### Models of the Cryogenian Glaciations
During the Cryogenian period (approximately 720 to 635 million years ago), Earth experienced widespread, severe glaciations. Geologists have proposed two models to explain the extent of the ice coverage.
Model 1 (Hard Snowball Earth)
This model asserts that glaciers reached the equator, and the entire surface of Earth's oceans was completely frozen over with ice sheets up to 1 kilometer thick. This global ice cover decoupled the oceans from the atmosphere, halting the hydrological cycle (evaporation and precipitation) and severely restricting photosynthesis due to the lack of sunlight penetrating the thick ice. According to Model 1, the glaciation ended only when carbon dioxide () released by volcanic outgassing accumulated in the atmosphere to extremely high levels (approximately 350 times modern levels), creating a massive greenhouse effect that rapidly melted the ice.
Model 2 (Slushball Earth)
This model asserts that while glaciers were widespread at high and middle latitudes, Earth was not completely frozen. A band of open water, or extremely thin sea ice, persisted around the equator. As a result, the hydrological cycle continued to function, albeit at a reduced rate. Marine photosynthetic microorganisms survived in these open equatorial waters. According to Model 2, the accumulation of from volcanic outgassing was also responsible for ending the glaciation, but the required concentration of to initiate melting was significantly lower because the albedo (reflectivity) of open water is much lower than that of solid ice.
Based on the passage, Model 1 and Model 2 agree on which of the following aspects of the Cryogenian glaciations?
- Volcanic outgassing was the primary driver that led to the termination of the glaciations.Cevap
- BThe thickness of the ice sheets covering the equatorial regions of Earth's oceans.
- CThe complete suspension of the global hydrological cycle during the glacial periods.
- DThe specific concentration of atmospheric carbon dioxide needed to initiate global melting.