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Temperature response of soil respiration largely unaltered with experimental warming.


ABSTRACT: The respiratory release of carbon dioxide (CO2) from soil is a major yet poorly understood flux in the global carbon cycle. Climatic warming is hypothesized to increase rates of soil respiration, potentially fueling further increases in global temperatures. However, despite considerable scientific attention in recent decades, the overall response of soil respiration to anticipated climatic warming remains unclear. We synthesize the largest global dataset to date of soil respiration, moisture, and temperature measurements, totaling >3,800 observations representing 27 temperature manipulation studies, spanning nine biomes and over 2 decades of warming. Our analysis reveals no significant differences in the temperature sensitivity of soil respiration between control and warmed plots in all biomes, with the exception of deserts and boreal forests. Thus, our data provide limited evidence of acclimation of soil respiration to experimental warming in several major biome types, contrary to the results from multiple single-site studies. Moreover, across all nondesert biomes, respiration rates with and without experimental warming follow a Gaussian response, increasing with soil temperature up to a threshold of ?25 °C, above which respiration rates decrease with further increases in temperature. This consistent decrease in temperature sensitivity at higher temperatures demonstrates that rising global temperatures may result in regionally variable responses in soil respiration, with colder climates being considerably more responsive to increased ambient temperatures compared with warmer regions. Our analysis adds a unique cross-biome perspective on the temperature response of soil respiration, information critical to improving our mechanistic understanding of how soil carbon dynamics change with climatic warming.

SUBMITTER: Carey JC 

PROVIDER: S-EPMC5137763 | biostudies-literature | 2016 Nov

REPOSITORIES: biostudies-literature

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Temperature response of soil respiration largely unaltered with experimental warming.

Carey Joanna C JC   Tang Jianwu J   Templer Pamela H PH   Kroeger Kevin D KD   Crowther Thomas W TW   Burton Andrew J AJ   Dukes Jeffrey S JS   Emmett Bridget B   Frey Serita D SD   Heskel Mary A MA   Jiang Lifen L   Machmuller Megan B MB   Mohan Jacqueline J   Panetta Anne Marie AM   Reich Peter B PB   Reinsch Sabine S   Wang Xin X   Allison Steven D SD   Bamminger Chris C   Bridgham Scott S   Collins Scott L SL   de Dato Giovanbattista G   Eddy William C WC   Enquist Brian J BJ   Estiarte Marc M   Harte John J   Henderson Amanda A   Johnson Bart R BR   Larsen Klaus Steenberg KS   Luo Yiqi Y   Marhan Sven S   Melillo Jerry M JM   Peñuelas Josep J   Pfeifer-Meister Laurel L   Poll Christian C   Rastetter Edward E   Reinmann Andrew B AB   Reynolds Lorien L LL   Schmidt Inger K IK   Shaver Gaius R GR   Strong Aaron L AL   Suseela Vidya V   Tietema Albert A  

Proceedings of the National Academy of Sciences of the United States of America 20161114 48


The respiratory release of carbon dioxide (CO<sub>2</sub>) from soil is a major yet poorly understood flux in the global carbon cycle. Climatic warming is hypothesized to increase rates of soil respiration, potentially fueling further increases in global temperatures. However, despite considerable scientific attention in recent decades, the overall response of soil respiration to anticipated climatic warming remains unclear. We synthesize the largest global dataset to date of soil respiration, m  ...[more]

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