We investigated the contribution of dissolved free amino acids (DFAA) and ammonium (NH4+) to the nitrogen demand (N-demand) of bacterioplankton in the subarctic Pacific and the Delaware Estuary. Bacteria were isolated from other microorganisms by gravity-filtration through 0.8 mu-m filters, and then bacterial abundance and nutrient concentrations were measured over time. During experiments lasting between 36 and 130 h, DFAA and NH4+ contributed 51 +/- 45 % and 64 +/- 54 % (n = 14) to the estimated N-demand, respectively. In 9 of the 14 experiments, DFAA and NH4+ contributed over 90 % of the estimated N-demand, implying that dissolved organic nitrogen aside from DFAA (e.g. dissolved combined amino acids) was not a significant source of nitrogen. Additions of glucose (0.1 to 1.0 mu-M) increased the contribution of NH4+ and DON other than DFAA to the bacterial N-demand. In most cases, measurements of amino acid and NH4+ uptake are sufficient for estimating bacterial nitrogen use.
CITATION STYLE
Keil, R., & Kirchman, D. (1991). Contribution of dissolved free amino acids and ammonium to the nitrogen requirements of heterotrophic bacterioplankton. Marine Ecology Progress Series, 73, 1–10. https://doi.org/10.3354/meps073001
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