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Methane Release Could Cause Abrupt, Far-Reaching Climate Change
May 29, 2008An abrupt release of methane, a powerful greenhouse gas, from ice sheets that extended to Earth's low latitudes some 635 million years ago caused a dramatic shift in climate, scientists funded by the National Science Foundation (NSF) report in this week's issue of the journal Nature.
The shift triggered events that resulted in global warming and an ending of the last "snowball" ice age.
The researchers believe that the methane was released gradually at first and then very quickly from clathrates--methane ice that forms and stabilizes beneath ice sheets.
When the ice sheets became unstable, they collapsed, releasing pressure on the clathrates. The clathrates then began to de-gas.
"Our findings document an abrupt and catastrophic global warming that led from a very cold, seemingly stable climate state to a very warm, also stable, climate state--with no pause in between," said geologist Martin Kennedy of the University of California at Riverside (UCR), who led the research team.
"What we now need to know is the sensitivity of the trigger," he said. "How much forcing does it take to move from one stable state to the other--and are we approaching something like that today with current carbon dioxide warming?"
This transition "from 'snowball Earth' into a warmer period shows the compelling need for research on abrupt climate change in Earth's history," said H. Richard Lane, program director in NSF's Division of Earth Sciences. "These changes have much to tell us about the modern human-induced threat of rapid climate change."
According to Kennedy and colleagues, methane clathrate destabilization acted as a runaway feedback to increased global warming, and was the tipping point that ended the last snowball Earth. (The snowball Earth hypothesis posits that the Earth was covered from pole to pole in a thick sheet of ice for millions of years at a time.)
"Once methane was released at low latitudes from destabilization in front of the ice sheets, warming caused other clathrates to destabilize," Kennedy said. "Clathrates are held in a temperature-pressure balance of only a few degrees."
Not all of Earth's methane was released millions of years ago. Methane clathrates are present today in Arctic permafrost and beneath the oceans at continental margins; they will remain dormant, it's thought, unless triggered by warming.
This trigger is a major concern, Kennedy said, because it's possible that very little warming could unleash this trapped methane.
Uncovering the methane reservoir could potentially warm the Earth tens of degrees, he said, and the mechanism could be very rapid.
Such a fast uncovering of clathrates could have triggered a catastrophic climate and biogeochemical reorganization of the ocean and atmosphere around 635 million years ago, Kennedy believes.
The abruptness of the glacial termination, along with changes in ancient ocean chemistry and chemical deposits in the oceans, have been a challenge to climate scientists.
"The geologic deposits of this period are quite different from what we find in subsequent deglaciation," Kennedy said. "They immediately precede the first appearance of animals on Earth, suggesting some kind of environmental link."
Also called marsh gas, methane is a colorless, odorless gas. As a greenhouse gas, it is about 30 times more potent than carbon dioxide.
"Today we're conducting a global-scale experiment with Earth's climate system," Kennedy said, "and witnessing an unprecedented rate of warming, all with little or no knowledge of what instabilities lurk in the climate system and how they can influence life on Earth.
"Much the same experiment was done 635 million years ago, and the outcome is preserved in the geologic record. We see that strong forcing on the climate, not unlike the current carbon dioxide forcing, results in the activation of latent controls in the climate system that, once initiated, change climate to a completely different state."
Kennedy and colleagues collected hundreds of marine sediment samples in South Australia for stable isotope analysis, an important tool used in climate reconstruction.
The scientists found the broadest range of oxygen isotopic variation ever reported from marine sediments, which they attribute to melting waters in ice sheets as well as destabilization of clathrates by glacial meltwater.
Kennedy was joined in the study by David Mrofka of UCR and Chris von der Borch of Flinders University, Australia.
The study also was supported by grants from NASA's Exobiology Program.
The National Science Foundation (NSF)
When the ice sheets became unstable, they collapsed, releasing pressure on the clathrates. The clathrates then began to de-gas.
"Our findings document an abrupt and catastrophic global warming that led from a very cold, seemingly stable climate state to a very warm, also stable, climate state--with no pause in between," said geologist Martin Kennedy of the University of California at Riverside (UCR), who led the research team.
"What we now need to know is the sensitivity of the trigger," he said. "How much forcing does it take to move from one stable state to the other--and are we approaching something like that today with current carbon dioxide warming?"
This transition "from 'snowball Earth' into a warmer period shows the compelling need for research on abrupt climate change in Earth's history," said H. Richard Lane, program director in NSF's Division of Earth Sciences. "These changes have much to tell us about the modern human-induced threat of rapid climate change."
According to Kennedy and colleagues, methane clathrate destabilization acted as a runaway feedback to increased global warming, and was the tipping point that ended the last snowball Earth. (The snowball Earth hypothesis posits that the Earth was covered from pole to pole in a thick sheet of ice for millions of years at a time.)
"Once methane was released at low latitudes from destabilization in front of the ice sheets, warming caused other clathrates to destabilize," Kennedy said. "Clathrates are held in a temperature-pressure balance of only a few degrees."
Not all of Earth's methane was released millions of years ago. Methane clathrates are present today in Arctic permafrost and beneath the oceans at continental margins; they will remain dormant, it's thought, unless triggered by warming.
This trigger is a major concern, Kennedy said, because it's possible that very little warming could unleash this trapped methane.
Uncovering the methane reservoir could potentially warm the Earth tens of degrees, he said, and the mechanism could be very rapid.
Such a fast uncovering of clathrates could have triggered a catastrophic climate and biogeochemical reorganization of the ocean and atmosphere around 635 million years ago, Kennedy believes.
The abruptness of the glacial termination, along with changes in ancient ocean chemistry and chemical deposits in the oceans, have been a challenge to climate scientists.
"The geologic deposits of this period are quite different from what we find in subsequent deglaciation," Kennedy said. "They immediately precede the first appearance of animals on Earth, suggesting some kind of environmental link."
Also called marsh gas, methane is a colorless, odorless gas. As a greenhouse gas, it is about 30 times more potent than carbon dioxide.
"Today we're conducting a global-scale experiment with Earth's climate system," Kennedy said, "and witnessing an unprecedented rate of warming, all with little or no knowledge of what instabilities lurk in the climate system and how they can influence life on Earth.
"Much the same experiment was done 635 million years ago, and the outcome is preserved in the geologic record. We see that strong forcing on the climate, not unlike the current carbon dioxide forcing, results in the activation of latent controls in the climate system that, once initiated, change climate to a completely different state."
Kennedy and colleagues collected hundreds of marine sediment samples in South Australia for stable isotope analysis, an important tool used in climate reconstruction.
The scientists found the broadest range of oxygen isotopic variation ever reported from marine sediments, which they attribute to melting waters in ice sheets as well as destabilization of clathrates by glacial meltwater.
Kennedy was joined in the study by David Mrofka of UCR and Chris von der Borch of Flinders University, Australia.
The study also was supported by grants from NASA's Exobiology Program.
The National Science Foundation (NSF)
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Energy-saving powder
It is currently estimated that natural gas resources will be exhausted in 130 years; however, those reserves where extraction is cost-effective will only flow for another 60 years or so.
Health care accounts for 8 percent of US carbon footprint
The American health care sector accounts for nearly a tenth of the country's carbon dioxide emissions, according to a first-of-its-kind calculation of health care's carbon footprint.
Interactions with aerosols boost warming potential of some gases
For decades, climate scientists have worked to identify and measure key substances -- notably greenhouse gases and aerosol particles -- that affect Earth's climate.
Report examines hidden costs of energy production and use
A new report from the National Research Council examines and, when possible, estimates "hidden" costs of energy production and use -- such as the damage air pollution imposes on human health -- that are not reflected in market prices of coal, oil, other energy sources, or the electricity and gasoline produced from them.
Caltech researchers reveal unexpected sources of nitrogen fixation
Researchers at the California Institute of Technology (Caltech) have identified an unexpected metabolic ability within a symbiotic community of microorganisms that may help solve a lingering mystery about the world's nitrogen-cycling budget.
Arctic land and seas account for up to 25 percent of world's carbon sink
In a new study in the journal Ecological Monographs, ecologists estimate that Arctic lands and oceans are responsible for up to 25 percent of the global net sink of atmospheric carbon dioxide.
Coal-mining hazard resembles explosive volcanic eruption, study shows
Worldwide, thousands of workers die every year from mining accidents, and instantaneous coal outbursts in underground mines are among the major killers. But although scientists have been investigating coal outbursts for more than 150 years, the precise mechanism is still unknown.
Mystery Solved: Marine Microbe Is Source of Rare Nutrient
A new study of microscopic marine microbes, called phytoplankton, by researchers at Woods Hole Oceanographic Institution (WHOI) and the University of South Carolina has solved a ten-year-old mystery about the source of an essential nutrient in the ocean.
Denver to Barcelona: Global cities and greenhouse gas emissions
Denver released the largest amount of greenhouse gases (GHG) and Barcelona the smallest amount in a new study documenting how differences in climate, population density and other factors affect GHG emissions in global cities.
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