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Temperature effects on the heterotrophic bacteria, heterotrophic ...

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108<br />

Aquat Microb Ecol 67: 107–121, 2012<br />

Oligotrophic plankt<strong>on</strong>ic ecosystems are resp<strong>on</strong>sible<br />

for nearly 22% of net primary producti<strong>on</strong> in <strong>the</strong><br />

oceans (Field et al. 1998). Their carb<strong>on</strong> biomass is<br />

dominated by plankt<strong>on</strong>ic microbes (Gasol et al. 1997),<br />

and >40% of <strong>the</strong>ir sec<strong>on</strong>dary <strong>bacteria</strong>l producti<strong>on</strong> is<br />

c<strong>on</strong>sumed by protists (Vázquez-Domínguez et al.<br />

2005). In <strong>the</strong>se ecosystems, nano flagellates are often<br />

top-down c<strong>on</strong>trolled by microzooplankt<strong>on</strong>, such as<br />

ciliates and dinoflagellates (Hansen 1991, Verity<br />

1991), which are more important than mesozooplankt<strong>on</strong><br />

as c<strong>on</strong>sumers of <strong>the</strong> lower trophic levels<br />

(Calbet & Landry 2004). In oligotrophic c<strong>on</strong>diti<strong>on</strong>s,<br />

<strong>the</strong> growth efficiencies of <strong>heterotrophic</strong> <strong>bacteria</strong> and<br />

protists are

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