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Utilizing one of the longest-running ecosystem experiments in the Arctic, a Colorado State University-led team of researchers has developed a better understanding of the interplay among plants, microbes and soil nutrients—findings that offer new insight into how critical carbon deposits may be released from thawing Arctic permafrost.

Estimates suggest that Arctic soils contain nearly twice the amount of carbon that is currently in the atmosphere. As climate change has caused portions of Earth's northernmost polar regions to thaw, scientists have long been concerned about significant amounts of carbon being released in the form of greenhouse gases, a process fueled by microbes.

Much of the efforts to study and model this scenario have focused specifically on how rising global temperatures will disrupt the carbon currently locked in Arctic soils. But warming is impacting the region in other ways, too, including changing plant productivity, the overall composition of vegetation across the landscape, and the balance of nutrients in the soil. These changes in plant composition will also affect the way carbon is cycled from the soil into the atmosphere, according to a study published this week in the journal Nature Climate Change.

The work was led by Megan Machmuller, a research scientist in CSU's Soil and Crop Sciences Department.

"Our work focused on pinpointing the mechanisms that are responsible for controlling the fate of carbon in the Arctic," Machmuller said. "We know temperature plays a large role, but there are also ecosystem shifts that are co-occurring with climate change in this region."

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