4.7 Article

Metal substitution in the active site of nitrogenase MFe7S9 (M = Mo4+, V3+, Fe3+)

Journal

INORGANIC CHEMISTRY
Volume 41, Issue 22, Pages 5744-5753

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/ic020474u

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Funding

  1. NIGMS NIH HHS [GM 39914] Funding Source: Medline

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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 Mossbauer 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 Mossbauer isomer shifts), our isomer shift calculations for the 4Fe2+4Fe3+ 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 (Mo4+) with vanadium (V3+) or iron (Fe3+) 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.

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