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#aquatic productivity

2 public questions tagged with this topic.

Where is photosynthetic activity highest in lakes?

The littoral zone is the shallow lake margin where sunlight reaches the bottom, allowing rooted macrophytes, attached algae, and phytoplankton to photosynthesize. Plants occupy both the sediment and water column, creating a large photosynthetic surface and structurally complex habitat. Nutrients arrive from shoreline soils, runoff, decomposing vegetation, and sediment recycling, while wave action and animal activity can return them to the water. Consequently, areal primary production is often especially high in the littoral region. The profundal zone lies below effective light penetration and is dominated by respiration and decomposition. The aphotic zone likewise lacks enough light for net photosynthesis. “Benthic” means the bottom habitat at any depth; a sunlit littoral bottom can be productive, but deep benthic sediment cannot be treated as uniformly photosynthetic. In large lakes, the open-water limnetic zone may contribute more total production because of its area, so “highest” depends on scale. Among the listed zones, however, littoral water best combines abundant light, rooted vegetation, periphyton, and nutrient access, explaining the keyed choice.

Ref: Ecology: Concepts and Applications, Molles, 9th Ed., Ch. 2-3

What nutrient often limits productivity in aquatic systems?

Phosphorus frequently limits primary productivity in freshwater because photosynthetic organisms require phosphate for ATP, nucleic acids, phospholipids, and many metabolic reactions, yet biologically available phosphate is often scarce. Unlike carbon and nitrogen, phosphorus has no large gaseous reservoir that rapidly replenishes most ecosystems. It enters lakes mainly through rock weathering, soil erosion, sewage, detergents, and fertilizer runoff, and it can become adsorbed to sediments or precipitated with minerals. When the supply of phosphate is below biological demand, adding more light or another nutrient produces little growth, whereas adding phosphorus can stimulate phytoplankton and aquatic plants. Excess input may therefore initiate eutrophication, algal blooms, decomposition, and oxygen depletion. The wording “aquatic systems” is broad: nitrogen often limits marine production, and nitrogen-phosphorus co-limitation is common. Nevertheless, among the substances listed, phosphorus is the standard limiting nutrient emphasized for many lakes and other fresh waters; potassium and sulfur are rarely the principal controls, while inorganic carbon is usually replenished through dissolved carbon and atmospheric exchange.

Ref: Ecology: Concepts and Applications, Molles, 9th Ed., Ch. 2-3