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Soil and Water Science Dep., P.O. Box 110510, Univ. of Florida, Institute of Food and Agric. Science, Gainesville, FL 32611.
* Corresponding author.
ABSTRACT
Field and laboratory experiments were conducted to measure forms, storages, and flux of C in the water-sediment colunm of a shallow, subtropical, hypereutrophic lake. High gross primary productivity in the lake (1.4 ± 0.3 kg C m–2 yr–1) was not significantly correlated with any water chemistry parameters measured. This suggested that the phytoplankton community was functioning at maximum levels and under nutrient nonlimiting conditions. Major C input to the lake is through gross primary productivity, of which 90% is lost through heterotrophic and microbial respiration processes within the water column. Resuspension of the bottom sediments was a major input of C into the water column, contributing 720 g C m–2 yr–1. In comparison, diffusive flux of dissolved organic C from the sediment was minimal (1.2 g C m–2 yr–1), as were external inputs into the water column (20 g C m–2 yr–1). High productivity of this system has resulted in a net accumulation of C (as sediments) of 118 g C m–2 yr–1.
Contribution of the Florida Agric. Exp. Stn. Journal Ser. no. R-03291.
Received for publication August 16, 1993.
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