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Determination of picomolar dissolved free amino acids along a South Atlantic transect using reversed-phase high-performance liquid chromatography

机译:使用反相高效液相色谱法测定南大西洋样带上皮摩尔溶解的游离氨基酸

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摘要

Dissolved free amino acids (DFAA) in seawater are a form of nitrogen (N) available for marine microbes. In oligotrophic environments where N-containing nutrients are the limiting factor for microbial growth, N nutrition from DFAA could be crucial, but as yet it is poorly resolved. Measurements of individual DFAA are challenging as concentrations are typically in the low nmol L− 1 range. Here we report modifications to methodology using o-phthaldialdehyde (OPA) derivatization and reversed phase high performance liquid chromatography (HPLC) that provide a 30-fold improvement in sensitivity enabling the detection of 15 amino acids in seawater with a limit of detection as low as 10 pmol L− 1 with accuracy and precision of better than 10%. This analytical methodology is now suitable for the challenging quantitation of DFAA in oligotrophic seawaters. The method was successfully applied to a suite of seawater samples collected on a cruise crossing the South Atlantic Ocean, where concentrations of DFAAs were generally low (sub nmol L− 1), revealing basin-scale features in the oceanographic distributions of DFAA. This unique dataset implies that DFAAs are an important component of the N cycle in both near-coastal and open oceans. Further calculations suggest that the proportions of organic N originating from DFAA sources were significant, contributing between 0.2 and 200% that of NH4 + and up to 77% that of total inorganic nitrogen in the upper 400 m in some regions of the transect.
机译:海水中溶解的游离氨基酸(DFAA)是用于海洋微生物的氮气(N)的形式。在含N型营养素是微生物生长的限制因素的低营养性环境中,DFAA的n营养可能是至关重要的,但尚未解决。作为浓度通常在低Nmol L-1范围内,单个DFAA的测量是具有挑战性的。在这里,我们使用O-Phthaldialdehyde(OPA)衍生化和反相高效液相色谱(HPLC)报告对方法的修饰,其提供30倍的灵敏度改善,使得海水中的15个氨基酸的检测有一个低于10 pmol l-1,精度和精度优于10%。这种分析方法现在适用于寡营海洋水域中DFAA的挑战性。该方法成功地应用于在南大西洋的巡航中收集的海水样本套装,其中DFAA的浓度通常低(亚Nmol L-1),揭示了DFAA的海洋分布中的盆地规模特征。这个独特的数据集意味着DFAAS是近沿岸和开放海洋的N个循环的重要组成部分。进一步的计算表明,来自DFAA来源的有机N的比例是显着的,在几个区域中,NH 4 +的NH 4 +和高达77%的NH 4 +和高达77%的含量为0.2和200%。

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