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BIOL 453
Page history last edited by Anonymous 3 yrs ago
Wetlands
marks
- final 40%
- wetland evaluation 35%
- midterm 25%
- wetland: land saturated during most of the year -> soil poor in oxygen -> supports specialized biotic communities
- canadian def: saturated -> promote wetland/aquatic processes as indicated by poorly-drained soils, hydrophytic vegetation, various biota adapted to wet environment
- 2 broad categories in Canada: 75% organic (peat) soils (>=40cm deep), and 25% mineral soils
- 1/3 of Canada's wetlands are frozen
- Sphagnaceae > Sphagnum
- carnivorous plants only in wetlands
wetland classification
- basin classification
- bedrock eg karst, volcanic, fault
- unconsolidated sediments eg glacial, river-activity, shoreline processes, isostatic uplift, wind-formed, biotic (eg beaver)
- water source classification (-genous = water)
- ombrogenous: mostly from atmosphere
- terrigeneous: mostly from surrounding land (or groundwater)
- soligenous: from surface
- littogenous: from literal (coastal) zone eg marine, riverin, estuarian, ?
- water flow can be vertically (up and down), horizontally both ways, and horizontally in one direction
- geochemical classification
- freshwater
- oligotrophic: low pH, low dissolved minerals
- ombrotrophic: same as oligatrophic but more extreme; input only from atmosphere
- minerotrophic: high pH, high dissolved minerals, neutral and alkaline
- in descending solutes: calcareous, rich, intermediate, poor
- saltwater: inland, sea, salt spray, estuary
- sediment/strata classification
- structure classification
- trees: greater or less than 15m tall
- shrubs: 1.5m and 0.5m classification boundaries
- herbaceous (roots location... (?))
- bryophytes
- floristic classification
canadian classification
- 2 major divisions
- mineral: insignificant organic accumulation, modified by water control structures (?)
- organic (aka peat or peatland): at least 40cm organics
- classification is Class > Form > Type
- classes
- swamp
- peatland/mineral
- water table at/just below surface
- minerotrophic
- soil: highly decomposted woody peat
- trees, tall shrub (thicket) cover
- strong surface and /or groundwater input = minerogenous -> high runoff, ET high (trees) maybe
- bog
- peatland
- water table at or just below surface
- ombrotrophic
- surfaced raised or level with surrounding land
- soil: semi-decomposed sphagnum with woody remains
- trees, shrubs, or treeless
- not well served by streams; ET dominates loss
- fen
- mostly peatland
- water table at or very close to surface
- minerotrophic mostly
- surface level with the water table
- soil: decomposed sedge or brown moss peat
- graminoid, shrub cover
- ET is high (basin shape, plants); runoff high when water above surface, but decreases a lot when water table is low
- marsh
- mineral (mostly)
- shallow surface water which fluctuates
- minerotrophic or eutrophic
- thin organic accumulation
- rushes, reeds, grasses, sedges, with emergent and floating aquatic herbaceous species
- shallow water
- standing/flowing water (<2m deep)
- limnetic, organic material
- floating leaved, submerged aquatic vegetation
- marsh AND shallow water
- high ET, mostly from open water; groundwater recharge could be significant; maybe no runoff
- HGM: hydrogeomorphic, the method used in the US
water stuff
- something about hydroperiods...
- dynamic storage (water volume that changes daily/seasonally) vs static storage (water in soil, doesn't change much annually)
- "flood control": depends on wetland type (relation to water table), runoff can dissipate or *not*
geochem stuff
- anaerobic -> biocem unique to reducint conditions
- although oxygen-rich above
- redox is sorta "oxygen vs hydrogen"
- typical thermodynamic sequence
- oxygen + hydrogen ions + electrons <-> water (uh...?)
- denitrification (disappearance of NO3-)
- creation of manganous Mn2+
- iron reduction -> ferrous Fe2+
- sulphate reduction -> H2S
- methanogenesis -> CH4
old midterm
- /10 - define 5/8 terms (2 marks each = make 2 points each, can draw)
- anoxia
- very low oxygen (okay, need more...)
- hydroperiod
- ? graph of water volume vs time for a particular wetland. looks different for types of wetlands and even individuals of the same type, shows cycles etc.
- swamp (answer copied from above)
- peatland/mineral
- water table at/just below surface
- minerotrophic
- soil: highly decomposted woody peat
- trees, tall shrub (thicket) cover
- string surface and /or groundwater input = minerogenous -> high runoff, ET high (trees) maybe
- ombrotrophic indicator
- ombrotrophic: low pH, low dissolved minerals (extreme); input only from atmosphere; so indicator is... ?
- redox
- hmn, what it really means, or how we learned it? ...
- groundwater discharge
- ombrogeny
- wetland's water comes mostly from the atmosphere (rain, snow, fog), rather than ground or surface water (is that enough for 2pts?)
- marl
- wp CaCO3-rich mud w/ clay
- /6 - 3 points on why wetland science deserves to be a distinct science
- /10 give water budget for 2 contrasting wetland classes (identified, with reasons)
- /10 describe typical thermodynamic reduction sequence for inorganics in wetland (assuming major stuff present)
- answer copied from above
- oxygen + hydrogen ions + electrons <-> water (uh...?)
- denitrification (disappearance of NO3-)
- creation of manganous Mn2+
- iron reduction -> ferrous Fe2+
- sulphate reduction -> H2S
- methanogenesis -> CH4
- /4 what's the point of wetlands classification
- each type has different biota, hydrology, etc. and classification gives us greater knowledge allowing us to treat them as such. for example if endangered species X lives in wetland type Y, we know that we need to preserve Y, as opposed to any particular wetland. so classification is useful for legislation, conservation, construction, research, etc.
- =/40 ?
Adaptations to Anoxia (low O2) Structural - aerenchyma: gas-filled lacunae system, held together with porous aerenchyma
- aerenchyma is 10-12% of root-cross section for flood-intolerant plants, 50-60% of flood-tolerant plants
- forms via cell wall separation, collapse of cells or enlargement of separations
- aerenchyma is proportional to reducing conditions
- it decreases resistance to flow by O2, allows CO2, etc. to escape
- allows gas to be stored (50% of leaf volume in cattails)
- roots
- adventitious roots: new roots that form laterally from main stem within days of flooding
- usually form in O2-rich water and less root biomass needs O2
- done via hormone auxin
- shallow rooting: woody/herbaceous plants have shallower roots than in terrestrial environments
- gives roots access to O2, nitrate
- pneumatophores: modified erect roots that grow up from roots (“knees”)
- height corresponds to maximum height of water
- most O2 used by pneumatophores, little is transported to the roots
- releases 3-22% more O2 than equivalent trunk area
- prop roots/deep roots: develop from lower part of stems/branches and grow out towards the substrate
- covered with lenticels that allow O2 to diffuse
- help anchor the plant
- stems
- rapid underwater shoot extension via hormone ethylene
- brings plants near (or to) the surface -> light, O2, CO2
- hypertrophy swelling of stem base in response to flooding in herbaceous/woody plants since accelerated cell expansion since separation/rupture
- increases porosity, aeration
- eg buttressing
- stem buoyancy to take up O2, CO2, especially for submerged plants
- Gas Transport Mechanism
- passive molecular diffusion
- most important!
- O2 about the same (21%) in the atmosphere as in the aerial parts of the plant, vs. 4% in the rhizomes
- pressurized ventilation
- helps diffusion
- air goes into stomata of young lives (smaller stomata -> higher gas concentration) and goes down the stems to the rhizomes then up stems and exists through old leaves
- underwater gas exchange
- gas exchange between the plants and water
- e.g. pneumatophores of mangroves
- venturi-induced convection
- based on wind speed gradient
- tall stems exposed to fast wind (lower air pressure)
- air pulled in through low stems to the rhizomes then out the tall stems
- in moderate wind, 80% or more O2 (theoretical)
- radial O2 loss (diffusion, etc.)
- submerged plants have less aerenchyma and radial O2 loss than emergents
- oxidizes toxic substances in rhizosphere
- forms plague on roots (e.g. iron)
- development of carbohydrate storage structures
- flood-intolerant plants can handle 3 days
- tolerant ones 4-90 days
- plants need more glucose (usually stored in rhizomes) when anaerobic
- plants with carbohydrates (fermenting makes it glucose) survive flooding
- more carbohydrates stored more in spring
Metabolic processes - can adjust in minutes to hours (to anaerobic) (based on lab experiments)
Salt-Water adaptations (halophytes (glycophytes don’t like salt)) - water acquisition
- water potential = free energy content of water / volume
- higher in soil water than within plant if non-saline
- salt decreases water potential
- osmotic adjustment (osmoregulation) produces compatible solutes
- salt avoidance
- exclude from roots, e.g. by Casparian bands
- some can recognize Na, Cl, and prevent uptake
- secrete via salt glands on leaves
- shed plant parts with salt in them
- succulents
- increasing cell size (thick leaves/shoots, few leaves) dilutes internal salt concentration
- can close stomata to keep water
Adaptations to Limited Nutrients - mycorrhizal associations
- symbiotic fungi (with plants’ roots)
- plant captures more water, phosphorus, etc.
- fungi get carbohydrates from roots
- endomycorrhizal (VAM) vs. ectomycorrhizal
- nitrogen fixation
- N2 made available to plants
- usually via bacteria (in nodules) which get their energy from plants
- in legumes, alder, sweet gale, etc.
- N-fixing cyanobacteria in mangroves
- carnivory
- zooplankton to insects, even frogs and birds
- mostly tropical and subtropical
- 65% of the 500 spp. are in Australia
- types
- pitfall e.g. pitcher plant
- lobster pot
- passive adhesive
- active adhesive
- bladder
- snap trap
- evergreen leaves
- common e.g. heath shrubs
- no need to re-grow leaves
Adaptations to Submergence - limited light
- ribbony leaves (high surface-to-volume ratio): light and gas diffusion
- greater concentration of chlorophyll in submergents/emergents
- low CO2
- more aerenchyma to increase buoyancy
- HCO3 for carbon
- water fluctuations
- heterophylly: different leaves so can handle wet and dry
Wetland Creation/Restoration - restoration: active (needs people to fix) vs. passive (duh)
- human-induced vs. artificial (requires continuous fixing)
- enhancement: increase some stuff, may decrease others
- mitigation: creation/restoration/enhancement
- mitigation banking: new wetland to “make up” for ones that one’ll get rid of (yay U.S. of A.)
- Canada’s lost up to 70% of wetlands in key areas
- duck habitat
- ideal is half each of open water and vegetation
- nutrients (P, N)
- 0.5-1 metres deep
- ecological engineering ? environmental engineering
- ecological engineering = ecotechnology
- design of human society with natural environment to help both
- why?
- pollution fix e.g. sludge recycling
- reduce/solve problem e.g. aquaculture
- disturbance recovery e.g. surface mine
- enhanced to solve a problem e.g. biomanipulation
- self-design, sustainable
- habitat
- water/wastewater fix
- flood control
- treating wastewater
- pond systems: stabilization, liners, forced aeration
- floating aquatic plants: duckweed, water hyacinth
- wetland types
- natural: marsh, shallow water
- man-made: surface flow, subsurface flow, floating plant systems (argh see my drawings)
- bureaucracy stuff
- performance criteria
- maintenance, monitoring
- UV kills E. coli
- plants encourage bacteria etc.
- expect non-plug flow and seasonal variation
- mosquitoes
- flood water vs. permanent water mosquitoes
Wetland Values - wetland values: services/commodities to humans
- population: waterfowl, birds, fur-bearers, trees, rare species
- ecosystem: flood control, aquifer protection/recharge, water quality, aesthetics
- regional/global: carbon and sulphur cycles
- wetland functions/processes
- ecological/environmental attributes
- socioeconomic functions
- wetland benefits: values society puts on wetland processes, socioeconomic functions/benefits
- conservation approaches
- creation, restoration, enhancement
- secure/protect
- Canadian government had said they’d protect 12% of landscape
- secured areas: government or private-owned for conservation
- national parks, etc.
- designate important sites
- Ramsar – 36 sites in Canada
- international biosphere reserves
- national, provincial sites
- ANSI: areas of natural or scientific interest
- development of policies/legislation
- federal policy on wetland conservation 1990
- most provinces have non-regulatory (consultative) processes
- policy, implementation, cooperative approach (huh?)
- North American Waterfowl Management Plan
- Ducks Unlimited
- industry/private sector
- local initiatives
- Canadian milestones
- 1979 etc classification system
- 1987 Ramsar
- 1990 national policy
- etc..
BIOL 453
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