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For much of the year P. rubescens resides near the metalimnion, that transition area between the warm epilimnion and the colder hypolimnion (see Lake Stratification in this issue). P. rubescens blooms are frequently reported in fall when lake temperatures cool and the water column starts mixing deeper. This change in lake thermal structure doesn’t necessarily promote the bloom of P. rubescens, but rather moves the bloom from the metalimnion to the surface. The colorful algae become apparent once this metalimnion has mixed with the cooling surface layer of the lake. Like many blue-greens, P. rubescens is capable of regulating its buoyancy, effectively moving itself up and down within the water column. When high in the water column they receive enough light to photosynthesize. During photosynthesis, they produce dense carbohydrates that eventually weigh the cells down, causing them to sink. Once in deeper water (sometimes the hypolimnion) where there isn’t enough light to photosynthesize, P. rubescens will respire, using the carbohydrates for energy, thus lightening their load. A by-product of their respiration is the expansion of their “gas vacuoles”. Eventually, with enough respiration, the gas vacuoles increase buoyancy enough to lift the algal cell back up in the water column.
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