Progressive decoupling between phytoplankton growth and microzooplankton grazing during an iron induced phytoplankton bloom in the Southern Ocean (EIFEX)

• Published in: Marine Ecology Progress Series
• Main Authors: Latasa, M., Henjes, J., Scharek, R., Assmy, P., Roettgers, R., Smetacek, V.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Inter-Research 2014
• Subjects: info:eu-repo/classification/ddc/551; Southern Ocean
• Online Access: https://publications.hereon.de/id/32193; https://publications.hzg.de/id/32193

Dilution experiments were performed to quantify growth and mortality rates of phytoplankton groups (as defined by pigment markers) for 5 weeks in a Fe-induced phytoplankton bloom during the European Iron Fertilization Experiment (EIFEX) conducted in the Southern Ocean. Rates could be reliably measured for the 2 main groups, diatoms and prymnesiophytes. Mean phytoplankton intrinsic growth rates were around 0.23 d–1, without a significant temporal trend. Mortality rates, however, decreased with time (from ~0.3 to ~0.06 d–1), leading to an increasing decoupling between phytoplankton growth and microzooplankton grazing. The decrease in grazing was correlated with the decrease of concentrations of small microprotozooplankton (<60 µm). As a consequence, net growth in the dilution experiments increased from values around 0 d–1 up to 0.13 d–1 measured in the last days of the experiment, 35 days after the initial Fe fertilization. This pattern did not reflect the dynamics of net phytoplankton accumulation in the fertilized patch which increased until Days 24 to 27 and decreased thereafter. The difference between experimental and natural phytoplankton net growth is the biomass that escapes microzooplankton grazing and does not accumulate in the surface mixed layer, i.e. the biomass that went to higher trophic levels plus that exported out of the mixed layer. It increased throughout EIFEX, and suggests a shift from a predominantly recycling system towards a more exporting one.