Division of Geological and Planetary Sciences, California Institute of Technology Pasadena, CA, USA.
Front Microbiol. 2013 Jan 30;3:419. doi: 10.3389/fmicb.2012.00419. eCollection 2012.
Nitrogenase enzymes have evolved complex iron-sulfur (Fe-S) containing cofactors that most commonly contain molybdenum (MoFe, Nif) as a heterometal but also exist as vanadium (VFe, Vnf) and heterometal-independent (Fe-only, Anf) forms. All three varieties are capable of the reduction of dinitrogen (N(2)) to ammonia (NH(3)) but exhibit differences in catalytic rates and substrate specificity unique to metal type. Recently, N(2) reduction activity was observed in archaeal methanotrophs and methanogens that encode for nitrogenase homologs which do not cluster phylogenetically with previously characterized nitrogenases. To gain insight into the metal cofactors of these uncharacterized nitrogenase homologs, predicted three-dimensional structures of the nitrogenase active site metal-cofactor binding subunits NifD, VnfD, and AnfD were generated and compared. Dendrograms based on structural similarity indicate nitrogenase homologs cluster based on heterometal content and that uncharacterized nitrogenase D homologs cluster with NifD, providing evidence that the structure of the enzyme has evolved in response to metal utilization. Characterization of the structural environment of the nitrogenase active site revealed amino acid variations that are unique to each class of nitrogenase as defined by heterometal cofactor content; uncharacterized nitrogenases contain amino acids near the active site most similar to NifD. Together, these results suggest that uncharacterized nitrogenase homologs present in numerous anaerobic methanogens, archaeal methanotrophs, and firmicutes bind FeMo-co in their active site, and add to growing evidence that diversification of metal utilization likely occurred in an anoxic habitat.
固氮酶含有复杂的铁-硫(Fe-S)辅因子,这些辅因子通常含有钼(MoFe、Nif)作为杂金属,但也存在钒(VFe、Vnf)和非杂金属(Fe 仅、Anf)形式。所有这三种形式都能够将氮气(N2)还原为氨(NH3),但在催化速率和底物特异性方面存在独特的金属类型差异。最近,在编码氮酶同源物的古菌甲烷营养菌和产甲烷菌中观察到了氮气还原活性,这些氮酶同源物在系统发育上与以前描述的氮酶没有聚类。为了深入了解这些未表征氮酶同源物的金属辅因子,生成并比较了氮酶活性位点金属辅因子结合亚基 NifD、VnfD 和 AnfD 的预测三维结构。基于结构相似性的聚类树表明,氮酶同源物根据杂金属含量聚类,未表征氮酶 D 同源物与 NifD 聚类,这表明酶的结构已进化以适应金属利用。氮酶活性位点结构环境的表征揭示了氨基酸的变化,这些变化在氮酶的每一类中都是独特的,定义了杂金属辅因子的含量;未表征的氮酶含有与 NifD 最相似的活性位点附近的氨基酸。总之,这些结果表明,在许多厌氧产甲烷菌、古菌甲烷营养菌和Firmicutes 中存在的未表征氮酶同源物在其活性位点结合 FeMo-co,并为金属利用多样化很可能发生在缺氧环境中的观点提供了更多证据。