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Lakes (& Ponds) Lake (& Pond) – body of water in one basin with realtively little flow. Limnology = study of lake ecology. Lentic system = more “still” (fresh)water system; Lacustrine = of/around lake/pond; limno = lake Lake Zones Euphotic zone = where light can support photosynthesis. Littoral zone = where attached macrophytes and periphyton can grow (euphotic periphery). Limnetic zone=“Open water” no macrophytes. Lake Strata (Layers) Epilimnion = warm upper layer in a lake. Much sunlight; affected by wave energy; lower nutrients; high dO2 Hypolimnion = cool lower layer in a lake. Little sunlight; little affected by waves; higher nnutrients; high or low/no dO2 Thermocline (Metalimnion) Epilimnion Hypolimnion Lake Turnover Stratification = thermal layering with a distinct epi- & hypolimnion Temperate lakes may “mix” in the fall & spring (turnover) = destratification. Wind can keep deep lakes from stratifying. surface warms surface cools Lake Turnover Turnover ensures hypolimnion oxygenation and increases nutrients in epilimnion. Permanently stratified lakes (e.g., deep tropical) may have anoxic hypolimnions; also can build up H2S in hypolimnion. Turnover in “permanently” stratified lakes can lead to “fish kills” or eutrophication. Fetch Fetch = the distance over which winds blow over a lake. Greater fetch = more/larger waves and more mixing; less likely to be stratified wind direction Lake Primary Production Emergent Macrophytes = Littoral; mostly flowering plants (Submerged) Macrophytes = Littoral; mostly flowering plants and green algae Periphyton = Littoral; mostly green algae, diatoms, and cyanobacteria Phytoplankton = Limnetic and Littoral; mostly green algae, diatoms, and cyanobacteria limnetic phytoplankton littoral submerged macrophytes littoral emergent macrophytes Allochthonous Inputs In most lakes some nutrients come from surrounding terrestrial environments and tributary streams. Given low flows most particulate organic matter (POM) sinks in lakes/ponds. Many lakes with substantial allochthonous inputs have macroinvertebrate shredders and collectors, like in streams (but usually different species). Littoral Zone Food Web runoff or groundwater entry leaf litter periphyton & macrophytes conditioning (microbial colonization) bacteria coarse particulate & fungi organic matter (CPOM) grazing grazing fishes insects & crustaceans shredding dissolved organic compounds (DOC) fine particulate organic matter (FPOM) insects & crustaceans collecting “predatory” fishes predatory insects & crustaceans insects, crust., nematodes, & annelids bacteria & fungi Limnetic & Euphotic Food Web phytoplankton phytobacteria microzooplankton phytoplanktivorous grazing zooplankton fishes predatory zooplankton “predatory” fishes dissolved organic compounds (DOC) bacteria Lake Grazing Zooplankton Cladocerans Copepods Cladocerans (Daphnia) Copepods Lake Predatory Zooplankton Cladocerans Insect Larvae (midge larvae) Ghost Midge Larva (Chaoborous) Cladocerans (Leptodora & Polyphemus) Insect Larvae and Decapods Insect Larvae = Many insect larvae are aquatic, esp. common in littoral. dragonflies, damselflies, mayflies, black flies, mosquitoes, horse flies. Crustaceans = crayfishes (in North America). “Lake Fishes” North Amercan Fishes 979 native freshwater species 82 exotic species 50 taxonomic families Arbitrarily divided into coolwater and warmwater ichthyofauna. Coolwater – water never warmer than 22°C Warmwater – water gets above 22°C Broad Lake Categories Oligotrophic Lakes = deep, cool, nutrient poor lakes. Usually stratified. Mountain lakes Eutrophic Lakes = shallow, warm, nutrient rich lakes. Often not stratified. Shallow Ponds Oligotrophic-Eutrophic continuum. Cultural Eutrophicaltion – anthropogenic nutrient (P & N) input; can cause anoxia Broad Lake Categories eutrophic oligotrophic Cultural Eutrophication Macrophyte vs. Algal Systems “Macrophyte systems” – Macrophytes and cladocerans more common. Cladocerans graze algae and macrophytes retain nutrients in tissues. Lower free nutrients in water. Water clear. “Algal systems” – Algae more common. Nutrients rapidly cycled through algae. Higher free nutrients in water. Water turbid. Nutrient increase, removal of macrophytes, or increase in planktiovorous fish can shift from a macrophyte to an algal system. North American Great Lakes “Gouged” out by glaciers. Experienced many introduced species. S. Great lakes experienced much pollution. Aral “Sea” Freshwater Lake. Its water input was diverted by the Soviets to irrigate parts of Kazakstan. As an arid environment water levels fell and salinity increased tremendously. Aral “Sea” Differences in Tropical Lakes Bacterial and fungal decomposition of allochthonous material is more rapid. Fewer aquatic insects. Fishes (and in some places decapod crustaceans) serve as the major shredders, collectors, and grazers. If deep, may be permanently stratified. Lake Victoria Many native cichlid (fish) species (300+). First some cultural eutrophicaltion then intro. of Nile perch (Lates nilotica) around 1960. Only <100 cichlid species still extant.