Lecture 9 Flashcards
1
Q
Nuclear research gave ecology tools and a model
A
- Radioactive tracers allowed following fates of chemicals in natural communities
- Manhattan project was classic model for collaborative “Big Science”, a model that ecologists tried to follow with limited success
2
Q
Aspects of selected biogeochemical cycles
A
- Carbon cycle
- Nitrogen cycle
- Human intervention: N fertilizer for crops
- Phosphorus cycle
- Human interventions: mining, pollution
3
Q
Chemistry of natural world
A
- Large organic molecules constantly being synthesized, consumed, and broken down
- Chemical elements aren’t created or destroyed, but they move around (cycling)
- Cycle comprises of pools and fluxes
- Stable, long-lived compounds can persist much as elements do
4
Q
C, N and P cycles
A
- All tied to hydrologic cycle
- Carbon cycle subsumes trophic webs
- N and P are two elements most likely to limit plant productivity
- Key for figures
- Solid black lines: strong natural fluxes
- Solid red lines: strong human fluxes
- Dashed black lines: weaker natural fluxes
5
Q
C cycle
A
- CO2 is gaseous phase, much C in organisms, inactive sedimentary pool of carbonates
- Limiting steps involve balance between creation by photosynthesis and respiration/combustion of organic matter
- Human intervention: Combustion of fossil fuels, land conversion
6
Q
Agricultural impacts on carbon
A
- Humans deforest land
- Aid to hunting (burning to open and maintain grasslands)
- Provide land for agriculture (cutting and burning)
- Remove agricultural waste
- In N. America, easternmost prairies would revert to forest without fire
- Important phenomenon since the dawn of agriculture
- Carbon sequestered in trees is released by fire
7
Q
Deforestation in the US
A
- 1620s: Forest mostly cover
- 1920s: Forest mostly eliminated
8
Q
Decadal losses in global forest over last three centuries
A
- Temperate forests on decline from 1900s
- Temparate regrowth from 2000s onwards
- Tropical on decline, mass deforestation
9
Q
Annual deforestation
A
- Peak of deforestation in tropical countries
10
Q
Tropical forests contain great stores of carbon
A
- Near maximum: Indonesian Kalimantan swamp forest on peat soils
- Living plants: 600 tonnes/hectare
- Dead plant material in soil(peat): 340 tonnes/ha
- Usually too wet to burn, logging causes drying
- If forest burns, peat burns too
11
Q
Human effects on carbon budget
A
- Larger carbon compounds oxidized to CO2, released into atmosphere
- Current annual rates of CO2 release
- Fossil fuel burning: 6 billion tonnes
- Deforestation: 1.6 billion tonnes
- Atmospheric CO2 from 280 ppm to 417 ppm
- Strengthening greenhouse effect
12
Q
N cycle
A
- Mostly gaseous compounds, highly soluble, minimal sedimentary pools
- Limiting steps involve converting inert N2 gas, which plants can’t use into usable soluble nitrate or ammonium
- Human intervention: Combustion of fuels, use of energy to make synthetic fertilizers
13
Q
Human intervention in nitrogen cycle
A
- An atmospheric cycle
- Anthropogenic reactive N inputs from fuel combustion now exceed natural production rates (in industrial areas, rainwater now a dilute fertilizer)
- Ecosystems being enriched
- Fast, growing, weedy plants favored
- Nitrate buildup in groundwater a hazard in agricultural areas
- Eutrophication of coastal waters, anoxia
14
Q
P cycle
A
- Gases not important, most compounds minimally soluble, sedimentary pools dominate, end up in ocean sediments
- Limiting steps involve weathering of rocks in soil, geological uplift
- Human intervention: Mining phosphate rock for fertilizer, fishing, sewage, agricultural runoff, erosion
15
Q
Phosphorus chemistry 101
A
- No gaseous forms, mostly in rocks
- Made available through weathering, geological uplift, mining
- Atmospheric dust sometimes important input
- Phosphate technically soluble, but can be bound by soil components; mycorrhizal fungi help pull it into solution so plant roots can get it
16
Q
Human intervention in phosphorus cycle
A
- A sedimentary cycle (slow)
- We can’t make P fertilizer; must mine phosphate rich rocks ( + guano deposits)
- Lost from terrestrial systems by runoff, erosion, over-application of fertilizers: eutrophication of rivers and lakes
- Much ends up back in marine sediments
17
Q
Phosphate rock for fertilizer in agriculture
A
- Mostly sedimentart rock (old seabed, uplifted)
- Biggest known reserves: Morocco, US, South Africa, Jordan, China, Russia, Senegal
- Depletion of reserves estimated to be within/in 40-400 years
- Offshore deposits to become targets
18
Q
Best seabird guano industry: islands off coast of Peru
A
- Seabirds nest on islands because island lacks predators
- Seabird colonies best developed where big fish populated
- Fish populations best developed where cold water upwelling
- Upwelling brings P-rich to surface into food chain
- Dry climate means guano not rapidly leached by rain