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组氨酸24和组氨酸119在形成脱辅基肌红蛋白pH 4折叠中间体时的质子化行为。

Protonation behavior of histidine 24 and histidine 119 in forming the pH 4 folding intermediate of apomyoglobin.

作者信息

Geierstanger B, Jamin M, Volkman B F, Baldwin R L

机构信息

Department of Biochemistry, Stanford University School of Medicine, California 94305-5307, USA.

出版信息

Biochemistry. 1998 Mar 24;37(12):4254-65. doi: 10.1021/bi972516+.

Abstract

Heteronuclear NMR methods are used to study the protonation of histidine and aspartate residues in the acid-induced unfolding of recombinant sperm whale apomyoglobin. The results are combined with fluorescence and circular dichroism measurements of acid-induced unfolding of wild-type and double mutant (H24V/H119F) proteins. They are consistent with a simple model in which the failure to protonate a single buried histidine, H24, is largely responsible for the partial unfolding of native (N) wild-type apomyoglobin to the pH 4 folding intermediate (I). H24 is known to form an unusual interaction in which its side chain is buried and hydrogen-bonded to the side chain of H119. Two-dimensional 1H-15N heteronuclear NMR spectra indicate that H24 is present in the rare delta tautomeric form and remains neutral until N unfolds to I, while H119 becomes protonated before the N --> I reaction occurs. In the H24V/H119F double mutant, all histidines are protonated in N and the N --> I reaction occurs at lower pH. Therefore, the protonation of aspartate and/or glutamate residues must provide an additional driving force for the N to I reaction. Two-dimensional 1H-13C NMR experiments are used to measure the protonation of aspartates in selectively 13C-labeled apomyoglobin; the results indicate that none of the aspartate residues has a strongly depressed pKa in N, as would be expected if it forms a stabilizing salt bridge.

摘要

异核核磁共振方法用于研究重组抹香鲸脱辅基肌红蛋白在酸诱导去折叠过程中组氨酸和天冬氨酸残基的质子化情况。研究结果与野生型和双突变体(H24V/H119F)蛋白酸诱导去折叠的荧光和圆二色性测量结果相结合。这些结果与一个简单模型相符,在该模型中,单个埋藏的组氨酸H24未能质子化在很大程度上导致了天然(N)野生型脱辅基肌红蛋白部分去折叠为pH 4折叠中间体(I)。已知H24会形成一种不寻常的相互作用,其侧链被埋藏并与H119的侧链形成氢键。二维1H-15N异核核磁共振谱表明,H24以罕见的δ互变异构形式存在,在N去折叠为I之前一直保持中性,而H119在N→I反应发生之前就已质子化。在H24V/H119F双突变体中,所有组氨酸在N中均质子化,且N→I反应在较低pH下发生。因此,天冬氨酸和/或谷氨酸残基的质子化必须为N到I的反应提供额外的驱动力。二维1H-13C核磁共振实验用于测量选择性13C标记的脱辅基肌红蛋白中天冬氨酸的质子化情况;结果表明,没有一个天冬氨酸残基在N中有显著降低的pKa,而如果它形成稳定的盐桥则会出现这种情况。

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