Department of Civil and Environmental Engineering, University of Washington, Seattle, 98195-2700, USA.
Annu Rev Microbiol. 2012;66:83-101. doi: 10.1146/annurev-micro-092611-150128.
The discovery of ammonia-oxidizing archaea (AOA), now generally recognized to exert primary control over ammonia oxidation in terrestrial, marine, and geothermal habitats, necessitates a reassessment of the nitrogen cycle. In particular, the unusually high affinity of marine and terrestrial AOA for ammonia indicates that this group may determine the oxidation state of nitrogen available to associated micro- and macrobiota, altering our current understanding of trophic interactions. Initial comparative genomics and physiological studies have revealed a novel, and as yet unresolved, primarily copper-based pathway for ammonia oxidation and respiration distinct from that of known ammonia-oxidizing bacteria and possibly relevant to the production of atmospherically active nitrogen oxides. Comparative studies also provide compelling evidence that the lineage of Archaea with which the AOA affiliate is sufficiently divergent to justify the creation of a novel phylum, the Thaumarchaeota.
氨氧化古菌(AOA)的发现,现在普遍认为对陆地、海洋和地热生境中的氨氧化起主要控制作用,这需要重新评估氮循环。特别是海洋和陆地 AOA 对氨的异常高亲和力表明,该群体可能决定了与相关微生物区系相关的可用氮的氧化状态,从而改变了我们对营养相互作用的现有理解。最初的比较基因组学和生理学研究揭示了一种新颖的、尚未解决的主要基于铜的氨氧化和呼吸途径,与已知的氨氧化细菌不同,可能与大气活性氮氧化物的产生有关。比较研究还提供了令人信服的证据,表明与 AOA 相关的古菌谱系足够分化,有理由创建一个新的门,即泉古菌门。