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126 Terms
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Ecosystem
an entity bound in space and time made up of a set of interacting elements that may be biological, physical, or chemical
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Sir Arthur Tansley
Though the organism may claim our primary interest ... we cannot separate them from their special environment, with which they form one physical system
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Energy flow
transformation and storage of energy (i.e., the tracking of C-C bonds)
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Material (nutrient) cycling
transformation, storage, reuse, and movement of materials (C,H,N,O,P,S, etc.) (nutrients in ecosystems)
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Structure
the distribution and abundance of materials within an ecosystem
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Standing stock
(kg/m2), animal-like materials, element of structure
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Standing crop
(kg/m2), plant-like materials, element of structure
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Organic matter (OM)
living or dead material generated by biota (composed mainly of CHNOPS)
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Function
rates of processes occurring within ecosystems that influence the distribution and abundance of energy and materials
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Metabolism
all biotically driven anabolic and catabolic chemical reactions within an ecosystem (mg C/m2/d, mgO2/m2/d, kg OM/ha/yr)
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Primary production
rate of carbon fixation by autotrophic organisms
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Respiration (R)
rate of biological oxidation of organic matter, amount of energy lost due to biological oxidation of organic matter
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Gross primary production (GPP or PG)
the amount of energy fixed as carbon per unit time
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Net primary production (NPP)/net ecosystem production (NEP)
amount of carbon fixed as biomass per unit time (i.e., after loss due to respiration is included)
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Relationship of GPP, R, and NPP/NEP
GPP = NPP + R or GPP = NEP - R
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Predictors of NEP
Temperature and moisture
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Predicting NPP across a tropical to arctic gradient
actual evapotranspiration (AET) = total amount of water that is evaporated through plants during a year (mm H2O/yr)
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NPP across various systems within a similar biome have features:
heat content is relatively similar and rates of NPP are driven water availability
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With a given water availability, primary production variation is related to...
...nutrient abundance
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Forest NPP is limited by...
...nitrogen availability
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Freshwater systems are limited by...
...phosphrous availability
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Ocean productivity is limited by...
...N, P, Si, and Fe
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Order of biome NPP rates (highest to lowest)
Estuaries/Swamps/Tropic Rain Forest, Temperate Forest, Deserts, Open Ocean
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Order of biome NPP amounts (highest to lowest)
Open Ocean (32%), Tropic Forests (29%), Temperate Forests (14%)
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Trophic level
a collection of biota at the same level of energy exchange as measured by the number of steps of energy assimilation starting with primary production
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Trophic transfer causes the loss of...
...energy via respiration
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Lindeman Ratio
10% of production at one trophic level becomes production at the next
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Each step of trophic interaction adds...
...OM to the detrital pool
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Decomposition
breakdown of organic matter including physical reduction in size and biotic oxidation of carbon
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Nutrient
elements required by organisms for development, maintenance, and reproduction
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Mineralization
conversion of nutrients from organic to inorganic form
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Decomposition Intrinsic factors
Features internal to OM influence rates and processes of decomposition e.g., lignin, toughness, internal nutrients (C:N), species (higher N is more tough)
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Decomposition Extrinsic factors
External environmental features influence rates of decomposition e.g., precipitation, nutrients, temperature,
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Biogeochemistry
The study how the basic chemical conditions of the Earth are affected by the existence of life.
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Nutrient Pool
The amount of a particular nutrient stored in a portion, or compartment, of an ecosystem
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Nutrient Flux
An areal rate of nutrient transformation or translocation
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Nutrient source
A portion of the biosphere where a particular nutrient is released more rapidly than it is consumed
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Nutrient sink
A portion of the biosphere where a particular nutrient is consumed more rapidly than it is released
Forms of N that cycle readily among living entities
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Nitrogen fixation (N-fixation)
Rate of conversion of N2 gas to a biologically available form, often found on the earth's surface
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Denitrification
Rate of converting nitrate (NO3-) into N2 gas via anaerobic respiration
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Non-reactive (inert) N
Atmospheric N2
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Biological N-fixation
Rate of biological conversion of N2 gas to Norg
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Autotrophic biological N-fixation
The use of light energy for N2 reduction to form internal organic N.
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Bluegreen bacteria
autotrophic N-fixers that can from Harmful Algal Blooms (HABs)
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Heterotrophic biological N-fixation
The use of existing organic C to fuel N2 reduction to organic N
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Root nodules in some plants...
(e.g., legumes) house heterotrophic symbiotic bacteria that carry out heterotrophic N-fixation.
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Industrial N-fixation
Rate of the industrial synthesis of ammonia (NH3 = NR) from nitrogen (N2) and hydrogen (H2), known as the Haber-Bosch process.
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Human industrial and agricultural N-fixations has...
...doubled the rate of input to the reactive N pool, while rates of removal from denitrification have remained constant. Reactive nitrogen pool has increased in size
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Glacier Bay (Vancouver and Muir)
Muir Glacier visible reduction in size over the course of a century, leaving behind newly uncovered surfaces
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Glacier National Park (Fagre)
USGS analysis has shown massive glacial retreat in the park since the 1960s
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Succession
gradual change in the structure and functioning of plant and animal communities following disturbance
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Pioneer community
early successional colonists capable of establishing populations on newly exposed area shortly after disturbance
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Primary succession
succession occurring on substrates not significantly modified by organisms (starting from scratch, no seed bank)
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Secondary succession
succession that occurs in areas where disturbance has removed the community but not destroyed the soil
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Climax community
a community whose composition remains stable until again influenced by disturbance
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Glacier Bay Succession
shows the changes of primary plant succession over 1000 years, understood due to the gradual retreat of the glaciers
alder trees (w/ nitrogen fixing symbionts), grow thicker as Dryas dies back
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GB PPS 100-200 Years
Spruce stands
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GB PPS 1000+ Years
Muskegs (peatland)
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Space for time substitution
An approach that uses different locations to represent different stages of succession based upon the age of individual positions in space. The influence of time is inferred from spatial comparison among sites with different time since disturbance.
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Primary succession species richness plateaus around...
...1500 years post disturbance
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Secondary succession happens...
...with similar trends to primary succession, but on a quicker timescale, as resident biota still exists to initiate growth and repopulation
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Plants and Old-field Succession
instances of plants recovering from agriculture, same shape of richness increases but at a quicker rate due to secondary succession
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Animals in old fields and secondary succession...
...mirror and follow the richness and influences of vegetation trends, similar species richness trends at a similar rate
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Ecosystem succession
changes in ecosystem structure and function following disturbance
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Succession increases...
...soil depth/development, soil OM, moisture, N
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Succession decreases...
...bulk density, pH, P
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Hardwood Watershed Disturbance (Bormann and Likens)
pair watershed approach, 60-year-old forest was clear cut after several years of observation, succession was repressed with herbicides (disturbance)
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When ecosystems are disturbed...
...they lose nutrients through their waterways (nitrate accumulation increased 10x) because no vegetation is present to use the nutrients
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During succession...
...primary production increases, and nutrient loss declines (nitrate back to baseline after 4 years, Ca and K still high after 7)
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Disturbance Related Mortality...
...changes the relative abundance of dead organic matter and the balance of production and respiration
Observed century-scale rise in the average temperature of the Earth's climate system and its related effects
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Fossil fuel
Carbon containing substances generated by geologic and biological processes used by man as an energy source
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Greenhouse effect
The process by which radiation from a planet's atmosphere warms the planet's surface to a temperature above what it would be without its atmosphere (radiatively-active gases = RAGs)