Department of Geology, University of Illinois, Urbana, IL 61801, USA.
Proc Natl Acad Sci U S A. 2012 Nov 27;109(48):19709-14. doi: 10.1073/pnas.1211238109. Epub 2012 Nov 12.
Agricultural and industrial practices more than doubled the intrinsic rate of terrestrial N fixation over the past century with drastic consequences, including increased atmospheric nitrous oxide (N(2)O) concentrations. N(2)O is a potent greenhouse gas and contributor to ozone layer destruction, and its release from fixed N is almost entirely controlled by microbial activities. Mitigation of N(2)O emissions to the atmosphere has been attributed exclusively to denitrifiers possessing NosZ, the enzyme system catalyzing N(2)O to N(2) reduction. We demonstrate that diverse microbial taxa possess divergent nos clusters with genes that are related yet evolutionarily distinct from the typical nos genes of denitirifers. nos clusters with atypical nosZ occur in Bacteria and Archaea that denitrify (44% of genomes), do not possess other denitrification genes (56%), or perform dissimilatory nitrate reduction to ammonium (DNRA; (31%). Experiments with the DNRA soil bacterium Anaeromyxobacter dehalogenans demonstrated that the atypical NosZ is an effective N(2)O reductase, and PCR-based surveys suggested that atypical nosZ are abundant in terrestrial environments. Bioinformatic analyses revealed that atypical nos clusters possess distinctive regulatory and functional components (e.g., Sec vs. Tat secretion pathway in typical nos), and that previous nosZ-targeted PCR primers do not capture the atypical nosZ diversity. Collectively, our results suggest that nondenitrifying populations with a broad range of metabolisms and habitats are potentially significant contributors to N(2)O consumption. Apparently, a large, previously unrecognized group of environmental nosZ has not been accounted for, and characterizing their contributions to N(2)O consumption will advance understanding of the ecological controls on N(2)O emissions and lead to refined greenhouse gas flux models.
农业和工业实践在过去一个世纪中将陆地固有固氮率提高了一倍以上,带来了严重的后果,包括大气中氧化亚氮(N(2)O)浓度的增加。N(2)O 是一种强效温室气体,也是破坏臭氧层的原因之一,其从固定氮中的释放几乎完全受微生物活动控制。减少向大气中排放 N(2)O 一直被归因于具有 NosZ 的反硝化细菌,该酶系统将 N(2)O 催化还原为 N(2)。我们证明,不同的微生物类群具有不同的 nos 簇,其基因与反硝化细菌的典型 nos 基因相关,但在进化上是不同的。具有非典型 nosZ 的 nos 簇存在于反硝化(44%的基因组)、不具有其他反硝化基因(56%)或进行异化硝酸盐还原为铵(DNRA;31%)的细菌和古菌中。与进行 DNRA 的土壤细菌 Anaeromyxobacter dehalogenans 的实验表明,非典型 NosZ 是一种有效的 N(2)O 还原酶,基于 PCR 的调查表明,非典型 nosZ 在陆地环境中丰富。生物信息学分析表明,非典型 nos 簇具有独特的调控和功能成分(例如,典型 nos 中的 Sec 与 Tat 分泌途径),并且以前针对 nosZ 的 PCR 引物不能捕获非典型 nosZ 的多样性。总的来说,我们的结果表明,具有广泛代谢和生境的非反硝化种群可能是 N(2)O 消耗的重要贡献者。显然,以前未被认识到的、具有广泛代谢和生境的非反硝化种群是 N(2)O 消耗的重要贡献者。显然,以前未被认识到的、具有广泛代谢和生境的非反硝化种群具有大量的、以前未被认识到的环境 nosZ 群体,对其对 N(2)O 消耗的贡献进行特征描述将有助于深入了解对 N(2)O 排放的生态控制,并导致对温室气体通量模型的改进。