From
the climate change denying publication 'par excellence'
Comments
from Kevin Hester that sum things up so well:
"If
there was one thing I would like NZ to learn from this speaking tour
it is that carbon is no longer in the drivers seat in this unfolding
train smash, methane is the real enemy. We all know it, it is the
general public that needs to be brought up to speed because as in the
Permian extinction it is methane that is going to get us."
Mysterious
microbes are speeding up climate change: New species is releasing
huge amounts of methane, study finds
- Scientists found the microbe in permafrost soil of northern Sweden
- The soil had begun to thaw under the effects of globally warming
- Microbes may have played a role in warming by releasing methane
- Methane gas is responsible for trapping heat in Earth's atmosphere
- Find could help scientists improve their models on climate change
24
October, 2014
Tiny
microbes hidden in the soil are one of the major amplifiers of global
warming.
But
researchers are unsure whether these microbes are slaves to their
environment or the cause of climate change.
Now,
scientists from the U.S., Sweden and Australia, claim to have
evidence that a single species of microbe found in Sweden may be
driving global warming.
Scientists
from the U.S., Sweden and Australia, claim to have shown that a
single species of microbe found in Sweden may be driving global
warming.
The
researchers installed special instruments for measuring methane
changes using Plexiglas chambers that trap the gases emanating from
the soil
The
discovery could help scientists improve their simulations of climate
change by including data on how microbes control the release of
gases, such as methane.
Earlier
this year, scientists found a single species of microbe in permafrost
soils of northern Sweden that had begun to thaw under the effect of
globally rising temperatures.
Researchers
suspected that the microbe played a role in global warming by
releasing vast amounts of carbon stored in permafrost soil close to
the Arctic Circle in the form of methane.
Methane
is a powerful greenhouse gas responsible for trapping heat in the
Earth's atmosphere.
But
the actual role of this microbe - dubbed Methanoflorens
stordalenmirensis, which roughly translates to 'methane-bloomer from
the Stordalen Mire' - was unknown.
The discovery in Sweden could help scientists improve their simulations of climate change by including data on how microbes control the release of gases, such as methane
The
international research team installed automated chambers that measure
greenhouse gases emanating from the soil as microbes metabolise
nutrients previously locked up in the permafrost soil.
The
new research pins down the role of the new microbe, finding that the
amount of Methanoflorens, should help to predict their collective
impact on future climate change.
'If
you think of the African savanna as an analogy, you could say that
both lions and elephants produce carbon dioxide, but they eat
different things,' said senior author Scott Saleska, an associate
professor at the University of Arizona.
'In
Methanoflorens, we discovered the microbial equivalent of an
elephant, an organism that plays an enormously important role in what
happens to the whole ecosystem.'
The
study revealed that because of these microbial activities, all
wetlands are not the same when it comes to methane release.
'This
has been a major shortcoming of current climate models,' said lead
author Carmody McCalley, at the University of New Hampshire.
'They
assume the wrong isotope ratio coming out of the wetlands, the models
overestimate carbon released by biological processes and
underestimate carbon released by human activities such as fossil-fuel
burning.'
To
study microbes, researchers drive cores into the ground at Abisko
National Park in northern Sweden
One
of the big questions facing climate scientists, according to
Professor Saleska, is how much of the carbon stored in soils is
released into the atmosphere by microbial activity.
'As
the "global freezer" of permafrost is failing under the
influence of warming, we need to better understand how soil microbes
release carbon on a larger, ecosystem-wide level and what is going to
happen with it,' he said.
'For
years, there's been a debate about whether microbial ecology
'matters' to what an ecosystem collectively does,' added Virginia
Rich from the University of Arizona.
'This
work shows that microbial ecology matters to a great degree, and that
we need to pay more attention to the types of microbes living in
those thawing ecosystems.'
Projected temperature change from 2081-2100. One of the big questions facing climate scientists, according to Professor Saleska, is how much of the carbon stored in soils is released into the atmosphere by microbes
Recently discovered microbe is key player in climate change
Recently
discovered microbe is key player in climate change
22
October, 2014
Tiny
soil microbes are among the world's biggest potential amplifiers of
human-caused climate change, but whether microbial communities are
mere slaves to their environment or influential actors in their own
right is an open question. Now, research by an international team of
scientists from the U.S., Sweden and Australia, led by University of
Arizona scientists, shows that a single species of microbe,
discovered only very recently, is an unexpected key player in climate
change.
The
findings, published in the journal Nature, should help scientists
improve their simulations of future climate by replacing assumptions
about the different greenhouse gases emitted from thawing permafrost
with new understanding of how different communities of microbes
control the release of these gases.
Earlier
this year, the international team discovered that a single species of
microbe, previously undescribed by science, was prominent in
permafrost soils in northern Sweden that have begun to thaw under the
effect of globally rising temperatures. Researchers suspected that it
played a significant role in global warming by liberating vast
amounts of carbon stored in permafrost soil close to the Arctic
Circle in the form of methane, a powerful greenhouse gas trapping
heat in the Earth's atmosphere. But the actual role of this
microbe—assigned the preliminary name Methanoflorens
stordalenmirensis, which roughly translates to "methane-bloomer
from the Stordalen Mire"—was unknown.
The
new research nails down the role of the new microbe, finding that the
sheer abundance of Methanoflorens, as compared to other microbial
species in thawing permafrost, should help to predict their
collective impact on future climate change.
"If
you think of the African savanna as an analogy, you could say that
both lions and elephants produce carbon dioxide, but they eat
different things," said senior author Scott Saleska, an
associate professor in the UA's Department of Ecology and
Evolutionary Biology and director of the UA's new Ecosystem Genomics
Institute. "In Methanoflorens, we discovered the microbial
equivalent of an elephant, an organism that plays an enormously
important role in what happens to the whole ecosystem."
Significantly,
the study revealed that because of these microbial activities, all
wetlands are not the same when it comes to methane release.
"The
models assume a certain ratio between different forms, or isotopes,
of the carbon in the methane molecules, and the actual recorded ratio
turns out to be different," said lead author Carmody McCalley, a
scientist at the Earth Systems Research Center at the University of
New Hampshire who conducted the study while she was a postdoctoral
researcher at UA.
"This has been a major shortcoming of current
climate models. Because they assume the wrong isotope ratio coming
out of the wetlands, the models overestimate carbon released by
biological processes and underestimate carbon released by human
activities such as fossil-fuel burning."
Soil
microbes can make methane two different ways: either from acetate, an
organic molecule that comes from plants, or from carbon dioxide and
hydrogen.
"Both
processes produce energy for the microbe, and the microbe breathes
out methane like we breathe out carbon
dioxide,"
McCalley said.
"But we find that in thawing permafrost, most
methane initially doesn't come from acetate as previously assumed,
but the other pathway. This ratio then shifts towards previous
estimates as the frozen soils are turned into wetlands and acetate
becomes the preferred carbon source."
One
of the big questions facing climate scientists, according to Saleska,
is how much of the carbon stored in soils is released into the
atmosphere by microbial activity.
"As
the 'global freezer' of permafrost is failing under the influence of
warming, we need to better understand how soil microbes
release carbon on
a larger, ecosystem-wide level and what is going to happen with it,"
he said.
Said
UA co-author Virginia Rich: "For years, there's been a debate
about whether microbial ecology 'matters' to what an ecosystem
collectively does—in this case, releasing greenhouse gases of
different forms—or whether microbes are just slaves to the system's
physics and chemistry. This work shows that microbial ecology matters
to a great degree, and that we need to pay more attention to the
types of microbes living in those thawing ecosystems."
Added
McCalley: "By taking microbial ecology into account, we can
accurately set up climate models to identify how much methane comes
from thawing permafrost versus other sources such as fossil-fuel
burning."
More
information: 'Methane
dynamics regulated by microbial community response to permafrost
thaw' Nature , 23 October 2014. DOI:
10.1038/nature13798
This is not entirely new. This is from the University of Queensland, in February
Newly discovered microbe holds key to global warming
Scientists
from The University of Queensland have discovered a microbe that is
set to play
19
February, 2014
UQ's
Australian Centre for Ecogenomics researcher Ben Woodcroft said the
methane-producing micro-organism, known as a ‘methanogen’, was
thriving in northern Sweden’s thawing permafrost in a thick
subsurface layer of soil that has previously remained frozen.
Mr Woodcroft said no one knew of the microbe’s existence or how it worked before the research discovery.
Mr Woodcroft said no one knew of the microbe’s existence or how it worked before the research discovery.
He
said global warming trends meant vast areas of permafrost would
continue to thaw, allowing the microbes to flourish in organic matter
and drive methane gas release, which would further fuel global
warming.
“The micro-organism generates methane by using carbon dioxide and hydrogen from the bacteria it lives alongside,” Mr Woodcroft said.
“The micro-organism generates methane by using carbon dioxide and hydrogen from the bacteria it lives alongside,” Mr Woodcroft said.
Lead
researcher and UQ’s Australian Centre for Ecogenomics Deputy
Director Associate Professor Gene Tyson said the findings were
significant.
“This
micro-organism is responsible for producing a substantial fraction of
methane at this site,” he said.
“Methane
is a potent greenhouse gas with about 25 times the warming capacity
of carbon dioxide.”
The researchers showed the organism and its close relatives live not just in thawing permafrost but in many other methane-producing habitats worldwide.
The team made the discovery by using DNA from soil samples and reconstructing a near-complete genome of the microbe, bypassing traditional methods of cultivating microbes in the lab.
The researchers showed the organism and its close relatives live not just in thawing permafrost but in many other methane-producing habitats worldwide.
The team made the discovery by using DNA from soil samples and reconstructing a near-complete genome of the microbe, bypassing traditional methods of cultivating microbes in the lab.
The
‘Discovery of a novel methanogen prevalent in thawing permafrost’
research is published here in
the journal Nature Communications.
PhD candidate Rhiannon Mondav who is student of UQ and Uppsala University based in Sweden, co-authored the paper alongside ACE researchers and international collaborators.
The work was funded by the United States Department of Energy Office of Biological and Environmental Research’s Genomic Science Program and the Australian Research Council.
PhD candidate Rhiannon Mondav who is student of UQ and Uppsala University based in Sweden, co-authored the paper alongside ACE researchers and international collaborators.
The work was funded by the United States Department of Energy Office of Biological and Environmental Research’s Genomic Science Program and the Australian Research Council.
Media:
ACE Deputy Director Associate Professor Gene Tyson,
07 3365
3829,g.tyson@awmc.uq.edu.au or
UQ Faculty of Science Communications Officer Monique Nevison, 07
3346 4129, m.nevison@uq.edu.au.
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