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
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2
Q

Aspects of selected biogeochemical cycles

A
  • Carbon cycle
  • Nitrogen cycle
    • Human intervention: N fertilizer for crops
  • Phosphorus cycle
    • Human interventions: mining, pollution
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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
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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
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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
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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
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7
Q

Deforestation in the US

A
  • 1620s: Forest mostly cover
  • 1920s: Forest mostly eliminated
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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
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9
Q

Annual deforestation

A
  • Peak of deforestation in tropical countries
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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
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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
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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
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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
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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
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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
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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