Articles | Volume 13, issue 4
https://doi.org/10.5194/bg-13-1237-2016
https://doi.org/10.5194/bg-13-1237-2016
Research article
 | 
01 Mar 2016
Research article |  | 01 Mar 2016

Thermo-erosion gullies boost the transition from wet to mesic tundra vegetation

Naïm Perreault, Esther Lévesque, Daniel Fortier, and Laurent J. Lamarque

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Cited articles

Akerman, H. J. and Johansson, M.: Thawing permafrost and thicker active layer in sub-arctic Sweden, Permafrost Periglac., 19, 279–292, 2008.
Allard, M.: Geomorphological changes and permafrost dynamics: key factors in changing arctic ecosystems, An example from Bylot Island, Nunavut, Canada, Geosci. Can., 23, 205–212, 1996.
Audet, B., Lévesque, E., and Gauthier G.: Seasonal variation in plant nutritive quality for Greater Snow Goose goslings in mesic tundra, Can. J. Bot., 85, 457–462, 2007.
Avis, C. A., Weaver, A. J., and Meissner, K. J.: Reduction in areal extent of high-latitude wetlands in response to permafrost thaw, Nat. Geosci., 4, 444–448, 2011.
Beck, I., Ludwig, R., Bernier, M., Lévesque, E., and Boike, J.: Assessing permafrost degradation and land cover changes (1986–2009) using remote sensing data over Umiujaq, sub-Arctic Québec, Permafrost Periglac., 26, 129–141, https://doi.org/10.1002/ppp.1839, 2015.
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Short summary
We investigated the impacts of climate change and thawing permafrost on vegetation dynamics in Bylot Island, Nunavut. The development of gullies has created new drainage systems within the wetlands, promoting the emergence of mesic plants at the expense of hydrophilic ones within 10 years after disturbance inception. The landscape transformation from wet to mesic plant communities can have substantial consequences on food availability for herbivores and methane emissions of Arctic ecosystems.
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