Helmholtz Association of
German Research Centres
20
March, 2019
Methane
(CH4) is a potent greenhouse gas that is roughly 30 times more
harmful to the climate than carbon dioxide (CO2). Both gases are
produced in thawing permafrost as dead animal and plant remains are
decomposed. However, methane is only formed if no oxygen is
available. Until now, it was assumed that larger amounts of
greenhouse gases are formed when the ground was dry and well
aerated—when oxygen was available. Christian Knoblauch and his
colleagues have now demonstrated that water-saturated permafrost
soils without oxygen can be twice as harmful to the climate as dry
soils—which means the role of methane has been greatly
underestimated.
Knoblauch
has, for the first time, measured and quantified in the laboratory
the long-term production of methane in thawing permafrost. The team
had to wait for three years before the approximately 40,000 year-old
samples from the Siberian Arctic finally produced methane. The team
observed the permafrost for a total of seven years, an unprecedented
long-term study.
They
found that without oxygen, equal amounts of methane and CO2 are
produced. But since methane is a far more potent
greenhouse gas,
it is more significant. Because methane
production couldn't
be measured, it was assumed that in the absence of oxygen only very
small amounts of it can be formed. "It takes an extremely long
time until stable methane-producing microorganisms develop in thawing
permafrost," explains Knoblauch. "That's why it was so
difficult to demonstrate methane production until now."
"By
combining process-based and molecular-microbiological methods, our
study shows for the first time that the methane-forming
microorganisms in the thawing permafrost have significant influence
on the greenhouse gas budget," adds co-author Susanne Liebner
from the Helmholtz Center Potsdam—GFZ German Research Center for
Geosciences.
The
team has used the new data to improve a computer model that estimates
how much greenhouse
gas is
produced in permafrost in the long term—and they've compiled a
first forecasts. According to the scientists: The permafrost soils of
Northern Europe, Northern Asia and North America could produce up to
1 gigaton of methane and
37 gigatons of carbon
dioxide by
2100. But there are uncertainties. To what depth will the soil
actually thaw by then? Will it be wet or dry? One thing, however, is
certain: the new
data will
enable more accurate predictions about the impacts of thawing
permafrost on our climate.
More
information: Knoblauch
C, Beer C, Liebner S, Grigoriev M N, Pfeiffer E-M (2018): Methane
production as key to the greenhouse gas budget of thawing
permafrost; Nature
Climate Change, DOI:
10.1038/s41558-018-0095-z
Provided
by: Helmholtz Association of German Research Centres
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