Articles | Volume 17, issue 20
https://doi.org/10.5194/bg-17-5163-2020
https://doi.org/10.5194/bg-17-5163-2020
Research article
 | 
26 Oct 2020
Research article |  | 26 Oct 2020

Thermokarst amplifies fluvial inorganic carbon cycling and export across watershed scales on the Peel Plateau, Canada

Scott Zolkos, Suzanne E. Tank, Robert G. Striegl, Steven V. Kokelj, Justin Kokoszka, Cristian Estop-Aragonés, and David Olefeldt

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Cited articles

Anderson, S. P.: Biogeochemistry of Glacial Landscape Systems, Annu. Rev. Earth Pl. Sc., 35(1), 375–399, https://doi.org/10.1146/annurev.earth.35.031306.140033, 2007. 
Beaulieu, E., Goddéris, Y., Donnadieu, Y., Labat, D., and Roelandt, C.: High sensitivity of the continental-weathering carbon dioxide sink to future climate change, Nat. Clim. Change, J2, 346–349, https://doi.org/10.1038/nclimate1419, 2012. 
Berner, R. A.: Weathering, plants, and the long-term carbon cycle, Geochim. Cosmochim. Ac., 56, 3225–3231, 1992. 
Berner, R. A.: A new look at the long-term carbon cycle, GSA Today, 9, 1–6, 1999. 
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Short summary
High-latitude warming thaws permafrost, exposing minerals to weathering and fluvial transport. We studied the effects of abrupt thaw and associated weathering on carbon cycling in western Canada. Permafrost collapse affected < 1 % of the landscape yet enabled carbonate weathering associated with CO2 degassing in headwaters and increased bicarbonate export across watershed scales. Weathering may become a driver of carbon cycling in ice- and mineral-rich permafrost terrain across the Arctic.
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