Isotopic constraints on the pre-industrial oceanic nitrogen budget

The size of the bioavailable (i.e., “fixed”) nitrogen inventory in the ocean influences global marine productivity and the biological carbon pump. Despite its importance, the pre-industrial rates for the major source and sink terms of the oceanic fixed nitrogen budget, N2 fixation and denitrification, respectively, are not well known. These processes leave distinguishable imprints on the ratio of stable nitrogen isotopes, δ15N, which can therefore help to infer their patterns and rates. Here we use δ15N observations from the water column and a new database of seafloor measurements to constrain rates of N2 fixation and denitrification predicted by a global three-dimensional Model of Ocean Biogeochemistry and Isotopes (MOBI). Sensitivity experiments were performed to quantify uncertainties associated with the isotope effect of denitrification in the water column and sediments. They show that the level of nitrate utilization in suboxic zones, that is the balance between nitrate consumption by denitrification and nitrate replenishment by circulation and mixing (dilution effect), significantly affects the isotope effect of water column denitrification and thus global mean δNO−3 . Experiments with lower levels of nitrate utilization within the suboxic zone (i.e., higher residual water column nitrate concentrations, ranging from 20 to 32 μM) require higher ratios of benthic to water column denitrification, BD : WCD= 0.75–1.4, to satisfy the global mean NO−3 and δNO−3 constraints in the modern ocean. This suggests that nitrate utilization in suboxic zones plays an important role in global nitrogen isotope cycling. Increasing the net fractionation factor εBD for benthic denitrification (εBD = 0–4 ‰) requires even higher ratios, BD : WCD= 1.4–3.5. The model experiments that best reproduce observed seafloor δ15N support the middle to high-end estimates for the net fractionation factor of benthic denitrification (εBD = 2–4 ‰). Assuming a balanced fixed nitrogen budget, we estimate that preindustrial rates of N2 fixation, water column denitrification, and benthic denitrification were between 195–350 (225), 65– 80 (76), and 130–270 (149) Tg N yr−1, respectively, with our best model estimate (εBD = 2 ‰) in parentheses. Although uncertainties still exist, these results suggest that marine N2 fixation is occurring at much greater rates than previously estimated and the residence time for oceanic fixed nitrogen is between ∼ 1500 and 3000 yr.