Cited by 6,919Soil Carbon and Nitrogen DynamicsClimate change and permafrostPeatlands and Wetlands Ecology

The DOI matches its Crossref record; 106 of the 108 references it cites were found in a registry or an index.

Temperature sensitivity of soil carbon decomposition and feedbacks to climate change

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Abstract

Significantly more carbon is stored in the world's soils--including peatlands, wetlands and permafrost--than is present in the atmosphere. Disagreement exists, however, regarding the effects of climate change on global soil carbon stocks. If carbon stored belowground is transferred to the atmosphere by a warming-induced acceleration of its decomposition, a positive feedback to climate change would occur. Conversely, if increases of plant-derived carbon inputs to soils exceed increases in decomposition, the feedback would be negative. Despite much research, a consensus has not yet emerged on the temperature sensitivity of soil carbon decomposition. Unravelling the feedback effect is particularly difficult, because the diverse soil organic compounds exhibit a wide range of kinetic properties, which determine the intrinsic temperature sensitivity of their decomposition. Moreover, several environmental constraints obscure the intrinsic temperature sensitivity of substrate decomposition, causing lower observed 'apparent' temperature sensitivity, and these constraints may, themselves, be sensitive to climate.

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Crossref · 10.1038/nature04514

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2 of the 108 references couldn’t be matched to a known paper.

Research works printed but not linked: 6

  1. Gruber, N. et al. in Toward CO2 Stabilization: Issues, Strategies, and Consequences (eds Field, C. B. & Raupach, M. R.) 45–76 (Island Press, Washington, DC, 2004)
  2. Janssens, I. A. et al. in Canopy Fluxes of Energy, Water and Carbon Dioxide of European Forests (ed. Valentini, R.) 235–256 (Springer, Berlin, 2003)
  3. Woodwell, G. M. in Changing Climate 216–241 (NAS Press, Washington DC, 1983)
  4. Reichstein, M. et al. Does the temperature sensitivity of decomposition vary with soil organic matter quality? Biogeosci. Discuss. 2, 737–747 (2005) · DOI
  5. Anisimov, O. A., Nelson, F. E. & Pavlov, A. V. Predictive scenarios of permafrost development under conditions of global climate change in the XXI century. Earth Cryology 3, 15–25 (1999)
  6. Michaelis, L. & Menten, M. L. Die kinetik der invertin wirkung. Biochem. Z. 49, 334–336 (1913)

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Metadata

Authors
Davidson, E. A., & Janssens, I. A.
Affiliations
  • Woodwell Climate Research Center (US)
  • University of Antwerp (BE)
Corresponding author
Davidson, Eric A.
Venue
Nature
Published
2006-03
Volume
440
Issue
7081
Pages
165-173
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W2083857556
Cited by
6,919
References
108
Citations by year
2026: 519 · 2025: 553 · 2024: 463 · 2023: 402 · 2022: 459 · 2021: 472 · 2020: 421 · 2019: 395 · 2018: 372 · 2017: 379 · 2016: 356 · 2015: 337 · 2014: 307 · 2013: 313 · 2012: 287
FWCI
27.72
Type
journal article
Language
en
Open access
Locations
  • Nature (publishedVersion)
  • PubMed (publishedVersion)
  • RePEc: Research Papers in Economics (submittedVersion)
Funders
  • National Science Foundation
  • U.S. Department of Energy
  • European Commission
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Climate change and permafrost
  • Physical Sciences › Environmental Science › Ecology › Peatlands and Wetlands Ecology
Keywords
soil carbon decomposition, temperature sensitivity, climate feedbacks, soil organic carbon, peatlands, permafrost, soil carbon stocks, decomposition kinetics, soil carbon dynamics
MeSH terms
Carbon, Carbon Dioxide, Plants, Soil, Temperature, Greenhouse Effect

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