Session 20 ( Paleoclimate) Flashcards
Paleoclimate
Measuring the earths climate prior to human existence
Climate Proxies
indirect forms of evidence to infer climate.
Commonly used proxies
- Sediments (fossils)
- Ice cores
- Tree rings
- lake varves
- coral bed rings
- Speleothems
Dendrochronology (tree rings) (1000 years)
Wider rings = more growth. Vise Versa.
Anoxic Lakes ( Varves) (Century- Millenium)
Runoff sediment composition.
Light = Mineral rich
Dark = Organic rich
Speleothens (cave dripstones) (seasonal to millennium)
formed as a part of the meteoric water cycle
Corals (100+ years)
Lighter shade show fast growth (summer) dark layers show slow growth (winter)
Ice Cores (Poles) 800,000 years
Lighter layers in summer vs darker in winter
When do Ice ages happen?
when CO2 concentrations are low
Slow Carbon Cycle
Plates shift forcing CO2 from plankton to go under volcanos making them erupt and add more CO2 back into the atmosphere
What can cause the sediments to have different colors?
Oceans became acidic from the PETM causing the color change
Paleocene–Eocene Thermal Maximum (PETM)
a period of rapid global warming caused by a massive injection of carbon into the ocean and atmosphere
What did PETM Cause
Caused rainforest to flourish but marine life struggled with intense ocean acidification causing loss in calcium.
Methane Hydrates
Crystal like cages that enclose a methane molecules thriving at low temperature and high pressure.
How did PETM affect Methane release
The intense heating of the ocean released methane into the atmosphere