abundance and production directly correlate to those of phytoplankton during the winter, spring, and summer. Ciliate predation on flagellates is a major regulatory mechanism, particularly during summer and among more productive lakes. The rapid generation rates of protists belie the modest instantaneous biomass of their communities. Flagellate growth rates are much greater than those of ciliates. In addition, flagellate densities are greater by a factor of approximately 1000 in comparison with ciliates (Wetzel 2001). As a result, heterotrophic flagellate production equals or exceeds that of ciliates in both planktonic and benthic habitats. The “microbial loop,” a model of pathways of organic carbon and nutrient cycling through the microbial communities, indicates many direct links among algae, bacteria, and heterotrophic protists. Protistan bacterivores can function largely as decomposers and efficient nutrient remineralizers. Some of the fixed organic carbon can be converted into larger microorganisms that may be consumed by larger metazoans and zooplankton. Under many conditions, however, the microbial loop functions as both a carbon and nutrient sink by which organic matter is respired. This appreciable organic matter is not directly available to higher animals and the nutrients are recycled without ever entering a metazoan gut. The bottom line is that in addition to their significant contributions to biodiversity, the protists are major decomposers and mediators of nutrient recycling in ecosystems. It is apparent that more than 90% of organic carbon mineralization and nutrient recycling is effected by microorganisms under 100 µm in size, largely protists. Yet less than 10% of our exploration of heterotrophic metabolism and regulation of material and energy fluxes has focused in this area. What a fantastic opportunity for young biologists to make significant contributions to our understanding of the operation of ecosystems! Were I starting over, I would devote my career to this area, to help fill one of the most important voids in contemporary understanding of the biosphere.
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