1/76
Looks like no tags are added yet.
3 key features used to define wetlands
Hydrology, soils, and hydrophylic vegetation
Threats to wetlands
Industrial development, climate change, and pollution
Ecosytem services provided by wetlands
Carbon sequestration and toxin removal
Wetlands that only have sedges and grasses
Marshes
Wetlands that only have trees
Swamps
Wetlands along __ margins are referred to as lacustrine
Lake
The seasonal variation of water levels in a wetland is also referred to as its
Hydroperiod
Bogs are sustained by groundwater inputs
False
Scientific and legal definitions of wetlands are the same
False
Wetlands with variable hydrologic conditions have higher species diversity
True
Discharge wetlands are created by inflowing groundwater
True
Wetlands along the margins of rivers, streams, or lakes
Riparian ecosystems
Obligate Wetland Plant
Species that almost always grows in wetlands under natural conditions
Facultative Wetland Plant
Plant species that usually occur in wetlands but are occasionally found in non-wetland areas
3 obligate wetland plants
Buttonbush
Alder
Cattail
Geomorphology
Topography, flat versus steep gradients, inflows and outflows
Discharge wetlands
Wetlands created due to inflowing groundwater
Recharge wetlands
Wetlands that lose water to the water table (need a lot of precipitation)
Flow-through wetlands
Wetlands that receive and release groundwater
Primary productivity
productivity increases with increase in flowthrough
greater amounts of nutrients
fresh sediment
new propagules
removal of toxins
Four major components of soil
Air (25%)
Water (25%)
Mineral Matter (45%)
Organic matter (5%)
Soil texture
size distribution of soil particles
Soil structure
soil particles are arranged together
Soil Color
Hue, Value (lightness or darkness), chroma (intensity or brightness)
12-18% or more of organic carbon or greater than 20-30% organic matter
Organic soils

Organic wetland soils
Histosols
Organic soil origins
Mosses
Herbaceous material: such as reed grasses
wood and leaf litter
Types of organic soils (Histosols)
Saprists: two thirds or more material is decomposed and less than one-third of the plant fibers are identifiable
Fibrists: less than one-third of material is decomposed and more than two-thirds of the plant fibers are identifiable
Hemists: conditions between saprist and fibrist soil
Folists: organic soils caused by excessive moisture
Oxygen content in the soil
20% to less than 5%
High to moderate oxygen content
aerobic condition
Low or negligible oxygen content
anaerobic condition
Two drainage conditions characteristic of wetland soils
poorly drained (PD)
Very poorly drained (VPD)
Loss of electrons
Oxidation
Gain of electrons
Reduction

MEMORIZE THIS

Hydrophyte
Water plant
Xerophyte
Dry plant
Mesophyte
no specific adaptations to too much or not enough water
Tolerators
Possess functional modification enabling them to survive inundation
Regulators
Avoid water stress or modify it to minimize effects
Species richness often increases as water flow or pulsing hydrology increases
true
Spatial heterogeneity creates additional ecological niches and enhances diversity
true
Structural (or morphological) adaptations to flooding
Aerenchyma tissue in roots and stem
adventitious roots
stem hypertrophy
fluted trunks
shallow root systems
lenticles (gas exchange)
cypress knees
Normal air space is - % of plant volume, while wetland roots may be up to __% air
2-7%
60%
due to aerenchyma tissue acting as a vent
difference between sedges, rushes, and grasses
Sedges have edges, rushes are round, grasses are hollow
Physiological adaptations to flooded areas
pressurized gas flow
rhizospheric oxygenation
decreased water uptake
altered nutrient absorption
sulfide avoidance
anaerobic respiration

Whole plant adaptation to flooded conditions
carnivory
floating seeds
timing of seed drop
asexual growth
vivipary (seeds germinate while fruit is still on the tree)
Wetland plant life forms
rooted floating: roots are in the substrate, but most leaves and flowers float on the water surface
rooted submerged: roots are in the substrate, and most leaves and stems are underwater
non-rooted floating: plant is not rooted at all
emergent: plant is rooted and most growth arises above the water surface
Persistent: plant form remains intact following winter dormancy
non- persistent: does not remain intact following winter dormancy
Natural sources of nitrogen
lightning
biological nitrogen fixation
Anthropogenic sources of nitrogen
burning of fossil fuels
widespread cultivation of N-fixing crops
use of fertilizers in agriculture— synthetic and animal manures
urban, suburban, rural sources— wastewater, lawn fertilizers, septic tanks
*Wetlands are referred to as the “kidneys” of the landscape
Because they help remove excess nitrogen from the soil and water
Key nitrogen polluter (difficult to control)
NO3
Available inorganic N forms
Nitrate
Ammonium
Mineralization
Conversion or organic N into inorganic N forms ( NH4+, NO3-) via processes like decomposition
Immobilization
Conversion of inorganic N forms to organic N forms (via processes like plant & biological uptake)
Nitrification
Aerobic only; microbial
conversion of ammonium —> nitrate
occurs in oxic soils- not in anoxic wetlands, therefore ammonium accumulates in wetlands because this process is shut off
Denitrification
anaerobic; facultative bacteria
process of conversion of nitrite and nitrate to nitrogen gas N2
Typically occurs in saturated soils
MAJOR ecosystem service by wetlands
Iron and Manganese Transformation
occur after nitrate on the redox scale
both Fe and Mn are reduced/oxidized by bacteria
Fe and Mn in their reduced forms are mobile and soluble
Ferrous causes grey-green coloring
Ferric causes reddish brown color
Sulfur reductions occur after Fe and Mn on the redox scale
True
S forms in wetlands:
Organic S (>70%)
Reduced inorganic sulfides such as pyrite (<10%)
Dissolved sulfate (<20%)
Gases (<5%)
Aerobic zone sulfur processes
immobilization
oxidation of inorganic sulfide and elemental sulfur
mineralization of organic S to sulfate
Anaerobic zone Sulfur processes
conversion of sulfate to H2S by reducing bacteria
H2S can be released to the atmosphere or can react with organic matter to form organic S
Biggest elements used by plants
nitrogen and phosphorus
3 main P forms
organic P
fixed mineral P
ortho-phosphate P
80-90% of the P in soils is in organic or fixed form
True
*In organic soils >95% of P is organic
Wetlands work very good for nitrogen removal but not as well for phosphorus
because organic soils cannot remove P; you need mineral soils rich in iron oxides (phosphorus binds to iron)
Last stage in redox sequence
carbon
Sources
when wetlands release more nutrients than they receive
Output > input
Transformers
when the nutrient form is converted. the ouput may not necessarily be reduced
inorganic N —> organic N
Inorganic P —> organic P
Sinks
when wetlands reduce the nutrient amount
(output < input)

Fermentation
organic matter broken down to produce lower acids, alcohol and CO2. by facultative or obligate anaerobes
Methanogenesis
when certain bacteria use CO2 as the electron acceptor and generate methane gas (CH4)
Methane oxidation
methane conversion to CO2 by methanotrophs under oxic conditions