Feedback on N:P Ratio

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Chain of events set in motion by a high nitrate to phosphate ratio in seawater, leading to a return in the ratio towards lower values

The nitrogen-phosphorus model contains the feedback on phosphate levels, but also contains a second feedback which stabilises the ocean's N:P (nitrate:phosphate) ratio. This feedback involves the ecological competition between nitrogen-fixing and non-nitrogen-fixing algae. It controls nitrate concentrations, pushing them continually slightly towards less than 16 times the phosphate concentration.

When the N:P ratio in the deep oceans falls too low, water upwelling from deep contains a deficit of fixed nitrogen relative to phosphate. After blooms of diatoms and other phytoplankton remove fixed nitrogen and phosphate in a ratio of about 16:1, fixed nitrogen becomes exhausted while quantities of phosphate remain. The model contains the key assumption that these conditions are ideal for the proliferation of nitrogen-fixing phytoplankton, because only they can meet their nitrogen needs from alternative sources, because they (uniquely) are able to take up the plentiful N2. Nitrogen fixation inputs increase. Following death and decay of these organisms, the nitrogen in their cells is released initially as ammonium and then converted via nitrification to nitrate. Blooms of nitrogen fixers act in this way as conduits for the creation of new fixed nitrogen. Stimulation of nitrogen-fixer proliferation thereby indirectly raises the N:P ratio, completing the negative fedback loop.

Conversely, when the [NO3-]:[PO4+] ratio rises too high, nitrogen-fixers become uncompetitive and nitrogen-fixation inputs decrease. The cutting off of a source of new fixed nitrogen tips the balance towards net destruction of fixed nitrogen, lowering the ratio.


  • Fixed nitrogen refers to the sum of nitrate (NO3), nitrite (NO2) and ammonium (NH4). It excludes the always plentiful N2. In deep waters fixed nitrogen is almost all made up of nitrate.
  • Fixed nitrogen is continually being destroyed in low oxygen environments by the processes of denitrification and anammox. The N:P ratio will rise or fall depending on whether the sum of inputs (in large part nitrogen-fixation) is greater or lesser than the sum out outputs (predominantly denitrification and anammox).
Chain of events set in motion by a high nitrate to phosphate ratio in seawater, leading to a return in the ratio towards lower values
Negative feedbacks on nitrate and phosphate as viewed in nitrate:phosphate space

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