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处于M期的HeLa S-3细胞及其后续细胞周期中的水合作用、体积变化和核磁共振质子弛豫时间

Hydration, volume changes and nuclear magnetic resonance proton relaxation times of HeLa S-3 cells in M-phase and the subsequent cell cycle.

作者信息

Wheatley D N, Inglis M S, Foster M A, Rimington J E

出版信息

J Cell Sci. 1987 Aug;88 ( Pt 1):13-23. doi: 10.1242/jcs.88.1.13.

DOI:10.1242/jcs.88.1.13
PMID:3443603
Abstract

Most mitotic HeLa cells divided into two daughter cells with half the volume of the parent; no additional reduction in volume was detectable during late telophase or the early part of G1. Synchronous growth throughout the next generation cycle was exponential, without an additional and sudden rise in volume being detectable as cells entered M-phase. Since the wet weight/dry weight ratio and the protein per unit mass of cells remained constant throughout the cycle, measurements based on volume changes accurately reflected growth parameters and cell water content. Nuclear magnetic resonance (n.m.r.) t1 (spin-lattice) proton relaxation times for intracellular water for M-phase cells measured at both 32 MHz (25 degrees C) and 80 MHz (37 degrees C) in a Bruker spectrometer had the same values as normal interphase cells. Furthermore, cells arrested in metaphase by nitrous oxide or alkaloids gave the same t1 values. Artificial manipulation of cell hydration by adjustment of the tonicity of the external medium led to t1 values that correlated well with the level of intracellular water. On this basis, a 40% increase in hydration raised t1 values by a factor of 1.29 at 32 MHz and 1.5 at 80 MHz. This is considerably less than the increase by a factor of 1.9 in t1 time reported with the 40% rise in cell water accompanying mitosis, measured at 30 MHz and 25 degrees C under isotonic conditions by others. The protein-synthesizing ability of hydrated cells was reduced to only half the normal level after a doubling of intracellular water. The data from these several different analyses, taken together, strongly indicate that the water content of mitotic cells is very similar to that of interphase cells, and that certain features unique to the mitotic phase of the cell cycle cannot be ascribed to an elevated (free) water content.

摘要

大多数有丝分裂的海拉细胞分裂成两个子细胞,其体积为母细胞的一半;在末期后期或G1期早期未检测到体积的进一步减小。在接下来的一个细胞周期中,同步生长呈指数增长,当细胞进入M期时,未检测到体积有额外的突然增加。由于整个周期中湿重/干重比以及单位质量细胞中的蛋白质保持恒定,基于体积变化的测量准确反映了生长参数和细胞含水量。在布鲁克光谱仪中,在32兆赫(25摄氏度)和80兆赫(37摄氏度)下测量的M期细胞胞内水的核磁共振(n.m.r.)t1(自旋晶格)质子弛豫时间与正常间期细胞的值相同。此外,被一氧化二氮或生物碱阻滞在中期的细胞给出相同的t1值。通过调节外部培养基的张力人工控制细胞水合作用,导致t1值与细胞内水水平密切相关。在此基础上,水合作用增加40%时,在32兆赫下t1值提高1.29倍,在80兆赫下提高1.5倍。这大大低于其他人在等渗条件下于30兆赫和25摄氏度测量的伴随有丝分裂细胞水含量增加40%时t1时间增加1.9倍的情况。细胞内水加倍后,水合细胞的蛋白质合成能力仅降至正常水平的一半。综合这些来自几种不同分析的数据,有力地表明有丝分裂细胞的含水量与间期细胞非常相似,并且细胞周期有丝分裂期特有的某些特征不能归因于升高的(游离)水含量。

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