Publication | Open Access
Limitation of phytoplankton production by Si and N in the western Atlantic Ocean
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2007
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EngineeringCalifornia Los AngelesCoral EcosystemsMarine ChemistryMarine SystemsOceanographyAmazon River PlumePrimary ProductionMarine EnvironmentMarine PollutionMicrobial EcologyBiological OceanographyPhytoplankton ProductionWestern Atlantic OceanOceanic SystemsLos AngelesBiogeochemistryPhytoplankton EcologyBiologyBloom EcologyMarine EcologyMarine Biology
MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 338:33-45 (2007) - doi:10.3354/meps338033 Limitation of phytoplankton production by Si and N in the western Atlantic Ocean Rebecca F. Shipe1,*, Edward J. Carpenter2, Sarah R. Govil2, Douglas G. Capone3 1Department of Ecology and Evolutionary Biology, University of California Los Angeles, Los Angeles, California 90095, USA 2Romburg Tiburon Center, San Francisco State University, Tiburon, California 94920, USA 3Wrigley Institute for Environmental Studies and Department of Biological Science, University of Southern California, Los Angeles, California 90089, USA *Email: rshipe@ucla.edu ABSTRACT: Large areas of the western tropical Atlantic Ocean are influenced by the Amazon River plume, in which dissolved inorganic nitrogen (DIN) concentrations are low and nutrient N:P and N:Si ratios are lower than elemental ratios typical of phytoplankton. Accordingly, nutrient concentrations and ratios measured during winter (January to February 2001) and summer (July to August 2001) cruises in the area 2 to 14°N and 57 to 40°W suggest that DIN may limit phytoplankton growth at the majority of the 40 stations sampled. As diatoms are the dominant plankton in the Amazon plumewaters, short-term nutrient enrichment experiments were conducted to determine whether ambient N, P, or Si limited silica production rates (SiP). Results indicated that SiP were substrate limited both above and below the pycnocline at the majority of stations during both high (summer cruise) and low (winter cruise) discharge conditons. DIN concentrations also limited SiP in plumewater stations, but N additions depressed SiP at other stations, possibly using energy to take up the limiting nutrient. Finally, primary production rates were limited by ambient dissolved silicon concentrations at 9 of 13 summer stations. These results indicate the importance of dissolved silicon availability in controlling phytoplankton growth rates in a diatom-dominated river plume system. KEY WORDS: Nutrient limitation · Nutrient enrichment · Tropical Atlantic Ocean · Amazon River plume · Silicon · Primary productivity · Diatoms Full text in pdf format PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 338. Online publication date: May 24, 2007 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2007 Inter-Research.
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