Abstract Photosynthetically-mediated calcite precipitation by phytoplankton and charophytes has been shown to be a significant pathway for the removal of epilimnetic Ca and P in hardwater lakes, but the role… Click to show full abstract
Abstract Photosynthetically-mediated calcite precipitation by phytoplankton and charophytes has been shown to be a significant pathway for the removal of epilimnetic Ca and P in hardwater lakes, but the role of submersed aquatic vascular plants has not been examined. We measured calcite precipitation on 5 species of submersed aquatic vascular plants in moderately hardwater Lake Pleasant semi-monthly during the growing season. Maximum mass-specific accumulation ranged from 22.9 mg Ca g −1 leaf dry weight in Megalodonta Beckii to 176.3 mg Ca g −1 leaf dry weight in Potamogeton Richardsonii . Analysis of the crude deposits gave mean Ca concentration of 318 mg g −1 dry wt., and mean total P concentration of 169.8 μg g −1 dry wt, however, only 38% of this total phosphorus was composed of chemical species specifically associated with Ca co-precipitation. We used whole-lake estimates of submersed aquatic vascular plant mass to calculate the mass of P co-precipitated with Ca. Results suggest that in spite of conspicuous precipitate on plants during midsummer in this lake, there is a negligible effect on epilimnetic P concentrations.
               
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