Module 7 Flashcards

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1
Q

Pollen grains in sedimentary rock (AE)

A
  • Distributed by winds → fossilised at bottom of lakes/bogs
    As climate + environment around lake changes, so does composition of pollen preserved in lake sediments
    → looking at composition of pollen to identify plant species and relate to climate, eg. alpine pollen = cold climate
    Pollen grains do not provide global temp → only LOCAL
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2
Q

Rock types and formations (AE)

A
  1. Vast chalk deposit in White Desert at Farafra depression
  2. Chalk- limestone composed of calcite
  3. Process of glaciation
  4. Surface exposure dating
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3
Q

Fossils and microfossils
 (AE)

A
  1. Fossil reefs, stromatolites, limestone deposits, Ediacaran fossils and sand ripples found in Australia.
  2. In SA, Cambrian limestone in Normanville on Fleurieu Peninsula.
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4
Q

Changing isotope ratios in rocks and deep sea sediments (AE)

A
  1. O-16 evaporates first into atmosphere = tropic oceans rich in O-18 molecules
  2. O-18 molecules precipitate/condense at lower, mid latitudes
  3. Evaporated O-16 molecules travel via clouds towards pole, then precipitates as snow
  4. O-16 trapped in glaciers during cooler periods
  5. When climate becomes warmer, O-16 rich glaciers melt back into the ocean, increasing ratio of O-16:O-18
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5
Q

Ice cores
(RE)

A

Warmer periods = more O-18 isotopes in frozen H2O = changes in snow fall from high to lower levels

  1. Winter seasons indicated by darker layers in ice core
  2. Summer is indicated by lighter layers
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6
Q

Dendrochronology (RE)

A
  1. 1 ring = 1 year of growth in an oak tree
  2. Scarring in rings = fires
  3. Disfigured rings = uneven growth from lack of sunlight
  4. Measure rings across several trees to reveal matching patterns (cross-dating)
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7
Q

Dendrochronology 2 (RE)

A
  1. Growth directly affected by surrounding conditions
  2. Indicates seasons in which growth was poorer/better helping infer climate conditions
  3. Captures climate conditions from periods older than tree life
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8
Q

Aboriginal art sites
 (RE)

A
  1. Now extinct species/environments recorded in form of rock painting
  2. Aboriginals in Aus for 50,000 years > - witnesses to changes in climates, ecosystems, native animals
  3. Art sites preserve iconic megafauna eg. Procoptodon
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9
Q

Human instrument records (RE)


A
  1. Thermometers measure atmospheric temperature
  2. Models predict effects of future climate change
  3. In past decade, human record of predictions have nearly all come true (most accurate form of data)
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10
Q

Changing isotope ratios in coral (RE)

A
  1. Calcium carbonate layers in their growth- rate read to show salinity, pH, temp
  2. Skeletal cores in UV/X-ray captures differences in growth rates through coral life
  3. Increasing pH creates stress by eating away at skeleton
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11
Q

Stalactites

A

Hanging in ceiling

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12
Q

Stalagmites

A

Growing from ground up

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13
Q

Isotope ratios in stalactites and stalagmites (RE)

A

Sampling their O:16-O:18 ratio provides info on their temp + growth rates reflect rainfall activity

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14
Q

Natural greenhouse effect

A

Some solar energy reflected back into space, some absorbed by GHG- this traps heat to warm atmosphere. This:

  1. Regulates average temp. to allow survival.
  2. Temp influenced by ice ages, interglacial periods every 100,000 years
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15
Q

Anthropogenic greenhouse effect

A

Fossil fuels, agriculture, growing populations
^^ increases GHG levels in atmosphere

  1. Temp rise by approx. 0.7 degrees since 20th century
  2. Increased ozone creates smog in city +blocks UV radiation
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16
Q

Influence of increasing GHG

A
  1. Biomass burning
  2. Methane (fossil fuel + livestock)
  3. Carbon dioxide (deforestation)
17
Q

Ocean acidification (OA)

A

Acidity changes in ocean as CO2 in atmosphere dissolves in water, lowering pH.

18
Q

Influence of ocean acidification (OA)

A

Since Industrial revolution, OA increased by 30%
1. Coral porosis = dissolution of coral itself - disease attacks skeletons on dead coral
2. Collapses reefs, affecting ecosystems
3. Cracked therapod shells exposure to predators

19
Q

Changing weather patterns (flow on effect)

A

More heat in atmosphere increases evaporation +convection, which changes climate systems.

This affects land + ocean temp, rain/snowfall, intensified bushfires/cyclones

20
Q

Changes in glaciers, sea ice, ice sheets (flow on effect)

A

Melting glaciers:
Rising + warming sea levels, disrupted ocean circulations.
1. Destructs coastal erosion/communities, intense coastal storms

Less ice forming:
1. Decreased breeding grounds + algae = limited food supply chain
2. Reduced albedo effect = ocean salinity, coastal erosion

21
Q

Changing range of species due to rising sea
level

A

Loss of land + coastal erosion:
1. animals cannot migrate due to natural borders + threatened ecosystems die

  1. Loss of mudflats /marshes which remove habitats for invertebrates = less food supply and therefore species extinction

eg. Dugong (northern AUS)
- Relies on reduced food source (seagrass)
→ rising sea levels reduce distribution of seagrass, shrinking population

22
Q

Burning of fossil fuels

A

Caused by size of population and standard of living.
1. Power stations are coal-driven.
2. Largely used energy for transport

23
Q

Land use and land cover change

A

Agriculture uses:
1. Fertilisers
2. Ruminant animals
3. Land clearing
4.Tilling/ ploughing

All contributes to nitrous oxides and carbon dioxides in atmosphere.

24
Q

Minimisation of GHG by humans in daily lives

A
  1. Eating less meat + buying local products
  2. Electric/hybrid cars
  3. Use of public transport
25
Q

Urban design (mitigation)

A
  1. Double glazing (insulation)
  2. Efficient public transport
  3. Green buildings

Eval. of insulation:
- Reduced electricity bills
- Less air conditioner noise
- Expensive to construct
- Difficult to retrofit in exisiting homes

26
Q

Urban design (adaptation)

A
  1. Elevated houses
  2. Sea walls
  3. Light surfaces reduce albedo effect

Eval. of elevated houses:
- Money saved in long run
- Easier cleanups after floods/ avoids damage
- Expensive to implement
- Requires zoning laws/building code approval

27
Q

Geosequestration (Geo-engineering- mitigation)

A

Captures CO2 from major power stations and injects them into geological formations, locking it away.

Evaluation:
- Reduces CO2 in atmosphere
- Benefits soil quality
- Unknown long term effects
- Risk of leakage

28
Q

Solar energy/ solar panels (alternate energy sources)

A

Pros:
- Sustainable
- Little maintenance
- Lower electricity bills

Cons:
- Inconsistent energy source
- Expensive to install
- Incompatible with certain roof types

Therefore should be paired with other energy sources to meet electricity demand.

29
Q

Hydroenergy/ hydroelectric dams (alternate energy sources)

A

Generates electricity as water passes through turbine.

Pros:
- Renewable + sustainable
- High efficiency (90% vs coal at 25%)
- Reliable (can meet peak demands due to actively flowing rivers)

Cons:
- Susceptibility to drought
- May obstruct fish migration, water temps. + ecosystem around river

30
Q

Agricultural practices of Aboriginal/ Torres Strait Islander peoples

A

Mosaic burning:
Lighting low fires in small areas manually to burn underbush.
1. Opens native seeds
2. Encourages native animals to migrate then come back to new growth

Insect diet:
1. Replacement of meat- reduces carbon footprint.
2. Higher in protein
3. Bogong moth- nutritious source eaten by Aboriginals