Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Research Network "Chemistry meets Microbiology", University of Vienna , Althanstraße 14, 1090 Vienna, Austria.
Anal Chem. 2017 Sep 5;89(17):9192-9200. doi: 10.1021/acs.analchem.7b01938. Epub 2017 Aug 22.
Soil fluxomics analysis can provide pivotal information for understanding soil biochemical pathways and their regulation, but direct measurement methods are rare. Here, we describe an approach to measure soil extracellular metabolite (amino sugar and amino acid) concentrations and fluxes based on a N isotope pool dilution technique via liquid chromatography and high-resolution mass spectrometry. We produced commercially unavailable N and C labeled amino sugars and amino acids by hydrolyzing peptidoglycan isolated from isotopically labeled bacterial biomass and used them as tracers (N) and internal standards (C). High-resolution (Orbitrap Exactive) MS with a resolution of 50 000 allowed us to separate different stable isotope labeled analogues across a large range of metabolites. The utilization of C internal standards greatly improved the accuracy and reliability of absolute quantification. We successfully applied this method to two types of soils and quantified the extracellular gross fluxes of 2 amino sugars, 18 amino acids, and 4 amino acid enantiomers. Compared to the influx and efflux rates of most amino acids, similar ones were found for glucosamine, indicating that this amino sugar is released through peptidoglycan and chitin decomposition and serves as an important nitrogen source for soil microorganisms. d-Alanine and d-glutamic acid derived from peptidoglycan decomposition exhibited similar turnover rates as their l-enantiomers. This novel approach offers new strategies to advance our understanding of the production and transformation pathways of soil organic N metabolites, including the unknown contributions of peptidoglycan and chitin decomposition to soil organic N cycling.
土壤通量组学分析可以为理解土壤生化途径及其调控提供关键信息,但直接的测量方法却很少见。在这里,我们描述了一种基于液相色谱和高分辨率质谱的氮同位素池稀释技术来测量土壤细胞外代谢物(氨基糖和氨基酸)浓度和通量的方法。我们通过水解来自同位素标记细菌生物量的肽聚糖来制备商业上不可用的氮和碳标记的氨基糖和氨基酸,并将它们用作示踪剂(氮)和内标(碳)。高分辨率(轨道阱 Exactive)MS 的分辨率为 50,000,使我们能够在大范围内分离不同的稳定同位素标记类似物。碳内标物的使用极大地提高了绝对定量的准确性和可靠性。我们成功地将这种方法应用于两种类型的土壤中,并定量了 2 种氨基糖、18 种氨基酸和 4 种氨基酸对映体的细胞外总通量。与大多数氨基酸的流入和流出率相比,发现氨基葡萄糖的情况类似,这表明这种氨基糖是通过肽聚糖和几丁质分解释放出来的,是土壤微生物的重要氮源。来自肽聚糖分解的 d-丙氨酸和 d-谷氨酸与它们的 l-对映体表现出相似的周转率。这种新方法为深入了解土壤有机氮代谢物的产生和转化途径提供了新的策略,包括肽聚糖和几丁质分解对土壤有机氮循环的未知贡献。