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SOIREE Experiment

The results of the SOIREE experiment were similar in many ways but were not as definitive with respect to carbon flux. In this experiment biomass increased 6-fold, nitrate was depleted by 2pmol 1 and carbon dioxide by 35-40 microatmospheres (3.5-4.0 Pa). This was a greatly attenuated signal relative to IronEx II. Colder water temperatures likely led to slower rates of production and bloom evolution and there was no observable carbon flux. [Pg.108]

Trull, T.W. and Armand, L. (2001) Insights into Southern Ocean carbon export from die S13C of particles and dissolved inorganic carbon during die SOIREE iron release experiment. Deep-Sea... [Pg.237]

An interesting example of a well defined localized perturbation of the plankton ecosystem was produced by the SOIREE iron fertilization experiment (Abraham et al., 2000) with the aim to test the hypothesis of iron limitation of growth in regions with high nutrient, but low natural phytoplankton concentration. As it was expected,... [Pg.219]

NADPH Reduced form of nicotinamide-adenine dinucleotide phosphate SOIREE Southern Ocean Iron Enrichment Experiment... [Pg.110]

SOIREE Southern Ocean Iron Enrichment Experiment... [Pg.184]

See other pages where SOIREE Experiment is mentioned: [Pg.1631]    [Pg.2956]    [Pg.229]    [Pg.106]    [Pg.107]    [Pg.109]    [Pg.1631]    [Pg.2956]    [Pg.229]    [Pg.106]    [Pg.107]    [Pg.109]    [Pg.16]    [Pg.66]    [Pg.574]    [Pg.1637]    [Pg.2955]    [Pg.104]    [Pg.106]    [Pg.106]    [Pg.180]    [Pg.173]    [Pg.174]    [Pg.174]    [Pg.175]    [Pg.175]    [Pg.183]    [Pg.180]    [Pg.271]   


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