School of Engineering and Science - Jacobs University
School of Engineering and Science - Jacobs University
School of Engineering and Science - Jacobs University
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DISCUSSION<br />
Microzooplankton grazers at the base <strong>of</strong> the North Sea food web<br />
“Classic” food chain theories stress the role <strong>of</strong> primary production <strong>of</strong> photosynthetic<br />
phytoplankton grazed by crustacean mesozooplankters (> 200 µm) <strong>and</strong> those consumed<br />
by larger predators such as fish. Towards the end <strong>of</strong> the last century scientific findings<br />
emphasized the role <strong>of</strong> the microbial loop (Azam et al., 1983) as a major biological<br />
force in the ocean (Azam, 1998) <strong>and</strong> the significant importance <strong>of</strong> microzooplankters (<<br />
200 µm) for the consumption <strong>of</strong> primary production. The aim <strong>of</strong> this thesis was to<br />
contribute in elucidating their role as phytoplankton grazers in the planktonic food web<br />
<strong>of</strong> the North Sea (Figure 1).<br />
Heterotrophic din<strong>of</strong>lagellates <strong>and</strong> ciliates are the most important groups within the<br />
microzooplankton (Capriulo et al., 1991) especially in water <strong>of</strong> higher productivity<br />
(Calbet, 2008) <strong>and</strong> from a biomass perspective this was also confirmed in this study.<br />
The monitoring program conducted as an important basis for this thesis (Chapter I)<br />
verified the importance <strong>of</strong> heterotrophic din<strong>of</strong>lagellates <strong>and</strong> ciliates. Summarized they<br />
showed carbon concentrations (652 µgC L -1 ) comparable to results from other studies<br />
(Riegman et al., 1993, Brussaard et al., 1995). During a phytoplankton spring bloom<br />
situation (Chapter III) the biomass <strong>of</strong> heterotrophic din<strong>of</strong>lagellates <strong>and</strong> ciliates made up<br />
around 70-96% <strong>of</strong> the biomass <strong>of</strong> the microzooplankton <strong>and</strong> other studies confirm such<br />
an importance <strong>of</strong> both groups in the North Sea (Brussaard et al., 1995, Stelfox-<br />
Widdicombe et al., 2004). Whereas in my experiment (Chapter III) the phytoplankton<br />
showed a maximum carbon biomass concentration <strong>of</strong> 269 µgC L -1 , the<br />
microzooplankton reached concentrations <strong>of</strong> up to 126 µgC L -1 . At its maximum,<br />
microzooplankton contributed more than 50% to the available carbon <strong>of</strong> the plankton<br />
size fraction > 5µm.<br />
Especially during bloom situations, unicellular microzooplankton can respond quickly<br />
to increased phytoplankton food availability (Johansson et al., 2004, Aberle et al.,<br />
2007). This pattern has also been observed during a mesocosm spring bloom situation<br />
(Chapter III) where the phytoplankton peak (24.03.09) was followed by a<br />
microzooplankton maximum with less than one week delay (30.03.09).<br />
A meta-analysis by Calbet & L<strong>and</strong>ry (2004) showed that microzooplankton grazing<br />
accounts on average for 60% <strong>of</strong> the mortality <strong>of</strong> the daily phytoplankton production in<br />
estuarine <strong>and</strong> coastal environments with chlorophyll a concentrations (3-13 µg L -1 )<br />
comparable to those at Helgol<strong>and</strong> Roads (0.05-28 µg L -1 , Chapter I). The results for the<br />
grazing impact <strong>of</strong> microzooplankton obtained during a typical North Sea spring bloom<br />
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