In an effort to identify the key mechanisms controlling biological productivity and food web structure in the Chesapeake Bay estuarine turbidity maximum (ETM), we measured plankton community metabolism on a series of surveys in the upper Chesapeake Bay during the winter and spring of 2007 and 2008. Measured quantities included primary production, bacterial production, planktonic community respiration, and algal pigment concentrations. These measurements revealed a classic minimum in photosynthesis in the vicinity of the ETM. Temporal variability in plankton community metabolism, primary production, respiration, and bacterial production were highest in the southern oligohaline region down-estuary of the ETM and appeared to be driven by dynamic bio-physical interactions. Elevated primary production and community respiration in this region were often associated with the presence of mixotrophic dinoflagellates. The dinoflagellate contribution to primary production and respiration appeared to be particularly large as a result of their mixotrophic capabilities, which allow them to obtain energy both autotrophically and heterotrophically. The present study suggests that mixotrophic dinoflagellates play a key role in the pelagic food web in the oligohaline region of Chesapeake Bay, supplying most of the labile organic matter during late winter and spring and also providing a vector for transferring microbial production to mesozooplankton.
KEY WORDS: Estuarine turbidity maximum · Plankton community metabolism · Mixotrophic dinoflagellate · Estuarine food web · Chesapeake Bay
Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 449: 65-82, 2012 66 aquatic sources. Estimating the quantity and quality of this organic matter is difficult due to the diverse origins and complex biogeochemical reactions that occur between dissolved and particulate organic matter and living organisms (Simon et al. 2002). In lakes, stable isotope analysis of organic carbon indicates that a greater fraction of heterotrophic metabolism is fueled by terrestrial organic matter than by autochthonous primary producers when environmental conditions limit autotrophic production (Carpenter et al. 2005, Pace et al. 2007). In Chesapeake Bay, primary production and chlorophyll a (chl a) concentrations are lowest in the oligohaline area (Smith & Kemp 1995), presumably due to light limitation (Fisher et al. 1999), suggesting that, as in lakes, terrestrial organic matter plays an important role in heterotrophic production.Understanding the relative importance of auto chthonous algal production compared to allochthonous input in the ETM is particularly important because this region is an area of high larval recruitment for many fish species including striped bass Morone saxatilis and white perch M. americana (North & Houde 2006). Mesozooplankton such as the calanoid copepods Eurytemora affinis and Acartia tonsa and the freshwater cladoceran Bosmina longirostris are also very abundant (Roman et al. 2001). E...