Articles | Volume 11, issue 24
Biogeosciences, 11, 7125–7135, 2014
https://doi.org/10.5194/bg-11-7125-2014
Biogeosciences, 11, 7125–7135, 2014
https://doi.org/10.5194/bg-11-7125-2014
Research article
16 Dec 2014
Research article | 16 Dec 2014

Drivers of trophic amplification of ocean productivity trends in a changing climate

C. A. Stock et al.

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Cited articles

Armstrong, R. A., Lee, C., Hedges, J. I., Honjo, S., and Wakeham, S. G.: A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals, Deep-Sea Res.-Pt. II, 49, 219–236, 2002.
Aumont, O., Maier-Reimer, E., Blain, S., and Monfray, P.: An ecosystem model of the global ocean including Fe, Si, P co-limitation, Global Biogeochem. Cy., 17, 1060, https://doi.org/10.1029/2001GB001745, 2003.
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Barange, M., Merino, G., Blanchard, J. L., Scholtens, J., Harle, J., Allison, E. H., Allen, J. I., Holt, J., and Jennings, S.: Impacts of climate change on marine ecosystem production in societies dependent on fisheries, Nature Climate Change, 4, 211–216, https://doi.org/10.1038/Nclimate2119, 2014.
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Short summary
Climate change projections suggest large regional ocean productivity shifts for mesozooplankton, an important food resource for fish, which are amplified relative to changes in phytoplankton production. Amplification is attributed to changes in planktonic food web dynamics under global warming. Results have implications for regional economies and food security. Improved understanding of the response of plankton food webs to climate change is essential to refine amplification estimates.
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