Thursday, January 31, 2013
In a study published this month in the prestigious journal
Nature Climate Change, Frey, professor of natural resources and the
environment, finds that warmer temperatures due to climate change could cause
soils to release additional carbon into the atmosphere, thereby enhancing
climate change – but that effect diminishes over the long term. The study sheds
new light on how soil microorganisms respond to temperature and could improve
predictions of how climate warming will affect the carbon dioxide flux from
soils.
Frey and co-authors Johan Six and Juhwan Lee of the
University of California Davis and Jerry Melillo of the Marine Biological
Laboratory were curious how increased temperatures due to climate change might
alter the amount of carbon released from soils. “While they’re low on the
charisma scale, soil microorganisms are so critically important to the carbon
balance of the atmosphere,” Frey says. “If we warm the soil due to climate
warming, are we going to fundamentally alter the flux of carbon into the
atmosphere in a way that is going to feed back to enhance climate change?”
Yes, the researchers
found. And no.
The study examined the efficiency of soil organisms – how
completely they utilize food sources to maintain their cellular machinery –
depending upon the food source and the temperature under two different
scenarios. In the first short-term scenario, these researchers found that
warming temperatures had little effect on soils’ ability to use glucose, a
simple food source released from the roots of plants. For phenol, a more
complex food source common in decomposing wood or leaves, soils showed a 60
percent drop in efficiency at higher temperatures.
“As you increase temperature, you decrease the efficiency –
soil microorganisms release more carbon dioxide to the atmosphere – but only
for the more complex food sources,” Frey explains. “You could infer that as the
soil warms, more carbon dioxide will be released into the atmosphere,
exacerbating the climate problem.”
That effect diminishes, however, in the second scenario, in
which soils were warmed to 5 degrees Celsius above the ambient temperature for
18 years. “When the soil was heated to simulate climate warming, we saw a
change in the community to be more efficient in the longer term,” Frey says,
lessening the amount of carbon dioxide the soils release into the atmosphere
and, in turn, their impact on the climate. “The positive feedback response may
not be as strong as we originally predicted.”
Frey and her colleagues hypothesize that long-term warming
may change the community of soil microorganisms so that it becomes more
efficient. Organism adaptation, change in the species that comprise the soils,
and/or changes in the availability of various nutrients could result in this
increased efficiency.
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