Integrating the evidence for a terrestrial carbon sink caused by increasing atmospheric CO2
Abstract
Atmospheric carbon dioxide concentration ([CO2]) is increasing, which increases leaf-scale photosynthesis and intrinsic water-use efficiency. These direct responses have the potential to increase plant growth, vegetation biomass, and soil organic matter; transferring carbon from the atmosphere into terrestrial ecosystems (a carbon sink). A substantial global terrestrial carbon sink would slow the rate of [CO2] increase and thus climate change. However, ecosystem CO2-responses are complex or confounded by concurrent changes in multiple agents of global change and evidence for a [CO2]-driven terrestrial carbon sink can appear contradictory. In this work, we synthesise theory and broad, multi-disciplinary evidence for the effects of increasing [CO2] (iCO2) on the global terrestrial carbon sink. Evidence suggests a substantial increase in global photosynthesis since pre-industry. Established theory, supported by experiments, indicates that iCO2 is likely responsible for about half of the increase. Global carbon budgeting, atmospheric data, and forest inventories indicate a historical carbon sink, and these apparent iCO2-responses are high in comparison with experiments and theory. Plant mortality and soil carbon iCO2-responses are highly uncertain. In conclusion, a range of evidence supports a positive terrestrial carbon sink in response to iCO2, albeit with uncertain magnitude and strong suggestion of a role for additional agents ofmore »
- Authors:
-
more »
- Oak Ridge Inst. for Science and Education (ORISE), Oak Ridge, TN (United States)
- Univ. of New South Wales, Sydney, NSW (Australia)
- Ludwig Maximilian Univ. of Munich, Munich (Germany)
- Univ. of Arizona, Tucson, AZ (United States); National Science Foundation (NSF), Alexandria, VA (United States)
- Stanford Univ., CA (United States)
- Univ. of California San Diego, La Jolla, CA (United States)
- Smithsonian Environmental Research Center, Edgewater, MD (United States)
- Western Sydney Univ., Penrith, NSW (Australia)
- School of Natural Resources and the Environment, Tucson, AZ (United States)
- Max Planck Inst. for Biogeochemistry, Jena (Germany)
- Smithsonian Conservation Biology Inst., Front Royal, VA (United States); Smithsonian Tropical Research Inst. (Panama)
- Univ. of Campania Luigi Vanvitelli, Caserta CE (Italy)
- Univ. of Leeds (United Kingdom)
- Aix‐Marseille Univ. (France); Swiss Federal Inst. for Forest, Snow and Landscape Research (WSL), Birmensdorf (Switzerland)
- Univ. of California, Santa Barbara, CA (United States)
- Commonwealth Scientific and Industrial Research Organisation (CSIRO) (Australia). Oceans and Atmosphere
- Univ. Paris-Saclay, Gif-sur-Yvette (France)
- Australian National Univ., Canberra, ACT (Australia)
- National Univ. of Singapore (Singapore); ETH Zurich (Switzerland)
- California Inst. of Technology (CalTech), Pasadena, CA (United States)
- Univ. of Arizona, Tucson, AZ (United States)
- Imperial College, London (United Kingdom)
- Northern Arizona Univ., Flagstaff, AZ (United States)
- Univ. of Bern (Switzerland)
- Univ. of California, Berkeley, CA (United States); Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Univ. of Basel (Switzerland)
- Auckland Univ. of Technology (New Zealand)
- Indiana Univ., Bloomington, IN (United States)
- Univ. of Oxford (United Kingdom)
- Commonwealth Scientific and Industrial Research Organisation (CSIRO), Canberra (Australia). Land and Water; Australian Research Council (ARC), Canberra (Australia). Centre of Excellence for Climate Extremes
- Univ. Autònoma de Barcelona (UAB) (Spain); CREAF, Barcelona (Spain)
- Ludwig Maximilian Univ. of Munich, Munich (Germany); Max Planck Inst. for Meteorology, Hamburg (Germany)
- Umeå Univ. (Sweden)
- Univ. of Exeter (United Kingdom)
- Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Univ. of California, Irvine, CA (United States)
- US Geological Survey, Arcata CA (United States)
- State Univ. of New York (SUNY), Albany, NY (United States)
- Rutgers Univ., New Brunswick, NJ (United States)
- Wageningen Univ. (Netherlands)
- Publication Date:
- Research Org.:
- Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States); Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA); USDOE Office of Science (SC), Biological and Environmental Research (BER); Australian Research Council (ARC); National Aeronautics and Space Administration (NASA); European Research Council (ERC); Smithsonian's Forest Global Earth Observatory (ForestGEO); Earth Systems and Climate Change Hub; Swiss National Science Foundation (SNF); German Research Foundation (DFG); USDA; National Institute of Food and Agriculture (NIFA); National Science Foundation (NSF); USGS
- OSTI Identifier:
- 1765497
- Alternate Identifier(s):
- OSTI ID: 1660527
- Report Number(s):
- LLNL-JRNL-814087
Journal ID: ISSN 0028-646X
- Grant/Contract Number:
- AC05-00OR22725; AC52-07NA27344; DP190101823; 80NSSC19M0103; 647204; NNH17AE86I; ERC-2013-SyG-2013-610028 IMBALANCE; AC02-05CH11231; 2018-67012-31496
- Resource Type:
- Accepted Manuscript
- Journal Name:
- New Phytologist
- Additional Journal Information:
- Journal Volume: 229; Journal Issue: 5; Journal ID: ISSN 0028-646X
- Publisher:
- Wiley
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; global carbon‐cycle; land‐atmosphere feedback; carbon dioxide; terrestrial ecosystems; free‐air CO2 enrichment (FACE); CO2‐fertilisation hypothesis; CO2‐fertilization; beta factor
Citation Formats
Walker, Anthony P., De Kauwe, Martin G., Bastos, Ana, Belmecheri, Soumaya, Georgiou, Katerina, Keeling, Ralph F., McMahon, Sean M., Medlyn, Belinda E., Moore, David P., Norby, Richard J., Zaehle, Sönke, Anderson‐Teixeira, Kristina J., Battipaglia, Giovanna, Brienen, Roel W., Cabugao, Kristine G., Cailleret, Maxime, Campbell, Elliott, Canadell, Josep G., Ciais, Philippe, Craig, Matthew E., Ellsworth, David S., Farquhar, Graham D., Fatichi, Simone, Fisher, Joshua B., Frank, David C., Graven, Heather, Gu, Lianhong, Haverd, Vanessa, Heilman, Kelly, Heimann, Martin, Hungate, Bruce A., Iversen, Colleen M., Joos, Fortunat, Jiang, Mingkai, Keenan, Trevor F., Knauer, Jürgen, Körner, Christian, Leshyk, Victor O., Leuzinger, Sebastian, Liu, Yao, MacBean, Natasha, Malhi, Yadvinder, McVicar, Tim R., Penuelas, Josep, Pongratz, Julia, Powell, A. Shafer, Riutta, Terhi, Sabot, Manon B., Schleucher, Juergen, Sitch, Stephen, Smith, William K., Sulman, Benjamin, Taylor, Benton, Terrer, César, Torn, Margaret S., Treseder, Kathleen K., Trugman, Anna T., Trumbore, Susan E., Mantgem, Phillip J., Voelker, Steve L., Whelan, Mary E., and Zuidema, Pieter A. Integrating the evidence for a terrestrial carbon sink caused by increasing atmospheric CO2. United States: N. p., 2020.
Web. doi:10.1111/nph.16866.
Walker, Anthony P., De Kauwe, Martin G., Bastos, Ana, Belmecheri, Soumaya, Georgiou, Katerina, Keeling, Ralph F., McMahon, Sean M., Medlyn, Belinda E., Moore, David P., Norby, Richard J., Zaehle, Sönke, Anderson‐Teixeira, Kristina J., Battipaglia, Giovanna, Brienen, Roel W., Cabugao, Kristine G., Cailleret, Maxime, Campbell, Elliott, Canadell, Josep G., Ciais, Philippe, Craig, Matthew E., Ellsworth, David S., Farquhar, Graham D., Fatichi, Simone, Fisher, Joshua B., Frank, David C., Graven, Heather, Gu, Lianhong, Haverd, Vanessa, Heilman, Kelly, Heimann, Martin, Hungate, Bruce A., Iversen, Colleen M., Joos, Fortunat, Jiang, Mingkai, Keenan, Trevor F., Knauer, Jürgen, Körner, Christian, Leshyk, Victor O., Leuzinger, Sebastian, Liu, Yao, MacBean, Natasha, Malhi, Yadvinder, McVicar, Tim R., Penuelas, Josep, Pongratz, Julia, Powell, A. Shafer, Riutta, Terhi, Sabot, Manon B., Schleucher, Juergen, Sitch, Stephen, Smith, William K., Sulman, Benjamin, Taylor, Benton, Terrer, César, Torn, Margaret S., Treseder, Kathleen K., Trugman, Anna T., Trumbore, Susan E., Mantgem, Phillip J., Voelker, Steve L., Whelan, Mary E., & Zuidema, Pieter A. Integrating the evidence for a terrestrial carbon sink caused by increasing atmospheric CO2. United States. https://doi.org/10.1111/nph.16866
Walker, Anthony P., De Kauwe, Martin G., Bastos, Ana, Belmecheri, Soumaya, Georgiou, Katerina, Keeling, Ralph F., McMahon, Sean M., Medlyn, Belinda E., Moore, David P., Norby, Richard J., Zaehle, Sönke, Anderson‐Teixeira, Kristina J., Battipaglia, Giovanna, Brienen, Roel W., Cabugao, Kristine G., Cailleret, Maxime, Campbell, Elliott, Canadell, Josep G., Ciais, Philippe, Craig, Matthew E., Ellsworth, David S., Farquhar, Graham D., Fatichi, Simone, Fisher, Joshua B., Frank, David C., Graven, Heather, Gu, Lianhong, Haverd, Vanessa, Heilman, Kelly, Heimann, Martin, Hungate, Bruce A., Iversen, Colleen M., Joos, Fortunat, Jiang, Mingkai, Keenan, Trevor F., Knauer, Jürgen, Körner, Christian, Leshyk, Victor O., Leuzinger, Sebastian, Liu, Yao, MacBean, Natasha, Malhi, Yadvinder, McVicar, Tim R., Penuelas, Josep, Pongratz, Julia, Powell, A. Shafer, Riutta, Terhi, Sabot, Manon B., Schleucher, Juergen, Sitch, Stephen, Smith, William K., Sulman, Benjamin, Taylor, Benton, Terrer, César, Torn, Margaret S., Treseder, Kathleen K., Trugman, Anna T., Trumbore, Susan E., Mantgem, Phillip J., Voelker, Steve L., Whelan, Mary E., and Zuidema, Pieter A. Wed .
"Integrating the evidence for a terrestrial carbon sink caused by increasing atmospheric CO2". United States. https://doi.org/10.1111/nph.16866. https://www.osti.gov/servlets/purl/1765497.
@article{osti_1765497,
title = {Integrating the evidence for a terrestrial carbon sink caused by increasing atmospheric CO2},
author = {Walker, Anthony P. and De Kauwe, Martin G. and Bastos, Ana and Belmecheri, Soumaya and Georgiou, Katerina and Keeling, Ralph F. and McMahon, Sean M. and Medlyn, Belinda E. and Moore, David P. and Norby, Richard J. and Zaehle, Sönke and Anderson‐Teixeira, Kristina J. and Battipaglia, Giovanna and Brienen, Roel W. and Cabugao, Kristine G. and Cailleret, Maxime and Campbell, Elliott and Canadell, Josep G. and Ciais, Philippe and Craig, Matthew E. and Ellsworth, David S. and Farquhar, Graham D. and Fatichi, Simone and Fisher, Joshua B. and Frank, David C. and Graven, Heather and Gu, Lianhong and Haverd, Vanessa and Heilman, Kelly and Heimann, Martin and Hungate, Bruce A. and Iversen, Colleen M. and Joos, Fortunat and Jiang, Mingkai and Keenan, Trevor F. and Knauer, Jürgen and Körner, Christian and Leshyk, Victor O. and Leuzinger, Sebastian and Liu, Yao and MacBean, Natasha and Malhi, Yadvinder and McVicar, Tim R. and Penuelas, Josep and Pongratz, Julia and Powell, A. Shafer and Riutta, Terhi and Sabot, Manon B. and Schleucher, Juergen and Sitch, Stephen and Smith, William K. and Sulman, Benjamin and Taylor, Benton and Terrer, César and Torn, Margaret S. and Treseder, Kathleen K. and Trugman, Anna T. and Trumbore, Susan E. and Mantgem, Phillip J. and Voelker, Steve L. and Whelan, Mary E. and Zuidema, Pieter A.},
abstractNote = {Atmospheric carbon dioxide concentration ([CO2]) is increasing, which increases leaf-scale photosynthesis and intrinsic water-use efficiency. These direct responses have the potential to increase plant growth, vegetation biomass, and soil organic matter; transferring carbon from the atmosphere into terrestrial ecosystems (a carbon sink). A substantial global terrestrial carbon sink would slow the rate of [CO2] increase and thus climate change. However, ecosystem CO2-responses are complex or confounded by concurrent changes in multiple agents of global change and evidence for a [CO2]-driven terrestrial carbon sink can appear contradictory. In this work, we synthesise theory and broad, multi-disciplinary evidence for the effects of increasing [CO2] (iCO2) on the global terrestrial carbon sink. Evidence suggests a substantial increase in global photosynthesis since pre-industry. Established theory, supported by experiments, indicates that iCO2 is likely responsible for about half of the increase. Global carbon budgeting, atmospheric data, and forest inventories indicate a historical carbon sink, and these apparent iCO2-responses are high in comparison with experiments and theory. Plant mortality and soil carbon iCO2-responses are highly uncertain. In conclusion, a range of evidence supports a positive terrestrial carbon sink in response to iCO2, albeit with uncertain magnitude and strong suggestion of a role for additional agents of global change.},
doi = {10.1111/nph.16866},
journal = {New Phytologist},
number = 5,
volume = 229,
place = {United States},
year = {Wed Aug 12 00:00:00 EDT 2020},
month = {Wed Aug 12 00:00:00 EDT 2020}
}
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