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Climate Impact on Plankton Ecosystems in the Northeast Atlantic
Anthony J. Richardson1* and
David S. Schoeman2
It is now widely accepted that global warming is occurring,yet its effects on the world's largest ecosystem, the marinepelagic realm, are largely unknown. We show that sea surfacewarming in the Northeast Atlantic is accompanied by increasingphytoplankton abundance in cooler regions and decreasing phytoplanktonabundance in warmer regions. This impact propagates up the foodweb (bottom-up control) through copepod herbivores to zooplanktoncarnivores because of tight trophic coupling. Future warmingis therefore likely to alter the spatial distribution of primaryand secondary pelagic production, affecting ecosystem servicesand placing additional stress on already-depleted fish and mammalpopulations.
1 Sir Alister Hardy Foundation for Ocean Science, The Laboratory, Citadel Hill, Plymouth, PL1 2PB, UK. 2 Department of Zoology, University of Port Elizabeth, Port Elizabeth, South Africa.
* To whom correspondence should be addressed. E-mail: anr{at}sahfos.ac.uk
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