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首页> 外文期刊>Biochemistry >Secondary structure extensions in Pyrococcus furiosus ferredoxin destabilize the disulfide bond relative to that in other hyperthermostable ferredoxins. Global consequences for the disulfide orientational heterogeneity.
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Secondary structure extensions in Pyrococcus furiosus ferredoxin destabilize the disulfide bond relative to that in other hyperthermostable ferredoxins. Global consequences for the disulfide orientational heterogeneity.

机译:激烈热球菌铁氧还蛋白的二级结构延伸使二硫键相对于其他高热铁氧还蛋白不稳定。对二硫键取向异质性的全球影响。

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摘要

The single cubane cluster ferredoxin (Fd) from the hyperthermophilic archaeon Pyrococcus furiosus (Pf) possesses several unique properties when compared even to Fds from other hyperthermophilic archaea or bacteria. These include an equilibrium molecular heterogeneity, a six- to seven-residue increase in size, an Asp rather than the Cys as one cluster ligand, and a readily reducible disulfide bond. NMR assignments and determination of both secondary structure and tertiary contacts remote from the paramagnetic oxidized cluster of Pf 3Fe Fd with an intact disulfide bond reported previously (Teng Q., Zhou, Z. H., Smith, E. T., Busse, S. C., Howard, J. B. Adams, M. W. W., and La Mar, G. (1994) Biochemistry 33, 6316-6328) are extended here to the 4Fe oxidized cluster WT (1H and 15N) and D14C (1H only) Fds with an intact disulfide bond and to the 4Fe oxidized WT Fd (1H and 15N) with a cleaved disulfide bond. All forms are shown to possess a long (13-member) alpha-helix, two beta-sheets (one double-, one triple-stranded), and three turns outside the cluster vicinity, each with tertiary contacts among themselves as found in other Fds. While the same secondary structural elements, with similar tertiary contacts, are found in other hyperthermostable Fds, Pf Fd has two elements, the long helix and the triple-stranded beta-sheet, that exhibit extensions and form multiple tertiary contacts. All Pf Fd forms with an intact disulfide bond exhibit a dynamic equilibrium heterogeneity which is shown to modulate a hydrogen-bonding network in the hydrophobic core that radiates from the Cys21-Cys48 disulfide bond and encompasses residues Lys36, Val24, Cys21, and Cys17 and the majority of the long helix. The heterogeneity is attributed to population of the alternate S and R chiralities of the disulfide bond, each destabilized by steric interactions with the extended alpha-helix. Comparison of the chemical shifts and their temperature gradients reveals that the molecular structure of the protein with the less stable R disulfide resembles that of the Fd with a cleaved disulfide bond. Both cluster architecture (3Fe vs 4Fe) and ligand mutation (Cys for Asp14) leave the disulfide orientational heterogeneity largely unperturbed. It is concluded that the six- to seven-residue extension that results in a longer helix and larger beta-sheet in Pf Fd, relative to other hyperthermostable Fds, more likely serves to destabilize the disulfide bond, and hence make it more readily reducible, than to significantly increase protein thermostability.
机译:与来自其他嗜热古菌或细菌的Fds相比,来自嗜热古菌Pyrococcus furiosus(Pf)的单个古巴簇铁氧还蛋白(Fd)具有几个独特的特性。这些包括平衡分子异质性,大小增加六至七个残基,作为一个簇配体的Asp而不是Cys,以及易于还原的二硫键。先前已报道过的NMR分配以及远离带有完整二硫键的Pf 3Fe Fd的顺磁性氧化簇的二级结构和三级接触的确定(滕Q.,周,ZH,史密斯,ET,布斯,SC,霍华德,JB亚当斯, MWW和La Mar,G.(1994)Biochemistry 33,6316-6328)在此扩展到具有完整二硫键的4Fe氧化簇WT(1H和15N)和D14C(仅1H)Fds和4Fe氧化WT具有二硫键断裂的Fd(1H和15N)。所有形式都显示出具有长的(13位成员)α-螺旋,两个β-折叠(一个双链,一个三链)和在簇附近的三匝,每一个彼此之间都具有三级接触,如其他Fds。虽然在其他超耐热Fds中发现了具有相似三级接触的相同二级结构元素,但Pf Fd具有两个元素,即长螺旋和三链β-折叠,它们具有延伸并形成多个三级接触。具有完整二硫键的所有Pf Fd形式均表现出动态平衡异质性,表明其可调节疏水核中从Cys21-Cys48二硫键辐射的氢键网络,并包含残基Lys36,Val24,Cys21和Cys17和长螺旋的大部分。异质性归因于二硫键的交替S和R手性的填充,每个手性都通过与延伸的α-螺旋的空间相互作用而不稳定。化学位移及其温度梯度的比较表明,具有不稳定的R二硫键的蛋白质的分子结构类似于具有断裂的二硫键的Fd的分子结构。簇结构(3Fe对4Fe)和配体突变(Asp14的Cys)都使二硫键取向异质性基本不受干扰。结论是,相对于其他高热稳定性Fds,六到七个残基的延伸导致Pf Fd更长的螺旋和更大的β-折叠,更可能使二硫键不稳定,从而使其更易于还原,而不是显着提高蛋白质的热稳定性。

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