author_facet Evans, Chris D.
Freeman, Chris
Cork, Lorna G.
Thomas, David N.
Reynolds, Brian
Billett, Michael F.
Garnett, Mark H.
Norris, David
Evans, Chris D.
Freeman, Chris
Cork, Lorna G.
Thomas, David N.
Reynolds, Brian
Billett, Michael F.
Garnett, Mark H.
Norris, David
author Evans, Chris D.
Freeman, Chris
Cork, Lorna G.
Thomas, David N.
Reynolds, Brian
Billett, Michael F.
Garnett, Mark H.
Norris, David
spellingShingle Evans, Chris D.
Freeman, Chris
Cork, Lorna G.
Thomas, David N.
Reynolds, Brian
Billett, Michael F.
Garnett, Mark H.
Norris, David
Geophysical Research Letters
Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
General Earth and Planetary Sciences
Geophysics
author_sort evans, chris d.
spelling Evans, Chris D. Freeman, Chris Cork, Lorna G. Thomas, David N. Reynolds, Brian Billett, Michael F. Garnett, Mark H. Norris, David 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2007gl029431 <jats:p>The stability of global soil carbon (C) represents a major uncertainty in forecasting future climate change. In the UK, substantial soil C losses have been reported, while at the same time dissolved organic carbon (DOC) concentrations in upland waters have increased, suggesting that soil C stocks may be destabilising in response to climate change. To investigate the link between soil carbon and DOC at a range of sites, soil organic matter, soilwater and streamwater DOC were analysed for radiocarbon (<jats:sup>14</jats:sup>C). DOC exported from C‐rich landscapes appears younger than the soil C itself, much of it comprising C assimilated post‐1950s. DOC from more intensively managed, C‐poor soils is older, in some cases &gt;100 years. Results appear consistent with soil C destabilisation in farmed landscapes, but not in peatlands. Reported C losses may to a significant extent be explained by mechanisms other than climate change, e.g. recovery from acidification in peatlands, and agricultural intensification in managed systems.</jats:p> Evidence against recent climate‐induced destabilisation of soil carbon from <sup>14</sup>C analysis of riverine dissolved organic matter Geophysical Research Letters
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title Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_unstemmed Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_full Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_fullStr Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_full_unstemmed Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_short Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_sort evidence against recent climate‐induced destabilisation of soil carbon from <sup>14</sup>c analysis of riverine dissolved organic matter
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/2007gl029431
publishDate 2007
physical
description <jats:p>The stability of global soil carbon (C) represents a major uncertainty in forecasting future climate change. In the UK, substantial soil C losses have been reported, while at the same time dissolved organic carbon (DOC) concentrations in upland waters have increased, suggesting that soil C stocks may be destabilising in response to climate change. To investigate the link between soil carbon and DOC at a range of sites, soil organic matter, soilwater and streamwater DOC were analysed for radiocarbon (<jats:sup>14</jats:sup>C). DOC exported from C‐rich landscapes appears younger than the soil C itself, much of it comprising C assimilated post‐1950s. DOC from more intensively managed, C‐poor soils is older, in some cases &gt;100 years. Results appear consistent with soil C destabilisation in farmed landscapes, but not in peatlands. Reported C losses may to a significant extent be explained by mechanisms other than climate change, e.g. recovery from acidification in peatlands, and agricultural intensification in managed systems.</jats:p>
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author Evans, Chris D., Freeman, Chris, Cork, Lorna G., Thomas, David N., Reynolds, Brian, Billett, Michael F., Garnett, Mark H., Norris, David
author_facet Evans, Chris D., Freeman, Chris, Cork, Lorna G., Thomas, David N., Reynolds, Brian, Billett, Michael F., Garnett, Mark H., Norris, David, Evans, Chris D., Freeman, Chris, Cork, Lorna G., Thomas, David N., Reynolds, Brian, Billett, Michael F., Garnett, Mark H., Norris, David
author_sort evans, chris d.
container_issue 7
container_start_page 0
container_title Geophysical Research Letters
container_volume 34
description <jats:p>The stability of global soil carbon (C) represents a major uncertainty in forecasting future climate change. In the UK, substantial soil C losses have been reported, while at the same time dissolved organic carbon (DOC) concentrations in upland waters have increased, suggesting that soil C stocks may be destabilising in response to climate change. To investigate the link between soil carbon and DOC at a range of sites, soil organic matter, soilwater and streamwater DOC were analysed for radiocarbon (<jats:sup>14</jats:sup>C). DOC exported from C‐rich landscapes appears younger than the soil C itself, much of it comprising C assimilated post‐1950s. DOC from more intensively managed, C‐poor soils is older, in some cases &gt;100 years. Results appear consistent with soil C destabilisation in farmed landscapes, but not in peatlands. Reported C losses may to a significant extent be explained by mechanisms other than climate change, e.g. recovery from acidification in peatlands, and agricultural intensification in managed systems.</jats:p>
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spelling Evans, Chris D. Freeman, Chris Cork, Lorna G. Thomas, David N. Reynolds, Brian Billett, Michael F. Garnett, Mark H. Norris, David 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2007gl029431 <jats:p>The stability of global soil carbon (C) represents a major uncertainty in forecasting future climate change. In the UK, substantial soil C losses have been reported, while at the same time dissolved organic carbon (DOC) concentrations in upland waters have increased, suggesting that soil C stocks may be destabilising in response to climate change. To investigate the link between soil carbon and DOC at a range of sites, soil organic matter, soilwater and streamwater DOC were analysed for radiocarbon (<jats:sup>14</jats:sup>C). DOC exported from C‐rich landscapes appears younger than the soil C itself, much of it comprising C assimilated post‐1950s. DOC from more intensively managed, C‐poor soils is older, in some cases &gt;100 years. Results appear consistent with soil C destabilisation in farmed landscapes, but not in peatlands. Reported C losses may to a significant extent be explained by mechanisms other than climate change, e.g. recovery from acidification in peatlands, and agricultural intensification in managed systems.</jats:p> Evidence against recent climate‐induced destabilisation of soil carbon from <sup>14</sup>C analysis of riverine dissolved organic matter Geophysical Research Letters
spellingShingle Evans, Chris D., Freeman, Chris, Cork, Lorna G., Thomas, David N., Reynolds, Brian, Billett, Michael F., Garnett, Mark H., Norris, David, Geophysical Research Letters, Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter, General Earth and Planetary Sciences, Geophysics
title Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_full Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_fullStr Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_full_unstemmed Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_short Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
title_sort evidence against recent climate‐induced destabilisation of soil carbon from <sup>14</sup>c analysis of riverine dissolved organic matter
title_unstemmed Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/2007gl029431