nerc.ac.uk

Abundant pre-industrial carbon detected in Canadian Arctic headwaters: implications for the permafrost carbon feedback

Dean, J.F.; van der Velde, Y.; Garnett, M.H.; Dinsmore, K.J.; Baxter, R.; Lessels, J.S.; Smith, P.; Street, L.E.; Subke, J.-A.; Tetzlaff, D.; Washbourne, I.; Wookey, P. A.; Billett, M.F.. 2018 Abundant pre-industrial carbon detected in Canadian Arctic headwaters: implications for the permafrost carbon feedback. Environmental Research Letters, 13 (3), 034024. 11, pp. 10.1088/1748-9326/aaa1fe

Before downloading, please read NORA policies.
[thumbnail of N519131JA.pdf]
Preview
Text
N519131JA.pdf - Published Version
Available under License Creative Commons Attribution.

Download (2MB) | Preview

Abstract/Summary

Mobilization of soil/sediment organic carbon into inland waters constitutes a substantial, but poorly-constrained, component of the global carbon cycle. Radiocarbon (14C) analysis has proven a valuable tool in tracing the sources and fate of mobilized carbon, but aquatic 14C studies in permafrost regions rarely detect ‘old’ carbon (assimilated from the atmosphere into plants and soil prior to AD1950). The emission of greenhouse gases derived from old carbon by aquatic systems may indicate that carbon sequestered prior to AD1950 is being destabilized, thus contributing to the ‘permafrost carbon feedback’ (PCF). Here, we measure directly the 14C content of aquatic CO2, alongside dissolved organic carbon, in headwater systems of the western Canadian Arctic – the first such concurrent measurements in the Arctic. Age distribution analysis indicates that the age of mobilized aquatic carbon increased significantly during the 2014 snow-free season as the active layer deepened. This increase in age was more pronounced in DOC, rising from 101 to 228 years before sampling date (a 120-125% increase) compared to CO2, which rose from 92 to 151 years before sampling date (a 59-63% increase). ‘Pre-industrial’ aged carbon (assimilated prior to ~AD1750) comprised 15-40% of the total aquatic carbon fluxes,demonstrating the prevalence of old carbon to Arctic headwaters. Although the presence of this old carbon is not necessarily indicative of a net positive PCF, we provide an approach and baseline data which can be used for future assessment of the PCF.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1088/1748-9326/aaa1fe
UKCEH and CEH Sections/Science Areas: Atmospheric Chemistry and Effects (Science Area 2017-)
ISSN: 1748-9326
Additional Information. Not used in RCUK Gateway to Research.: Open Access paper - full text available via Official URL link.
Additional Keywords: carbon dioxide (CO2), dissolved organic carbon (DOC), methane (CH4), Arctic catchments, inland waters, radiocarbon (14C)
NORA Subject Terms: Ecology and Environment
Agriculture and Soil Science
Atmospheric Sciences
Date made live: 29 Jan 2018 16:30 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/519131

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...