Hilliard P R, Smith R M, Rill R L
J Biol Chem. 1986 May 5;261(13):5992-8.
Natural abundance carbon-13 nuclear magnetic resonance spectra (67.9 MHz) were obtained for native nucleosome cores: cores dissociated in 2 M NaCl and 2 M NaCl, 6 M urea; and cores degraded with DNase I plus proteinase K. Phosphorus-31 NMR spectra of native and dissociated cores and core length DNA were also obtained at 60.7 MHz. The 31P resonance and spin-lattice relaxation time (T1) of DNA were only slightly affected by packaging in nucleosome cores, in agreement with other reports, but 13C resonances of DNA were essentially unobservable. The loss of DNA spectral intensity suggests that rapid internal motions of DNA sugar carbons in protein-free DNA previously demonstrated by 13C NMR methods are partly restricted in nucleosomes. The 13C spectrum of native cores contains many narrow intense resonances assigned to lysine side chain and alpha-carbons, glycine alpha-carbons, alanine alpha- and beta- carbons, and arginine side chain carbons. Several weaker resonances were also assigned. The narrow line widths, short T1 values, and non-minimal nuclear Overhauser enhancements of these resonances, including alpha- and beta-carbons, show that some terminal chain segments of histones in nucleosomes are as mobile as small random coil polypeptides. The mobile segments include about 9% of all histone residues and 25% of all lysines, but only 10% of all arginines. The compositions of these segments indicate that mobile regions are located in amino- or carboxyl-terminal sequences of two or more histones. In addition, high mobility was observed for side chain carbons of 45-50% of all lysines (delta and epsilon carbons) and about 25% of all arginines (zeta carbon) in histones (including those in mobile segments), suggesting that basic residues in terminal histone sequences are not strongly involved in nucleosome structure and may instead help stabilize higher order chromatin structure.
对天然核小体核心颗粒进行了自然丰度碳-13核磁共振谱(67.9兆赫)测定:包括在2M氯化钠、2M氯化钠与6M尿素中解离的核心颗粒,以及用DNA酶I加蛋白酶K降解的核心颗粒。还在60.7兆赫下获得了天然及解离核心颗粒和核心长度DNA的磷-31核磁共振谱。与其他报道一致,DNA的31P共振和自旋晶格弛豫时间(T1)仅受到核小体核心颗粒包装的轻微影响,但DNA的13C共振基本上无法观测到。DNA光谱强度的损失表明,先前通过13C核磁共振方法证明的无蛋白DNA中DNA糖碳的快速内部运动在核小体中受到部分限制。天然核心颗粒的13C谱包含许多狭窄且强烈的共振峰,这些共振峰归属于赖氨酸侧链和α-碳、甘氨酸α-碳、丙氨酸α-和β-碳以及精氨酸侧链碳。还归属了几个较弱的共振峰。这些共振峰(包括α-和β-碳)的窄线宽、短T1值和非最小核Overhauser增强表明,核小体中组蛋白的一些末端链段与小的无规卷曲多肽一样具有流动性。这些可移动片段包括所有组蛋白残基的约9%和所有赖氨酸的25%,但仅占所有精氨酸的10%。这些片段的组成表明,可移动区域位于两个或更多组蛋白的氨基或羧基末端序列中。此外,在组蛋白(包括可移动片段中的组蛋白)中,观察到所有赖氨酸的45 - 50%(δ和ε碳)和约25%的所有精氨酸(ζ碳)的侧链碳具有高流动性,这表明组蛋白末端序列中的碱性残基与核小体结构的关联不强,反而可能有助于稳定更高阶的染色质结构。