Continental flood basalt weathering as a trigger for Neoproterozoic Snowball Earth
Atmospheric CO2 levels and global climate are regulated on geological timescales by the silicate weathering feedback. However, this thermostat has failed multiple times in Earth's history, most spectacularly during the Cryogenian (c. 720–635 Ma) Snowball Earth episodes. The unique middle Neopro...
| Main Authors: | , , , , , , , , , |
|---|---|
| Format: | Journal Article |
| Published: |
Elsevier BV
2016
|
| Online Access: | http://hdl.handle.net/20.500.11937/40979 |