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14天6°头低位卧床休息期间骨转换标志物的变化

Changes in bone turnover markers during 14-day 6 degrees head-down bed rest.

作者信息

Kim Hyeteok, Iwasaki Kenichi, Miyake Takeo, Shiozawa Tomoki, Nozaki Sadahiko, Yajima Kazuyoshi

机构信息

Department of Hygiene and Space Medicine, Nihon University School of Medicine, 30-1 Oyaguchi-kamimachi, 173-8610 Tokyo, Itabashi-ku, Japan.

出版信息

J Bone Miner Metab. 2003;21(5):311-5. doi: 10.1007/s00774-003-0426-6.

Abstract

Osteoporosis caused by exposure to microgravity represents a serious clinical concern, but the mechanisms have yet to be fully elucidated. The present research aimed to elucidate the effects of microgravity environments on bone turnover, with a specific focus on changes in bone resorption markers such as type I collagen cross-linked N-telopeptides (NTx) and deoxypyridinoline (Dpyr), for which scant data are available regarding detailed time course. Methods using 6 degrees head-down bed rest were utilized to simulate a microgravity environment. Eleven adult male volunteers underwent 6 degrees head-down bed rest for 14 days; measurements were made of serum and urine Ca concentrations, in addition to osteocalcin (OC), bone alkaline phosphatase (ALP), NTx, and Dpyr as bone turnover markers. By the end of bed rest, concentrations of bone ALP had significantly increased, but OC displayed a tendency toward decrease. Concentrations of Dpyr significantly increased from day 6, remaining elevated until the end of bed rest. Concentrations of NTx significantly increased on day 13 and at the end of bed rest. Serum and urinary concentrations of Ca increased significantly at the end of bed rest. Bone ALP represents a relatively early marker of osteoblast differentiation at the matrix maturation phase and OC is a late marker in osteoblast differentiation at the calcification phase. The present results therefore suggest an absolute increase in bone resorption and normal or reduced bone formation, together causing prominent uncoupling and rapid bone loss after simulated microgravity. Moreover, the present results suggest that bone resorption is enhanced at an early stage of exposure to microgravity environments.

摘要

暴露于微重力环境导致的骨质疏松是一个严重的临床问题,但其机制尚未完全阐明。本研究旨在阐明微重力环境对骨转换的影响,特别关注骨吸收标志物的变化,如I型胶原交联N-端肽(NTx)和脱氧吡啶啉(Dpyr),目前关于其详细时间进程的数据很少。采用头低位6°卧床休息的方法来模拟微重力环境。11名成年男性志愿者进行了14天的头低位6°卧床休息;除了骨钙素(OC)、骨碱性磷酸酶(ALP)、NTx和Dpyr作为骨转换标志物外,还测量了血清和尿液中的钙浓度。卧床休息结束时,骨ALP浓度显著升高,但OC呈下降趋势。Dpyr浓度从第6天开始显著升高,一直持续到卧床休息结束。NTx浓度在第13天和卧床休息结束时显著升高。卧床休息结束时,血清和尿液中的钙浓度显著增加。骨ALP是基质成熟阶段成骨细胞分化的相对早期标志物,而OC是钙化阶段成骨细胞分化的晚期标志物。因此,本研究结果表明骨吸收绝对增加,而骨形成正常或减少,共同导致模拟微重力后明显的解偶联和快速的骨质流失。此外,本研究结果表明,在暴露于微重力环境的早期阶段,骨吸收增强。

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