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Title: Fine-root functional trait responses to experimental warming: a global meta-analysis

Journal Article · · New Phytologist
DOI:https://doi.org/10.1111/nph.17279· OSTI ID:1779156
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3];  [4]; ORCiD logo [5]; ORCiD logo [6]; ORCiD logo [6]; ORCiD logo [7]; ORCiD logo [8]; ORCiD logo [9];  [6]; ORCiD logo [10]
  1. Chinese Academy of Sciences (CAS), Beijing (China); Northern Arizona Univ., Flagstaff, AZ (United States)
  2. Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
  3. The Morton Arboretum, Lisle IL (United States)
  4. Beijing Forestry University (China)
  5. Chinese Academy of Sciences (CAS), Beijing (China)
  6. Northern Arizona Univ., Flagstaff, AZ (United States)
  7. Lanzhou University (China)
  8. Shandong Agricultural University, Taian (China)
  9. Jiangxi Agricultural University, Nanchang (China)
  10. Chinese Academy of Sciences (CAS), Beijing (China); University of Chinese Academy of Sciences, Beijing (China)

Whether and how warming alters functional traits of absorptive plant roots remains to be answered across the globe. Tackling this question is crucial to better understanding terrestrial responses to climate change as fine-root traits drive many ecosystem processes. In this work, we carried out a detailed synthesis of fine-root trait responses to experimental warming by performing a meta-analysis of 964 paired observations from 177 publications. Warming increased fine-root biomass, production, respiration and nitrogen concentration as well as decreased root carbon : nitrogen ratio and nonstructural carbohydrates. Warming effects on fine-root biomass decreased with greater warming magnitude, especially in short-term experiments. Furthermore, the positive effect of warming on fine-root biomass was strongest in deeper soil horizons and in colder and drier regions. Total fine-root length, morphology, mortality, life span and turnover were unresponsive to warming. Our results highlight the significant changes in fine-root traits in response to warming as well as the importance of warming magnitude and duration in understanding fine-root responses. These changes have strong implications for global soil carbon stocks in a warmer world associated with increased root-derived carbon inputs into deeper soil horizons and increases in fine-root respiration.

Research Organization:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
Sponsoring Organization:
USDOE Office of Science (SC); National Natural Science Foundation of China (NSFC); Second Tibetan Plateau Scientific Expedition and Research (STEP)
Grant/Contract Number:
AC05-00OR22725
OSTI ID:
1779156
Journal Information:
New Phytologist, Vol. 230, Issue 5; ISSN 0028-646X
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English

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