Chapter 17: Phanerozoic Eon Flashcards
1
Q
Characteristics of the Cambrian Period 542-488mya
A
- Rodinia
- Life was only in the sea, not on land (species evolve quickly)
- Extinction in this time was due to competition, glacial cooling, oxygen depletion
2
Q
Characteristics of the Ordovician Period 488-444mya
A
- Gondwana covered in glaciers
- Lots of volcanoes due to subduction= CO2
- Greenhouse period, sudden short lived intense glaciations ended the greenhouse conditions
- Life flourished
- 2 extinction events
- In the end, all the glaciers sucked up the water, niches eliminated
3
Q
Characteristics of the Silurian Period 444-416mya
A
- Still ice sheets
- Higher sea levels and more abundant warm shallow seas
- Greenhouse period
- Sea life moved onto land
4
Q
Characteristics of the Devonian period 416-359 mya
A
- Europe, NA and Asia all joined
- Some glaciers
- CO2 consumed fast by growing forests (cooling)
- The age of fish, developed strong lungs and could crawl in and out of water
- Plants developed seeds
- 370 extinction caused by an asteroid
- 360 extinction caused by anoxia due to algal decay
5
Q
Characteristics of the Carboniferous period 359-299 mya
A
- Icehouse, glaciation= low sea levels
- Production of the largest coal deposits ever made
- fish evolved into amphibians
- Mild extinctions due to climate and sea level issues
6
Q
Characteristics of the Permian period 299-251 mya
A
- Pangea formed
- Rich in marine and terrestrial life
- Conifer trees evolved
- Lizard-like creatures dominated + diversified
- Oxygen catastrophe ????
7
Q
Characteristics of the Triassic Period 251-201.6 mya
A
- Pangea slowly drifting apart creating new oceans+ shallow water environments
- No glaciation
- Age of the reptiles
- ended the period with one mass extinction due to anoxic events
8
Q
Characteristics of the Jurassic Period 201.6-145.5 mya
A
- More spreading center volcanism= more CO2, strengthening the greenhouse
- no glaciation
- Warm oceans= plankton devlopped
- Golden age for dinos
9
Q
Characteristics of the Cretaceous period 145.5-65.5 mya
A
- Pangea was broken up
- Chalky because of all the shell organisms
- Worlds largest petroleum deposit formed by marine organisms
10
Q
Characteristics of the Cenozoic Era 65.5-Now
Tertiary period 65.5-2.6 mya
A
- Fragments continue to drift away
- heading towards an Icehouse
- Reptile were replaced by mammals after the extinction
- Most of the vegetation was burned= great fertilizer for plants to flourish
- PETM event casued 35-50% loss of marine species
11
Q
Characteristics of the Quaternary period 2.6-Now
A
- Icehouse
- Holocene mass extinction is widespread and on going