Articles | Volume 10, issue 3
https://doi.org/10.5194/esurf-10-421-2022
https://doi.org/10.5194/esurf-10-421-2022
Research article
 | 
10 May 2022
Research article |  | 10 May 2022

Organic carbon burial by river meandering partially offsets bank erosion carbon fluxes in a discontinuous permafrost floodplain

Madison M. Douglas, Gen K. Li, Woodward W. Fischer, Joel C. Rowland, Preston C. Kemeny, A. Joshua West, Jon Schwenk, Anastasia P. Piliouras, Austin J. Chadwick, and Michael P. Lamb

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on esurf-2021-80', Jordon Hemingway, 10 Dec 2021
  • RC2: 'Comment on esurf-2021-80', Anonymous Referee #2, 22 Dec 2021
  • AC1: 'Comment on esurf-2021-80', Madison Douglas, 18 Mar 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Madison Douglas on behalf of the Authors (18 Mar 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Mar 2022) by Robert Hilton
RR by Jordon Hemingway (30 Mar 2022)
ED: Publish subject to technical corrections (12 Apr 2022) by Robert Hilton
ED: Publish subject to technical corrections (12 Apr 2022) by Andreas Lang (Editor)
AR by Madison Douglas on behalf of the Authors (14 Apr 2022)  Author's response   Manuscript 
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Short summary
Arctic rivers erode into permafrost and mobilize organic carbon, which can react to form greenhouse gasses or be re-buried in floodplain deposits. We collected samples on a permafrost floodplain in Alaska to determine if more carbon is eroded or deposited by river meandering. The floodplain contained a mixture of young carbon fixed by the biosphere and old, re-deposited carbon. Thus, sediment storage may allow Arctic river floodplains to retain aged organic carbon even when permafrost thaws.