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Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession

Human activity causes ocean acidification (OA) though the dissolution of anthropogenically generated CO(2) into seawater, and eutrophication through the addition of inorganic nutrients. Eutrophication increases the phytoplankton biomass that can be supported during a bloom, and the resultant uptake...

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Detalhes bibliográficos
Publicado no:Proc Biol Sci
Main Authors: Flynn, Kevin J., Clark, Darren R., Mitra, Aditee, Fabian, Heiner, Hansen, Per J., Glibert, Patricia M., Wheeler, Glen L., Stoecker, Diane K., Blackford, Jerry C., Brownlee, Colin
Formato: Artigo
Idioma:Inglês
Publicado em: The Royal Society 2015
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Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC4375859/
https://ncbi.nlm.nih.gov/pubmed/25716793
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspb.2014.2604
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