Cookies

We use cookies to ensure that we give you the best experience on our website. By continuing to browse this repository, you give consent for essential cookies to be used. You can read more about our Privacy and Cookie Policy.


Durham Research Online
You are in:

Erosion of organic carbon in the Arctic as a geological carbon dioxide sink.

Hilton, R.G. and Galy, V. and Gaillardet, J. and Dellinger, M. and Bryant, C. and O’Regan, M. and Gröcke, D.R. and Coxall, H. and Bouchez, J. and Calmels, D. (2015) 'Erosion of organic carbon in the Arctic as a geological carbon dioxide sink.', Nature., 524 (7563). pp. 84-87.

Abstract

Soils of the northern high latitudes store carbon over millennial timescales (thousands of years) and contain approximately double the carbon stock of the atmosphere1, 2, 3. Warming and associated permafrost thaw can expose soil organic carbon and result in mineralization and carbon dioxide (CO2) release4, 5, 6. However, some of this soil organic carbon may be eroded and transferred to rivers7, 8, 9. If it escapes degradation during river transport and is buried in marine sediments, then it can contribute to a longer-term (more than ten thousand years), geological CO2 sink8, 9, 10. Despite this recognition, the erosional flux and fate of particulate organic carbon (POC) in large rivers at high latitudes remains poorly constrained. Here, we quantify the source of POC in the Mackenzie River, the main sediment supplier to the Arctic Ocean11, 12, and assess its flux and fate. We combine measurements of radiocarbon, stable carbon isotopes and element ratios to correct for rock-derived POC10, 13, 14. Our samples reveal that the eroded biospheric POC has resided in the basin for millennia, with a mean radiocarbon age of 5,800 ± 800 years, much older than the POC in large tropical rivers13, 14. From the measured biospheric POC content and variability in annual sediment yield15, we calculate a biospheric POC flux of teragrams of carbon per year from the Mackenzie River, which is three times the CO2 drawdown by silicate weathering in this basin16. Offshore, we find evidence for efficient terrestrial organic carbon burial over the Holocene period, suggesting that erosion of organic carbon-rich, high-latitude soils may result in an important geological CO2 sink.

Item Type:Article
Full text:(AM) Accepted Manuscript
Download PDF
(2675Kb)
Status:Peer-reviewed
Publisher Web site:http://dx.doi.org/10.1038/nature14653
Date accepted:03 June 2015
Date deposited:13 October 2015
Date of first online publication:05 August 2015
Date first made open access:No date available

Save or Share this output

Export:
Export
Look up in GoogleScholar