Sj. Bury et al., Size-fractionated primary production and nitrogen uptake during a North Atlantic phytoplankton bloom: implications for carbon export estimates, DEEP-SEA I, 48(3), 2001, pp. 689-720
Citations number
118
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
A Lagrangian experiment was set up at 47 degreesN 20 degreesW in the northe
ast Atlantic as part of the Joint Global Ocean Flux Study (JGOFS) programme
. As an integral part of the programme, this study investigated the uptake
of carbon and nitrogen into different algal size classes, and quantified th
e export of carbon using N-15 stable isotope and C-14 radioisotope studies.
Good quality f-ratio field data is of fundamental importance to multi-comp
artment nitrogen-based upper ocean ecosystem modelling of carbon fluxes: th
is study provides an appraisal of current north Atlantic field measurements
making comparisons with our findings. A phytoplankton bloom was tracked fo
r 18 d from 1 May 1990. Waters were initially well-mixed with surface nutri
ents of 4-6 mmol NO3 m(-3) and 1.5-2.5 mmol SiO4 m(-3) and surface biomass
of 1-1.5 mg chl a m(-3), indicating the likely onset of a bloom. Increased
insolation and vertical stability produced a diatom-dominated bloom with a
surface biomass peak of 3.5 mg chl a m(-3), decreased nutrient values (0.5
mmol NO3 m(-3), 0.35 mmol SiO4 m(-3)), and maximum integrated carbon uptake
values of 1970 mg C m(-2) d(-1) on 17 May. Maximum nitrogen uptake values
of 251 mg NO3 m(-2) d(-1) were measured on 14 May during the greatest flage
llate growth phase. Integrated production rates over the experiment ranged
from 0.5 to 1.0 g C m(-2) d(-1), and carbon export was estimated at 480 (us
ing NO3 uptake and Redfield ratios) or 570 (using integrated C assimilation
values and the mean weighted f-ratio) mg C m(-2) d(-1). The decoupling of
maximum carbon and nitrogen uptake rates over a three-day period indicates
that it may not be appropriate to use Redfield ratios to convert nitrate-es
timated new production to carbon export values, even over time scales of a
month. Primary production values are comparable to 1989 North Atlantic Bloo
m Experiment (NABE) data, despite the fact that phytoplanktonic taxonomic d
ata for the 1990 bloom were very different from the more typical bloom cond
itions of 1989. Throughout the experiment the greatest biomass occurred in
the 1-5 mum size range, which accounted for an average of 50% of the total
production and > 50% of nitrate uptake and ammonium uptake. In addition, bo
th the net- and nanoplankton communities preferentially assimilated nitrate
, which challenges the assumption that new production can be directly equat
ed to export production on the time-scale of weeks. (C) 2000 Elsevier Scien
ce Ltd. All rights reserved.