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海洋氨氧化古菌产生一氧化氮以及一氧化氮清除剂对古菌氨氧化的抑制作用。

The production of nitric oxide by marine ammonia-oxidizing archaea and inhibition of archaeal ammonia oxidation by a nitric oxide scavenger.

作者信息

Martens-Habbena Willm, Qin Wei, Horak Rachel E A, Urakawa Hidetoshi, Schauer Andrew J, Moffett James W, Armbrust E Virginia, Ingalls Anitra E, Devol Allan H, Stahl David A

机构信息

Department of Civil and Environmental Engineering, University of Washington, Seattle, WA, 98195, USA.

School of Oceanography, University of Washington, Seattle, WA, 98195, USA.

出版信息

Environ Microbiol. 2015 Jul;17(7):2261-74. doi: 10.1111/1462-2920.12677. Epub 2015 Jan 27.

Abstract

Nitrification is a critical process for the balance of reduced and oxidized nitrogen pools in nature, linking mineralization to the nitrogen loss processes of denitrification and anammox. Recent studies indicate a significant contribution of ammonia-oxidizing archaea (AOA) to nitrification. However, quantification of the relative contributions of AOA and ammonia-oxidizing bacteria (AOB) to in situ ammonia oxidation remains challenging. We show here the production of nitric oxide (NO) by Nitrosopumilus maritimus SCM1. Activity of SCM1 was always associated with the release of NO with quasi-steady state concentrations between 0.05 and 0.08 μM. NO production and metabolic activity were inhibited by the nitrogen free radical scavenger 2-phenyl-4,4,5,5,-tetramethylimidazoline-1-oxyl-3-oxide (PTIO). Comparison of marine and terrestrial AOB strains with SCM1 and the recently isolated marine AOA strain HCA1 demonstrated a differential sensitivity of AOB and AOA to PTIO and allylthiourea (ATU). Similar to the investigated AOA strains, bulk water column nitrification at coastal and open ocean sites with sub-micromolar ammonia/ammonium concentrations was inhibited by PTIO and insensitive to ATU. These experiments support predictions from kinetic, molecular and biogeochemical studies, indicating that marine nitrification at low ammonia/ammonium concentrations is largely driven by archaea and suggest an important role of NO in the archaeal metabolism.

摘要

硝化作用是自然界中还原态氮库和氧化态氮库平衡的关键过程,它将矿化作用与反硝化作用和厌氧氨氧化的氮损失过程联系起来。最近的研究表明,氨氧化古菌(AOA)对硝化作用有重大贡献。然而,量化AOA和氨氧化细菌(AOB)对原位氨氧化的相对贡献仍然具有挑战性。我们在此展示了嗜盐亚硝化球菌SCM1产生一氧化氮(NO)的过程。SCM1的活性总是与NO的释放相关,其准稳态浓度在0.05至0.08μM之间。无氮自由基清除剂2-苯基-4,4,5,5-四甲基咪唑啉-1-氧基-3-氧化物(PTIO)抑制了NO的产生和代谢活性。将海洋和陆地AOB菌株与SCM1以及最近分离出的海洋AOA菌株HCA1进行比较,结果表明AOB和AOA对PTIO和烯丙基硫脲(ATU)的敏感性存在差异。与所研究的AOA菌株类似,在沿海和公海站点氨/铵浓度为亚微摩尔级的水体总硝化作用受到PTIO的抑制,且对ATU不敏感。这些实验支持了动力学、分子和生物地球化学研究的预测,表明在低氨/铵浓度下海洋硝化作用主要由古菌驱动,并暗示了NO在古菌代谢中的重要作用。

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