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固氮酶的同位素杂化物。对P簇选择性富集57Fe的钼铁蛋白的穆斯堡尔研究。

Isotopic hybrids of nitrogenase. Mössbauer study of MoFe protein with selective 57Fe enrichment of the P-cluster.

作者信息

McLean P A, Papaefthymiou V, Orme-Johnson W H, Münck E

机构信息

Department of Chemistry, Massachusetts Institute of Technology, Cambridge 02139.

出版信息

J Biol Chem. 1987 Sep 25;262(27):12900-3.

PMID:2820958
Abstract

Previous Mössbauer and EPR studies of the MoFe protein (approximately 30 Fe and 2 Mo) of nitrogenase have revealed the presence of two unique clusters, namely, the P-clusters (presumably of the Fe4S4 type) and the molybdenum- and iron-containing cofactors (or M-clusters). Mössbauer components D (approximately 10-12 Fe) and Fe2+ (approximately 4 Fe) represent subsites of the P-clusters while component S (approximately 2 Fe) appeared to belong to a separate, unidentified cluster. In order to refine the analyses of Mössbauer spectra, we have constructed an isotopic hybrid of the Klebsiella pneumoniae protein which contains 57Fe-enriched P-clusters and 56Fe-enriched M-clusters. The highly resolved 57Fe Mössbauer spectra of this hybrid show that component S behaves spectroscopically like the P-cluster sites D and Fe2+ in oxidized and reduced MoFe protein. This suggests that S is a subset of the P-clusters rather than a different cluster type. The present study shows, for the first time, that the Debye-Waller factors of different P-cluster subsites have a different temperature dependence. Thus, the Fe2+/D absorption ratio is 4.0:10.0 at 4.2 K and 4.0:11.6 at 173 K. We propose that the reduced MoFe protein contains two pairs of P-clusters: one pair containing one Fe2+ and three D-sites and the other one Fe2+, two D, and one S-site. We have argued previously that the oxidized P-clusters occur in pairs as well.

摘要

此前对固氮酶钼铁蛋白(约含30个铁原子和2个钼原子)进行的穆斯堡尔谱和电子顺磁共振研究揭示了两种独特的簇,即P簇(可能是Fe4S4类型)和含钼铁辅助因子(或M簇)。穆斯堡尔谱成分D(约10 - 12个铁原子)和Fe2 +(约4个铁原子)代表P簇的亚位点,而成分S(约2个铁原子)似乎属于一个单独的、未鉴定的簇。为了完善对穆斯堡尔谱的分析,我们构建了肺炎克雷伯菌蛋白的同位素杂合体,其中含有富含57Fe的P簇和富含56Fe的M簇。这种杂合体的高分辨率57Fe穆斯堡尔谱表明,在氧化和还原的钼铁蛋白中,成分S在光谱行为上与P簇位点D和Fe2 +相似。这表明S是P簇的一个子集,而不是一种不同类型的簇。本研究首次表明,不同P簇亚位点的德拜 - 瓦勒因子具有不同的温度依赖性。因此,Fe2 + / D的吸收比在4.2 K时为4.0:10.0,在173 K时为4.0:11.6。我们提出,还原态的钼铁蛋白包含两对P簇:一对含有一个Fe2 +和三个D位点,另一对含有一个Fe2 +、两个D位点和一个S位点。我们之前曾提出,氧化态的P簇也是成对出现的。

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