Articles | Volume 22, issue 12
https://doi.org/10.5194/bg-22-2871-2025
https://doi.org/10.5194/bg-22-2871-2025
Research article
 | 
20 Jun 2025
Research article |  | 20 Jun 2025

Organic carbon, mercury, and sediment characteristics along a land–shore transect in Arctic Alaska

Frieda P. Giest, Maren Jenrich, Guido Grosse, Benjamin M. Jones, Kai Mangelsdorf, Torben Windirsch, and Jens Strauss

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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 egusphere-2024-3683', Anonymous Referee #1, 07 Feb 2025
    • AC1: 'Reply on RC1', Jens Strauss, 23 Mar 2025
  • RC2: 'Comment on egusphere-2024-3683', Anonymous Referee #2, 12 Feb 2025
    • AC2: 'Reply on RC2', Jens Strauss, 23 Mar 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (24 Mar 2025) by Sebastian Naeher
AR by Jens Strauss on behalf of the Authors (26 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (31 Mar 2025) by Sebastian Naeher
AR by Jens Strauss on behalf of the Authors (31 Mar 2025)
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Short summary
Climate warming causes permafrost to thaw, releasing greenhouse gases and affecting ecosystems. We studied sediments from Arctic coastal landscapes, including land, lakes, lagoons, and the ocean, finding that organic carbon storage and quality vary with landscape features and saltwater influence. Freshwater and land areas store more carbon, while saltwater reduces its quality. These findings improve predictions of Arctic responses to climate change and their impact on global carbon cycling.
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