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探索生物固氮的替代方法。

Exploring the alternatives of biological nitrogen fixation.

机构信息

Institute of Biological Chemistry, Washington State University, Pullman, WA 99163, USA.

出版信息

Metallomics. 2018 Apr 25;10(4):523-538. doi: 10.1039/c8mt00038g.

Abstract

Most biological nitrogen fixation (BNF) results from the activity of the molybdenum nitrogenase (Mo-nitrogenase, Nif), an oxygen-sensitive metalloenzyme complex found in all known diazotrophs. Two alternative forms of nitrogenase, the vanadium nitrogenase (V-nitrogenase, Vnf) and the iron-only nitrogenase (Fe-only nitrogenase, Anf) have also been identified in the genome of some organisms that encode for Nif. It has been suggested that alternative nitrogenases were responsible for N2-fixation on early Earth because oceans were depleted of bioavailable Mo. Results of recent phylogenetic- and structure-based studies suggest, however, that such an evolutionary path is unlikely, and favor a new model for a stepwise evolution of nitrogenase where the V-nitrogenase and the Fe-only nitrogenase are not the ancestor of the Mo-nitrogenase. Rather, Mo-nitrogenase emerged within the methanogenic archaea and then gave rise to the alternative forms suggesting they arose later in response to the availability of fixed N2 and local environmental factors that influenced metal availability. This review summarizes the current state of knowledge on (1) the biochemistry of these complex systems highlighting the common and specific structural features and catalytic activities of the enzymes, (2) the recent progress in defining the discrete set of genes associated to N2-fixation and the regulatory features that coordinate the differential expression of genes in response to metal availability, and (3) the diverse taxonomic and phylogenic distribution of nitrogenase enzymes and the evolutionary history of BNF from the perspective of metal content and metal availability.

摘要

大多数生物固氮(BNF)是由钼氮酶(Mo-nitrogenase,Nif)的活性引起的,钼氮酶是一种在所有已知固氮生物中都存在的对氧敏感的金属酶复合物。在一些编码 Nif 的生物体的基因组中,也发现了两种替代形式的氮酶,即钒氮酶(V-nitrogenase,Vnf)和铁单氮酶(Fe-only nitrogenase,Anf)。有人认为,替代氮酶是早期地球上固氮的原因,因为海洋中生物可利用的钼已经枯竭。然而,最近基于系统发育和结构的研究结果表明,这种进化途径不太可能,并且支持一个关于氮酶逐步进化的新模型,其中钒氮酶和铁单氮酶不是钼氮酶的祖先。相反,钼氮酶是在产甲烷古菌中出现的,然后产生了替代形式,这表明它们是后来为了适应固定氮的可用性和影响金属可用性的局部环境因素而出现的。本综述总结了目前关于(1)这些复杂系统的生物化学的知识状态,强调了酶的共同和特定的结构特征和催化活性,(2)最近在定义与固氮相关的一组离散基因方面的进展以及协调基因表达对金属可用性的差异的调控特征,以及(3)氮酶酶的多样的分类和系统发生分布以及从金属含量和金属可用性的角度来看的 BNF 的进化历史。

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