4.8 Article

Stimulation of soil respiration by elevated CO2 is enhanced under nitrogen limitation in a decade-long grassland study

Publisher

NATL ACAD SCIENCES
DOI: 10.1073/pnas.2002780117

Keywords

elevated CO2; nitrogen deposition; soil respiration; metagenomics; Earth ecosystem model

Funding

  1. National Science Foundation of China [41825016]
  2. Second Tibetan Plateau Scientific Expedition and Research program [2019QZKK0503]
  3. special fund of the State Key Joint Laboratory of Environment Simulation and Pollution Control [19L01ESPC]
  4. US Department of Agriculture (USDA) through NSF-USDA Microbial Observatories Program [2007-35319-18305]
  5. Long-Term Ecological Research (LTER) [DEB-0620652, DEB-1234162, DEB-1831944]
  6. Long-Term Research in Environmental Biology (LTREB) [DEB-1242531, DEB-1753859]
  7. Biological Integration Institutes [NSF-DBI-2021898]
  8. Ecosystem Sciences [DEB-1120064]
  9. Biocomplexity grant [DEB-0322057]
  10. US Department of Energy Programs for Ecosystem Research grant [DE-FG0296ER62291]
  11. University of Minnesota
  12. USDA through the NSF-USDA Microbial Observatories Program [2007-35319-18305]
  13. US Department of Energy, Office of Science, Genomic Science Program [DE-SC0004601, DE-SC0010715, DE-SC0014079, DE-SC0016247, DE-SC0020163]
  14. Office of the Vice President for Research at the University of Oklahoma
  15. U.S. Department of Energy (DOE) [DE-SC0020163] Funding Source: U.S. Department of Energy (DOE)

Ask authors/readers for more resources

Whether and how CO2 and nitrogen (N) availability interact to influence carbon (C) cycling processes such as soil respiration remains a question of considerable uncertainty in projecting future C-climate feedbacks, which are strongly influenced by multiple global change drivers, including elevated atmospheric CO2 concentrations (eCO(2)) and increased N deposition. However, because decades of research on the responses of ecosystems to eCO(2) and N enrichment have been done largely independently, their interactive effects on soil respiratory CO2 efflux remain unresolved. Here, we show that in a multifactor free-air CO2 enrichment experiment, BioCON (Biodiversity, CO2, and N deposition) in Minnesota, the positive response of soil respiration to eCO(2) gradually strengthened at ambient (low) N supply but not enriched (high) N supply for the 12-y experimental period from 1998 to 2009. In contrast to earlier years, eCO(2) stimulated soil respiration twice as much at low than at high N supply from 2006 to 2009. In parallel, microbial C degradation genes were significantly boosted by eCO(2) at low but not high N supply. Incorporating those functional genes into a coupled C-N ecosystem model reduced model parameter uncertainty and improved the projections of the effects of different CO2 and N levels on soil respiration. If our observed results generalize to other ecosystems, they imply widely positive effects of eCO(2) on soil respiration even in infertile systems.

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