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Climate change enhancing soil respiration
The vast reservoir of carbon stored beneath our feet is entering Earth's atmosphere at an increasing rate, most likely as a result of warming temperatures, suggest observations collected by a team of US-scientists from a variety of the Earth's many ecosystems.
In a study published in Nature on the 2nd August, US scientists of the Pacific Northwest National Laboratory, Richland, and the University of Maryland show that this process is speeding up as Earth warms and is happening faster than plants are taking in carbon through photosynthesis. The team found that the rate at which microbes are transferring carbon from soil to the atmosphere has increased by 1.2 per cent over a 25-year period, from 1990 to 2014.
While that may not seem like a big change, such an increase on a global scale, in a relatively short period in Earth history, is massive. The finding, based on thousands of observations made by scientists at hundreds of sites around the globe, is consistent with the predictions that scientists have made about how Earth might respond to warmer temperatures.
Findings are based on studies from around the globe
"It's important to note that this is a finding based on observations in the real world. This is not a tightly controlled lab experiment," said first author Ben Bond-Lamberty of the Joint Global Change Research Institute, a partnership between the US Department of Energy's Pacific Northwest National Laboratory and the University of Maryland.
Globally, soil holds about twice as much carbon as Earth's atmosphere. In a forest where stored carbon is manifest in the trees above, even more carbon resides unseen underfoot. The fate of that carbon will have a big impact on our planet. Will it remain sequestered in the soil or will it enter the atmosphere as carbon dioxide, further warming the planet?
To address the question, the team relied heavily on two global science networks as well as a variety of satellite observations. The Global Soil Respiration Database includes data on soil respiration from more than 1,500 studies around the globe. And FLUXNET draws data from more than 500 towers across the world that record information about temperature, rainfall and other factors.
"Most studies that address this question look at one individual site which we understand very well," said author Vanessa Bailey, a soil scientist at the Pacific Northwest National Laboratory. "This study asks the question on a global scale. We're talking about a huge quantity of carbon. Microbes exert an outsize influence on the world that is very hard to measure on such a large scale."
Rising “soil respiration”
The study focused on a phenomenon known as "soil respiration," which describes how microbes and plants in the soil take in substances like carbon to survive, and then give off carbon dioxide. Soils don't exactly breathe, but as plants and microbes in soil take in carbon as food, they convert some of it to other gases which they give off –much like we do when we breathe.
Scientists have known that as temperatures rise, soil respiration increases. Bond-Lamberty's team sought to compare the roles of the two main contributors, increased plant growth and microbial action.
The team discovered a growing role for microbes, whose action is outstripping the ability of plants to absorb carbon. In the 25-year span of the study, the proportion of soil respiration that is due to microbes increased from 54 to 63 per cent. Warmer temperatures can prompt more microbial action, potentially resulting in more carbon being released from carbon pools on land into the air.
"We know with high precision that global temperatures have risen," said Bond-Lamberty. "We'd expect that to stimulate microbes to be more active. And that is precisely what we've detected. Land is thought to be a robust sink of carbon overall, but with rising soil respiration rates, you won't have an intact land carbon sink forever."
Ben Bond-Lamberty, Vanessa L. Bailey, Min Chen, Christopher M. Gough, Rodrigo Vargas. Globally rising soil heterotrophic respiration over recent decades. Nature, 2018; 560 (7716): 80 DOI: 10.1038/s41586-018-0358-x
The Pacific Northwest National Laboratory, Richland, USA
The University of Maryland, Baltimore, USA
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