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固氮酶MFe(7)S(9)(M = Mo(4+)、V(3+)、Fe(3+))活性位点中的金属取代

Metal substitution in the active site of nitrogenase MFe(7)S(9) (M = Mo(4+), V(3+), Fe(3+)).

作者信息

Lovell Timothy, Torres Rhonda A, Han Wen-Ge, Liu Tiqing, Case David A, Noodleman Louis

机构信息

Department of Molecular Biology TPC-15, The Scripps Research Institute, La Jolla, CA 92037, USA.

出版信息

Inorg Chem. 2002 Nov 4;41(22):5744-53. doi: 10.1021/ic020474u.

Abstract

The unifying view that molybdenum is the essential component in nitrogenase has changed over the past few years with the discovery of a vanadium-containing nitrogenase and an iron-only nitrogenase. The principal question that has arisen for the alternative nitrogenases concerns the structures of their corresponding cofactors and their metal-ion valence assignments and whether there are significant differences with that of the more widely known molybdenum-iron cofactor (FeMoco). Spin-polarized broken-symmetry (BS) density functional theory (DFT) calculations are used to assess which of the two possible metal-ion valence assignments (4Fe(2+)4Fe(3+) or 6Fe(2+)2Fe(3+)) for the iron-only cofactor (FeFeco) best represents the resting state. For the 6Fe(2+)2Fe(3+) oxidation state, the spin coupling pattern for several spin state alignments compatible with S = 0 were generated and assessed by energy criteria. The most likely BS spin state is composed of a 4Fe cluster with spin S(a) = (7)/(2) antiferromagnetically coupled to a 4Fe' cluster with spin S(b) = (7)/(2). This state has the lowest DFT energy for the isolated FeFeco cluster and displays calculated Mössbauer isomer shifts consistent with experiment. Although the S = 0 resting state of FeFeco has recently been proposed to have metal-ion valencies of 4Fe(2+)4Fe(3+) (derived from experimental Mössbauer isomer shifts), our isomer shift calculations for the 4Fe(2+)4Fe(3+) oxidation state are in poorer agreement with experiment. Using the Mo(4+)6Fe(2+)Fe(3+) oxidation level of the cofactor as a starting point, the structural consequences of replacement of molybdenum (Mo(4+)) with vanadium (V(3+)) or iron (Fe(3+)) in the cofactor have been investigated. The size of the cofactor cluster shows a dependency on the nature of the heterometal and increases in the order FeMoco < FeVco < FeFeco.

摘要

随着含钒固氮酶和仅含铁固氮酶的发现,钼是固氮酶中必需成分这一统一观点在过去几年发生了变化。替代固氮酶出现的主要问题涉及其相应辅因子的结构、金属离子价态分配,以及与更广为人知的钼铁辅因子(FeMoco)是否存在显著差异。自旋极化破缺对称性(BS)密度泛函理论(DFT)计算用于评估仅含铁辅因子(FeFeco)的两种可能金属离子价态分配(4Fe(2+)4Fe(3+)或6Fe(2+)2Fe(3+))中哪一种最能代表基态。对于6Fe(2+)2Fe(3+)氧化态,生成了与S = 0兼容的几种自旋态排列的自旋耦合模式,并通过能量标准进行评估。最可能的BS自旋态由自旋S(a) = (7)/(2)的4Fe簇与自旋S(b) = (7)/(2)的4Fe'簇反铁磁耦合组成。对于孤立的FeFeco簇,该状态具有最低的DFT能量,并且显示出与实验一致的计算穆斯堡尔同质异能位移。尽管最近有人提出FeFeco的S = 0基态具有4Fe(2+)4Fe(3+)的金属离子价态(源自实验穆斯堡尔同质异能位移),但我们对4Fe(2+)4Fe(3+)氧化态的同质异能位移计算与实验的一致性较差。以辅因子的Mo(4+)6Fe(2+)Fe(3+)氧化水平为起点,研究了辅因子中用钒(V(3+))或铁(Fe(3+))替代钼(Mo(4+))的结构后果。辅因子簇的大小显示出对异金属性质的依赖性,并按FeMoco < FeVco < FeFeco的顺序增加。

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