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Title: 2.2 Nutrient Cycles in Ecosystems p.68-91


1
Chapter 2
  • 2.2 Nutrient Cycles in Ecosystems p.68-91
  • Words to Know
  • cellular respiration photosynthesis
  • denitrification sedimentation
  • nitrification weathering
  • Nutrients

2
2.2 Nutrient Cycles in Ecosystems
  • Nutrients - chemicals needed for plant and animal
    growth.
  • Nutrient cycles the flow of nutrients IN and
    OUT of the land, ocean, atmosphere and deep rock.
  • The health of our ecosystems depends on the
    balance of
  • Carbon, Nitrogen, Phosphorous, Hydrogen and
    Oxygen
  • C N P
    H O


3
Nutrient Cycle Diagram
4
Nutrient CyclesThe Carbon Cycle
  • CARBON CYCLE
  • A. Carbon Facts
  • Carbon is an element found in the molecules of
    all living and dead things.
  • It is important for plant growth.
  • Places carbon is found are called stores or
    sinks.
  • Short-term Stores Long-term Stores
  • living things in water and on land underground
    (oil, gas, natural
  • rotting tissue of plants and animals gas and
    coal)
  • atmosphere (air) sedimentary rock (limestone)
  • ocean (dissolved in the water) ocean floor (old
    shells)


5
  • How Carbon Changes Form
  • 1. Photosynthesis (in plants, algae and
    cyanobacteria)
  • CO2 H2O sunlight ? C6H12O6 O2
  • 2. Cellular respiration (in cells of all living
    things)
  • C6H12O6 O2 ? CO2 H2O ENERGY
  • (energy is used for growth, repair etc.)
  • Decomposition (rotting)
  • cellulose ? CO2
  • Only done by bacteria and fungi

6
  • Ocean Processes
  • Ocean mixing moves CO2 around the world
  • CO2 sinks in cold ocean waters ? flows to the
    warm equator and evaporates into the air.

7
  • Combustion (burning, engines, volcanoes, forest
    fires)
  • fossil fuels O2 ? CO2 H2O ENERGY
  • (oil, gas, natural gas, coal)

8
CARBON CYCLE DIAGRAM
See page 76
9
Nutrient CyclesThe Carbon Cycle (continued)
  • Human Activities Have Increased CO2 in the
    atmosphere.
  • Burning Fossil Fuels.
  • CO2 in atmosphere has increased 30 in past 160
    years (since Industrial Revolution began).
  • In the 160,000 years before that, it only
    increased 1-3.
  • Carbon is being removed from long-term storage
    more quickly than it naturally would as we mine
    coal and drill for oil and gas.
  • CO2 is also a greenhouse gas, which traps heat in
    the atmosphere.

See page 77
10
  • Removing Trees.
  • Large trees and shrubs absorb CO2 from the
    atmosphere, so when they are cut down, there is
    more CO2 in the air.
  • Crops that replace the trees dont remove as
    much CO2

11
Nutrient CyclesThe Nitrogen Cycle
  • Nitrogen Cycle
  • Nitrogen Facts
  • Makes up DNA and proteins (muscle function).
  • Help plants grow.
  • Where Nitrogen is Found
  • Atmosphere (78 is N2)
  • Oceans
  • Organic matter in soil
  • Lakes, marshes, organisms

See page 78
12
  • How Nitrogen Changes Form.
  • N2 is not usable by plants or animals, so it has
    to be converted to other forms.
  • Plants can use NO3- (nitrate) and NH4 (ammonium)
  • Nitrogen Fixation
  • Lightning changes N2 (nitrogen gas) ? NO3-
    (nitrate).
  • Rain washes nitrate into soil. This only fixes
    a tiny amount of nitrogen.
  • Bacteria in soil (rhizobium) and cyanobacteria in
    water
  • change N2 (nitrogen gas) ? NH4 (ammonium).
  • This processes fixes most nitrogen.
  • Rhizobium live on the roots of legumes (peas,
    alfalfa, beans) and alder trees.

13
Nutrient CyclesThe Nitrogen Cycle (continued)
  • Nitrification
  • NH4 (ammonium) ? NO2- (nitrite) ?
    NO3- (nitrate)
  • This is done by nitrifying bacteria.
  • Uptake
  • NO3- is sucked into plants and used for growth.
  • Herbivores eat the plants and use the Nitrogen
    for making proteins and DNA.
  • Denitrification
  • NO3- ? N2 done by denitrifying bacteria
  • N2 is also returned to the atmosphere through
    volcanic eruptions.

See pages 78 - 79
14
Nitrogen Cycle
See page 81
15
Nutrient CyclesThe Nitrogen Cycle (continued)
  • Human activities affect the nitrogen cycle.
  • The amount of nitrogen in the ecosystem has
    doubled in the last 50 years due to
  • Burning fossil fuels and sewage treatment.
  • NO and NO2 are byproducts
  • Land-clearing by burning.
  • acid rain is formed which contains nitric acid
    (HNO3).
  • Overfertilization
  • excess NH4 and NO3- leach into the soil and
    waterways.
  • This promotes huge growth in aquatic algae
    eutrophication
  • These algal blooms use up all CO2 and O2 and
    block sunlight, killing many aquatic organisms.
  • The algal blooms can also produce neurotoxins
    that poison animals.

16
Nutrient CyclesThe Phosphorous Cycle
  • Phosphorous Cycle
  • Phosphorous Facts
  • Phosphorous is a part of the molecule that
    carries energy in cells (ATP).
  • Phosphorous helps root growth, stem strength and
    seed production.
  • In animals, phosphorous is important for strong
    bones.
  • Where Phosphorous is Found
  • Not in atmosphere, but in phosphate rocks (PO43,
    HPO42, H2PO4) and sediments on the ocean floor.

See pages 83 - 84
17
  • How Phosphorous Changes Form.
  • 1. Weathering (breaking down rock into smaller
    pieces).
  • a) Chemical weathering
  • acid rain or lichens releases phosphates
    (PO43- )
  • b) Physical weathering
  • wind, water and freezing release the
    phosphates.
  • Uptake
  • plants suck up PO43- for growth, then are eaten
    by animals.

18
  • Decomposition (rotting)
  • Bacteria break down dead plants and animals and
    phosphorous is returned to soil.
  • Geologic Uplift
  • when rocks under the ground are pushed up ?
    mountains ? weathering.

19
The Phosphorous Cycle
20
  • C. Human activities affect the Phosphorous
    Cycle.
  • 1. Mining
  • Increases P in ecosystems quickly. Natural
    stores are not replaced.
  • 2. Slash-and-burn forest practices.
  • Turns P into ash, which runs into waterways.

21
How Changes in Nutrient Cycles Affect
Biodiversity
  • To Review
  • Any significant changes to any of these nutrients
    (C, H, O, N or P) can greatly impact
    biodiversity.
  • Carbon cycle changes ? climate change and global
    warming.
  • Too much nitrogen can allow certain plant species
    to out-compete other species.
  • Decreased levels of phosphorous ? slow
  • growth of algae (important producers).

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