The importance of microzooplankton versus phytoplankton to copepod populations during late winter and early spring in Lake Michigan
Marie H. Bundy, Henry A. Vanderploeg, Peter J. Lavrentyev, Paul A Kovalcik
Abstract
Marie H. Bundy, Henry A. Vanderploeg, Peter J. Lavrentyev, Paul A Kovalcik
Abstract
Feeding rates of the calanoid copepod Leptodiaptomus sicilis on natural assemblages of phytoplankton and microzooplankton were evaluated during late winter and early spring in Lake Michigan. Microzooplankton were the preferred food source for this copepod, and larger size fractions of phytoplankton were preferred to smaller size fractions. Ingestion rates of total chlorophyll a ranged from 2 to 14 ng·copepod1·day1, while ingestion rates of micro zoo plank ton biomass ranged from 0.04 to 0.15 µg C·copepod1·day1. In these experiments, microzooplankton carbon accounted for 22%74% of the total carbon ingested. Clearance rates of microzooplankton carbon were positively related to the larger size fractions of chlorophyll a and to total suspended solids. Measured ingestion rates of microzooplankton and phyto plankton carbon suggest that calanoid copepod populations have the potential to control microzooplankton production in late winter and early spring, and even with an abundance of phytoplankton carbon, food availability may limit the reproduction of L. sicilis. Because microzooplankton contribute significantly to the diet of these copepods, stimulation of the microbial food web by terrigenous inputs of nutrients and carbon may be transmitted to higher trophic levels (i.e., mesozooplankton and their predators) through heterotrophic flagellates and protozoans.
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Feeding rates of the calanoid copepod Leptodiaptomus sicilis on natural assemblages of phytoplankton and microzooplankton were evaluated during late winter and early spring in Lake Michigan. Microzooplankton were the preferred food source for this copepod, and larger size fractions of phytoplankton were preferred to smaller size fractions. Ingestion rates of total chlorophyll a ranged from 2 to 14 ng·copepod1·day1, while ingestion rates of micro zoo plank ton biomass ranged from 0.04 to 0.15 µg C·copepod1·day1. In these experiments, microzooplankton carbon accounted for 22%74% of the total carbon ingested. Clearance rates of microzooplankton carbon were positively related to the larger size fractions of chlorophyll a and to total suspended solids. Measured ingestion rates of microzooplankton and phyto plankton carbon suggest that calanoid copepod populations have the potential to control microzooplankton production in late winter and early spring, and even with an abundance of phytoplankton carbon, food availability may limit the reproduction of L. sicilis. Because microzooplankton contribute significantly to the diet of these copepods, stimulation of the microbial food web by terrigenous inputs of nutrients and carbon may be transmitted to higher trophic levels (i.e., mesozooplankton and their predators) through heterotrophic flagellates and protozoans.
Key concepts: Copepod, Phytoplankton, Plankton, Zooplankton, Biomass (ecology), Trophic level, Biology, Chlorophyll a