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			by Jonathan Benson 
			December 22, 2011  
			from
			
			NaturalNews Website 
			  
			  
			When a Russian team recently stumbled upon a few methane "fountains" 
			releasing large amounts of methane gas from shallow arctic waters 
			directly into the atmosphere, they had no idea that there were 
			hundreds, if not thousands, more.
 
			  
			The
			
			UK's Daily Mail reports that the 
			Russian research vessel Academician Lavrentiev has identified at 
			least 100 large methane plumes in the East Siberian Arctic Shelf 
			that are
			
			releasing high amounts of the methane gas 
			into the environment. 
				
				"We found more than 100 fountains, 
				some more than a kilometer (just over three-fifths of a mile) 
				across," said Dr. Igor Semiletov, who was involved in the 
				discovery.    
				"These are methane fields on a scale 
				not seen before. The emissions went directly into the 
				atmosphere." 
			Under normal circumstances, methane 
			leaks deep in the ocean oxidize long before they reach the surface.
			 
			  
			Microbes in both marine and freshwater 
			sediments convert methane into carbon dioxide on its way up to the 
			ocean surface. But since the area where the methane fountains have 
			been discovered is in relatively shallow water, there is not enough 
			time for this conversion to take place.
 According to the National 
			Science Foundation (NSF), methane gas is 30 times more potent, 
			gram for gram, than carbon dioxide in affecting the climate.
 
			  
			If true, this means that continuous, 
			high-level releases of this gas from melting "permafrost" under the 
			sea has the potential to rapidly alter normal climate conditions - 
			and there really is nothing anyone can do about it. 
				
				"Earlier we found torch or 
				fountain-like structures like this," added Semiletov about prior 
				methane release discoveries in the area. "This is the first time 
				that we've found continuous, powerful and impressive seeping 
				structures, more than 1,000 meters (about 3,280 feet) in 
				diameter. It's amazing." 
			On the flip side, some question the 
			validity of the theory that methane contributes to climate 
			change on any significant level, alleging that, like carbon 
			dioxide, it is not much of a threat to the planet.  
			  
			Research conducted by Dr. Joel 
			Kauffman, Emeritus Professor of Chemistry at The University of 
			the Sciences in Philadelphia, for instance,
			
			actually found that methane is 
			not really the active "greenhouse gas" that some claim it is.
 
 
			
 
 
 
 
 
 
 
			  
			  
			
 
			-  
			
			A Greenhouse Gas 30 times More Potent Than 
			Carbon Dioxide   - 
			
			
			'Fountains' of Methane 
			...1,000m 
			Across Erupt from Arctic Ice 
			13 December 2011 
			from
			
			DailyMail Website
 
				
					
						| 
						'Methane fields on a scale 
						not seen before'.More than 100 fountains, but could be 'thousands'.
 Could cause rapid climate change.
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 The Russian research vessel Academician Lavrentiev conducted a 
			survey of 10,000 square miles of sea off the coast of eastern 
			Siberia.
 
 They made a terrifying discovery - huge plumes of methane bubbles 
			rising to the surface from the seabed.
 
				
				'We found more than 100 fountains, 
				some more than a kilometer across,' said Dr Igor Semiletov, 
				'These are methane fields on a scale not seen before. The 
				emissions went directly into the atmosphere.' 
			
			 
			Far East Siberia 
			The melting of 
			'permafrost' under the sea has led 
			to huge releases of 
			methane - far more abrupt and intense than anything on land
 
			Earlier research conducted by 
			Semiletov's team had concluded that the amount of methane currently 
			coming out of the East Siberian Arctic Shelf is comparable to the 
			amount coming out of the entire world’s oceans.
 Now Semiletov thinks that could be an underestimate.
 
 The melting of the arctic shelf is melting 'permafrost' under the 
			sea, which is releasing methane stored in the seabed as methane gas. 
			These releases can be larger and more abrupt than any land-based 
			release.
 
			  
			The East Siberian Arctic Shelf is a 
			methane-rich area that encompasses more than 2 million square 
			kilometers of seafloor in the Arctic Ocean. 
			  
			
			 
			Methane bubbles 
			trapped in ice 
			Normally, bubbles 
			from the seabed turn into carbon dioxide before reaching the 
			surface, 
			but the East Siberian 
			Arctic Shelf is so shallow the methane travels directly into the 
			atmosphere 
				
				'Earlier we found torch or fountain-like structures like this,' 
				Semiletov told the Independent. 'This is the first time that 
				we've found continuous, powerful and impressive seeping 
				structures, more than 1,000 meters in diameter. It's amazing.'
 
 'Over a relatively small area, we found more than 100, but over 
				a wider area, there should be thousands of them.'
 
			Semiletov's team used seismic and 
			acoustic monitors to detect methane bubbles rising to the surface.
 Scientists estimate that the methane trapped under the ice shelf 
			could lead to extremely rapid climate change. Current average 
			methane concentrations in the Arctic average about 1.85 parts per 
			million, the highest in 400,000 years. Concentrations above the East 
			Siberian Arctic Shelf are even higher.
 
 The shelf is shallow, 50 meters or less in depth, which means it has 
			been alternately submerged or above water, depending on sea levels 
			throughout Earth’s history.
 
 During Earth’s coldest periods, it is a frozen arctic coastal plain, 
			and does not release methane.
 
 As the planet warms and sea levels rise, it is inundated with 
			seawater, which is 12-15 degrees warmer than the average air 
			temperature.
 
 In deep water, methane gas oxidizes into carbon dioxide before it 
			reaches the surface. In the shallows of the East Siberian Arctic 
			Shelf, methane simply doesn’t have enough time to oxidize, which 
			means more of it escapes into the atmosphere.
 
 That, combined with the sheer amount of methane in the region, could 
			add a previously uncalculated variable to climate models.
 
 
			  
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