Articles | Volume 11, issue 21
Biogeosciences, 11, 6147–6157, 2014
Biogeosciences, 11, 6147–6157, 2014

Research article 13 Nov 2014

Research article | 13 Nov 2014

The fractionation of nitrogen and oxygen isotopes in macroalgae during the assimilation of nitrate

P. K. Swart1, S. Evans1,*, T. Capo2, and M. A. Altabet3 P. K. Swart et al.
  • 1Division of Marine Geology and Geophysics, Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, 4600 Rickenbacker Causeway, Miami, Fl 33149, USA
  • 2Division of Marine Biology and Fisheries, Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, 4600 Rickenbacker Causeway, Miami, Fl 33149, USA
  • 3School for Marine Science and Technology, University of Massachusetts Dartmouth, New Bedford, MA 02744, USA
  • *now at: Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725-1535, USA

Abstract. In order to determine and understand the stable isotope fractionation of 18O and 15N manifested during assimilation of NO3 in marine macro-benthic algae, two species (Ulva sp. and Agardhiella sp.) have been grown in a wide range of NO3 concentrations (2–500 μM). Two types of experiments were performed. The first was one in which the concentration of the NO3 was allowed to drift downward as it was assimilated by the algae, between 24 hour replacements of media. These experiments proceeded for periods of between 7 and 10 days. A second set of experiments maintained the NO3 concentration at a low steady-state value by means of a syringe pump. The effective fractionation during the assimilation of the NO3 was determined by measuring the δ15N of both the (i) new algal growth and (ii) residual NO3 in the free-drift experiments after 0, 12, 24 and 48 h. Modelling these data show that the fractionation during assimilation is dependent upon the concentration of NO3 and is effectively 0 at concentrations of less than ~2 μM. The change in the fractionation with respect to concentration is the greatest at lower concentrations (2–10 μM). The fractionation stablizes between 4 and 6‰ at concentrations of between 50 and 500 μM. Although the δ18O and δ15N values of NO3 in the residual solution were correlated, the slope of relationship also varied with respect to NO3 concentration, with slopes of greater than unity at low concentration. These results suggest shifts in the dominant fractionation mechanism of 15N and 18O between concentrations of 1 and 10 μM NO3. At higher NO3 concentrations (>10–50 μM), fractionation during assimilation will lead to δ15N values in algal biomass lower than the ambient NO3 and 15N enrichments in the residual NO3.

Short summary
The ratio of nitrogen-15 to nitrogen-14 of macroalgae has been termed the DNA of sewage. Higher amounts of N-15 have been suggested to indicate the influence of sewage-derived N. But what exactly does the ratio of 15N/14N record? We found that the nitrogen isotopic ratio was dependent upon not only the value in the water but also its concentration of nitrate. At low concentration there was little fractionation, but at higher values the uptake by algae left more of the N-15 in the water.
Final-revised paper