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Patterns in Aquatic Ecosystems Shallow vs Deep Fresh vs Salt Swift vs Stagnant Changing vs Constant Ephemeral vs Permanent Limnology vs Oceanography
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Patterns of Aquatic Ecosystems Important Properties of Water Types of Organisms Freshwater Ecosystems Marine Ecosystems Transition Areas
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Important Properties of Water High specific heat –Warms and cools slowly –Large amount of heat necessary to raise temperature Reaches max density at 4 o C –Ice floats –Warm water above cold water
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Properties of Water 800x more dense than air –Organisms still more dense –Need buoyancy
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Properties of Water More viscous than air –More energy to move through water –Leads to streamlined shapes
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Properties of water… Light attenuates quickly –Photosynthesis only in shallow waters
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Properties of Water Phosphorus and Nitrogen limiting nutrients Less oxygen than air –Enters at surface and via photosynthesis –Cold water holds more Carbon dioxide and buffering
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Properties of Water High surface tension –Can have organisms on surface
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Types of Organisms Can classify based on mode of life/location Can classify based on trophic mode
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Mode of life Benthos - attached or resting on bottom –Epifauna: live on bottom (crabs, scallops) –Periphyton: attach to stems & leaves of rooted plants –Infauna: buried in sediment (clams, worms)
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Mode of life Plankton –Floating, weak swimmers Phytoplankton: photosynthesize Zooplankton: herbivores & carnivores
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Mode of life Nekton –Swimming organisms –Go where they want –Fish, squid, frogs, turtles, seals, octopus http://www.berkeley.edu/news/media/releases/20 05/03/images/aculeatus_walk.mov
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Mode of life Neuston –Rest or swim on surface
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Trophic Mode Decomposers –Many insects, bacteria –Break down organic matter –Bacteria, fungi Photsynthesizers (primary producers) –Derive energy from sunlight
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Trophic Mode Deposit feeders –Eat organic material on bottom –Worms, some snails and clams Filter feeders –Remove food from water –Clams, mussels, baleen whales…
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Trophic Mode Grazers –Eat living plant material –Insects, sea urchins.. Carnivores –Eat animals
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Types of Aquatic Ecosystems Freshwater Marine Transitions between land & sea
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Freshwater Ecosystems Lentic –Standing water –Lakes, ponds, bogs Lotic –Running water –Streams, rivers
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Lentic Zonation Limnetic: to depth of light penetration Profundal zone: beyond depth of light penetration –Usually absent in ponds
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Lentic Zones Littoral zone –Shallow, light penetrates to bottom –Rooted plants –High diversity –Subzones of vegetation Emergent, floating, submergent
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Lentic Zonation Limnetic zone –Depth of effective light penetration - compensation point –No benthos and few if any neuston
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Lentic Zonation Profundal zone –Bottom and deep water region –Fewer plankton and no neuston –Absent in ponds
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Physical Factors Transparency –Turbidity –Secchi Disk Alkalinity (buffering capacity)
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Thermal Stratification Epilimnion: warm surface water Metalimnion: 0 C changes with depth Hypolimnion: cold deeper waters Changes with season
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Thermal Stratification
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Seasonal Changes
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Stratification Temperate lakes - mixed twice/year –Brings oxygen to bottom, nutrients to top Tropical lakes –Low elevation: Warm water on top, doesn’t cool regularly Poor to no mixing –High elevation Can stratify and mix daily
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Lake Productivity Oligotrophic –Deep, sandy or gravel bottom –Low nutrients –low plant growth low productivity –Low decomp at bottom oxygen not depleted
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Lake Productivity Eutrophic –Shallow, muddy, nutrient rich –High plant growth high productivity –Summer stratifies no mixing –Decomposition depletes O 2
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Oligotrophic vs Eutrophic
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Oligotrophic vs. Eutrophic
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Times of Low Oxygen Interesting Dimictic vs. Meromictic lakes Hypolimnion in the summer when no oxygen input –Productive lakes –Deep water fishery disappears Heavy Snow Cover –No algal photosynthesis
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Dystrophic Kettlehole bog
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