Widespread phytoplankton blooms triggered by 2019–2020 Australian wildfires

• Published in: Nature
• Main Authors: Tang, W, Llort, J, Weis, J, Perron, MMG, Basart, S, Li, Z, Sathyendranath, S, Jackson, T, Sanz Rodriguez, E, Proemse, B, Bowie, AR, Schallenberg, C, Strutton, PG, Matear, R, Cassar, N
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Nature Publishing Group 2021
• Subjects: wildfire; phytoplankton bloom; Australian wildfires; Southern Ocean
• Online Access: https://eprints.utas.edu.au/37826/

Droughts and climate-change-driven warming are leading to more frequent and intense wildfires1,2,3, arguably contributing to the severe 2019–2020 Australian wildfires4. The environmental and ecological impacts of the fires include loss of habitats and the emission of substantial amounts of atmospheric aerosols5,6,7. Aerosol emissions from wildfires can lead to the atmospheric transport of macronutrients and bio-essential trace metals such as nitrogen and iron, respectively8,9, 10. It has been suggested that the oceanic deposition of wildfire aerosols can relieve nutrient limitations and, consequently, enhance marine productivity11,12, but direct observations are lacking. Here we use satellite and autonomous biogeochemical Argo float data to evaluate the effect of 2019–2020 Australian wildfire aerosol deposition on phytoplankton productivity. We find anomalously widespread phytoplankton blooms from December 2019 to March 2020 in the Southern Ocean downwind of Australia. Aerosol samples originating from the Australian wildfires contained a high iron content and atmospheric trajectories show that these aerosols were likely to be transported to the bloom regions, suggesting that the blooms resulted from the fertilization of the iron-limited waters of the Southern Ocean. Climate models project more frequent and severe wildfires in many regions1,2,3. A greater appreciation of the links between wildfires, pyrogenic aerosols13, nutrient cycling and marine photosynthesis could improve our understanding of the contemporary and glacial–interglacial cycling of atmospheric CO2 and the global climate system.