wetlands 2014
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GEOLOGY,
HYDROLOGY AND FW
HABITATS (CH. 4)Introductory Comments
Continuity of FW Habitats
How are FW habitats defined?
Geology (geomorphology)
Water movement through the environment
hydrologic cycle
How that movement varies spatially and
temporally hydrodynamics
Links between terrestrial and aquatic
environments and between different aquatic
ecosystems
FIGURE 4.2
The Hydrologic Cycle
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WETLANDS (CH. 5)
Interfaces between Terrestrialand Aquatic Ecosystems
Defining Wetlands Synonyms: swamps, bogs, marshes, potholesetc.
Ecotone transitional habitat; terrestrial andaquatic species
Can contribute to high biodiversity
Key defining features:
Shallow water or saturated soil (hydric)
Distinct plant life hydrophytes; emergentmacrophytes and trees; floating vegetation
Organically-rich soil that differs from surroundinguplands
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Global Distribution of Wetlands
Climate and geomorphology
Wetlands are more prevalent in cool and wet
climates than in hot and dry Cool climates less loss to evapotranspiration
Wet climates excess precipitation
Steep terrains have fewer wetlands than flat,gently-sloping landscapes
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Most Endangered Aquatic Habitat
70% of U.S. riparian wetlands lost
50% of prairie potholes gone
Half of Everglades drained
22 states have lost more than half of theirwetlands in the last 200 years
Kansas: only 48% remain
Wetlands lost in other countries: Cameroon(80%), New Zealand (90%), Australia (95%),Thailand (96%), Vietnam (>99%)
No Net-Loss Policy attempt at mitigation
The Reclamationof the MississippiDelta
What are some Services provided by
Wetlands?
Critical components to watersheds
Recharging water supplies
Stabilize shorelines, retaining sediment andreducing erosion
Water filtration purifies water, chemical sink
Carbon sinks 400-500 Gt
Flood control slows run-off; water storage
Maintain biodiversity larger the better
Consumer goods
Recreation
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Coastal Wetlands
Mangroves (subtropical totropical)
Halophytic mangrove trees Low wave action and high
sedimentation rates
Anoxic sediments; many species have
pneumatophores
Above and below the water habitats diverse
assemblage of invertebrates and vertebrates
Export lots of production to open waters as detritus
Inland Wetlands
Marshes; swamps; riverine or riparian wetlands;peatlands
Riverine, fringe and depressionalgeomorphologies
U.S. Marshesdominated by emergentvegetation whereas swampsby trees
Inland marshes and swamps most extensivetype of wetland worldwide
Freshwater Marsh (worldwide)
Diverse wetlands; grasses, sedges and otheremergent hydrophytes; floating plants
Very productive and diverse
Prairie potholes; Everglades; Great Lakes
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Riparian/Riverine Wetlands (worldwide)
Wetlands along rivers; floodplains of large rivers
Range from seasonal to permanent inundation
Exchange of nutrients and energy betweenfloodplain and river channel
Inundated floodplains as nursery grounds
Peatland (Northern Wetlands)
Cool temps low rates of decomposition
Accumulation of decaying organic matter
Bogs little or no water flow; precipitation only
Acidic soils predominance of Sphagnummoss
Fens inputs from runoff and groundwater
Support a wider range of plant species
Holds 1/3 of soil carbon Where is most of thewarming taking place?
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Wetland Hydrology: Master Variable
Water depth, flow patterns, duration andfrequency of flooding and flushing
Influence biochemistry of water and soils Ultimate selection of wetland biota
Water sources and hydrodynamics
Precipitation standing water; low water
movement; subject to anoxia
Surface water episodic flooding and flushing;
extended periods of standing water
Groundwater constant flow and flushing
Hydrology and Nutrient Input
Wetlands range from eutrophic to oligotrophic
Surface-water sourced floodplain andlandscape inputs diverse plant communities
Groundwater-sourced constant input of flowand nutrients stable communities
Precipitation-sourced little nutrient input; lowproductivity and diversity
Together with variation in salinity, pH and otherchemical parameters strong determinant of
plant community
Okavango Delta