Articles | Volume 15, issue 21
https://doi.org/10.5194/bg-15-6637-2018
https://doi.org/10.5194/bg-15-6637-2018
Research article
 | 
08 Nov 2018
Research article |  | 08 Nov 2018

Spatiotemporal transformation of dissolved organic matter along an alpine stream flow path on the Qinghai–Tibet Plateau: importance of source and permafrost degradation

Yinghui Wang, Robert G. M. Spencer, David C. Podgorski, Anne M. Kellerman, Harunur Rashid, Phoebe Zito, Wenjie Xiao, Dandan Wei, Yuanhe Yang, and Yunping Xu

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (24 Aug 2018) by Luo Yu
AR by Yunping Xu on behalf of the Authors (30 Aug 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (03 Sep 2018) by Luo Yu
RR by Anonymous Referee #1 (17 Sep 2018)
RR by Anonymous Referee #3 (24 Sep 2018)
ED: Reject (28 Sep 2018) by Luo Yu
ED: Publish subject to minor revisions (review by editor) (13 Oct 2018) by Steven Bouillon
AR by Yunping Xu on behalf of the Authors (24 Oct 2018)  Author's response   Manuscript 
ED: Publish as is (26 Oct 2018) by Steven Bouillon
AR by Yunping Xu on behalf of the Authors (26 Oct 2018)
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Short summary
With global warming, thawing of permafrost releases dissolved organic matter (DOM) into streams. By analyzing DOM along an alpine stream on the Qinghai–Tibet Plateau, we found DOM was mainly from the active layer, but with deepening of the active layer, the contribution of the deep permafrost layer increased, causing a change in the chemical composition of DOM. From the head- to downstream, DOM is undergoing rapid degradation, but some components are persistent and can be transported downstream.
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