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嗜热栖热菌氧化型Fe4S4铁氧化还原蛋白的1H核磁共振研究。超精细位移共振、序列特异性归属及二级结构

1H nuclear-magnetic-resonance investigation of oxidized Fe4S4 ferredoxin from Thermotoga maritima. Hyperfine-shifted resonances, sequence-specific assignments and secondary structure.

作者信息

Wildegger G, Bentrop D, Ejchart A, Alber M, Hage A, Sterner R, Rösch P

机构信息

Lehrstuhl für Struktur und Chemie der Biopolymere, Universität Bayreuth, Germany.

出版信息

Eur J Biochem. 1995 May 1;229(3):658-68. doi: 10.1111/j.1432-1033.1995.tb20511.x.

Abstract

The oxidized Fe4S4 ferredoxin from the hyperthermophilic bacterium Thermotoga maritima has been investigated by one- and two-dimensional NMR in order to characterize its hyperfine-shifted resonances originating from the cysteinyl cluster ligands and to assign its resonances in the diamagnetic shift range. The chemical shift and relaxation time pattern of the hyperfine-shifted signals is very similar to other oxidized Fe4S4 ferredoxins. A tentative sequence-specific assignment of these resonances according to a general pattern of chemical shift of cysteine protons versus sequence position of cluster ligand is presented. Furthermore, sequence-specific assignments for 85% of the amino acid residues that were obtained without any guidance by known X-ray structures of ferredoxins are given. They reveal the formation of at least two elements of secondary structure by the polypeptide chain of T. maritima ferredoxin: an alpha-helix comprising residues C43-D49 and a double-stranded antiparallel beta-sheet consisting of the N- and C-terminal parts of the protein. This folding pattern is very similar to that of the crystallographically characterized ferredoxin from the mesophile Desulfovibrio gigas [Kissinger, C.R., Sieker, L.C., Adman E.T. & Jensen, L.H. (1991) J. Mol. Biol. 219, 693-715] and therefore suggesting different mechanisms of stabilization for T. maritima ferredoxin and the ferredoxin from the hyperthermophilic archaeon Pyrococcus furiosus that was recently investigated by NMR [Teng, Q., Zhou, Z.H., Smith, E.T., Busse, S. C., Howard, J.B., Adams M.W.W. & La Mar, G.N. (1994) Biochemistry 33, 6316-6326].

摘要

为了表征嗜热栖热菌(Thermotoga maritima)中氧化型Fe4S4铁氧化还原蛋白源自半胱氨酰簇配体的超精细位移共振,并在抗磁位移范围内归属其共振信号,对该蛋白进行了一维和二维核磁共振研究。超精细位移信号的化学位移和弛豫时间模式与其他氧化型Fe4S4铁氧化还原蛋白非常相似。根据半胱氨酸质子化学位移与簇配体序列位置的一般模式,给出了这些共振的初步序列特异性归属。此外,还给出了在没有铁氧化还原蛋白已知X射线结构指导的情况下,对85%氨基酸残基的序列特异性归属。这些归属揭示了嗜热栖热菌铁氧化还原蛋白的多肽链形成了至少两个二级结构元件:一个包含C43-D49残基的α-螺旋和一个由蛋白质N端和C端部分组成的双链反平行β-折叠。这种折叠模式与中温嗜热栖热菌巨大脱硫弧菌(Desulfovibrio gigas)晶体学表征的铁氧化还原蛋白非常相似[基辛格,C.R.,西克,L.C.,阿德曼,E.T. & 詹森,L.H.(1991)《分子生物学杂志》219,693 - 715],因此表明嗜热栖热菌铁氧化还原蛋白和最近通过核磁共振研究的嗜热古菌激烈火球菌(Pyrococcus furiosus)铁氧化还原蛋白的稳定机制不同[滕,Q.,周,Z.H.,史密斯,E.T.,布斯,S.C.,霍华德,J.B.,亚当斯,M.W.W. & 拉马尔,G.N.(1994)《生物化学》33,6316 - 6326]。

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