Thawing microbes could control the climate

As the Arctic permafrost melts over the coming decades, long-frozen 
microorganisms will thaw out and start feasting on the soil. The first have 
already begun to wake up – and early signs are that they will have a major 
impact on how Earth's climate changes.

As the Arctic 
permafrost<http://www.newscientist.com/article/mg18925374.500-arctic-permafrost-set-to-disappear-over-next-century.html>
 thaws, runaway global 
warming<http://www.newscientist.com/article/mg19125713.300-climate-change-one-degree-and-were-done-for.html>
 may ensue, because the huge amounts of organic 
carbon<http://www.newscientist.com/article/mg20026855.000-arctic-tundra-releases-annual-methane-burp.html>
 the permafrost contains will escape into the 
atmosphere<http://www.newscientist.com/article/mg20127011.500-arctic-meltdown-is-a-threat-to-humanity.html>.

To find out how the permafrost's microorganisms will respond to a thaw, Janet 
Jansson<http://esd.lbl.gov/about/staff/janetjansson/> of the Lawrence Berkeley 
National Laboratory in Berkeley, California, and colleagues collected three 
cores from permafrost soil in central Alaska. Back in the lab, they thawed 
samples of each core and kept them at 5 °C. For the first two days the melting 
ice released lots of methane that had been trapped when it formed, but the rate 
then quickly dropped.

That's because soil microorganisms thawed out, and although some began making 
methane that added to the emissions, others consumed it and converted it into 
carbon dioxide instead. "It's a very rapid response," Jansson says. Her team 
took samples of DNA from the permafrost as it warmed up, allowing them to track 
how the microbial population changed.

Many studies have examined the gases that escape from thawing permafrost, but 
we knew little about how the microbes within influence the process, says Torben 
Christensen<http://lucci.lu.se/people_christensen.html> of Lund University in 
Sweden. The permafrost ecosystem is almost entirely unexplored. "Most of the 
microorganisms in permafrost have never been cultivated, and more than 90 per 
cent are unidentified," Jansson says.

Chilly microbes

Methane is a stronger greenhouse gas than 
CO2<http://www.newscientist.com/article/dn17625-as-arctic-ocean-warms-megatonnes-of-methane-bubble-up.html>,
 although it does not stay in the atmosphere as long. Jansson says a release of 
CO2 is still bad news, but preferable to methane.

It's long been known that methane-munching microorganisms will get to work in 
thawing permafrost, Christensen says. "At least 50 per cent of the gross 
production of methane will be oxidised." In other words, consumed.

The question is, will the methane-eaters be able to consume the bulk of the gas 
once the permafrost starts melting in a big way? Christensen says that will 
depend on what happens to the water table. Higher water tables mean more 
methane and fewer microorganisms to eat it, while lower water tables mean the 
opposite.

No laughing matter

Also adding to our worries are indications that thawing permafrost may release 
large quantities of nitrous oxide<http://dx.doi.org/10.1038/ngeo803> – aka 
laughing gas – which is an even more powerful greenhouse gas than 
methane<http://www.newscientist.com/article/mg19125695.000-nitrous-oxide--no-laughing-matter-for-forests.html>,
 and damages the ozone 
layer<http://www.newscientist.com/article/dn17698-laughing-gas-is-biggest-threat-to-ozone-layer.html>
 into the bargain.

As the team's permafrost samples thawed they saw no boost in the levels of 
microbes that produce nitrous oxide reductase, an enzyme that converts nitrous 
oxide into harmless nitrogen. Without this boost, the nitrous oxide could 
escape.

Christensen has set up a monitoring system to track greenhouse gas emissions 
from thawing permafrost, and is increasingly tracking nitrous oxide as well as 
CO2 and methane. "It may be a player," he says.

Journal reference: Nature<http://www.nature.com/nature/index.html>, DOI: 
10.1038/nature10576

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