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The influence of nutrient enrichment on the specific growth rates of bacterioplankton in oligotrophic lake water batch cultures was determined. The specific growth rates (SGRs) were calculated based on the changes in biovolumes and bacterial populations. Results showed that addition of inorganic phosphorus significantly increased SGRs while addition of organic carbon alone did not. This observation which is significant in the lake areas with high phosphatase activity implied a direct competition for inorganic phosphorus between bacterioplankton and phytoplankton.

Bachmann et al. (1999) postulated that wind energy initiated, and has maintained, high turbidity in hypertrophic (mean chlorophyll a = 92Mug l-1) Lake Apopka, Florida (mean depth = 1.6 m; area =12 500 ha). They asserted that the turbid condition was initiated bya hurricane in late 1947 that destroyed submersed plant beds and that high turbidity has since been maintained by wind-driven resuspension of fluid sediments. In their view, there has been sufficient light for re-establishment of submersed plants over about 38% of the lake bottom, but plant growth has been precluded by the fluid character of the sediments. They concluded that the restoration program of the St.Johns River Water Management District, which includes reduction of the phosphorus (P) loading rate, will not restore water clarity or submersed vegetation. An alternative explanation for Lake Apopka's turbid state is that it was initiated, and has been maintained, by excessive P loading that led to algal blooms and elimination of submersed vegetation through light limitation. The transition to the turbid statewas contemporaneous with drainage of 7300 ha of the floodplain wetland to create polders for farming, beginning in the early 1940s. Lake P budgets indicate that drainage of the farms caused a seven-fold increase in the P loading rate (0.08 g TP m-2 yr-1to 0.55 g TP m-2 yr-1). Paleolimnological analysis of lake sediments also indicates an increase in the P loading rate in mid-century, concomitant with the decline in submersed vegetation and the increase in phytoplankton abundance. After the increase inP loading, wind disturbance may have accelerated the transition to the turbid state; but, before the increase in P loading, wind disturbance was insufficient to elicit the turbid state, as evidenced by the stability of the clear-water state in the face of 14 hurricanes and 41 tropical storms fro m 1881 to 1946. Measurements of photosynthetically act [ABSTRACT FROM AUTHOR]