Permafrost collapse after shrub removal shifts tundra ecosystem to a methane source

• Published in: Nature climate change Vol. 5; no. 1; pp. 67 - 70
• Main Authors: Nauta, Ake L., Heijmans, Monique M. P. D., Blok, Daan, Limpens, Juul, Elberling, Bo, Gallagher, Angela, Li, Bingxi, Petrov, Roman E., Maximov, Trofim C., van Huissteden, Jacobus, Berendse, Frank
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 01-01-2015; Nature Publishing Group
• Subjects: 631/158/2165; 704/106/125; 704/158/2445; alaska; arctic tundra; Climate Change; Climate Change/Climate Change Impacts; Climatic conditions; Collapse; Ecosystems; Environment; Environmental Law/Policy/Ecojustice; expansion; Global warming; Greenhouse gases; ice; letter; Methane; Organic carbon; Permafrost; thaw; Thawing; Tundra; Vegetation changes; Vegetation cover; Woody plants; Russia, Siberia; PN, Arctic
• ISSN: 1758-678X; 1758-6798
• DOI: 10.1038/nclimate2446

The release of carbon from decomposing Arctic soils, following permafrost thaw, is a potentially important climate feedback. Research now shows how shrub cover protects permafrost carbon reservoirs. Manipulative experiments show that the loss of shrub cover leads to a transition of the tundra to waterlogged methane-emitting conditions.
Arctic tundra ecosystems are warming almost twice as fast as the global average
1
. Permafrost thaw and the resulting release of greenhouse gases from decomposing soil organic carbon have the potential to accelerate climate warming
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,
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. In recent decades, Arctic tundra ecosystems have changed rapidly
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, including expansion of woody vegetation
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,
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, in response to changing climate conditions. How such vegetation changes contribute to stabilization or destabilization of the permafrost is unknown. Here we present six years of field observations in a shrub removal experiment at a Siberian tundra site. Removing the shrub part of the vegetation initiated thawing of ice-rich permafrost, resulting in collapse of the originally elevated shrub patches into waterlogged depressions within five years. This thaw pond development shifted the plots from a methane sink into a methane source. The results of our field experiment demonstrate the importance of the vegetation cover for protection of the massive carbon reservoirs stored in the permafrost and illustrate the strong vulnerability of these tundra ecosystems to perturbations. If permafrost thawing can more frequently trigger such local permafrost collapse, methane-emitting wet depressions could become more abundant in the lowland tundra landscape, at the cost of permafrost-stabilizing low shrub vegetation.