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Title: Quantifying global soil carbon losses in response to warming

Abstract

The majority of the Earth’s terrestrial carbon is stored in the soil. If anthropogenic warming stimulates the loss of this carbon to the atmosphere, it could drive further planetary warming. Despite evidence that warming enhances carbon fluxes to and from the soil, the net global balance between these responses remains uncertain. Here we present a comprehensive analysis of warming- induced changes in soil carbon stocks by assembling data from 49 field experiments located across North America, Europe and Asia. We find that the effects of warming are contingent on the size of the initial soil carbon stock, with considerable losses occurring in high-latitude areas. By extrapolating this empirical relationship to the global scale, we provide estimates of soil carbon sensitivity to warming that may help to constrain Earth system model projections. Our empirical relationship suggests that global soil carbon stocks in the upper soil horizons will fall by 30 ± 30 petagrams of carbon to 203 ± 161 petagrams of carbon under one degree of warming, depending on the rate at which the effects of warming are realized. Under the conservative assumption that the response of soil carbon to warming occurs within a year, a business-as-usual climate scenario would drivemore » the loss of 55 ± 50 petagrams of carbon from the upper soil horizons by 2050. This value is around 12-17 per cent of the expected anthropogenic emissions over this period. Despite the considerable uncertainty in our estimates, the direction of the global soil carbon response is consistent across all scenarios. This provides strong empirical support for the idea that rising temperatures will stimulate the net loss of soil carbon to the atmosphere, driving a positive land carbon–climate feedback that could accelerate climate change.« less

Authors:
 [1];  [2];  [3];  [4];  [5];  [6];  [7];  [8];  [9];  [10];  [11];  [12];  [13];  [14];  [15];  [16];  [17];  [18];  [19];  [20] more »;  [21];  [22];  [23];  [24];  [25];  [12];  [26];  [19];  [27];  [28];  [29];  [30];  [31];  [32];  [19];  [33];  [31];  [14];  [21];  [12];  [32];  [20];  [12];  [19];  [34];  [2];  [35];  [10];  [36];  [1] « less
  1. Netherlands Inst. of Ecology, Wageningen (The Netherlands); Yale Univ., New Haven, CT (United States)
  2. Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
  3. Yale Univ., New Haven, CT (United States)
  4. National Center for Atmospheric Research, Boulder, CO (United States); Univ. of Colorado, Boulder, CO (United States)
  5. Marine Biological Lab., Woods Hole, MA (United States)
  6. Colorado State Univ., Fort Collins, CO (United States)
  7. Netherlands Inst. of Ecology, Wageningen (The Netherlands); Wageningen Univ., Wageningen (The Netherlands)
  8. Chinese Academy of Meteorological Sciences, Beijing (China); Nanjing Univ. of Information Science & Technology, Nanjing (China)
  9. Chinese Academy of Meteorological Sciences, Beijing (China)
  10. Univ. of California, Irvine, CA (United States)
  11. Kansas State Univ., Manhattan, KS (United States)
  12. Univ. of Oregon, Eugene, OR (United States)
  13. Michigan Technological Univ., Houghton, MI (United States)
  14. Western Sydney Univ., Penrith, NSW (Australia)
  15. Western Sydney Univ., Penrith, NSW (Australia); Univ. of Minnesota, St. Paul, MN (United States)
  16. Duke Univ., Durham, NC (United States)
  17. Univ. of Copenhagen, Copenhagen (Denmark); Univ. of Tennessee, Knoxville, TN (United States)
  18. Univ. of Sydney, Camden, NSW (Australia)
  19. Univ. of Copenhagen, Copenhagen (Denmark)
  20. Environment Centre Wales, Bangor (United Kingdom). Centre for Ecology and Hydrology
  21. Spanish National Research Council (CSIC), Catalonia (Spain); Centre for Ecological Research and Forestry Applications (CREAF), Catalonia (Spain)
  22. Univ. of New Hampshire, Durham, NH (United States)
  23. Northeast Normal Univ., Jilin Province (China)
  24. Univ. of California, Berkeley, CA (United States)
  25. Univ. of Oklahoma, Norman, OK (United States)
  26. Magyar Tudomanyos Akademia Centre for Ecological Research (MTA), Budapest (Hungary)
  27. Swedish Univ. of Agricultural Sciences, Umeå (Sweden)
  28. Colorado State Univ., Fort Collins, CO (United States); Univ. of Manchester, Manchester (United Kingdom)
  29. Univ. of Oklahoma, Norman, OK (United States); Tsinghua Univ., Beijing (China)
  30. National Univ. of Singapore, Singapore (Singapore)
  31. Chinese Academy of Sciences (CAS), Beijing (China)
  32. Univ. of Hohenheim, Stuttgart (Germany)
  33. Univ. of Georgia, Athens, GA (United States)
  34. Hampshire College, Amherst, MA (United States)
  35. Boston Univ., Boston, MA (United States)
  36. Univ. of Alaska, Anchorage, AK (United States)
Publication Date:
Research Org.:
Univ. of Tennessee, Knoxville, TN (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1501388
Grant/Contract Number:  
SC0010562
Resource Type:
Journal Article: Accepted Manuscript
Journal Name:
Nature (London)
Additional Journal Information:
Journal Volume: 540; Journal Issue: 7631; Journal ID: ISSN 0028-0836
Publisher:
Nature Publishing Group
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES

Citation Formats

Crowther, T. W., Todd-Brown, K. E. O., Rowe, C. W., Wieder, W. R., Carey, J. C., Machmuller, M. B., Snoek, B. L., Fang, S., Zhou, G., Allison, S. D., Blair, J. M., Bridgham, S. D., Burton, A. J., Carrillo, Y., Reich, P. B., Clark, J. S., Classen, A. T., Dijkstra, F. A., Elberling, B., Emmett, B. A., Estiarte, M., Frey, S. D., Guo, J., Harte, J., Jiang, L., Johnson, B. R., Kröel-Dulay, G., Larsen, K. S., Laudon, H., Lavallee, J. M., Luo, Y., Lupascu, M., Ma, L. N., Marhan, S., Michelsen, A., Mohan, J., Niu, S., Pendall, E., Peñuelas, J., Pfeifer-Meister, L., Poll, C., Reinsch, S., Reynolds, L. L., Schmidt, I. K., Sistla, S., Sokol, N. W., Templer, P. H., Treseder, K. K., Welker, J. M., and Bradford, M. A. Quantifying global soil carbon losses in response to warming. United States: N. p., 2016. Web. doi:10.1038/nature20150.
Crowther, T. W., Todd-Brown, K. E. O., Rowe, C. W., Wieder, W. R., Carey, J. C., Machmuller, M. B., Snoek, B. L., Fang, S., Zhou, G., Allison, S. D., Blair, J. M., Bridgham, S. D., Burton, A. J., Carrillo, Y., Reich, P. B., Clark, J. S., Classen, A. T., Dijkstra, F. A., Elberling, B., Emmett, B. A., Estiarte, M., Frey, S. D., Guo, J., Harte, J., Jiang, L., Johnson, B. R., Kröel-Dulay, G., Larsen, K. S., Laudon, H., Lavallee, J. M., Luo, Y., Lupascu, M., Ma, L. N., Marhan, S., Michelsen, A., Mohan, J., Niu, S., Pendall, E., Peñuelas, J., Pfeifer-Meister, L., Poll, C., Reinsch, S., Reynolds, L. L., Schmidt, I. K., Sistla, S., Sokol, N. W., Templer, P. H., Treseder, K. K., Welker, J. M., & Bradford, M. A. Quantifying global soil carbon losses in response to warming. United States. https://doi.org/10.1038/nature20150
Crowther, T. W., Todd-Brown, K. E. O., Rowe, C. W., Wieder, W. R., Carey, J. C., Machmuller, M. B., Snoek, B. L., Fang, S., Zhou, G., Allison, S. D., Blair, J. M., Bridgham, S. D., Burton, A. J., Carrillo, Y., Reich, P. B., Clark, J. S., Classen, A. T., Dijkstra, F. A., Elberling, B., Emmett, B. A., Estiarte, M., Frey, S. D., Guo, J., Harte, J., Jiang, L., Johnson, B. R., Kröel-Dulay, G., Larsen, K. S., Laudon, H., Lavallee, J. M., Luo, Y., Lupascu, M., Ma, L. N., Marhan, S., Michelsen, A., Mohan, J., Niu, S., Pendall, E., Peñuelas, J., Pfeifer-Meister, L., Poll, C., Reinsch, S., Reynolds, L. L., Schmidt, I. K., Sistla, S., Sokol, N. W., Templer, P. H., Treseder, K. K., Welker, J. M., and Bradford, M. A. 2016. "Quantifying global soil carbon losses in response to warming". United States. https://doi.org/10.1038/nature20150. https://www.osti.gov/servlets/purl/1501388.
@article{osti_1501388,
title = {Quantifying global soil carbon losses in response to warming},
author = {Crowther, T. W. and Todd-Brown, K. E. O. and Rowe, C. W. and Wieder, W. R. and Carey, J. C. and Machmuller, M. B. and Snoek, B. L. and Fang, S. and Zhou, G. and Allison, S. D. and Blair, J. M. and Bridgham, S. D. and Burton, A. J. and Carrillo, Y. and Reich, P. B. and Clark, J. S. and Classen, A. T. and Dijkstra, F. A. and Elberling, B. and Emmett, B. A. and Estiarte, M. and Frey, S. D. and Guo, J. and Harte, J. and Jiang, L. and Johnson, B. R. and Kröel-Dulay, G. and Larsen, K. S. and Laudon, H. and Lavallee, J. M. and Luo, Y. and Lupascu, M. and Ma, L. N. and Marhan, S. and Michelsen, A. and Mohan, J. and Niu, S. and Pendall, E. and Peñuelas, J. and Pfeifer-Meister, L. and Poll, C. and Reinsch, S. and Reynolds, L. L. and Schmidt, I. K. and Sistla, S. and Sokol, N. W. and Templer, P. H. and Treseder, K. K. and Welker, J. M. and Bradford, M. A.},
abstractNote = {The majority of the Earth’s terrestrial carbon is stored in the soil. If anthropogenic warming stimulates the loss of this carbon to the atmosphere, it could drive further planetary warming. Despite evidence that warming enhances carbon fluxes to and from the soil, the net global balance between these responses remains uncertain. Here we present a comprehensive analysis of warming- induced changes in soil carbon stocks by assembling data from 49 field experiments located across North America, Europe and Asia. We find that the effects of warming are contingent on the size of the initial soil carbon stock, with considerable losses occurring in high-latitude areas. By extrapolating this empirical relationship to the global scale, we provide estimates of soil carbon sensitivity to warming that may help to constrain Earth system model projections. Our empirical relationship suggests that global soil carbon stocks in the upper soil horizons will fall by 30 ± 30 petagrams of carbon to 203 ± 161 petagrams of carbon under one degree of warming, depending on the rate at which the effects of warming are realized. Under the conservative assumption that the response of soil carbon to warming occurs within a year, a business-as-usual climate scenario would drive the loss of 55 ± 50 petagrams of carbon from the upper soil horizons by 2050. This value is around 12-17 per cent of the expected anthropogenic emissions over this period. Despite the considerable uncertainty in our estimates, the direction of the global soil carbon response is consistent across all scenarios. This provides strong empirical support for the idea that rising temperatures will stimulate the net loss of soil carbon to the atmosphere, driving a positive land carbon–climate feedback that could accelerate climate change.},
doi = {10.1038/nature20150},
url = {https://www.osti.gov/biblio/1501388}, journal = {Nature (London)},
issn = {0028-0836},
number = 7631,
volume = 540,
place = {United States},
year = {Thu Dec 01 00:00:00 EST 2016},
month = {Thu Dec 01 00:00:00 EST 2016}
}

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journal, November 2019


A meta-analysis of global fungal distribution reveals climate-driven patterns
journal, November 2019


Tidal wetland resilience to sea level rise increases their carbon sequestration capacity in United States
journal, November 2019


A global, empirical, harmonised dataset of soil organic carbon changes under perennial crops
journal, May 2019


Discrete taxa of saprotrophic fungi respire different ages of carbon from Antarctic soils
journal, May 2018


Increased microbial growth, biomass, and turnover drive soil organic carbon accumulation at higher plant diversity
journal, August 2019


Origin of volatile organic compound emissions from subarctic tundra under global warming
journal, January 2020


Accounting for Carbon Stocks in Soils and Measuring GHGs Emission Fluxes from Soils: Do We Have the Necessary Standards?
journal, July 2017


Increasing Temperature and Microplastic Fibers Jointly Influence Soil Aggregation by Saprobic Fungi
journal, September 2019


Flooding Irrigation Weakens the Molecular Ecological Network Complexity of Soil Microbes during the Process of Dryland-to-Paddy Conversion
journal, January 2020