Swanner Elizabeth D, Templeton Alexis S
Department of Geological Sciences, University of Colorado Boulder, CO, USA.
Front Microbiol. 2011 Dec 20;2:254. doi: 10.3389/fmicb.2011.00254. eCollection 2011.
The existence of life in the deep terrestrial subsurface is established, yet few studies have investigated the origin of nitrogen that supports deep life. Previously, 16S rRNA gene surveys cataloged a diverse microbial community in subsurface fluids draining from boreholes 3000 feet deep at Henderson Mine, CO, USA (Sahl et al., 2008). The prior characterization of the fluid chemistry and microbial community forms the basis for the further investigation here of the source of NH(4) (+). The reported fluid chemistry included N(2), NH(4) (+) (5-112 μM), NO(2) (-) (27-48 μM), and NO(3) (-) (17-72 μM). In this study, the correlation between low NH(4) (+) concentrations in dominantly meteoric fluids and higher NH(4) (+) in rock-reacted fluids is used to hypothesize that NH(4) (+) is sourced from NH(4) (+)-bearing biotite. However, biotite samples from the host rocks and ore-body minerals were analyzed by Fourier transform infrared (FTIR) microscopy and none-contained NH(4) (+). However, the nitrogenase-encoding gene nifH was successfully amplified from DNA of the fluid sample with high NH(4) (+), suggesting that subsurface microbes have the capability to fix N(2). If so, unregulated nitrogen fixation may account for the relatively high NH(4) (+) concentrations in the fluids. Additionally, the amoA and nxrB genes for archaeal ammonium monooxygenase and nitrite oxidoreductase, respectively, were amplified from the high NH(4) (+) fluid DNA, while bacterial amoA genes were not. Putative nitrifying organisms are closely related to ammonium-oxidizing Crenarchaeota and nitrite-oxidizing Nitrospira detected in other subsurface sites based upon 16S rRNA sequence analysis. Thermodynamic calculations underscore the importance of NH(4) (+) as an energy source in a subsurface nitrification pathway. These results suggest that the subsurface microbial community at Henderson is adapted to the low nutrient and energy environment by their capability of fixing nitrogen, and that fixed nitrogen may support subsurface biomass via nitrification.
深层陆地地下存在生命这一点已得到证实,但很少有研究调查维持深层生命的氮的来源。此前,16S rRNA基因调查对美国科罗拉多州亨德森矿3000英尺深处钻孔排出的地下流体中的多种微生物群落进行了编目(萨尔等人,2008年)。先前对流体化学和微生物群落的表征构成了在此进一步研究NH₄⁺来源的基础。报告的流体化学组成包括N₂、NH₄⁺(5 - 112μM)、NO₂⁻(27 - 48μM)和NO₃⁻(17 - 72μM)。在本研究中,主要为大气降水的流体中低NH₄⁺浓度与岩石反应流体中较高NH₄⁺浓度之间的相关性被用于推测NH₄⁺源自含NH₄⁺的黑云母。然而,通过傅里叶变换红外(FTIR)显微镜对来自主岩和矿体矿物的黑云母样品进行分析,均未发现含有NH₄⁺。然而,从NH₄⁺含量高的流体样品的DNA中成功扩增出了编码固氮酶的nifH基因,这表明地下微生物具有固定N₂的能力。如果是这样,不受调控的固氮作用可能是流体中NH₄⁺浓度相对较高的原因。此外,分别从高NH₄⁺流体DNA中扩增出了古菌铵单加氧酶和亚硝酸盐氧化还原酶的amoA和nxrB基因,而细菌amoA基因未被扩增出来。基于16S rRNA序列分析,推测的硝化生物与在其他地下位点检测到的铵氧化泉古菌和亚硝酸盐氧化硝化螺菌密切相关。热力学计算强调了NH₄⁺作为地下硝化途径中能量来源的重要性。这些结果表明,亨德森的地下微生物群落通过其固氮能力适应了低营养和低能量环境,并且固定的氮可能通过硝化作用支持地下生物量。