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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Detalles Bibliográficos
Autores principales: 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: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2015
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4375859/
https://www.ncbi.nlm.nih.gov/pubmed/25716793
http://dx.doi.org/10.1098/rspb.2014.2604

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4375859/
https://www.ncbi.nlm.nih.gov/pubmed/25716793
http://dx.doi.org/10.1098/rspb.2014.2604

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