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An overview of wetlands and aquatic ecosystems, including their classification, characteristics, and services they offer to humans. It covers different types of wetlands such as swamps, marshes, bogs, fens, and mangroves, and discusses their fauna. The document also explains the importance of aquatic ecosystems, which cover 71% of the earth's surface, and their classification into freshwater, marine, and brackish water. It further discusses the importance of freshwater ecosystems, including lakes, and their stratification, as well as the concept of life zones in lakes.
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In between fully aquatic and fully terrestrial ecosystems
Standing water for at least part of the year
Vegetation adapted to growing with submerged roots
Classified by vegetation type: Swamps – woody plants and shrubs Marshes – reeds, rushes, other grasses Bogs – sphagnum moss Fens – sedges, rushes Mangroves
Perform services useful to humans
Purify water by trapping sediments and breaking down toxic wastes and chemicals that run off agricultural land
Serve as reservoirs that reduce the risk of flooding
Water covers 71% of the Earth’s surface
Only 1% of water is freshwater
Only 0.3% of freshwater is available on the Earth’s surface, the rest is locked in glaciers, polar ice and underground aquifers
Include:
Standing water (ponds and lakes) Flowing water (streams and rivers)
Oligotrophic lake
Eutrophic lake
In temperate zones, deep lakes are stratified in summer Epilimnion – Surface layer, warm from solar radiation, least dense Thermocline – Thin middle layer Hypolimnion – Lower layer, cold, most dense
Layers do not usually mix; less dense water floats on top of more dense water
In winter, ice forms on the surface, maintaining a uniform temperature
Overturn is repeated again in spring as the ice melts
Lakes can be stratified into different life zones according to: Amount of sunlight penetration Nutrient levels Temperature Amount of dissolved oxygen
Bodies of water that move continuously in one direction
May originate from springs, runoffs from melting snow or ice, or outlets of lakes
Structure changes from their point of origin ( headwaters ) to where they empty into a larger body of water ( mouth )
Headwaters:
Water is clear Little sediment Few nutrients Channel is narrow Rocky substrate Water flows swiftly
Partially enclosed body of water where freshwater and seawater mix
River meets the ocean
Salinity varies greatly
Highly productive due to nutrients brought in by rivers
High biodiversity
These organisms must be able to adapt to changing salinity
Estimated over half of all marine fishes require development in estuaries