Measuring carbon flux from soil at Toolik Field Station in Arctic Alaska. Photo by: Jim Tang
While scientists and policy experts debate the impacts of global warming, the Earth’s soil is releasing roughly nine times more carbon dioxide to the atmosphere than all human activities combined. This huge carbon flux from soil—due to the natural respiration of soil microbes and plant roots—begs one of the central questions in climate change science: As the global climate warms, will soil respiration rates increase, adding even more carbon dioxide to the atmosphere and accelerating climate change?
Previous experimental studies of this question have not produced a consensus, prompting Marine Biological Laboratory scientists Joanna Carey, Jianwu Tang and colleagues to synthesize the data from 27 studies across nine biomes, from the desert to the Arctic. Their analysis, published this week in Proceedings of the National Academy of Sciences, represents the largest dataset to date of soil respiration response to experimental warming.
One prediction from this synthesis is that rising global temperatures result in regionally variable responses in soil respiration, with colder climates being considerably more responsive. “Consistently across all biomes, we found that soil respiration increased with soil temperature up to about 25 degrees Celsius (77 degrees Fahrenheit),” said Carey, a postdoctoral scientist in the MBL Ecosystems Center. Above the 25-degree Celsius threshold, respiration rates decreased with further increases in soil temperature.
“That means the Arctic latitudes, where soil temperatures rarely, if ever, reach 25 degrees Celsius, will continue to be most responsive to climate warming. Because there is so much carbon stored in frozen soils of the Arctic, this has really serious repercussions for future climate change,” Carey said.
The team also found that soil microbes in experimental warming studies showed no sign of adaptation—meaning a muted respiration response to rising temperatures—in all of the biomes studied, except desert and boreal forest. This indicates that “soils will typically respond strongly to increasing temperature by releasing more carbon dioxide,” said Tang, the study’s lead investigator.
To understand how global carbon in soils will respond to climate change, the authors stress, more data are needed from under- and non-represented regions, especially the Arctic and the tropics.
Other MBL scientists who contributed to this study include Mary Heskel, Jerry Melillo, Edward B. Rastetter and Gaius R. Shaver.
Citation: Carey, Joanna A. et al (2016) Temperature response of soil respiration largely unaltered with experimental warming. Proceedings of the National Academy of Sciences. DOI: 10.1073/pnas.1605365113
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