Preprints
https://doi.org/10.5194/bg-2023-10
https://doi.org/10.5194/bg-2023-10
 
23 Jan 2023
23 Jan 2023
Status: this preprint is currently under review for the journal BG.

Biogeochemistry of climate driven shifts in Southern Ocean primary producers

Ben J. Fisher1, Alex J. Poulton2, Michael P. Meredith3, Kimberlee Baldry4, Oscar Schofield5, and Sian F. Henley1 Ben J. Fisher et al.
  • 1School of GeoSciences, University of Edinburgh, Edinburgh, United Kingdom
  • 2The Lyell Centre for Earth and Marine Science, Heriot-Watt University, Edinburgh, United Kingdom
  • 3British Antarctic Survey, Cambridge, United Kingdom
  • 4Institute for Marine and Antarctic Studies, College of Sciences and Engineering, University of Tasmania, Hobart, TAS, Australia
  • 5Center of Ocean Observing Leadership, School of Environmental and Biological Sciences, Rutgers University, New Brunswick, NJ 08901, USA

Abstract. As a net source of nutrients fuelling global primary production, changes in Southern Ocean productivity are expected to influence biological carbon storage across the global ocean. Following a high emissions, low mitigation pathway, primary productivity in the Southern Ocean is predicted to increase by up to 40 % over the 21st century. The ecophysiological response of marine phytoplankton experiencing climate change will be a key determinant in understanding the impact of Southern Ocean productivity shifts on the carbon cycle. Yet, phytoplankton ecophysiology is poorly represented in CMIP6 climate models, leading to substantial uncertainty in the representation of their role in carbon sequestration. Here we synthesise the existing spatial and temporal projections of Southern Ocean productivity from CMIP6 models, separated by phytoplankton class and identify key processes where greater observational data coverage can help to improve future model performance. We find bidirectional changes in iron and light limitation of phytoplankton, while the greatest changes in productivity occur in the coastal zone of the Southern Ocean. Different phytoplankton groups are responsible for driving productivity increases at different latitudes, yet we observe that models disagree on the ecological mechanism behind these productivity changes. We propose that an evidence-based sampling approach targeting climate-driven changes in ocean biogeochemistry and community assemblages in the regions of rapid projected productivity changes could help to resolve the empirical principles underlying phytoplankton community structure in the Southern Ocean.

Ben J. Fisher et al.

Status: open (until 06 Mar 2023)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Ben J. Fisher et al.

Ben J. Fisher et al.

Viewed

Total article views: 193 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
123 66 4 193 11 2 2
  • HTML: 123
  • PDF: 66
  • XML: 4
  • Total: 193
  • Supplement: 11
  • BibTeX: 2
  • EndNote: 2
Views and downloads (calculated since 23 Jan 2023)
Cumulative views and downloads (calculated since 23 Jan 2023)

Viewed (geographical distribution)

Total article views: 193 (including HTML, PDF, and XML) Thereof 193 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 28 Jan 2023
Download
Short summary
The Southern Ocean is warming faster than the global average. As a globally important carbon sink and nutrient source, climate driven changes in ecosystems can be expected to cause widespread changes to biogeochemical cycles. We analysed earth system models and showed that productivity is expected to increase across the Southern Ocean, driven by different phytoplankton groups at different latitudes. These predictions carry large uncertainties, we propose targeted studies to reduce this error.
Altmetrics