Module 7 Flashcards
Pollen grains in sedimentary rock (AE)
- 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
Rock types and formations (AE)
- Vast chalk deposit in White Desert at Farafra depression
- Chalk- limestone composed of calcite
- Process of glaciation
- Surface exposure dating
Fossils and microfossils (AE)
- Fossil reefs, stromatolites, limestone deposits, Ediacaran fossils and sand ripples found in Australia.
- In SA, Cambrian limestone in Normanville on Fleurieu Peninsula.
Changing isotope ratios in rocks and deep sea sediments (AE)
- O-16 evaporates first into atmosphere = tropic oceans rich in O-18 molecules
- O-18 molecules precipitate/condense at lower, mid latitudes
- Evaporated O-16 molecules travel via clouds towards pole, then precipitates as snow
- O-16 trapped in glaciers during cooler periods
- When climate becomes warmer, O-16 rich glaciers melt back into the ocean, increasing ratio of O-16:O-18
Ice cores (RE)
Warmer periods = more O-18 isotopes in frozen H2O = changes in snow fall from high to lower levels
- Winter seasons indicated by darker layers in ice core
- Summer is indicated by lighter layers
Dendrochronology (RE)
- 1 ring = 1 year of growth in an oak tree
- Scarring in rings = fires
- Disfigured rings = uneven growth from lack of sunlight
- Measure rings across several trees to reveal matching patterns (cross-dating)
Dendrochronology 2 (RE)
- Growth directly affected by surrounding conditions
- Indicates seasons in which growth was poorer/better helping infer climate conditions
- Captures climate conditions from periods older than tree life
Aboriginal art sites (RE)
- Now extinct species/environments recorded in form of rock painting
- Aboriginals in Aus for 50,000 years > - witnesses to changes in climates, ecosystems, native animals
- Art sites preserve iconic megafauna eg. Procoptodon
Human instrument records (RE)
- Thermometers measure atmospheric temperature
- Models predict effects of future climate change
- In past decade, human record of predictions have nearly all come true (most accurate form of data)
Changing isotope ratios in coral (RE)
- Calcium carbonate layers in their growth- rate read to show salinity, pH, temp
- Skeletal cores in UV/X-ray captures differences in growth rates through coral life
- Increasing pH creates stress by eating away at skeleton
Stalactites
Hanging in ceiling
Stalagmites
Growing from ground up
Isotope ratios in stalactites and stalagmites (RE)
Sampling their O:16-O:18 ratio provides info on their temp + growth rates reflect rainfall activity
Natural greenhouse effect
Some solar energy reflected back into space, some absorbed by GHG- this traps heat to warm atmosphere. This:
- Regulates average temp. to allow survival.
- Temp influenced by ice ages, interglacial periods every 100,000 years
Anthropogenic greenhouse effect
Fossil fuels, agriculture, growing populations
^^ increases GHG levels in atmosphere
- Temp rise by approx. 0.7 degrees since 20th century
- Increased ozone creates smog in city +blocks UV radiation