100-50mya
Cretaceous period
- ‘green Antarctica’ separates from Pangea and starts to move south
50mya
Paleocene/Ecocene thermal maximum
- no ice caps at poles
- Indian and Eurasian pates collide
35mya
30mya
20mya
10mya
-further cooling from erosion of the Himalayas locking up carbon in deepsea sediments
6mya
Messinian salinity crisis
- strait of Gibraltar closes
- Gulf stream slows down due to lack of saline input from the Mediterranean
- Atlantic much colder
5.3mya
4.5mya
2.5mya
800,000ya
Mid-Pleistocene transition
- 41,000yr glacial-interglacial cycle switches to 100,000yr cycle
- larger ice sheets mean more of a stimulus is needed to switch between glacial and interglacial, but they are more unstable, meaning the cycle is more intense and changes are more rapid
21,000ya
10,000ya to now
7,000ya
5,000ya
4,200ya