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Related: About this forumOn warmer Earth, most of Arctic may remove, not add, methane (ISME Journal)
https://blogs.princeton.edu/research/2015/08/14/on-warmer-earth-most-of-arctic-may-remove-not-add-methane-isme-journal/[font face=Serif][font size=5]On warmer Earth, most of Arctic may remove, not add, methane (ISME Journal)[/font]
Posted on August 14, 2015
By Morgan Kelly, Office of Communications
[font size=3]In addition to melting icecaps and imperiled wildlife, a significant concern among scientists is that higher Arctic temperatures brought about by climate change could result in the release of massive amounts of carbon locked in the regions frozen soil in the form of carbon dioxide and methane. Arctic permafrost is estimated to contain about a trillion tons of carbon, which would potentially accelerate global warming. Carbon emissions in the form of methane have been of particular concern because on a 100-year scale methane is about 25-times more potent than carbon dioxide at trapping heat.
However, new research led by Princeton University researchers and published in The ISME Journal in August suggests that, thanks to methane-hungry bacteria, the majority of Arctic soil might actually be able to absorb methane from the atmosphere rather than release it. Furthermore, that ability seems to become greater as temperatures rise.
The researchers found that Arctic soils containing low carbon content which make up 87 percent of the soil in permafrost regions globally not only remove methane from the atmosphere, but also become more efficient as temperatures increase. During a three-year period, a carbon-poor site on Axel Heiberg Island in Canadas Arctic region consistently took up more methane as the ground temperature rose from 0 to 18 degrees Celsius (32 to 64.4 degrees Fahrenheit). The researchers project that should Arctic temperatures rise by 5 to 15 degrees Celsius over the next 100 years, the methane-absorbing capacity of carbon-poor soil could increase by five to 30 times.
The researchers found that this ability stems from an as-yet unknown species of bacteria in carbon-poor Arctic soil that consume methane in the atmosphere. The bacteria are related to a bacterial group known as Upland Soil Cluster Alpha, the dominant methane-consuming bacteria in carbon-poor Arctic soil. The bacteria the researchers studied remove the carbon from methane to produce methanol, a simple alcohol the bacteria process immediately. The carbon is used for growth or respiration, meaning that it either remains in bacterial cells or is released as carbon dioxide.
[/font][/font]
Posted on August 14, 2015
By Morgan Kelly, Office of Communications
[font size=3]In addition to melting icecaps and imperiled wildlife, a significant concern among scientists is that higher Arctic temperatures brought about by climate change could result in the release of massive amounts of carbon locked in the regions frozen soil in the form of carbon dioxide and methane. Arctic permafrost is estimated to contain about a trillion tons of carbon, which would potentially accelerate global warming. Carbon emissions in the form of methane have been of particular concern because on a 100-year scale methane is about 25-times more potent than carbon dioxide at trapping heat.
However, new research led by Princeton University researchers and published in The ISME Journal in August suggests that, thanks to methane-hungry bacteria, the majority of Arctic soil might actually be able to absorb methane from the atmosphere rather than release it. Furthermore, that ability seems to become greater as temperatures rise.
The researchers found that Arctic soils containing low carbon content which make up 87 percent of the soil in permafrost regions globally not only remove methane from the atmosphere, but also become more efficient as temperatures increase. During a three-year period, a carbon-poor site on Axel Heiberg Island in Canadas Arctic region consistently took up more methane as the ground temperature rose from 0 to 18 degrees Celsius (32 to 64.4 degrees Fahrenheit). The researchers project that should Arctic temperatures rise by 5 to 15 degrees Celsius over the next 100 years, the methane-absorbing capacity of carbon-poor soil could increase by five to 30 times.
The researchers found that this ability stems from an as-yet unknown species of bacteria in carbon-poor Arctic soil that consume methane in the atmosphere. The bacteria are related to a bacterial group known as Upland Soil Cluster Alpha, the dominant methane-consuming bacteria in carbon-poor Arctic soil. The bacteria the researchers studied remove the carbon from methane to produce methanol, a simple alcohol the bacteria process immediately. The carbon is used for growth or respiration, meaning that it either remains in bacterial cells or is released as carbon dioxide.
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On warmer Earth, most of Arctic may remove, not add, methane (ISME Journal) (Original Post)
OKIsItJustMe
Aug 2015
OP
Agnosticsherbet
(11,619 posts)1. Great article and an interesting bit of science.
OKIsItJustMe
(19,938 posts)2. I found it interesting
I love findings which overturn conventional wisdom.
Fred Sanders
(23,946 posts)3. Interesting science, but not at all the magic bullet it may seem, for the earth or global warming...no research on that.
At our study sites, we are more confident that these soils will continue to be a sink under future warming. In the future, the Arctic may not have atmospheric methane increase as much as the rest of the world, Lau said. We dont have a direct answer as to whether these Arctic soils will offset global atmospheric methane or not, but they will certainly help the situation.
And of course Arctic methane increase is not the only source of carbon dioxide and global warming.
Agnosticsherbet
(11,619 posts)4. If we can come to understand it, and use it, then it is one tool
in the toolbox we will need to handle these problems.
OKIsItJustMe
(19,938 posts)5. No, of course not.
The researchers project that should Arctic temperatures rise by 5 to 15 degrees Celsius over the next 100 years, the methane-absorbing capacity of carbon-poor soil could increase by five to 30 times.