2017
DOI: 10.1016/j.marchem.2017.09.008
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Determination of picomolar dissolved free amino acids along a South Atlantic transect using reversed-phase high-performance liquid chromatography

Abstract: 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 … Show more

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Cited by 9 publications
(5 citation statements)
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References 50 publications
(52 reference statements)
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“…The concentrations of many of the compounds measured in environmental samples by CX‐SPE analysis are within or close to the environmental concentration ranges reported by other studies of dissolved metabolites such as amino acids (Lee and Bada 1975; Fuhrman and Ferguson 1986; Sabadel et al 2017), TMAO (Gibb and Hatton 2004), creatine (Wawrik et al 2017), DMSP (Kiene and Slezak 2006), and arsenobetaine (Glabonjat et al 2018) (Table 1). Furthermore, the concentrations of some compounds measured for the first time using CX‐SPE such as glycine betaine were of roughly the same order of magnitude (low nM) as those predicted by uptake kinetics studies (Kiene and Slezak 2006; Boysen et al 2022; Mausz et al 2022).…”
Section: Discussionsupporting
confidence: 83%
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“…The concentrations of many of the compounds measured in environmental samples by CX‐SPE analysis are within or close to the environmental concentration ranges reported by other studies of dissolved metabolites such as amino acids (Lee and Bada 1975; Fuhrman and Ferguson 1986; Sabadel et al 2017), TMAO (Gibb and Hatton 2004), creatine (Wawrik et al 2017), DMSP (Kiene and Slezak 2006), and arsenobetaine (Glabonjat et al 2018) (Table 1). Furthermore, the concentrations of some compounds measured for the first time using CX‐SPE such as glycine betaine were of roughly the same order of magnitude (low nM) as those predicted by uptake kinetics studies (Kiene and Slezak 2006; Boysen et al 2022; Mausz et al 2022).…”
Section: Discussionsupporting
confidence: 83%
“…CX‐SPE LODs were lower than the derivatization/GC–MS method (60–1000 nM) (Sogin et al 2019). CX‐SPE did not achieve comparable LODs for amino acids (0.025–6.8 nM) compared with focused dissolved free amino acid (DFAA) methods (0.009–0.163 nM) (Sabadel et al 2017), but CX‐SPE did still enable the quantification of many DFAAs in environmental samples. The CX‐SPE LODs for DFAAs and other compounds can potentially be improved in the future through the use of larger sample volumes and micro or nanoflow HPLC systems.…”
Section: Discussionmentioning
confidence: 99%
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“…There were no significant correlations between concentrations of chl a and any amino acids (DFAA, DCAA and THAA) in this study. This result was inconsistent with other research [5,50,51], indicating that impact of plankton biomass on amino acids was very limited in the euphotic layer of the Yap Trench [35]. Amino acids and chl a are labile components in seawater with high turnover rates [44,52], and their concentrations are affected by various processes, such as phytoplankton production, biodegradation and ocean current [3,35].…”
Section: Amino Acids In Euphotic Layercontrasting
confidence: 61%
“…When measured as dissolved free amino acids, phenylalanine and tryptophan display a variety of concentrations ranging from hundreds to thousands of picomolar (Mopper and Lindroth 1982) from 0 to 170 m in the Baltic Sea. A study in the south Atlantic determined that dissolved phenylalanine concentrations were in the pmol L À1 range at the southern edge of the South Atlantic Gyre but increased to low nmol L À1 concentrations closer to the coast (Sabadel et al 2017). In our study, concentrations of tryptophan and phenylalanine varied from < 10 pmol L À1 (deep ocean) to hundreds of pmol L À1 (surface ocean).…”
Section: Discussionmentioning
confidence: 99%