Abstract

We measured primary production during spring–summer 2006–2007 to determine the carbon supply to the low-salinity pelagic food web of the San Francisco Estuary (SFE). Weekly or biweekly samples were taken at three stations of fixed salinity for size-fractionated primary production and biomass, both as chlorophyll and from biovolume based on counts. Error variance in productivity estimates arose mainly from the depth integration of 14C uptake, showing the importance of productivity measurements at high light levels for estimates of depth-integrated production. Temporal and spatial variability in production were surprisingly small. Combining data from this study with long-term monitoring data, productivity and biomass were variable in time and salinity but without persistent patterns and with infrequent blooms. Production within the low-salinity zone was unresponsive to variation in freshwater flow, in contrast to findings in other estuaries where nutrient loading drives variability in production and other regions of the SFE where production responds to residence time or to stratification. Estimated annual primary production was only 25 and 31 g C m−2 year−1 during 2006 and 2007, only half of it in cells >5 μm. These results imply that phytoplankton provided poor food web support for higher trophic levels, probably contributing to the long-term decline in fish abundance in the brackish to freshwater region of the estuary.

Highlights

  • We measured primary production during spring– summer 2006–2007 to determine the carbon supply to the low-salinity pelagic food web of the San Francisco Estuary (SFE)

  • Phytoplankton primary production is a key driver of the productivity and dynamics of estuarine food webs

  • We present the results of primary productivity measurements made in the low-salinity zone (LSZ) of the San Francisco Estuary during spring and summer of 2006 and 2007

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Summary

Introduction

We measured primary production during spring– summer 2006–2007 to determine the carbon supply to the low-salinity pelagic food web of the San Francisco Estuary (SFE). Estimated annual primary production was only 25 and 31 gC m−2 year−1 during 2006 and 2007, only half of it in cells >5 μm These results imply that phytoplankton provided poor food web support for higher trophic levels, probably contributing to the long-term decline in fish abundance in the brackish to freshwater region of the estuary. Primary production where light is limiting has been estimated from relationships with chlorophyll concentration, incident photosynthetically active radiation (PAR), and extinction coefficient (Cole and Cloern 1984; Jassby et al 2002). These relationships are useful for estimating primary production only if the underlying physiological parameters of the phytoplankton do not change. In addition to error in measuring 14C uptake, there are errors in estimating time-integrated PAR and extinction coefficient (for the more common simulated in situ incubations) and in the mathematical models used to integrate data from individual measurements of 14C uptake at a limited number of light levels

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