OceanRep
Determination of picomolar dissolved free amino acids along a South Atlantic transect using reversed-phase high-performance liquid chromatography.
Sabadel, A. J. M., Browning, Thomas J. , Kruimer, D., Airs, R. L., Woodward, E. M. S., Van Hale, R. and Frew, R. D. (2017) Determination of picomolar dissolved free amino acids along a South Atlantic transect using reversed-phase high-performance liquid chromatography. Marine Chemistry, 196 . pp. 173-180. DOI 10.1016/j.marchem.2017.09.008.
Text
Sabadel.pdf - Published Version Restricted to Registered users only Download (644kB) | Contact |
|
Text
Sabadel_Suppl.docx - Supplemental Material Restricted to Registered users only Download (1MB) | Contact |
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 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.
Document Type: | Article |
---|---|
Keywords: | amino aciddissolved matterlimiting factorliquid chromatography, marine environment, nutrient dynamics, oligotrophic environment, open ocean, performance assessment, seawater, transect, South Atlantic Ocean |
Research affiliation: | OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-CH Chemical Oceanography OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-CH Chemical Oceanography > FB2-CH Water column biogeochemistry |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Elsevier |
Projects: | UK-GEOTRACES |
Date Deposited: | 20 Nov 2017 10:04 |
Last Modified: | 23 Apr 2021 11:00 |
URI: | https://oceanrep.geomar.de/id/eprint/40169 |
Actions (login required)
View Item |
Copyright 2023 | GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel | All rights reserved
Questions, comments and suggestions regarding the GEOMAR repository are welcomed
at bibliotheksleitung@geomar.de !