Temporal changes in global soil respiration since 1987
As the second-largest terrestrial carbon (C) flux, soil respiration ( R S ) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, w...
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| Published in | Nature communications Vol. 12; no. 1; pp. 403 - 9 |
|---|---|
| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
London
Nature Publishing Group UK
15.01.2021
Nature Publishing Group Nature Portfolio |
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| Abstract | As the second-largest terrestrial carbon (C) flux, soil respiration (
R
S
) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global
R
S
observations from 1987–2016.
R
S
increased (
P
< 0.001) at a rate of 27.66 g C m
−2
yr
−2
(equivalent to 0.161 Pg C yr
−2
) in 1987–1999 globally but became unchanged in 2000–2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration (
R
h
) derived from microbial decomposition of soil C increased in 1987–2016 (
P
< 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global
R
S
rise. This study of naturally occurring shifts in
R
S
over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges.
Soils hold massive amounts of carbon that hangs in the balance of microbial respiration and climate warming. Here the authors analyze a global dataset starting in 1987 and find through modeling that though soil respiration change had flatlined, recently it has resumed increasing owing to global warming. |
|---|---|
| AbstractList | As the second-largest terrestrial carbon (C) flux, soil respiration (R
) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global R
observations from 1987-2016. R
increased (P < 0.001) at a rate of 27.66 g C m
yr
(equivalent to 0.161 Pg C yr
) in 1987-1999 globally but became unchanged in 2000-2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration (R
) derived from microbial decomposition of soil C increased in 1987-2016 (P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global R
rise. This study of naturally occurring shifts in R
over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges. As the second-largest terrestrial carbon (C) flux, soil respiration ( R S ) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global R S observations from 1987–2016. R S increased ( P < 0.001) at a rate of 27.66 g C m −2 yr −2 (equivalent to 0.161 Pg C yr −2 ) in 1987–1999 globally but became unchanged in 2000–2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration ( R h ) derived from microbial decomposition of soil C increased in 1987–2016 ( P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global R S rise. This study of naturally occurring shifts in R S over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges. Soils hold massive amounts of carbon that hangs in the balance of microbial respiration and climate warming. Here the authors analyze a global dataset starting in 1987 and find through modeling that though soil respiration change had flatlined, recently it has resumed increasing owing to global warming. As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global RS observations from 1987–2016. RS increased (P < 0.001) at a rate of 27.66 g C m−2 yr−2 (equivalent to 0.161 Pg C yr−2) in 1987–1999 globally but became unchanged in 2000–2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration (Rh) derived from microbial decomposition of soil C increased in 1987–2016 (P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global RS rise. This study of naturally occurring shifts in RS over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges.Soils hold massive amounts of carbon that hangs in the balance of microbial respiration and climate warming. Here the authors analyze a global dataset starting in 1987 and find through modeling that though soil respiration change had flatlined, recently it has resumed increasing owing to global warming. As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global RSobservations from 1987–2016.RSincreased (P < 0.001) at a rate of 27.66 g C m-2 yr-2(equivalent to 0.161 Pg C yr-2) in 1987–1999 globally but became unchanged in 2000–2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration (Rh) derived from microbial decomposition of soil C increased in 1987–2016 (P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global RSrise. This study of naturally occurring shifts inRSover recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges. As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global RS observations from 1987-2016. RS increased (P < 0.001) at a rate of 27.66 g C m-2 yr-2 (equivalent to 0.161 Pg C yr-2) in 1987-1999 globally but became unchanged in 2000-2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration (Rh) derived from microbial decomposition of soil C increased in 1987-2016 (P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global RS rise. This study of naturally occurring shifts in RS over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges.As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global RS observations from 1987-2016. RS increased (P < 0.001) at a rate of 27.66 g C m-2 yr-2 (equivalent to 0.161 Pg C yr-2) in 1987-1999 globally but became unchanged in 2000-2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration (Rh) derived from microbial decomposition of soil C increased in 1987-2016 (P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global RS rise. This study of naturally occurring shifts in RS over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges. Soils hold massive amounts of carbon that hangs in the balance of microbial respiration and climate warming. Here the authors analyze a global dataset starting in 1987 and find through modeling that though soil respiration change had flatlined, recently it has resumed increasing owing to global warming. As the second-largest terrestrial carbon (C) flux, soil respiration ( R S ) has been stimulated by climate warming. However, the magnitude and dynamics of such stimulations of soil respiration are highly uncertain at the global scale, undermining our confidence in future climate projections. Here, we present an analysis of global R S observations from 1987–2016. R S increased ( P < 0.001) at a rate of 27.66 g C m −2 yr −2 (equivalent to 0.161 Pg C yr −2 ) in 1987–1999 globally but became unchanged in 2000–2016, which were related to complex temporal variations of temperature anomalies and soil C stocks. However, global heterotrophic respiration ( R h ) derived from microbial decomposition of soil C increased in 1987–2016 ( P < 0.001), suggesting accumulated soil C losses. Given the warmest years on records after 2015, our modeling analysis shows a possible resuscitation of global R S rise. This study of naturally occurring shifts in R S over recent decades has provided invaluable insights for designing more effective policies addressing future climate challenges. |
| ArticleNumber | 403 |
| Author | Guo, Xue Lei, Jiesi Zhou, Jizhong Yang, Yunfeng Gao, Qun Zeng, Yufei |
| Author_xml | – sequence: 1 givenname: Jiesi surname: Lei fullname: Lei, Jiesi organization: State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University – sequence: 2 givenname: Xue orcidid: 0000-0002-4309-6140 surname: Guo fullname: Guo, Xue organization: State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University – sequence: 3 givenname: Yufei surname: Zeng fullname: Zeng, Yufei organization: State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University – sequence: 4 givenname: Jizhong orcidid: 0000-0003-2014-0564 surname: Zhou fullname: Zhou, Jizhong organization: Institute for Environmental Genomics, University of Oklahoma, Department of Microbiology and Plant Biology, University of Oklahoma, Earth and Environmental Sciences, Lawrence Berkeley National Laboratory – sequence: 5 givenname: Qun orcidid: 0000-0002-2148-5807 surname: Gao fullname: Gao, Qun email: gaoqun998@163.com organization: State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Institute for Environmental Genomics, University of Oklahoma – sequence: 6 givenname: Yunfeng orcidid: 0000-0001-8274-6196 surname: Yang fullname: Yang, Yunfeng email: yangyf@tsinghua.edu.cn organization: State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/33452246$$D View this record in MEDLINE/PubMed https://www.osti.gov/servlets/purl/1815958$$D View this record in Osti.gov |
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| PublicationDateYYYYMMDD | 2021-01-15 |
| PublicationDate_xml | – month: 01 year: 2021 text: 2021-01-15 day: 15 |
| PublicationDecade | 2020 |
| PublicationPlace | London |
| PublicationPlace_xml | – name: London – name: England – name: United States |
| PublicationTitle | Nature communications |
| PublicationTitleAbbrev | Nat Commun |
| PublicationTitleAlternate | Nat Commun |
| PublicationYear | 2021 |
| Publisher | Nature Publishing Group UK Nature Publishing Group Nature Portfolio |
| Publisher_xml | – name: Nature Publishing Group UK – name: Nature Publishing Group – name: Nature Portfolio |
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| Snippet | As the second-largest terrestrial carbon (C) flux, soil respiration (
R
S
) has been stimulated by climate warming. However, the magnitude and dynamics of... As the second-largest terrestrial carbon (C) flux, soil respiration (R ) has been stimulated by climate warming. However, the magnitude and dynamics of... As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by climate warming. However, the magnitude and dynamics of such... As the second-largest terrestrial carbon (C) flux, soil respiration (RS) has been stimulated by climate warming. However, the magnitude and dynamics of... Soils hold massive amounts of carbon that hangs in the balance of microbial respiration and climate warming. Here the authors analyze a global dataset starting... |
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| SubjectTerms | 631/158/2165 704/106/694 704/47/4113 Anomalies Carbon Climate change ENVIRONMENTAL SCIENCES Global warming Humanities and Social Sciences Microorganisms Modelling multidisciplinary Respiration Resuscitation Science Science (multidisciplinary) Soil dynamics Soil temperature Soils Temporal variations |
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| Title | Temporal changes in global soil respiration since 1987 |
| URI | https://link.springer.com/article/10.1038/s41467-020-20616-z https://www.ncbi.nlm.nih.gov/pubmed/33452246 https://www.proquest.com/docview/2478165083 https://www.proquest.com/docview/2556548219 https://www.proquest.com/docview/2478594739 https://www.osti.gov/servlets/purl/1815958 https://pubmed.ncbi.nlm.nih.gov/PMC7810831 https://doaj.org/article/d4acef7e191a4ebf880019f8ca6919ec |
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