Optimality-based model of phytoplankton growth and diazotrophy

The notion that excess phosphorus (P) and high irradiance favour pelagic diazotrophy is difficult to reconcile with diazotroph behaviour in laboratory experiments and also with the observed distribution of N-2-fixing Trichodesmium, e. g. in the relatively nitrogen (N)-rich North Atlantic Ocean. Nevertheless, this view currently provides the stateof- the-art framework to understand both past dynamics and future evolution of the oceanic fixed N inventory. In an attempt to provide a consistent theoretical underpinning for marine autotrophic N-2 fixation we derive controls of diazotrophy from an optimality-based model that accounts for phytoplankton growth and N-2 fixation. Our approach differs from existing work in that conditions favourable for diazotrophy are not prescribed but emerge, indirectly, from trade-offs among energy and cellular resource requirements for the acquisition of P, N, and carbon. Our model reproduces laboratory data for a range of ordinary phytoplankton species and Trichodesmium. The model predicts that (1) the optimal strategy for facultative diazotrophy is switching between N-2 fixation and using dissolved inorganic nitrogen (DIN) at a threshold DIN concentration; (2) oligotrophy, especially in P and under high light, favours diazotrophy; (3) diazotrophy is compatible with DIN: DIP supply ratios well above Redfield proportions; and (4) communities of diazo trophs competing with ordinary phytoplankton decouple emerging ambient and supply DIN: DIP ratios. Our model predictions appear in line with major observed patterns of diazotrophy in the ocean. The predicted importance of oligotrophy in P extends the present view of N-2 fixation beyond a simple control by excess P in the surface ocean.