4.8 Article

Integrating the impact of global change on the niche and physiology of marine nitrogen-fixing cyanobacteria

Journal

GLOBAL CHANGE BIOLOGY
Volume 28, Issue 23, Pages 7078-7093

Publisher

WILEY
DOI: 10.1111/gcb.16399

Keywords

climate change; earth system models; elemental use efficiency; marine nitrogen fixation; microbial thermal fitness

Funding

  1. H2020 European Research Council [724289]
  2. National Science Foundation [OCE 1851222, OCE 2149837]
  3. Natural Environment Research Council [NE/L002469/1]
  4. European Research Council (ERC) [724289] Funding Source: European Research Council (ERC)

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Marine nitrogen fixation is an important source of new nitrogen in the ocean, but climate change may affect the ecological niche and physiology of nitrogen-fixing organisms. Warming can increase the nitrogen fixation-specific elemental use efficiency (EUE) of diazotrophs, reducing their nutrient requirements. A new model predicts a global decline in nitrogen fixation in the future, but regional responses are influenced by the thermal performance curves and EUE of diazotrophs.
Marine nitrogen fixation is a major source of new nitrogen to the ocean, which interacts with climate driven changes to physical nutrient supply to regulate the response of ocean primary production in the oligotrophic tropical ocean. Warming and changes in nutrient supply may alter the ecological niche of nitrogen-fixing organisms, or 'diazotrophs', however, impacts of warming on diazotroph physiology may also be important. Lab-based studies reveal that warming increases the nitrogen fixation-specific elemental use efficiency (EUE) of two prevalent marine diazotrophs, Crocosphaera and Trichodesmium, thus reducing their requirements for the limiting nutrients iron and phosphorus. Here, we coupled a new diazotroph model based upon observed diazotroph energetics of growth and resource limitation to a state-of-the-art global model of phytoplankton physiology and ocean biogeochemistry. Our model is able to address the integrated response of nitrogen fixation by Trichodesmium and Crocosphaera to warming under the IPCC high emission RCP8.5 scenario for the first time. Our results project a global decline in nitrogen fixation over the coming century. However, the regional response of nitrogen fixation to climate change is modulated by the diazotroph-specific thermal performance curves and EUE, particularly in the Pacific Ocean, which shapes global trends. Spatially, the response of both diazotrophs is similar with expansion towards higher latitudes and reduced rates of nitrogen fixation in the lower latitudes. Overall, 95%-97% of the nitrogen fixation climate signal can be attributed to the combined effect of temperature on the niche and physiology of marine diazotrophs, with decreases being associated with a reduced niche and increases resulting due to a combination of expanding niche and temperature driven changes to EUE. Climate change impacts on both the niche and physiology of marine diazotrophs interact to shape patterns of marine nitrogen fixation, which will have important implications for ocean productivity in the future.

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