖性Pi摄取活性的两倍。通过小鼠牙齿免疫组化,证实了Npt-2a和Npt-2b基因产物NaPi-2a和NaPi-2b的存在。这两种共转运蛋白均可在完全分化、极化的成牙本质细胞中检测到,但在牙本质形成前的成牙本质细胞中未检测到。在相邻骨和成釉细胞中均检测到这两种共转运蛋白。研究矿化MRPC-1培养物的离子摄取,发现随着矿物形成的开始,磷酸盐的摄取增加了400%,而钙的摄取开始下降。Pi摄取的增加被发现是由于激活了NaPi-2a共转运蛋白。MRPC-1细胞在培养开始时已经表达了成牙细胞样表型,但为了形成涉及离子转运体的矿物分化似乎是必要的。计算牙本质形成所需离子传输的理论速率,并与本论文的研究数据进行比较,表明跨细胞离子传输既可能又足够满足牙本质形成对磷酸盐和钙的需求。
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