{"title":"棘突大鼠类骨的基质囊泡与钙化。","authors":"T F Johnson, D C Morris, H C Anderson","doi":"","DOIUrl":null,"url":null,"abstract":"<p><p>Tibiae from rachitic weanling rats were studied during healing to examine the mechanism of bone mineralization. Rickets was induced by feeding the animals a low phosphate, low vitamin D diet for five weeks. Calcification was reinstituted in three ways; group I animals received 1.0 ml of NaH2PO4 i.p. and the rachitogenic diet in a darkened room; group II animals were placed in a lighted room and given standard laboratory chow; group III animals were placed in lighted room, given standard laboratory chow and received 1.0 ml of 0.1M NaH2PO4 i.p. Group I healed slowly while II and III were found to heal rapidly and at nearly identical rates. Groups II and III revealed a significantly elevated serum alkaline phosphatase activity and became hyperphosphatemic as the rickets healed suggesting a more vigorous recovery. Ultrastructurally, numerous matrix vesicles were noted in unhealed rachitic bone matrix and these structures acquired mineral upon initiation of healing. Vesicle-associated mineral aggregates increased in size penetrating through and beyond the vesicle membrane and were incorporated into the advancing mineralization front. By 48 hrs. post-healing initiation, the osteoid borders were almost completely mineralized in groups II and III. These observations suggest that in addition to pre-existing mineral, matrix vesicles can also serve as nucleating sites in the osteoid of post-fetal bone.</p>","PeriodicalId":73745,"journal":{"name":"Journal of Experimental Pathology","volume":"4 3","pages":"123-32"},"PeriodicalIF":0.0000,"publicationDate":"1989-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Matrix vesicles and calcification of rachitic rat osteoid.\",\"authors\":\"T F Johnson, D C Morris, H C Anderson\",\"doi\":\"\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p><p>Tibiae from rachitic weanling rats were studied during healing to examine the mechanism of bone mineralization. Rickets was induced by feeding the animals a low phosphate, low vitamin D diet for five weeks. Calcification was reinstituted in three ways; group I animals received 1.0 ml of NaH2PO4 i.p. and the rachitogenic diet in a darkened room; group II animals were placed in a lighted room and given standard laboratory chow; group III animals were placed in lighted room, given standard laboratory chow and received 1.0 ml of 0.1M NaH2PO4 i.p. Group I healed slowly while II and III were found to heal rapidly and at nearly identical rates. Groups II and III revealed a significantly elevated serum alkaline phosphatase activity and became hyperphosphatemic as the rickets healed suggesting a more vigorous recovery. Ultrastructurally, numerous matrix vesicles were noted in unhealed rachitic bone matrix and these structures acquired mineral upon initiation of healing. Vesicle-associated mineral aggregates increased in size penetrating through and beyond the vesicle membrane and were incorporated into the advancing mineralization front. By 48 hrs. post-healing initiation, the osteoid borders were almost completely mineralized in groups II and III. These observations suggest that in addition to pre-existing mineral, matrix vesicles can also serve as nucleating sites in the osteoid of post-fetal bone.</p>\",\"PeriodicalId\":73745,\"journal\":{\"name\":\"Journal of Experimental Pathology\",\"volume\":\"4 3\",\"pages\":\"123-32\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1989-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Experimental Pathology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Experimental Pathology","FirstCategoryId":"1085","ListUrlMain":"","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
本研究以断颈断奶大鼠胫骨为研究对象,探讨骨矿化的机制。佝偻病是通过给这些动物喂食低磷酸盐、低维生素D的食物5周而诱发的。钙化以三种方式重新开始;ⅰ组动物在暗室中给予1.0 ml NaH2PO4灌胃和致鼠性饲料;第二组动物置于有灯光的房间,给予标准实验室食物;III组置于光照充足的室内,给予标准实验室饲料,并给予1.0 ml 0.1M NaH2PO4 i.p.。I组愈合缓慢,II组和III组愈合迅速,愈合速度几乎相同。II组和III组显示血清碱性磷酸酶活性显著升高,并随着佝偻病愈合而变得高磷血症,这表明恢复更加有力。超微结构上,未愈合的棘骨基质中可见大量基质囊泡,这些结构在愈合开始时获得矿物质。与囊泡相关的矿物聚集体的大小增加,穿透和超越囊泡膜,并被纳入推进的矿化前沿。48小时前。愈合开始后,II组和III组骨样边界几乎完全矿化。这些观察结果表明,除了先前存在的矿物质外,基质囊泡也可以作为胎后骨类骨的成核位点。
Matrix vesicles and calcification of rachitic rat osteoid.
Tibiae from rachitic weanling rats were studied during healing to examine the mechanism of bone mineralization. Rickets was induced by feeding the animals a low phosphate, low vitamin D diet for five weeks. Calcification was reinstituted in three ways; group I animals received 1.0 ml of NaH2PO4 i.p. and the rachitogenic diet in a darkened room; group II animals were placed in a lighted room and given standard laboratory chow; group III animals were placed in lighted room, given standard laboratory chow and received 1.0 ml of 0.1M NaH2PO4 i.p. Group I healed slowly while II and III were found to heal rapidly and at nearly identical rates. Groups II and III revealed a significantly elevated serum alkaline phosphatase activity and became hyperphosphatemic as the rickets healed suggesting a more vigorous recovery. Ultrastructurally, numerous matrix vesicles were noted in unhealed rachitic bone matrix and these structures acquired mineral upon initiation of healing. Vesicle-associated mineral aggregates increased in size penetrating through and beyond the vesicle membrane and were incorporated into the advancing mineralization front. By 48 hrs. post-healing initiation, the osteoid borders were almost completely mineralized in groups II and III. These observations suggest that in addition to pre-existing mineral, matrix vesicles can also serve as nucleating sites in the osteoid of post-fetal bone.