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Turbidity Maximum Entrapment of Phytoplankton in the Chesapeake Bay

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Abstract

Estuarine turbidity maxima (ETM) play an important role in zooplankton and larval fish productivity in many estuaries. Yet in many of these systems, little is known about the food web that supports this secondary production. To see if phytoplankton have the potential to be a component of the ETM food web in the Chesapeake Bay estuary a series of cruises were carried out to determine the biomass distribution and floral composition of phytoplankton in and around the ETM during the winter and spring using fluorometry, high-performance liquid chromatography (HPLC), and microscopy. Two distinct phytoplankton communities were observed along the salinity gradient. In lower salinity waters, biomass was low and the community was composed mostly of diatoms, while in more saline waters biomass was high and the community was composed mostly of mixotrophic dinoflagellates, which were often concentrated in a thin layer below the pycnocline. Phytoplankton biomass was always low in the ETM, but high concentrations of phytoplankton pigment degradation products and cellular remains were often observed suggesting that this was an area of high phytoplankton mortality and/or an area where phytoplankton derived particulate organic matter was being trapped. These results, along with a box model analysis, suggest that under certain hydrodynamic conditions phytoplankton derived organic matter can be trapped in ETM and potentially play a role in fueling secondary production.

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Acknowledgements

We thank the captain and crew of the R/V Hugh R. Sharp for their assistance on eight research cruises to the Chesapeake Bay ETM. We also thank everyone involved in the BITMAXII project for helpful discussions and their assistance collecting water samples on these cruises. Finally, we also thank Anne Thessen for doing the microscopic identification of phytoplankton in preserved samples, Larry Sanford and Y. Kim for allowing us to collect water samples during their DIPSTIC settling tube experiments, and Anne Gustafson for providing guidance on fluorometric chlorophyll analysis methods. This research was supported by the National Science Foundation (Grant OCE-0453905) and it represents UMCES contribution no. 4783.

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Table S1

Box model volume calculation data. The total volume of each box is the sum of the corresponding volume data compiled by Cronin and Pritchard (1975). The volumes of the surface and bottom portions of boxes 2 and 3 were computed from the volume data, which reported in 1 nautical mile by 1 m segments, and based on the average pycnocline depth (~7m) during the transects (i.e. for each Cheasapeake Bay segment the surface portion was the volume of the upper 7 m and the bottom portion was from 8 m to the bottom). (PDF 60 kb)

Figure S1

Contour plots of salinity (white dashed lines), turbidity, and the concentration of chlorophyll a, selected accessory pigments, and chlorophyll degradation products along the main channel of the upper Chesapeake Bay on Feb 23, 2007. CTD survey and water sampling station locations are indicated by the open circles. (PDF 391 kb)

Figure S2

Contour plots of salinity (white dashed lines), turbidity, and the concentration of chlorophyll a, selected accessory pigments, and chlorophyll degradation products along the main channel of the upper Chesapeake Bay on May 8, 2007. CTD survey and water sampling station locations are indicated by the open circles. (PDF 529 kb)

Figure S3

Contour plots of salinity (white dashed lines), turbidity, and the concentration of chlorophyll a, selected accessory pigments, and chlorophyll degradation products along the main channel of the upper Chesapeake Bay on January 26, 2008. CTD survey and water sampling station locations are indicated by the open circles. (PDF 546 kb)

Figure S4

Contour plots of salinity (white dashed lines), turbidity, and the concentration of chlorophyll a, selected accessory pigments, and chlorophyll degradation products along the main channel of the upper Chesapeake Bay on April 23, 2008. CTD survey and water sampling station locations are indicated by the open circles. (PDF 552 kb)

Figure S5

Box model sensitivity analysis results for Box 2 (bottom) Chl a flux sensitivity to variations in the sinking factor (X 2 ). Fluxes were calculated for each modeled transect with sinking factor intervals of 0.01 (i.e., 0.50, 0.51, 0.52, etc.). (PDF 68 kb)

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Keller, D.P., Lee, D.Y. & Hood, R.R. Turbidity Maximum Entrapment of Phytoplankton in the Chesapeake Bay. Estuaries and Coasts 37, 279–298 (2014). https://doi.org/10.1007/s12237-013-9692-2

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