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Inter Research, Marine Ecology Progress Series, (545), p. 49-62, 2016

DOI: 10.3354/meps11600

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Dissolved N:P ratio changes in the eastern tropical North Atlantic: effect on phytoplankton growth and community structure

Journal article published in 2016 by Jms Czerny, H. Hauss, Cr Löscher, U. Riebesell ORCID
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Abstract

Results from previous bioassays conducted in the oligotrophic Atlantic Ocean determined availability of inorganic nitrogen (N) as the proximal limiting nutrient control of primary production, but additionally displayed a synergistic growth effect of combined N and P addition. To classify conditions of nutrient limitation of coastal phytoplankton in the tropical ocean, we performed an 11-day nutrient enrichment experiment with a natural phytoplankton community from shelf waters off Northwest Africa in shipboard mesocosms. We used pigment and gene fingerprinting in combination with flow cytometry for classification and quantification of the taxon-specific photoautotrophic response to differences in nutrient supply. The developing primary bloom was dominated by diatoms and significantly higher in the treatments receiving initial N addition. The combined supply of N and P did not induce a further increase in phytoplankton abundance compared to high N addition alone. A secondary bloom during the course of the experiment displayed again higher primary producer standing stock in the N-fertilized treatments. Bacterial abundance correlated positively with phytoplankton biomass. Dominance of the photoautotrophic assemblage by N-limited diatoms in conjunction with a probable absence of any P-limited phytoplankton species prevented an additive effect of combined N and P addition on total phytoplankton biomass. Furthermore, after nutrient exhaustion dinitrogen (N2) fixing cyanobacteria succeeded the bloom-forming diatoms. Shelf waters in the tropical East Atlantic may thus support growth of diazotrophic cyanobacteria such as Trichodesmium sp. subsequent to upwelling pulses.