Articles | Volume 14, issue 18
https://doi.org/10.5194/bg-14-4229-2017
https://doi.org/10.5194/bg-14-4229-2017
Research article
 | 
21 Sep 2017
Research article |  | 21 Sep 2017

Biogeochemical cycling at the aquatic–terrestrial interface is linked to parafluvial hyporheic zone inundation history

Amy E. Goldman, Emily B. Graham, Alex R. Crump, David W. Kennedy, Elvira B. Romero, Carolyn G. Anderson, Karl L. Dana, Charles T. Resch, Jim K. Fredrickson, and James C. Stegen

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Status: closed
Status: closed
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: Publish subject to minor revisions (Editor review) (27 Jun 2017) by Clare Woulds
AR by Amy Goldman on behalf of the Authors (07 Jul 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (01 Aug 2017) by Clare Woulds
AR by Amy Goldman on behalf of the Authors (15 Aug 2017)  Author's response    Manuscript
ED: Publish as is (23 Aug 2017) by Clare Woulds
AR by Amy Goldman on behalf of the Authors (28 Aug 2017)  Author's response    Manuscript
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Short summary
The history of river inundation influences shoreline sediment biogeochemical cycling and microbial dynamics. Sediment exhibited a binary respiration response to rewetting, in which respiration from less recently saturated sediment was suppressed relative to more recently saturated sediment, likely due to inhibition of fungal metabolic activity. River shorelines should likely be integrated as a distinct environment into hydrobiogeochemical models to predict watershed biogeochemical function.
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