An iron cycle cascade governs the response of equatorial Pacific ecosystems to climate change

Type Article
Date 2020-11
Language English
Author(s) Tagliabue Alessandro1, Barrier Nicolas2, Du Pontavice Hubert3, 4, Kwiatkowski Lester5, Aumont Olivier5, Bopp Laurent6, Cheung William W. L.4, Gascuel Didier3, Maury Olivier2
Affiliation(s) 1 : School of Environmental Sciences University of Liverpool Liverpool, UK
2 : MARBEC (IRD, Univ. Montpellier, CNRS, Ifremer) Sète, France
3 : ESE, Ecology and Ecosystem Health Institut Agro Rennes, France
4 : Nippon Foundation‐Nereus Program Institute for the Oceans and Fisheries University of British Columbia Vancouver BC ,Canada
5 : LOCEAN Sorbonne Université‐CNRS‐IRD‐MNHN Paris ,France
6 : ENS‐LMD Paris ,France
Source Global Change Biology (1354-1013) (Wiley), 2020-11 , Vol. 26 , N. 11 , P. 6168-6179
DOI 10.1111/gcb.15316
WOS© Times Cited 1
Keyword(s) climate change, iron, marine ecosystems, net primary production, ocean

Earth System Models project that global climate change will reduce ocean net primary production (NPP), upper trophic level biota biomass and potential fisheries catches in the future, especially in the eastern equatorial Pacific. However, projections from Earth System Models are undermined by poorly constrained assumptions regarding the biological cycling of iron, which is the main limiting resource for NPP over large parts of the ocean. In this study, we show that the climate change trends in NPP and the biomass of upper trophic levels are strongly affected by modifying assumptions associated with phytoplankton iron uptake. Using a suite of model experiments, we find 21st century climate change impacts on regional NPP range from −12.3% to +2.4% under a high emissions climate change scenario. This wide range arises from variations in the efficiency of iron retention in the upper ocean in the eastern equatorial Pacific across different scenarios of biological iron uptake, which affect the strength of regional iron limitation. Those scenarios where nitrogen limitation replaced iron limitation showed the largest projected NPP declines, while those where iron limitation was more resilient displayed little future change. All model scenarios have similar skill in reproducing past inter‐annual variations in regional ocean NPP, largely due to limited change in the historical period. Ultimately, projections of end of century upper trophic level biomass change are altered by 50%–80% across all plausible scenarios. Overall, we find that uncertainties in the biological iron cycle cascade through open ocean pelagic ecosystems, from plankton to fish, affecting their evolution under climate change. This highlights additional challenges to developing effective conservation and fisheries management policies under climate change.

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Tagliabue Alessandro, Barrier Nicolas, Du Pontavice Hubert, Kwiatkowski Lester, Aumont Olivier, Bopp Laurent, Cheung William W. L., Gascuel Didier, Maury Olivier (2020). An iron cycle cascade governs the response of equatorial Pacific ecosystems to climate change. Global Change Biology, 26(11), 6168-6179. Publisher's official version : , Open Access version :