SI
SI
discoversearch

We've detected that you're using an ad content blocking browser plug-in or feature. Ads provide a critical source of revenue to the continued operation of Silicon Investor.  We ask that you disable ad blocking while on Silicon Investor in the best interests of our community.  If you are not using an ad blocker but are still receiving this message, make sure your browser's tracking protection is set to the 'standard' level.
Gold/Mining/Energy : Gold and Silver Juniors, Mid-tiers and Producers

 Public ReplyPrvt ReplyMark as Last ReadFilePrevious 10Next 10PreviousNext  
From: koan1/30/2007 10:06:47 PM
  Read Replies (1) of 78417
 
Alladen posted this to me in a Pm, but it is too good to not share:
295 million years ago 95% of all life on earth was wiped out.


Alladen: Found a likely answer I believe of a reversal mechanism, well not exactly a reversal. Looks to me like the plant life corrected things ultimately. Methane reacts with oxygen to form CO2 so plants over time could have restored the oxygen balance. No large heat increase is really evident according to this article , not enough to cause mass extinction according to this theory.. basically the big methane belch caused mass suffocation with oxygen levels lowered too much. Irrespective of heat or suffocation though the knowledge that methane converts to CO2 is the crux..

newscientist.com

Suffocation suspected for greatest mass extinction

* 09:30 09 September 2003
* NewScientist.com news service
* Jeff Hecht
The oxygen-starved aftermath of an immense global belch of methane left land animals gasping for breath and caused the Earth's largest mass extinction, suggests new research.

Greg Retallack, an expert in ancient soils at the University of Oregon in Eugene, says his theory also explains the mysterious survival of a barrel-chested reptile that became the most common animal on the planet after the end of the Permian period, 251 million years ago.

Paleontologists have long puzzled over the mass extinction at the end of the Permian. There is no evidence for a large asteroid impact, but sharp changes in carbon isotope ratios indicate something triggered massive releases of frozen methane hydrates from under the sea floor and in permafrost.

Methane is a strong greenhouse gas, and it reacts with atmospheric oxygen to produce carbon dioxide, which also would turn up the global thermostat. This dramatic climate shift has been blamed for the extinctions.

But Retallack was not convinced after working in the Karoo desert of South Africa. Fossils there show that the extinction claimed 88 per cent of late Permian genera. Yet the fossil soils he examined did not show evidence of the tremendous climate change needed for the wipe out.
Plummeting oxygen

Inspiration struck when Retallack saw a study of long-term effects of the methane release. Bob Berner of Yale University calculated that a cascade of effects on wetlands and coral reefs would have reduced oxygen levels in the atmosphere from 35 per cent to just 12 per cent in only 20,000 years - a fleeting moment in geological time.

Retallack knows the effects of low oxygen levels all too well. "I've just about died of mountain sickness at [the equivalent of] 12 per cent oxygen" while working at high altitudes, he told New Scientist. "I know exactly what it's like."

Lungs used to higher oxygen levels strain desperately for oxygen, and fill with fluid. The lack of oxygen would have left most Permian land animals gasping for breath, suffering from nausea, headaches, and inflamed lungs. Marine life would have suffocated in the oxygen-poor water.
Short nostrils

Yet the ungainly meter-long reptile Lystrosaurus survived because it had evolved to live in burrows, where oxygen levels are low and carbon dioxide levels high. It had developed a barrel chest, thick ribs, enlarged lungs, a muscular diaphragm and short internal nostrils to get the oxygen it needed. Retallack says Sherpas have developed some similar adaptations by living at high altitudes for generations.

While most Permian animals died gasping for breath, Lystrosaurus spread rapidly. In some areas, it accounts for 90 per cent of the fossils found after the extinction.

Oxygen depletion also could explain why coal swamps and coral reefs disappeared for millions of years after the extinction, says Retallack, as both are highly sensitive to oxygen levels.

He acknowledges that more work is needed to confirm his theory, and suggests looking at how Lystrosaurus changed as it spread in the post-methane world. He predicts a thick backbone would be an adaptation for low oxygen.


Reply | Delete | File
Report TOU ViolationShare This Post
 Public ReplyPrvt ReplyMark as Last ReadFilePrevious 10Next 10PreviousNext