School of Environment, Earth and Ecosystem Sciences, The Open University, Milton Keynes, MK7 6AA, UK
Organic Geochemistry Unit, The Cabot Institute, School of Chemistry, School of Earth Sciences, The University of Bristol, Bristol, BS8 1TH, UK
Bristol Research Initiative for the Dynamic Global Environment (BRIDGE), The Cabot Institute, School of Geographical Sciences, The University of Bristol, BS8 1TH, UK
Bristol Research Initiative for the Dynamic Global Environment (BRIDGE), The Cabot Institute, School of Geographical Sciences, The University of Bristol, BS8 1TH, UK
David J. Beerling
Department of Animal and Plant Sciences, The University of Sheffield, Sheffield, S10 2TN, UK
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Total article views: 1,704 (including HTML, PDF, and XML)
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1,180
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1,704
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PDF: 472
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Supplement: 119
BibTeX: 69
EndNote: 60
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448
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Total article views: 2,405 (including HTML, PDF, and XML)
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Total article views: 1,704 (including HTML, PDF, and XML)
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Total article views: 701 (including HTML, PDF, and XML)
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Methane is an important greenhouse gas naturally produced in wetlands (areas of land inundated with water). Models of the Earth's past climate need estimates of the amounts of methane wetlands produce; and in order to calculate those we need to model wetlands. In this work we develop a method for modelling the fraction of an area of the Earth that is wetland, repeat this over all the Earth's land surface and apply this to a study of the Earth as it was around 50 million years ago.
Methane is an important greenhouse gas naturally produced in wetlands (areas of land inundated...
