Liu Ying, Hedwig Sebastian, Schäffer Andreas, Lenz Markus, Martinez Mathieu
Institute for Ecopreneurship, School of Life Sciences, University of Applied Sciences and Arts Northwestern Switzerland, Muttenz, Switzerland.
Institute for Environmental Research, RWTH Aachen University, Aachen, Germany.
Appl Environ Microbiol. 2021 May 26;87(12):e0010421. doi: 10.1128/AEM.00104-21.
Selenium (Se) deficiency affects many millions of people worldwide, and the volatilization of methylated Se species to the atmosphere may prevent Se from entering the food chain. Despite the extent of Se deficiency, little is known about fluxes in volatile Se species and their temporal and spatial variation in the environment, giving rise to uncertainty in atmospheric transport models. To systematically determine fluxes, one can rely on laboratory microcosm experiments to quantify Se volatilization in different conditions. Here, it is demonstrated that the sulfur (S) status of bacteria crucially determines the amount of Se volatilized. Solid-phase microextraction gas chromatography mass spectrometry showed that Pseudomonas tolaasii efficiently and rapidly (92% in 18 h) volatilized Se to dimethyl diselenide and dimethyl selenyl sulfide through promiscuous enzymatic reactions with the S metabolism. However, when the cells were supplemented with cystine (but not methionine), a major proportion of the Se (∼48%) was channeled to thus-far-unknown, nonvolatile Se compounds at the expense of the previously formed dimethyl diselenide and dimethyl selenyl sulfide (accounting for <4% of total Se). Ion chromatography and solid-phase extraction were used to isolate unknowns, and electrospray ionization ion trap mass spectrometry, electrospray ionization quadrupole time-of-flight mass spectrometry, and microprobe nuclear magnetic resonance spectrometry were used to identify the major unknown as a novel Se metabolite, 2-hydroxy-3-(methylselanyl)propanoic acid. Environmental S concentrations often exceed Se concentrations by orders of magnitude. This suggests that in fact S status may be a major control of selenium fluxes to the atmosphere. Volatilization from soil to the atmosphere is a major driver for Se deficiency. "Bottom-up" models for atmospheric Se transport are based on laboratory experiments quantifying volatile Se compounds. The high Se and low S concentrations in such studies poorly represent the environment. Here, we show that S amino acid status has in fact a decisive effect on the production of volatile Se species in Pseudomonas tolaasii. When the strain was supplemented with S amino acids, a major proportion of the Se was channeled to thus-far-unknown, nonvolatile Se compounds at the expense of volatile compounds. This hierarchical control of the microbial S amino acid status on Se cycling has been thus far neglected. Understanding these interactions-if they occur in the environment-will help to improve atmospheric Se models and thus predict drivers of Se deficiency.
全球数以百万计的人受到硒(Se)缺乏的影响,甲基化硒物种向大气中的挥发可能会阻止硒进入食物链。尽管硒缺乏的情况很普遍,但人们对挥发性硒物种在环境中的通量及其时空变化知之甚少,这导致大气传输模型存在不确定性。为了系统地确定通量,可以依靠实验室微观实验来量化不同条件下的硒挥发情况。在此,研究表明细菌的硫(S)状态对挥发的硒量起着关键作用。固相微萃取气相色谱 - 质谱分析表明,托拉斯假单胞菌通过与硫代谢的混杂酶促反应,高效且快速地(18小时内达到92%)将硒挥发为二甲基二硒化物和二甲基硒基硫化物。然而,当细胞补充胱氨酸(而非甲硫氨酸)时,大部分硒(约48%)被导向迄今未知的非挥发性硒化合物,而之前形成的二甲基二硒化物和二甲基硒基硫化物的产量则减少(占总硒量的不到4%)。离子色谱和固相萃取被用于分离未知物,电喷雾电离离子阱质谱、电喷雾电离四极杆飞行时间质谱和微探针核磁共振光谱被用于鉴定主要未知物为一种新型硒代谢物,2 - 羟基 - 3 -(甲基硒基)丙酸。环境中的硫浓度通常比硒浓度高出几个数量级。这表明实际上硫状态可能是控制硒向大气通量的主要因素。从土壤到大气的挥发是硒缺乏的主要驱动因素。大气硒传输的“自下而上”模型基于量化挥发性硒化合物的实验室实验。此类研究中高硒和低硫浓度并不能很好地代表实际环境。在此,我们表明硫氨基酸状态实际上对托拉斯假单胞菌中挥发性硒物种的产生具有决定性影响。当该菌株补充硫氨基酸时,大部分硒被导向迄今未知的非挥发性硒化合物,而挥发性化合物的产量则减少。微生物硫氨基酸状态对硒循环的这种层级控制迄今一直被忽视。了解这些相互作用(如果它们在环境中发生)将有助于改进大气硒模型,从而预测硒缺乏的驱动因素。