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Trophic Transition in a Lake on the Virginia Coastal Plain

Mellisa A. Pensa* and Randolph M. Chambers

Department of Biology, College of William and Mary, Williamsburg, VA 23187



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Fig. 1. Outline of the Lake Matoaka watershed in southeastern Virginia, showing the location of five perennial streams (solid lines) and associated subwatersheds (dotted lines). Subwatershed coring stations in the five stream deltas in the lake are shown.

 


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Fig. 2. Median separation plots for HCl-extractable Fe (open circles = 0.03–0.14%, filled circles = 0.15–0.40%) and total P (open circles = 0.02–0.12%, filled circles = 0.13–0.30%) in surface sediments of Lake Matoaka.

 


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Fig. 3. Median separation plots for weight percent organic matter (open circles = 5–13%, filled circles = 14–40%) and biogenic silica (open circles = 0.01–0.10%, filled circles = 0.11–0.25%) in surface sediments of Lake Matoaka.

 


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Fig. 4. Molar C to N ratios in surface sediments of Lake Matoaka. Open circles = C to N ratio of <20, filled circles = C to N ratio of ≥20. One-meter depth contours are shown; depths of >3 m are shaded darker.

 


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Fig. 5. Depth profiles of biogenic silica and total P from delta cores downstream of more-developed Subwatersheds 1 and 2 (solid symbols) and less-developed Subwatersheds 3, 4, and 5 (open symbols).

 





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