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Evidence against recent climate‐induced destabilisation of soil carbon from 14C analysis of riverine dissolved organic matter
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Zeitschriftentitel: | Geophysical Research Letters |
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Personen und Körperschaften: | , , , , , , , |
In: | Geophysical Research Letters, 34, 2007, 7 |
Format: | E-Article |
Sprache: | Englisch |
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American Geophysical Union (AGU)
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Schlagwörter: |
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 |
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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 |
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 >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 |
doi_str_mv |
10.1029/2007gl029431 |
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American Geophysical Union (AGU), 2007 |
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American Geophysical Union (AGU), 2007 |
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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 >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. |
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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 >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 >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 |