Limited sign of soil adaptation to climate warming

Date:

January 30, 2017

Source:

University of New Hampshire

Summary:

While scientists and policy experts debate the impacts of global warming, 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, which is 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?

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While scientists and policy experts debate the impacts of global warming, 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, which is 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 University of New Hampshire scientist Serita Frey, professor of natural resources and the environment, and more than 40 researchers from across the globe to review data from 27 studies across nine biomes, from the desert to the Arctic. Their analysis was published recently in Proceedings of the National Academy of Sciences. This work represents the world's largest dataset to date of soil respiration response to experimental warming.

"This work is important because, rather than focusing on the warming response at a single site, it aggregates data collected from many sites across a range of ecosystems. This makes the conclusions and predictions more robust," Frey said.

One conclusion from the 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° C (77° F)," said Joanna Carey, a postdoctoral scientist in the Marine Biological Laboratory Ecosystems Center in Woods Hole, Mass., and the lead scientist on the study. Above the 25°C threshold, respiration rates decreased with further increases in soil temperature. "

"That means the Arctic latitudes, where soil temperatures rarely, if ever, reach 25°C, 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 Jianwu Tang with the Marine Biological Laboratory Ecosystems Center and a lead scientist on the study.

"Going forward, we need to better explore the biome-specific responses as global temperatures shift beyond the historic range," Frey said. To understand how global carbon in soils will respond to climate change, the authors stress, more data are needed from under- and nonrepresented regions, especially the Arctic and the tropics.

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Materials provided by University of New Hampshire. Note: Content may be edited for style and length.

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Journal Reference:

1. Joanna C. Carey, Jianwu Tang, Pamela H. Templer, Kevin D. Kroeger, Thomas W. Crowther, Andrew J. Burton, Jeffrey S. Dukes, Bridget Emmett, Serita D. Frey, Mary A. Heskel, Lifen Jiang, Megan B. Machmuller, Jacqueline Mohan, Anne Marie Panetta, Peter B. Reich, Sabine Reinsch, Xin Wang, Steven D. Allison, Chris Bamminger, Scott Bridgham, Scott L. Collins, Giovanbattista de Dato, William C. Eddy, Brian J. Enquist, Marc Estiarte, John Harte, Amanda Henderson, Bart R. Johnson, Klaus Steenberg Larsen, Yiqi Luo, Sven Marhan, Jerry M. Melillo, Josep Peñuelas, Laurel Pfeifer-Meister, Christian Poll, Edward Rastetter, Andrew B. Reinmann, Lorien L. Reynolds, Inger K. Schmidt, Gaius R. Shaver, Aaron L. Strong, Vidya Suseela, Albert Tietema. Temperature response of soil respiration largely unaltered with experimental warming. Proceedings of the National Academy of Sciences, 2016; 113 (48): 13797 DOI: 10.1073/pnas.1605365113