Diazotrophic cyanobacteria, including those responsible for harmful algal blooms, fix atmospheric dinitrogen (N2) to sustain growth when they are limited by dissolved inorganic nitrogen (DIN) supply. Conventional models fail to accurately predict the timing and magnitude of N2 fixation, partly because of oversimplified assumptions about diazotrophic species responses to N. We hypothesized that cellular carbon (C) and N would co‐vary with DIN availability, and cellular N quota reduced below a critical threshold would trigger heterocyst differentiation and N2 fixation. Conversely, we hypothesized that heterocysts would be discarded, and N2 fixation would cease at another higher cellular N quota threshold. To test this hypothesis, we undertook experiments to provide data to calibrate a model of cellular C and N of N2 fixation in the cyanobacterium Raphidiopsis raciborskii. The model incorporated internal N quotas, external DIN supply and a time lag for N2 fixation as key regulators of heterocyst production and N2 fixation, explaining > 70% of the variation in measured cellular N and C : N molar ratios. Heterocysts were predicted to form at a cellular N quota of 0.085 mg N mg−1 C and were discarded from filaments at 0.275 mg N mg−1 C. There was a 5‐d time lag between DIN deprivation and initiation of N2 fixation. Continuous DIN supply was predicted to enhance N2 fixation more than an equivalent one‐off pulse. Our study highlighted the need to consider cellular N and N supply regimes in driving N2 fixation to provide more accurate predictions of the response of cyanobacteria to DIN availability.
Nitrogen fixation is driven by cellular nitrogen stores in a diazotrophic cyanobacterium: Evidence from culture experiments and model validation
Man Xiao,Michele A. Burford,M. Frassl,A. Willis,Melanie E. Roberts,D. P. Hamilton
Published 2026 in Limnology and Oceanography
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2026
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Limnology and Oceanography
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2026-02-01
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