W3: L13 = Palaeozoology [Palaeontology Introduction] (Prof. Shaw) Flashcards
Palaeoecology?
= study of the past interactions between organisms & their environments.
Palaeoecology attributes? (3)
- Reconstructs ancient ecosystems.
- Integrates biology, geology & ecology to understand past life forms.
- Helps predict future environmental changes.
Fossil record attributes? (2)
- Provides ancient biodiversity, evolutionary patterns & extinct species’ behaviours.
- Reconstructs ancient environments & understand ecological dynamics.
Dating methods/techniques? (3)
- Radiometric dating.
- Stratigraphy.
- Biostratigraphy.
Radiometric dating?
= decay of isotopes to determine age of rocks & fossils.
Stratigraphy?
= sedimentary layers to understand sequence of geological events.
Biostratigraphy?
= fossil distribution within rock layers to correlate & date strat.
What do these dating methods help with?
They help build chronological frameworks.
Palaeoclimate?
= reveal past climates by analysing geological & biological proxies like ice cores & tree rings.
Palaeoclimate attributes? (3)
- Provide data on temperature, rainfall & atmospheric composition.
- How ecosystems & life forms responded to climate changes.
- Predict how current climate change might affect future ecosystems.
Use of extinction events/What do they help us with? (2)
- Understand the causes & consequences of widespread biodiversity loss.
- Inform conservation efforts by highlighting patterns & triggers of extinction.
What do ancient flora help us with? (3)
- Evolution of flora & their role in shaping ecosystems.
- Early plants pave way for development of complex environments.
- Understand the adaptibility & spread of vegetation over geological time.
Ancient flora?
= fossilised plants.
What do ancient fauna help us with? (2)
- Show diversity & evolution of ancient fauna.
- Examining skeletons & footprints reveals evolution, behaviour & habitat of extinct species.
What do sediment analysis show us? (2)
- Past climatic conditions, vegetation & animal life.
- Chemical composition, grain size & isotopic content of sediments help to infer past environments.