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REGULATION OF MINERALIZATION IN SKELETAL TISSUES

REGULATION OF MINERALIZATION IN SKELETAL TISSUES
骨骼组织矿化的调节
批准号:
6534485
负责人:
THORSTEN KIRSCH
金额:
$24.56万
依托单位国家:
美国
项目类别:
财政年份:
2002
资助国家:
美国
项目状态:
已结题
起止时间:
2002-09-28 至 2004-08-31

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项目成果

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中文摘要
翻译
生物矿化在骨骼和牙齿发育过程中起着至关重要的作用,并允许骨骼组织在成年期发挥其应有的功能。 尽管其重要性显而易见,但人们对其监管知之甚少。 组织中矿物质形成的调节对于其正常功能至关重要。 例如,过多的矿物质沉积伴随着动脉粥样硬化和骨关节炎。 在后者中,关节表面区域的晶体形成可能在炎症的发作和关节破坏的进展中起主要作用。 另一方面,在骨质疏松症中看到的矿化损失导致骨骼脆弱和骨折。基质囊泡是一种由膜包裹的小颗粒,在颅面骨、长骨、软骨和牙本质等多种组织中具有启动矿化的关键作用。虽然已经确定这些颗粒是从质膜释放的,但尚不清楚基质囊泡的释放是如何调节的,以及囊泡在释放到细胞外基质中后如何启动矿物质形成。 在我们的初步研究中,它是第一次显示,只有细胞进行矿化释放膜联蛋白II和V丰富,钙/Pi复合物(核芯),含有基质囊泡,能够启动矿化,而nonmineralizing细胞释放囊泡不矿化。 此外,我们提供的证据表明,膜联蛋白II和V的形式在基质囊泡中的Ca 2+通道,使Ca 2+流入这些颗粒和第一腔内晶体的形成和生长。这些富含膜联蛋白II和V的基质囊泡的释放伴随着膜联蛋白II和V表达以及胞质Ca 2+浓度[Ca 2 +]i的增加。 我们的假设是,(i)增加细胞内Ca 2+浓度和膜联蛋白II和V的表达所需的释放的矿化能力的基质囊泡,和(ii)膜联蛋白II和V与核芯合作,使Ca 2+流入囊泡,形成的第一个矿物相和矿化的启动。 该项目将通过使用不同的实验策略直接测试这些假设,包括细胞培养,Ca 2+通道研究,定点诱变和突变膜联蛋白分子的表达。 目前的建议将提供一些最有趣的和重要的功能,调节体内矿化的新见解。 这一信息将是至关重要的,在病理条件下,在几个组织中的不受控制的矿化的预防。
英文摘要
Biomineralization plays a crucial role during skeletal and tooth development and allows skeletal tissues to exert their proper functions during adulthood. Despite its obvious importance little is known about its regulation. Regulation of mineral formation in tissues is critical for their proper function. For example, excessive mineral deposition accompanies atheriosclerosis and osteoarthritis. In the latter, crystal formation in the articular surface area may play a major role in the onset of inflammation and the progression of joint destruction. On the other hand, loss of mineralization as seen in osteoporosis leads to fragile bones and bone fractures. Matrix vesicles, small membrane-enclosed particles, have the critical role of initiating mineralization in many tissues, including craniofacial bones, long bones, cartilage and dentin. While it is well established that these particles are released from the plasma membrane, it is unclear how the release of matrix vesicles is regulated and how, following their release into the extracellular matrix, vesicles initiate mineral formation. In our Preliminary Studies it is shown for the first time that only cells undergoing mineralization release annexins II and V-rich, Ca2+/Pi complexes (nucleational core)-containing matrix vesicles which are able to initiate mineralization, while nonmineralizing cells release vesicles which do not mineralize. In addition, we provide evidence that annexins II and V form Ca2+ channels in matrix vesicles, allowing Ca2+ influx into these particles and the formation and growth of the first intralumenal crystals. Release of these annexins II and V-rich matrix vesicles is accompanied by increases in annexins II and V expression and cytosolic Ca2+ concentration, [Ca2+]i. Our hypotheses are that (i) increases in both cytosolic Ca2+ concentration and annexins II and V expression are required for the release of mineralization-competent matrix vesicles, and that (ii) annexins II and V cooperate with the nucleational core to enable Ca2+ influx into the vesicles, formation of the first mineral phase and initiation of mineralization. This project will test these hypotheses directly by the use of diverse experimental strategies, including cell culture, Ca2+ channel studies, site-directed mutagenesis and expression of mutated annexin molecules. The present proposal will provide new insights into some of the most intriguing and important features which regulate mineralization in vivo. This information will be of critical importance for the prevention of uncontrolled mineralization in several tissues during pathological conditions.
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