mollwollfumble said:
> The end-Permian extinction has generally been blamed on massive volcanic eruptions that took place at the same time.
So far as I can tell, every major extinction event on the Earth has been associated with massive volcanic eruptions at about the same time, though that isn’t the only explanation for some extinctions.
Massive volcanic eruptions put so much sulfur dioxide and similar gases into the air that everything that breathes air (including ammonites, near-surface fish, plesiosaurs, non-hibernating animals, Ediacaran fauna, non-hibernating plants and fungi) suffocated.
Extreme climate change has been responsible for most mass extinctions. Why the climate actually changed can be attributed to many factors and no doubt several at the same time, not unlike the article and subject of this thread. Widespread suffocation is largely restricted to the oceans and waterways and is due to stratification and the lack of oxygen in the water column, and is probably why the ammonites and other aquatic life went extinct.
>>Oxygen depletion, is a phenomenon that occurs in aquatic environments as dissolved oxygen (DO; molecular oxygen dissolved in the water) becomes reduced in concentration to a point where it becomes detrimental to aquatic organisms living in the system. Dissolved oxygen is typically expressed as a percentage of the oxygen that would dissolve in the water at the prevailing temperature and salinity (both of which affect the solubility of oxygen in water; see oxygen saturation and underwater). An aquatic system lacking dissolved oxygen (0% saturation) is termed anaerobic, reducing, or anoxic; a system with low concentration—in the range between 1 and 30% saturation—is called hypoxic or dysoxic. Most fish cannot live below 30% saturation. A “healthy” aquatic environment should seldom experience less than 80%. The exaerobic zone is found at the boundary of anoxic and hypoxic zones.
Where hypoxia occurs
Hypoxia can occur throughout the water column and also at high altitudes as well as near sediments on the bottom. It usually extends throughout 20-50% of the water column, but depending on the water depth and location of pycnoclines (rapid changes in water density with depth). It can occur in 10-80% of the water column. For example, in a 10-meter water column, it can reach up to 2 meters below the surface. In a 20-meter water column, it can extend up to 8 meters below the surface.<<
http://en.wikipedia.org/wiki/Hypoxia_(environmental)