1/63
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced |
---|
No study sessions yet.
Aquatic vs Hydraulic civilizations
Aquatic: Adapt to water abundant floodplains and deltas, working within the aquatic landscape
Hydraulic: Control water flow with dikes, dams, pumps, etc. seeking to control the natural world
U.S. Historical view on wetlands
seen as wastelands
often viewed as areas with pests and threats
were often hydrologically altered
How this influenced wetland policies:
for over 120 years, it was US policy to drain wetlands
swamp lands act → drained wetlands used for agruculture
Direct effects on wetlands
Agriculture, forestry, and mosquito elimination practices
stream chanellization/dredging (flood control)
filling → roads and development
water pollution
wetland mining
groundwater withdrawl
Indirect effects on wetlands
sediment retention by dams
hydrologic alteration by roads, canals, etc
land subsidence due to resource extraction & river alterations
Natural effects on wetlands
subsidence
sea level rise
drought
hurricanes/storms
erosion
biotic effects
Conversion
Draining, dredging, and filling
mostly due to conversion to agriculture
most notable in the midwest bottomland hardwood forests
for urban and industrial development
loss trongly correlated with population density
Hydrologic modifications
Flood control:
draining wetlands and adjacent uplands → mosquito control, limiting riparian area flooding
Navigation and transportation:
improved transport among ports
canal formation
hydrologic isolation from highway construction
Industrial activity:
canals dredged for oil well access and pipelines
Peat mining
75% of peat harvest occurs in Ireland and northeastern Europe
peat is harvested for fuel, horticulture, and agriculture
sustainable practices are almost impossible given how slow peat accumulates
Water pollution
Eutrophication: changes in species composition and oxygen content of water
Toxic inputs: acutely harm wetland communities
“No Net Loss”
National Wetlands Policy Forum (1988)
Interim goal: no net loss of wetland area and function
Future goal: net gain of wetland area and function
Clean Water Act (1972 Ammendments)
Considered the “primary vehicle” for wetland protection in the US
Section 404 of the CWA: Dredging or filling of “waters of the US” (WOTUS) requires a permit from the US army corps of engineers
404 permit screening seeks 3 things, in this order:
1) Avoidance: avoid wetland impacts where possible
2) Minimization: minimize the potential impacts on wetlands
3) Mitigation: provide compensation for any remaining, unavoidable impacts through wetland restoration and creation
Swampbuster (1985)
Provision within Food Security Act: Denies federal subsidies to any farm owner who knowingly converts wetlands to farmlands
prior to this provision, normal ag. and sivilculture activities were exempt from section 404 permit requirements
emphasizes soils component of wetland designation
Wetland Deliniation
USACE → developed guidelines to determine regulatory (jurisdictional) wetlands, 1987
this process = wetland deliniation
USACE publishes regional supplements and some states have more specific wetland policy, which affects deliniation
Four realities of the Millenium Ecosystem Assessment
1) Humans have changed Earth’s ecosystems over the last 50 years of the twentieth century more than any other period in human history
2) These changes have contributes to substantial gains in wellbeing and economic development, but at the cost of losing many ecosystem services.
3) The ecological degradation is expected to grow significantly worse in the first half of the twenty-first century
4) reversing this degradation will involve significant changes in policies, practices, and institutions that are not yet in place
Ecosystem Services (broad definition)
The benefits people obtain from ecosystems
Supporting ecosystem services
Benefits of biodiversity that allow ecosystems to exist
primary production
soil formation
nutrient cycling
Provisioning ecosystem services
Benefits of biodiversity that provide products for human use
animals harvested for pelts
waterfowl and other birds
fish and shellfish (as habitat and nurseries)
vegetation and building materials, fiber, and food
peat harvest
Regulating ecosystem services
Benefits of biodiversity that mitigate disturbance or disaster
flood mitigation
storm abatement and coastal protection
climate regulation
aquifer recharge
water quality
Cultural ecosystem services
Benefits of biodiversity that provide aesthetic, spiritual, or recreational value
Effects of wetlands on climate change → Sequestration and Storage
Sequestering carbon is not the same as storing carbon
20-30% of C in Earth’s soils is stored in wetlands
boreal peatlands store an enormous amount of C → they are considered true carbon sinks
Effects of wetlands on climate change → Emissions
wetlands emit CH4 (methane) and N2O (nitrous oxides) via natural processes. These are potent greenhouse gasses
disturbance of wetland soils turns carbon sinks into carbon sources via CH4 release.
Effects of wetlands on climate change → Thermal Buffering
“Hydrologic setting mediates local growth sensitivity to changes in ambient climate conditions” (Raney et al. 2016)
water has a higher specific heat capacity than does air, so it changes temperature more slowly
groundwater flow is particularly stable in terms of amount and temperature
Effects of climate change on wetlands → Sea Level Rise
If sea level rise is not met with equivalent sediment accreation, coastal wetlands will disappear due to Increased inundation, erosion, and saltwater intrusion
Effects of climate change on wetlands → Inland Wetland Function & Distribution
changes in precipitation and evapotransporation alter wetland function and distribution
temperature increases and precipitation decreases produce the most dramatic wetland loss
permafrost (boreal peatlands) melting = wetland loss and carbon emissions
Ecological valuation
Quantifies wetland values based on the functional services and biological components
Economic valuation
Quantifies wetland values based on the dollar amount the public is willing to pay for the good or service rather than be without it (e.g. “replacement value”)
Problems with quantifying ecosystem services
terms “value” and “service are anthropocentric and don’t acknowledge ecological etities’ intrinsic value
value of a wetland depends on its landscape context
most valuable wetland products are “common” recources
large scale ecosystem services (nutrient cycling, carbon sequestration, etc.) are hard to fully characterize and harder to quantify
The Faustian Bargain
The need to justify conservation with economic reasons, while knowing that conservation is important for reasons beyond economic or material benefit.
Intrinsic Value
Value of ecosystems (their components and functions) is not tied to economic benefit or judgement of human worth
ex: they provide a habitat for various biota
The Precautionary Principle
Biodiversity elements (species, genes, etc.) with potential use should not be lost simply because we currently do not know their value
Loss of biodiversity is generally irreversible
Why is wetland management subjective?
before protective legislation → draining, dredging, and filling was considered “managing”
currently → “management” refers to maintaining or enhancing wentland functions and values
Ecosystem perspective
Focuses on function
water recharge
Nitrogen sink
“Self design”
species relatively less important than valued functions
wetland functions primarily a product of hydrologic setting
Community perspective
Focuses on natural community patterns
species composition and structure
Characteristic species patterns suggest characteristic functions also being performed
recognition that species can be important drivers of ecosystem functions
General perspective on wetland management
Sound management for wetlands considers both ecosystem perspective AND community perspective
The site context (landscape, social, political, economic) affects whether one takes more of an ecosystem or community perspective
Human Impacts Model
Considers broad categories of human alterations to wetlands:
hydrologic modification
hydroperiod
water source
flow rate
Biogeochemical modification
nutrient loading
pH modification
salinization
freshening
thermal alteration
Disturbance Regime modification
type
frequency
duration
intensity
timing
Species pool modification
Invasion
extinction
habita fragmentation/dispersal limitation
exhaustion from seed bank
Water level management guidelines
Water level should…
vary from year to year and/or within-year
be lowest during the growing season
Nutrient inputs management guidelines
Restrict nutrient inputs because…
the more kinds of infertile (marginal) habitats available, the more plant species can coexist
eutrophication generally reduces species richness
Monitoring
The key to success and flexibility, which is adaptive management
Ecological restoration
Process of assisting the recovery of an ecosystem that has been damaged, degraded, or destroyed
Main takeaways:
many restored ecosystems needs active management for some time after recovery
some restoration involves the creation of new wetlands
recovery of hydrology, biogeochemistry, community adaptations and traits, and succesional processes
restoration may be incomplete or incapable of completely reversing anthropogenic impacts
Reference ecosystem
ecosystem that is a model for a degraded system’s restoration → a target
must incorporate a range of conditions, and mechanisms of resistance and resilience
Threshold approach
restoration efforts (and decisions) initially based on which threshold(s) a degraded ecosystem has crossed
If the threshold is controlled by abiotic limitations, recovery is longer and harder
Directing succession
Land managers take advantage of successional pathways or stages to restore ecosystem function
Habitat heterogeneity
A variety of habitat types
causes: natural legacy effects, natural disturbances, human activity
can generate species diversity at local and regional scales
Habitat fragmentation
Large expanse of habitat is transformed into many smaller patches of habitat
General effects:
total amount of habitat decreases
number of patches increases
amount of edge habitat increases
patch isolation increases
effects of fragment size:
smaller fragment size = lower spp. diversity
smaller fragment size = increased trophic cascades
effects of fragment edges:
ecotones form along edges
edges change the abiotic conditions and spp. composition of the habitat
Corridors, connectivity, and conservation:
metapopulation: regionally connected populations of a spp.
corridors → allow connectivity between habitat patches
conservation efforts often week to protect metapopulations w/ corridors
Biodiversity hotspots
Biodiversity is not evenly distributed across earth
Norman Myers (1988) established regions of conservation priority based on endemism and vulnerability → these are hotspots
Hotspot criteria:
irreplaceable (ex: at least 1500 endemic spp. of vascular plants)
Threatened (lost at least 70% of original habitat)
SLOSS
Single Large Or Several Small → two different approaches to conservation
Given the same total amount of land area…
single large favors one sizeable, contiguous preserve
several small favors multiple smaller areas of land
Swamp Land Acts 1849, 1850, 1860 (Drainage Acts)
Up until the 1970’s, US army corps of engineers promoted wetland drainage thru the Natural Resources Conservation Service
Wetland mitigation
offsets for unavoidable impacts to wetlands under a permit
mitigation bank → built ahead of impacts
in lieu fee program → built within 3 years of credit sale
Permittee responsible → built concurrent with impacts
Sources used by Dr. Landis
Paleoecology
archaeology
missionary records
maps/surveys
oral history
ethnobotany
What communities did Dr. Landis find?
shrub swamp
cedar swamp
inland salt marsh
rich fen
beech-maple forest
General impacts of flooding on plants
Changed hormone levels
Ethylene → structural adaptations
Abscisic acid → stomatal closure
Reduced gas exchange
reduced water uptake
altered nutrient uptake
Morphological (structural) plant adaptations to flooding
Aerenchyma:
allows oxygen to diffuse to flooded plant parts
decreases respiratory demand → reduced cellular density
Adventitious roots:
new root growth from stems or leaves
above the anaerobic zone
Stem hypertrophy:
swelling of lower stem
buttressing, helps with stability
Stem elongation
rapid vertical stem growth
keeps photosynthetic organs out of the water → think lillypad
Lenticels:
small pores on woody plant surfaces
conduits to aerenchymous tissue
Root adaptations:
shallow root systems
pneumatophores or “knees”
Physiological (funcional) plant adaptations
Pressurized gas flow:
pushes oxygen to roots
pressure gradient driven by temp. differences
Rhizosphere oxidation:
extra oxygen pushed out of plant roots
Decreased water uptake:
intolerant of anaerobic conditions
flooding limits root metabolism
Altered nutrient absorption:
sybiotic plant root+fungi relationship
carnivory → increased nitrogen intake
Sulfide avoidance:
oxidation of sulfide to make it safer
metabolic tolerance
Anarobic respiration:
less efficient, and causes toxic byproducts
Whole plant strategies
Timing of seed production:
delayed or accelerated flowering
seeds made in non-flood season
Buoyant seeds and seedlings:
float until they reach high or unflooded ground
viviparous seedlings
Persistent seed banks:
cache of dormant seeds in soil
wait for non-flooded conditions for germination and establishment
Resistant roots, tubers, and seeds
can survive long periods of submergence
Evergreen sclerophyllus foliage:
tough, leathery leaves → protection from wilting and herbivory
Brittle twigs:
rapid twig breaking protects main trunk/stem
twigs also often propagules
Facilitation
the presence of one species alters the environment in a way that enhances the growth, survival, or reproduction of another species
Interspecific competition
Individuals from one species consume or drive down the abundance of a resource or defend the resource, to the point that individuals from another species cannot persist
Clementsian community
Communities are “superorganisms” with each association of species being an interacting, integrated component of a larger unit.
species in association rise to max abundance at the same point
transitions between communities are narrow or sharp
Autogenic
interdependent species assembly
Gleasonian community
Community continuum concept: species coexist in communities due to similarities in their tolerance and requirements, but are not exclusive to that association
changes in species abundance and transition along a gradient are gradual and difficult to identify.
allogenic
Independent species assembly
Modern community boundaries summary
Clementsian and Gleasonian views both accepted, but Gleasonian view (community continuum concept) is considered the most broadly accurate.
Zonation
changes in physical and biological structures of communities as one moves across the landscape. It manifests by changes in species composition and/or diversity
often driven by:
physical processes (sediment deposition, flooding)
abiotic gradients (salinity, pH)
competetive heirarchies
Life History Strategies (C-S-R model) (Grime)
There are tradeoffs to being a good competitor, or stress-tolerator, or disturbance-tolerator.
competetively dominant spp. can outcompete and exclude weaker competitors
less competitive spp. often occupy niches that are physiologically suboptimal
Centrifugal Organization Model (Keddy)
Dominant spp. occupy core habitat and exclude weaker competitors to “peripheral” habitats that are more stressful/more disturbed.
greater species richness in peripheral habitats
peripheral or marginal habitats are important for conservation → higher densities of rare spp.
Environmental Sieve Model (Van der Walk)
Vegetation patterns in a community are predicted by 3 traits:
propagule longevity (in the seedbank)
plant lifespan (annual or perrenial)
propagule establishment requirements (drawdown)
The “sieve” selects for particular traits
How does the bog climax hypothesis counter hydrarch succession?
Allogenic factors such as precipitation play a major role in the bog climax
persistence of wet conditions
sphagnum moss dominance
Classical Hydrarch Succession = Predictable, linear progression from water → land.
Bog Climax Hypothesis = Wetland may reach a stable, non-forested climax, contradicting the idea that succession always ends in upland forest.