Global vulnerability of peatlands to fire and carbon loss

The amount of carbon stored in peats exceeds that stored in vegetation. A synthesis of the literature suggests that smouldering fires in peatlands could become more common as the climate warms, and release old carbon to the air. Globally, the amount of carbon stored in peats exceeds that stored in v...

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Veröffentlicht in:	Nature geoscience Jg. 8; H. 1; S. 11 - 14
Hauptverfasser:	Turetsky, Merritt R., Benscoter, Brian, Page, Susan, Rein, Guillermo, van der Werf, Guido R., Watts, Adam
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	London Nature Publishing Group UK 01.01.2015 Nature Publishing Group
Schlagworte:	704/106/47 704/106/694/2739 704/158/2465 704/172/169 Carbon cycle Carbon sequestration Climate change Combustion Earth Sciences Earth System Sciences Fires Geochemistry Geology Geophysics/Geodesy Peat Peatlands progress-article Tropical environments Water table
ISSN:	1752-0894, 1752-0908
Online-Zugang:	Volltext
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Abstract	The amount of carbon stored in peats exceeds that stored in vegetation. A synthesis of the literature suggests that smouldering fires in peatlands could become more common as the climate warms, and release old carbon to the air. Globally, the amount of carbon stored in peats exceeds that stored in vegetation and is similar in size to the current atmospheric carbon pool. Fire is a threat to many peat-rich biomes and has the potential to disturb these carbon stocks. Peat fires are dominated by smouldering combustion, which is ignited more readily than flaming combustion and can persist in wet conditions. In undisturbed peatlands, most of the peat carbon stock typically is protected from smouldering, and resistance to fire has led to a build-up of peat carbon storage in boreal and tropical regions over long timescales. But drying as a result of climate change and human activity lowers the water table in peatlands and increases the frequency and extent of peat fires. The combustion of deep peat affects older soil carbon that has not been part of the active carbon cycle for centuries to millennia, and thus will dictate the importance of peat fire emissions to the carbon cycle and feedbacks to the climate.
AbstractList	The amount of carbon stored in peats exceeds that stored in vegetation. A synthesis of the literature suggests that smouldering fires in peatlands could become more common as the climate warms, and release old carbon to the air. Globally, the amount of carbon stored in peats exceeds that stored in vegetation and is similar in size to the current atmospheric carbon pool. Fire is a threat to many peat-rich biomes and has the potential to disturb these carbon stocks. Peat fires are dominated by smouldering combustion, which is ignited more readily than flaming combustion and can persist in wet conditions. In undisturbed peatlands, most of the peat carbon stock typically is protected from smouldering, and resistance to fire has led to a build-up of peat carbon storage in boreal and tropical regions over long timescales. But drying as a result of climate change and human activity lowers the water table in peatlands and increases the frequency and extent of peat fires. The combustion of deep peat affects older soil carbon that has not been part of the active carbon cycle for centuries to millennia, and thus will dictate the importance of peat fire emissions to the carbon cycle and feedbacks to the climate. Globally, the amount of carbon stored in peats exceeds that stored in vegetation and is similar in size to the current atmospheric carbon pool. Fire is a threat to many peat-rich biomes and has the potential to disturb these carbon stocks. Peat fires are dominated by smouldering combustion, which is ignited more readily than flaming combustion and can persist in wet conditions. In undisturbed peatlands, most of the peat carbon stock typically is protected from smouldering, and resistance to fire has led to a build-up of peat carbon storage in boreal and tropical regions over long timescales. But drying as a result of climate change and human activity lowers the water table in peatlands and increases the frequency and extent of peat fires. The combustion of deep peat affects older soil carbon that has not been part of the active carbon cycle for centuries to millennia, and thus will dictate the importance of peat fire emissions to the carbon cycle and feedbacks to the climate.
Author	van der Werf, Guido R. Rein, Guillermo Page, Susan Turetsky, Merritt R. Benscoter, Brian Watts, Adam
Author_xml	– sequence: 1 givenname: Merritt R. surname: Turetsky fullname: Turetsky, Merritt R. email: mrt@uoguelph.ca organization: Department of Integrative Biology, University of Guelph – sequence: 2 givenname: Brian surname: Benscoter fullname: Benscoter, Brian organization: Department of Biological Sciences, Florida Atlantic University – sequence: 3 givenname: Susan surname: Page fullname: Page, Susan organization: Department of Geography, University of Leicester – sequence: 4 givenname: Guillermo surname: Rein fullname: Rein, Guillermo organization: Department of Mechanical Engineering, Imperial College London – sequence: 5 givenname: Guido R. surname: van der Werf fullname: van der Werf, Guido R. organization: Faculty of Earth and Life Sciences, VU University Amsterdam – sequence: 6 givenname: Adam surname: Watts fullname: Watts, Adam organization: Division of Atmospheric Sciences, Desert Research Institute
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Snippet	The amount of carbon stored in peats exceeds that stored in vegetation. A synthesis of the literature suggests that smouldering fires in peatlands could become... Globally, the amount of carbon stored in peats exceeds that stored in vegetation and is similar in size to the current atmospheric carbon pool. Fire is a...
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SubjectTerms	704/106/47 704/106/694/2739 704/158/2465 704/172/169 Carbon cycle Carbon sequestration Climate change Combustion Earth Sciences Earth System Sciences Fires Geochemistry Geology Geophysics/Geodesy Peat Peatlands progress-article Tropical environments Water table
Title	Global vulnerability of peatlands to fire and carbon loss
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