Iron availability limits the ocean nitrogen inventory stabilizing feedbacks between marine denitrification and nitrogen fixation
Figure S2: The N* tracer (= ([NO3−] + [NH4+]) − 16 * [PO4−]) averaged over sub-euphotic zone depths (103–215 m) plotted over time for each of the case experiments at global and basin scales. (776.5Kb)
Figure S3: The minimum O2 concentration within the water column at each location plotted from the World Ocean Atlas 2001 data, from our control (year 2050) and case experiment simulations (year 200). (1.187Mb)
Figure S4: Spatial patterns for the N* tracer (= ([NO3−] + [NH4+]) − 16 * [PO4−]) averaged over euphotic zone depths (<103 m) for the WOA2001 and each of our case experiments. (1.165Mb)
Table S2: Global scale fluxes and inventories from our control simulation (year 2050) and the difference from our six case experiments. (2.122Kb)
MetadataShow full item record
Recent upward revisions in key sink/source terms for fixed nitrogen (N) in the oceans imply a short residence time and strong negative feedbacks involving denitrification and N fixation to prevent large swings in the ocean N inventory over timescales of a few centuries. We tested the strength of these feedbacks in a global biogeochemical elemental cycling (BEC) ocean model that includes water column denitrification and an explicit N fixing phytoplankton group. In the northern Indian Ocean and over longer timescales in the tropical Atlantic, we find strong stabilizing feedbacks that minimize changes in marine N inventory over timescales of ∼30–200 years. In these regions high atmospheric dust/iron inputs lead to phosphorus limitation of diazotrophs, and thus a tight link between N fixation and surface water N/P ratios. Maintenance of the oxygen minimum zones in these basins depends on N fixation driven export. The stabilizing feedbacks in other regions are significant but weaker owing to iron limitation of the diazotrophs. Thus Fe limitation appears to restrict the ability of N fixation to compensate for changes in denitrification in the current climate, perhaps leading the oceans to lose fixed N. We suggest that iron is the ultimate limiting nutrient leading to nitrogen being the proximate limiting nutrient over wide regions today. Iron stress was at least partially alleviated during more dusty, glacial times, leading to a higher marine N inventory, increased export production, and perhaps widespread phosphorus limitation of the phytoplankton community. The increased efficiency of the biological pump would have contributed to the glacial drawdown in atmospheric CO2.
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 21 (2007): GB2001, doi:10.1029/2006GB002762.
Suggested CitationArticle: Moore, J. Keith, Doney, Scott C., "Iron availability limits the ocean nitrogen inventory stabilizing feedbacks between marine denitrification and nitrogen fixation", Global Biogeochemical Cycles 21 (2007): GB2001, DOI:10.1029/2006GB002762, https://hdl.handle.net/1912/3403
Showing items related by title, author, creator and subject.
Cole, Marci L.; Kroeger, Kevin D.; McClelland, James W.; Valiela, Ivan (2005-07-18)Eutrophication is a major agent of change affecting freshwater, estuarine, and marine systems. It is largely driven by transportation of nitrogen from natural and anthropogenic sources. Research is needed to quantify ...
Phosphate availability and the ultimate control of new nitrogen input by nitrogen fixation in the tropical Pacific Ocean Moutin, T.; Karl, David M.; Duhamel, Solange; Rimmelin, P.; Raimbault, P.; Van Mooy, Benjamin A. S.; Claustre, Hervé (Copernicus Publications on behalf of the European Geosciences Union, 2008-01-29)Due to the low atmospheric input of phosphate into the open ocean, it is one of the key nutrients that could ultimately control primary production and carbon export into the deep ocean. The observed trend over the last 20 ...
Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes Brunelle, Brigitte G.; Sigman, Daniel M.; Cook, Mea S.; Keigwin, Lloyd D.; Haug, Gerald H.; Plessen, Birgit; Schettler, Georg; Jaccard, Samuel L. (American Geophysical Union, 2007-03-02)In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured over the last glacial/interglacial cycle. ...