Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration
Ice core records show that the atmospheric concentration of methane (CH 4 ) during the Last Glacial Maximum (LGM) (~21,000 years ago) was 40% lower than the preindustrial Holocene. The contribution of natural wetlands to the global CH 4 budget during the LGM is determined by modelling their spatial...
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ftopenunivgb:oai:oro.open.ac.uk:32784 2023-06-11T04:12:43+02:00 Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration Boardman, C. Gauci, V. Beerling, D. 2008-12 https://oro.open.ac.uk/32784/ http://www.agu.org/cgi-bin/wais?mm=B11F-05 unknown Boardman, C. <http://oro.open.ac.uk/view/person/cpb247.html>; Gauci, V. <http://oro.open.ac.uk/view/person/vg8.html> and Beerling, D. (2008). Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration. In: American Geophysical Union, Fall Meeting 2008, 15-18 Dec 2008, San Francisco, USA. Conference or Workshop Item None PeerReviewed 2008 ftopenunivgb 2023-05-28T05:48:11Z Ice core records show that the atmospheric concentration of methane (CH 4 ) during the Last Glacial Maximum (LGM) (~21,000 years ago) was 40% lower than the preindustrial Holocene. The contribution of natural wetlands to the global CH 4 budget during the LGM is determined by modelling their spatial extent and productivity. Although models provide an estimated flux of ~75-180 Tg yr -1 , they adopt present day physiological relationships to reconstruct past wetland emissions. Here we show that the LGM (180 ppm) carbon dioxide (CO 2 ) concentration lowers CH 4 emissions from peat cores incubated in controlled environments compared to cores maintained under a modern atmospheric CO 2 concentration (380 ppm). Peat cores (110 x 400 mm) collected from a UK minerotrophic fen and upland ombrotrophic bog were maintained either in a [CO 2 ] of 180 ppm or 380 ppm over 21 months. CH 4 fluxes were measured on a monthly/weekly basis using static chambers with [CH 4 ] measured via an LGR Fast CH 4 Analyser and GC-FID. Results show that total CH 4 flux from the minerotrophic fen was suppressed by 17 and 31% in season 1 and 2 respectively under LGM CO 2 starvation. The ombrotrophic bog cores were suppressed by 20% in year 1 and 10% in year 2. Both peat types exhibited a rapid initial response to the sub-ambient [CO 2 ] treatment with a change in CH 4 flux recorded 5 days into the experiment. We also measured the influence of an LGM [CO 2 ] atmosphere on CH 4 flux temperature response during years 1 and 2. These results suggest that both wetland plants, and the underlying biogeochemistry of the rhizosphere, are sensitive to a reduction in [CO 2 ] in the atmosphere and this has yet to be incorporated into global wetland CH 4 models. Conference Object ice core The Open University: Open Research Online (ORO) Fid ENVELOPE(-65.939,-65.939,-68.664,-68.664) |
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The Open University: Open Research Online (ORO) |
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description |
Ice core records show that the atmospheric concentration of methane (CH 4 ) during the Last Glacial Maximum (LGM) (~21,000 years ago) was 40% lower than the preindustrial Holocene. The contribution of natural wetlands to the global CH 4 budget during the LGM is determined by modelling their spatial extent and productivity. Although models provide an estimated flux of ~75-180 Tg yr -1 , they adopt present day physiological relationships to reconstruct past wetland emissions. Here we show that the LGM (180 ppm) carbon dioxide (CO 2 ) concentration lowers CH 4 emissions from peat cores incubated in controlled environments compared to cores maintained under a modern atmospheric CO 2 concentration (380 ppm). Peat cores (110 x 400 mm) collected from a UK minerotrophic fen and upland ombrotrophic bog were maintained either in a [CO 2 ] of 180 ppm or 380 ppm over 21 months. CH 4 fluxes were measured on a monthly/weekly basis using static chambers with [CH 4 ] measured via an LGR Fast CH 4 Analyser and GC-FID. Results show that total CH 4 flux from the minerotrophic fen was suppressed by 17 and 31% in season 1 and 2 respectively under LGM CO 2 starvation. The ombrotrophic bog cores were suppressed by 20% in year 1 and 10% in year 2. Both peat types exhibited a rapid initial response to the sub-ambient [CO 2 ] treatment with a change in CH 4 flux recorded 5 days into the experiment. We also measured the influence of an LGM [CO 2 ] atmosphere on CH 4 flux temperature response during years 1 and 2. These results suggest that both wetland plants, and the underlying biogeochemistry of the rhizosphere, are sensitive to a reduction in [CO 2 ] in the atmosphere and this has yet to be incorporated into global wetland CH 4 models. |
format |
Conference Object |
author |
Boardman, C. Gauci, V. Beerling, D. |
spellingShingle |
Boardman, C. Gauci, V. Beerling, D. Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
author_facet |
Boardman, C. Gauci, V. Beerling, D. |
author_sort |
Boardman, C. |
title |
Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
title_short |
Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
title_full |
Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
title_fullStr |
Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
title_full_unstemmed |
Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
title_sort |
wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration |
publishDate |
2008 |
url |
https://oro.open.ac.uk/32784/ http://www.agu.org/cgi-bin/wais?mm=B11F-05 |
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ENVELOPE(-65.939,-65.939,-68.664,-68.664) |
geographic |
Fid |
geographic_facet |
Fid |
genre |
ice core |
genre_facet |
ice core |
op_relation |
Boardman, C. <http://oro.open.ac.uk/view/person/cpb247.html>; Gauci, V. <http://oro.open.ac.uk/view/person/vg8.html> and Beerling, D. (2008). Wetland methane emission response to last glacial maximum atmospheric carbon dioxide concentration. In: American Geophysical Union, Fall Meeting 2008, 15-18 Dec 2008, San Francisco, USA. |
_version_ |
1768388766593974272 |