Articles | Volume 16, issue 6
https://doi.org/10.5194/esd-16-2101-2025
https://doi.org/10.5194/esd-16-2101-2025
Research article
 | 
20 Nov 2025
Research article |  | 20 Nov 2025

Irreversible phytoplankton community shifts over Subpolar North Atlantic in response to CO2 forcing

Dong-Geon Lee, Eun Young Kwon, Jonghun Kam, and Jong-Seong Kug

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Cited articles

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An, S. Il, Park, H. J., Kim, S. K., Shin, J., Yeh, S. W., and Kug, J. S.: Intensity changes of Indian Ocean dipole mode in a carbon dioxide removal scenario, npj Clim. Atmos. Sci., 5, 1–8, https://doi.org/10.1038/s41612-022-00246-6, 2022. 
Anderson, S. I., Barton, A. D., Clayton, S., Dutkiewicz, S., and Rynearson, T. A.: Marine phytoplankton functional types exhibit diverse responses to thermal change, Nat. Commun., 12, 1–9, https://doi.org/10.1038/s41467-021-26651-8, 2021. 
Archibald, K. M., Dutkiewicz, S., Laufkötter, C., and Moeller, H. V.: Thermal Responses in Global Marine Planktonic Food Webs Are Mediated by Temperature Effects on Metabolism, J. Geophys. Res. Ocean., 127, 1–18, https://doi.org/10.1029/2022JC018932, 2022. 
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Short summary
Phytoplankton communities in the Sub-Polar North Atlantic shift towards smaller species under greenhouse warming, with limited recovery even under CO2 removal. This shift results from reduced surface nutrient availability caused by the weakened Atlantic Meridional Overturning Circulation (AMOC), which recovers slowly. Nutrient depletion disrupts trophic dynamics, decreasing diatoms and increasing smaller phytoplankton, leading to a significant reduction in the ocean's carbon export capacity.
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